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H6!9&5 (fJ6/a | ѵ;kUQU_.lHÉGx| ;wX[[8lv<4x ւM#. /}#1%3sxyώ7|C.,b׽ YZ~ЎO꤮8s3   ;gjl:p'l [N/`il|Uj~9 پCd=~Ezhtx-iSSj٭+̵jUv^4)oGt N/F.!5Q?Wz6x!tyxaQǷc/ b F6HP LaserJet 4100 PCL 6HP LaserJet 4100 PCL 6IM_HP_LJ4100DTNd2" @ Tahomahg#h%" @ Tahoma`,  Detailx &bqSIa:. d5U7`6ab c,d#  Label0 "Verify Veg Stratax zc#yMT4 h1U`6 aTb buttonStrata "Verify Veg Strata~ "[Event Procedure]x \F2sjC<㥁h1U`6aTbi Command4 (Verify AA Veg Strata~ "[Event Procedure]x ڪe)9H-#)h1U`6 apbi Command5 2Verify Vegetation Details~ "[Event Procedure]x T87H& ADOBo *\G{020 1-10-8 AA006D2EA4}#2.1#0#C:\Program Files\Common System\ado\ms21.tlb#Microsoft ActiveX Data Objects , LibraryH\OWC10\OWC10\A\2E550U0C\46}0#1.0\JOf fice\12\OFF>.DLL] XP Web {ponentsEӀstdole>stdole@-h^QE-043\-2E-WINDOWS\sQW32\C2VOLE Autom`ation@DAO>%DAO  5E|@ON5N|GQShared\\dao360.dllPa 3.6}K|}@*Form_frmVerifyStr@G(AVrm_fVYri@yS^raA@a@ JJQPHMFJSXVVNDSIHNYKIAONR@VVB28AJQPHMFSXV@NSI`NYK@RNRBBB@S@Sa,1"" +bͬ" fraERj$Detaild Label0h buttonStratah Command4h Command5h Command6h ButtonAADetailsh ButtonPlotsNulld Label10d Label11h Command12LVAL4 8 Mn}xME PS<S<S<< <<<<Xe dN0{7266871D-9A1B-4561-AA94-EFDDE8526A24}P m X % x% "%`$?`&`(Rj$`*ec`, hA p % %`$`& [   % @% "`%`$`&`(`*`, f 8 % X% "x%`$`&`(`*`, 8 W  % % "%`$`& M ` % %`$`& i@%' "  (08 @HP X    (8 @Pjh d@ ,Hxj bpxj dpxj fpxj `hpxj fhp *x  vH  j dh    j  `h    j  ``    j  dX    j  fX    j  `Xj dP     0 8"@h p "x   8 HX  p *Z(*0X`*\P*X\*LVALX x*^*\H*`@*H^x*Vh*pZ  ( 0 @ HX `"h  "        l fl dl fl hl bl h l  h   !l! f!!!"l" h"""#l# b###$l$ f$$$ %% % (% 8% @%P% X%"`%% %"%% %%%%% %%%  %R&  P(`( x( (( ((L( Z)x)))J) X)H*P*X*Jp* \* +(+0+LH+ \++,,L , Xp,,,,L, ^@----J- \.x...J. V.H/P/X/Jp/ V/0 0(0L@0 `0001L1 ^h1111J1 V@2222J2 Z3p3x3 333 3 3 33 3"34  4"4 4  (4 84@4 H4P4`4 h4 "p4x4 44444 P4  56 6 06@6 H6X6Np6 \6 7(707LH7 Z7788L 8 ^p8888N8 ^H9999N9 Z ::::N: `:X;`;h;N; ^;0<8<@<JX< b<== =N8= `=== (= l > h> > ? ((? jP? l? 0@ H@ `@p@@ @ @ @@ @"@@  @"@A AAA A LVAL(A A AA  AB B* BXPBB*BVB8C*@CZpCC*CZDhD*pDVDD*E\0EE*EZE(F*0FZ`FF*FTFPG*XGTGG*G^HxH*H\HI*ITHII*IXI0J  8JHJXJ `J pJ J JJ J"JJ  J " J JKKxh]@]`]]]]]]SELECT tblPlotDetails.PlotCode, tblVegetation.* FROM tblPlotDetails INNER JOIN tblVegetation ON tblPlotDetails.PlotID = tblVegetation.PlotID'.et 0B@2i 4. . %6. B@8olb'& !:a_EG ">$<eta [VegDetailID]tblVegetationDetails$[Stratum] = 'T1' And VegetationID = "B$@$<S\CPlot "FC, stratum Emergent has no corresponding tblVegetationDetail record.A@Dk& Cover_Class = Strata!EmergCovTotk "H$< [VegDetailID]tblVegetationDetails$[Stratum] = 'T2' And VegetationID = "B$@$<Plot "FA, stratum Canopy has no corresponding tblVegetationDetail record.A@Dkk "J$< [VegDetailID]tblVegetationDetails$[Stratum] = 'T3' And VegetationID = "B$@$<Plot "FD, stratum Subcanopy has no corresponding tblVegetationDetail record.A@DkHk@ "L$< [VegDetailID]tblVegetationDetails$[Stratum] = 'S1' And VegetationID = "B$@$<Plot "FE, stratum Tall Shrub has no corresponding tblVegetationDetail record.A@DkHk@ "N$< [VegDetailID]tblVegetationDetails$[Stratum] = 'S2' And VegetationID = "B$@$<Plot "F@, stratum Shrub has no corresponding tblVegetationDetail record.A@DkPkH "P$< [VegDetailID]tblVegetationDetails$[Stratum] = 'S3' And VegetationID = "B$@$<Plot "FF, stratum Dwarf Shrub has no corresponding tblVegetationDetail record.A@DkPkH# If Not IsNull(Strata!HerbHt) Then If IsNull(DLookup("[VegDetailID]", "tblVegetationDetails", "([Stratum] = 'Ht' Or [Stratum] = 'H') And VegetationID = " & Strata!VegetationID)) Thenp MsgBox "Plot " & Strata!Plotcode & ", stratum Herbaceous has no corresponding tblVegetationDetail record." End If End If "R$< [VegDetailID]tblVegetationDetails$[Stratum] = 'H1' And VegetationID = "B$@$<Plot "FD, stratum Graminoid has no corresponding tblVegetationDetail record.A@Dkk "T$< [VegDetailID]tblVegetationDetails$[Stratum] = 'H2' And VegetationID = "B$@$<Plot "F?, stratum Forb has no corresponding tblVegetationDetail record.A@Dkk "V$< [VegDetailID]tblVegetationDetails$[Stratum] = 'H3' And VegetationID = "B$@$<Plot "F?, stratum Fern has no corresponding tblVegetationDetail record.A@Dkk "X$< [VegDetailID]tblVegetationDetails$[Stratum] = 'H4' And VegetationID = "B$@$<Plot "FC, stratum SLVALeedling has no corresponding tblVegetationDetail record.A@Dkk "Z$< [VegDetailID]tblVegetationDetails#[Stratum] = 'N' And VegetationID = "B$@$<Plot "FF, stratum Nonvascular has no corresponding tblVegetationDetail record.A@Dkk "\$< [VegDetailID]tblVegetationDetails#[Stratum] = 'V' And VegetationID = "B$@$<Plot "F?, stratum Vine has no corresponding tblVegetationDetail record.A@Dkk "^$< [VegDetailID]tblVegetationDetails#[Stratum] = 'E' And VegetationID = "B$@$<Plot "FC, stratum Epiphyte has no corresponding tblVegetationDetail record.A@Dkk B@` & '& B@B DoCmd.Closeb` 0B@2|H@ d!f Record  &A@Dbo]X]x]]SELECT tblAADetails.AACode, tblAAVegetation.* FROM tblAADetails INNER JOIN tblAAVegetation ON tblAADetails.AAID = tblAAVegetation.AAID'. 0B@2 4. . %6. B@8'& !:a ">$< "j$< Plot "l:, stratum Emergent has mismatched null in tblAAVegetation.A@Dk "H$< "n$< Plot "l8, stratum Canopy has mismatched null in tblAAVegetation.A@Dk@ "J$< "p$< Plot "l;, stratum Subcanopy has mismatched null in tblAAVegetation.A@Dk "L$< "r$< Plot "l<, stratum Tall Shrub has mismatched null in tblAAVegetation.A@Dk "N$< "t$< Plot "l7, stratum Shrub has mismatched null in tblAAVegetation.A@Dk "P$< "v$< Plot "l=, stratum Dwarf Shrub has mismatched null in tblAAVegetation.A@Dk "x$< "z$< Plot "l<, stratum Herbaceous has mismatched null in tblAAVegetation.A@DkP "|$< "~$< Plot "l?, stratum Tree Seedling has mismatched null in tblAAVegetation.A@Dk "Z$< "$< Plot "l>, stratum Non-Vascular has mismatched null in tblAAVegetation.A@Dk "\$< "$< Plot "l6, stratum Vine has mismatched null in tblAAVegetation.A@Dk "^$< "$< Plot "l:, stratum Epiphyte has mismatched null in tblAAVegetation.A@Dk B@` & '& B@Bb 0B@2|  d!f Record  &A@Dbh o` P ]](]H]h]]]]SELECT tblAADetails.AACode, tblAAVegetation.* FROM tblAADetails INNER JOIN tblAAVegetation ON tblAADetails.AAID = tblAAVegetation.AAID order by tblAAVegetation.AAID'. 4. . %6. 0B@2 B@8'& !:a ">$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'T1' And VegetationID = "B$@$<Plot "lE, stratum Emergent has no corresponding tblAAVegetationDetail record.A@Dkk "H$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'T2' And VegetationID = "B$@$<Plot "lC, stratum Canopy has no corresponding tblAAVegetationDetail record.A@Dkk "J$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'T3' And VegetaLVALtionID = "B$@$<Plot "lF, stratum Subcanopy has no corresponding tblAAVegetationDetail record.A@Dkk "L$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'S1' And VegetationID = "B$@$<Plot "lG, stratum Tall Shrub has no corresponding tblAAVegetationDetail record.A@Dkk "N$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'S2' And VegetationID = "B$@$<Plot "lB, stratum Shrub has no corresponding tblAAVegetationDetail record.A@Dkk "P$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'S3' And VegetationID = "B$@$<Plot "lH, stratum Dwarf Shrub has no corresponding tblAAVegetationDetail record.A@Dkk "x$< [VegDetailID]tblAAVegetationDetails#[Stratum] = 'H' And VegetationID = "B$@$<Plot "lG, stratum Herbaceous has no corresponding tblAAVegetationDetail record.A@Dkk "|$< [VegDetailID]tblAAVegetationDetails$[Stratum] = 'H4' And VegetationID = "B$@$<Plot "lE, stratum Seedling has no corresponding tblAAVegetationDetail record.A@Dkk "Z$< [VegDetailID]tblAAVegetationDetails#[Stratum] = 'N' And VegetationID = "B$@$<Plot "lH, stratum Nonvascular has no corresponding tblAAVegetationDetail record.A@Dkk "\$< [VegDetailID]tblAAVegetationDetails#[Stratum] = 'V' And VegetationID = "B$@$<Plot "lA, stratum Vine has no corresponding tblAAVegetationDetail record.A@Dk"k" "^$< [VegDetailID]tblAAVegetationDetails#[Stratum] = 'E' And VegetationID = "B$@$<Plot "lE, stratum Epiphyte has no corresponding tblAAVegetationDetail record.A@Dk!k! B@` & '& B@B 0B@2|  d!f Record  &A@Dp oh X ] ]@]`]]]]] strSQL = "SELECT tblPlotDetails.PlotCode, tblVegetationDetails.* FROM tblPlotDetails RIGHT JOIN (tblVegetation RIGHT JOIN tblVegetationDetails ON tblVegetation.VegetationID = tblVegetationDetails.VegetationID) ON tblPlotDetails.PlotID = tblVegetation.PlotID"JSELECT DISTINCT tblPlotDetails.PlotCode, tblVegetationDetails.Stratum, tblVegetationDetails.VegetationID FROM tblPlotDetails RIGHT JOIN (tblVegetation RIGHT JOIN tblVegetationDetails ON tblVegetation.VegetationID = tblVegetationDetails.VegetationID) ON tblPlotDetails.PlotID = tblVegetation.PlotID ORDER BY tblPlotDetails.PlotCode'$ 4. $ %6. 0B@2 B@8'& !:a ",T1 [EmergHt] tblVegetationVegetationID = "B$@$<Plot "F:, stratum T1 has no Emergent cover class in tblVegetation.A@Dkkx ",T2[CanHt] tblVegetationVegetationID = "B$@$<Plot "F8, stratum T2 has no Canopy cover class in tblVegetation.A@Dkk ",T3[SubHt] tblVegetationVegetationID = "B$@$<Plot "F;, stratum T3 has no Subcanopy cover class in tblVegetation.A@Dkk ",S1 [TallShHt] tblVegetationVegetationID = "B$@$<Plot "F<, stratum S1 has no Tall Shrub cover class in tblVegetation.A@Dkk ",S2 [ShrubHt] tblVegetationVegetatLVAL ionID = "B$@$<Plot "F7, stratum S2 has no Shrub cover class in tblVegetation.A@Dk0k( ",S3 [DwarfHt] tblVegetationVegetationID = "B$@$<Plot "F=, stratum S3 has no Dwarf Shrub cover class in tblVegetation.A@DkXkP ",H1[GramHt] tblVegetationVegetationID = "B$@$<Plot "F;, stratum H1 has no Graminoid cover class in tblVegetation.A@Dkkx ",H2[ForbHt] tblVegetationVegetationID = "B$@$<Plot "F6, stratum H2 has no Forb cover class in tblVegetation.A@Dkk ",H3[FernHt] tblVegetationVegetationID = "B$@$<Plot "F6, stratum H3 has no Fern cover class in tblVegetation.A@Dkk ",H4 [SeedlHt] tblVegetationVegetationID = "B$@$<Plot "F?, stratum H4 has no Tree Seedling cover class in tblVegetation.A@Dkk ",N [NonvasHt] tblVegetationVegetationID = "B$@$<Plot "F=, stratum N has no Non-Vascular cover class in tblVegetation.A@Dk0k( ",V[VineHt] tblVegetationVegetationID = "B$@$<Plot "F5, stratum V has no Vine cover class in tblVegetation.A@Dk`kX ",E[EpiHt] tblVegetationVegetationID = "B$@$<Plot "F9, stratum E has no Epiphyte cover class in tblVegetation.A@Dkk B@` & '&X B@Bb@ 0B@2|(  d!f Record  &A@Dbo 0B@B| d!fA@Do8]x]]]]HSELECT DISTINCT tblAADetails.AACode, tblAAVegetationDetails.Stratum, tblAAVegetationDetails.VegetationID FROM tblAADetails RIGHT JOIN (tblAAVegetation RIGHT JOIN tblAAVegetationDetails ON tblAAVegetation.VegetationID = tblAAVegetationDetails.VegetationID) ON tblAADetails.AAID = tblAAVegetation.AAID ORDER BY tblAADetails.AACode'$ 4. $ %6. 0B@2 B@8'& !:a ",T1 [EmergHt]tblAAVegetationVegetationID = "B$@$<Plot "l<, stratum T1 has no Emergent cover class in tblAAVegetation.A@Dkk ",T2[CanHt]tblAAVegetationVegetationID = "B$@$<Plot "l:, stratum T2 has no Canopy cover class in tblAAVegetation.A@Dkk ",T3[SubHt]tblAAVegetationVegetationID = "B$@$<Plot "l=, stratum T3 has no Subcanopy cover class in tblAAVegetation.A@Dk( k ",S1 [TallShHt]tblAAVegetationVegetationID = "B$@$<Plot "l>, stratum S1 has no Tall Shrub cover class in tblAAVegetation.A@DkP kH ",S2 [ShrubHt]tblAAVegetationVegetationID = "B$@$<Plot "l9, stratum S2 has no Shrub cover class in tblAAVegetation.A@Dkx kp ",S3 [DwarfHt]tblAAVegetationVegetationID = "B$@$<Plot "l?, stratum S3 has no Dwarf Shrub cover class in tblAAVegetation.A@Dk k ",H [HTotalHt]tblAAVegetationVegetationID = "B$@$<Plot "l=, stratum H has no Herbaceous cover class in tblAAVegetation.A@DkLVAL! k ",H4[H4Ht]tblAAVegetationVegetationID = "B$@$<Plot "lA, stratum H4 has no Tree Seedling cover class in tblAAVegetation.A@Dkk ",N [NonvasHt]tblAAVegetationVegetationID = "B$@$<Plot "l?, stratum N has no Non-Vascular cover class in tblAAVegetation.A@Dkk" If Strata!Stratum = "V" Thene If IsNull(DLookup("[VineHt]", "tblVegetation", "VegetationID = " & Strata!VegetationID)) Thenb MsgBox "Plot " & Strata!AAcode & ", stratum V has no Vine cover class in tblVegetation." End If End If" If Strata!Stratum = "E" Thend If IsNull(DLookup("[EpiHt]", "tblVegetation", "VegetationID = " & Strata!VegetationID)) Thenf MsgBox "Plot " & Strata!AAcode & ", stratum E has no Epiphyte cover class in tblVegetation." End If End If B@` & '&x B@Bb` 0B@2|H@ d!f Record  &A@Dbo]H]h]]SELECT tblPlotDetails.PlotCode, tblVegetation.* FROM tblPlotDetails INNER JOIN tblVegetation ON tblPlotDetails.PlotID = tblVegetation.PlotID'. 0B@2 4. . %6. B@8'& !:a ">$< "j$< Plot "F8, stratum Emergent has mismatched null in tblVegetation.A@DkP "H$< "n$< Plot "F6, stratum Canopy has mismatched null in tblVegetation.A@Dk "J$< "p$< Plot "F9, stratum Subcanopy has mismatched null in tblVegetation.A@Dk( "L$< "r$< Plot "F:, stratum Tall Shrub has mismatched null in tblVegetation.A@Dk "N$< "t$< Plot "F5, stratum Shrub has mismatched null in tblVegetation.A@Dk "P$< "v$< Plot "F;, stratum Dwarf Shrub has mismatched null in tblVegetation.A@Dkh "$< "$< Plot "F:, stratum Herbaceous has mismatched null in tblVegetation.A@DkE "R$< "$< Plot "F9, stratum Graminoid has mismatched null in tblVegetation.A@Dk8E "T$< "$< Plot "F4, stratum Forb has mismatched null in tblVegetation.A@DkD "V$< "$< Plot "F4, stratum Fern has mismatched null in tblVegetation.A@DkD "X$< "$< Plot "F=, stratum Tree Seedling has mismatched null in tblVegetation.A@DkC "Z$< "$< Plot "F<, stratum Non-Vascular has mismatched null in tblVegetation.A@DkB "\$< "$< Plot "F4, stratum Vine has mismatched null in tblVegetation.A@DkXB "^$< "$< Plot "F8, stratum Epiphyte has mismatched null in tblVegetation.A@DkA B@` & '&A B@B DoCmd.ClosebpA 0B@2|XAPA d!f Record  &A@Db AoA 0B@o@@ Attribute VB_Name = "Form_frmVerifyStrata" Bas0{7266871D-9A1B-4561-AA94-EFDDE8526A24} |GlobalSpacIFalDse dCrezb"lTru Pr@edeclaId"Expose_TemplPateDtvCustomizaD$Option Comp@ DT Priv* Sub ton_Click() OLVAL"n Error GoTo_s! Dim db As DAf'S<`o(o(, g (g )) 01Aousf}PN>b"GramO*O*'HRO* _>"O*O*G* inoid___3[?>_{ཞRHR??`??7 ?p%/(Fe>rO 'HRID)) Then MsgBox "Plot " & St rata!Int@~r% A P&-@PrXiva[ 151() On @or GoTo5_aC/ Dim db As DAO.Databa9ASaE*seB]NewYSQL?@ h!!IntegerGC;*/`Heig>h6`k ' = "SELECT!zAĎ.aC,GLVAL* FROM RIGHT JOIN ( )  ON .g⛑j)DmB ID DISTIN!.,%j&l&& 7'4ID&gd& ORDER BY?!F+![Seti= CuntDY %ad@b.OpenFi(1u`q,Tru`pbFirso h=Do Until.EOF/#!uma "T1",qEmergHt(*A )y y2!,?yT1ye`^cB c"@in4r.q xgy_AT2_Can?on??__?MT25opyveraQg!bt"3Sub}_"t P9_"_",a]3canoOo"C"o"d3SCS3[TallSh 3 a"rS3 Shrub"X""3u3[B|_E S4//E%o""PVS4/[Dwarf//////tVS&4" E;H4HO4[Gram H&4inoid44{__4_[ForW0/h/h!aW W 44H4 n tblVegetation." End If< 4If Strata! um = "H3" ThenLIsNull(DLookup("[FernHt]p", " I2DQ &f )) f MsgBox "Plot "6code _sH3 h@as no  cover class iJ4!Seedl4ED Tree $in.gFҊNaFNopnvasFʤ-NEF@#-Vascula@V!FVineEEV"/aD!E!"[Epi!?D+E!@phyte'?">".M MNextRecordCount+ 1ApCClose @ Exit_Ba_Click:DoCmd.HourgBFalCA Subrr$Err.Descripȡ#V ±[(]Resume C``Priva* Command6()  On or GoToA_kC k"k"M#  ButtonAAD`ils9a Dim db As DAO.D ba9!Sbsc2se%NewPSQLb qInt r1pQ SELECT DISTIN.AACz,,AAt. um s.) FROM RIGHT JOIN (bONm =Z) eyAAbIL`ORDER BYA`Set= CurrentD: {te Bdb.Open(@3"?TruBb"GFirs !=FDo Until.EOFA C?T1\ Emerg\ ///$a!AAT1\\l yT2Cah_$_on_`T2Uopy?? 0[??f?Sub"g"s"qID""" 9P4at1İcanoA""Q/4S/4o[TallSh"w$ S64 Shrub##0#_4[b4Q40#Sv4OESOO*So4KǴup("[DwarfHt]", "tblAAVegetation4ID = " & Strata! d)) Th en MsgBox "Plot lAAcodesIum S3 has no  Shrub cover class in ."mEnd If IfgmH" IsNull(DLookHTotal|HHerbaceousZ4bF4E:H4ETree SeedlingFN!FNonvas?G:GNF@#-Va`scula|'[#{r#Ve# q iVineG#LJߌÑIDƌ , V%#AEg 2"E?"`Epi"f5" E" phyte"@ ".M NNextRecord`Countȩ+l 1ApCClose Exit_b8a_@Click:DoCmd.HourgFalA!A SubrrGErr.De`scripa +[(]Resume  ҢPriva* Button"C() On or G8oToAA Dim db As DAO.Dba!SBCse"/`'SQL Intrsrt1rSELECT w Dils.5C|,3* FROM INNER JOIN O2/x!IDB}Trup" ``t1= CurrentD S=.Open(c@ QÃ+FirsY=*Do Until.EOF'@(O!EmergHt) +5QCovtotM= -1|_Mr>!_r`2=mismatched n`擅< #[ Can a!` E_HE t opy ll G Sub a!` y can OE7O;#TallShy a!   ot_#1# ;/ #C*B ѽ    ¿ # D/; m     a!q m D ! Gram a!q m `inoidGGn ForG q m  dIf (IsNull(Strata!FernHt) + Covtot)) = -1 Then  MsgBox "Plot 0" & code"", sum  has mismatc hed n in tblVegetation."bEnd If SeedlGTree )ingaNonv`     @ @ @ @        :;<=?@HV%&'()*n @@@@@@@@      V%)*&'( : ? @  :;:<:=:H @@@@ @@@M`OLJikMokmd`UidofkOJmJJMMQkkfJUQkOJmJLJkQk Sdi`kY`QukfQMk`dOo^Qk`kvkJMMQkkkmdiJUQ+iddmfidfOJmJ iQfdimkkMiYfmk qLJ`kvkJMMQkkkmdiJUQ+kMiJmMWJMQkkqLJOJmJ%qLJfid[QMmfid[QMm*fid[QMms`)qLJ+qLJ+fid[QMm'OYi([[hfW`S[kuqqbOkYWbv\YJdbiqqL& 6 OYiOJmJ fidfOJmJ6 OYiOJmJL^dL :L^dL:L^dLOQ^mJ:fidfOJmJ:mvfQYbSdS YN((Y PM Y Y   Y , Y , Y  Id LValueObjectGuidObjectNameProperty Value, , ,() , , ,(* , , ,(+ ,YYYId$ObjectGuidProperty$ObjectNameProperty(Hv1b ' ' '>YN-- Y Y MY  Y Y ,Y  Y   Filter FlagsIdNamePosition SelectedObjectIDType , ,-/, YIdv1@@a,uCustom ^Tables2"w V,... RY N11  Y Y Y  Y Y ,Y  Y   FlagsGroupCategoryIDIdName"Object Type GroupObjectIDPosition , ,13,  , ,14, YYGroupCategoryIDIdv1/0 yL|O  wCustom Group 162.*  w w w w w w w 0 @222222222 0 @22222222 2 Y``N66```Y Y Y Y  Y ,>Y >/Y / FlagsGroupIDIconIdNameObjectIDPosition>,/>,/>69/,>>,/>,/>6:/,>YYGroupIDIdv1(5VyLk> ] 0  | O " n A  ` 3   R % qDc6 U(tGf9 X+wJi<V  oU oT oSL oRK oQ J oPI oOH oNG oMF oLE oKD oJC oIB oHA oG@ oF? oE> oD= oC< oB; oA: o@9 o?8 o>7 o=6 o<5 o;4 o:3 o92 o81 o70 o6/ o5. o4- o3q, o2M+ o1* o0) o/( o.' o-& o,% o+y$ o*o# o)O" o(G! o'  o& o% o$ o# o" o!i o m o< o& o oY oL  oH o o o o o o o  o  o  o  o  o o  o  o  o  o  o' o o  o o o o o o5 yLk>`5  o_0  o^,  o]  o\  o[  oZ  oY@ oX$ oW  o 5 @ @ @ @ @ @ @ @ @ @ @ @77777777777777 7!7"7#7$7%7&7'7(7)7*7+7,7-7.7/707172737475767778797:7;7<7=7>7?7@7A7B7C7D7E7F7G7H7I7J7K7L7M7N7O7P7Q7R7T7U8888888888 777 7 7 7 7 777777777777S7 5 @ @ @ @ @ @ @ @ @ @ @ @77777777 7 7  7  7  7 7 77777777777777777 7!7 "7!#7"$7#%7$&7%'7&(7')7(*7)+7*,7+-7,.7-/7.07/170271372473574675776877978:79;7:<7;=7<>7=?7>@7?A7@B7AC7BD7CE7DF7EG7FH7GI7HJ7IK7JL7KM7LN7MO7NP7OQ7PR7QS7RT7SU7TV7UW8X8Y8Z8[8\8]8^8_8`8 RYN<<Y  Y Y IdNameTypedv;Oh=dA z [  c , u 4 ~ ? 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O    G qryPlotIDLinktblEnvironmentj@ SG+  Expr1Landform!tblEnvironmentDetails1.LandformX+  NewEnvIDEnvironmentID"[tblEnvironment].[EnvironmentID]i;!  tblEnvironment---  qryPlotIDLink+++  tblEnvironmentDetails1===  tblEnvironment1///  tblEnvironmentDetails;;; O    G kptblPlotDetails1tblEnvironment1^@ YM/ M2V8tB K C  N  M  GL;E1})xmForbCovTot[tblVegetation1].[ForbCovTot]P% wForbHtblVegetation1].[ForbHt]D wGramCovTot[tblVegetation1].[GramCovTot]P% wGramHtblVegetation1].[GramHt]D wHerbCovTot[tblVegetation1].[HerbCovTot]P% wHerbHtblVegetation1].[HerbHt]D wDwarfCovTot [tblVegetation1].[DwarfCovTot]S' wDwarfHt[tblVegetation1].[DwarfHt]G wShrubCovTot [tblVegetation1].[ShrubCovTot]S' wShrubHt[tblVegetation1].[ShrubHt]G wTallShCovTot![tblVegetation1].[TallShCovTot]V) wTallShHt[tblVegetation1].[TallShHt]J! wSubCovTot[tblVegetation1].[SubCovTot]M# w SubHt[tblVegetation1].[SubHt]A w CanCovTot[tblVegetation1].[CanCovTot]M# w CanHt[tblVegetation1].[CanHt]A w EmergCovTot [tblVegetation1].[EmergCovTot]S' w EmergHt[tblVegetation1].[EmergHt]G wPhysiognom[tblVegetation1].[Physiognom]P% wLeafTypeCommentsF@=1 wLeafType[tblVegetation1].[LeafType]J! wPhenology[tblVegetation1].[Phenology]M# wAssociations![tblVegetation1].[Associations]V) wAlliance[tblVegetation1].[Alliance]J! wProvCommunityNameH@?3 wPlotIDblPlotDetails].[PlotID]D wtblVegetation1--- tblPlotDetails1/// tblPlotDetails--- tblVegetation+++ O  GtblPlotDetails1tblPhotos1`@OC/ tblPlotDetailstblPlotDetails1p@WK- PhotoComments[tblPhotos1].[PhotoComments]U+ wPhotographer[tblPhotos1].[Photographer]R) wPhotoOtherblPhotos1].[PhotoOther]L% wPhotoFrameblPhotos1].[PhotoFrame]L% wPhotoRoll[tblPhotos1].[PhotoRoll]I# wPhotoType[tblPhotos1].[PhotoType]I# wPlotIDblPlotDetails].[PlotID]D wPhotoID[tblPhotos1].[PhotoID]C wtblPhotos1%%% tblPlotDetails1/// tblPlotDetails--- tblPhotos### O  G tblFuelsqryPlotIDLink^@G;!  tblFuels1qryPlotIDLink`@I=# 4RG 6 * D & | 4 o $ m!{M/{2nD&hx GtblFinalClassificationtblVegetationt@&cW= tblVegetation.FinalAssocNamen@%UI wtblVegetation+++ tblFinalClassification===  G  GT@$ 'tbl_Romme_PlotstblPlotLocationd@#YM/ tblPlotLocation.UTMZone"12"Q? wtblPlotLocation.Datum[tbl_Romme_Plots.Datum]`; wtblPlotLocation.InPark[tbl_Romme_Plots.InPark]c= wtblPlotLocation.UTMNorthing[tbl_Romme_Plots.Y_27]kG wtblPlotLocation.UTMEasting[tbl_Romme_Plots.X_27]iE wtblPlotLocation.GPSComments[tbl_Romme_Plots.GPSComment]qG wtblPlotLocation/// tbl_Romme_Plots///  G  GtblVegetation1tblVegetationDetails1@"cW- tblVegetationqryPlotIDLink\@!QE+ tblVegetation1qryPlotIDLink^@ SG- Diagnostic"tblVegetationDetails1.DiagnosticS% wSpecimenNumberH@9- wSpecimenCollectedN@?3 wCoverClass"tblVegetationDetails1.CoverClassS% wSpeciestblVegetationDetails1.SpeciesJ wTSNtblVegetationDetails1.TSN> wStratumtblVegetationDetails1.StratumJ wNewVegIDVegetationIDtblVegetation.VegetationIDa9! tblVegetationDetails1;;; tblVegetation1--- tblVegetation+++ qryPlotIDLink+++  GtblVegetationDetails999 O  GtblPlotDetailstblPlotDetails1p@WK- tblPlotDetails1tblVegetation1h@WK/ $EpiTotCov[tblVegetation1].[EpiTotCov]M# w#EpiHt[tblVegetation1].[EpiHt]A w"VineTotCov[tblVegetation1].[VineTotCov]P% w!VineHtblVegetation1].[VineHt]D w NonvasCovTot![tblVegetation1].[NonvasCovTot]V) wNonvasHt[tblVegetation1].[NonvasHt]J! wSeedlCovTot [tblVegetation1].[SeedlCovTot]S' wSeedlHt[tblVegetation1].[SeedlHt]G wFernCovTot[tblVegetation1].[FernCovTot]P% wFernHtblVegetation1].[FernHt]D w3Dj:w k $ y  a  I  8  `dF( x|^@8d:\kM/`Sheet1 ` G` G` ` G`tblPlotDetailstblFinalClassification~@FeY- `tblFinalClassification.PlotIDblPlotDetails].[PlotID]rK w`tblFinalClassification=== `tblPlotDetails--- ` G` ` G`@F '`qrytblVegWithPlotcodetblFinalClassification@Fsg; `B@F g`F@F g`"[qrytblVegWithPlotcode].[PlotID]? g`D@F g`tblFinalClassification=== `qrytblVegWithPlotcode;;; ` ` G`tblFinalClassificationqrytblVegWithPlotcodex@Fsg= `Expr1qrytblVegWithPlotcode.FinalAssocNameH@Foc `qrytblVegWithPlotcode;;; `tblFinalClassification=== ` G` G` ` GtblPlotDetailstblVegetationT@FSG- tblVegetation.*. gtblPlotDetails.PlotCode6 gtblVegetation+++ tblPlotDetails---   G@) '!tblPlotLocation.IsObservationPt> gtblPlotLocation.UTMZone6 gtblPlotLocation.Datum4 gtblPlotLocation.InPark5 gtblPlotLocation.UTMNorthing: gtblPlotLocation.UTMEasting9 gtblPlotLocation.GPSComments: gtblPlotLocation.PlotCode7 gtblPlotLocation///  G G  GtblPlotDetailstblPlotDetails1h@(WK- NewPlotIDblPlotDetails].[PlotID]J## oOldPlotIDtblPlotDetails1.PlotIDG## o[tblPlotDetails].[PlotCode]: gtblPlotDetails1/// tblPlotDetails---   GtblPlotDetails1tblFuels1R@'MA/ tblFuels1.FuelsID0 gtblPlotDetails1.PlotID5 gtblPlotDetails1.PlotCode7 gtblFuels1### tblPlotDetails1///  G G E @ @ @ @ @ @ @ @ @ @ @ @ @ @                                         ! " # $ % & ' ( ) * + , - .  / !0 "1 #2 3 @  @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @  @  @  @  @  @ @ @ @! @" @# @ @$ @& @' @( @) @* @+ @, @- @. @/ @0 @1 @2  @3  @4  @5 @6 A A @%AAAAAAA A A A A AAAAAAAAAAAAAAAAAA A  A! A" A# A$A%A&A'A(A)A*A+A,A-A.A/A0A1BBBBB B!B"B#B$B B B AB BBBBBBBBBBBBBBBBBB BB!B"B#B$B%B&B'B(B)B*B+B B,B.B/B0B1B2B-B3CCCB (D @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ A A @%AAAAAAA A A A A AAAAAAAAAAAAAAAAAA A  A! A" A# A$A%A&A'A(A)A*A+A,A-A.A/A0A1BBBBB B!B"B#B$B B B AB BBBBBBBBBBBBBBBBBB BB!B"B#B$B%B&B'B(B)B*B+B B,B.B/B0B1B2B-B3CCCCCCCCCC C C C CCCC CCCCCCCCCCCCCCCC!C"C#C$C%C C&C(C)C*C+C,C-C'C.C0C1C2C3C4C5C6C7C/C8C:C;C<C=C>C9C?CACBCCGGGC@GGGGGG, LVAL db   P "CARE." & "9000"+CLng(Right([tblPlotLocation]![PlotCode],4))Sheet1.Field1=tblPlotLocation.PlotCode[tblPlotDetails].[PlotCode]=[tblFinalClassification].[PlotCode]((([qrytblVegWithPlotcode].[PlotID])<>[tblFinalClassification].[PlotID]) And (([tblFinalClassification].[PlotCode]) Is Not Null))[qrytblVegWithPlotcode].[PlotCode]=[tblFinalClassification].[PlotCode][tblFinalClassification].[PlotID][tblFinalClassification].[PlotCode][qrytblVegWithPlotcode].[PlotCode]tblFinalClassification.PlotID = qrytblVegWithPlotcode.PlotIDtblFinalClassification.Final_JC_NametblPlotDetails.PlotID=tblVegetation.PlotID 3%tblPlotLocation.PlotCodex@ FMA wtblPlotLocation///  G G  G`Sheet1tblPlotLocationL@ FG; `tblPlotLocation.*0 g`tblPlotLocation/// Y''NII''Y Y nID Field1\ihpiIKonYPrimaryKeyv1 H'eF'mN/ u V 7  } ^ ?  f G 'CARE.9441&CARE.9434%CARE.9367$CARE.9365#CARE.9364"CARE.9361!CARE.9359 CARE.9346CARE.9341CARE.9330CARE.9325CARE.9311CARE.9303CARE.9224CARE.9209CARE.9201CARE.9192CARE.9172CARE.9161CARE.9160CARE.9146CARE.9142CARE.9140CARE.9131CARE.9086CARE.9084 CARE.9071 CARE.9070 CARE.9065 CARE.9060 CARE.9057CARE.9056CARE.9050CARE.9036CARE.9030CARE.9018CARE.9017CARE.9008CARE.9005 H @ @ @ @ @JJJJJJJJ J J  J  J  J J JJJJJJJJJJJJJJJJJ J!J "J!#J"$J#%J$&J%'J&YYNMM Y  Y Y Y  Y , Y TmpPlotIDGPSCommentX_27Y_27 InPark Datum,,MX,ƀYTmpPlotIDv1?L/^H  y e j%@*YCr\KAPACARE.9037No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?*APACARE.9035 YesNAD 278,&$?.Z+AAȹPACARE.9034No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?s,A7qrOPACARE.9033No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?I.APACARE.9032 YesNAD 278,&$?Kx/A [L PACARE.9031No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?R*ṽ6ACvPACARE.9029No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?Ѧ5AiPACARE.9028No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@V;A@PACARE.9027 YesNAD 278,&$?<APACARE.9026 YesNAD 278,&$?A<A`PACARE.9025 YesNAD 278,&$?@=APACARE.9024 YesNAD 278,&$?]Kh<A=IPACARE.9023No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?:BAPACARE.9022 YesNAD 278,&$?`EA`PACARE.9021 YesNAD 278,&$?7EAPACARE.9020 YesNAD 278,&$?%hAR'OACARE.9019No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?eAOACARE.9016 YesNAD 278,&$?JrABOACARE.9015 YesNAD 278,&$?yJsvA{OACARE.9014No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? wA`OACARE.9013 YesNAD 278,&$?XA`yOACARE.9012 YesNAD 278,&$?AOACARE.9011 NoNAD 276*&$?~gA OACARE.9010No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?VA@OACARE.9009 YesNAD 278,&$?`A OACARE.9007 YesNAD 278,&$?AYOACARE.9006 YesNAD 278,&$?pAEdXOACARE.9004No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? }A OACARE.9003 YesNAD 278,&$? }AyZ5OACARE.9002No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?c͘ A{OACARE.9001No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L&/^ J  4 e O ? p+\FcM!`VA@.PACARE.9082 YesNAD 278,&$?/ܹ0^AM~.PACARE.9081No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?F{ pA+:.PACARE.9080No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? (A?.PACARE.9079 YesNAD 278,&$?A-PACARE.9078 YesNAD 278,&$?^J]Ao/i*-PACARE.9077No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@yFA@9PACARE.9076 YesNAD 278,&$?FA9PACARE.9075 YesNAD 278,&$?`}TA_9PACARE.9074 YesNAD 278,&$?CŽKA1* 9PACARE.9073No GPS; Romme locations modified based on plant community descriptions.NoNAD 27$?@A PACARE.9072 YesNAD 278,&$?A PACARE.9069 YesNAD 278,&$?`A PACARE.9068 YesNAD 278,&$?}:AJia@PACARE.9067No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`A>PACARE.9066 YesNAD 278,&$?@AV?PACARE.9064 YesNAD 278,&$?$A?PACARE.9063 YesNAD 278,&$?A@PACARE.9062 YesNAD 278,&$?ƼAeAPACARE.9061 YesNAD 278,&$?TNA>"APACARE.9059 YesNAD 278,&$?)wABAPACARE.9058 YesNAD 278,&$?O,A}yAPACARE.9055 YesNAD 278,&$?.o./AɶAPACARE.9054 YesNAD 278,&$?AOACARE.9053 NoNAD 276*&$? 8ApOACARE.9052 NoNAD 276*&$?G#A PACARE.9051 YesNAD 278,&$?W*A PACARE.9049No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?60A PACARE.9048 YesNAD 278,&$?]2A* PACARE.9047 YesNAD 278,&$?A PACARE.9046 YesNAD 278,&$?2]A- PACARE.9045No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@}A$ PACARE.9044 YesNAD 278,&$?16APACARE.9043 YesNAD 278,&$?`^4A PACARE.9042 YesNAD 278,&$?5A PACARE.9041 YesNAD 278,&$?@SA`PACARE.9040 YesNAD 278,&$? }QAQNPACARE.9039No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?BvޖgNA PACARE.9038No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L/` J  4  M | S=qꅰAo8PACARE.9111No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?J_83A8PACARE.9110No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A 8PACARE.9109 YesNAD 278,&$?A8PACARE.9108 YesNAD 278,&$?@AE*PACARE.9107 YesNAD 278,&$?sKQ$Am*PACARE.9106No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? 1A)PACARE.9105 YesNAD 278,&$?rA)PACARE.9104 YesNAD 278,&$?"pHA!<%+PACARE.9103No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`,LA+PACARE.9102 YesNAD 278,&$?jW4EAč+PACARE.9101No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?U4Av'PACARE.9100No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? A/)PACARE.9099 YesNAD 278,&$?AlAN"b)PACARE.9098No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?˜A3)PACARE.9097No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ܞ qwAuS)PACARE.9096No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?S9mA7Ou.*PACARE.9095No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?#NAqU9PACARE.9094No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?7SA 9PACARE.9093 YesNAD 278,&$?t~MA~19PACARE.9092No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`oKA9PACARE.9091 YesNAD 278,&$?MA@9PACARE.9090 YesNAD 278,&$?1n(A\t(.PACARE.9089No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`]A`;.PACARE.9088 YesNAD 278,&$?A-PACARE.9087 YesNAD 278,&$?@,A -PACARE.9085 YesNAD 278,&$?A -PACARE.9083No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$??L/^H w 2 a  N}8i$S=71AOACARE.9144 YesNAD 278,&$?9\;A( OACARE.9143 YesNAD 278,&$?I:A\mOACARE.9141No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? A~OACARE.9139No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? A`?OACARE.9138 YesNAD 278,&$?GA *PACARE.9137 YesNAD 278,&$?JZ7AĔH;)PACARE.9136No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?BA)PACARE.9135 YesNAD 278,&$?_ DAΈ )PACARE.9134No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?#>A`(PACARE.9133 YesNAD 278,&$? A *PACARE.9132 YesNAD 278,&$?AE*PACARE.9130 YesNAD 278,&$?`A *PACARE.9129 YesNAD 278,&$? A%PACARE.9128 YesNAD 278,&$?D9TA8Q%PACARE.9127No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?0K;EHAz?%PACARE.9126No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? +mA~:/PACARE.9125No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?AWA3#t0PACARE.9124No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?\WA0Z@0PACARE.9123No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?jA 7PACARE.9121 YesNAD 278,&$?@wAPACARE.9120 YesNAD 278,&$?rAPACARE.9119 YesNAD 278,&$?@գA@PACARE.9118No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?APACARE.9117 YesNAD 278,&$?ZhŬAQi[PACARE.9116No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? "eaA ,|PACARE.9115No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@6A@ 7PACARE.9114 YesNAD 278,&$?kABo.7PACARE.9113No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ٕAAz5PACARE.9112No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L#/` { 6 Q = [^@AOACARE.9184 YesNAD 278,&$?[AOACARE.9183 YesNAD 278,&$?@ APACARE.9182 YesNAD 278,&$?PA.7PACARE.9181No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?AEA}\"PACARE.9180No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?AdPACARE.9179No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? 7A PACARE.9178 YesNAD 278,&$?APACARE.9177 YesNAD 278,&$?P~VA̓sPACARE.9176No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A3PACARE.9175 YesNAD 278,&$?mA$YPACARE.9174No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?}˜nAގpPACARE.9173No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`APACARE.9171 YesNAD 278,&$?;vAm&PACARE.9170No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`OA-PACARE.9169 YesNAD 278,&$?A,PACARE.9168 YesNAD 278,&$?`A@PACARE.9167 YesNAD 278,&$?`A@PACARE.9166 YesNAD 278,&$?A`PACARE.9165 YesNAD 278,&$?@A`/PACARE.9164 YesNAD 278,&$?`A.PACARE.9163 YesNAD 278,&$?A PACARE.9162 YesNAD 278,&$?XA@OACARE.9159 YesNAD 278,&$?4fC_AOACARE.9158No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`FAOACARE.9157 YesNAD 278,&$?h>AOACARE.9156 YesNAD 278,&$?`6AOACARE.9155 YesNAD 278,&$?+%AO]OACARE.9154No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@P/A +OACARE.9153 YesNAD 278,&$?@N)AOACARE.9152 YesNAD 278,&$?`V!AOACARE.9151 YesNAD 278,&$?%AOACARE.9150 YesNAD 278,&$?MA:PACARE.9149 YesNAD 278,&$?KA t:PACARE.9148 YesNAD 278,&$?,A~!OACARE.9145No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L/H  c P :i$S=l'V`]APACARE.9214 YesNAD 278,&$?mZALtPACARE.9213No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?=0A`OACARE.9212 YesNAD 278,&$?o$w?A9#VOACARE.9211No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?=A@OACARE.9210 YesNAD 278,&$?hN 7A4cMOACARE.9208No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?Mɵ7ADOACARE.9207No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?8)A@LOACARE.9206 YesNAD 278,&$?)ְA ܺoOACARE.9205No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ATOACARE.9204No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?%AOACARE.9203 YesNAD 278,&$?ɸA3OACARE.9202 YesNAD 278,&$?AjOACARE.9200 YesNAD 278,&$?6A "OACARE.9199 YesNAD 278,&$?uZhA~jX!OACARE.9198No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?3A}OACARE.9197No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?Za<A^KȇOACARE.9196No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@AOACARE.9195No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?%A@OACARE.9194 YesNAD 278,&$?@3uA:OACARE.9193 YesNAD 278,&$?y |A4;OACARE.9191No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?nA`7OACARE.9190 YesNAD 278,&$?~jA@5OACARE.9189 YesNAD 278,&$?~$a}A/$rOACARE.9188No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?nk A7OuOACARE.9187No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A@OACARE.9186 YesNAD 278,&$?ݯvAlOOACARE.9185No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L/`  4 c  M | 7 fP :=t"VAl&$PACARE.9321No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? 3A0'PACARE.9320No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?5A`'PACARE.9319 YesNAD 278,&$?6A`'PACARE.9318 YesNAD 278,&$?Aԍ*Aߡx-PACARE.9317No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ZCA W*PACARE.9316No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?IEs%A@$PACARE.9315No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$? APACARE.9314 YesNAD 278,&$?яA PACARE.9313 YesNAD 278,&$?H¼7AKvlOACARE.9312No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A /PACARE.9310 YesNAD 278,&$?`~AB/PACARE.9309 YesNAD 278,&$?Տ5TA=S.PACARE.9308No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?GJqi]AK!{.PACARE.9307No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?jA/PACARE.9306 YesNAD 278,&$? AB/PACARE.9305No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$??AOOACARE.9304No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A`5PACARE.9302 YesNAD 278,&$?֎lADUZ3PACARE.9301No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?d"AeS 4PACARE.9300No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?fvWA˄_x"PACARE.9221No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?`YAPACARE.9220 YesNAD 278,&$?jaAPACARE.9219 YesNAD 278,&$?lcA PACARE.9218 YesNAD 278,&$?bA/PACARE.9217 YesNAD 278,&$?a^APACARE.9216 YesNAD 278,&$?)