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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 fmE/s. d5U7`6ab c,d#  Label0 "Verify Veg Stratax 2`s@p2d h1U`6 aTb buttonStrata "Verify Veg Strata~ "[Event Procedure]x #8 K?hCi{h1U`6aTbi Command4 (Verify AA Veg Strata~ "[Event Procedure]x [uN7Du#h1U`6 apbi Command5 2Verify Vegetation Details~ "[Event Procedure]x *fe)BV!Rh1U`6 a b i Command6 Close Form~ "[Event Procedure]x hUKqh1U`6apbi ButtonAADetails "Verify AA Details~ "[Event Procedure]x >͖_Kqtnh1U`6 a bi ButtonPlotsNull .Check Plots Null Fields~ "[Event Procedure]x gm J&͐ /d5U7`6 LVAL atbc,,d# e% Label10  Plotsx v^Z Cstd@olerh%^*\G{00020430-;C 0046}#2.0#0#C:\WINDOWS\sys@tem32\e2.tlb#OLE Automation0hOWC10> OWC10DD(E55D1DProgram Files\Microsoft Of fice\12\OFF>.DLL#  XP Web ComponentsEY ADODBYADOBY.Y110-8AA006D2EA4N1N,@mon/SS\ado\ms@ 21TG,ActiveX Data Objects 2.1 Lib0rary@$B@DAO>BDDA- C,25E0,0t0-{5Y,'S@hared\\dao360.d ll[ 3.6-, }@*Form_frmVerifyStr=G(A@rm_fV@ri@yS@ra@a@ DQRAADEIUIBWTDKHTEAGJKXNJIYF28AQRIxEIUBT{KHTE@GJKXNIYzFB@*S@,HF""+bͬ" (0I*SIDetaild Label0h buttonStratah Command4h Command5h Command6h ButtonAADetailsh ButtonPlotsNulld Label10d Label11h Command12LVAL 8 Mn}HxME PS<S<S<< <<<<Xe dN0{28F6BE0C-9730-491E-A3C8-F72AF3FE5349}P m X~ % x|% "%`$?`&`(SI`*`, hA p % %`$`& [   % @% "`%`$`&`(`*`, f 8 % X% "x%`$`&`(`*`, 8 W  % % "h%`$op`&ol M `s\ % gb%`$Fi`& F iil@%' "  (08 @HP X    (8 @Pjh d@ ,Hxj bpxj dpxj fpxj `hpxj fhp *x  vH  j dh    j  `h    j  ``    j  dX    j  fX    j  `Xj dP     0 8"@h p "x   8 HX  p *Z(*0X`*\P*X\*LVALX x*^*\H*`@*H^x*Vh*pZ  ( 0 @ HX `"h  "        l fl dl fl hl bl h l  h   !l! f!!!"l" h"""#l# b###$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'. M 0B@2ell3 4.86 . %6.Pr B@8 Fi'& !:aTim ">$<m;C [VegDetailID]tblVegetationDetails$[Stratum] = 'T1' And VegetationID = "B$@$<ox\Plot "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@DZkHk@ "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 VegetaLVAL tionID = "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{28F6BE0C-9730-491E-A3C8-F72AF3FE5349} |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`     @ @ @ @        NOPQST\g%&'()*n @@@@@@@@      g%)*&'( N S T  NONPNQN\ @@@@ @@@M`OLJikMokmd`UidofkOJmJJMMQkkfJUQkOJmJLJkQk Sdi`kY`QukfQMk`dOo^Qk`kvkJMMQkkkmdiJUQ+iddmfidfOJmJ iQfdimkkMiYfmk qLJ`kvkJMMQkkkmdiJUQ+kMiJmMWJMQkkqLJOJmJ%qLJfid[QMmfid[QMm*fid[QMms`)qLJ+qLJ+fid[QMm'OYi(OhiJJOQYoYLsmO\WmQJU[\ub[YvS& 6 OYiOJmJ fidfOJmJ6 OYiOJmJL^dL NL^dLNL^dLOQ^mJNfidfOJmJNmvfQYbSdS YN))Y  Y Y L  Y , Y ,~ Y ~Id LValueObjectGuidObjectNameProperty Value,~,~,)*~,~,~,)+~,~,~,),~,YYYId$ObjectGuidProperty$ObjectNameProperty)Hv1b ( ( (>YN.. Y Y Y  Y Y ,.Y .EY E Filter FlagsIdNamePosition SelectedObjectIDTypeE.,E.,.0,.EYIdv1a-uCustom ^Tables%"w V-/// RY$$N22$$$Y Y Y  Y Y ,nY nY  FlagsGroupCategoryIDIdName"Object Type GroupObjectIDPositionn,n,24,nn,n,25,nYYGroupCategoryIDIdv1 : 1$yL|O" n A  ` 3   R % q D  $ w# w" w! w  w wh w w  w w w w w w  w  w  w  w  w w w w w  w  w  w  w  wCustom Group 162.