>#^AM-[UPACARE.9215No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?L/^H w M | 7  <m( oAA;6=PACARE.9352No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?stA.>PACARE.9351No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?VҊAe6G>PACARE.9350No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?]eA*PACARE.9349 YesNAD 278,&$?[AbA c*9+PACARE.9348No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?@/_A +PACARE.9347 YesNAD 278,&$?A<)PACARE.9345 YesNAD 278,&$?H1A)PACARE.9344 YesNAD 278,&$?;A`'PACARE.9343 YesNAD 278,&$?fA"PACARE.9342 YesNAD 278,&$?@uApPACARE.9340 YesNAD 278,&$?ƒxAR`PACARE.9339No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?,oA](PACARE.9338No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ftAz&PACARE.9337No GPS; Romme locations modified based on plant community descriptions.NoNAD 27$?A`'PACARE.9336 YesNAD 278,&$?`A'PACARE.9335 YesNAD 278,&$?@APACARE.9334 YesNAD 278,&$?!se҈A(QPACARE.9333No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?A`uPACARE.9332 YesNAD 278,&$?A@PACARE.9331 NoNAD 276*&$?8Aypo5PACARE.9329No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?nǵZA.5PACARE.9328No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?rA>y8PACARE.9327No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?J?fsA/w8PACARE.9326No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?CsA8PACARE.9324 YesNAD 278,&$?5@ih]A^K%PACARE.9323No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?eOB;]A5^=%PACARE.9322No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$??L/^  I  L6e  ;l'V&A m7PACARE.9415 YesNAD 278,&$?@A7PACARE.9414 YesNAD 278,&$?oA7PACARE.9413 YesNAD 278,&$?haA`VPACARE.9406 YesNAD 278,&$?`AX@PACARE.9405 YesNAD 278,&$?"5dA~@PACARE.9404No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?1A7+PACARE.9403 YesNAD 278,&$?@ A&PACARE.9401 YesNAD 278,&$?)u\A&ZOACARE.9372No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?+ӟA3ıOACARE.9371No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?̣A`OACARE.9370 YesNAD 278,&$?)ƯA 0OACARE.9369No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ޮA *PACARE.9368No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?Z A"r1PACARE.9366No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?εA1PACARE.9363 YesNAD 278,&$?A`t/PACARE.9362 YesNAD 278,&$?k A/PACARE.9360No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?Gp "AeTpOACARE.9358No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?$x#gAYOACARE.9357No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?#_AIWQOACARE.9356No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?ʍ"HA[rh:PACARE.9355No GPS; Romme locations modified based on plant community descriptions.YesNAD 27$?h+#AyzvN66BN66DN66HN686N688N68:N 68<N 68>N 68@N 68BN 68HN6:6N6:8N6::N6:<N6:>N6:@N6:BN6:DN6:FN6:HN6<8N6<:N6<<N6<>N6<@N66O6>8O6>:O6><O6>>O6>@O6>BO6>DO 6>FO 6>HO 6@8O 6@:O 6@<O6@>O6@@O6@FO6@HO6B8O6B:O6B<O6B>O6BBO6BDO6BFO6BHO6D:O6D<O6D>O6D@O6DBO6DDO 6DFO!6DHO"6F6O#6F8O$6F:O%6F<P6F@P6FDP6FFP6FHP6H6P6H8P6H:P6H<P6H>P 6H@P 6HBP 6HDP 6HFP 6HHP866P868P86:P86<P86>P86@P86BP86DP86FP86HP886P888P88:Q88<Q88>Q88@Q88BQ88DQ88FQ88HQ8:6Q8:8Q 8:<Q 8:>Q 8:@Q 8:BQ 8:DQ8:FQ8:HQ8<6Q8<:Q8<<Q8<>Q8<@Q88Q8><Q8>>Q8>@R8>FR8>HR8@6R8@8R8@:R8@<R8@>R8@@R8@BR 8@DR 8@FR 8@HR 8B:R 8B<R8B>R8B@R8BBR8BDR8BFR8BHR8D6R8D8R8D<R8D>R8D@R8DBR8DDR8DFR8DHR8F6R8F8R8F:R 8F<R!8F>R"8F@S8FBS8FDS8FFS8FHS8H6S8H8S8H<S8H>S8H@S 8HBS 8HDS 8HFS 8HHS :66S:6:S:6<S:6>S:6@S:6BS:6DS:6FS:86S:88S:8:S:8<S:8>S:8@T:8BT:8DT:8FT:8HT::6T::8T<66T<68T<6:T <6>T <6@T <6BT <6DT <6FT<6HT<86T<8:T<8<T<8>T<8@T<8BT<8DT<8FT<8HT<:6T<:8T<::U<:<U<:>U<:BU<:DU<:FU<:HU<<8U<<:U<<<U <<>U <<@U <6U<>:U<><U<>>U<>@U<>DU<>FU<>HU<@6U<@8U<@:U<@<V<@>V<@@V<@BV<@DV<@FV68V>6<V>6>V>6@V>6BV>6DV>6FV>6HV>86V>88V>8:V>8<V>8>V>8@V>8BW>8DW>8FW>8HW>:6W>:8W>::W>:<W>:>W>:@W >:BW >:DW >:FW >:HW iQH8F@SMJiQH8FBSMJiQH8FDSMJiQH8FFSMJiQH8FHSMJiQH8H6SMJiQH8H8SMJiQH8H<SMJiQH8H>SMJiQH8H@S MJiQH8HBS MJiQH8HDS MJiQH8HFS MJiQH8HHS MJiQH:66SMJiQH:6:SMJiQH:6<SMJiQH:6>SMJiQH:6@SMJiQH:6BSMJiQH:6DSMJiQH:6FSMJiQH:86SMJiQH:88SMJiQH:8:SMJiQH:8<SMJiQH:8>SMJiQH:8@TMJiQH:8BTMJiQH:8DTMJiQH:8FTMJiQH:8HTMJiQH::6TMJiQH::8TMJiQH<66TMJiQH<68TMJiQH<6:T MJiQH<6>T MJiQH<6@T MJiQH<6BT MJiQH<6DT MJiQH<6FTMJiQH<6HTMJiQH<86TMJiQH<8:TMJiQH<8<TMJiQH<8>TMJiQH<8@TMJiQH<8BTMJiQH<8DTMJiQH<8FTMJiQH<8HTMJiQH<:6TMJiQH<:8TMJiQH<::UMJiQH<:<UMJiQH<:>UMJiQH<:BUMJiQH<:DUMJiQH<:FUMJiQH<:HUMJiQH<<8UMJiQH<<:UMJiQH<<<U MJiQH<<>U MJiQH<<@U ^ Y!(#mNZZ!!!!!!!!Y  Y Y  Y 2 Y dAAID AACodeSurveyDateSurveyorsCameraUsedescZrVCeescZzFwmPtZ~ldtrsCeZ lYYmYYiY<YYY.rD.rF.rG.rHL{1C150AAA-945A-4D3E-95E3-C30E467195B1}PlotCode PlotIDPrimaryKeyHv1b |<0Y:~<x6 p . j ( d $ b " \  Cy7s0`K >Z;;@@CARE_AA.0363Pete WilliamsOlympus Stylus;+:@@CARE_AA.0310Sarah ToppOlympus Stylus8(9`@CARE_AA.0295Stephanie ShoemakerCanon SureshotA18@CARE_AA.0285Stephanie ShoemakerCanon SureshotA17 @CARE_AA.0249Bruce CondieMinolta FZ6*6 @CARE_AA.0233Pete WilliamsOlympus Stylus;+5@CARE_AA.0201Stephanie ShoemakerCanon SureshotA14 @CARE_AA.0193Stephanie ShoemakerCanon SureshotA13@CARE_AA.0182Stephanie ShoemakerCanon SureshotA12@CARE_AA.0181Pete WilliamsOlympus Stylus;+1@CARE_AA.0168Sarah ToppOlympus Stylus8(0@CARE_AA.0161Sarah ToppOlympus Stylus8(/@CARE_AA.0149Bruce CondieMinolta FZ6*. @CARE_AA.0135Sarah ToppOlympus Stylus8(-`@CARE_AA.0117Sarah ToppOlympus Stylus8(, @CARE_AA.0087Sarah ToppOlympus Stylus8(+@CARE_AA.0074Stephanie ShoemakerCanon SureshotA1*`@CARE_AA.0068Stephanie ShoemakerCanon SureshotA1)`@CARE_AA.0066Bruce CondieMinolta FZ6*(@CARE_AA.0030Sarah ToppOlympus Stylus8('@@CARE_AA.0026Sarah ToppOlympus Stylus8(&`@CARE_AA.1774Amy TendickMinolta FZ5)% @CARE_AA.1515Liz BallengerMinolta FZ7+$`@CARE_AA.1452Liz BallengerMinolta FZ7+# @CARE_AA.1344Liz BallengerMinolta FZ7+" @CARE_AA.1192Stephanie ShoemakerMinolta FZ=1!`@CARE_AA.1189Liz BallengerMinolta FZ7+ `@CARE_AA.1060Amy TendickMinolta FZ5) @CARE_AA.1030Amy TendickMinolta FZ5)`@CARE_AA.0966Amy TendickMinolta FZ5)`@CARE_AA.0964Amy TendickMinolta FZ5)`@CARE_AA.0901Stephanie Shoemaker, Amy TendickCanon SureshotN> @CARE_AA.0879Liz BallengerMinolta FZ7+`@CARE_AA.0844Liz BallengerMinolta FZ7+@@CARE_AA.0833Liz BallengerMinolta FZ7+ @CARE_AA.0830Amy TendickMinolta FZ5)@@CARE_AA.0802Liz BallengerMinolta FZ7+ @CARE_AA.0801Amy TendickMinolta FZ5)`@CARE_AA.0768Amy TendickMinolta FZ5)`@CARE_AA.0701Amy TendickMinolta FZ5) @CARE_AA.0673Amy TendickMinolta FZ5)@@CARE_AA.0665Liz BallengerMinolta FZ7+@@CARE_AA.0662Liz BallengerMinolta FZ7+@CARE_AA.0571Liz BallengerMinolta FZ7+`@CARE_AA.0487Liz BallengerMinolta FZ7+ @CARE_AA.0417Liz BallengerMinolta FZ7+ `@CARE_AA.0394Amy TendickMinolta FZ5) `@CARE_AA.0383Liz BallengerMinolta FZ7+ `@CARE_AA.0311Liz BallengerMinolta FZ7+ @CARE_AA.0287Liz BallengerMinolta FZ7+ @CARE_AA.0283Liz BallengerMinolta FZ7+ @CARE_AA.0269Liz BallengerMinolta FZ7+@@CARE_AA.0267Liz BallengerMinolta FZ7+ @CARE_AA.0226Amy TendickMinolta FZ5)`@CARE_AA.0222Liz BallengerMinolta FZ7+ @CARE_AA.0091Liz BallengerMinolta FZ7+ @CARE_AA.0060Amy TendickMinolta FZ5) @CARE_AA.0010Liz BallengerMinolta FZ7+SY8|7Y I  v * U H  { : j)PGt3^N :Zs`@CARE_AA.1177Sarah ToppOlympus Stylus8(r @CARE_AA.1168Pete WilliamsOlympus Stylus;+q`@CARE_AA.1138Stephanie ShoemakerCanon SureshotA1p@CARE_AA.1128Sarah ToppOlympus Stylus8(o@CARE_AA.1120Sarah Topp, Bruce CondieCanon SureshotF6n@CARE_AA.1107Stephanie ShoemakerCanon SureshotA1m@@CARE_AA.1064Pete WilliamsOlympus Stylus;+l@@CARE_AA.1061Bruce CondieMinolta FZ6*k`@CARE_AA.1057Bruce CondieMinolta FZ6*j`@CARE_AA.1046Pete WilliamsOlympus Stylus;+i @CARE_AA.1013Sarah ToppOlympus Stylus8(h @CARE_AA.1005Pete WilliamsOlympus Stylus;+g`@CARE_AA.0982Bruce 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B`!C`"D`#E`$F`%G`&H`'I`(J`)K`*L`+M`,N`-O`.P`/Q`0R`1S`2T`3U`4V`5W`6X`7Y`8Za[a\a]a^a_a`aaabaca da ea fa ga haiajakalamanaoapaqarasatauavawaxayaza {a!|a"}a#~a$a%a&a'a(a)a*a+a,a-a.a/a0a1a2a3a4a5a6a7a8a9bbbbbbbbbb b b b b bbbbbbbbbbbbbbbbbbb b!b"b#b$b%b&b'b(b)b*b+b,b-b.b/b0b1b2b3b4b5b6b7b8b9b:cccccccccc c c c c ccccccccccccccccccc c!c"c#c$c%c&c'c(c)c*c+c,c-c.c/c0c1c2c3c4c5c6c7c8c9 d d d d dddddd d d d d ddddddddd d!d"d#d$d%d&d'd(d)d *d!+d",d#-d$.d%/d&0d'1d(2d)3d*4d+5d,6d-7d.8d/9d0:d1;d2<d3=d4>d5?d6@d7Ad8Bd9CeDeEeFeGeHeIeJeKeLe Me Ne Oe Pe QeReSeTeUeVeWeXeYeZe[e\eY                                                                                                                                                      ]e^e_e`eaebece de!ee"fe#ge$he%ie&je'ke(le)me*ne+oe,pe-qe.re/se0te1ue2ve3we4xe5ye6ze7{e8|e9}f~fffffffff f f f f fffffffffffffffffff f!f"f#f$f%f&f'f(f)f*f+f,f-f.f/f0f1f2f3f4f5f6f7f8f9f:gggggggggg g g g g ggggggggggggggggggg g!g"g#g$g%g&g'g(g)g*g+g,g-g.g/g0g1g2g3g4g5g6g7g8g9g:hhhhhhhhhh h h h h hhhhhhhh h h h h hhhhhhh h!h"h#h$h%h&h'h(h)h*h+h, h-!h."h/#h0$h1%h2&h3'h4(h5)h6*h7+h8,h9-h:.h;/i0i1i2i3i4i5i6i7i8i 9i :i ;i <i =i>i@iAiBiCiDiEiGiHiIiJiKiLiMiNiOiQiRi Si!Ti"Ui#Vi$Wi%Xi&Yi'Zi([i)\i*]i+^i,_i-`i.ai/bi0ci1di2ei3fi4gi5hi6ii7jjkjljmjnjojpjqjrjsj tj uj vj wj xjyjzj{j|j}j~jjjjjjjjjjjjj j!j"j#j$j%j&j'j(j)j*j+j,j-j.j/j0j1j2j3j4j5j6j7j8kkkkkkkkkk k k k k kkkkkkkkkkkkkkkkkkk k!k"k#k$k%k&k'k(k)k*k+k,k-k.k/k0k1k2k3k4k5k6k7k8llllllllll l l l l lllllllllllllllllll l!l"l#l$l%l&l'l(l)l*l+l, l- l. l/ l0 l1l2l3l4l5l6l7l8l9mmmmmmmmmm  m !m "m #m $m%m&m'm(m)m*m+m,m-m.m/m0m1m2m3m4m5m6m 7m!8m"9m#:m$;m%<m&=m'>m(?m)@m*Am+Bm,Cm-Dm.Em/Fm0Gm1Hm2Im3Jm4Km5Lm6Mm7Nm8Om9PnQnRnSnTnUnVnWnXnYn Zn [n \n ]n _n`nanbncndnenfngnhninjnknlnmnnnonpnqn rn!sn"tn#un$vn%wn&xn'yn(zn){n*|n+}n,~n-n.n/n0n1n2n3n4n5n6n7n8oooooooooo o o o o ooooooooooooooooooo o!o"o#o$o%o&o'o(o)o*o+o,o-o.o/o0K Y @ @ @ @ @ @ @ @ @ @ @ @ @ o1o2o3o4o5o6o7o8pppppppppp p p p p ppppppppppppppppppp p!p"p#p$p%p&p'p(p)p*p+p,p-p.p/p0p1p2p3p4p5p6p7p8p9qqqqqqqqqq q q  q  q  q q qqqqqqqqqqqqqqqqq q!q" q#!q$"q%#q&$q'%q('q)(q*O Y!2>!B @N!!!!!!Y Y  Y d Y d Y dY  Y d Y  Y  Y    Y    Y    Y   Y   Y   Y   Y   Y  Y  Y  Y  Y  Y  Y  Y  Y EnvironmentIDAAID Slope AspectTopoPositionElevationElevSource*EnvironmentalCommentsGeologyBareSoilBedrockSandMoss OtherOtherPctDesc Litter Rocks Lichen GravelLiveVegLitterLiveVegWoodWoodLichenRocksLichenGround"DarkCyanobacteria Water,voeConceos,nert"oiY&YYYYY.rDL{8FE66CF6-BFB3-4FB2-959B-78B6AB1AED8C}EnvironmentID PlotIDPrimaryKeyv1b<<PkK+immZmmJD%HHTJRLVALr~  F>$|(Very sandy, broad terrace with weak crypto development.Sandy, broad terrace with steep colluvial slopes just outside plot to the east.Broad alluvial terrace in the stream bend.Colluvium from above mixed in with rolling alluvial terrace here.AA point at the mouth of a side canyon - Geology of the Fold could also be new alluvium - very sandy with lots of huge rocks mixed in. Two sizeable drainage channels, as well as the edge of Halls Creek, run through the plot.Big drainage channel bounds plot to the east, (many JUNOST along drainage), and across drainage is a very different community with ATRCON looking across rockier soils over there.Rolling, sandy Aeolian deposits over Entrada - quite a bit of bedrock exposed here.Vegetation growing on sandy soil between Entrada outcrops.Very rolling, duney area with many small channels running through. Some dunes have lots of crypto, others look active and shifting.Small channels running through plot where JUNOST are concentrated. Undulating terrain.Deep, sandy soils through most of plot; though west side has ridge of Dakota Sandstone showing through. Tons of old cow tracks and poo.Notom Road bounds plot on one side, & ridge of Oyster Shell Reef bounds the other. Deep, sandy soils through most of plot; though west side has ridge of Dakota Sandstone poking up. Tons of old cow tracks and poo.Sandstone peeking through pebbly soil in places - deep soils @ lower (E) end of plot. Tons of old cow tracks & poo. Possibly Dakota Sandstone?Very sandy, rolling duney area. Point wraps around the sides and high slope of a dune.Wide, sandy wash runs through point - hills surrounding wash also very sandy.Point on a sandy island between two channels.Wash runs through plot - very sandy area. Burr Trail runs along edge of plot.Dirt road to Peek-a-boo Camp runs through plot. Tons of cow tracks through plot. Wash and surrounding hills very sandy.X$ F  a  o3M CSs614Low slopeGPS@New Alluvium50002Dark cyanoP0000000000jhfdb`^\ZXVTHFDB@>0$&1290MidslopeGPS@Navajo Sandstone1-a070002Cryptos, mossesPP0P00T0000{ywusqomkigeTPNLHC1% 0N/ALow levelGPS@New Alluvium0401-a001-bP0030000000igeca_][WUSNNLJEC?1%  y3288Low levelGPS2@Obscured by soil0400001-aT0P00T0000hfdb`^\ZXVTOOMKIGC1% !^21260MidslopeGPS@Talus/Colluvium/LandslidesP0000T050050000000rpnljhfd`^ZXXVTRPN2&!32280Low LevelGPSX@New Alluvium090000P0000000000a_][YWUSQOMKKIGEC?1%  0397Low levelGPSn@New Alluvium090000P0000000000`^\ZXVTRPNLJJHFDB>0$ 34246Low levelGPS@New Alluvium090000P00T0000000a_][YWUSQOMKKIGEC?1% $*0N/ALow levelGPST@New Alluvium07000002T0P00P0000ca_][YWUSQOKKIGEC?1% 10variableMidslopeGPS@New Alluvium070000P1-b01-b0000000mkigeca_ZXSQQOMKIE7+&5116Low levelGPS@ Carmel Formation0501-a0PWaterP0201-b00T0000trpnljhfa_[YRPNIGC1% 2029MidslopeGPSd@ Eolian Sands09000PCryptoT0000000000igeca_][YWUSKIGEC?1%  8287MidslopeGPS@ Entrada Sandstone0702000P0000000000geca_][YWUSQQOMKGC0$ 5270Low levelGPSt@ Entrada Sandstone0603001-acryptoPP0T00T0000sqomkigeca_]UPNLHD1%  12VariableMidslopeGPS@ Eolian Sands080001-bCryptoP001-b0000000usqomkigb`^\TOMKIE7+& 2252Low levelGPS@Obscured by soil080T00P001-b0000000hfdb`^\ZUSQOOMKIGC1%  #6777High SlopeGPS@Dakota Sandstone081-b0001-b00000T0000kigeca_][YWRRPNLGC1% :777High SlopeGPS@Dakota Sandstone071-b0001-bT0T00T0000kigeca_][YWRRPNLGC1%  /960MidslopeGPS @Morrison Formation061-a0001-aP00200T0000mkigeca_[YWRRPNLGC/#12Var.MidslopeGPS@Eolian deposits0900001-b0000000000igeca_][YWUPPNLJHD3'""0N/ALow levelGPSNone.New Alluvium0401-a00020000000000mkigeca_][YUUSQLJF8% 1N/ALow levelGPS@New Alluvium06002001-a0000000000fdb`^\ZXVTRMMKIEC?1% 10Low LevelGPSZ@New Alluvium0701-b000200000T0000ca_][YWUSQOKKIGB@<."%260Low LevelGPS@New Alluvium0701-b0002T0P00P0000eca_][YWUSQMMKIDB>0$0N/ALow levelGPS@New Alluvium0701-a0PDirt road1-bT0P0000000rpnljhfdb`^YNLJEC?1% LVAL  0 b$HDune area with low to high (>2 m.) mounds often capped with EPHVIR, but COLRAM and ARTFIL are definitely the co-dominants. COLRAM is very large and healthy-looking here!Petrified Carmel dunes and sandstone exposures with aeolian dunes at their bases which are capped in QUEHAV and a mixture of shrubs (ARTFIL occurring mostly along the small drainage channels).Fine, deep alluvial soils w/crust development.Slope is variable because it descends steeply to the SW into the wash community, then flattens out on the slope ridgetop before sloping gradually to the E where an old road/trail runs through a portion of the plot. A lot more small rock cover here than I've seen in most of the polygon.Deep, fine, alluvial soils with minor crust development. JUNOST seem to be invading this community from all directions. EPHVIR and STIHYM are co-dominant, with the other listed shrubs more associated with adjacent wash community, which is included in this polygon for some reason even though it's a totally different community (should map this separately!).Slope is an average, as northern 1/4 of plot has a steeper slope descending into the adjacent wash. Deep, sandy, alluvial soils with minor crust development throughout. Old road runs through east side of the plot.Step-like Navajo bedrock hogback with vegetation growing mostly linear (N to S) in cracks and in shallow soil pockets stabilized be well-developed cryptos and mosses. Vegetation stunted due to the shallow soils, and often mounded.Community is linear along stream bank, so we observed a linear AA point 8m wide. Observed 2 point bars - plot crosses a wash ~8m wide.Maybe used to be agricultural area? Recent mowing at south end of plot. Ditch running through plot east to west. Lots of dieback on ATRCAN and CHRNAU.Substrate pebbly & littered with large rocks to car-sized boulders - pretty steep talus slope.Broad, sandy terrace with almost no cryptos.Y W  ` - HZ@w//1678MidslopeGPSt@ Moenkopi Formation04T0001-aP00400T0000ljhfdb`^ZXVQQOMKIE1% .c5360MidslopeGPSp@Salt Wash Sandstone Member of the Morrison Formation051-aT001-a1-a00300T0000zuusqojf0$-`variablevariableInterfluveGPS@Salt Wash Sandstone Member of the Morrison Formation1-b1-bT00T1-b00700T0000{E94(,7333MidslopeGPSp@Salt Wash Sandstone Member of the Morrison Formation34000P20P00P0000~|zxvtrppnljhf0$+52Low slopeGPSp@Salt Wash Sandstone Member of the Morrison Formation0404T00TP0P00T0000~|zxvtrrpnlhd."*P1713High SlopeGPSn@Salt Wash Sandstone Member of the Morrison Formation1-a08T00TT0T00T0000~|zxxvtrni3'")X1720Low slopeGPSR@Salt Wash Sandstone Member of the Morrison Formation0405T00PP0P00P0000~|zxvvtrplh2&!(}2194ToeslopeGPS@Mancos shale080000020000000000b`^\ZXVTRPNJJHFDB>0$'74236ToeslopeGPS@Mancos shale90000T0000000000^\ZXVTRPNLJHHFDB@>0$&>V12310Low slopeGPSf@Moenkopi Formation1-bTT0PDirt roadTT0080000000wusqomkieca_TRPNLG3'"%2066High SlopeGPS"@Salt Wash Sandstone Member of the Morrison Formation03P000P0200400P0000}{wuusqomi3'"$K1945High SlopeGPSB@Salt Wash Sandstone Member of the Morrison Formation1-b0200TCryptosP1-b00400P0000xvtrni3'"#1633Low slopeGPS@Dakota Sandstone05P000T1-a0030000000kigeca_]YWRPPNLJHD2&!"696ToeslopeGPSf@Alluvial deposits0801-a00P00T0000000geca_][YWUSQQOMHFB/#!145Low levelGPS@New Alluvium090P00P00T00T0000`^\ZXVTRPNLJJHFDB>0$ variablevariableLow levelGPS@New Alluvium060030PCryptos1-a00000T0000~|zxvtrpni`^\XVRD83( rollingvariableHigh SlopeGPS@Eolian Sands090000T0000000000sqomkigeca_]][YWUQC72& 8168MidslopeGPST@ Eolian Sands090000P0000000000`^\ZXVTRPNLJJHFDB>0$~rollingn/aLow levelGPS@ Eolian Sands0207000PT0T00T0000omkigeca_][YYWUSOK=1,!lRollingN/ALow levelGPS\@Alluvial deposits0700002Crypto000P0000000|zxvtrpnljhf^ZXVTP=1,!uvariablevariableMidslopeGPS>@New Alluvium040P00TP0030000000usqomkigca_]][YWUQC72(q4123Low levelGPS@New Alluvium60001-bCryptos, mossPP0T00T0000qomkigeca_][LGECA?1% LVALB ~ \Fairly steep slope covered with small, cobbly rocks and less bare ground exposed, also scattered large rock chunks (1/2 - 2 sq. meters). Scattered, old JUNOST skeletons still standing around. Plot is near ridgetop. Mixture of shrubs here, but most have low cover values.Shrubs are mounded, often with crypto patches around their bases. Soil surface is covered with small cobblestones (1.5-5 cm), some conglomerated into bedrock, so very little exposure of bare soil. More slickrock/bedrock outcrops near the ridgetop (to the W) and on the S end of the plot.Slope is for half of the plot, the other half is where the slope levels out and is a more disturbed area dominated by BROTEC and weedy forbs. Geology is on the borderline between Dakota sandstone and the Mancos formation.More evidence of cattle grazing here (cow pies, hoof prints, and lots of weedy grasses and forbs). Lots of drought die-back on the ATRCAN. Fairly major drainageway (1-2 m. tall by 2-6 m. wide) flows east through the SE portion of the plot. NW portion of plot is on a hill with a steeper slope (~15 deg.).Disturbed understory/abundance of weedy grasses and forbs from cattle grazing, evidenced by cow pies and hoof prints. Deep, alluvial soils here with trace amounts of small rocks on the surface. 1-2 m. deep by 2-3 m. wide gully meanders through plot. Some drought die-back on the ATRCAN here and old JUNOST skeletons still standing are scattered about.Plot captures ~40 m. wide, broad drainage bottom running NE, as well as toeslope hills of the Oyster Shell Reef draining N into this bottom area. Lots of drought die-back and deaths of JUNOST and ATRCAN, making the herbaceous cover look deceivingly dominant here. Disturbed, weedy understory due to cattle grazing evidenced by cow pies and hoof prints.Higher dunes with sandier soils and different species associated with the ARTFIL than #1060. Lots of die-back on the POLINC.LVAL < \ L h  < <n0lPoint lies at the base of a sandstone reef and soils are composed of sand & pebbles eroded from above. The main road crosses the plot on its eastern edge. The area has been altered seriously by cattle grazing.This is a cow-affected area with deep soil.This is a cow-affected area with deep soil. Many annual weeds are present this year.This is an area of deep soil and little rock. Cows dine here enthusiastically. Many annual weeds are here this year.This site has sandy soil with a few pebbles.This is a sandy site with lots of adolescent biocrust.The terrain is rolling hills with meandering gullies.The terrain is rounded hills and meandering gullies. The soil is sandy with some gravel and rocks around.The site has sandy soil and this year, a carpet of annual forbs.Many large boulders & small flat rocks.The terrace where the trees sit is about two feet above the wash bottom. Debris in the trees shows that the terrace gets flooded occasionally. The trees are very large and healthy looking.Many large flat rocks and extensive biocrust decorate the surface.This site has rocky soil and extensive biocrust.The ground is mostly covered with small flat rocks.Soil is mostly covered with flat rocks and pebbles.The soil surface is mostly covered with rocks and pebbles.This side of the hogback is eroded into sand and gravel.This hogback is highly eroded and dissected creating many aspects. It slopes generally E.N.E. The rock is crumbly, coarse conglomerate.Bedrock exposures alternate with pockets of deeper soil.Bedrock exposures alternate with deeper pockets of soil.The hogback is coarse, crumbly, conglomerate sandstone.Hogback is coarse conglomerate sandstone.Shallow gullies meander through this broad toe slope. The wet spring has grown many annuals her.The terrain is a broad toeslope stretching from the cliffs east of here. Many gullies have sculpted the area.Surface of ground is covered with small flat rocks.[b . 1 2~I+KE'i460Low slopeGPS@Salt Wash Sandstone Member of the Morrison Formation03004001-bT00200T0000}{yttrpljf0$DZ575Low slopeGPS@Salt Wash Sandstone Member of the Morrison FormationTT0600P000400T0000~|xvtrrpnjhf0$CTu8100MidslopeGPSVery sandy soil at this site.Salt Wash Sandstone Member of the Morrison Formation07PT001-aT0T00T0000O$BUu5108MidslopeGPSSoil is deep and sandy.Salt Wash Sandstone Member of the Morrison Formation07PT0002T01-a00T0000I$Awe4130Low slopeGPSV@Salt Wash Sandstone Member of the Morrison Formation0700001-a00000T0000~|zxssqomkg1% @=d390Low slopeGPS@Salt Wash Sandstone Member of the Morrison Formation0500000300T00T0000~|zxvrrpnljf0$?l_360Low slopeGPS@Salt Wash Sandstone Member of the Morrison Formation06P000PT00200T0000~|xvtrrpnljf0$>k^8140MidslopeGPSX@Entrada Sandstone08PT00PT0P00T0000eca_][YWUSQOOMKIGC0$=ZS0N/ALow levelGPSl@New Alluvium0800001-b0000000000db`^\ZXVTRPKKIGEC?1% <CM0N/ALow levelGPSThis site has silty soil.New Alluvium070000020000000000~|zxvtrpnljffdb`^ZL% ;\R3120Low levelGPSSoil here is very sandy.New Alluvium60P00200000T0000ywusqomkigecca_][YK% :LvariablevariableLow slopeGPSj@Carmel Formation33P0PWater2T0P00T0000}{ywusqomkig`^\ZXVD83(9gM563Low slopeGPS@Carmel Formation070P001-aP0P00T0000geca_][YWUSNNLJHFB0$8)>582Low slopeGPSThis site has sandy soil.New Alluvium60000200000T0000ywusqomkigecca_][YK$7NG3180Low slopeGPSThis is a very sandy site.New Alluvium0600000200000T0000}{ywusqomkggeca_[M% 6^<0N/ALow levelGPS@New Alluvium050P000400000T0000ca_][YWUSQOKKIGEC?1% 525230MidslopeGPSN@Chinle Formation020000P0500300P0000jhfdb`^\XVRPPNLJHD2&!4]144Low levelGPS|@New Alluvium30P003T0300P0000^\ZXVTRPNLJHHFDB@>0$3V290Step in slopeGPS@ Moenkopi Formation02P0002biocrust030200200P0000|zxvtrpnjhd`VRPNLH4(#2320High LevelGPS`@ Moenkopi Formation03000004P00200P0000kigeca_]YWUQQOMKIE1% 1SD17136MidslopeGPSf@ Moenkopi Formation0202000020200200P0000pnljhfdb^\XTTRPNJF2&!0G+6110Step in slopeGPSf@ Moenkopi Formation02T00002P00500P0000omkigeca][YUUSQOMI5)$LVAL  b^VhSteep erosional gullies of W face of hogback.Small flat shaley rocks litter ground surface. A small gully transects point which has a lot of Bromus tectorum in it.Some very old disturbance from cows, otherwise quite stable. A depression where moisture collects supports a variety of annuals. Small pebbles litter ground surface. Well developed rain crust.Plot lies between 2 ridges of landslide deposits and includes the sides of each facing each other. In the low lying area are 2 gullies where the mixture of "T" shrubs and the lone juniper are.Some landslide deposits & large rocks are dribbling into the east end of the plot. Lots of dead Stipa grass & branches/whole plants of ATRCAN. A narrow wash runs through plot. ARTFIL is concentrated there.Many annuals weeds on flat and dead Stipa bunches.Point falls on top of a rise (hill or terrace) a few meters above the valley floor. A narrow, rocky wash runs through plot where the rabbit-brush live. The blackbrush also likes the shallower, rockier soil on the wash bank. The ricegrass looks more vigorous here than other places I've seen in Halls Creek.Most of the plot has sort of low, undulating duney feel to it. The eastern 1/3 or so of the plot is sort of a low depression supporting ATRCAN and many annuals only. Many dead bunches of Stipa and dead branches of Atriplex. A foot trail runs through plot, but has no effect.Terrace above the wash supports many annuals this year. Significant mortality on the ACHHYM. Soils are very sandy, but do have some loam content.This point occupies a south facing slope littered with large volcanic boulders with abundant grass and evenly spaced shrubs. Young Junipers are widely scattered. Erosion is minimal as the slope is well stabilized by plants and rocks.Some dead branches on ATRCAN, ~50% of most plants. The sandier areas of the plot have fewer annual weeds than on the more loamy soils.5bv ?  r iwnq\|12102MidslopeGPS|@Talus/Colluvium/Landslides02P000020200300P0000vtrpnljhdb^ZZXVTRN2&![fVariableVariableInterfluveGPS*@Moenkopi Formation09P000TT0T0000000{ywusqomkigeeca_]YE94(Z25240MidslopeGPS@ Chinle Formation030000P0400300P0000jhfdb`^\XVRPPNLJHD2&!Y3135Low slopeGPS@Chinle Formation04TP001-b1-b00400P0000mkigeca_[YTOOMKIGC1% XpvariablevariableLow levelGPS:@Chinle Formation1-b000Pcryptos031-a00500P0000}{wuplca_][VD83(W11345Low slopeGPS2@New Alluvium0400003Biocrust1-a00T00T0000qomkigeca_]XNJHFD@2&!V00N/ALow levelGPS@New Alluvium05P1-a001-a1-a00300P0000ljhfdb`^ZXSNNLJEC?1% U(varvarLow levelGPS@New Alluvium07P1-a0Pbiocrust1-bP01-a00P0000xvtrpnljeca\RPNIGC5)$T:variablevariableHigh SlopeGPSv@Salt Wash Sandstone Member of the Morrison Formation031-aT001-a0300300P0000{E94(S?w5110High SlopeGPS@Salt Wash Sandstone Member of the Morrison Formation06P02001-bT0T00P0000}{vvtrnlh2&!RWVariableVariableInterfluveGPS@Mancos shale061-a000PP00400T0000zxvtrpnlhfdbb`^\WSE94(Q.VariableVariableToeslopeGPSZ@ Mancos shale05P000PP0040000000usqomkigca_]][YWUQC72(PivariablevariableLowslopeGPSR@Mancos shale05P000P1-b0040000000xvtrpnljfd_]][YWUQC72(OBVariableVariableLow levelGPS@ Mancos shale040000P00040000000vtrpnljhdb`^^\ZXVRD83(N,VariableVariableLow levelGPS@Mancos shale08T000PP01-a0000000wusqomkidb`^^\ZXVRD83(MecVariableVariableStep in slopeGPS@Curtis Formation02031-a003Biotic crustP1-a0020000000}{migb^ZH<7(L-U3226Low levelGPS@New Alluvium08000PBiotic crust1-aP0T0000000rpnljhfdb`^YKIGEC?1% KOR4248ToeslopeGPSd@New Alluvium0800001-aT0P0000000ca_][YWUSQOJJHFDB>0$J<M4154High SlopeGPSj@New Alluvium0700001-aP01-a0000000hfdb`^\ZUSQLLJHFD@2&!IKG0N/ALow levelGPS*@New Alluvium080000020000000000ca_][YWUSQOKKIGEC?1% HxC0N/ALow levelGPS"Stream terrace with sandy soils.New Alluvium090000P00T00T0000}{ywusqommkigeaS% GsB0N/ALow levelGPS&@New Alluvium08P000PP01-b00T0000db`^\ZXVQOMKKIGEC?1% Fo16122MidslopeGPS@Old Alluvium03000002020050000000hfdb`^\ZVTPLLJHFD@2&!LVAL   L>Very disturbed area next to Burr Trail.Slope is littered w/pale boulders. Fallugia is restricted to upper slope.Plot is relatively level, but has wide & shallow gullies running through it where the shrubs are only slightly more concentrated. Soils are shallow & covered with flat shaley rocks of various sizes. Trees are mature, but short. Probably a pretty hot, dry area.There are some younger trees mixed in with the mature ones but they don't really constitute a subcanopy layer. A few spots have well developed biotic crust.Point is on gently sloping wash terrace. The trees are clumped at the bend in the wash where the terrace is flatter & the grasses are on the open slope.Plot encompasses the terrace edge about 1.5m above the wash & the braided channel that wraps around the west & south of it. The sagebrush & PJ are restricted to the point bar and the cottonwoods to the channel & wash edge.The wash / road transects the plot. The terraces slope gently up from the wash, but probably just a couple of feet on each side get flooded. The Rabbitbrush is not restricted to the wash edges.A mighty uplift with lots of large conglomerate boulders and tilted bedrock. Plot falls right along the spine of this feature. Many small pebbles are on the rocks and clayey soil underneath. A narrow drainage channel transects plot. Veg doesn't vary with aspect, except less SHEROT on E face lower on the slope.An eroding sandstone reef top runs through the western edge of plot. Soils are deep away from the reef. The pinyons prefer the sandstone. The grasses are concentrated on the deeper soils. Dead branches on ATRCAN.Steep narrow erosional gullies. Large outcroppings of bedrock & some bunches of broken bedrock are visible throughout plot.Large flat shaley rocks on a steep west facing slope. A narrow drainage runs through the west facing and bottom of plot. Maybe the weedy annuals represent an invasion.nLVAL Z ` >RPlot straddles a low, broken exposure of Entrada with mostly deeper Entrada soils on the surface.Plot is transected by narrow wash channel with only occasional CHRNAU. Most of plot is cheatgrass, with significant areas of dense tamarisk. SARVER shrubland occupies a higher valley floor level to west of plot. Area is very heavily disturbed.Plot is located on a low, subsidiary hogback immediately E of the main Entrada exposures in this area. Thin, biotic soils over Entrada slickrock limit vegetation, although some shallow dunes occur with Q. welshii on E face of ridge line.AA center sits in the center of a shallow wash channel with both soil and bedrock banks included in plot area. Mahonia is likely dense in the area because of the relatively large amounts of exposed Entrada bedrock, unique to this part of the polygon.Disturbed, broad flats along wash channel.Plot is located right where a significant, steep, rocky slide canyon enters the main Muley Twist Canyon - so it includes areas of the main canyon flood plain and a broader area of boulder-and-shrub wash bottom. A significant portion is also located on dry, south-facing slopes. A mish-mash of environments.Canyon bottom here is a little broader, slightly less steep and drier than in AA points 1820, 1276. Less shaded habitat under large boulders too.Slightly flatter, broader wash area here than AA 1276, may favor slightly different shrub mix. Less Chinle mixed into the soils than that point too. Still a steep, bouldery canyon.Plot is located in a steep. bouldery canyon. Soils include some Chinle exposures here and there, with Wingate-derived alluvium and boulders overlying most areas. Plot includes wash channelAtriplexes are limited to flatter, more stable areas. ERICOR is more common on steeper slopes. Occasional dead ERICOR. Most of plot is unvegetated. Most of plot is steep, 33 degree slope, but on opposite sides of a narrow ridge. Plot does include gully bottoms of a swell.,S 0 $ 6 y4&W#hsbVariableVariableHigh LevelGPS@Eolian depositsP02P004Crypto1-aP0P00T0000}{ywusqld`^\XVE94(rj40n/aLow levelGPSZ@New Alluvium070P001-bP0P00P0000db`^\ZXVTRPKKIGEC?1% qv60n/aLow levelGPSr@New Alluvium080T001-a00000T0000db`^\ZXVTRPKKIGEC?1% pF20124MidslopeGPS~@ Talus/Colluvium/Landslides1-b000PBiotic soil, moss1-a050030000000}ywsn[YWUSN2&!oDvariablevariableLow slopeGPS6@ Eolian depositsP0080PBiotic soil, Moss1-aT0T00T0000}{yta_]YWUD83(n{3171Low slopeGPS@New Alluvium08P1-a0PBiotic soil1-aT0T00T0000trpnljhfdb`[NLJEC?1% mu2286High LevelGPSj@Old Alluvium1-a00001-b1-a0030000000kigeca_]YWRMMKIGE@2&!l@VariableVariableLow slopeGPS@New Alluvium07PP0TBiotic soilPP0T00T0000}{ywusqomk^\ZXVRD83(k;12212MidslopeGPSD@Eolian deposits1-a0090TBiotic soilT00000T0000usqomkigeca_RPNJHC2&!jR0N/ALow levelGPS@New Alluvium070T0PMoss, biotic soil0200000P0000vtrpnljhfdb^KIGEC?1% im0N/ALow levelGPSH@New Alluvium080P0TMoss, biotic soil0300T00T0000vtrpnljhfdb^KIGEC?1% h_7142MidslopeGPS@Eolian deposits080P00T00000T0000ca_][YWUSQOMMKIGEA0$gEVariableVariableHigh SlopeGPS@ Entrada Sandstone09P00PBiotic soilTT0T00T0000}{ywusqdb`^\XE94(fL0N/ALow levelGPS@New Alluvium0800000200000T0000ca_][YWUSQOKKIGEC?1% ehvariablevariableMidslopeGPS@Carmel Formation070T003Biotic soilTT0T00T0000~|zxvtrpc_][YUC72(d60N/ALow levelGPS@New Alluvium080P000200000T0000ca_][YWUSQOKKIGEC?1% cQvariablevariableHigh SlopeGPS@Entrada Sandstone07P0002CyanobacteriaP00T00T0000}{ywufb`^\XE94(bvariablevariableLow levelGPS@New Alluvium030302001-b00000T0000{ywusqomkigbb`^ZVRD83(ar1246Low levelGPST@New Alluvium0900001-b00000P0000db`^\ZXVTRPKKIGEC?1% `variablevariableToeslopeGPSN@ Alluvial deposits90T0TmossPT0000T0000|zxvtrpnljhf`^\ZXVC72(_27120Low slopeGPSj@Talus/Colluvium/Landslides020T0TBiotic soil020300300T0000~|zxvtpnjfYWUSQM1% ^ac8105Low slopeGPS$@Talus/Colluvium/Landslides03000PBiotic soil031-b00300T0000}{ywuqojfYWUSQM1% ]10100MidslopeGPSl@Talus/Colluvium/Landslides030T00031-b00300T0000wusqomkiec^ZZXVTRN2&!:LVAL   0^Steep colluvial landslide with a wide variety of rock sizes from pebbles to large boulders. Surface is unstable, though small sheltered areas have patches of moss or biotic soil development.Sandy, semi-active dunes along valley edge. Line of dense JUNOST borders polygon at the base of Entrada slickrock. Lots of standing dead stems on ARTFIL.A small wash transects plot along a small bedrock exposure, and the JUNOST and FRAANO are located in cracks along this minor deviation from the rest of the area. Soils appear to be Entrada-derived alluvium.Lots of small rock on surface, Black basalt boulders.Wash is bounded equally by steep Carmel shale slopes w/sparse veg and small, sloped new alluvium terrace.Active Entrada-derived sand dunes.Plot is centered on a short transition slope between two level topographies. Primary association is on higher, sandy valley floor. Secondary and/or tertiary are on the lower wash terrace, also sandy soils.High stream terrace with slightly rolling terrain here and there - perhaps remnants of now stabilized dunes. These higher spots tend to have the patches of HILJAM.Aeolian, Entrada-derived sands on a rolling terrain. Hill crest and patches on edge of plot are active dunes, but majority of plot is stable soils w/o the dune topography. Clumps of dead perennial grasses occur in the area - probably Stipa hymnodies.Community is on a low floodplain or wash terrace, in a relatively poorly drained area - mud shrink cracks on surface. For some indiscernable reason the majority of CHRNAU and BROTEC is concentrated in an area approx. 1/3 of plot. The presence of the occasional ARTFIL is a mystery. Note that SARVER is absent from CHRNAU areas - which also show evidence of flood debris.Gypsiferous badlands transected by a deep, narrow gully make for a sparsely populated, steep-sloped spot. E. bicolor adds a dramatic splash of bright blooms, but all the rest of the vegetation has experienced lots of drought mortality, with lots of dead stems.LVAL4 . 8 \46XIn wash, but most of point in rolling hills of deep sandy soil w/good crust cover. Other Surface Geology: Eolian deposits.Fine deep alluvial soils w/crust development.Point lies in a wash. I made the point more of a rectangle to stay within the polygon, which is just the wash.This point is on the high banks (terrace) of a wash. The slope is zero, except at the bank which is 5 ft higher than the wash.This is near an Entrada sandstone bluff.There is a road that runs along the point on the margins. The area is maintained as a park. It is watered and mowed. The point is adjacent to the CARE Visitor Center.The soils are eroded Moenkopi with limestone rock mixed in (probably from neighboring Kaibab).Plants growing in cracks in slickrock.This point is at the head of a wash, in a narrow Navajo canyon.Point is on a sandy, level HIGH terrace at the base of the Waterpocket Fold. Sand dunes 40' lie due south. Oystershell Reef is on the other side of the valley (to east). Site is highly disturbed by grazing past and present. Substrate is a pure Entrada Sand. Never floods.Plot is on a tall dune (~40' high) piled up against the east face of the Waterpocket Fold.Other Surface Geology: Talus Point lies high on a slope between Navajo domes and an Entrada formation. The slope has large rocks on the SW side and exposed bedrock and sand on NE side.Wash is narrow, so veg is poorly sorted. Road runs through plot.This point is in the Kayenta between Navajo Domes.The point lies between Navajo Domes, in which there are dunes of Aeolian sand which has amazing crust development, these are bisected by washes. Bedrock is exposed intermittently, so soil is somewhat shallow.Plot is centered on a wash channel bank, with 50% in a high mixed shrub terrace community, and the other a riparian corridor. Terrace is about 5 meters above channel floor.This area is pretty homogenous, with deep alluvial soils.ZY [ - q # +Li<A0n/aLow levelGPS@Mancos shale1-a00009pond water00000000000pnljhfdb`^\ZNJHFD?1% y17164MidslopeGPSNear base of Entrada outcrop.Carmel FormationP00003CryptoP020030000000}ywokigecQ&!qVariableVariableLow slopeGPS@Alluvial deposits02P1-a01-bCryptoP0200300T0000}ywsqidb][WD83(*l254Low slopeGPSZ@Alluvial deposits070P002CryptoP0000000000omkigeca_][YQMKIGC0$zh0N/ALow levelGPS@Alluvial deposits0300800TT0T0000000hfdb`^\ZXVTRRPNJHD1% [p0N/ALow levelGPS@ Alluvial deposits06T030PCryptoT00P0000000pnljhfdb`^\ZRPNJHD1% 92VariableLow slopeGPSP@ Eolian Sands0701-a00PT0P0000000igeca_][YWUSSQOJHD6*%Hx2104Low levelGPSR@ Obscured by soil030001-aRoad0300000T0000pnljhfdb`^\XRMKIGC1% M8170High LevelGPS@ Old Alluvium0200001-bP00500T0000geca_][YUSQLLJHFD@2&!18260MidslopeGPSL@ Navajo SandstoneP08000P0000000000fdb`^\ZXVTRPPNLJFD2&!IvariablevariableLow slopeGPS~@Navajo Sandstone031-bP003crypto1-aP0P00T0000~|zxvtogca_ZVD83(0N/ALow levelGPS(@New Alluvium070P000200000T0000ca_][YWUSQOKKIGEC?1% ~40N/AStep in slopeGPS@Eolian deposits050P001-a0000000000kigeca_][YWRRPNLJF5)$}d 18132High slopeGPSt@Carmel FormationPPP0PCryptobiotic soilP1-a01-a0000000}{ywusqljecPNLJHF4(#|0N/ALow levelGPS@New Alluvium0300400PT0P00T0000ca_][YWUSQOMMKIEC?1% {~0n/aLow levelGPSNo comments provided.Alluvial deposits1-a00600T1-a01-a0000000~|zxsqljjhfb`[H% zV0n/aLow levelGPSNone.Alluvial deposits1-a00600TP01-a0000000sqomkige`^\ZZXVRPK8% y80N/ALow levelGPSNone.Alluvial deposits1-a00500T1-a01-a0000000vtrpnljhca\ZZXVRPK8% x+evariablevariableLow levelGPSDunes intersected with washesEolian deposits0301-a003cryptoT00000T0000zxtc83(w5Z0N/AStep in slopeGPSNoneEolian depositsP0300PCryptoPP00300P0000xvtrpnljfdb`XVTRNL;)$vn2388High SlopeGPSNone.Kayenta FormationP03000P1-a00200P0000trpnljhfb`[YYWUSOM:'"u32294High SlopeGPSNoneKayenta FormationP03000PP00300T0000pnljhfdb^\ZXXVTRNL9'"t16100MidslopeGPSd@Kayenta FormationP04T0PCryptoPP00400T0000qomkigec_][YQOMKGE2&!LVAL `  Z ( J Zd XBdlbThe Entrada hills are highly sculpted by erosion.The Entrada hills are highly sculpted by erosion.The slope and aspect are an average for the plot and not the side of the interfluve.Some blown in sand covers parts of the slickrock.The canyon is highly shaped by erosion.Plants are mostly growing in cracks.Dune is stabilized by vegetation.The dune is stabilized by vegetation.Many dark rocks litter the sandy surface.Sandy soil has collected in potholes and small dunes.The area has been chained and seeded for the pleasure of beeves. It looks like the P-J is trying to return.This is a steep, boulder-strewn slope.Huge boulders from the Wingate above cover most of the Chinle slope.The terrain is gently rolling with sandy soil.Vegetation is on the banks and bars of wash.Much limestone bedrock exposed at this site.Highly eroded clay badlands have every slope and aspect.Steep slope is dissected with drainages and littered with boulders.Steep slope is highly dissected with drainages.Steep slope is highly dissected with drainage and littered with boulders.Large rocks and boulders litter the surface.This area has been cleared and seeded with non-native grasses for the use of Beeves. Shrubs are returning strongly and P-J is slowly moving in.This site has rocky soil cut by many drainageways.Soil is stabilized by plants and a little biocrust.Plot has alternating rocky and sandy sections.Soil is sandy. Terrace is 3 - 5 feet above wash bottom.Sand is stabilized by biocrust and vegetation.Sand has been stabilized by biocrust and plants.The wash has made a channel through rolling terrain. The vegetation is on benches, banks and bars.Narrow, shady canyon appears to flood from wall to wall intermittently. Vegetation is on low terraces and banks.Heavy clay soils with little cover. Site appears to be semi-permanently flooded.Heavy clay soils with little cover. Site appears to be semi-permanently flooded.F_ " + 2 /]w34variablevariableInterfluveGPSp@Chinle Formation07T000PT00200T0000{ywusqomigecca_][WE94(30352MidslopeGPS@Chinle FormationP000020400200T0000hfdb`^\ZVTPLLJHFDD2&!j2520MidslopeGPS^@ Chinle Formation041-aT00021-a01-b00T0000pnljhfdb][VRRPNLGC1% 1050InterfluveGPS@ Chinle Formation02P000020200200P0000mkigeca_[YUQQOMKIE3'"7185High SlopeGPSX@ Moenkopi Formation02PT00030301-b00P0000omkigeca\ZVRRPNLJF2&!$2326High LevelGPS"@ Obscured by soil050T000300000T0000hfdb`^\ZXVTPPNLJHD2&!J3223Low slopeGPS!The soil is rocky and gravelly.Entrada Sandstone030P001-aP00300T0000~zxvqqomkieR% {D3276Low slopeGPS!Soil is a little gravelly here.Entrada Sandstone05PP001-aT00200T0000~zxvqqomkieR% ,A4190Low slopeGPSd@ Entrada Sandstone050T001-bP00200T0000kigeca_]YWUPPNLJHD1% O5231InterfluveGPSf@Entrada Sandstone080001-aBiocrust1-b00000T0000wusqomkigec^TOMKIE2&!I4176Low slopeGPS\@Entrada Sandstone070T001-bT0P00T0000igeca_][YWUPPNLJHD1% H3218Low slopeGPSThis is a sandy site.Entrada Sandstone080T001-aT0T00T0000~|zxvtrpnlggeca_[H% 30N/ALow levelGPSSoil is sandy.Entrada Sandstone0600000200000T0000xvtrpnljhfd``^\ZXTA% <435Low levelGPSCows frequent this area.Entrada Sandstone0600000200000T0000}{ywusqomiigeca]J$80N/ALow levelGPSp@New Alluvium060T00020000000000ca_][YWUSQOKKIGEC?1% '90N/ALow levelGPSSoil is sandy.New Alluvium0400000500000T0000sqomkigeca_[[YWUSOA% 1911High SlopeGPS\@Navajo Sandstone04PT002Biocrust0200000P0000usqomkigeca]SOMKIE3'"%14103High SlopeGPS`@Navajo Sandstone0404T01-aBiocrust1-a00000T0000zxvtrpnljhfaWRPNJF4(#226Low levelGPS@Carmel Formation050P0003T0P00P0000fdb`^\ZXVTRNNLJHFB0$M220Low levelMap@Navajo Sandstone02PT00020300200T0000jhfdb`^\XVRNNLJHFB0$YVariableVariableLow slopeGPS"Plant growing in cracks in rock.Navajo Sandstone1-a03P01-aCryptobiotic crust1-aP0T00P0000}xf83(J0n/aLow levelGPSTAMCHI are mostly dead.Mancos shale080000P0000000000zxvtrpnljhfddb`^\XJ% t0n/aLow levelGPS@Mancos shale1-a00009Water00000000000kigeca_][YWUNJHFD?1% [] T  d  w hX=t9kVarVarLow slopeGPSb@Entrada Sandstone050P0002T0T00P0000ljhfdb`^\ZXTTRPNLH5)$JsVarVarInterfluveGPSb@Entrada Sandstone060T0002T0T00T0000mkigeca_][YUUSQOMI6*%@2218InterfluveGPS@Mancos shale080000P0000000000b`^\ZXVTRPNLLJHFD@2&!VariableVariableMidslopeGPSThis is a loose dune.Navajo Sandstone04004001-a00000T0000zzxvrplZ72(VariableVariableLow slopeGPS"There is deep sand at this site.Navajo Sandstone040040002T0T00T0000~|xf83(X488Low levelGPSNone.Navajo Sandstone0403P0002T0T00P0000omkigeca_][WWUSQMI7$<1280High SlopeGPSb@Navajo Sandstone0602T001-aT0T00P0000ljhfdb`^\ZXSSQOMIE3'"8196Low slopeGPS"Plants mostly growing in cracks.Navajo Sandstone0207T00PT0T00T0000}{ywussqomieS% bVariableVariableInterfluveGPSN@Navajo Sandstone0403T0003T0T00P0000}{ywusqomkieeca_[WE94(dO1262MidslopeGPSH@Navajo Sandstone1-a09000TT0T00T0000hfdb`^\ZXVTRRPNLHC1% :7153MidslopeGPSB@Navajo Sandstone07PT0002T0T00T0000fdb`^\ZXVTRNNLJHFB0$G8224High SlopeGPS!Soil is stabilized by biocrust.Navajo Sandstone031-aT003Biocrust02T0T00T0000vrpnieS&!=890MidslopeGPSJ@Eolian Sands071-a00TBiocrust1-bT0T00T0000omkigeca_][VLJHFA=/#/1588MidslopeGPSR@Navajo Sandstone0404T0TBiocrustPP0P00T0000qomkigeca_][QOMKGC1% 3142Low slopeGPSj@Navajo Sandstone0404T0TBiocrustPT0T00P0000qomkigeca_][QOMKGC1% 3300LowslopeGPS@Obscured by soil05000003T0P001-b0000igeca\ZXVTRNNLJHFB0$10212MidslopeGPSL@Chinle Formation04P0001-a0300200P0000mkigeca_[YUPPNLJHD2&!22150MidslopeGPS@Talus/Colluvium/Landslides030T001-a0601-a00P0000xvtrpnljec_ZZXVTRN2&!3168Low levelGPS\@Moenkopi Formation07000002T0P00P0000igeca_][YWUQQOMKIE1% G,8264High SlopeGPSNoneMoenkopi Formation05P00002P00300P0000rpnljhfd`^\XXVTRPL8&!0N/AHigh LevelGPSPebbles cover the surface.Moenkopi Formation04000002T00300T0000~|zvtrnnljhfbN&!392Low levelGPSX@Moenkopi Formation1-b02P00P0400200T0000mkigeca_[YUSSQOMID0$Y&789High SlopeGPSX@Kaibab Limestone0204000020200200P0000mkigeca_[YUQQOMKGC1% LVAL Z v H .RPlot is located in a canyon encompassing a N & S-facing slope and the narrow draw between them. Vegetation is sparser overall on the S-face. Soil is pebbly.Colluvial slope with eroded clay gullies and ridges. Many large sandstone boulders from above and flat shaley rocks. The highly eroded clay gully slides have no vegetation.Steep colluvial slope with frequent rockfall and slope movement.Soil surface is covered with flat platey rocks - mostly broken into small pieces.Area had been cleared long ago to remove sage and planted later with the Elymus bunchgrass. Many weedy annuals here.Plot encompasses a sandstone outcrop, a draw, shifting dunes, and stabilized soil with a pebbly surface. The Ephedra and ricegrass dominate the NE quadrant and should probably be part of the adjacent polygon, although those species are represented throughout the plot. Other Surface Geology: Eolian sands.This plot occupies the 2nd terrace above the wash. Very little well-developed biocrust is developed here. The grass component is high relative to the shrubs. Soils are well stabilized with poorly developed crust. Many dead ricegrass bunches.Plot occupies the 1st low terrace above the wash about 1m. Probably not subjected to flooding.Plot drains into a wash at bottom of a large outcrop of Entrada.A hill on N end of plot has rockier soil and not sand sage. Several shallow gullies transect plot. Plants are on mounds & most litter has blown away.Landslide deposits which have eroded into a maze of gullies and hills. Pebbles cover the soil surface and medium-sized rocks are scattered around. Other Surface Geology: CurtisMany pebbles in & on soil surface. Many dead ricegrass bunches.Point hugs 2 drainages. Soils are sandy, derived from the bedrock, and vary in thickness.Soils are sandy, but stabilized. A narrow drainage runs through plot.The terrace is about six feet above the wash bottom.db I  u u Z \551High SlopeGPSNone.Moenkopi Formation031-a001-aBiocrust031-b002001-a0000{ywsqlh^YWUPL8% x0N/ALow levelGPSP@Obscured by soil0200004Biocrust/moss0400000T0000xvtrpnljhfd`QMKIGC1%  0N/AHigh LevelGPSB@Moenkopi Formation05P00002P00300P0000ljhfdb`^ZXVRRPNLJF2&!1052MidslopeGPSf@Moenkopi Formation02000PBiocrust1-a0200500P0000xvtrpnljfd`[QOMKIE1% nD790Low slopeGPSb@Kaibab Limestone04P001-bBiocrust1-b1-a00300P0000ywusqomkge`[QLJHFB0$3138High LevelGPS@Moenkopi Formation03000PBiocrust02T00500P0000vtrpnljhdb`\RPNLJF2&!variablevariableLow slopeGPS<@Chinle Formation06P00PBiocrust021-a00001-a0000}{ywuplb`^\ZVD83(K27360MidslopeGPS\@ Chinle Formation050000021-b002001-a0000pnljhca_[YTPPNLJHD2&!25360MidslopeGPS@ Colluvial deposits0200000203003001-a0000qomkidb`\ZVRRPNLJF2&!variablevariableHigh SlopeGPS@ Moenkopi Formation03000PBiocrust02P00500P0000}{wusoeca_]YE94(0N/ALow levelGPS@ Obscured by soil080000P0000000000eca_][YWUSQOOMKIGC1% =e582Low slopeGPSf@ Entrada Sandstone05021-a01-aBiocrust1-aP00300T0000|zxvtrpnjhfaWRPKGC0$]0N/ALow levelGPS@New Alluvium080001-aBiocrust1-a00T0000000qomkigeca_]XNIGEC?1% [0N/ALow levelGPS@New Alluvium0300006Biocrust1-aP01-b0000000sqomkige`^\WMIGEC?1% 6322Low slopeGPS@Entrada Sandstone0600002biotic crust1-aP0020000000{ywusqomige`RNLJHD1% &VariesVariesStep in slopeGPS.@Entrada Sandstone07TT002BiocrustPP0020000000}{ywsqomc_][YUB61"yvariablevariableHigh SlopeGPSd@Colluvial deposits05000PMoss1-a1-a0040000000}{wupkeca_]YE94(wvvariablevariableStep in slopeGPS@Entrada Sandstone070001-aMoss1-b00020000000}ywupjeca_[H<7(VariableVariableLow slopeGPS@Navajo Sandstone02PP004Biocrust03T0T00P0000~|zxvtrnd`^\ZVD83(hVariableVariableLow slopeGPS@Navajo Sandstone05PP002Biocrust03T0T00P0000~|zxvtrnd`^\ZVD83(variablevariableLow slopeGPS!A sandy wash runs through plot.Carmel Formation041-bP002Biocrust02T0T00P0000{we83(a0N/ALow levelGPSh@Entrada Sandstone040P000300000T0000hfdb`^\ZXVTPPNLJHD1% LVALR H  Plot encompasses the terraces on either side of a wash. Terraces are subjected to periodic flooding. Area has been disturbed by grazing.Plot encompasses a gully & hill to the east of it. TAMCHI is in the gully. Other species are well-distributed. Area disturbed by grazing w/high cover of BROTEC.The cheatgrass is confined to a shallow gully. The Eriogonum and Hilaria are localized in some anomaly which is lacking a rain crust.Plot sits on a finger ridge with both N and S steep facing slopes. Many large lava boulders are embedded in the soil.Plot encompasses 2 wide, shallow drainages and the slopes between. An old road and irrigation ditch run through the eastern part of plot. That is where the young cottonwood and Salix are. Plenty of dead sagebrush on plot. Some pines are very tall and big here.About 1/4 plot is on Moenkopi shale and 3/4 of plot is on deeper soils obscuring geology.An old road runs through east edge of plot and lacks regulation. There are many young junipers here. Lots of dieback on the sage and dead shrubs too.Plot encompasses a wide wash and the slope above to the east. The bank is about 3m above the wash. An irrigation ditch transects the slope running N-S, but is no longer in use as evidenced by the dead tamarisk. The slope between the ditch and the wash has suffered deep gullying. The slope above the ditch has a more natural appearance.Many dead sage shrubs. Deep soils.Area was chained to remove P-J & sage and planted, long ago. Piles of tree wood everywhere.The juniper is an invader from another polygon.Deep soils with well developed biocrust.Soil is covered with small rocks.Many small rocks on soil surface. Area is gullied.Rocky shallow soils with relatively short mature trees. Area is dissected by narrow, steep, rocky gullies. Plot is on interfluve between Moenkopi above and White Rim ss below.Small rocks create a "desert pavement" feel to this place. Trees are mostly 2-3m tall.ZM M <"u10variablevariableHigh SlopeGPS@Entrada Sandstone1-b0000TP0080000000}{ywusqokigeeca_]XE94(`352Low level1:24K Quad@Kayenta Formation02T02001-b0200200T0000usqomkigca]XXVTPNJ7+`352Low level1:24K Quad@Kayenta Formation0P06001-a1-a00300T0000trpnljhfb`[VVTRNLJ7+X2250Low level1:24K Quad0@Colluvial deposits1-aTP001-b0701-b00T0000xvtrpnljec_ZZXVTRM9-!?12220Low slopeGPS@Summerville Formation03P000021-a00400P0000sqomkigea_ZVVTRPNJ3'"z3248ToeslopeGPS@Mancos shale070000030000000000b`^\ZXVTRPNJJHFDB>0$VariableVariableLow levelGPS@Mancos shale07000003T0T0000000vtrpnljhfdb^^\ZXVRD83( VariableVariableLow levelGPSF@Mancos shale0800001-aT0P00T0000wusqomkigec^^\ZXVRD83(VariablevariableLow levelGPS @ Mancos shale090000P0000000000trpnljhfdb`^^\ZXVRD83(variablevariableInterfluveGPS@ Carmel Formation0200000302003001-a0000~|zusqmkgcca_][WE94(384Low slopeGPS@ Obscured by soil050001-bMoss, biocrust031-a01-b001-a0000~|zusqljeaQLJHFB0$6104MidslopeGPS@ Obscured by soil07000PBiocrust021-a01-b00P0000vtrpnljhca\XNLJHFB0$}485Low slopeGPS.@ Obscured by soil0200003Biocrust/moss031-a01-a00P0000}{ywusqojhc_PLJHFB0$5304Low slopeGPS@Obsured by soil0201-a003Moss/Biocrust02P00200P0000|zxvtrpnjhfbSOMHFB1% a272High SlopeGPSF@Obscured by soil070001-aBiocrust/moss0300000T0000ywusqomkigeaRMKIGC1% 372High SlopeGPS Deep soils.Obscured by soil0500002Biocrust/moss0300000P0000}{ywusqm^ZXVTP>% !0N/AHigh LevelGPS!Some drought-mortality of sage.Obscured by soil060001-aMoss/biocrust0300000P0000tomkieS&!0N/AHigh LevelGPSDeep soils, cattle grazing.Obscured by soils060001-bMoss0300000T0000}{wqljhfbO&!0N/AHigh LevelGPSCattle grazingObscured by soil07000PMoss0200T00T0000~|zxvtrpnljf`^\ZXTB&!3352MidslopeGPS Deep soils.Obscured by soil0700002Moss/Biocrust1-b00T00T0000}{ywusql]YWUSO=$2242ToeslopeGPS@Obscured by soil0600000200P00020000hfdb`\ZXVTRNNLJHFB0$0N/ALow levelGPS^@Obscured by soil060001-bMoss0300P00T0000pnljhfdb`^\XRMKIGC1% LVAL f n ~$tZThis is a hill of Carmel - shaley-soil on top of Navajo bedrock. There are scattered Navajo boulders in it.Half of plot is in Carmel Formation, half in Navajo and each has the distinct plant communities associated with it. Lots of bedrock exposure (with fractures) in Navajo- supports JUNOST and FRAANO.Fairly steep COLRAM hill with fairly flat ATRCAN terrace below. Below terrace is Halls Creek. COLRAM hill has very coarse rocks throughout.Plot encompasses an area where TAMCHI have been cut down and is in the old river channel, now dry. Lots of dieback on the SALEXI and dead stands with some resprouts from the base. Understory is predominantly MUHASP. Deep, clay-loam soils with lots of litter and downed wood covering the surface.Sandy soil with fairly well-developed cryptos.Badlands covered with basketball-sized volcanic rocks. Gravelly rocks covering most of the rest of the surface. Weird rock wall of volcanic boulders just outside plot (N).Rolling badlands covered with baseball - basketball -sized black volcanic rocks. Surface also littered with small light - colored rocks.Rolling badlands with small rocks covering the surface. Many small channels dissecting plot in all directions.Narrow slotty canyon, very sheltered with 200 ft. sheer cliffs on either side.Narrow canyon, sheltered, with very steep walls. Tough to access!!This is an alcove with steep, bouldery slopes. Whole alcove is ~80m wide, & is surrounded by 150 ft tall Kayenta cliffs. Other Surface Geology: Talus.Slope is gullied with many large boulders, bits of bedrock and many small rocks on soil surface. More vegetation where soil is more developed, especially lower on the slope. Several dead Juniper trees on plot.Cow disturbance. As far as I can see this whole part of the valley has been artificially seeded with Agropyron cristatum. The shrubs are more sparse in the valley bottom, and there is more seeded grass.EN_ j + Ok{`!990MidslopeGPS@Obscured by Soil0500001-bT00300T0000hfdb`^\ZVTRMMKIGEA/#+12129Low slopeGPS*@Obscured by Soil08000002T0P00T0000igeca_][YWUQQOMKIE3'"874InterfluveGPS@ Dakota Sandstone051-aT00PT00400P0000jhfdb`^\XVTRRPNLGC1% 1299InterfluveGPSb@ Dakota Sandstone1-a1-aT00PT00700T0000mkigeca_[YWUUSQOJE3'"VariableVariableInterfluveGPS*@ Brushy Basin Shale Member of the Morrison Formation04P000P1-a00500T0000~zE94(649Step in slopeGPST@ Obscured by Soil0800001-b00000T0000kigeca_][YWRRPNLJF4(#625Step in slopeGPS@ Obscured by Soil0600000300000P0000jhfdb`^\ZXVRRPNLJF4(#3109Low levelGPS>@New Alluvium0601-a01-bCrypto1-a1-a01-a00P0000xvtrpnljec^YQLJEC?1% 1959MidslopeGPSr@Wingate SandstonePT0001-a0601-b00T0000ljhfdb`^YWSNNLJHFD1% v4105Low levelGPS@New Alluvium080P00PT01-b00T0000db`^\ZXVQOMKKIGEC?1% 3b0n/aLow levelGPS@Alluvial deposits0201-b001-b0401-b00T0000qomkigec^\XSSQOJHD1% 0P275Low levelGPS@Alluvial deposits0201-b00P1-b00600T0000mkigeca_[YTRRPNIGC0$3280MidslopeGPS@Kayenta Formation1-a000TbiocrustP080P00T0000sqomkigeca][QOMKID1% |)3175MidslopeGPS@Kayenta FormationP0000P080P00T0000fdb`^\ZXVTPNNLJHFD1% 84193Low LevelGPS@New Alluvium100000PT0T0000000a_][YWUSQOMKKIGEC?1% 6745High SlopeGPS$@Carmel Formation1-aT000T1-b0080000000kigeca_]YWRPPNLJHC1% e22100MidslopeGPS@ Carmel FormationPP000P050050000000hfdb`^\ZVTPNNLJHFD2&!2187Low slopeGPS@ carmel formation, Navajo sandstone1-a03000P1-b00500T0000~|zxvtrnlgeeca_[V2&!b1851MidslopeGPS@ Navajo Sandstone031-a000P030030000000ljhfdb`^ZXTRRPNLGC1% 0n/aLow levelGPST@ New Alluvium0600001-b000001-b0000geca_ZXVTRPKKIGEC?1% 195Low levelGPS!Broad terrace with sandy soils.New Alluvium0700000300T00T0000}{ywusqokkigec_Q$295Low levelGPS\@New Alluvium0800000200P00T0000b`^\ZXVTRPNJJHFDB>0$275MidslopeGPSZ@Carmel Formation1-b0000T050040000000hfdb`^\ZVTPNNLJHFA/#variablevariableMidslopeGPS@Carmel Formation1-b0000T050040000000|zxvtrpnjhdbb`^\ZUC72(vLVAL v8,Toeslope right at the edge of the valley where Notom Road runs through. Soils more rocky here than on the flats below where there's little to no PJ.Rolling toeslope with pebbly soil surface and sandstone showing through in places- soils appear thin here.Rolling toeslopes with tan, pebbly-sandy clayish soils. A few places with smooth, tan sandstone showing through. Slope is an average - many small channel running through plot.Pebbly rocks mixed into silty soil - colorful gray and red mud hills are visible just below point. Pretty exposed area - P-J looks a little stunted.Hard to find good topo position/ landform names here- nothing fits well. Broad slightly sloping area coming off the fold with deep soils. Lots of past grazing evidence.Broad slightly rolling area with some crypto development. Lots of old dead junipers around.Shallow Rocky wash about five to eight meters wide with rolling, hilly terraces on either side. Terraces not all that sandy, and have well- developed cryptos.Fairly steep colluvial slope with large (1-2 m) boulders.This is a broad terrace- more like a valley, with a shallow wash running though it.Shallow, rocky wash with narrow (5-8m wide) terrace surrounded by cliffs.Rocky, pebbly shallow wash about 15m wide and 0.5 m deep. Terraces on either side are sandy and narrow with many large rocks mixed in. Steep colluvial slopes beyond the wash terrace with PJ.Huge truck-sized (and house-sized) boulders jumbling down this slope. Healthy, big PJ's growing on soil pockets/ ledges between rocks.Very steep colluvial slope with huge semi/ RV- sized boulders scattered throughout. Healthy PJ growing where there are soil pockets though.Broad terrace above Halls Creek- very sandy soils. The slight rise that AA point is on is dominated by COLRAM- but ATRCON everywhere else.Rolling hills of Carmel over Navajo sandstone. Soil surface is covered with small red rocks (Carmel) and scattered large white rocks (Navajo ?).LVAL<< : F Lhb2"This AA point covers both sides of the steeply sloping benches on the floor of the canyon. Well developed, though rocky/bouldery soils.This AA point covers the benches on both sides of this wash, which is 2 to 5m across and has water flowing through it. Benches are gently sloping, 20 to40 m wide and about ten feet above the wash.Steep colluvial slope with large, one meter, car-sized boulders. PJ and shrubs growing between rocks in soil pockets.Fairly steep colluvial slope, but center of plot falls on a nice flat spot with well-developed soils & cryptos.Steep colluvial slopes above the wash, which is about 5 m wide. AA point encompasses both slopes above wash.Thin, very sandy soils over slickrock. Many little channels running through the area, which could explain why there's more AMEUTA?Steep-sided gully with narrow 1 m. wide wash at the bottom. Gully sides are rocky and have some bedrock exposure.I'm at the high point of the Circle Cliffs, a fairly thin layer of soil over Navajo sandstone (Navajo is visible outside plot to the east and west with large sloping cliffs!)Fairly thin soils over a layer of Navajo sandstone (visible just outside plot).This is a valley ~80m wide between two Navajo uplifts. Rolling, cracked slickrock is the dominant substrate.Sheltered wash in the hills just east of the Carmel/Navajo interface. Gently sloping terraces ~5-10 m. wide, with shallow wash ~3-5 m. wide.Broad valley bottom, ~50m from Notom Road. Evidence of having been previously trashed cows.Rocky uplift of sandstone- small-large rocks everywhere. Not sure of geology- could also be Salt Wash or Dakota? Grasses are mainly on the west side of this ridge.Rolling toeslope with pebbly soil surface and a bit of bedrock showing through in places. Soil is probably fairly shallow here.Rolling toeslope just above Notom Road Valley. Very pebbly soil surface and apparently deep soil.v] R  n " e gDbd50N/ALow levelGPS@Alluvial deposits040P004Crypto (pinnacles)T00000T0000|zxvtrpnljhfRNLJHD1% }variablevariableLow levelGPS@Wingate Sandstone030P0006P01-a00T0000~|zxvtrpkigcca_][WD83(2329Low slopeGPSD@Wingate Sandstone1-a000007000001-a0000mkige`^\ZXVRRPNLJE2&!2010MidslopeGPSz@Wingate Sandstone02000Pcryptos06P0P00P0000qomkigeca_]YPNLJHD1% 33340MidslopeGPS@Wingate SandstoneT0000020400300T0000kigeca_]YWSOOMKIGE2&!3386MidslopeGPS@Wingate SandstoneP0T00050200200P0000jhfdb`^\XVRNNLJHFD1%  V3269Low levelGPS0@Wingate Sandstone020T0003030P00P0000kigeca_][YUQQOMKIE2&! variablevariableLow levelGPSN@Wingate Sandstone1-aTT00071-a0T001-a0000~|zusqomhddb`^\WD83( HvariablevariableLow levelGPS@Wingate Sandstone1-a0T00071-b0T00P0000}{ywusqomhddb`^\WD83( |variablevariableLow levelGPS@ New Alluvium1-a000PWater04030P00T0000~|zxvtrpnjf_][YWRD83( 28345MidslopeGPS@ talus/ColluviumT0001-b0500400T0000hfdb`^\ZVTPKKIGGEC2&!e23249MidslopeGPS@ Obscured by Soil1-b000PBiocrust040201-b00P0000xvtrpnljec_[QOMKID2&!variablevariableMidslopeGPS@ Kayenta Formation03TP00T0400400T0000|zxvtrpnjhdbb`^\ZVC72(s513High SlopeGPS!Very sandy, duney rolling area.Eolian deposits0600000300000P0000}{ywusoomkigcR% v1470High SlopeGPS@ Kayenta Formation041-bT00041-a01-a0000000sqomkige`^YUUSQOJF3'"~1073Low levelGPS@Navajo Sandstone03PT00031-a00300T0000mkigeca_[YTPPNLJHD2&!677High SlopeGPS\@Obscured by Soil02000003P003001-a0000ljhfd_][WUSOOMKIGC1% 884High SlopeGPS@Obscured by Soil02T000031-a00300P0000ljhfdb`^ZXSOOMKIGC1% 13145Low levelGPS@Navajo Sandstone1-b07T00PP0P00T0000jhfdb`^\ZXVTTRPNJE3'"654Low levelGPS@New Alluvium0401-a00031-b01-b00P0000kigeca_]XVQMMKIDB>0$?0N/ALow levelGPS@Obscured by Soil090000P0000000000eca_][YWUSQOOMKIGC1% 25variableMidslopeGPSJ@Brushy Basin Shale Member of the Morrison Formation1-a1-a0001-a0200600T0000||zxvql7+&12100MidslopeGPS@Dakota Sandstone051-a00002T00200P0000mkigeca_[YWSSQOMHD2&!lLVAL ~ : | f 6^rThin sandstone layer of Mancos with patches of shaley soil on surface. Trees rooted in bedrock fractures.Near AA pt. 1052, but less steep, more (still thin) soils, less bedrock.Slope is the general trend of the top surface of the interfluve. Edges of plot may slope in a variety of aspects. Note that there's a cairn in the plot - old mineral claim?Paved road borders plot. Beavers have cut a number of Cottonwoods, reducing their number. Trees are mostly young, with some mature - no decadent individuals here.A fine, deep soil floodplain from a tributary wash to the Fremont River.Fine, deep soils of probable Summerville origin. This is an alluvial terrace or bench above the Fremont floodplain.Plot is in a broad, level flood plain of the Fremont River.Plot is located in a very disturbed area - next to a paved road and including a channelized wash (downstream of a culvert under the road).Disturbed areas of flood plain comprise half of plot - roads and nearby stock corral. Less disturbed areas are reflected in assoc. names and are a low flood plain with young POPFRE and Tamarisk and an understory of ERINAU.Very few trees on terraces, but more on hills.Deep, sandy soil with good crypto development (no lichens/mosses though) so seems stabilized.Plot encompasses both wash benches and the narrow wash in between. Wash has water flowing now.Well- developed, sandy soils here.Sandy soils here with well-developed cryptos in a few places.Steep, rocky slope. Majority of aspect is as stated above, but part of plot also wraps around to the NE.Steep, rocky/bouldery slope down to a narrow wash, which right not has water flowing in it.This AA point covers mostly the steep NE-facing slope of this side canyon. The narrow wash at the bottom & some of the opposite bank was included also.This AA point covers both sides of the steeply sloping benches on the floor of this canyon (right below a pouroff). Well developed, though rocky/bouldery soils here.]i * > v  ~7AKZ+c3352Low levelGPSDeep shaley soils.Mancos shale0800001-b00000T0000xvtrpnljhfd__][YWSE% *;0N/ALow levelGPSp@New Alluvium03000007T0000P0000ca_][YWUSQOKKIGEC?1% )-g2200High LevelGPS@ Eolian deposits07000PBiotic soil02T0T00P0000trpnljhfdb`\OMKIGC2&!(f2200High LevelGPSJ@ Mancos shale07000PBiotic soil0200T00P0000qomkigeca_]YLJHFD@2&!'h5284MidslopeGPS&@Mancos shale06P00TBiotic soil1-bT01-a00T0000sqomkige`^\WJHFDB>0$&nVariable120ToeslopeGPS<@Mancos shale0700000200000T0000pnljhfdb`^\XXVTRPL>2-#%91270MidslopeGPS@Mancos shaleP08T0PBiotic soilPP01-a00T0000qomkigec^\ZXKIGEA?1% $1170MidslopeGPS@Mancos shaleP0700TBiotic soilT1-b0T00T0000qomkigeca_ZXKIGEA?1% #7v48MidslopeGPS@Mancos shale031-a00PBiotic soil1-bP00300T0000rpnljhfd`^\WJHFD?;-!"1290MidslopeGPS@Kayenta Formation02020001-a0200200P0000omkigeca][WRRPNLHD1% !Us17120MidslopeGPS~@Kayenta FormationP05000P0301-a00T0000ljhfdb`^YWSQQOMKGE2&!  25262MidslopeGPSv@Chinle Formation0302000T0300300T0000ljhfdb`^ZXTRRPNLHD2&!VariableVariableToeslopeGPS6@New Alluvium1-a0P0TWater1-a0400400T0000~|zxvtpnje^\ZXVQC72(718132MidslopeGPS@Chinle Formation02P000TP00800T0000hfdb`^\ZVTRPPNLJHD2&!VariableVariableMidslopeGPS@Talus/Colluvium/Landslides03P00TBiotic soilP0300300T0000~zxkigec_C72(_>228High LevelGPS\@Talus/Colluvium/Landslides05000TBiotic soil1-b1-a00300P0000~|zxvrpkfYWUSQM1% I0N/ALow levelGPSH@New Alluvium0600000300T00P0000ca_][YWUSQOKKIGEC?1% N0N/ALow levelGPS@ New Alluvium0700000300000T0000ca_][YWUSQOKKIGEC?1% s3250Low levelGPS@ New Alluvium09000PCyanobacteriaT00T00T0000pnljhfdb`^\ZKIGEC?1% L0N/ALow levelGPSv@ New Alluvium0800000200000T0000ca_][YWUSQOKKIGEC?1%  389Low levelGPS@ New Alluvium0701-a0TBiotic soil02T0P00T0000rpnljhfdb`^ZMKIDB>0$2102Low levelGPS@ New Alluvium0600002Biotic soilPT0P00T0000pnljhfdb`^\ZMIGEC?1% Z0N/ALow LevelGPS\@Alluvial deposits03TT007CryptoT00000T0000pnljhfdb`^\ZRNLJHD1% 676Low slopeGPSNone.Obscured by soil03P000T00050000000mkigeca_[YWUUSQOMI7$_ W  y , y/S'tYmVariableVariableHigh LevelGPS<@Eolian deposits05TP003Biotic soil1-a00000P0000~|zxvqd`^\ZVE94(li2033MidslopeGPS,@Kayenta Formation050300PBiotic soil1-bP0P00T0000xvtrpnljhfd_RPNLHD1% ki4354Low slopeGPS@New Alluvium06P1-a01-bbiotic soil1-bP0T00T0000wusqomkigec^QLJEC?1% j10332MidslopeGPS@Kayenta Formation0402001-bBiotic soils1-aP0P00T0000}{ywusqomkidVQOMIE2&!ivariablevariableHigh LevelGPS@Eolian deposits0500301-bBiotic soil0200000P0000~|zxtgb`\ZVE94(hpvariable150High SlopeGPS^@Wingate SandstoneP0900PBiotic soilPT0000T0000~|zxvtrpnl_][YUS@4/#gRVariableVariableToeslopeGPS@Chinle Formation070000P1-a0020000000|zxvtrpnjhcaa_][YUC72(fm5336ToeslopeGPS`@Moenkopi Formation090000T00T0000000fdb`^\ZXVTRPPNLJHD0$e*980MidslopeGPS|@Moenkopi Formation1-aT000021-a0060000000mkigeca_[YTPPNLJHC/#d-l3110Low levelGPS@New Alluvium0P1-a00041-a0P00T0000geca_][YWUPLLJHCA?1% ce5170MidslopeGPS@ Kayenta Formationp0800PBiotic soilPP0P00T0000rpnljhfdb`^\OMKIEC0$b2098MidslopeGPSL@ Kayenta Formation0203000P0300200T0000ljhfdb`^ZXTRRPNLHD1% a~12162MidslopeGPSF@ Kayenta Formation1-a0500PBiotic soilsP0201-b00T0000}{ywusqojhdbTRPNJE2&!`10128High SlopeGPSp@ Kayenta Formation1-b0500TBiotic soilP0200200T0000}{ywusqokiecVTRPLG4(#_AR0n/aLow levelGPS@ New Alluvium0000009000001-a0000db`^\WUSQOMIIGECA?1% ^F0n/aLow levelGPS@New Alluvium040P0PWater04T0T00P0000jhfdb`^\ZXVRKIGEC?1% ].:0N/ALow levelGPS@New Alluvium1-a0P01-aWater07T0T00T0000nljhfdb`^\ZVOJHFD?1% \s70n/aLow levelGPS@New AlluviumP01-b0008T0T00P0000db`^\ZXVTRPLLJHCA?1% [J142Low levelGPSZ@New Alluvium050030002P0P00T0000db`^\ZXVTRPLLJHDB>0$Z%2variablevariableToeslopeGPSh@Salt Wash Sandstone Member of the Morrison Formation1-b1-a0001-a0200500T0000~yC72(YHn10266High LevelGPS@Salt Wash Sandstone Member of the Morrison Formation1-b030001-a0200300T0000~yywusoj4(#XU17229MidslopeGPSX@Salt Wash Sandstone Member of the Morrison Formation1-a0001-a0400500T0000~|xssqommh2&!W\13210ToeslopeGPS@Chinle Formation1-bT000P0300600T0000kigeca_]YWSQQOMKID2&!^H - " k  y/.>Itp240High SlopeGPSh@Carmel Formation1b1a001bcrypto1a02005001a0000ywusqmkiec_[SOMKGC1% so940MidslopeGPS@Entrada Sandstone0500004biocrustPT0T0000000pnljhfdb`^\ZPLJHFB/#rn 10122High SlopeGPS(@Carmel Formation1a00001a0008001a0000nljhfb`^ZXVRRPNLJF4(#qm0n/aHigh LevelGPS@Eolian deposits040001acrypto1a0004001a0000usqomigea_]YQMKIGC2&!plvariablevariableLow slopeGPS@Entrada SandstoneT06000T020020000000}{ywusqokiecca_]YWD83(ok 5102High SlopeGPSF@Boulder depositsT0000081-b0T00P0000igeca_][YWRNNLJHFD2&!nj 1550ToeslopeGPS@Boulder depositsT0T00081-b0T00P0000hfdb`^\ZXVQMMKIGEC1% mi!variablevariableInterfluveGPS\@Carmel Formation03P000PT00600T0000{ywusqomigecca_][WE94(lh32variesInterfluveGPS@Carmel Formation08P0001-aT01-b00T0000qomkigec^\ZUUSQOMI7+&kg 166High SlopeGPS@ Carmel Formation02000Pcrust04T004001-a0000sqomkfdb^\ZVOMKIGC1% jfa 1490High SlopeGPS`@ Carmel Formation00000T000900T0000geca_][YUSQOOMKIGE3'"ieI variesvariesLow levelGPS@ Navajo Sandstone04T000041-a0P00P0000wusqomkige`\\ZXVTP>2-"hd:17172High SlopeGPS@Carmel Formation05P000TT00500T0000jhfdb`^\XVTRRPNLJF4(#gc3 35324ToeslopeGPSv@Navajo Sandstone030000020300200T0000ljhfdb`^ZXTPPNLJHD2&!fb3133High LevelGPS@Obscured by Soil1-b0001-acrypto041-b0P001-a0000zxvtrmkige`\TOMKID2&!ea11173High SlopeGPS@Boulder deposits1-b0001-bMoss, Cryptos020300200P0000}{ywusomieVQOMKF4(#d`1329ToeslopeGPSl@Obscured by Soil0400004Dark Cyano0200000P0000usqomkigeca]QMKIGC1% c_ variesvariesInterfluveGPS @Navajo Sandstone030300PCryptos03P0T00P0000~|zxvtrpnlh_][YUQ?3."b^58100High SlopeGPS@Boulder deposits000002crypto1a0200600T0000trpnljhfb`\XPLJHFD2&!a]x0n/aHigh LevelGPSl@Obscured by Soil0400000400P00T0000hfdb`^\ZXVTPPNLJHD2&!`\s7156High SlopeGPS@Salt Wash Sandstone Member of the Morrison Formation0200001-a1-b0060000000~yttrpnlh2&!_[ variablevariableHigh LevelGPS@Boulder deposits01b1a00071b0000T0000}{ywusqomieeca]YWE94(^ZvariesvariesLow levelGPS@ New Alluvium0300004dark cyano1-b1-b0P0000000~|zxvtrpkfZVTRPL>2-"+"P M|  ) e J \ HAc2.Ed5Bk6dmi u@X4ͮ@tlkpPhysiogClassSk@ NNNBBBBBBB@ @fe u@UF@tlkpPhotoTypesS@ JJJ>>>>>>>< @^x8-@8-@tlkpPhotographerS@ NNNBBBBBBB@ @)8-@)8-@tlkpPhotoCommentsS@ PPPDDDDDDDB @b u@UF@tlkpParksS@ @@@44444442 @,\ u@X4ͮ@tlkpLeafTypeSa@ FFF:::::::8 @! 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Drainage  Dunes Dune dunes valley bottom Bench valley bottom Toeslope hogback Wash terrace Valley floor Mesa Terrace Terrace Second terrace stream terrace Terrace wash terrace valley side  Valley side  Valley  Valley side  valley floor  hogback  Hogback Valley side dunes Wash wash terrace Wash terrace Wash terrace wash terrace &nO/ yX7 u U 5   g N 3   k T < % t T ; "  x ` D *  jP2}fO8! nJ3kP6}_=&v[@% dH0fM4 Canyon  Canyon  canyon  Canyon floor  canyon side canyon side canyon side monocline  monocline  gully  monocline  Monocline  valley wash terrace valley floor Ridge toeslope toeslope toeslope toeslope toeslope Toeslope toeslope toeslope wash ridge Valley wash wash Colluvial Slope canyon side Valley floor hill Hill monocline Hill Old oxbow Floodplain Terrace Badlands badlands Badlands canyon floor canyon floor alcove Colluvial slope valley Wash Erosional gullies valley Interfluve Slope Slope slope wash bottom Rise Rise rise Rise rise Slope valley valley Monocline valley Ridge canyonlands Canyonlands plateau canyon valley side Colluvial slope Ridge valley sand ramp Terrace terrace sandsheet bench Landslide deposits valley basin Basin Drainage stream terrace valley valley valley bottom dune dune Canyon bottom Canyon canyon canyon Ridge Dune Ridge Dune ridge Slickrock basin Valley Colluvial slope Colluvial slope Basin canyon mesa top Canyon Canyon badlands colluvial slope Colluvial slope Colluvial slope Plateau plateau Valley bottom valley bottom valley bottom stabilized dune valley bottom Valley bottom Valley bottom valley bottom stream terrace stream terrace stabilized dune stabilized dune Wash slot canyon toeslope petrified dunes Valley bottom Valley floor toeslope Valley bottom Valley floor canyon Valley floor &iF*{^A# | d L '  a B #  n O 5  f L 2  s Q :  mJ+vS9  }Y6iP7qT8fF-kQ2hQ1valley bottom Hill hill ridge slope Mesa Hill Stream terrace Terrace Terrace Valley floor terrace terrace Terrace Terrace Valley bottom floodplain Valley bottom Wash canyon canyon bottom ~Strike valley }Monocline |terrace {Terrace zwash yplain xplain wToeslope ~vhillslope }uInterfluve |tInterfluve {sInterfluve zrPlateau yqValley xpValley woalluvial terrace vninterfluve umvalley tlvalley skValley rjvalley qihillslope phHillslope ogvalley nfhillslope meHill ldwash kcAlluvial terrace jbAlluviall terrace iaalluvial terrace h`alluvial terrace g_alluvial terrace f^Alluvial terrace e]Wash d\Valley c[hogback bZstabilized dunes aYstabilized dune `XStabilized dune _WStabilized dune ^VValley ]Udune field \TValley [SStable dunes ZRStabilized dunes YQdune field XPAlluvial terrace WOalluvial terrace VNalluvial plain UMAlluvial plain TLartificial embankment! SKwash RJColluvial slope PHterrace OGstream terrace NFValley side MEFins LDfins KCmonocline JBmonocline IAplateau H@plateau G?Canyon side F>Plateau E=ridge D<Ridge C;Ridge B:Ridge A9Ridge @8valley floor ?7hogback >6valley floor =5Valley floor <4Valley floor ;3Wash terrace :2valley floor 91Hogback 80valley floor 7/valley floor 6.Valley floor 5-valley floor 4,valley floor 3+Valley floor 2*stream terrace 1)bench 0(Bench /'Bench .&Valley bottom/side -%bench ,$bench +#bench *"Monocline )!Monocline ( colluvial slope 'Gully &Interfluve %Gully sides $Interfluve #floodplain "Floodplain !bench  floodplain Floodplain Floodplain Alluvial terrace Hillslope alluvial terrace Canyon floor canyon side canyon side Canyon side canyon side &~^>ybK4 n N .  e I ,  t T 8  y b K 1   ~ d K 2  }`D-kS;!eM1{aJ0gN5rZB*x^F/y_E*Plateau )Plateau (Plateau 'ridge &ledge %badlands $Badlands #Badlands "Badlands !Mesa  ridge Plateau Plateau plateau Bench plateau plateau Plateau Bench Bench bench Bench Bench bench bench bench Bench Draw Badlands  Canyon  Canyon  Canyon  Canyon  plateau Canyon rim Plateau Hill Hill Plateau Rise Plateau hill Plateau hillslope bench Bench Bench Plateau Hillslope hillslope hillslope bench  hillslope plateau Canyon Hillslope hillslope plateau plateau Plateau slope Bench Bench Hillslope Hillslope wash alluvial terrace Hillslope hillslope Flat Hillslope Interfluve zBank fold Canyon Hogback drainage Wash Colluvial Slope alcove Canyon Terrace Floodplain Terrace Valley floor Mesa Slope Mesa Mesa Terrace Mesa Mesa Valley floor Terrace Creek wash Mesa valley bottom valley bottom creekside Valley bottom Valley bottom Depression Old river channel Depression Depression Depression Interfluve Hillslope canyon side terrace toeslope Toeslope Toeslope Canyon bottom canyon bottom Canyon bottom Canyon bottom canyon bottom canyon bottom terrace terrace strike valley toeslope Wash wash fold Wash Wash wash Wash Valley bottom Valley bottom valley bottom valley bottom valley bottom Valley bottom Hill terrace Terrace Wash valley bottom LVAL ,& z ,P*Deep, sandy soils. Lots of dead JUNOST skeletons. In contrast to AA 711, nearby soils here have an aeolian character, with some shrubs collecting drifted soil around them. Soil surfaces are stabilized, however, with lots of physical crusting.Flat area along rim of small canyon. Relatively deep, sandy soils on top of the rim-forming sandstone layer in Mancos. Lots pf dead (old) juniper skeletons in area.Deeper soils here, with minor surficial gullying throughout polygon. Lots of dead standing (old) trunks of juniper. Wind and rain are ubiquitous!Part of plot is on Mancos toe slopes, the rest on lower-angle valley floor. Species are slightly segregated by these various slopes, but ATRCON is universal.Most of community is limited to small joint-pattern gully or wash in white "slickrock" member of Mancos. Slope is actually variable throughout plot, but majority of veg. is in gully w/similar slope & aspect.White "slickrock" layer in Mancos, with vegetation limited to small pothole gardens and joint fractures.Association is on tilted, stratified beds of Kayenta along the crest of the Waterpocket Fold monocline. Lots of bedrock to collect water for veg. - most of which is in cracks or thin soils.Plot is on a colluvial slope with lots of exposed Chinle bedrock. Most of talus/soils are also Chinle-derived. This band or layer of Chinle has a fair amount of thin limestone outcrops.Plot is in a narrow, steep-sided gully or wash, with most vegetation on the banks. Banks are generally cut into the toeslopes of surrounding talus slopes.High small rock surface cover is similar to desert pavement, though it looks like surface gets stirred a bit by freeze-thaw cycles.Some of plot includes a steep-sided gully cut through the veneer of talus into the Chinle. The rest of the plot is still steep, but less so, and has more colluvial cover. Short (S2) shrubs were all in the steep, inner gully channel.vLVAL " , j vSteep, rocky slope. Grasses have soil/rock piled up against their uphill sides. Slight gully transects plot, doesn't seem to affect shrub cover.Deep, sandy soils. Navajo-derived. Stable under tree crowns and litter. Slightly duney under ARCPAT. Old growth PJ. Less duney, more litter than AA1356.Deep, shifting sands in between tree crown litter areas. Navajo-derived sands. These are old growth trees.Shallow canyon side w/layers at base of Navajo formation. Ledgey outcrops w/deeper sandy soils on flatter areas.A little more clay in soil, and a little rockier than previous pts. in polygon to S of here.Several small, shallow washes run through plot, and shrubs are concentrated here.Sandy soils on a narrow ridge crest area. Some areas of active dunes.Sandy soils. No dune evidence here.Deeper , sandy soils. Some evidence of blowouts in opening between crowns (small rock in surface of slight depressions), but needle litter is extensive and indicates stable (if slightly mounded) soils under trees.Some areas have duney character - these tend to be sparse understory. Others have stable, rocky soils - and have the Shepherdia. Ledgey areas favor the Cercocarpus.Slope is an average of steeper slope on E side of plot and toe slopes on W. Soils are deep, shaley clay.Low areas near wash - in the flood plain only during apocalyptic events. Highly disturbed.Plot includes flat areas and some areas inclining downwards to polygon to W. Deep, shaley soils.Deep, shaley soils in the lower Mancos. Area is on valley floor, not in the wash floodplain, but neither is it a toeslope.Fine, sandy soil on a low hill in the valley floor - presumably alluvial sands remaining from an eroding alluvial plain.A sandstone layer of lower Mancos creates a ledgey hogback here. CERINT is on exposed bedrock areas, other shrubs are in deeper soils.Deep, shaley soils heavily transected by narrow gullies.Deep alluvial soils transected by deep drainages nearby.+R T d  j 3GLQ iCF1724MidslopeGPS^@Kayenta Formation02T000030300300T0000ljhfdb`^ZXTPPNLJHD1% B1842MidslopeGPS$@Kayenta Formation02P000030300300T0000ljhfdb`^ZXTPPNLJHD1% A444MidslopeGPS8@Eolian Sands03PP0PBiotic soil0500000P0000nljhfdb`^\ZVIGECA=/#@~338MidslopeGPS@Eolian Sands030030PBiotic soil0200000P0000pnljhfdb`^\XKIGCA=/#?25262MidslopeGPS@Navajo Sandstone0202000020200200P0000nljhfdb`\ZVRRPNLHD2&!> 3204High LevelGPS@ Kayenta Formation04000TBiotic soil031-b00200P0000{ywusqomigb^QOMKIE2&!=}5222High SlopeGPS@ Kayenta Formation08T00TBiotic soil1-aP00200P0000ywusqomkgec^QOMKIE2&!<o844High SlopeGPS@ Kayenta Formation030030003P0T00P0000jhfdb`^\ZXVRRPNJHD1% ;0N/AHigh LevelGPSH@ Kayenta Formation04000PBiotic soil0400000P0000vtrpnljhfdb^QOMKIE2&!:T230High LevelGPS@ Kayenta Formation04TT000500T00P0000hfdb`^\ZXVTPPNLJHD1% 97242High SlopeGPSL@Kayenta Formation04P020TBiotic soil03T0P00P0000xvtrpnljhfd`SQOKIE2&!80N/ALow levelGPSNoneMancos shale0800001-b00T00T0000jhfdb`^\ZXVQQOMKIE7% 7/22308ToeslopeGPS@Mancos shale10000000000000000b`^\ZXVTRPNLLJHFD@2&!6*o0N/ALow levelGPS@Mancos shale06000TMoss0300000T0000igeca_][YWUQKIGEC?1% 5gVariable308Low levelGPS@Mancos shale0800001-a0000000000rpnljhfdb`^YYWUSQM?3.#4Sy3122Low levelGPS@Mancos shale0700000200T00T0000ca_][YWUSQOKKIGEC?1% 3z0N/ALow levelGPS Low wash terrace w/sandy soilsNew Alluvium060P000300T0000000}{ywusqokkigec_Q% 2#~18Step in slopeGPS@New Alluvium0900001-b00000T0000eca_][YWUSQLLJHFD@2&!12288MidslopeGPS@Mancos shale031-b0001-a0200300T0000kigeca_]YWSNNLJHC?1% 01290Low levelGPSDeep, shaley soilsMancos shale09000Pmoss1-a00000T0000~|zxvtrpnlje_][YWSE% /3280Low levelGPSDeep, shaley soils.Mancos shale09000Pmoss1-a00000T0000}{ywusqomkf`^\ZXTF% .~3268Low levelGPSp@Mancos shale0900001-a00000T0000db`^\ZXVTRPKKIGEC?1% -u3264Low levelGPSDeep, shaley soils.Mancos shale0800001-b0000000000ywusqomkige``^\ZXTF% ,B3278Low levelGPSDeep, shaley soils.Mancos shale080000020000000000xvtrpnljhfd``^\ZXTF% LVAL|P B h zll*((Point is on hogback ridge with steep slope, vegetation growing in benches near top of hogback, benches are about 20 ft by 10 ft.In the Navajo domes, in the flat area where alluvial and eolian deposits had woodland.Level area within Navajo domes that have alluvial and eolian deposits of sandy soil that is formed into duney areas of woodland.This is a small woodland on sandy deeper duney soil. Soil was brought in by wind and water and deposited to Navajo dome level areas.This point is a high level duney woodland wind deposited sand that is stabilized (has crust development & litter).E side has stable dunes, but W side is sandy & flat.Flatter sandsheet area of valley.Has some stable dunes hence the variable slope & aspect.Stable dunes that have high cover of pinnacled crypto crust in a valley.Stable dunes with high crypto soil in valley.I used terrace because there is a bank to the river and the point is on the alluvial soil.This point lies on an embankment (man-made) in the same alluvial plain as point 1414 that is next to the Fremont River.Point on a colluvial slope w/Navajo rock exposed.Majority of plot is on a stream terrace about 1 meter above wash channel bottom. Lots of dead ARTTRI-T, especially in areas farther from wash channel.Plot includes a major wash channel and the banks on either side, plus a broad terrace/floodplain about 1 meter higher than wash bottom. Lots of dead ARTTRI in area.Plot straddles a low ridge on deep, clay Mancos soils. Slopes range from 25 to 5 degrees. Aspect doesn't appear to affect vegetation.Slope and aspect across plot are highly variable, but #'s represent the drainage areas where veg. is located. Steep sandstone fins transect polygon.Relatively flat, sand soils between sandstone fines. Community is well-watered by run-off, and shallow drainage channels transect vegetated areas.Rocky soils and ledges. Trees look young here.ae  t ( v  B 5t0B[A2668High SlopeGPS@Mancos shaleT09000TT0T00T0000ca_][YWUSQOMMKIGCA3'"ZDh0n/aHigh LevelGPS@Alluvial depositsT03T01-bcryptoP0200300T0000vtrpnljhdb^\TOMKGE2&!YJ0n/aHigh LevelGPS@Alluvial depositsT02T002cryptoP000200T0000sqomkigea_][SOMKGE2&!XA0n/aHigh LevelGPS @New AlluviumT05T004cryptoPT0P00T0000ljhfdb`^\ZXVNJHFB@2&!WPA0N/AHigh LevelGPS@New AlluviumP05P004CryptoPT0P00T0000ljhfdb`^\ZXVNJHFB@2&!V`VariableVariableLow levelGPSh@ Alluvial deposits1-a01-a006CryptosT001-a0000000}xvtriec^\WD83(UeVariableVariableLow levelGPSStable dunes in valley.Alluvial deposits1-a01-a007CryptoT0000000000~|wup]83(TiVariableVariableLow levelGPSB@ Alluvial deposits1-a01-a006CryptoT0000000000}{ywusqiec^\WD83(ShVariableVariableLow levelGPSp@ Alluvial deposits1-a01-a006CryptoT0000000000}{ywusqiec^\WD83(ReVariableVariableLow levelGPS@ Alluvial deposits1-a01-a006CryptoP0000000000}{ywusqiec^\WD83(Q;eVariableVariableLow levelGPSZ@ Alluvial deposits02002005Crypto (no lichens/mosses, but pinnacled)T0000000000gca][WD83(P0N/ALow levelGPSNone.Alluvial deposits030P007CryptoTT000000000wusqomkigecaYUSQOK8% O(0N/ALow levelGPS@Alluvial deposits0801-a002CryptoT0000000000sqomkigeca_]UQOJHD1% N0n/aLow levelGPSOff Scenic Drive.Alluvial depositsP008001-a00T0000000|zxvtrpnljhcca_[YWD% M0n/aLow levelGPSOff Scenic DriveAlluvial depositsT00600020000000000zxvtrpnljhfbb`^ZXVC% L0n/aLow levelGPS@Alluvial deposits080000T00P0000000fdb`^\ZXVTRPPNLJHD1% K0N/ALow levelGPSNone.Alluvial depositsP00800P00P00T0000mkigeca_][YWWUSOMK8% JR1468MidslopeGPSb@Navajo SandstoneT09T0TCrypto, dark cyanoTP0P00T0000ywusqomkigecOMKIEC1% H}264Low levelGPS.@New Alluvium080P0TMoss1-b00T00T0000igeca_][YWUPJHFDB>0$G{VariableVariableLow levelGPSJ@New Alluvium060P0002T0T00P0000vtrpnljhfdb^^\ZXVRD83(FkVariableVariableToeslopeGPS@Mancos shale070000P0000000000sqomkigeca_]][YWUQC72(E2160Low levelGPS,@Mancos shale1-b07P0TBiotic soilPT0T00T0000qomkigeca_][NLJHD?1% D22138Low levelGPS&@Mancos shale02051-a00P1-a0P00T0000igeca_][YWRPPNLGC?1% LVAL8 > T & :H6tA low level plain in which there are many washes running throughout. Deep sandy soil hence I called it alluvial deposits.Deep sandy soil bisected by washes.This is in the Morrison soil area on the bottom of a hillside. The hillside is adjacent (bottom of ) a plateau.This is higher up on a toe slope (to a plateau) in the Morrison soil area.This is an area that is lower compared to surrounding formations and is bisected by many washes, soil is Morrison.This is in an area that leads to a plateau, but the soil is Morrison and very bisected by washes.Area that leads to higher plateau; is bisected by many washes (hence interfluves).Deep sandy soil with crypto development and some dunes.The point is between two large, steep-sided washes/rivulets (in a valley), deep shaley soil.Centroid is on one side of interfluve but point encompasses both sides of interfluve.Low area with washes throughout. Note weeds are 16% of herbaceous cover.Clayey soil that has rivulets running throughout valley.Valley of clayey Mancos soil with rivulets running throughout.Deep sandy soil with good pinnacled crypto soil.Along Notom Road. Some evidence of physical crustingon a hill, soil has evidence of physical crusting.Geology obscured by soil. There is pinnacling of soil, but I think it is more a physical crust than crypto. There is pinnacling to soil but I thin it is more a physical crust than crypto crust.Soil is deep, sandy on alluvial bench in a valley.In an alluvial terrace in a valley.On an alluvial terrace in a valley.On an alluvial terrrace in a valley.The point is on an alluvial terrace with deep narrow washes running throughout. Soil is clayey. Point is in a valley bottom.Point is right at wash, therefore primary name, but on E side is SARVER/ARTTRI (closest to point) & further east and W side of bank is SARVER/ATRCON.This point is within a pocket of solid ground that turns into many rivulets and washes to the North.9i6 b  j 0 ?X [_wsvariablevariableToeslopeGPS@Brushy Basin Shale Member of the Morrison Formation000004Cryptos with lichensP000400P0000~|zxC72(r0n/aLow levelGPSn@Eolian deposits1-a00004Crypto, moss, lichens1-b000001-a0000~|wusqomhQMKIGB1% qo0n/aLow levelGPSDeep shaley soils.Mancos shale070T00T0000000000usqomkigeca__][YWSE% ps0n/aLow levelGPS@Mancos shale090000T0000000000a_][YWUSQOMKKIGEC?1% oa0n/aLow levelGPSPoint off a wash.Alluvial deposits080T00P0000000000ywusqomkigecca_][WD% npvariesvariesToeslopeGPS@Alluvial deposits05TP00TT00500T0000trpnljhfb`^\\ZXVTP=1,"mi0n/aLow levelGPS@ Alluvial deposits08000TcryptoP0000000000nljhfdb`^\ZXPNLJHD1% l:o0N/ALow levelGPSp@ Mancos shale080T00P00000T0000a_][YWUSQOMKKIGEC?1% k\p0n/aLow levelGPSValley of clayey Mancos soil.Mancos shale080T00P00000T0000~|zxvtrpnljjhfdb^P% j)z0n/aLow levelGPS|@ Mancos shale080T00P001-a0000000db`^\ZXVQOMKKIGEC?1% i5302Low slopeGPS`@ obscured by soilT0P008cryptoP00P00T0000mkigeca_][YWOKIGEC1% hp3354Low slopeGPS On a hill.Obscured by soil04000PcryptoPT00400T0000{ywusqomigec[YWUSO=% go0n/aLow levelGPSj@ obscured by soil040P00PT00400T0000geca_][YUSQOOMKIGC1% fCm5328Low slopeGPSd@obscured by soil040000PT00400T0000geca_][YUSQOOMKIGC1% e"g6144Low slopeGPS@Obscured by Soil040000TP00400T0000geca_][YUSQOOMKIGC1% dP0n/aLow levelGPSPoint on a wash bankAlluvial depositsP00800TP0P000000zxvtrrpnljhffdb^\ZG% c0N/ALow levelGPSVery close to bank.Alluvial deposits070P00PT000000000{ywusqomkigeeca_]YF% bO0N/ALow levelGPSd@New Alluvium080T00P0000000000a_][YWUSQOMKKIGEC?1% at0N/ALow levelGPSF@Alluvial deposits080000T0000000000fdb`^\ZXVTRPPNLJHD1% `0n/aLow levelGPSF@Alluvial deposits080000T0000000000fdb`^\ZXVTRPPNLJHD1% _0N/ALow levelGPSH@Alluvial deposits080000T0000000000fdb`^\ZXVTRPPNLJHD1% ^0N/ALow levelGPS@Alluvial deposits080000P0000000000fdb`^\ZXVTRPPNLJHD1% ]0N/ALow levelGPS*@New AlluviumP00800000T0000000a_][YWUSQOMKKIGCA?1% \[0n/aLow levelGPS@New Alluvium090T00P0000000000a_][YWUSQOMKKIGEC?1% G8o  ]  { EMXp-0N/ALow levelGPS@New Alluvium0200003Dark cyano03000001-b0000trpnlgeca_]YMIGEC?1% 0N/ALow levelGPSj@New Alluvium0201-a003Cryptos03000001-a0000trpnlgeca_]YPLJEC?1% 0n/aLow levelGPS@New Alluvium0600000200000P0000ca_][YWUSQOKKIGEC?1% rn/an/aLow levelGPST@New Alluvium0501-a000300P00P0000jhfdb`^\ZXVRRPNIGC5)$i0n/aLow levelGPSD@New Alluvium0700001-b001-a00T0000geca_][YTRPKKIGEC?1% ^0n/aLow levelGPS@New Alluvium0501-a002Dark cyanoPP01-a00T0000usqomkigb`^\PLJEC?1% 2240Low levelGPS@ New Alluvium0301-a004Dark cyanoPP0P0000000rpnljhfdb`^\PLJEC?1% n/an/aLow levelGPS.@New AlluviumP0001-bMoss1-a1-a00500T0000trpnljhfb`[VPKIGEC5)$m0n/aLow levelGPS"@New Alluvium06000PCryptos1-bT0T00T0000mkigeca_][YTKIGEC?1% 0n/aLow levelGPS@New Alluvium0500001-aP00300T0000fdb`^\ZXTRPKKIGEC?1% 2570MidslopeMapr@Talus/Colluvium/LandslidesPP0001-b0701-a00P0000usqomkigb`\WWUSQOM1% VariableVariableToeslopeMap@New Alluvium020P00061-a0P001-b0000{ywusnljhfa]][YWUQC72(~0N/ALow levelGPS@New Alluvium0900001-a00000T0000db`^\ZXVTRPKKIGEC?1% }p452Low slopeGPSx@Carmel Formation050P0004P0P00T0000fdb`^\ZXVTRNNLJHFB0$|345Low levelGPSZ@New Alluvium040P0004P01-a00T0000eca_][YWRPNJJHFDB>0${356Low levelGPSv@New Alluvium050P0003P0P00P0000b`^\ZXVTRPNJJHFDB>0$z0n/aLow levelGPSNoneAlluvial depositsT0P005crypto02T0T001-a0000ywusqljhfdb^VRPNLJ7% y0n/aLow levelGPS@Alluvial depositsT0T007cryptoP00T00P0000nljhfdb`^\ZXPLJHFD1% x0n/aLow levelGPSF@Alluvial depositsT0T006crypto0200T00T0000pnljhfdb`^\XPLJHFD1% wl2238Low slopeGPS@Brushy Basin Shale Member of the Morrison Formation00T004cryptoP000400T0000~|zrnljhf1% v22238ToeslopeGPS@Brushy Basin Shale Member of the Morrison FormationT0T004cryptoP000400P0000}{somkig2&!uvariesvariesToeslopeGPS@Brushy Basin Shale Member of the Morrison FormationT0T004cryptos with lichensPP00400T0000~zxvtr=1,"t>variablevariableToeslopeGPS@Brushy Basin Shale Member of the Morrison FormationT0T004cyano with lichensP000400P0000~|zxC72(&LVAL 0 * $(HTwo drainageways (~1/2 sq. meters) run SW through the S and N sides of the plot. Lots of dark cyano cover in the flat area between drainages. Two anomalous POPFRE seedlings growing in the drainages.A hodgepodge polygon with vegetation growing linearly, parallel to Highway 112, the most mesic species farthest from the road. (See drawing on sheet).Depression area adjacent to highway, dominated by mesic species. CHRNAU abundance could be due to roadside disturbance. Anomalous TAMCHI patch.A disturbed area close to the east entrance road to CARE dominated by ATRCAN, CHRNAU, and SARVER. Point fell in a broad wash channel and encompassed parts of a pull-out road, so CHRNAU density may be higher in plot, and ATRCAN-SARVER look more dominant outside plot in polygon. Small TAMCHI patch adjacent to wash and road.Steep, colluvial slope at the head of a canyon below large Wingate cliffs. Colluvium are car to truck sized. Vegetation growing mostly on the sides of the canyon, both N and S-facing.Slightly ecotonal because I'm near the edge of the polygon. Lots of downed wood. Steeper bank slopes have more bare soil, but still lots of litter under the QUEGAM. Understory shrubs still the same as rest of the polygon, but canopy is becoming less dense.Broad, flat valley, trashed from grazing. This stand occurs on a broad terrace. JUNOST seems more associated with the wash below on one side, and the toeslopes of the Carmel Formation on the other.This community growing on the benches that slope directly from the Carmel hills to the wash at the mouth of a canyon in the Waterpocket Fold. Wash cut very deep/sharp here - ~5-6 ft deep.Fairly narrow benches (~20m wide) above a wash at the mouth of a canyon in the Waterpocket Fold. Steep Carmel Hills with sparse vegetation just outside plot on either side.Plot is right at the entrance to a canyon coming out of Waterpocket Fold. Benches above this wash are broad, slightly rolling, and sandy. Plot crosses wash and encompasses both benches.LVAL d : \bLedgey slope with many bands of slickrock outcrops which are crumbling and covering the slope with flat rock flakes. P-J are fairly sparse here and there's lots of unvegetated ground.Steep, W-facing slope covered in flat rocks. Lots of unvegetated areas between trees, as EPHVIR grows clustered around trees and grass clumps are small.Plot centered in a large wash that is flowing, but shallow. Slopes on either side of the wash face N & S and have exposed bedrock ledges breaking off into rock chunks that cover the surface. Smaller rocks cover the surface on top where it flattens out.Plot encircled both the W & E banks of Hall's Creek (as well as the creek between). POPFRE here are mostly seedlings along the banks.Closer to the creek here, so POPFRE are younger. CHRNAU is the only dominant shrub in the understory, but there is also an abundant herbaceous layer. Many individual POPFRE trees with small canopies and some dead branches.Lots of downed POPFRE branches. POPFRE look mature and have some die-back. Lots of Opuntia in the understory!POPFRE Woodland with fairly dense and really diverse shrub understory on a stream terrace. Lots of branches and litter on the ground surface; also a lot of die-back on the Baccharis. Not an ecotone because shrubs are mixed throughout area, in strips or clumps, but doesn't look like 2 separate communities.Seems like a disturbed site because of the abundance of Bromes. Lots of die-back on the TAMCHI.Deep, sandy soils of the creekside terrace. Lots of understory diversity here. Second level terrace POPFRE look mature, but those right along the creek edge look young.Deep, alluvial soils on a terrace.Deep, alluvial soils on this terrace, somewhat stabilized by cryptos. Plot includes a part of Hall's Creek Trail and a wash (~2 m. deep by 5-15 m. wide) with a few large PURMEX growing in it. Understory on the terrace dominated by weedy annuals and OPUPHA.Y O 6  rSNR>VariableVariableToeslopeGPS@New Alluvium1-aT1-a00040200200P0000}{ywusqokieaa_]XVQC72(<VariableVariableToeslopeGPS@New Alluvium1-bP1-b01-bCryptos031-b01-b00P0000}xvqmd_]XVQC72(0N/aLow levelGPS@New Alluvium02P1-a00020300200T0000jhfdb`^\XVRNNLJEC?1% 4360Low levelGPS$@Obscured by soil0600002Dark cyano02T0P00P0000usqomkigeca]QMKIGC1% q4190Low levelGPS@ Obscured by soil0600002Cryptos1-bT0P00P0000sqomkigeca_ZQMKIGC1% .9312Low levelGPS@Obscured by soil0400003Cryptos0300T00P0000rpnljhfdb`^ZQMKIGC1% 6320Low levelGPS@Obscured by soil0400002Moss, cryptos02P01-a00P0000{ywusqomhfd`QMKIGC1% y4330Low levelGPS@Obscured by soil060001-bdark cyano0200T00P0000vtrpnljhfdb^RMKIGC1% 5360Low levelGPS@Obscured by soil0500002Cryptos03T0T00P0000rpnljhfdb`^ZQMKIGC1%  13113MidslopeGPS@Brushy Basin Shale Member of the Morrison Formation031-b000021-a00200P0000zvvtrpkg2&!VariableVariableLow levelGPS@New Alluvium0300003Cryptos, moss0300000P0000}{ywuso`\ZXVRD83(`2335Low levelGPS@New Alluvium06000003T0T00T0000ca_][YWUSQOKKIGEC?1%  4170Low levelGPS@New Alluvium03000PCrust04P01-a00T0000mkigeca_ZXVRKIGEC?1% 480Low levelGPSr@Obscured by soil0400003Moss, cryptos02001-a00P0000zxvtrpnlgec_PLJHFB0$480Low levelGPS@Obscured by soil (Salt Wash of Morrision)0400002Crusts0300P00P0000}{ywuqieca_[0$2460MidslopeGPSz@Moenkopi FormationP1-b001-bCryptos1-a1-a00600P0000|zxvtrpnjhc^UPNLGE1% v479MidslopeGPSf@Moenkopi Formation1-b0001-aCrusts02P00600P0000usqomkigca_[SNLJHC/#-VariableVariableHigh LevelGPS@Moenkopi Formation1-aP001-aCryptos1-bP00500P0000{ywridb`^YE94(17203MidslopeGPSp@ Moenkopi Formation1-a020001-a02003001-a0000usqomhfd`^ZUUSQOKF2&!D21270High SlopeGPS2@ Moenkopi FormationPP000020200500P0000nljhfdb`\ZVRRPNLJH4(#VariableVariableHigh LevelGPS@Moenkopi FormationP03P0PWater020200300P0000~|zvtpleca_[YE94(]0N/ALow levelGPS @New Alluvium0300301-aWater1-aP00200P0000rpnljhfd`^\WPKIEC?1% 0N/ALow levelGPS@New Alluvium0300002Dark cyano0300000P0000qomkigeca_]YMIGEC?1% LVAL H h 0\tSloping S instead of N here with a few surficial drainage channels. Really a JUNOST Woodland because PINEDU are so sparse.Slope is an average for this hilly spot. A lot of small rock cover on the steeper areas and more bare ground where the slope flattens out a lot. Very shrubby understory and a mixture, also a moderate herbaceous cover in the understory.Slope and aspect are variable. Slope ranges from 2-10 degrees and aspect is mostly S and SE. Small gullies (up to 3/4m deep) cut through plot area. Main wash is just outside plot to the S. Other Surface Geology: Brushy Basin of the MorrisonBroad terrace in a horseshoe of the wash with sandy clay loam soils (seem deep). P-J are invading from Morrison clay hills to the S (the SHEROT associated with the P-J). Other Surface Geology: Brushy Basin of the MorrisonDeep (?) sandy soils in a floodplain with some pebbly rocks and crusts on the surface. P-J are young here - invading the ARTTRI Shrubland.Gently sloping area with trees and shrubs mounded. Few surficial drainages run E through plot. Very homogenous, clean community. Some dieback on JUNOST. ARTTRI are short in stature.Gently sloping area with trees and shrubs mounded. ARTTRI are pretty short. Quite a few standing JUNOST skeletons. Few surficial drainage channels run E through plot area. Sandy soils with slight crust development in areas.Steep, NE-facing slope covered in small rock flakes and chunks. Soil interspaces stabilized by moss and well-developed cryptos. Sparse shrub cover in the understory, herbaceous-dominated.Large, unvegetated areas between trees, with EPHVIR mostly clumped around the bases of trees. Ground is covered with small rock flakes and some well developed cryptos in patches.Rocky soils with soil interspaces mostly stabilized by well-developed cryptos. Point fell on small ridge with slopes running S, SW & SE and steep (~15-20 degrees). P-J here are stunted, due to shallow soils, I suppose.(LVALtz FThis plot nearly overlaps with #945, so I made this circle abut that one and stretch a little more to the W to avoid an overlap. Wash banks are shorter here (1-3m high) and part of plot is on a flat terrace with the opposite side being steep SE-facing toeslopes. Lots of shrub diversity, but the Quercus spp. are clearly dominant.Since polygon included wash and surrounding toeslopes, I made the plot circular to also include both, which resulted in extremely high shrub and graminoid diversity. Toeslopes on either side of the wash face mostly N and NE. Banks of wash range from 1-6m high and surrounding steep toeslopes are stabilized with cryptos and some small rocks on the surface.Steep N-facing slope on one side of this wash and flat terrace to the N. ARTTRI probably invading from adjacent polygon to the E. Wash is ~2-3m wide x 1/2-1m deep with large rocks strewn along banks. High shrub diversity, but none of the dominants are very diagnostic.More ATRCAN here and less HILJAM. P-J look mature and healthy. Very slight crust development. E end of plot encompasses part of the Notom Road.Slightly steeper slope with large mounds that trees are growing on. Deep, fairly sandy soil with moss and slight crypto development throughout. P-J looks mature here, and again, much more JUNOST than PINEDU.Sloping area with deep, fairly sandy soils and some slight crust development in areas. A surficial drainage channel runs NNW through plot. A lot more JUNOST than PINEDU, but PINEDU seedlings look healthy and more abundant than those of JUNOST.Deep, fairly sandy soils with slight crust development in patches. Few surficial drainage channels run N through plot. JUNOST look younger here and have quite a bit of dieback. Lots of JUNOST skeletons standing around. A lot more JUNOST than PINEDU.Sloping area with many surficial drainage channels running N through plot. Sparse understory. Young and mature P-J which are mounded. Crypto development is slight. A lot more JUNOST than PINEDU.LLVAL 4 lnSteep toeslope banks of main wash in Coleman Canyon. Vegetation mounded on upslope sides. High shrub cover in the understory.Steep N and S-facing toeslopes near the head of North Coleman Canyon.Anomalous KRALAN patch here, may be due to soils? Some slight soil crusting. P-J invading from toeslopes to the W.Fairly flat terrace E of main wash. Slope on E end of terrace has few perennial grasses and more weedy annuals. Deep sandy loam soils with slight crust development. CHRNAU presence probably due to close proximity to wash.Very homogenous shrub herbaceous community with a mixture of 4 diagnostic grasses, all with moderate cover values. Broad floodplain in a strike valley with deep, sandy loam soils. Few surficial drainage channels weave through plot. JUNOST are invading from toeslopes to the E and W.Steep Navajo slickrock slopes on the backside (W) of a hogback with vegetation growing in cracks and on shallow soil pockets. Soil areas are slightly duney.Broad wash (4-6m wide) with banks up to 3m tall, rocky-bottom and devoid of vegetation in the channel. Terraces to either side (N&S) are dune-like and dominated by QUEWEL. Quite a bit of shrub diversity, including QUEGAM/Point landed in a wash running E out of the Waterpocket Fold with steep Navajo slickrock slopes to the N and S. Wash is rocky and mostly devoid of vegetation along its course. Slopes have a lot of exposed bedrock, with vegetation growing in cracks, shallow soil pockets, and along the banks of the wash.Sort of a depression between the Waterpocket Fold to the W and another Navajo slickrock uplift to the E. One main channel runs N through plot. Lots of die-back on the ARCPAT, otherwise its cover would be higher. Slopes on the sides are slickrock with shallow soils on top stabilized by cryptos.In canyon wash between Navajo fins in the Waterpocket Fold. Diverse and dense shrub understory. Wash is narrow (1-2 m. wide) with sandy or slickrock ledgey banks up to 10 m. high or more.I  k  o  eT`F3245LowslopeGPS8@Entrada Sandstone05P000PP0040000000geca_][YUSQOOMKIGC0$variablevariableMidslopeGPS@Mancos shale040T00000040000000usqomkigca_]][YWUQC72(f18110MidslopeGPS`@Mancos shale1-a01-a003Crypto pinnaclesT00030000000|zxvtrpnjhfdRNLGE@2&!125MidslopeGPS@Navajo Sandstone02030002Cryptos02P0P00P0000rpnljhfdb`^ZQMKIEA/#EVariableVariableLow levelGPS@New Alluvium021-a1-a002Cryptos031-a0P00P0000~|zxsofb`[VRD83(122350Low slopeGPS@ Wingate Sandstone05000002P00300P0000ljhfdb`^ZXVRRPNLJF3'"Variable340MidslopeGPSn@Obscured by SoilP0000061-a0P001-b0000xvtrpkigec^ZZXVTRP>2-#25308ToeslopeGPSx@Wingate Sandstone020000041-b00200P0000nljhfdb`\ZUQQOMKIE2&!VariableVariableToeslopeGPSZ@Wingate SandstoneP00000900000P0000xvtrpnljhfd``^\ZXVC72(Variable320ToeslopeGPS@Wingate Sandstone1-b0000061-a01-b001-a0000}{ywrpnigb^^\ZXVQ>2-#Variable335ToeslopeGPS@Wingate Sandstone02000006P01-b00P0000xvtrpnljeca]][YWUQ>2-#QVariableVariableToeslopeGPS@New AlluviumP1-aP00071-b0P00P0000ywusqomkigb^^\ZXSQC72(VariableVariableToeslopeGPS@New AlluviumP1-aP0008P0T00P0000vtrpnljhfdb^^\ZXSQC72(VariableVariableToeslopeGPS@New AlluviumP1-aP00071-a0P00P0000ywusqomkigb^^\ZXSQC72(475ToeslopeGPS@New Alluvium060001-bCryptos1-aT01-a0000000qomkigec^\ZULGECA=/#MVariableVariableLow levelGPS@New Alluvium070001-bDark cyano1-b0000000000~|zxvtrma\ZXVRD83(3295Low levelGPS:@New Alluvium0700000200P00T0000ca_][YWUSQOKKIGEC?1% z11343MidslopeGPS:@Navajo Sandstone1-b060001-b1-a0P00T0000omkigeca_]XSSQOMID2&!VariableVariableLow levelGPS@New Alluvium0301-a0005P01-b00P0000|zxvtrpnigeaa_]XVRD83(variablevariableToeslopeGPSb@Navajo SandstoneP041-a0Pcryptos021-b01-b00T0000}xvqmdb`[WUC72(variablevariableToeslopeGPSR@Navajo Sandstone1-a02P003Cryptos, moss03T0T001-a0000}{yufb`^ZUC72(WvariablevariableToeslopeGPSz@New Alluvium1-a031-a00031-b01-b00P0000}{ywusnlgcca_ZVQC72(zLVAL z b >X@Possibly aeolian, fairly shallow soils atop Navajo bedrock slopes (N-facing). Quite a mixture of shrubs. Lots of die-back on the ARCPAT or it's cover would be higher. Slight crust development on soil pockets.Plot encompassed rocky wash bottom (4-8m wide) and the terraces 2-4m above wash to the E and W. Terraces are semi-duney and capped in QUEWEL, with ARTTRI and MAHFRE mixed in. Soil surface of terraces has some biocrust development. Quite a bit of PINEDU recruitment.Seems like an anomalous patch of horsetail due to point falling in a drainage/depression on the toeslope and in a very shaded area. Woodland area with mostly a tall shrub understory.Steep, fairly rocky slope to the S of the main stream channel in Coleman Canyon. NW-facing exposure favors the more mesic species, namely CERMON. Lots of litter. Soils seem fairly deep.Extremely dense shrub layer so that it is hard to walk through plot and ground is covered in leaf and needle litter. Slopes are variable and range from about 15-25 degrees.N-facing toeslope in upper N. Coleman Canyon. Canopy and sub-canopy trees have nearly equal cover and QUEGAM is the dominant understory. Slope varies from 4-24 degrees, and plot captures/crosses wash where slope is nearly flat.N-facing toeslope in upper N. Coleman Canyon. Canopy and sub-canopy trees have nearly equal cover and QUEGAM is the dominant understory. Slope varies from gradual near the base of Kayenta cliffs (to the S) to very steep as it drops off to the creek below (to the N).Steep N and S facing toeslopes at the narrow head of Coleman Canyon which drop off steeply to the narrow, winding creek, all encompassed by plot. Huge trees and ground is covered needle litter.At the head of Coleman Canyon in a narrow part of the canyon with steep toeslopes dropping off into the narrow creek channel. PINPON are huge here and the ground is covered in needle litter. Plot encompasses creek channel and the toeslopes to the S and N.LVAL F : |"Point is next to Navajo cliff at base. Soil is light colored, deep and forming mounds there is eolian sand on top of soil.Point at base of Navajo cliff. It is on a hill slope with large boulders and rocks throughout.This point is near a Navajo cliff base which has a slope with many benches (steps) coming up to it. The step has eolian sand built up into mounds.On a large plateau top or bench near the Circle Cliffs, entire area seems the same elevation and soil type (deep, sandy).Hillside overlooking Circle Cliffs off of Dry Bench.Deep red soil with high small rock content, crypto and litter.This point is up on high hillside in a steep canyon wash or stream. Many larger boulders within wash, trees and plants throughout wash.On a slight hillslope on the Dry Bench plateau there is a Navajo cliff nearby. Soil has high small rock and crypto content and bedrock (Navajo) shows at points throughout area.Point centroid is in small wash but on a flat plateau.Deep sandy soil of light color with cryptos, level ground no mounding or coppices.This point is relatively flat but has a variable slope/aspect because there are mounds of soil (eolian) with crypto and some bedrock exposed.Point next to wash and banks go up from it hence variable slope and aspect.Wash in hillslope up high near ridge bordering Bear Canyon.Deeper soils that are bisected by gullies, lots of bedrock and smaller rocks present.Flat area is interwoven with small rivulets forming low mounds of bare soil (that shows physical crusting).This community is on dissected slope eroded from Entrada with pebbles of other geologies on the surface. The COLRAM shrubland to W is on the valley floor proper, no pebbles. All are in the same polygon. ATRCON/PLEJAM is in lower spots between low ridges that make up most of the plot.Point is midslope of an interfluve of Mancos soil. Seems like physical crusting.On a hill in Mancos soil with high rock content.7 N 3 v  aO1+@0284High SlopeGPS&@Obscured by SoilT051-b001-b1-a01-a001-a0000usqomhfd_]XSSQOJFD2&!0n/aHigh LevelGPS@obscured by soilT00003crypto03000001-a0000sqomkfdb`^\XPLJHFD2&!22335High SlopeGPSh@ Kayenta Formation1-b00001-b02002001-a0000trpnlgec_]YTTRPNLG4(#[0n/aHigh LevelGPS|@ Obscured by Soil1-a1-a0002crypto02T01-a001-a0000|zxvtomkfdb^VRPNID2&!28346High SlopeGPS@ Obscured by Soil1-a00001-a0201-b001-a0000trpnlgec^\XSSQOMKF4(##24282High SlopeGPSNone.Obscured by Soil1-b0001-acrypto021-b01-b001-b0000~ywupnie]XVTRM;(#3218High SlopeGPSb@ Obscured by Soil002001-bcrypto1-b1-a002001-a0000|zxvtomkge`[SNLJFD2&!5220High LevelGPSl@ Obscured by SoilP1-b1-a002crypto1-b000001-b0000zxvtrmkigec^VRPKFD2&!0n/aHigh LevelGPS@Obscured by SoilT00009crypto00000000000nljhfdb`^\ZXPLJHFD2&!]yvariablevariableHigh LevelGPS@Obscured by Soil01-a0002crypto1-a1-a01-a001-a0000zxsnfb`^YWE94(8134Low slopeGPSNoneMoenkopi Shale1-a00001-a1-a00600P0000rpnljhfd`^YTTRPNLG7% 0n/aLow levelGPSNone.Moenkopi FormationP0001-acrypto1-a1-a00600P0000}{ywusqmkfaYTRPNL8% r280Low slopeGPSNone.Moenkopi Formation00001-acrypto1-a1-a0060000000~|zxvtrplje`XSQOMK7$2044High SlopeGPSNone.Moenkopi Formation1-b000001-b0070000000vtrpnljhdb][[YWUSN:'""21224High SlopeGPSNone.Moenkopi Formation01-a0002crypto1-a1-b002001-a0000zxvrpkf^ZXVQO;(#variesvariesLow levelGPS@Alluvial deposits02000Pcrypto021-a00200P0000~|zxvtpnie][YWUQ>2-">!0n/aLow levelGPSNoneAlluvial deposits0200001-b0002001-b0000trpnlgec_][VVTRPNJ7% `10340High SlopeGPSv@Obscured by Soil1-a01-a01-aCrypto1-a1-a01-a001-a0000}{vtrmkfaYTRMKF4(#1560MidslopeGPS@Obscured by Soil1-a020001-a1-a002001-a0000sqomkfdb^\WRRPNLHC1% (0n/aLow levelGPS@Moenkopi Formation090000000P0000000geca_][YWUSQQOMKIE1% "3338ToeslopeGPSNone.Moenkopi Formation09T0000P0P0000000mkigeca_][YWWUSQOK7$DvariablevariableLow levelGPSRight off Scenic Drive.Moenkopi Formation09TT000T0T0000000}}{ywuq]83(Z H ] N cyqdd398ToeslopeGPS@Moenkopi Formation05T000P0200300T0000igeca_][WUQOOMKIGC/#VariableVariableInterfluveGPS@Moenkopi Formation090000TP0P0000000{ywusqomkigeeca_]YE94(E342MidslopeGPS@Navajo SandstoneP081-a0PBiocrust1-aT0T00T0000sqomkigeca_ZPNLGCA/#l15304MidslopeGPS@Navajo Sandstone1-a030004Biocrust021-a01-a00P0000}{ywusqojhc_UQOMID2&!Ve6342MidslopeGPS|@ Navajo SandstoneP060003Biocrust1-bP0P00P0000sqomkigeca_ZPLJHDB0$e11128MidslopeGPS@ Navajo Sandstone1-a040004Biocrust1-bP01-a00T0000{ywusqomhfd_UQOMID2&!0n/aHigh LevelGPSH@ Obscured by Soil030001-bBiocrust05000001-a0000xvtrpkigeca]SNLJHD2&!|k7201MidslopeGPS@ Kayenta Formation020200003P00300P0000kigeca_]YWUQQOMKGC0$K574High SlopeGPSn@ Obscured by soil060001-bBiocrust0300T00P0000trpnljhfdb`\RMKIGC1% =5338MidslopeGPS@Obscured by soil05000004000001-a0000igeca\ZXVTRNNLJHFB0$<6358MidslopeGPS@@Obscured by soil030001-aMoss0600000P0000omkigeca_][WQLJHFB0$50N/AHigh LevelGPSl@Obscured by soil05000PBiocrust05000001-a0000usqomhfdb`^ZPNLJHD2&!432MidslopeGPSj@Obscured by soil0600000400000P0000eca_][YWUSQMMKIGEA/#0n/aHigh LevelGPS@Obscured by Soil05000PBiocrust05000001-a0000usqomhfdb`^ZPNLJHD2&!6330MidslopeGPSSoils are sandy.Obscured by Soil05000005000001-a0000{ywusnljhfd``^\ZXTB$0n/aHigh LevelGPSDeep sandy soils.Obscured by Soil0300000300000020000}{ywuqomkigcca_][WE&!14348High SlopeGPSP@Obscured by Soil1-b00002crypto02T0T001-b0000xvtrpkigeca]UQOMKF4(#0n/aHigh LevelGPS@Obscured by Soil03P0004000001-a0000igeca\ZXVTRNNLJHHD2&!0n/aHigh LevelGPS@Obscured by Soil030T000300T00P0000hfdb`^\ZXVTPPNLJHD2&!0n/aHigh LevelGPS@Obscured by Soil0301-a000200T001-a0000nljhfa_][YWSSQOJHD2&!v0n/aHigh LevelGPS@Obscured by Soil021-b02001-a000001-a0000qomkidb`^\ZUUSQMHD2&!l14258High SlopeGPSSoils seem Navajo derived.Obscured by Soil1-a020001-b02002001-b0000|zvqqomkgbP(#16270High SlopeGPS@Obscured by SoilP00001-a03002001-a0000pnljhca_[YUPPNLJHF4(#LVALT , V  p   8$ r0Soils are very sandy, but stable.This area has a mixture of tree ages from very old to young & seedlings.The Chrysothamnus is restricted to the SE edge of polygon/plot, where soils are shallower. The deeper soil to the N has much more Stipa grass.Plot includes a wide gulley which is where most of the vegetation is found. Soil is covered with rocks wherever the slope is not too steep and erodable. A rusted culvert sticks out of the hill.The scenic drive road runs just west of plot edge. Plot encompasses some highly erodable badlands. The grasses are confined to the less gullied, flatter portion of the plot. Plates of white mica are exposed in lines on the soil surface.Much bedrock here - plants growing in cracks or on sandy sheets in the biocrust.Trees are stunted due to shallow soil. A few, dead, down Ponderosa on plot.Trees are stunted in shallow soil. Lots of bedrock showing.Trees are stunted due to shallow soils. In fact, all the plants are stunted.Tall trees, very park-like and open.A ledgey, rocky slope with shallow soils above canyon cliff. The SHEROT seems to be most abundant below the Navajo.Sandy soils, fairly well-stabilized. Some dead ARTTRI.Looks like a fire came through once. Several downed & charred trees on the ground.This hillside burned some time ago. A few charred snags are visible. The oak are in two size/age classes - some clumps 2m or more tall, others ~1/2meter tall.An open, park-like area with large, well-spaced trees.Sandy soils. Oak is regenerating in spots from fire.A large, open park-like area with tall trees and large openings.Deep sandy light brown soil with crypto.Deep sandy soil that forms mounds (coppice) that have QUEGAM/AMEUTA ect.This point has deep sandy soil that has formed low mounds (seems eolian) with diverse shrubs on top.Deep sandy soils with surface eolian sand and coppice mounds (that are low, not tall).W N ! p % 8)@l6VariableVariableMidslopeGPS@Moenkopi Formation08P000TP0P0000000ywusqomkigecca_][WC72(<VariableVariableMidslopeGPS@Carmel Formation05T0004Gypsiferous mineral crust & lichensPT0T0000000c_][YUC72(.VariableVariableLow levelGPS @ Carmel FormationP1-a0008Gypsiferous mineral curst & lichensPP0P00T0000ea_]XVD83(Z5VariableVariableHigh SlopeGPS@ Carmel FormationTP0008Gypsiferous mineral crustPP0P00T0000~c_][YWE94(_0N/AHigh LevelGPS@ Moenkopi Formation04000PMoss02P00400P0000rpnljhfd`^\XRPNLJF2&!B836High SlopeGPS@ Moenkopi Formation03P00003P00400P0000kigeca_]YWUQQOMKIE1% y8344High SlopeGPS@Obscured by Soil05P00004P0P00P0000hfdb`^\ZXVTPPNLJHD2&!b0n/aHigh LevelGPSSoil is sandy but stable.Obscured by Soil0600000400000P0000}{ywusqokkigec_M&!z352High SlopeGPSSoil is sandy but stable.Obscured by Soil0700000300T00P0000~|zxvtrpnjjhfdb^L% m6344High SlopeGPS@Kayenta Formation02T000031-b00500P0000nljhfdb`\ZUQQOMKIE2&!Mh362High SlopeGPS@Obscured by Soil04T001-aBiocrust05P0P001-a0000wusqojhfdb`\RMKIGC1% 4360MidslopeGPS@Obscured by Soil0600000400000P0000fdb`^\ZXVTRNNLJHFB0${0N/AHigh LevelGPS@Obscured by Soil05000PBiocrust04000001-b0000usqomhfdb`^ZPNLJHD2&!437High SlopeGPS@Obscured by Soil05T00004P01-a00P0000jhfdb`^\WUSOOMKIGC1% n0N/AHigh LevelGPSD@Obscured by Soil05000PMoss, biocrust0400P001-b0000{ywusnljhfd`PNLJHD2&!459High LevelGPS@Obscured by Soil03000PMoss, biocrust0500P001-b0000zxvtrmkigec_OMKIGC1% 0N/AHigh LevelGPSSoils are sandy & stable.Obscured by Soil06000003000001-a0000~ywusqokkigec_M&!0N/AHigh LevelGPSDeep sand, stable soils.Obscured by Soil06000PMoss03000001-a0000~|zxvtpjhfdb^L&!PVariableVariableHigh LevelGPS0@Obscured by soil050001-aMoss04000001-a0000zxvtrplfa_][WE94(S3284ToeslopeGPSB@Eolian Sands0500000400000T0000b`^\ZXVTRPNJJHFDB>0$384High SlopeGPS@Obscured by soil050001-aMoss & biocrust04T01-a00P0000~|zxvtrpkigcRMKIGC1% 0N/AHigh LevelGPS@Moenkopi Formation05000PMoss1-aP00400T0000sqomkigea_]XRPNLJF2&!LVAL  & z $,"Point fell near the bottom of a gully, but includes the gully sides and upper, level area too. The Stanleya is near the wash bottom.Plot includes the rolling flat & drops down into a steep erosional gully with some bedrock ledges in it. Vegetation is the same on the gully sides & bottom, just more sparse than on the level. Gypsiferous crust w/lichens is well developed everywhere.Many small rocks in soil. Many annuals & the 4-o'clocks all growing in shade of trees.Gravelly soil. A few dead bunches of Elymus. Trees are fairly stunted due to shallow soil.This area consists of a gentle rise with shallow soil where most of the tall shrubs (and buffalo berry) occur, along with most of the trees. It also has a flatter area which is more open and has an old 2-track running through it, where the gramma grass is.Small rocks cover the soil, soil is shallow. Area occupies the sloping bench above the canyon rim. Trees are mostly young-ish.This point occupies the gently sloping shelf above the canyon rim & may be influenced in part by the tall shrub species over the rim edge. To the east of plot the terrain levels off and the tall shrubs really thin out. Soils are still deep here.Young trees & Gambell's Oak possessing a clumpy, tall shrub form. Trees are youngish.Almost 50% of the pine trees are dead or dying here. Looks like beetle kill. Most are standing dead.A couple of shallow gullies run through plot, but have no significant impact.Area is approaching old growth. Trees are showing decadence even though there are younger trees also. Small mounds of sand support the most cacti & Muhly grass.This area is approaching old growth. Although there are multiple-aged trees, many are large and gnarly, showing some decadence.A couple of burned out snags from lightning strikes. Soils are sandy, but well stabilized. An old 2-track runs through plot, but is mostly grown over.LVAL: L  N  jF| Z<Narrow canyon whose wash doesn't look like it gets much action. Wash floor very sandy, ~3-5m wide, with lots of rocks mixed in. Steep Navajo Sandstone cliffs ~50-70 ft wide border the wash.Long-dry old oxbow - very trashed-looking. Big slash piles of tamarisk piled up everywhere. Tamarisk in plot = small reprintsRocky, hot and dry south-facing slope just below Wingate cliffs of Capitol Gorge.The gypsum soil is covered with biocrust. The steep and deep badlands have every slope and aspect.The gypsiferous soil is covered with biocrust.The terrain is highly sculpted by erosion.The steep, rocky hillside is cut by many drainage channels.A depression in the sandstone has accumulated some soil and a drainage passing through supplies moisture, allowing a host of shrubs to congregate.A depression in the slickrock has allowed soil to accumulate and shrubs have moved in.The vegetation is mostly growing in cracks. The Ponderosa pines are stunted.Soil is very sandy and blowing out in spots.The soil appears deep and is sandy.This is a rocky slope with sandy soil.The terrain is rocky with sandy soil.This point falls on a rocky slope between a flat area above and a swale below.The soil is sandy but well-stabilized.The site is ledgey with rocky soil.The site is a little duney but mostly stabilized by vegetation.The terrain is duney with soil blowing out.This plot is on the Navajo-Carmel interface, but most of the soil comes form the Carmel.The terrain here is sandy steps and ledges.The soil is very sandy and blowing out in spots.The soil is very sandy and blowing out in spots.The terrain here is gently rolling with sandy soil.The plot is on a wide ledge about 20 feet above the wash bottom.This highly eroded site generally faces east with many different slopes and aspects.Many mini gullies. A hard-baked area with slightly more rain crust than gypsiferous mineral crust.V =  _  k /U\&pW1057High SlopeGPSX@Obscured by soil0500000400000P0000igeca_][YWUQQOMKIE3'"T557High SlopeGPSSoil is deep and sandy.Obscured by soil0300000600000T0000~|zxvtrpnlhhfdb`\J% 4340High SlopeGPSThe soil is deep and sandy.Obscured by soil0300000600000T0000}{ywusqmmkigeaO&!{3142High LevelGPS"The soil is deep and sandy here.Obscured by soil0400000500000P0000~|zxvrrpnljfT&! /0N/AHigh LevelGPSThe soil is deep and sandy.Obscured by soil0400000500000P0000}{ywusqmmkigeaO&! G0n/aHigh LevelGPSThe soil is deep and sandy.Obscured by soil0300000600000T0000}{ywusqmmkigeaO&! 0n/aHigh LevelGPSF@Obscured by soil0200000700000P0000hfdb`^\ZXVTPPNLJHD2&! x12133High SlopeGPSL@Navajo Sandstone03P00005P0P00P0000jhfdb`^\ZXVRRPNLJF4(# }8334High SlopeGPSJ@ Navajo Sandstone02T00006P0T00P0000hfdb`^\ZXVTPPNLJHD2&!~9310High SlopeGPS@ Navajo Sandstone04P00005P0P00T0000hfdb`^\ZXVTPPNLJHD2&!0n/aHigh LevelGPSL@ Obscured by soil0500000400000T0000hfdb`^\ZXVTPPNLJHD2&!316266High SlopeGPSF@ Navajo Sandstone04P00002T00200P0000ljhfdb`^ZXVRRPNLJF4(#4314High SlopeGPS~@ Eolian Sands0300000500000P0000db`^\ZXVTRPLLJHFD@2&!5310High SlopeGPSV@Eolian Sands03003000300000P0000fdb`^\ZXVTRNNLJFD@2&!5270High SlopeGPSSoil here is very sandy.Navajo Sandstone0400000400T00P0000~|zxvtrpnjjhfdb^L&!23346High SlopeGPS@Carmel Formation04PT0003P0P00P0000jhfdb`^\ZXVRRPNLJF4(#r14288High SlopeGPSV@Kayenta Formation031-b00004P0P00P0000nljhfdb`^\ZVVTRPKG4(#0N/AHigh LevelGPS`@Obscured by soil0400000500000P0000hfdb`^\ZXVTPPNLJHD2&!210High LevelGPS`@Obsured by soil0300000500T00P0000fdb`^\ZXVTRNNLJHFB1% 0n/aHigh LevelGPSThe soil is very sandy here.Obscured by soil0400000400T00P0000~|zxvtrnnljhfbP&!variablevariableHigh LevelGPSf@Obscured by soil0500000300000P0000{ywusqomkigcca_][WE94(19116High SlopeGPSNone.Moenkopi Formation05P000P1-b00300T0000vtrpnljhdb][[YWUSO;(#11154Step in slopeGPS@Moenkopi Formation021-a000P0300300T0000trpnljhfb`\ZZXVTOK7+&R R d  Q \(:DN)o0N/ALow levelGPS@ New Alluvium1-b0000021-b01-b00T0000jhfdb`^\WUPLLJHFD?1% (i0N/AHigh LevelGPSD@ Terrace gravel deposits0200001-b030030000000trpnljhfb`\WWUSQOK2&!''14142High SlopeGPSB@Terrace gravel deposits1-a0000020400300T0000vtrpnljhdb^ZZXVTRM4(#&29223High SlopeGPS@Terrace gravel deposits1-a00001-a0300400T0000wusqomkiec_ZZXVTRM4(#%^27140MidslopeGPS2@Moenkopi Formation1-aP000P0400400T0000mkigeca_[YUSSQOMKF2&!$k8177High SlopeGPS,@Moenkopi FormationP1-a0001-a0300500T0000pnljhfdb^\XSSQOMHF2&!#0N/AHigh LevelGPS@Moenkopi Formation0200001-b1-b00600T0000pnljhfdb^\WRRPNLJF2&!"1762High SlopeGPS@Moenkopi FormationPT0001-b0400500T0000nljhfdb`\ZVQQOMKIG3'"!`1390High SlopeGPS@Moenkopi FormationPT000020601-b00P0000nljhfdb`[YUQQOMKIG3'" a0N/ALow levelGPS`@New Alluvium07000002T0P00P0000ca_][YWUSQOKKIGEC?1% #284Low levelGPS@New Alluvium1-b00300PP00400T0000eca_][YWSQOMMKIEC>0$94355Low levelGPS~@Navajo Sandstone1-a020400P0200200T0000nljhfdb`\ZVTTRPLHC1% 0N/ALow levelGPS@New Alluvium050001-aBiocrust04T0T00P0000pnljhfdb`^\XNIGEC?1% :27223MidslopeGPS@Talus/Colluvium/Landslides1-a0000P0600300T0000usqomkigca][[YWUSN2&!8\VariableVariableInterfluveGPS@Carmel Formation1-b020006Biocrust0P0P0000000~|zxvtrhdb`\WE94(q6VariableVariableMidslopeGPS\@Carmel Formation05P0004BiocrustTT0P0000000}{ywusqomc_][YUC72(1085MidslopeGPST@Entrada Sandstone09TT00T00P0000000fdb`^\ZXVTRPPNLJHD1%  -2640Low slopeGPSv@Moenkopi Formation02P0001-a0200500T0000omkigeca][WRRPNLJF2&!cC4110Low slopeGPS$@Navajo Sandstone0202P0PBiocrust03P0P00P0000sqomkigeca_[QOMKGC1% +=10110MidslopeGPS@Navajo Sandstone020500002T0T00T0000jhfdb`^\ZXVRRPNLHD2&!gU1579MidslopeGPS@Navajo SandstoneT09000TT0T00T0000eca_][YWUSQOOMKIEC1% h3244High LevelGPSSite's soil seems sandy.Obscured by soil0400000500000P0000~|zxvtrpnjjhfdb^L&!896High SlopeGPSSoil is sandy.Obscured by soil0600000300000T0000wusqomkigec__][YWSA% }0N/AHigh LevelGPSSoil is sandy.Obscured by soil0400000500000T0000xvtrpnljhfd``^\ZXTB&!LVAL  ^ ~ R ~<8Plot is in red & gray clay slopes of Chinle, with lots of flat rock talus as well.Baked-looking, cracked soil with lots of small volcanic rocks & a smattering of large volcanic boulders throughout. Dirt road runs right through plot.Part of the broad, sandy floodplain in this valley. Highly disturbed area - this polygon is squashed in between the Fruita Schoolhouse & Behunin grove & bordered on other side by main park road.Second terrace of the Fremont River. Rocky/sandy soil with some areas of well-developed crypto.Exposed, windy mesa top with little black rocks & golf ball to basketball-sized black volcanic rocks scattered around. Hiking trail goes through one end of plot.Seemingly deep soils with small pebbly volcanic rocks & large volcanic boulders. Open and windy! Slope is an average of flatter mesa top and steeper mesa side.Steep, rocky/bouldery slope. Plot also stretches up to the flat top of the mesa.Platey brown rocks covering some of area, other areas have more developed-looking rocky gray soil. Large volcanic rocks & boulders scattered throughout.Plot mainly in a platey-rock-covered areas, with some big volcanic rocks scattered around. A bit of Moenkopi-cliffs are exposed in west part of plot.Apparently deep soils with pebbly pea-sized rocks covering surface, & big black volcanic rocks scattered around.Very rocky hillside - surface totally covered with small to pie-sized chunky rocks.Typical Moenkopi hillside with small & large platey rocks covering the surface.Broad terrace ~40m wide, with a wider second terrace (and orchard) to the north. Area is pretty disturbed - surrounded by roads & there's a lot of tamarisk slash piles around.Broad, shallow, gravelly wash ~5-7m wide, with terraces of varying width. In this part of the canyon, there's quite a broad, sloping terrace ~20m wide with many grasses growing in the sandy soil. Most of the shrubs are clustered closer to the wash edge.wgQ ) o  f Y>(m?VariableVariableHigh LevelGPS@Navajo Sandstone040001-aCrypto0400000P0000~|zxvtrnfa_][WE94(>VariableVariableHigh LevelGPS@Navajo Sandstone0500003Crypto0300T00P0000}{ywusqmea_][WE94(=VariableVariableHigh LevelGPS@Navajo Sandstone05PP0TCrypto0400T00P0000}{ywusqokca_][WE94(<0890High slopeGPSv@Kayenta Formation05T00PCrypto03T0T00P0000pnljhfdb`^\XPNLJHD1% ;VariableVariableHigh LevelGPS@Obscured by soil0000PCrypto0400P0000000}{ywusqomia_][YWE94(:18255High LevelGPS@Navajo Sandstone0302001-bCrypto03P0P00P0000wusqomkigec_WRPNJF4(#9VariableVariableHigh LevelGPS@Navajo Sandstone1-b1-a1-b01-bCrypto04T01-a00P0000}{yumhfa\WE94(8Q15340MidslopeGPS@Moenkopi Formation1-b040001-b0200200P0000rpnljhfd`^ZUUSQOKF2&!7VVariableVariableToeslopeGPS@Moenkopi Formation1-aT000PP00800T0000|zxvtrpnjhfddb`^\WC72(6sVariableVariableHigh LevelGPS@ Moenkopi FormationP1-a0001-a0701-b00T0000~|zxvqokffdb`[YE94(5I31210MidslopeGPS@ Chinle Formation1-aP000T040050000000kigeca_]YWSQQOMKID2&!4E25206MidslopeGPS @Chinle Formation1-aP000T0400500T0000kigeca_]YWSQQOMKID2&!3XvariablevariableToeslopeGPSv@Moenkopi ShalePP000P1-a00800T0000xvtrpnljfd_]][YWUSC72(2!|VariableVariableStep in slopeGPS@Moenkopi Formation08P000T1-b01-b0000000~|zxvqojhhfdb`\H<7(1wvariablevariableToeslopeGPS2@Moenkopi Shale04000Pdirt roadT030030000000~|zxvrplj_][YWSC72(0RtvariablevariableToeslopeGPS@Moenkopi Formation050001-adirt roadT0301-b0000000~ywsqfa_][WC72(/xwvariablevariableToeslopeGPS@Moenkopi Formation080000TP0020000000{ywusqomigecca_][WC72(.VariableVariableLow levelGPS@Moenkopi Formation070000T0201-b0000000}{ywusqljfddb`^\XD83(- VariableVariableLow levelGPS@Moenkopi Formation090000TT01-b0000000}{ywusqojhfddb`^\XD83(,VariableVariableLow levelGPSx@Moenkopi Formation09T000TP01-a0000000}{ywusqojhfddb`^\XD83(+|0N/ALow levelGPS.@ Moenkopi Formation060001-aDirt roadT1-b0040000000zxvtrpnlhfa_TOMKIE1% *4i3189Low levelGPS@ New Alluvium06000003T0P00P0000ca_][YWUSQOKKIGEC?1% FLVAL  L 4 2zhPlatey, brown rocks covering the surface of these Moenkopi hills. Flat tops and steep sides characterize the area. Electric poles with wires run through plot. P-J is kind of short and stumpy here.Steep, rocky Chinle slopes below Meeks Mesa. This plot wraps around a steep toeslope, with aspect being applicable for most of plot.Platey rock covered Moenkopi hills, with many toeslopes and channels running off in various directions. Plot is next to a fairly large wash, which may be somewhat influencing vegetation.Typical-looking badlands w/toeslopes going off in all directions. Black volcanic boulders scattered throughout. Cracked, baked-looking brown soil with some exposed bedrock and ledges in places.Baked looking badlands with big volcanic boulders and small platey rocks throughout. Road runs through north end of plot. Many small drainage channels.Not a great place for this plot! On edge of another polygon, and has dirt rod running through it. Otherwise, it's typical environment for the area-baked looking brown soils some small platey rocks, many drainage channels, and many black volcanic boulders.Rolling badlands area with cracked, baked looking brown soil. A variety of small rocks scattered around, including whitish platey rocks, volcanic black rocks, and flat clear crystals. A few large volcanic boulders too. Many small drainage channels run through plot.Rolling badlands area with cracked, baked-looking brown soil and many large black boulders. A variety of small rocks scattered - some are flat and clear-crystals. Many drainage channels through plot.Slightly rolling, badland-like area with cracked, baked-looking brown soil. Small volcanic rocks & little drainage channels scattered throughout. This plot next to a hillside with P-J/PLEJAM on it (outside park)Slightly rolling badland-y area with cracked, baked-looking soil & small volcanic rocks scattered throughout. CHRVIS & HILJAM seem limited to small drainage channels running through plot.fLVAL@| f b H :  \JPlot is part of the big uplift of Moenkopi west of the Scenic Drive, & sits halfway up a hogback which is part of that monocline. Plot wraps over the top of hogback, so slope/aspect are for majority of plot. Substrate covered w/platey brown rocks.Ledges of broken slickrock with plants growing in cracks and soil pockets. Well-developed cryptos on some of the soil pockets.Rolling topography with large (3-5m wide) wash running through plot. Well-developed cryptos here.Rolling topography with various slopes & aspects. A large (3-5m wide) wash runs through plot.Slightly rolling topography - slope & aspect are for overall larger area. Very sandy soils w/well-developed cryptos. A fairly large wash (1-2m across) runs through plot.Slightly rolling, mostly flat topography with very sandy soil & well-developed cryptos.Rolling sandy area with well-developed cryptos. A fairly big wash (~1m across) runs through E end of plot.Rolling, micro topography with duney areas. Good crypto development on some of the dunes.Rolling micro topography here with stabilized duney areas & well-developed cryptos.Rolling, stabilized duney area with many slopes & aspects - not much crypto.Rolling, duney area under PJ. Some well-developed cryptos.Rolling topography next to a wash channel w/reddish brown soils & a few well-developed cryptos. A couple smaller drainages run through plot.Ledgey, sloping Navajo slickrock outcrops w/P-J & CERINT growing on shelves/pockets. Well-developed cryptos on many soil pockets.Very sandy soils, rolling terrain with gentle slopes of Navajo slickrock outcrops. A couple sizeable washes run through west side of plot.Hard to describe landform here in these Moenkopi hills - if it were more dry/eroded-looking, I'd say badlands. But, lots of bedrock exposure here - thick & solid, with trees/shrubs growing in cracks, on ledges & soil pockets.Several toeslopes in plot, with drainage channels running through PURMEX growing along channels.^E  ^  l " :\iKV5164Step in slopeGPS,@Kayenta Formation1-b0600PCrypto1-b1-a0P00T0000{ywusqomkid_WUSQMH5)$U]VariableVariableHigh LevelGPS@Kayenta Formation1-b1-b0001-b1-a00400T0000~|zxtrmhhfdb]XE94(TV14352High LevelGPS@ Eolian deposits04P001-bCrypto04T0000P0000trpnljhfdb`\TOMKIE4(#S gVariableVariableHigh LevelGPS@ Eolian deposits04000PCrypto0400000P0000~|zxvtrpnjb`^\ZVE94(R7202High SlopeGPS@ Kayenta Formation031-b000030201-b00P0000qomkigec^\XTTRPNIE2&!Q)1014Step in slopeGPS@ Kayenta Formation1-a020001-b0300300T0000usqomkigca]XXVTRNI6*%P 30320ToeslopeGPS@ Chinle Formation1-a0000P0300600T0000kigeca_]YWSQQOMKID2&!O5322ToeslopeGPSJ@Chinle Formation090000TT01-a0000000geca_][YTRPNNLJHFB0$N5304ToeslopeGPSJ@Chinle Formation090000TP0p0000000db`^\ZXVTRPNNLJHFB0$M537Low levelGPS@Moenkopi Formation1-bT1-a00031-a00400P0000qomkigec_]XTTRPKID0$L0n/aLow levelGPST@New Alluvium080001-aCryptos1-aT0P00T0000pnljhfdb`^\WNIGEC?1% K870MidslopeGPS@Moenkopi FormationPP000030500200P0000igeca_][WUQMMKIGEC/#J$1173High SlopeGPS@Moenkopi FormationP0000030300300P0000mkigeca_[YUQQOMKIG3'"I1270High SlopeGPS@Moenkopi Formation1-a0000030200400P0000pnljhfdb^\XTTRPNLG3'"H1085MidslopeGPS@Moenkopi Formation1-a0000020300500P0000nljhfdb`\ZVRRPNLJE1% G1380MidslopeGPS@Moenkopi FormationP0000041-b00400P0000ljhfdb`^ZXSOOMKIGE1% F200MidslopeGPS@Moenkopi FormationPP0001-a0200600T0000jhfdb`^\XVRMMKIGEC/#E a2536High LevelGPS@Navajo Sandstone1-a0400PCrypto021-a01-b00P0000zxvtrpnlge`\TRPNJE3'"DfVariableVariableHigh LevelGPS@ Navajo Sandstone03P1-b002Cryptos0300T00P0000}{ywuqhdb][WE94(CVariableVariableHigh LevelGPS@ Navajo Sandstone0401-a01-bCrypto03T0P00P0000}{ywuqidb][WE94(B8194High LevelGPSV@ Navajo Sandstone02P1-a003Crypto03P0T00P0000usqomkigeca]UQOJHD2&!AVariableVariableHigh LevelGPS@ Navajo Sandstone0200003Crypto04000001-a0000{ywusqmea_][WE94(@VariableVariableHigh LevelGPS@ Navajo Sandstone02PP002Crypto04T0T00P0000}{ywusqmea_][WE94(LVAL*   L``Wide, gentle toeslopes tapering off the colluvial slopes of Meeks Mesa. Soils between large rocks seem well developed & deep.Large, rolling dunes that are fairly well-stabilized with cryptos & grasses.Rolling dunes here in the PJ - not many cryptos here; these dunes are probably pretty active.Lots of ledgey Kayenta outcrops with broad, shallow pockets of sandy soil.Big ledges of slickrock exposed everywhere, making a series of wide steps to the canyon below. Many small rocks embedded in soil, and lots of small drainage channels. Quite a few dead CERINT & lots of dieback on it.This plot wraps around both sides of a toeslope on a colluvial slope, but the majority of the plot falls on the slope & aspect given above. Lots of Wingate breakdown over the Chinle base. Hot and sunny here!Rolling toeslopes with many drainages running through plot. Soil is dark brown & baked-looking/cracked. Cliffs just outside plot to the east of Chinle and Wingate.Rolling toeslopes with many drainages running through plot. Soil is dark brown & baked-looking / cracked. Cliffs just outside plot to the east of Chinle & Wingate.Slightly rolling terrace on both sides of a wash. Soils dark brown & covered with pebbly rocks. Platey brown rocks covering the slopes above.Polygon encompasses both a higher bench dominated by STIHYM and a lower bench dominated by ATRCAN-OPUPOL. These benches are adjacent to the dirt road/Capitol Gorge wash.Broken slickrock chunks everywhere, with lots of scattered small rocks around. A few well-developed cryptos on soil in cracks.Surface covered with light-colored pebbly and some chunky rocks. Gently sloping, wide-open plain.Light tan pebbly and some chunky rocks cover the surface. Wide-open, gently sloping plain.Light-colored large & small rocks cover everything. Gently sloping, wide open plain.Substrate here covered with lighter-colored, pebbly & some bigger, chunky rocks. Wide, sloping plain here.LVAL^2  T&0Plot encompasses a transition area where a narrow wash canyon opens up into a broader park area. Vegetation varies from spot to spot, with shrubs generally grouped into large patches by species.Plot is at the interface of Kayenta and Navajo Formations. Bare, slickrock with small pockets of soil and veg.Thin soils on slabby slickrock ledges.Thin soils on slabby ledge systems.Slabby sandstone ledges w/thin soils along a canyon rim.There was once a lot of Russian olive here, but it's all recently been cut down. Higher wood ground cover is the result.Plot straddles Fremont River channel, and records vegetation on both stream terraces on either side. Lots of flood debris under POPFRE.Plot includes two distinct areas; a stream terrace with ARTTRI - T and lower floodplain areas on both sides of the Fremont River channel.Low floodplain by Fremont River. Lots of woody flood litter under willows and trees.Area is on a low stream terrace/floodplain of the Fremont River, which clearly gets inundated during high water events. Several dead POPFRE in plot - one live tree on edge.Coarse-textured bedrock and large rock exposures and lots of gravel characterize this site. Plot wraps around both sides of toeslopes, so slope and aspect vary. PJ looks stunted.Coarse-textured bedrock and large rock exposures everywhere, with lots of gravel covering soil and bedrock. Rolling topography here, but overall slope and aspect is as entered above. PJ looks stunted. Plot on edge of cliff.Large, rolling hills with lots of black volcanic basketball-sized rocks. Very rocky/gravelly soil. Some bedrock outcrops just SW of plot. JUNOST quite small/ young here.A band of exposed slickrock ~30-40m wide with shallow soil pockets & well developed cryptos in places. Steep talus slope bordering plot to the north.Plot center is on top of this point & also covers slopes on 3 sides, so slope & aspect vary. Soil here seems thin & is covered with small tan pebbly rocks. Navajo slickrock outcrops jut up just outside plot.>LVAL $" < ":fGypsiferous soils. Plot is on the side and top of a low hill. Slope ranges from 28 degrees to 8 degrees.Small rock permeates soils. Trees very stunted, and a number of old skeletons in plot. Limey member of the Carmel.Soil is rocky with small rock, beneath surface as well as on top. Trees are generally small, especially the JUNOST, which are typically little more than a meter high, but these are not seedlings. Limey member of the Carmel.Classic slickrock community growing in fractures and shallow soils. Trees are all very short here.Duney topography, though dunes are will-stabilized by biotic soil crusts. Dunes overlie a Navajo bedrock, which appears to be close to surface in most areas.Steep, ledgey slopes with lots of bare bedrock. Soils are thin and patchy. Slope is average for plot, but most vegetation is on lower-angled ledges.Small wash with deep soils on banks at one end of plot, but much of plot lower banks, thinner soils, and lower plant density. Moisture is concentrated in deeper soils from run-off from cliffs and slabs upslope.Slope is an average, plot includes soils on steeper and flatter surfaces plus some bedrock rim areas. Upslope on steeper soils is a sandstone rim, with blocks from that scattered on the slopes.Duney topography. Part of the plot is flat, a stabilized (grass-covered) blow-out. Rest is rolling stabilized dunes. Some dead PINEDU here, some standing, several older skeletons on the ground.Wingate slickrock with the beginnings of joint patterns deepening towards the main canyon. The joints define the aspect. Vegetation is in joints and pockets with thin soils.Chinle clay soils, with some small and large rock on surface. Polygon is badlands toe slopes, with lots of aspect/slope variety.Classic Moenkopi Badlands, with deep clay soils.Soils are rocky below surface as well as on top. Small exposure of fractured bedrock in plot has small concentration of JUNOST. Lots of dead Hilaria, probably last year's drought mortality.RV 6 . (x-[ w1120Low levelGPS@New Alluvium000800PT01-b00T0000db`^\ZXVQOMKKIGCA?1% :378Low levelGPS>@New AlluviumT00000900000P0000`^\ZXVTRPNLHHFDB@>0$$2VariableLow levelGPS@New Alluvium060020002T01-a00T0000mkigeca_ZXVRRPNJHD6*%2VariableLow levelGPS@New Alluvium0501-b0TWater02T01-a00T0000usqomkigb`^ZSQOJHD6*%O0N/ALow levelGPSf@New Alluvium070P0003T0T00T0000ca_][YWUSQOKKIGEC?1% 0N/ALow levelGPS`@ New Alluvium0700000300000T0000ca_][YWUSQOKKIGEC?1% ~33316MidslopeGPS@ Chinle Formation030000P0300300T0000jhfdb`^\XVRPPNLJHD2&!}Y0n/aLow levelGPS"@ New AlluviumP0070PBiotic soil1-a1-a01-a00T0000wusqomkidb]XKIGCA?1% |U9160High SlopeGPS@ Old Alluvium020000020200400T0000hfdb`^\ZVTPLLJHFD@2&!{VariableVariableHigh SlopeGPS"@ Kayenta FormationP09000PT0T00T0000zxvtrpnljhfddb`^ZXE94(zj6348High SlopeGPS\@Kayenta Formation041-a0001-bP00400T0000omkigeca][YTTRPNIE2&!y15120MidslopeGPS@Navajo Sandstone020500PBiotic soil1-b1-b01-b00T0000~|zxvtrpkid_RPNLHD2&!xmvariablevariableLow levelGPS@New Alluvium060P001-bP0P00T0000wusqomkigec^^\ZXVRD83(wcvariablevariableLow levelGPS@Eolian deposits1-b0060003P0T00T0000|zxvtrpnljhddb`\ZUD83(vaG1variableLow levelGPS@New AlluviumPP04001-b0200200T0000mkigeca_[YUPPNLHFD6*%u3variablevariableLow levelGPS@New Alluvium0007001-a1-a01-a00T0000}{ywusqojhc^^\ZVTRD83(tDvariablevariableToeslopeGPSv@Navajo Sandstone0030300T0300200T0000}{ywusqokiecca_[WUC72(suRvariable100MidslopeGPS@Navajo Sandstone0206000P0200200T0000xvtrpnljfd`^^\ZXTP>2-#rFPVariableVariableHigh SlopeGPSH@Carmel Formation06P0004Biotic crustTT0T0000000}{ywusea_][WE94(qhbVariableVariableHigh SlopeGPS@ Carmel Formation0P0005Biotic crustsTT0T0000000~|zxvtrc_][YWE94(p1088MidslopeGPS@ Carmel Formation0400001-aP00400T0000jhfdb`^\XVTOOMKIGC1% o,882MidslopeGPS@ Carmel Formation0400001-aP00400T0000hfdb`^\ZVTRMMKIGEA/#nz11220MidslopeGPS@ Navajo Sandstone0207001-aBiotic soilPT0T00T0000xvtrpnljhfdbUPNLHD2&!LVAL. . , ff@PHigher terrace area along major wash channel, with deep, fine soils.Narrow canyon bottom here means no large or homogenous patches of vegetation not influenced or invaded by talus species.Mostly sandy stream terraces, some cobble areas on banks. Plot includes wash, with some water. This is a more mesic channel here than in most of canyon, though the effects don't extend beyond immediate vicinity of channel.Compact, stable sandy soils on low stream terraces.Broad, low stream terrace of sandy, stable soil.Steep, eroding slopes with some Wingate-derived colluvium, but soils are Chinle.Broad, sandy stream terrace next to Pleasant Creek. Lots of areas of large cobbles. Significant cottonwood seedlings or small saplings in plot.Black volcanic boulder country. Soils are full of small pebbles.Plot is located on a broken, cliffy area on the rim of an escarpment. The area is transected by lots of joint fractures w/small pockets of soil.Very rocky, shallow soils and exposed bedrock.Lots of exposed bedrock, with some areas of deeper soils. Soils are rocky and heavily transected by shallow rock-bottomed gullies.Plot is centered in wash channel, and encompasses two discrete communities along the banks and the higher stream terraces.Duney topography in a wider area of the canyon floor, with some actively moving sands.Narrow wash bank/stream terrace, plus part of wash channel included in plot.Plot includes some bedrock on wash edge with CERINT, but most of plot is alluvium in channel and on a low stream terrace.The main wash occupies center of plot, essentially without vegetation, so plot in practice records the vegetation on the toeslopes that border wash channel, mostly bedrock and thin soils.Slabby canyon sides with small ledges. Soils limited to ledge areas.Gypsiferous soils. Plot is centered in the bottom of a steep-sided wash gulley, so there's less biotic crust than there might otherwise be in the vicinity of plot.LLVAL  h(bpGently sloping mesa top covered in small, basalt rock chunks and scattered volcanic boulders. High native grass density.Lots of small, basalt rock chunks on the surface and scattered volcanic boulders. Clean community.Navajo slickrock exposures/rises at the base of large Navajo cliffs. Vegetation growing in cracks and in shallow soil pockets. Lots of small, flat rock chunks and black volcanic boulders on top of bedrock and soil areas. P-J are fairly stunted. Other Surface Geology: Boulder depositsBroad, abandoned river channel in the oxbow. POPFRE are young here and mostly occur near the base of the rock wall face, where they receive pour-off from above possibly. Some moss development.Deep, sandy soils on this alluvial terrace in a narrow canyon bottom. Heterogeneous understory here. EQULAE probably present because there is surface water, though it's pretty stagnant. Mature POPFRE.On an alluvial terrace at the base of N-facing Navajo walls and S of the wash in this narrow canyon bottom. Homogenous ACENEG woodland and the ground carpeted in BROTEC and litter.At the head of the side canyon in an alcove below a large pour-off on the Wingate walls. Toeslopes face NW & SE and are covered in the 3 co-dominant tall shrubs with a POAFEN understory. Very narrow canyon here, so probably shaded most of the day. Small wash runs N through plot and is interspersed with large Wingate boulders.Broad wash nearly devoid of vegetation, more bare soil and small rocks than anything else. Fairly narrow canyon with small colluvial toeslopes to the E and W.Point landed on a small knoll with a steeper slope than majority of polygon. Other Surface Geology: BB-SW interfaceA slightly higher bar in a braided wash channel, clearly flooded during intermittent flash floods - ARTTRI has lots of collected debris on it.Area is separated from Fremont River by State Highway, but is really part of the Fremont floodplain - a high terrrace up against the canyon wall. Deep soils.gYi  p n rr ` c_N/AN/ALow levelGPS@Obscured by Soil/lawnP00003Road gravel/parking area0600000T0000~|zxvrXTRPNL5)$\N/AN/ALow levelGPS6@New Alluvium020001-aWater05P0T00020000sqomkgeca_]YRMKIGC5)$o3340High LevelGPS@Terrace gravel deposits1-a0000030200400T0000trpnljhfb`\XXVTRPK2&!4307High LevelGPS @ Terrace gravel deposits1-a0000030200400T0000trpnljhfb`\XXVTRPK2&!w2343High LevelGPSV@Terrace gravel deposits020000031-a00400T0000trpnljhfb`[WWUSQOK2&!3334High LevelGPS@ Terrace gravel deposits1-b0000031-b00400T0000usqomkigca\XXVTRPK2&!VariableVariableHigh LevelGPSF@Terrace gravel deposits030000031-b00200T0000}{yusnjjhfdb^E94(B4335High LevelGPS@Terrace gravel deposits020000031-b0040000000trpnljhfb`[WWUSQOK2&!2332High LevelGPS0@Terrace gravel deposits1-a0000031-a0050000000usqomkigca\XXVTRPK2&!y5326High LevelGPS@ Terrace gravel deposits1-a0000031-b0050000000usqomkigca\XXVTRPK2&!3120High LevelGPSF@Terrace gravel deposits1-b0000031-b0040000000usqomkigca\XXVTRPK2&!N4129High LevelGPS@Terrace gravel deposits1-b0000031-b0040000000usqomkigca\XXVTRPK2&!1972MidslopeGPS@Terrace gravel depositsP000003020040000000pnljhfdb^\XTTRPNLJ1% ;fN/AN/ALow levelGPS^@New Alluvium0200000600000020000igeca][YWUSOOMKIGC5)$e453High LevelGPSf@Obscured by soil0300002Cryptos021-a00200T0000wusqomkiec^ZQMKIGC1% ZvariablevariableHigh LevelGPS@@Navajo SandstoneP030001-a0200300T0000~|zxvtrnlhcca_]YWE94(t0N/ALow levelGPS@New Alluvium0500002Moss1-b1-a01-a00P0000rpnljhfd_]XSMIGEC?1% J0N/ALow level1:24K Quad@New Alluvium00040PWater031-b01-a001-b0000zxvtrmkidb]YRPNJHF8, T0N/ALow level1:24K Quadj@New AlluviumT000008T00001-b0000kigec^\ZXVTPPNLJHF8,  b0N/ALow level1:24K Quad@Chinle Formation04T00004020P00T0000pnljhfdb`^ZVVTRPNJ8, @2210Low level1:24K Quad>@New Alluvium0T0400T0200400T0000ljhfdb`^ZXTRRPNJHF8, X)10VariableMidslopeGPS@Morrison Formation04P0001-aP0040000000rpnljhfd`^\WWUSQOK7+&?3210Low levelGPS@New Alluvium07000PBiotic crust0200P00T0000qomkigeca_]YKIGEC?1% zLVAL < V TXGently sloping mesa top covered in small, basalt rock chunks and scattered volcanic boulders. P-J invading from polygon and toeslopes to the W.Gently sloping mesa top covered in small, basalt rock chunks and scattered volcanic boulders. JUNOST are associated with wash/drainage channel just outside plot to the E.Variable slopes that drain into small wash running N through plot. Less small, basalt rock cover here and more P-J, both may be attributed to the wash, I suppose.Gently sloping mesa top covered in small, basalt rock chunks and scattered volcanic boulders. Clean community with high native grass density and diversity. P-J invading from toeslopes to the W.Gently sloping mesa top covered in small, basalt rock chunks and scattered volcanic boulders. Some possibly invasive P-J just outside plot to the west.Lots of small, basalt rock chunks covering the soil surface and some volcanic boulders scattered. Quite a lot of native grass diversity on this S end of the mesa.Gently sloping mesa top with soil surface covered in small basalt rock chunks with some large volcanic boulders scattered around.Fairly steep NE-facing slope with high grass cover. Lots of dark, volcanic boulder deposits and small basalt rock chunks covering the soil surface. Hard to key out due to the diversity of shrubs and grasses and the low to moderate J-J cover.The TAMCHI and ELAANG have been removed/cut back to their bases and there are dead branches from them scattered all over. POPFRE look mature, maybe a little young right next to the creek. Huge grass diversity in the understory, many of which are non-native, some possibly seeded from adjacent orchard.Fairly sloping bench at the base of Navajo slickrock walls. Soil surface is variable: covered with moss and volcanic boulders towards the cliff face (to the SW) and covered with small gravel farther from the cliff face (to the N) where slope is flatter. Quite a few small JUNOST skeletons standing around.LVAL L B jPoint fell in the dry wash of the canyon bottom and included both the N and S-facing canyon sides. The N-facing slope had denser vegetation, but both sides were the same community. Lots of shale flakes covering the ground.On a sloping canyon side atop the mesa about halfway between wash below (N) and small cliff band uphill (S). Few surficial drainage channels run through plot. Ground covered in flakes of shale rock.Side slope of a small canyon atop this mesa. Small cliff face at the top of the hill (to the S) and a small cliffy pour-off into the drainage channel below (to the N). Lots of flaked-off shale pieces covering the ground.Fairly steep, shaley ridge side above the mesa top. P-J seem pretty stunted here, possibly due to shallow soils. Lots of flat, shaley rocks covering the ground.Point fell on the side of a shaley ridge above the mesa top. Ledgey bedrock exposure are flaking off into small-to-large flat shale chunks. Understory is fairly sparse, but clearly has w co-dominants.Near beginning of the Fremont River Trail in a very dense shrubby area. Point included part of the Fremont and a section of the trail. SALEXI and PHRAUS are growing in thick patches on this terrace above the river.In a maintained park in Fruita with mowed grass under mature (huge) POPFRE. Point included a portion of the road gravel-filled parking area up to the riparian area along the Fremont River (where the SALEXI and other shrubs occurred).Very heterogeneous riparian area. Russian olive and tamarisk have been cut back to their bases, though some are still standing. Also, trees have been trimmed back under the power lines, so there are piles of dead wood here and there. Point includes a portion of the Fremont River.Slightly transitional to a more JUNOST (or P-J) dominated community to the W of here. Other than the presence of JUNOST and SHEROT though it looks like the rest of this polygon - same substrate and dominant grass spp./\n d  b f NTkN/AN/ALow levelGPS:@New Alluvium05000005T0T00T0000geca_][YWUSOOMKIGC5)$n/an/aLow levelGPS@New Alluvium06000003T0T00P0000geca_][YWUSOOMKIGC5)$Q10220High LevelGPST@Navajo Sandstone0403001-aCryptos1-bP0P00P0000ywusqomkige`WRPNJF4(#2variablevariableHigh LevelGPS@Eolian Sands0500003Dark cyano1-b00000P0000~|zxvtrma][YWSE94(variablevariableHigh LevelGPS@Navajo SandstoneP02T01-aCryptos021-b00300P0000~zxsofa_]YWE94(}variablevariableHigh LevelGPS@Eolian Sands040P003Dark cyano0200000P0000}{ywusqma][YWSE94(variablevariableHigh LevelGPS@Eolian Sands031-aP002Dark cyano03P0T001-a0000~|zxvtpd`^\WSE94()variablevariableHigh LevelGPS@Eolian Sands0400004Dark cyano1-b00T00P0000~|zxvtrma][YWSE94(9128High LevelGPS.@Eolian Sands021-b0002Dark cyano02P01-a001-b0000{ywusnljeca]QMKID@2&!5142High LevelGPS@Eolian Sands02T0003Dark cyano03T0T001-b0000usqomhfdb`^ZNJHFD@2&!C9300High LevelGPS2@Eolian Sands06P00003T0000P0000db`^\ZXVTRPLLJHFD@2&!8335High LevelGPSJ@Navajo Sandstone1-b1-b001-bDark cyano031-b00200T0000~|zxvtrnlgcWRPNID2&!0N/ALow levelGPSj@New Alluvium031-aP01-aWater1-b0201-b00T0000vtrpnljhca]XQLJHC?1% z%20120High SlopeGPS@Kaibab Limestone0200001-b0200500T0000omkigeca][WRRPNLJF4(#VariableVariableLow levelGPS@Moenkopi FormationP020001-b0300300P0000}{ywusomiddb`^ZXD83(13347MidslopeGPSN@Moenkopi FormationP1-b0001-b0300400P0000pnljhfdb^\XSSQOMHF2&!15355Low slopeGPSZ@Moenkopi FormationP1-a0001-a0400400P0000qomkigec_]YTTRPNIG3'"7VariableVariableLow levelGPS@Moenkopi Formation1-a1-a000020400300P0000~|zxvrplhhfdb]XD83(16318MidslopeGPS@Moenkopi FormationP1-a0001-b04003001-a0000sqomkfdb^\XSSQOMHF2&!22343MidslopeGPS@Moenkopi FormationP020001-b0300400P0000omkigeca][WRRPNLHF2&!20353MidslopeGPSH@Moenkopi FormationPP0001-b0300500P0000mkigeca_[YUPPNLJHF2&!10150MidslopeGPS@Moenkopi FormationP030001-a1-b00500P0000pnljhfdb^\WRRPNLHF2&!_0N/ALow levelGPS@New AlluviumP0001-aWater07P01-b00P0000nljhfdb`[YWSLGECA?1% LVAL X  b0Sloping mini-hogbacks covered in small, flat rocks. Very homogenous community.Duney area at the base of Navajo fins. Lots of dead wood in plot, some dead trees still standing but most have fallen over. Two surficial drainages run E and SE through plot. Dunes are stabilized by dark cyano.Duney area at the base of Navajo fins with a little bedrock exposure in the plot. Scattered P-J with a dense understory dominated by OPUFRA and MUHPUN.Sort of a depression area between Navajo fins and formations. Very little JUNOST in comparison to the high PINEDU cover. Vegetation growing in shallow soils atop bedrock. Ground surface covered in litter, tiny rolly rocks and some dark cyano. P-J more stunted where soils are more shallow.Riparian strip to the S of Sulfur Creek mostly, as cliff face is on the N side of the creek. Point captured a section of the creek and the trail alongside it. SALEXI look young, just recolonizing perhaps. CHRNAU is thick on the lower terrace, with more of a ATRCAN - CHRNAU mix on the second level terrace.On a steep N-facing Kaibab slope. Lots of shrub and grass diversity. Some JUNOST skeletons scattered around. Lots of small rocks covering the ground and "Velcro" boulders are all over as well. ATRCAN are very dwarfed her.Point fell along wash in the canyon bottom atop this mesa. Included the steep, S-facing slope which has really sparse vegetation, and lots of bedrock/cliff band exposure, as well as the more gradual N-facing slope which has vegetation more typical of the polygon. Still, lots of shaley rock flakes covering the ground.Fairly steep canyon side atop this mesa. Some bedrock ledgey exposures upslope (to the S) are actively flaking off. Ground is covered in small to large shale flakes.Fairly steep, low slope of the N-facing canyon side atop this mesa. Few ledgey bedrock exposures actively flaking off, and ground is covered in small to large shale flakes.>LVAL R ~ 2^A weedy/disturbed terrace, though native grass cover is low to moderate. CHRNAU and ATRCAN are co-dominants and JUNOST are scattered throughout the polygon.Fairly level terrace that is carpeted with BROTEC; though just outside point to the WNW the polygon is an ERINAU/BOUGRA-STIHYM shrub herbaceous type that has scattered JUNOST, SHEROT and MAHFRE throughout.Broken ledges and Navajo outcrops along the base of a Navajo fin. Sort of a small polygon/community here which transitions to adjacent polygon to the W right near point.Fairly flat area atop this mesa with small moundy hills that P-J are growing on top of. OPUFRA so thick that it is hard to walk around in here. Some die-back/dying PINEDU, possibly from the bark beetle.Broken ledges below a Navajo fin cliff face. Lots of small rolly rocks on the surface and some crypto development. ARCPAT restricted to the wash running SW through plot. P-J are stunted on the shallow soils atop bedrock and larger near the wash. Hilly area with variable slopes and aspects, mostly sloping SW away from the cliff face.Duney area right at the base of Navajo fins somewhat stabilized by dark cyano. Wash runs along the E margin of the plot. Understory component has been homogenous throughout the polygon and dominated by OPUFRA and MUHPUN.Duney area right at the base of a Navajo fin. Some soil areas stabilized by dark cyano. Wash runs S through plot and the CERINT and SHEROT are associated with it. Lots of dead wood, some recently that still has brown needles on it.Duney hills at the base of Navajo fins stabilized by dark cyano. Quite a bit of dead wood scattered around. Understory clearly has 2 co-dominants, but no association name puts them together.Duney hills below Navajo fins with much of the soil surface stabilized by dark cyano. More Navajo bedrock exposure in this plot, especially in the west half. Few surficial drainages run S and SE through plot. Lots of dead wood here, some standing but most lying on the ground.LVAL \ ` df0:Broad (~6m), flat wash bottom covered in small rocks. Banks are 1/2 - 1m high and lined with JUNOST and a desert shrub mixture. Not much growing in the wash bottom.Broad floodplain dominated by SARVER, except for this small polygon which has an odd shrub mixture. Seems like the Atriplex spp. are the most dominant. Soils are very sandy, so I called all the bare soil 'sand'.Badlands toeslopes below Wingate cliffs bisected by multiple drainages. Sparse vegetation. Some gypsum salt crystals scattered about on the soil surface.On a steep, N-facing colluvial toeslope on the side of Spring Canyon. Lots of shrub diversity. A few bouldery drainage channels run downslope.Wider canyon here and wash channel much broader and sandier (so much so that called all the bare soil here sand). POPFRE are mature. Less litter and more sandy terraces in this plot.Narrow canyon bottom with Navajo fins to the NW and SE. Wash has several channel here, all of which have EQULAE growing along their sides. POPFRE are mature. Sandy, alluvial soils.POPFRE Woodland with a POPANG subcanopy, not something I've seen yet! Lots of downed wood and litter covering the ground. ARTTRI appear to be invading this terrace from the higher terrace to the N.High bench/terrace above Pleasant Creek and South Draw Road with homogenous ATRCAN community. Deep alluvial soils and lots of litter around the shrubs. ATRCAN is very thick in here!Slightly rolling microtopography with several surficial drainage channels running N through plot. Ground is covered in small rocks. JUNOST are much fewer than the PINEDU here and are all stunted (<2m tall), even though PINEDU are a more average height.Creek has been diverted to a ditch which wraps around the west margin of the polygon, so that it is now flowing 4-6 meters higher than the old terrace because of a man-made dam/barrier. Old creek channel (now dry) runs along the west margin of the polygon so point is on a interfluve/hill between the walled-up ditch and the old channel.g! N  _ # VD:,>175High LevelGPS@Alluvial deposits080001-aBiotic crust1-a00T00P0000zxvtrpnljhfaSNLJHD1% D195High LevelGPS@ Alluvial deposits0700003Biotic crustP00T00T0000vtrpnljhfdb`RNLJHD1% @1173High LevelGPS@Alluvial deposits0500004biotic crust1-a00000P0000zxvtrpnljhfaSOMKIE2&!G283High LevelGPS@Alluvial deposits0600003Biotic crust1-a00T00P0000ywusqomkige`RNLJHD1% H273High LevelDEM@Alluvial deposits0500004Biotic crust1-a00T00P0000ywusqomkige`RNLJHD1% I1271High LevelDEM@Alluvial deposits0700002biotic crustPT0T00T0000wusqomkigecaSOMKIE2&!LvariablevariableInterfluveGPS@Moenkopi FormationP000Tcryptos02T00700P0000~|zxtrplca_][YE94(543High LevelGPS@Moenkopi Formation03000003T00500P0000kigeca_]YWUQQOMKIE1% 0n/aLow levelGPS(@Obscured by soil0800001-a00P00T0000hfdb`^\ZXVTOOMKIGC1% 5variableLow levelGPSB@New Alluvium05P1-a00P1-a00300T0000nljhfdb`\ZUSSQOJHD6*%w0N/AHigh LevelGPSBedrock exposed - Kayenta (?)Obscured by soil002001-bCryptos1-b001-b001-a0000{rmkiecQ&!N7358MidslopeGPS@Salt Wash Sandstone Member of the Morrison FormationP1-a00PCryptos1-bP00600T0000|sqomhf0$&145Low levelGPSL@ New Alluvium030P001-a1-b00500T0000hfdb`^\ZVTOJJHFDB>0$1N/AN/ALow levelGPS@New Alluvium0009001-bP0T00T0000hfdb`^\ZXVTOOMKGEC5)$VariableVariableToeslopeGPS6@Moenkopi Formation100000P00T0000000ywusqomkigecca_][WC72([1047MidslopeGPS@Moenkopi FormationPP000PP0090000000geca_][YUSQOOMKIGE1% 2832MidslopeGPS @Wingate Sandstone02P0001-a0300400T0000mkigeca_[YUPPNLJHD1% -N/AN/ALow levelGPSp@New Alluvium00070003T0T00P0000geca_][YWUSOOMKGEC5)$)N/AN/ALow levelGPSn@New Alluvium05P00005T0T00P0000geca_][YWUSOOMKIGC5)$2186Low levelGPS@New AlluviumP00000600000030000ca_][WUSQOMIIGECA?1% \0N/ALow levelGPSn@New Alluvium05000005T0T00T0000ca_][YWUSQOKKIGEC?1% 4329High LevelGPS@Carmel Formation1-b000PCryptos021-a00500P0000wusqomkiec^ZQOMKID2&!z0N/ALow levelGPS@New Alluvium05000004P0T00P0000ca_][YWUSQOKKIGEC?1% LVAL T P 2Hillside with small hummocks and depressions between. Good cover by biotic crust. Lot of small mammal activity.Flat areas with small hummocks and areas of deflation that have been stabilized by biotic crust. Very few shrubs here because it is more of a sand flat w/out the small dunes of previous points in the polygon.Relatively flat area with small areas of deflation and minor hummocks. Surface stabilized by biotic crust. Old burrowing activity. The soils are deep, but have less hummocking than at previous sites in the polygon.Site similar to 508, has stabilized dunes w/good biotic crust development. Dune tops have more ERINAU and slopes and basins have more ERIMIC. ACHHYM distributes throughout. Lot of small mammal activity.Point lies on stabilized dunes with undulating topography. Active dunes (very small) to the NW/W have SARVER shrubs. Biotic crust here has stabilized the soil. Quite a lot of small mammal burrowing.Western edge of a large alluvial plain. Soils are deep with minor hummocking, biotic crust present and controlling erosion. Minor areas of deflation. Large wash to the west approximately 50 meters is incised up to 2 meters.Rolling hills that resemble toeslopes with small canyons on N & S sides. Soil surface covered in small, platey rocks, few pockets of well-developed cryptos. Some signs of drought-stress on PJ.Soils appear deep here and are covered with platey rocks. Healthy P-J stand.Broad flat area with a ditch running through the middle and man-made berms bordering one side of plot. Well-developed cryptos through most of plot.Plot encompasses sloping wash terraces on both sides of this wash, so slope and aspect vary. Wash bounded for ~50m of the plot on one side by big Kayenta cliff.Low, almost stunted JUNOST Woodlands with a mixed shrub, fairly sparse understory with 2 co-dominants. Soils are shallow and rocky atop conglomeratic bedrock. Lots of pebbly rocks on the surface and some cryptos.LVAL 8 :tSoil is hummocked with small mounds around clumps of grass and shrubs. Small depressions are formed between. There is some biotic crust. Some elk scat.Flat plain with many small mammal burrows. Minor hummocks under grass clumps and small depressions between. Fair biotic crust. Lot of GUTSAR- past disturbance.Slightly raised areas are present around perennial grass clumps. Only minor biotic crust development, but soil is not eroding rapidly. Lot of small mammal activity here.Small hill at boundary fence has relatively level surface that is protected by biotic crust. Exposure is such that there are few shrubs.Area has small hummocks and a few small blow-outs to 40 cm. deep. Shrub cover is low with past drought die-off notable for ERINAU shrubs. A lot of small mammal activity. A fair biotic crust helps to control erosion.Area of small hummocks and depressions with sufficient biotic crust to control erosion. Lots of small mammal activity. There are several dead ERINAU shrubs, likely the result of past drought.Steep exposure of bouldery talus or colluvium from the mesa to the west. It extends onto the flats and delivers runoff water. This slope is deeply dissected by runoff channels.Site has sparsely-vegetated hummocks and depressions and some deeper hummocks. Soil has good erosion protection with biotic crust cover. There are a fair amount of small mammal burrows here.Area with small hummocks and depressions - SW-face stabilized by biotic crust and vegetation. Lot of small mammal burrowing. Shrubs are generally distributed across this site.Site near the boundary fence consists of small hummocks and depressions. The soil surface has good cover of biotic crust and erosion is presently minimal.Area of small hummocks and areas of deflation that have stabilized with biotic crust and vegetation. Lot of burrowing activity by small mammals. Some shrubs have up to 30cm of stem exposed due to past movement of soil by wind.FR W N H FB11X188High LevelGPS\@Entrada Sandstone02P0006Biotic crust1-aT0P00P0000ywusqomkige`RNLJHD1% ;28263Low LevelGPS@Entrada Sandstone02P00TBiotic crustT0400400T0000zxvtrpnlhfb`RPNLJF3'"o7271High LevelGPS@ Intrusive volcanics02T000P0400400P0000mkigeca_[YUSSQOMKG2&!W116High LevelGPSR@Alluvial deposits08000PBiotic crust1-a00T00P0000wusqomkigec^PNLJHD1% R1291High LevelGPSr@Alluvial deposits0600002Biotic crust1-a00000P0000zxvtrpnljhfaSOMKIE2&!k693High LevelGPS(@Alluvial deposits1-b020005Biotic CrustP1-a0P00T0000|zxvtrpnljecUQOMID1% \3254Low LevelGPSv@Alluvial deposits0700002Biotic crustTT01-b00T0000ywusqomkfdb`RNLJHD1% Y1348High LevelGPSB@Alluvial deposits0500004Biotic crustP00T00P0000wusqomkigecaSOMKIE2&!<2272MidslopeGPSN@Alluvial deposits0600003Biotic crustP00T00T0000usqomkigeca_QMKIGC0$=281High LevelGPS@Alluvial deposits0700002Biotic crustP00T00T0000vtrpnljhfdb`RNLJHD1% ?2361High LevelGPS@Alluvial deposits09000PBiotic crustP00T00T0000usqomkigeca_QOMKIE2&!71281High LevelGPS|@Alluvial deposits09000TBiotic crustP00T00T0000usqomkigeca_QOMKIE2&!>2107MidslopeGPS4@ Alluvial deposits080001-aBiotic crustP00T00P0000vtrpnljhfdb`RMKIGC0$;3108MidslopeGPS@ Alluvial deposits0600003biotic crustP00T00P0000usqomkigeca_QMKIGC0$A1291High LevelGPSD@ Alluvial deposits0700002Biotic crustP00T00P0000wusqomkigecaSOMKIE2&!>0n/aHigh LevelGPSV@Alluvial deposits070001-abiotic crustP00T00T0000xvtrpnljhfdbTOMKIE2&!<3295MidslopeGPS@Alluvial deposits0400004Biotic crust1-a00000P0000xvtrpnljhfd_QMKIGC0$<163High LevelGPS@Alluvial deposits0601-a003Biotic crustP00T00P0000ywusqomkigecUQOJHD1% >110High LevelGPS@Alluvial deposits0700002Biotic crustP00T00P0000vtrpnljhfdb`RNLJHD1% K1872ToeslopeGPSd@Entrada Sandstone1-b0000T0700200T0000kigeca_]YWSQQOMKID1% C2195High LevelGPS@Alluvial deposits0300006Biotic crustP00T00P0000wusqomkigecaSOMKIE2&!>2281High LevelGPSb@Alluvial deposits0500004Biotic crustP00T00P0000wusqomkigecaSOMKIE2&!C2195High LevelGPS6@Alluvial deposits080001-aBiotic crustP00T00T0000xvtrpnljhfdbTOMKIE2&!`LVAL  : 4 HP.J. woodland is limited to volcanic exposures at this elevation. The stands are mostly J, growing among volcanic boulders. There are many dead trunks from historic fire and drought. There is an intrusive volcanic dike here.Site is near a canyon rim and the soils are less deep, probably more alkaline. Only low small mammal activity occurs, as the soils are nearly level with fewer hummocks.Area of deep alluvium with some minor surface hummocks formed. Lot of small mammal activity. Site is a mild flat with some gentle low ridges further east. Many OPUPOC are dying here.This site includes sheer cliffs of Entrada sandstone to the western edge, therefore it contains alluvium, rockfall (sandstone, shale, and basalt rocks deposited higher up), and is dissected by small drainages eroded to 1 to 3 meters deep. Biotic crust is very well developed.An area of alluvium washed down from mesa to the north. Small mounds of eolian material have formed on an otherwise hard crust and support most vegetation. There is some biotic crust development. A drainage cuts across the southern edge of the AA point, about 15 meters wide. Highly dissected by small drainage.Soils are clay and alkaline, exhibit cracks to 2 cm wide after drying. There is good biotic crust development in patches, but not throughout. Elk use the area.Soils are relatively flat here, with little of the hummocking that occurs to the west. Biotic crust helps to protect from erosion. Small mammal activity is moderate.Minor hummocks have formed on this site, but soils are stabilized by biotic crust development.Grazed site with livestock trail in point area. Only a small amount of biotic crust remains. Perennial grasses and shrubs grow on elevated patches of land with depressions to 10 cm deep in between.Grazed land about 40 m north of existing fence line. The surface is nearly flat and quite weedy with Eriogonum species (annual). There is no small mammal activity. Trampling by livestock.RLVAL D z tvPoint has old dunes to 1.5 meters tall and deflation areas between. The dunes are stable and support encroaching JUNOST trees. Soils are very deep here.Site is a broad bench of Middle Desert Wash, about 50 meters from the wash. Alluvial soils are very deep with some biotic crust development. The shrubs here are stunted possibly due to alkalinity or to distance to ground water.Moderate slope with volcanic boulder (basalt) rocks and relatively deep soil. There is little biotic crust. Downed wood is common due to age of stand and fire history.Slope of mixed PJ that are short- stature. There is good recruitment of both species here. The site is near the campground, but only a trail appears to be disturbed. Minor biotic crust development. Rock here is volcanic- basalt.Brood desert wash with banks of ERINAU on the banks and on all cobble piles. Recent erosion cut away 25 meters of bank to six meters deep. Wash bottom is armored with basalt rock cobble.Moderate dunes here, up to two meters high, that have a few small active areas. Old dunes are stabilized by biotic crust. Colonizing grass is MUHPAN. Lot of small mammal activity.Area of small hummocks and minor drainages, has fair cover by biotic crust. Shrubs are rooted in hummocks and grasses in depressions.Area with soil hummocks to about one meter tall with small basins between. Good biotic crust formation. Shrubs occupy hummocks and MUHPUN occupies depressions.Area of soil mounds with small areas of deflation and dissected by drainages. Some biotic crust formation. Little small mammal activity here.Thin soil covers bedrock exposure here, site is alkaline. Good biotic crust development. There are a few scattered JUNOST trees north of the site, where bedrock is exposed.Steep highly dissected side canyon to Middle Desert Wash. Some erosion faces are devoid of vegetation, while soil remaining between drainages supports most vegetation. Many volcanic boulders are present on the sandstone.WP C < - 2=AAe333High LevelGPS@Alluvial deposits0600002Biotic crust0200000T0000xvtrpnljhfd`RNLJHD1% p3265High LevelGPS>@Alluvial deposits09000PBiotic crustP00T00T0000usqomkigeca_QOMKIE2&!372Low LevelGPSL@Entrada Sandstone08000PBiotic crust1-a00T00P0000vtrpnljhfdb]OMKIGC0$283Low LevelGPSj@Entrada Sandstone08000PBiotic crustPT0P00P0000sqomkigeca_]OMKIGC0$298High LevelGPSZ@Entrada Sandstone07000Pbiocrust1-b00T00P0000sqomkigeca_ZPNLJHD1% 383High LevelGPS4@ Entrada Sandstone070001-bbiocrust1-a00T00T0000vtrpnljhfdb]SNLJHD1% 288Low LevelGPS@Entrada Sandstone0700002biocrustP00T00T0000qomkigeca_][QMKIGC0$493Low LevelGPSV@Entrada Sandstone09000PbiocrustPT0P00T0000omkigeca_][YOMKIGC0$185High LevelGPS"@Entrada Sandstone08000PbiocrustP00T00P0000pnljhfdb`^\ZPNLJHD1% 5192High LevelGPS@Entrada Sandstone07000PBiocrust1-a00000P0000trpnljhfdb`[QOMKIE2&!1762Low LevelGPS@Entrada Sandstone06000PBiocrustTP00300T0000sqomkigea_][QOMKIE2&!673Low LevelGPS@Entrada Sandstone060001-bbiocrustTT00300T0000trpnljhfb`^\RMKIGC0$483Low LevelGPS@Entrada Sandstone080001-bbiocrustPP0P00T0000rpnljhfdb`^\RMKIGC0$3185High LevelDEM@Entrada Sandstone0600002Biotic crustPT00200T0000ywusqomkgecaSOMKIE2&!18Low LevelGPSZ@Alluvial deposits050001-bBiotic crust1-b020P00P0000ywusqomkigc^PKIGEA."195Low LevelGPS@ Alluvial deposits0500002Biotic crust1-bP01-a00P0000{ywusqomhfd_QMKIGC0$t10108MidslopeGPSR@Entrada Sandstone02000PBiotic crust041-b003001-a0000}{ywrpnjhc_QOMKIE2&!^4106MidslopeGPS@Entrada Sandstone0400002Biotic crust020201-b00P0000|zxvtrpnigc_QMKIGC0$2175Low LevelGPSx@Alluvial depositsP01-a00T0300500T0000jhfdb`^\XVRPPNLGEC0$<396High LevelGPSl@Alluvial deposits0700002Biotic crust1-a00T00T0000ywusqomkige`RNLJHD1% 5293High LevelGPS @Alluvial deposits0600003Biotic crust1-a00000P0000ywusqomkige`RNLJHD1% 1278High LevelGPSD@Alluvial deposits0500004Biotic crust1-b00000P0000ywusqomkige`RNLJHD1% 22360High LevelGPS@Alluvial deposits0500004Biotic crust1-b00000P0000zxvtrpnljhfaSOMKIE2&!bLVAL @NSite includes a drainage about 20 meters wide that is salt encrusted. Vegetation only grows on mounds of soil where salt is exposed. Soils on terraces and flats are mounded with minor deflation areas. Very popular lick for elk.Shale soil that has eroded from pinnacles to the west. Site consists of fans dissected by drainages, many of them pure white with salts. Quite a bit of elk activity here.Flat area of deep alluvium with some deep drainage channels in the vicinity. Utah Juniper and a few Pinion trees are encroaching into this site.Site a sloping plain with a drainage about five meters wide by 4-5 meters deep. Soils are fine sand, subject to blowing. Surface has been tracked, broken by elk. Annual weed skeletons here SALTRA, there are a few Juniper trees invading.A toeslope eroded from Entrada sandstone pinnacles on the west side of the point. Mostly shale soil on fans with rills to 1-3 meters deep present. Sandy alluvium occurs to the east where ERIMIC is common.This is the toeslope eroded from pinnacles on the western side of the point. It is comprised of shale soil fans dissected by rills to one meter deep. Sand alluvium occurs to the east where ERICOR is replaced by ERIMIC.Toeslope of ridge that is composed of deep alkaline soil. Small drainage in point about 4 meters wide and incised 3-4 meters deep - bottom crusted with salts. There are some basalt rocks on this landscape.Sparsely vegetated area at the toe of pinnacles to the north. Sand and silt eroded from these pinnacles are deep and alkaline. Runoff is rapid with many small rills present, a drainage about 5 meters wide by 2 to 3 meters deep is on the south edge of the point.Point is on the first terrace of Middle Desert Wash, a broad terrace that continues to the cliff face. The wash is incised (sic) up to 4m and is ~10m wide. Shrubs here are short, possibly due to alkalinity) or to depth of ground water. Point is bisected by an old 2-track road that is revegetating.HLVAL < b*$:nSeries of small ridges dissected by gullies. The entire area is subject to erosion by water and wind.P-J trees retain small mounds of soil and litter under the drip lines creating low hummocks, otherwise much of the site is flat. There are a few small rills armored by basalt rocks. Quite a few down trees and branches.Stunted stand of PJ growing from shale soil in basalt boulders and gravel. Small drainage run through area, most trees are on elevated hummocks of soil.Mature PJ trees with many dead trunks and wood on the ground. The soils are deep, shale-derived and have desiccation cracks to 1 cm wide. Most of the inter tree space is barren and the trees have accumulated mounds of soil and litter up to their drip lines.Area of alluvium with minor hummocks and adjoining deflation areas. Site is ~25 m. from the road. Lots of elk use here. Biotic crust development is good.Deep alluvium about 50 meters from road. Some soil has piled around shrubs, but most is level. There is fair biotic curst development. Elk use the area.This in the area collecting erosion from vertical cliffs including rockfall debris and shale soil. It is steep, hard-packed and highly erosive with many drainage channels.Deep alluvium adjacent to cliffs. Surface is mounded with small rills present. Soil is alkaline.An area of alluvium that has been partially disturbed by historic road construction. The road track is revegetating. The alluvium is very deep and hummocked.Point is at the edge of the large plain and near the primary access road. Soils are alluvial that are deep and dissected by drainages. Some biotic crust has formed.The point lie on alluvium with moderate hummocking adjacent to a wash, but not its terrace. The wash bottom is about 5m wide and is unvegetated. With terrace it is about 15m wide.Deep alluvium that has low hummocks, small depressions and rills. There is elk activity and more Opuntia than elsewhere in the polygon. GUTSAR is present in large numbers.w\ K U  e hkSX,27175Low LevelGPS@Entrada Sandstone021-b000T0300300T0000omkigeca][WUUSQOJF3'" g773Low LevelGPS@Alluvial deposits0300005Biotic crustP1-b0P00P0000xvtrpnljhfa_QMKIGC0$  l571Low LevelGPS,@Alluvial deposits0600003Biotic crustPT0T00P0000usqomkigeca_QMKIGC0$  W281Low LevelGPS@Alluvial deposits0200001-a0300400T0000ljhfdb`^ZXTOOMKIGC0$  J3174High LevelGPS@Alluvial deposits060001-bBiotic crust02T0T00T0000zxvtrpnljhfbTOMKIE2&!  4291MidslopeGPS@Alluvial deposits0300004Biotic crust02000001-b0000zxvtrmkigec_QMKIGC0$ 893High LevelGPS*@Alluvial deposits1-a0001-aBiotic crust1-a05003001-a0000~|zusqmkgbTOMKID1% 298High LevelGPS@Alluvial deposits050001-bBiotic crust0300T00P0000ywusqomkigeaSNLJHD1% 1141High LevelGPS@Alluvial deposits0500002Biotic crust0200T00T0000ywusqomkigeaSOMKIE2&!184Low LevelGPS@Alluvial deposits04000002020P00P0000igeca_][YWSOOMKIGC0$8112MidslopeGPS@Boulder deposits030001-bBiotic crust1-a0300200P0000|zxvtrpnjhd_QLJHFB0$22281Low LevelGPS@Boulder deposits020000P0400300P0000kigeca_]YWSQQOMKIE3'"16High LevelGPS@Alluvial deposits07000PBiotic crust0200000P0000trpnljhfdb`\NLJHFB/#5178High LevelGPS8@Alluvial deposits070001-bbiotic crust0200000P0000zxvtrpnljhfbTOMKIE2&!437MidslopeGPS\@Boulder depositsP000003P004001-a0000hfdb`[YWSQOKKIGECA/#698High LevelGPS@Boulder depositsP00000302004001-a0000ljhfd_][WUQMMKIGEC1% U31168Low LevelGPS@Alluvial deposits0200001-b0500200P0000omkigeca][WRRPNLJF3'"1276High LevelGPS@ Alluvial deposits1-a000TDark cyano030300200P0000zxvtrpnlhfb^RPNLJE2&!3165High LevelGPS2@ Alluvial deposits02000030200300P0000kigeca_]YWSOOMKIIE2&!M1351High LevelGPS@Alluvial deposits060200PBiotic Crust0200P001-a0000|zxvtomkigeaSQOMIE2&!\1101High LevelGPS8@Alluvial deposits0500004Biotic crust1-a00T00T0000zxvtrpnljhfaSOMKIE2&!Z291High LevelGPS4@Alluvial deposits0600003Biotic crust1-b00T00P0000ywusqomkige`RNLJHD1% d21281MidslopeGPSX@Entrada Sandstone041-b000T0200200T0000nljhfdb`\ZVTTRPNIE2&!LVAL 0 6XLevel area with small hummocks supporting most of the vegetation. There are some small, barren, hard pans Deflation areas are small and have some biotic crust development. The access road crosses the S edge of the AA point.This is a broad wash bottom high in the drainage. The channel is incised (sic) up to 2m deep and is ~5m wide. The point falls on it's first terrace which is lined with boulders adjacent to the channel.A confusing area of basalt rock capped ridge and fine-shale soil slopes that are highly eroded. The P-J ranges from sapling to mature and occupies areas with rock cover. There is some biotic crust cover between basalt rocks and boulders.Steep slope with a veneer of basalt rocks and gravel. It is dissected by gullies up to 5m deep. The P-J trees are somewhat stunted although mature and there are several dead trees here. There is mistletoe on some JUNOST.Deep alluvial soil with extensive cover by BOUGRA. There is little biotic crust development but the herbaceous cover stabilizes the soil. Old shrubs have pedestals of soil to 0.4 m. deep around their drip line.Site is deep alluvium that is very level. Biotic crust development is poor. A very dense stand of BOUGRA is present and serves to stabilize the soil well.Site is mostly volcanic gravel on the surface with only a few small boulders. The trees are mature and there is a lot of down wood. There is some recruitment of both P & J.Mild slope covered with basalt rocks and gravel with pockets of soil between. Trees have built small platforms of soil and rock on their uphill side. There is good recruitment of pinyon trees here. Stand is mature with fair amount of down wood.Site occupies an eroding slope of fine soil and basalt boulders. The slope is seepy in places exuding salts that support ATRCAN and SPOAIR. P-J and SHEROT grow on elevated fans between drainages. The drainages are armored by basalt rocks. LVAL  ^ ,.Site is quite mounded with hummocks up to 1 - 1.5m high. These have mostly held together by shrubs. There is wind erosion from the flat surfaces and mound edges. SPOAIR cover is good and helps to control erosion.Area of deep alluvium with hummocks to 1 meter high. There is some biotic crust present, along with vegetation cover. Erosion appears minimal. Small mammal use is high.This point includes talus toeslopes from adjacent cliffs that are characterized by eroded shale and rockfall, in addition to gullying. There is a wash about 15 meters wide at the base of the talus--it is devoid of vegetation.Point lies on a small ridge in the floodplain that is capped by basalt rocks. Gullies have eroded on either side of the ridge to 3 m. deep. Soils are hummocked with some areas of deflation. There is good biotic crust development.Point lies on a toeslope of a shale deposit that is eroding into the valley. It consists of mounds to 3-4 m. tall and drainages (swales and gullies).This wash has a central drainage ~5 m. wide that has incised up to 4 m. deep. It is lined by basalt boulders and cobble which channelize it. Terraces are elevated 1-2 m. above the channel at this point.Gently sloping area of deep alluvium that is well vegetated and is only lightly eroding. Small hummocks have formed around the few shrubs present. The area is used by elk. Soils show cracking at the surface to ~2 cm. wide in this area.Very deep alluvium that supports a dense stand of ARTTRItri just above incised gullies. There is good biotic crust development. Some JUNOST trees have died and toppled possibly due to historic fire.Area of fans and ridges with deep gullies, most armored by basalt rocks. Soils are present as pockets among rocks and some good biotic crust occurs.Terrace or plain at the base of the South Cliffs, long abandoned by drainage. The alluvium is very deep and level. Elk use the area quite a bit. The basin big sagebrush shrubs are becoming decadent with dead branches and dead shrubs present.HQ Q  u  { 1Sa")&'3382MidslopeGPS@Entrada Sandstone1-b05000T0200200T0000mkigeca_[YUSSQOMID1% %&v35High LevelGPS@Entrada Sandstone0700002Biotic crust1-a00P00T0000wusqomkigec^PLJHFB/#$%4281High LevelGPSH@Entrada Sandstone0200003Biotic crustPT00400T0000ywusqomkgecaSOMKIE2&!#$f2171MidslopeGPS@Entrada Sandstone080000PT00200T0000geca_][YUSQOOMKIGC0$"#6173Low LevelGPS@Entrada Sandstone020000P0200500T0000jhfdb`^\XVRPPNLJHD1% !"6184MidslopeGPS@Entrada Sandstone020000P0200500T0000igeca_][WUQOOMKIGC0$ !W2715MidslopeGPS@Entrada Sandstone1-a00000203004001-a0000pnljhca_[YUQQOMKID1%   27189High LevelGPS@ Boulder deposits1-b00001-b04003001-a0000sqomkfdb^\XSSQOMKF4(#23174MidslopeGPS@Boulder deposits1-b0000030200300P0000mkigeca_[YUQQOMKID2&!386High LevelGPSH@Alluvial deposits0900001-b00000P0000igeca_][YWUPPNLJHD1% 4111High LevelGPS2@Entrada Sandstone060000T0201-b00T0000ljhfdb`^YWSQQOMKIE2&!742MidslopeGPS@Entrada Sandstone090000TP01-b00T0000geca_][YTRPNNLJHFB/#3262High LevelGPS @Entrada Sandstone090000TP0P00T0000geca_][YWUSQQOMKIE2&!1251High LevelGPS@Alluvial deposits0600002Biotic crustPT0P00T0000wusqomkigecaSOMKIE2&!1295MidslopeGPS@Entrada Sandstone030000P1-b00500T0000kigeca_]YWRPPNLJHD1% 8184MidslopeGPS@Entrada Sandstone04000PBiotic crustPP00400T0000usqomkigca_]OMKIGC0$1816High LevelGPS@Entrada Sandstone020600PBiotic crustTP0P00T0000xvtrpnljhfdbTRPNJF3'"1101High LevelGPSV@Alluvial deposits0800001-b00000T0000jhfdb`^\ZXVQQOMKIE2&!682High LevelGPSv@Alluvial deposits1-b0000PP00700T0000igeca_][WUSQQOMKID1% 4272MidslopeGPS@ Entrada Sandstone05P000TP00300T0000geca_][YUSQOOMKIGC0$284Low LevelGPS@Alluvial deposits0700000200000T0000geca_][YWUSOOMKIGC0$18348Low LevelGPS|@Entrada Sandstone020001-bbiotic crustP1-a00600T0000~|zxvtrpljecUPNLJF3'"2191High LevelGPS@ Alluvial deposits0500002Biotic crust0200000P0000ywusqomkigeaSOMKIE2&!192High LevelGPSP@Alluvial deposits070001-bbiotic crust0200000P0000ywusqomkigeaSNLJHD1% LVAL  6 N xThis is a very exposed site both to sun and to wind, thus stunted trees. There is heavy cover by volcanic boulders.Area of low hills, ridges, and toeslopes that are highly eroded. Only minor amounts of volcanic rock occurs here. The site is dissected by small hills, and deeper gullies, some to 3 meters wide. Soils here are very compacted and little vegetation cover persists.Area is a relatively flat plain of alluvium with a few small mounds of Entrada Sandstone. Site drains to large gully ~5m wide x 3m deep that is included on its western side. Soils exhibit cracking or drying ~2cm wide cracks. There is a fair amount of SALTRA here.The site includes hills, ridges, and slopes that have a veneer or mulch (sic) of angular volcanic rock and gravel. Most plants are rooted within this rock-covered area. Erosion is prominent with rills and small gullies present.Site consists of shale hills and ridges capped broken angular basalt rocks and gravel. Areas with the (illegible) of rocks support most of the vegetation cover. The site is conducive to erosion and some rills and swales are present.Exposed Entrada Formation ridges that are eroding fairly rapidly. A 1955 survey marker at this site is exposed ~1m.Flat sloping surface that is quite smooth. Soil cracks to 1-1.5 cm wide and present. There is some sheet erosion. This site has a lot of SALTRA skeletons and seedlings.Ridge of alluvium capped by basalt rocks and gravel. Each ridge is subtended (sic) by gullies on either side. Erosion is checked by the veneer of gravel. Other Surface Geology: EntradaSite is the upland adjacent to the 1st terrace of small wash and contains many of the same species. The soil is mounded where shrubs collect it and there are areas of deflation between mounds.Face of toeslope that has formed off cliffs to the south and flows over time down the wash. These slopes are erosive during precipitation events, but are armored against the wind by gravel.LVAL <Toeslope of two small hills converge on a wide flat, the soil is very deep. The flat supports ATRCAN while the slopes support EPHTOR. There is quite a bit of wind erosion and SALTRA is common.Toeslopes with rock fall boulders from adjacent cliffs. Slope dissected by rills and gullies, some to 2 m. wide. Most vegetation is rooted on fans between the channels. The fans are covered with a veneer of gravel.Small opening within P-J stands, the soils are more alkaline that the surrounding. The soil is armored by volcanic rocks and gravel helping to curb erosion. The area is heavily tracked by cattle and elk.N-facing ridge supports a woodland stand on slopes covered by volcanic rock. There is a lot of downed wood probably due to a historic fire. Runoff rapid, but erosion is limited by the rock veneer. Little understory is present.South-facing slope covered by basalt boulders and gravel. Several PINEDU trees are dead, likely due to drought. There is recruitment for both P and J trees. These trees are stunted. Because of the boulder mulch, these slopes are eroding very little.Site is grazed with signs of recent livestock use. OPUERI is quite dense in some areas. The surface of the ground is mounded with most shrubs growing from them. Barren areas in between are wind eroded. An old road is in the eastern portion of the site, but it has not been used in some years.Mildly sloping area of Entrada mounds and outwash materials. The site is actively eroding with many small hills and gullies. There are many volcanic boulders here, but less gravel than at other sites. Soils are expansive, cracks to 1.5 cm wide and encrusted with salt in drainages.Area of low ridges and hills that have various amounts of volcanic rock present. The slopes are highly eroded with many hills and gullies--lower slopes and swales are salt-encrusted. Soils are expansive with some cracks up to 1.5 cm -- 2 cm wide.@LVAL  nh~fDeep soils that are mildly mounded where shrubs are rooted. There is fair biotic crust development. Cattle have recently grazed the area.Deep alluvium comprising the second and third terraces of this large wash. Shrubs occupy hummocks that are up to one meter tall. Area has been recently grazed by livestock.Steep shale slope with fans of material and gullies along its face. Very rapid runoff on this platy surface.Site is an allluvial fan heavily encrusted with biotic crust. The surface is hard- only minor rills have formed.Broad wash that has recently flooded and is being grazed by cattle. This site occupies the broad first terrace and has some ERINAU. Unflooded second terrace occupies about 30 percent of the site and has deep soil with biotic crust.This very broad wash has four zones. One devoid of vegetation (channel), 2) ERINAU, 3) ATRCON and 4) SARVEM. They occur on each successive terrace. The soils are deep and unfolded on the ATRCON terrace, but have been flooded recently on the ERINAU terrace.Area of alluvium deposited from mesa top- fairly deep. It is stabilized by vegetation and biotic crust so there is little erosion. Only a few shrubs persist.toeslope at the base of a 25 meter high slope, that has a veneer of volcanic rock and gravel. There are some patches of Biotic crust development. The area is sparsely vegetated and subject to rill and gully erosion. Soils are absent or shallow.Area with small dunes to one meter tall and barren flats with a veneer of volcanic gravel. There is some gullying with channels to two meters wide.Area of ledging sandstone bedrock that has rockfall and a layer of volcanic rocks in addition to pockets of soil. Sparsely vegetated site.Low, small hill that is well vegetated. Soils are very deep and support a good amount of small mammal activity.Relatively flat plain with one small drainage to the west. Very evenly vegetated and good biotic crust formation. There is a good veneer of gravel on the surface. bf h  f XIU\=>14255High SlopeGPSX@Eolian Sands0500500P0000000000fdb`^\ZXVTRPPNLHFB4(#<=RollingVariableHigh LevelGPS@Moenkopi Formation040000PP00500P0000{ywusqomigecca_][WC72&;<4106High LevelGPS@Moenkopi Formation0700003Dark cyanoP00T00T0000vtrpnljhfdb`TPNLJF2&!:;240High LevelGPS@Moenkopi Formation020001-bCryptos03T00400P0000wusqomkieca]TOMKIE1% 9:VariableVariableMidslopeGPSd@ Navajo SandstoneP031-a01-bMoss, cryptobiotic crust03P0P00P0000gb`[WUC72(890N/ALow levelGPS@Blue Gate Shale Member of the Mancos Shale0300005WaterP00000T0000~|zxvtrkgeca]1% 78 12252Low slopeGPS@Blue Gate Shale Member of the Mancos Shale080000P001-b0000000~|zxvqomkkigec_3'"67VariableVariableToeslopeGPS@@Entrada Sandstone0403001-aCryptosPT00200T0000~|zvtrpgb`^ZVC72(56478High LevelGPS@Old Alluvium0400001-bP0040000000fdb`^\ZXTRPKKIGEC?1% 45VariableVariableInterfluveGPS@Moenkopi Formation03T000T0200300T0000}{ywusqmkgeeca_]YE94(344183High LevelGPSZ@Alluvial deposits0200006Biotic crust1-b00000T0000zxvtrpnljhfaSOMKIE2&!237192Low LevelGPS@Alluvial deposits07000PBiotic crust02000001-a0000ywusqljhfdb^PNLJHD1% 122175Low LevelGPSf@Alluvial deposits050001-bBiotic crustPT00300T0000ywusqomkgecaSNLJHD1% 01182Low LevelGPS@Alluvial deposits0800001-b000001-a0000kigec^\ZXVTOOMKIGC0$/0163Low LevelGPS@ Alluvial deposits080001-bbiotic crust1-a00000P0000ywusqomkige`RMKIGC0$./183Low LevelGPS\@ Alluvial deposits080001-bBiotic crust1-b000001-a0000|zxvtomkige`RMKIGC0$-.2591MidslopeGPS@ Entrada Sandstone1-b0000T0400500T0000kigeca_]YWSQQOMKID1% ,-2351Low LevelGPS@Alluvial deposits0300003Biotic crustPP00300P0000xvtrpnljfdb`RNLJHD1% +,168Low LevelGPS@Alluvial deposits080001-bBiotic crust1-b00000P0000ywusqomkige`RMKIGC0$*+172Low LevelGPS@Alluvial deposits090000TT0P00P0000eca_][YWUSQOOMKIGC0$)*p6281Low LevelGPS>@Entrada Sandstone0200005Biotic crust0200T00P0000xvtrpnljhfd`RNLJHD1% ()8279Low LevelGPS@Entrada Sandstone021-a0002Biotic crustT0300300T0000}{ywusqokiecUQOMHD1% '(419High LevelGPS(@Entrada Sandstone07T000PP00200T0000hfdb`^\ZVTRPPNLJHD1% FLVAL B  hPlot captures both S & N sloping sides of this wash; the N-facing side is mostly new alluvium stabilized with moss & cryptos and carpeted w/oak & pine needle litter; the S-facing side is predominantly exposed Navajo bedrock. Small wash channel (~1m wide x 1/2m deep) sandy with some accumulations of rock.Heavy clay soils. Heavy grazing in plot area. Lots of dieback on the TAMCHI which appear to be invading the ATRCAN shrubland.Heavily grazed, disturbed site full of weedy annuals and few shrubs. Soils are deep and extremely clayey, with hoof prints and cow pies everywhere! 3/4 of plot occurs on west-facing slope, but flattens out at the top (E side) and bottom (W side).Polygon appears to capture mostly slickrock outcrops of the Entrada formation with shallow, aeolian soils on top characterized by sparse P-J cover and COLRAM and FRAANO dominant shrubs. Just west of the polygon are deeper soils of the toeslope hills at the base of the Oyster Shell Reef.On top of Johnson Mesa where soil is old alluvium with volcanic boulders and covered with small rocks.Denser, more herbaceous community a reflection of north-facing slope with more mesic conditions. Plot is on more of an old alluvium slope covered with volcanic, basalt boulders, while polygon is more of a badlands type, also covered with basalt boulders.This site is mounded with deflation basins between. There is a high cover of biotic crust that has nearly halted erosion. Lot of OPUERI, probably due to livestock grazing.The site lies on dunes to 4 meters tall, that are wind-eroded. Excellent small mammal habitat.Large bend in the wash where water energy lessens and gravel is deposited. The point has quite a lot of gravel on the terrace, second terrace. This location was flooded earlier.Site is a terrace between two main channels of the wash - it would be an island if water were flowing. Spring flooding flowed over the site, depositing additional sediment. It is highly disturbed with a mix of vegetation.LVAL8 \ dtBxThis Chinle shale slope is nearly completely covered by Wingate talus, ranging in size from pebbles to Univac.Plot encompasses channel and parts of 2 point bar/terrace sets on opposite sides of the channel.Big piles of eolian sands in the canyon bottom.Big piles of sand in every "point bar" of this canyon.Substrate is a silty sand with cracking.Substrate is sticky clay, derived from Carmel shales.Vegetation rooted in joints in the slickrock, except for the rare potholes where sand collects. 85% of the plot is slickrock. Trees are mostly stunted from growing in cracks/shallow soils.COLRAM/PLEJAM occupies ridge. ATRCON occupies swale to N, also adjacent polygon to E. Plot is located on a low ridge on the valley floor, supported by Entrada sandstone outcrop on W side.Red Carmel sandstone makes plates on top of red Carmel Shale.PW comments: Limey sandstone pebble layer on clay, often gypsiferous soils. AT comments: A sloping mesa top (to the E) with badland hills and depressions covered in small, flat, white shaley rocks and loamy soils that are somewhat stabilized by cryptos. Depression areas have higher shrub densities and diversities, but overall the whole polygon has a high mixture of shrubs.Very active dunes - sand ripples everywhere!Soft, fairly sandy soils with lots of small rocks on the surface (soil color is a red-brown). Some P-J recruitment. Very sparse cover of weedy annual. Plot includes 2 shallow, fairly wide (~2m) drainages with the CHRNAU in and along these drainageways.PINEDU looks attacked by something (Bark beetle?). Road runs across S margin of plot (cover included in bare soil). The few, large MAHFRE captured by plot appear to be anomalous in the polygon.Soil surface covered in small rocks with pockets of well-developed cryptos and quite a bit of dead wood lying around. Understory is very sparse here, more litter than understory by far! Trees show some signs of drought-stress.5W~ G = Jh(7Ns]Yy16338High SlopeGPSRocky soil here.Salt Wash Sandstone Member of the Morrison Formation02P000021-a00500P0000|F(#\X 1011High SlopeGPS@ Carmel Formation02000004P00200P0000kigeca_]YWUQQOMKIE3'"[W 25113MidslopeGPS@ Carmel Formation03P0001-b1-b00300P0000nljhfdb`\ZUPPNLJHD2&!ZV1051ToeslopeGPS@ Obscured by Soil0600001-a1-a01-b0000000nljhfdb`[YTOOMKIGC1% YU614High SlopeGPS@ Carmel Formation1b00004crypto1b000400T0000sqomkigea_]YQMKIGC1% XTZ 4114Low levelGPS*@Navajo Sandstone0400002cryptos0300P00T0000rpnljhfdb`^ZQMKIGC1% WS 5128High SlopeGPS$@Boulder deposits00000040300001b0000jhfdb^\ZXVRNNLJHFD2&!VRS0n/alow slopeGPS@Obscured by Soil070000030000000000geca_][YWUSOOMKIGC1% UQ 13138High SlopeGPS<@Boulder depositsP000006020P001-a0000mkige`^\ZXTPPNLJHF4(#SO0n/aHigh LevelGPS@Obscured by Soil060000400T00P0000fdb`^\ZXVTRNNLJHHD2&!RN10209High SlopeGPSd@Eolian Sands1-b00800P0000000000geca_][YWUSQQOMIGB4(#OMvariablevariableLowslopeGPSV@Eolian Sands080000PP0P00T0000sqomkigeca_]][YWUQC72(NLvariable85Step In SlopeGPS@Navajo Sandstone041-b000P0301-b00T0000~|zxvtrpkiecca_]XTB61"MK28340MidslopeGPS@ Chinle Formation1-aT000P0700300T0000kigeca_]YWSQQOMKID2&!LJn1226Low LevelGPS@Obscured by Soil0600001-b00T0000000hfdb`^\ZXVTOOMKIGC1% KIvariablevariableLowslopeGPS@ New Alluvium0302020002P01-b00T0000|zxvtrpnigeaa_]YUQC72(JHvariablevariableLow LevelGPS^@ Eolian Sands020P004crypto crust0200T00T0000~|zxvtrn`\ZXVRD83(IG3186Low LevelGPSl@ Eolian Sands05002001-b00000T0000fdb`^\ZXVTRMMKIEC?1% GE0n/aLow LevelGPSP@ New Alluvium0600000200T0000000ca_][YWUSQOKKIGEC?1% FD0n/aLow LevelGPSj@Obscured by Soil0500001-b00000T0000hfdb`^\ZXVTOOMKIGC1% EC1492MidslopeGPSx@Navajo SandstoneP08000P00T00T0000eca_][YWUSQOOMKIEC1% DB4220InterfluveGPSv@Entrada Sandstone06P0001-b00T0000000jhfdb`^\ZXVQQOMKIE2&!CA8115LowslopeGPSz@Carmel Shale1-bP0001-a0200600T0000hfdb`^\ZVTPKKIGEC>0$>@c560MidslopeGPS@Carmel Formation1-b00002CryptosP0200600T0000sqomkigea_[YPLJHFA/#.LVALd 6  P ,ZN@ZSmall hills with broad, flat plains to the south. Volcanic boulder deposits and small rock chunks cover the ground.Rolling terrace 3-6m above wash level; FRAANO & RHUTRI & PJ along edge of wash. Higher terrace more of an EPHTOR/Stipa spp. Shrubland.The mostly clay soil has many small flat white rocks along with a sprinkling of volcanic stones.This is a steep-sided , ledgey canyon. The clay soil is mostly covered with small flat rocks.Entrada-derived soils with many small white rocks and larger black volcanic rocks. Plot is at the base of a hill with a broad valley to the east (part of polygon) and a deep wash channel to the west.A less steep Carmel mesa that has less steep hills throughout mesatop and wash. Soil has a lot of great crypto crust and lichens and small rocks. There is large empty area near centroid without trees or shrubs.Plot is on a small plateau between wash of Deep Creek and the drainage of a side canyon. Lots of cryptos here and grassier than most of the polygon.This hill is directly at the bottom of the steep large hill that forms the Upper Deep Creek drainage. Lots of large volcanic boulders and litter.A few drainages run through the polygon; one minor one runs through plot.Rolling terrain at the edge of a steep hill which leads down to Deep Creek - slope and aspect vary somewhat here - that given is for the majority of the plot.An old 2-track runs though plot. Soil is deep, sandy. A few dead pines scattered around.Very duney area- active shifting sands everywhere.Plot is a series of gullies and ridges in soft Carmel mixed with Entrada sands. The junipers and oak are concentrated in the gullies, the COLRAM and Ephedra on the ridges.COLRAM where sands are deeper. PJ and other shrubs where bedrock is shallow and there are cracks to root in.This belt of ATRCAN runs N-S closest to the eastern valley escarpment. To SW of point is a large area of EPHVIR/ACHHYM-STICOM (different polygon). Substrate is sandy but only rudimentary crypto development.LVAL X D HRMost of the doug fir have succumbed to mistletoe. A large opening in the plot has significant crust development. Where litter isn't covering it, the soil surface is covered with white, shaley rocks.The ground is covered completely by small, white, platey rocks. Point is on a hillside off of the main southern ridge of Bulberry Canyon. Some dead standing and downed trees.Plot is at base of a small side canyon of Deep Creek. Plot slopes up both sides of this side canyon, so slope/aspect vary.Very rocky soils, flakey rock. Plot is transected by several shallow gullies, and shrubs are concentrated there.Steep, rocky, sandy soils. Canyon side in this area is regularly transected by shallow, steep gullies, where serviceberry is concentrated, whereas Cercocarpus is on ribs between gullies.Lots of 1/2 - 1 meter across black volcanic boulders scattered around. Good crypto development in a few open soil pockets.Boulder-laden hillside, most half-buried, with some minor crust development and scattered green tufts of BOUGRA. Very pretty!Dune-like toe-slope hills beneath a steep North facing, rocky slope to the south and above the four to eight meter deep Deep Creek wash to the north. A diverse mix of an understory.Plot is on an interfluve between Deep Creek and one of it's tributaries so slope and aspect vary-thin soils with lots of bedrock exposures here.This point is on a hill that is west of the hillside with point AA0703. It has black volcanic boulder deposits throughout and small white rocks and litter filling in between. There is a wash between the two hillsides with Navajo rock exposed and black boulders on top.There are a few dead sagebrush here. P-J is invading.This point is on north side of Upper Deep Creek and is fairly flat but does have some rolling hills. There are Navajo cliffs to west and north of point. Navajo bedrock, volcanic boulders and litter are on soil.LVAL r * ~rF4~bSandy soil is probably derived from the EntradaAgain, dark volcanic boulder deposits in soil and there are gravel sized black rocks as well (not small white rocks as elsewhere around here).The surface has many large boulders and pebbles.Steep, flakey rock soils, eroding downhill.Large black volcanic boulders throughout with smaller white and grey rocks and litter and wood make up rest of cover. Some snags around.Rolling terrain on this bank above Deep Creek, so slope and aspect vary. Lots of PINPON needles everywhere.Colluvial slope with large volcanic rocks.Point is down on mesa/hill by a main drainage PSEMEN moving in from wash/drainage.This point is on top of a mesa that is east of Bulberry Creek. The mesa is bisected by washes and forms hills and flat areas. Many smaller yearling PINEDU about 1 to 3 feet tall.Erosion runnels and black boulders punctuate the low Entrada hillsMany small white and brown rocks throughout soil, litter under trees and shrubs. Point overlooking Navajo cliffs forming canyon sides of drainages.Flat area near base of Navajo cliff with many small, white rocks.On Entrada hills made up of soil-like, partially eroded bedrock, forming spires and domes. Much of the polygon covered with baseball to head-size volcanic boulders and smaller rock chunks. BLM survey rod/point in plot center.Plot is on a relatively flat interfluve area. ARTTRI only occurs where edge of plot moves onto a steep S-facing edge of interfluve. Lots of the PINPON are young.Plot includes a minor tributary wash channel to Deep Creek, but vegetation isn't impacted by it - except that Cercocarpus ledifolius may be moving down the drainage floor from steep south-facing hillsides to the northwest of polygon.The surface is covered with flat, white rocks.Plot encompasses a narrow E_W ridge with steep slopes to the North and South. The northern aspect has more vegetation than the south aspect.v] < K < NTWR 12235High SlopeGPS@ Boulder deposits0000007030000T0000jhfdb`^\ZXTPPNLJHF4(#1015MidslopeGPS@Carmel Formation1-a00001-aP00700T0000kigeca_]YWUPPNLJHC1% w2097High SlopeGPSP@Salt Wash Sandstone Member of the Morrison FormationP00001-a0500400T0000~|xssqomki3'"0n/aLow levelGPS@Obscured by Soil0800001-a00000T0000hfdb`^\ZXVTOOMKIGC1% 330High LevelGPS!Many pebbles decorate the soil.Obscured by Soil0300000500P00T0000~|zxvtppnljhdR% 518High SlopeGPS~@Carmel FormationT0000T1a00900T0000geca_][YUSOMMKIGEC1%  8328High SlopeGPS@Carmel Formation1a00001a0008001a0000ljhfd`^\XVTPPNLJHD2&!m17307LowslopeGPS@Colluvial depositsPP00TBiocrustT0200700T0000trpnljhfb`\ZPNLJHF2&!)variablevariableInterfluveGPSF@Carmel Formation03P0001-aT00500T0000~|zxvtrpljhcca_][WE94(~ 252MidslopeGPS@Boulder depositsT0000081-b0T00P0000fdb`^\ZXVTOKKIGECA/#}. 1890MidslopeGPSr@Extrusive volcanics1-a0000051-a003001-a0000sqomkfdb^\WSSQOMKF1% |3145Low levelGPS^@New Alluvium05000004T0T0000000ca_][YWUSQOKKIGEC?1% {Y2180High SlopeGPS@Boulder deposits1a000Tcrypto1a03005001a0000vtrpnjhfb`\XPNLJHD2&!~z1723MidslopeGPS`@volcanic boulders020000031-a00300P0000mkigeca_[YTPPNLJHD1% }y 1046High SlopeGPSVery rocky soilsCarmel Formation0400001-bP00400P0000~|zxvtrpljhcca_][WE'"|x27142MidslopeGPSSteep, flaky rock soils.Carmel Formation05P000PP00400T0000~|zxvtpnljjhfdb^L&!{w332High LevelGPSPebbly soil surface.volcanic02000005T0030000000wusqomkieca]][YWUQG% zv25150MidslopeGPSV@ Carmel Formation04P000PP00500T0000hfdb`^\ZVTRPPNLJHD2&!yuM20182High SlopeGPS@ Boulder deposits1a00000202003001a0000pnljhdb`\ZVRRPNLJF4(#xtH variesvariesLow levelGPS@ Obscured by Soil02000Pcrypto06P0T00P0000|zxvtrpnljhd\ZXVTP>2-"wsD28354MidslopeGPST@ Carmel Formation040000021-b00300P0000mkigeca_[YTPPNLJHD2&!vr15228ToeslopeGPSHot, dry spot.Salt Wash Sandstone Member of the Morrison Formation05000P0050000000~||zv@$uq056High SlopeGPS@ Carmel Formation1a1a0001a0008001a0000mkigea_]YWUQQOMKGC1% *LVALB & 2jlZLots of black volcanic boulders and small white rocks and litter on a steep slope that leads to a dry wash opposite a large Navajo cliff.Fairly steep slope below Carmel cliffy outcrops volcanic boulders and small bedrock flakes cover the ground. A volcanic intrusion juts out of cliff band in plot area. Wash to the S lined with FRAANO, CHRNAU, RHUTRI.Stand is multi-aged, with some very old bristlecone pines. Large volcanic rocks are embedded in gravelly soil.Plot landed on the edge of some steep, deep gullies. Upslope on flatter ground vegetation is probably slightly denser, but similar.Millions of chert chips litter the surface. There are numerous bedrock exposures.This wash probably never flows more than a few inches since there is biocrust growing above that.The clay soil is sprinkled with pebbles.Boulders throughout soil layer and litter on top. Heavier PJ in subcanopy than the canopy cover of PINPON PSEMEN.Ground is covered with white rocks / gravel - some of them 10cm or larger.Slope covered in head-sized volcanic boulders and smaller rock chunks. Juniper dwarfed to less than 2 meters tall. A mixed shrub understory with moderate grass cover.Fairly flat area in the bottom of South Desert Valley. Horse packing trail about 30m south (through plot) and volcanic boulder covered hills of Entrada sandstone to the east. About 60m. No crypto development.On the same hillside as last two points in polygon but near a small wash that abuts a red Carmel small ridge. Ground covered with small white rocks. Vegetation sparse except PJ AND SHEROT.Soil covered by small light brown rocks and some medium sized rocks. On a hillslope off of main ridge on south side of Bulberry Canyon.This slope has elements of salt wash Morrison and Curtis mixed-togetherFlat white rocks cover the surface.Steep hillside with lots of litter over basalt boulders. A mix of tree ages and sizes here. Significant amounts of dead doug fir.Round rocks and small pebbles lie beneath the duff layer.*b L A % nLg N f0n/aHigh LevelGPS@ Extrusive volcanics03000004T00300T0000mkigeca_[YWSSQOMKG2&!21126High SlopeGPSr@ Boulder depositsPP0001-b0400400P0000mkigeca_[YUPPNLJHF4(#495High LevelGPSl@ Extrusive volcanics03000004P00300T0000ljhfdb`^ZXVRRPNLJF1% u variablevariableLow levelGPSR@ Navajo Sandstone0200002Crypto03P00200P0000~|zxtrpld`^\ZVD83( 11172MidslopeGPS@ Boulder deposits0000007030000P0000hfdb`^\ZXVRNNLJHFD2&!6858ToeslopeGPS@Salt Wash Sandstone Member of the Morrison Formation050000P00050000000}{wusqqomkie/#variablevariableLow levelGPS @Obscured by Soil080000PP0P0000000xvtrpnljhfdbb`^\ZVD83(8320High SlopeGPSZ@Carmel FormationT0000T1-b0090000000igeca_][WUPNNLJHFD2&!b280Low LevelGPSV@New Alluvium070000030000000000b`^\ZXVTRPNJJHFDB>0$U 33180MidslopeGPS@Boulder deposits05P0001-b030P00P0000kigeca_][YUPPNLJHD2&!variablevariableLowslopeGPS@Salt Wash Sandstone Member of the Morrison Formation06P00002T00200P0000}yC72(0n/aHigh LevelGPSr@Eolian deposits02002002Cryptos02000001b0000vtrpnjhfdb`\SOMIGC2&!P8160High SlopeGPS@Boulder deposits00001-bCrypto, mosses1-b03006001-b0000}{ytrpljfaQLJHFD2&!330High LevelGPS"The soil is clayey with pebbles.Obscured by Soil0300000500P00T0000}{ywuqqomkieS% n 14190High slopeGPS@Navajo Sandstone1-b00002dark cyano1-b0200300P0000~|zxvtrpljfaUQOMKF4(#30228High SlopeGPS@Boulder deposits01-a0001-a04005001-a0000sqomkfdb^\XSSQOMHF4(#16145Low slopeGPS@Carmel Formation0302000P1-a0040000000nljhfdb`\ZUSSQOMIE3'" 5140Step In SlopeGPS@Carmel Formation1-a0000051-a00300P0000qomkigec_]XTTRPNLG5)$i variable26High SlopeGPS@ Carmel Formation0200002biotic soil1-b1-a00400T0000~|xvql_[YWUQ?3." 8102MidslopeGPSRocky soils.Carmel Formation04000002P00300P0000vtrpnljhdb`\\ZXVTP>$296High LevelGPS@ Salt Wash Sandstone Member of the Morrison Formation05P00002T00200P0000{ywssqomkg1% 3187Low levelGPS@ Curtis Formation05T00PbiocrustTP00400T0000qomkigec_][YOMKIGC1% z0n/aHigh LevelGPSP@ Obscured by Soil0600000300P00T0000hfdb`^\ZXVTPPNLJHD2&!2LVAL4^ < 2LV&HbThis point is near eastern edge of a large mesa close to Deep Creek. The Carmel soil has a lot of crypto crust with lichens and small white rocks throughout.Large black volcanic boulders throughout.This is a rocky slope with much tree litter.Small volcanic pebbles litter soil surface. Desiccation is evident from drought on about 1/3 of the sagebrush.Rocky slope, mix of large boulders and small rock chunks.Soil is very rocky. A narrow gully runs through the plot but has no impact on the vegetation. A more major gully also runs through plot and has some large trees associated with it.Plot straddles a small wash (which now has flowing water after yesterday's storm) and covers both steep banks, so slope and aspect vary. Lots of flat Navajo rocks here.Bouldery slope, some mostly buried, others on the surface. Ground covered in thick litter, where there are fewer boulders.These toeslope areas of polygon have more species diversity and denser veg than the lower, flatter areas downslope.Rolling hills of soil derived from the Entrada formation. A small drainage bisects the plot. A few volcanic rocks scattered around.Many small platey rocks and some larger ones.The soil is drying into geometric patterns.Plot includes south facing slope with volcanic boulder deposits, as well as flatter high slope with some Navajo bedrock exposures and shallow bare soil on top. South boundary of polygon is Deep Creek, lined with Cornus sericea and Rosa woodsii.This plot has an anomalous area of white shaley dirt which supports several annuals and the shadscale. Most of the plot has gravelly soil.Flat area near Navajo cliff with deep, light, sandy soil.This point has large black volcanic boulders throughout and small white rocks, litter, and moss in between.Some pinyon in plot are pretty dwarfed. High rock cover with some crust development. No ponderosa in plot, but just outside plot there are. The Cercocarpus intricatus looks like it might be a hybrid with Cercocarpus ledifolius.Qb g B ^  ^km.# 14155MidslopeGPSp@Carmel Formation02000004P004001-a0000mkige`^\XVTPPNLJHD2&!%10174High SlopeGPS@Boulder deposits0300001-a0200300T0000omkigeca][WRRPNLJF4(#A variablevariableLow levelGPS@Navajo SandstoneP06P001-b1-b01-a00T0000}{ywusnlgbb`^\XVD83(ovariablevariableMidslopeGPSv@Salt Wash Sandstone Member of the Morrison Formation02P001-acryptos020200300T0000}yC72(3360High LevelGPSV@Extrusive volcanics03000003T00300P0000mkigeca_[YWSSQOMKG2&!1415Step in slopeGPS@ Carmel Formation03P00003P00300P0000nljhfdb`\ZXTTRPNLH6*%variablevariableLow levelGPS@ Entrada Sandstone0503000T1-a01-b0000000}{ywusnlgeeca_[WD83(variablevariableMidslopeGPS@ Entrada Sandstone03P000P030040000000|zxvtrpnjhdbb`^\ZVC72( 28333MidslopeGPS@ Boulder depositsP000006020P001-a0000kigec^\ZXVRNNLJHFD2&!+1230High SlopeGPS@Carmel FormationT0000T1-a00900T0000jhfdb`^\XVQOOMKIGE3'"p13204High SlopeGPS@Salt Wash Sandstone Member of the Morrison FormationP08000PT0P00T0000~|zxvvtrplj4(#Z 7154Low levelGPSR@Navajo Sandstone1-b0001-acryptos04P00200P0000vtrpnljhdb`\SNLJHC1% 5variablevariableLow slopeGPSl@Navajo Sandstone1-b05P01-aBiotic soil1-a1-a0T00T0000zuhca_[VD83(535Low levelGPS@Salt Wash Sandstone Member of the Morrison Formation030T004CryptosPT00200T0000}tpnljf0$evariablevariableHigh LevelGPS2@Salt Wash Sandstone Member of the Morrison Formation1-a1-b00Pcryptos02T00500T0000{E94( 554High SlopeGPS6@Boulder depositsT000006020T00020000igeca][YWUQMMKIGEC1% 5280High SlopeGPSRocky, gravelly soil.Salt Wash Sandstone Member of the Morrison Formation040001-abiocrust02T00300P0000I&!40n/aLow levelGPS@Alluvial depositsT00500T00050000000hfdb`^\ZVTRPPNLHFD1%  127High SlopeGPSL@Carmel Formation03000003P005001-a0000ljhfd_][WUSOOMKIGC1% 1020High SlopeGPS<@Carmel FormationTT0002CryptoT000800T0000qomkigec_][YQMKIGE3'"w6195High SlopeGPSR@Boulder deposits1-b0001-bcrypto1-b03003001-b0000|zxvtomkgea\TOMKID2&! 27149MidslopeGPSX@Boulder deposits03000005P0P00T0000hfdb`^\ZXVTPPNLJHD2&!LVAL   R:fThere's a cliff just below the plot and a steeper slope above making this a large, rock and soil filled ledge.Area is full of low, rolling Entrada hills w/scattered volcanic rocks and drainages braiding throughout. Plot falls in an especially barren area, with the center on top of an Entrada pinnacle.A depression on the side of Entrada hills with slopes coming into it from all directions all with several drainage courses running down their face. Many volcanic boulders and rock chunks on the ground.Lots of large, lichen covered boulders (1/2 - 1m across) firmly embedded in the steep slope.Tons of small white rocks on top of soil some weird volcanic, black boulders and some dead and down. Very very little herbaceous, just seedling shrubs. Ground is mostly platey small white rocks.The terrain is mostly exposed bedrock consisting of coarse sandstone and gravel conglomerate. The plants are growing in cracks in the rock.Plot sits atop a small rise between two drainages that lead into Deep Creek. Slope and aspect are for the overall area- not the slopes of the plot toward each drainage.Plot includes a shallow, sandy wash channel with slabby bedrock on one side and aeolian soils on the other. Some basalt boulders are present, but they're in a matrix of white sands.Rolling lowland surrounded by Salt Wash hills with some ledgey bedrock exposures. Small sandy drainage channel runs through plot. Soil crusts consistent throughout plot area and well-developed.Lots of chunky bedrock exposures and gravelly small rocks. Some well-developed cryptos in soil pockets. Rolling terrain with variable slope and aspect.There are medium sized reddish boulders on soil that is mostly covered with litter and some medium sized rocks. There are dead and downed trees and snags.Point on wash which does not have an elevated bank. Deep sandy soil with some small rocks.Small rocks are covering soil surface.LVAL 4 ~ *zJRolling low hills of soil derived from Entrada formation. Many small drainages bisecting the area, and some crypto development.Pretty flat broad floodplain terrace covered consistently with SPOAIR and dotted with a mixture of shrubs. Small rocks scattered on the soil surface.There's a little dieback on the shrubs here.Point on a hillside that makes up mesa east of Bulberry Creek. Mesa has many washes throughout. Soil is light brown with crypto and small white rocks.Slightly sloping ridgetop. PJ are a little stunted, due to shallow soils maybe. Lots of half- buried, large volcanic boulders scattered around. Huge drop- off to Deep Creek just outside plot to the North and East.Plot area along narrow, north edge of creek and up onto some Navajo bedrock ledges that are sparsely vegetated. Lots of boulders in and along creek, making small pools and tiny waterfalls.This point is in hillside off a small drainage on the mesatop east of Bulberry Creek. There are larger platey flat rocks as well as small white rocks and crypto crust.The sagebrush is restricted to the minor drainage which runs through plot. Two large areas dominated by halogeton may once have been prairie dog towns, but now there are some large anthills there.Small rocks on soil surface. Mistletoe on the doug fir.A little more soil compared to boulders in this relatively level area of polygon.Large ravine (6 to 10 meters deep) runs through center of plot with some small cliffy bedrock exposures on the sides, and small rocks to large boulders along its course. CERINT next to the wash are very large.Gently rolling, rocky hills with many small drainages bisecting the area. Quite a few black basketball-sized volcanic rocks around. A few exposures of grey conglomerate looking bedrock.A few dead juniper trees around, very long dead. Some drought stress (dead branches) in sagebrush and a few dead individuals. Small volcanic pebbles are on soil surface.)eG R  k  cz4Eg:1529High SlopeGPS@ Carmel FormationT0000T1-a00900T0000jhfdb`^\XVQOOMKIGE3'" 1058MidslopeGPS@ Boulder depositsT0000081-a0T00P0000hfdb`^\ZXVQMMKIGEC1% 2890MidslopeGPS@ Boulder deposits0400001-aP00400T0000jhfdb`^\XVTOOMKIGC1% ^3335High SlopeGPS@ Boulder deposits0300003Crypto1-b0200001-b0000xvtrpkigec_ZRNLJHD2&!0n/aLow levelGPSF@ New Alluvium0700003BiocrustTT0T0000000mkigeca_][YWMIGEC?1% ^290Low LevelGPS@Obscured by Soil06000002P00200T0000hfdb`^\ZVTRNNLJHFB0$<22200High SlopeGPSL@Boulder depositsT0000T0500500T0000jhfdb`^\XVRPPNLJHF4(#23206High SlopeGPS@Boulder deposits1-a00001-b0400400T0000pnljhfdb^\XSSQOMKF4(# 1093High SlopeGPS@Boulder deposits1-a000005030T00P0000ljhfdb`^\ZVRRPNLJE3'"24184MidslopeGPS@Boulder depositsP0000030300300P0000jhfdb`^\XVRNNLJHFD2&!E0n/aLow LevelGPS@Obscured by Soil08000Pbiocrust020000000000qomkigeca_]YOMKIGC1% 3344High SlopeGPSX@Boulder deposits021-a0001-a0300400T0000qomkigec_]YTTRPNIE3'"^ rollingvariableMidslopeGPS@Navajo SandstoneP1-b001-aCryptos03P004001-a0000|zxtrplc^\ZUSA50& 0n/aHigh LevelGPS$@Boulder deposits040000020200200P0000ljhfdb`^ZXTPPNLJHD2&!variablevariableLow levelGPS@ Obscured by Soil080000PP01-a0000000{ywusqomhfdbb`^\ZVD83(297Low levelGPS,@ New Alluvium080000P00020000000b`^\ZXVTPNLJJHFDB>0$0n/aHigh LevelGPSX@ Obscured by Soil0300000500P00T0000hfdb`^\ZXVTPPNLJHD2&!652High SlopeGPS0@ Carmel FormationT00004crypto02000400T0000qomkigec_][WOKIGEC1% 5129High LevelGPS@Boulder deposits020000030300200P0000ljhfdb`^ZXTPPNLJHD2&!i 0n/aLow levelGPSz@Navajo Sandstone1-a03T0PWater03020P001-a0000vtrpnigeca]YRPNLHC1% |0n/aHigh LevelGPSThe shrubs have some dieback.Obscured by Soil0400000400P00T0000}{ywusoomkigcQ&!12100High SlopeGPSVery rocky soils.Carmel Formation030000020200300T0000}{ywusomieeca_]YG(#26126High SlopeGPSP@Carmel FormationT00002CryptoT0500300T0000trpnljhfb`\ZRNLJHF4(#80n/aLow LevelGPS@Obscured by Soil060000400P0000000eca_][YWUSQMMMKIGC1%  LVAL f  f Zf8NVery steep, boulder-covered slope- most half-buried. Ground between boulders carpeted in thick needle litter. Quite a few fallen snags. PSEMEN young here.Hard to know what to put for geology because hills are partially stabilized aeolian dunes with scattered volcanic boulder deposits, but in the few drainage channels bisecting plot there is exposed Navajo bedrock. Also a diverse understory with nothing clearly dominant.This point is on the same hill slope as other points around here but this one is closer to bottom where there is much more gullying. Volcanic boulders and dikes of black rock. Less than 1% herbaceous.Rocky soils with basalt boulders. Purshia is mostly in open areas of canopy.This is a steep-sided gully cutting through the coarse volcanic substrate.Black volcanic boulders throughout and crypto and deep sandy soil and litter otherwise.Clay and sand mix in this alluvium.A gullied area runs through the south part of plot. The rabbitbrush is restricted to that area.There are large, black volcanic boulder deposits throughout hillside east of Paradise Flats. Small light colored rocks in between boulders, some dead standing snags.Plot is on a ridge of large basalt boulder deposits, with a gravelly matrix of soil.Melon-sized and larger, lichen-covered volcanic boulders embedded everywhere. Lots of ponderosa litter and cones.Very rocky, somewhat unstable slope just above a wash. Big rocks and boulders here are dark/volcanic.The biocrust is on small humps. The density of the grasses and the weeds is patchy.Plot encompasses the ridgetop, but much of it is on a steep north facing slope. Navajo bedrock outcrops occasionally in this area, but the basalt boulder deposits prevail.Small, rolling hills covered in small rock flakes and with some bedrock outcroppings. Vegetation denser here, but the same mixture of species.Flat ridgeline with a fairly sparse, dwarf- shrub / herbaceous understory. Fewer boulders, more than half- buried, but lots of small rock chunks.aS N  ;  T XFA@0n/aLow levelGPS@Navajo Sandstone1-a03000041-a0P00P0000mkigeca_][VRRPNLHC1% p5352LowslopeGPS@Salt Wash Sandstone Member of the Morrison Formation03T00003P00300P0000~zxvrrpnljf0$322High LevelGPSH@Obscured by Soil06000004T0P00T0000geca_][YWUSOOMKIGC1% 4 330High LevelGPS@Boulder deposits1-b0000030300200P0000ljhfdb`^ZXTPPNLJHC1% 125MidslopeGPS@Carmel Formation02P0007biocrustTT0T00T0000omkigeca_][YOKIGEA/#variablevariableLow levelGPS@Eolian deposits0400004cryptos0200000T0000~|zxvtrplc_][YUD83( 1860MidslopeGPS @Boulder deposits1-a0000030401-a001-a0000pnljhca_ZXTPPNLJHC1% 758High SlopeGPS@ Carmel Formation0200002crypto02000500T0000sqomkigea_]YQMKIGC1% n278High LevelGPSr@ Salt Wash Sandstone Member of the Morrison Formation0600001-a00030000000|zxssqomkg1% d High SlopeGPSr@ Carmel Formation1a00002crypto1a0007001a0000omkigca_[YWSKGECA=+variablevariableHigh SlopeGPS@ Carmel FormationPP0008LichensPP0P0000000~|zxvtrpnlc_][YWE94(23169MidslopeGPS@ Boulder deposits1-b0000020400200P0000mkigeca_[YUQQOMKID2&!19210MidslopeGPS@Boulder depositsP0000020601-b00P0000kigeca_]XVRNNLJHFD2&!6359Low levelGPS@New Alluvium1-a0001-bcrypto030201-b001-a0000wusqojhfa_[WOJHFD?1% 324High LevelGPSP@Obscured by Soil0600000300P00T0000geca_][YWUSOOMKIGC1% Y0n/aLow LevelGPS@Obscured by Soil08000002T0P0000000geca_][YWUSOOMKIGC1% 4164High LevelGPS@Salt Wash Sandstone Member of the Morrison Formation061-a001-abiocrust02P00200P0000zusqlh2&!6134High SlopeGPSD@volcanic boulders04000004P01-a00P0000ljhfdb`^YWUQQOMKIE2&!t 551MidslopeGPSF@Boulder deposits0000006020T00020000geca_[YWUSOKKIGECA/#2346Low slope1:24K Quad@Talus/Colluvium/Landslides03P00005P0P00T0000ywusqomkigeaa_][YU9-!variablevariableToeslopeGPSF@Eolian Sands0400005Dark cyano1-aP0T00P0000~|zxvtrpk_[YWUQC72(x 326Low slopeGPS:@Boulder deposits0000004060000P0000fdb`^\ZXVTPLLJHFDB0$8220MidslopeGPS@Eolian Sands041-a00PDark Cyano021-b0T001-a0000wusqojhfdb]YMKIGB>0$TLVAL l >Z~Gently rolling duney area which slopes off to the east and west as it hits big Navajo cliffs. Decent crypto development here.Very bouldery / rocky slope (volcanic rocks). Greenish lichens all over the rocks. Entrada sandstone exposures visible about 100 meters north.On hillside of high level mesa top that generally slopes down to north with washes throughout.Clean, homogenous community on this broad, flat mesa top.Point has small white rocks on soil and crypto crust with lichens (looks like gypsum). There are dead trees on ground and standing. Point is off ridge to the south of Bulberry Canyon.Plot center is in the bottom of a steep-sided, narrow gulley; inaccessible from hiking up the gulley and also from above (where I am). Most of the shrubs are in the bottom; nearly unvegetated up here.Fairly stable slope with lichen covered, dark volcanic rocks embedded in the soil. Plot center is about 40 meters from a wash about 8-10 meters wide. Some Entrada sandstone outcrops are visible about 60 meters east of here below the plot.Boulder-laden hillside, making slope step-like and less steep seeming. BOUGRA consistent throughout polygon.See classification comments above - Plot is mainly on south side of wash, so slope/aspect are for the majority of the plot.The clay soil is sprinkled with pebbles.The rabbit brush is restricted to the narrow wash which runs through the south side of plot.Large bedrock exposures and pebbly gravel characterize this substrate. Large volcanic rocks are scattered around.Black boulders decorate this plot.The soil is deeper sandy light- brown with heavy litter and red brown boulders and rocks throughout. Point is below a steep hill, midway down slope to Deep Creek.This steep canyon side has volcanic boulders Carmel Shale and Navajo Sandstone all mixed together.Rolling, stabilized dunes at the toeslopes of surrounding hills. PJ really petering out, transitioning to an herbaceous park-like area in the valley to the south.LVALPB h d |  h2j,Large, ramp-like exposure of Navajo bedrock in plot, resulting in the appearance of CERINT. PJ are pretty stunted due to shallow soils. Hill covered in half- buried boulders.Plot straddles a dry wash channel, but encompasses both slopes on either side. The channel itself is relatively insignificant in its impact on the vegetation.Bouldery, North facing slope with the ground totally covered in two to three inch thick pine needle/ cone litter. Lots of recruitment in plot, though most are sapling size so I lumped their cover with the mature canopy species.Plot occurs at the transition from steeper slopes to flatter at the base of a north facing hill. The aspens occur sporadically at the lowest edge of plot.Lots of dark volcanic boulders scattered around. Decent crypto development in soil pockets.Gypsiferous soils with lots of biotic cover. Lots of shallow gullying in plot.Substrate/geology is a real mix here - large volcanic boulders mixed in with Navajo sandstone chucks and small rocks.Large volcanic rocks are embedded in an otherwise shale-rocky soil surface. Mistletoe is in the doug fit.Navajo-derived sandy soils. Lots of old juniper skeletons in this area. Not as duney as AA1299, and a bit weedier.The pinyons and junipers are invading.Plot is long and narrow at the base of big Navajo sandstone cliffs. Shelves with Cercocarpus intricatus growing on slickrock in plot. Small sandy drainage channel runs through Pinyon-Juniper for the length of the plot.Plot is situated at the head of a canyon, with 2 gullies converging here. Many pebbly rocks on soil surface.A few old cut tree stumps on plot. An anomalous weedy patch about 10 square meters in one part of plot. Some drought desiccation on the sagebrush from past years.Lots of volcanic boulders and pebbles embedded in the soil. Soil too rocky for crypto development.This is some more of that gypsum soil. The terrain is highly sculpted by water erosion.xb' $ B BU(wvariablevariableLow levelGPSV@ Eolian Sands0300004Dark Cyano, Moss02000001-a0000~|zxvr`\ZXVRD83(0n/aHigh LevelGPSr@ Eolian deposits0300003crypto0300000T0000qomkigeca_]YQMKIGC2&!u11190High SlopeGPSf@ Salt Wash Sandstone Member of the Morrison Formation04T000021-a00300P0000zvvtrpnj4(# 12165High LevelGPS@ Boulder deposits1b000003050P00P0000ljhfdb`^\ZVRRPNLJF4(#250Low slopeGPS@Alluvial depositsT00600T0200200T0000igeca_][WUQOOMKGEC0$LvariablevariableHigh LevelGPS@@Salt Wash Sandstone Member of the Morrison Formation021-a001-acryptos1-b000400T0000{E94( 0n/aMidslopeGPS@Boulder depositsT000007030T00T0000fdb`^\ZXVTPLLJHFDB0$b3490MidslopeGPS@Carmel Formation021a0006lichensP1b0000T0000trpnljhfdb^\SOMKGC1%  379High LevelGPS@Boulder deposits0202000040301-a00P0000nljhfdb`[YUQQOMKGC1% <950High SlopeGPSR@volcanic boulders02000003T00400T0000jhfdb`^\XVTPPNLJHD1% 18115High SlopeGPS"@Boulder deposits1-b1-a0001-b0400300P0000sqomkigea_[VVTRPKF4(#d 0n/aHigh LevelGPSx@Carmel Formation021a0001a0200200T0000nljhfdb`\ZVRRPNLHD2&!1220High SlopeGPSH@Carmel FormationTT0009LichensP00P0000000pnljhfdb`^\ZQMKIGE3'"13156Low slopeGPS`@Boulder depositsP02001-aCryptos, Moss020401-a00P0000~|zxvtrmkgcTOMKGE3'"20variableToeslopeGPS>@ Boulder deposits0200001-b0300400T0000rpnljhfd`^ZUUSQOMI7+&k 23360Low slopeGPS@ Boulder deposits0000007020000P0000igeca_][YWSOOMKIGE3'" 1520ToeslopeGPS6@ Boulder depositsT000009P0T00P0000eca_][YWUSQMMKIGEC1% 443High LevelGPS@ Obscured by Soil1-b0001-acrypto030201-a001-a0000{ywusnljec_[SNLJHC1% + 1512MidslopeGPS@ Carmel Formation0200003Biotic soils02P00300P0000ywusqomkgec_QMKIGC1%  16219MidslopeGPS@Obscured by Soil1-a0000040300200P0000mkigeca_[YUQQOMKID2&! 1167MidslopeGPS@Carmel Formation02000004P004001-a0000ljhfd_][WUSOOMKIGC1% t162Low levelGPS@Eolian deposits070000200000P0000ca_][YWUSQOKKIGEEA0$0n/aHigh LevelGPSL@Obscured by Soil0500000400T00T0000hfdb`^\ZXVTPPNLJHD2&!(LVAL@   0HXLots of large, black, lichen-covered volcanic rocks the size of basketballs embedded in the soil. Lots of small pebbly rocks too. Soil seems too rocky for crypto development here.Many pebbly rocks on soil surface.Gently rolling area with overall slope and aspect as stated above - lots of Salt Wash bedrock exposure, and tons of conglomerate gravel breakdown. Well-developed, tall black cryptos on soil pockets.A lot more crust development here and less bedrock exposure. Also a more diverse and developed herbaceous understory.Small, rolling dunes along the base of Navajo sandstone fins. PINEDU next to cliffs are very tall! Really a diverse understory, hard to know what to call this community.This generally flat area ha some rolling hills within it.Rocky, gravelly soil. A few dead pines are around.Plot located near a small ridgeline that slopes northward to Deep Creek, and more gradually southward into a small valley. PINPON sparse on this south side. Very bouldery, mostly half- buried.The point falls next to a wash between a Navajo cliff and a park dominated by PJ/HESCOM.Lots of salt wash gravel over bedrock and some soil pockets with very well-developed black cryptos. Gently rolling small hills with varying slopes and aspects.Point in level area halfway down slope (which had steep slope above point ( to the south) toward Deep Creek) and below.Steep slope with bedrock ledges. The soil surface is covered with a hard crust; a combination of lichens and physical crust.Melon-sized and larger lichen covered rocks embedded in the soil. Lots of ponderosa litter aroundMany small volcanic rocks cover the soil.Sparse understory here. Soils obviously shallow, evidenced by Navajo bedrock exposures. Many boulders here, some very large (nearly car-sized).Large light brown boulders throughout this hilltop spur off of a mesa top. Soil is light brown with small rocks throughout. This spur is flat on top and drops off steeply on three sides.Crusty lichens are the soil surface.nDo  S  e  ;M4oVvariablevariableLow levelGPS@New AlluviumT00300P0300400T0000xvtrpnljfd`^^\ZVTRD83( 4138Step In SlopeGPSMany pebbles on soil surface.Extrusive volcanics02000004P00400P0000}{yuusqomiT)$25224MidslopeGPSj@Carmel Formation03P000P0200300T0000jhfdb`^\XVRPPNLJHD2&! -variablevariableLow levelGPS@New Alluvium01-a02001-a0500200P0000~|zxvtrpljfaa_]YTRD83( 2117High LevelGPS<@ Salt Wash Sandstone Member of the Morrison Formation0300001-aP00600T0000}{yttrpnlh2&!  variablevariableHigh SlopeGPS@ Carmel Formation00000T1-a00900T0000|zxvtrpnjhcaa_][YWE94( 14163High SlopeGPSd@ Boulder depositsP0000020601-b00P0000mkigeca_ZXTPPNLJHF4(#  0n/aHigh LevelGPSD@ Salt Wash Sandstone Member of the Morrison Formation04000003T00300P0000|zxttrpnlh2&! 548High LevelGPST@ Boulder deposits04000004P0020000000igeca_][WUSOOMKIGC1%  417High LevelGPSZ@Obscured by Soil0700000200P00P0000geca_][YWUSOOMKIGC1%  variablevariableLow LevelGPSH@Obscured by Soil04T00002P00400T0000|zxvtrpnjhfbb`^\ZVD83( m0n/aHigh SlopeGPS@Salt Wash Sandstone Member of the Morrison Formation031-b001-bBiocrust, lichens03P00200P0000zusqlh2&!90n/aLow LevelGPS@Obscured by Soil0400003Biocrust0300P0000000sqomkigeca_[QMKIGC1% <0n/aLow levelGPS@Alluvial deposits04004001-a1-a000000000nljhfdb`^\WRRPNJHD1% R 27126MidslopeGPS@Boulder depositsP000006020T00P0000hfdb`^\ZXVRNNLJHFD2&!1628LowslopeGPSL@Entrada Sandstone02P00PBiocrust1-a1-a00500T0000xvtrpnljfd_ZPNLJHD1% 988High SlopeGPSZ@Boulder deposits020000021-a00400P0000ljhfdb`^ZXSOOMKIGC1% 55122Low slopeGPS@Eolian deposits06PP0Pbiotic soil1-a1-a00200T0000ywusqomkge`[NLJHFB1%  0n/aHigh LevelGPSj@Boulder deposits1-b00000303002001-a0000pnljhca_[YUQQOMKID2&!y0n/aHigh SlopeGPSD@Salt Wash Sandstone Member of the Morrison Formation04000003T003001-a0000|zxttrpnlh2&!O7299High LevelGPS@Salt Wash Sandstone Member of the Morrison Formation1-a1-a001-bcryptos1-bT00500T0000{vtrmh2&!` rollingvariableLow levelGPS@ Navajo SandstonePP0003Cryptos021-a00300P0000~|zxtrmi`\ZXVTB61&LVAL b 0 hvL8Wash runs through center of plot, with mostly bedrock exposed, but some sandy areas also in it course. Pinyon - Juniper pretty dwarfed.Broad, meandering wash in this canyon bottom 10-12m wide by 1-3m deep filled with volcanic boulders, small rocks and sand.Steep, flakey rocks soils, actively eroding downhill.Meandering wash (6-8m wide by 2-3m deep) below Navajo sandstone walls in this narrow canyon. Wash is filled with large volcanic boulders.Broad, flat mesa top covered in a large, homogenous Ephedra torreyana / Herbaceous community. High grass diversity! Some standing juniper skeletons in plot.Point is in a draw at the bottom of a large hill that is bisected by wash/gully/draws near the north end, lower down in elevation toward the South Desert. Herbaceous is less than 1 % - moonscape!!Very bouldery hills. Pretty homogenous community.Many pebbly rocks on soil surface.Large volcanic rocks embedded in the soil.The soil is sandy and sprinkled with pebbles.This plot is not entirely homogenous since most of it lies above the wash terrace, but the rise above (S) and its backslope are also included. Pebbly soil surface.Plot is located atop the head of a canyon. Most of the plot is on level ground, but the community spills over the edge to the slopes below. A bedrock cliff about 5m high separate. Many small rocks on soil surface, along with bedrock slabs.A minor wash runs through the plot. The sagebrush is restricted to that area.Point on a large flat area with washes (dry) throughout. Deep, sandy soil.The terrain is steep and rocky. The soil surface is mostly covered by litter.A variety of rocks decorate this site.The ground is covered with volcanic boulders.Plot landed in a shallow swale or wash area, with some slabby exposures of Navajo bedrock, but mostly aeolian soils of Navajo origin. Part of plot also has exposures of the basalt boulder deposits, but even here soils are modified by drifted in sands._< , + 2 r0IG+'0n/aHigh LevelGPS@Obscured by Soil040001-bcrypto031-b0T00P0000vtrpnljhfd_[SNLJHD2&!*&21160MidslopeGPSp@Boulder depositsP00001-b0500300P0000kigeca_]YWSNNLJHFD2&!)%1053InterfluveGPS@Carmel Formation04P0005biocrustTT0T0000000sqomkigeca_]SOMKIE3'"($g variablevariableLow levelGPSl@Navajo SandstonePP00Pcrypto04P00400T0000~|zxvtpnlh`^\ZXVD83('#: 18212High SlopeGPS@Carmel Formation020000021-a00500P0000omkigeca][VRRPNLJF4(#&" 8105High SlopeGPSD@ Boulder depositsT0000081-a0000P0000igeca_][YWRNNLJHFD2&!%!# 1019MidslopeGPS"@ Carmel Formation0203000020200200P0000mkigeca_[YUQQOMKGC1% $ }0n/aHigh LevelGPSF@ Obscured by Soil0400000400P00T0000hfdb`^\ZXVTPPNLJHD2&!#l 4150High LevelGPS@ Boulder depositsP0000040301-b001-a0000nljhfa_]XVRNNLJHFD2&!"520High SlopeGPS@ Carmel FormationT0001-acryptoT1-a00800T0000sqomkigea_ZXPKIGEC1% !20340High SlopeGPSVery rocky soils.Carmel Formation03T000020200300T0000}{ywusomieeca_]YG(# 346High LevelGPS!Soil is quite rocky and pebbly.Extrusive volcanics03000005P0020000000{ywssqomkgR% 32High LevelGPS@Obscured by Soil04000004T00200T0000geca_][YUSQMMKIGEA/#613Low slopeGPS@Curtis Formation0700000200P00T0000fdb`^\ZXVTRNNLJHFB0$325High LevelGPSPebbly soil surface.Extrusive volcanics03000004T0030000000~|zxvtpnlhhfdb`\G% 3158Low levelGPS@New Alluvium0500004dark cyanoP00P0000000omkigeca_][YMIGEC?1%  649High SlopeGPS@Boulder deposits0000007030000T0000geca_][YWUQMMKIGEC1%  variablevariableInterfluveGPST@Carmel Formation05P0002biocrustPT00200T0000}{yusqoea_][WE94(_ 0n/aHigh LevelGPS@Boulder deposits1-a0000040301-b001-a0000qomkidb`[YUQQOMKID2&! variablevariableLow levelGPSJ@Entrada Sandstone0203001-acrypto03P0P00P0000~|zxvtphca_[WD83( 7140High SlopeGPS,@Boulder deposits1-b0000050201-a001-a0000qomkidb`[YUQQOMKID2&! 4190High LevelGPS@Boulder deposits02000Pcrypto030301-b00P0000usqomkigb`\XPNLJHD2&!n variablevariableLow levelGPS@Navajo Sandstone1-a02P002biocrust021-b00200P0000|zuqgca_[VD83(>LVAL 0 4 F ~\"FpSome large black volcanic rocks half-buried in the soil. Skimpy crypto development in the open soil areas.Boulder and small rock-covered slope. PJ fairly stunted.Plot straddles steep banks on both sides of a wash (which now has running water from yesterday's storm) so slope and aspect vary. Lots of small platey Navajo rocks scattered around.Gravelly, shaley soil with small rocks covering soil surface. Several of the larger ponderosa pines are dead and standing.Many of the PINPON here are young.This is a yellow, ledgey, sandstone member of Carmel. Trees are generally stunted in height in this area, probably because of the shallow soils.The soil is sprinkled with pebbles.Dark, volcanic lichen-covered rocks everywhere - lots of colorful pebbly rocks too. Soil too rocky for crypto development.On a hillslope with steeper gullies. Soil is covered with small white rocks, there are also large areas with complete cover of crypto/lichens.A shallow erosional gully runs through plot; that is where most of the small junipers are.This patch of dirt has somehow escaped being eroded into badlands like the surrounding areas.Broad, fairly flat floodplain terrace just S of the wash less small rock cover here, but some slight crust development.This point is at the bottom of a steep hill which borders near Deep Creek. There are large volcanic boulders throughout soil.The terrain is highly sculpted by erosion.1/2 - 1 meter across volcanic boulders (covered with green lichens) everywhere. Quite a few colorful pebbly rocks in the soil as well.Ledgey bedrock outcrops which make shelves off both sides of a small rise, so slope and aspect vary. A fair amount of crypto development in the red sandy soil here.Small drainage course runs through plot and the ARTTRI are associated with it. Also an old ATV trail/ road in plot. Rocks in plot are mostly buried.Lots of big, black, lichen-covered volcanic rocks embedded in the soil. Soil is too rocky for much crypto development here.LVALd VHVFThis slope is covered with volcanic boulders.The surface has many small white rocks and a few large black boulders.Lots of dark grey rocks and gravel on soil surface, as well as some small white rocks. Area looks like it may have burned long ago. Many juniper skeletons around.This point is right on top of a small cliff about 20 ft tall that has white rocks and gypsum and lichens rest of soil is light brown with lots of small rocks.White, shaley rocks on soil surface, along with large round rocks of volcanic origin.Duney, sandy soils of Navajo origin.There are large red-brown boulders on soil which is nearly completely covered with litter.Very rocky soils. Deep, steep gully transects east edge of plot, but vegetation remains similar.The soil seems to be gypsum rich and is sprinkled with black volcanic rocks.Moist depression area on this hillside with slightly rolling microtopography. Many small pebbly rocks on the soil surface, from the Salt Wash member.Some shallow erosional tracks run through plot. An anomalous area of about 1/4 of the plot is home to the Russian thistle, goosefoot and snakeweed.The soil seems a little gypsiferous, having washed down from the Carmel above. A four-foot deep gully cuts through the plot without much effect on the vegetation.Plot is at the edge of the ridge; the head of a canyon also begins here and runs through the plot. It is about 10m deep here and many of the tall shrubs are there, although they are growing above on the flat also.This point is pretty sparse except for PJ & SHEROT most of ground is covered by small white rocks there is a switch to golden brown soil without white rocks and with crypto crust half way through plot. Rim with cliffs is close.This plot includes two types of geology with a different community on each type. It appears that some Entrada badlands are on the east side of the plot, or maybe it's just a non-gypsiferous type of Carmel.}W I 2 = LTCcB> variable6High SlopeGPS$@Boulder depositsT0000081-b0T00P0000trpnljhfdb]YYWUSQO=1, A= 9192MidslopeGPSx@Obscured by SoilP0000060003001-a0000igeca\ZXTRPLLJHFDB0$@<179MidslopeGPSZ@volcanic boulders1-b0000041-a00300P0000ljhfdb`^ZXSOOMKIGB/#?; 12125MidslopeGPSD@Boulder depositsT0000091-a0000P0000igeca_][YWRNNLJHFD2&!>:variablevariableLow levelGPSh@New AlluviumP0001-acryptos0303002001-a0000zxvrplh_ZXVTRD83(=918350High SlopeGPSRocky soils.Carmel Formation030000020200300P0000|zxvtrpnjhd``^\ZXTB(#<827107MidslopeGPSl@Entrada Sandstone050000P0401-b0000000ljhfdb`^YWSQQOMKIE2&!;7 27134High SlopeGPS@ Carmel Formation04P000PP00300T0000jhfdb`^\XVTRRPNLJF4(#:6 477MidslopeGPS@Boulder depositsT0000091-a0T00P0000fdb`^\ZXVTOKKIGECA/#95{337High LevelGPSThe PJ are slowly invading.Boulder deposits04000003T00200T0000~|zxtrplljhfd`N% 84 16187MidslopeGPS@Navajo Sandstone1-a020000202002001-a0000rpnljeca][WSSQOMID2&!731270High SlopeGPSH@ Carmel FormationP00001-a020070000000ljhfdb`^ZXTOOMKIGE3'"62p 12350High SlopeGPS<@ Carmel Formation1-a00001-a0008001-a0000qomkidb`\ZXSSQOMKF4(#514 2097MidslopeGPS@ Carmel Formation020000021-a004001-a0000omkigb`^ZXSOOMKIGC1% 40YvariablevariableLow levelGPSH@ Eolian deposits0700000200000T0000ywusqomkigeaa_][YUD83(3/ 1050MidslopeGPS@Boulder deposits00000060301a001a0000kigec_][WUQMMKIGEC1% 2.( 12100High SlopeGPS@Carmel Formation0200001-b0200500T0000omkigeca][WRRPNLJF4(#1-variablevariableInterfluveGPS@Carmel Formation0500004biocrustTT0T0000000}{ywusqoea_][WE94(0,variablevariableStep in slopeGPS,@Obscured by Soil0500001-b00030000000}{ywusomkffdb`^ZH<7(/+34High LevelGPS(@Obscured by Soil04000004T0020000000geca_][YUSQMMKIGEA/#.*429LowslopeGPSF@New Alluvium060T003biocrustTT0P0000000kigeca_][YWUKGECA=/#-)s310High LevelGPS@Salt Wash Sandstone Member of the Morrison Formation041-a00Pbiocrust03P00200P0000vtrpkg1% ,(1330High SlopeGPS@Carmel FormationT0001acryptoT1a00800T0000sqomkigea_[YQMKIGE3'"LVAL & R rV.:The ground is covered with volcanic rocks of various sizes.There are large red-brown boulders on ground and dead trees downed, soil is mostly covered by litter.Slightly rolling microtopography with pretty skimpy crypto development in the open soil areas. Only a few large volcanic rocks, barely exposed here.On hillside on top of mesa east of Bulberry Creek. Lots of snags here and small white rocks on soil.The surface is almost covered with tree litter.A narrow wash runs through plot where the rabbitbrush grows.A large opening in the tree canopy is included in plot. Lots of PINPON are young.Plot is perched on the rim of a steep hillside, partially with an aspect of about 8 and partially about 25. Soils rocky with old basalt boulders.Plot is on a gentle slope leading down to Deep Creek. Soil is probably thin here - lots of exposed Navajo sandstone visible from plot - and there are lots of small white rocks on surface.Fewer boulders here, all mostly buried. Quite a few rotted out, fallen logs. Ground carpeted with litter two to four inches thick. Some die-back on the PURTRI.Plot encompasses the wash (8-12 meters wide) and its sharply sloping terraces on either side, which are mainly covered with volcanic boulders. Wash is very rocky/bouldery as well.Plot is on the side of long ridge tapering off the Entrada cliffs above the South Desert. Tons of big, black volcanic rocks around, as well as small pebbles from the Morrison above.A depression between hills with mostly embedded volcanic boulder deposits scattered around. Ground is carpeted in two to four inch thick layer of pine needle / cone litter. Lots of PINPON recruitment, mostly sapling size.Large gully cuts through the center of plot, and has small, cliffy bedrock exposures. Purshia tridentata growing only in wash bottom. General aspect is south, but gully sides are steep, rocky, east and west facing slopes. Some dead doug fir skeletons standing around.qar ' x : ]Y gKYU` 208High SlopeGPSj@volcanic bouldersT000005040P00T0000hfdb`^\