*  w w w w w w w 1 @ @ @ @3 3 3 3 3 3333333333333333333 3!3"3#333333333 1 @ @ @ @33333333 3 3  3  3  3 3 33333333333333333 3!3 "3!#3"$3# YJJN77JJJY Y Y Y  Y ,Y EY E FlagsGroupIDIconIdNameObjectIDPosition,E,E79E,,E,E7:E,YYGroupIDIdv1\6JyLk> ] 0  | O " n A  ` 3   R % qDc6 U(tGf9 X+J6< oI1; oH-: oGB oFA oE@ oD ? oC> oB= oA9 o@8 o?7 o>6 o=5 o<4 o;3 o:2 o91 o80 o7/ o6. o5- o4, o3+ o2* o1) o0( o/' o.& o-% o,$ o+# o*" o)! o(  o' o& o% o$l o#B o" o! o  o o o os o' o oh o_ o o o  o  o  o  ov  oZ oD o o  o  o  o  o ( o o  o  o o o o o o 6 @ @ @ @ @ @ @ @ @8888888888888888888888888 8!8"8#8$8%8&8'8(8)8*8+8,8-8.8/808182838485868788898:8;8<8=8>8?8@8A8B8C8D8E8F8G8H8I888 8 8 8 8 8 6 @ @ @ @ @ @ @ @ @88888888 8 8  8  8  8 8 88888888888888888 8!8 "8!#8"$8#%8$&8%'8&(8')8(*8)+8*,8+-8,.8-/8.08/180281382483584685786887988:89;8:<8;=8<>8=?8>@8?A8@B8AC8BD8CE8DF8EG8FH8GI8HJ8IRYG:\nN<<Y c Y dY IdNameTypedv;Ph=dA z [ 8 D ^ !  { N  | A  k,o<vEi.zO"h;{JU,tlkpStructureStages0,tlkpStratatlkpStatestlkpSoilTexture($tlkpSoilDrainage*&tlkpPlotShapes&"tlkpPJAgetlkpPhysiogClass*&tlkpPhotoTypes&"tlkpPhotographer*&tlkpPhotoComments,(tlkpParkstlkpLeafType"tlkpLeafPhen"tlkpLandform"tlkpHydrology$ tlkpHeightClass($tlkpGeology tlkpCowardin"tlkpCoverAA tlkpCovertlkpCameratlkpAssociations*&tlkpAlliances$ tlkpAAVegAssocRanks0,tlkpAAVegAssociation2.tblVegetationDetails2.tblVegetation$ ltblPlotLocation($BtblPlotDetails&"tblPhotostblNCPNPlants$ tblGeneralSpecimens0,tblGeneralPhotos*&tblFuelsDetails($tblFuelsstblFinalAssociationNamesPlotsD@'tblFinalAssociationNamesAA>:tblEnvironmentDetails40htblEnvironment&"_tblDataMgmtLog&"tblAAVegetationDetails62tblAAVegetation($tblAAVegAssociation0,tblAAPhotos tblAALocation$ tblAAEnvironmentDetails84vtblAAEnvironment*&ZtblAADetails"Dtbl_Final_Classification:6slgnamesslgII slgI qryTallyPlantSpecies2. Qry_GIS_veg ;MSysNavPaneObjectIDs2.6MSysNavPaneGroupToObjects<81MSysNavPaneGroups,(-MSysNavPaneGroupCategories>:(MSysAccessXML$ MSysAccessStorage,( h:\piii\remoteclass\slgi:6 c:\slgIAdmin frmVerifyStrata($AccessLayout "SysRelScriptsReportsModulesFormsDataAccessPages($MSysRelationships,(MSysQueries MSysACEsMSysObjects MSysDbRelationships$ DatabasesTables;4qFZ 7 u  R _  f  u4OT w,Gp9L[v<tlkpUSGS_QuadtblPlotLocationB>;tlkpTopographytblEnvironmentB>:tlkpSurveyorstblPlotDetails@<9tlkpStructureStagestblFuelsDetailsNJ8tlkpStratatblVegetationDetailsFB7tlkpStatestblPlotLocation<86tlkpSoilTexturetblEnvironmentD@5tlkpSoilDrainagetblEnvironmentFB4tlkpPlotShapestblPlotDetailsB>3tlkpPJAgetblFuels,(2tlkpPhysiogClasstblVegetationD@1tlkpPhotoTypestblPhotos840tlkpParkstblPlotLocation:6/tlkpLeafTypetblVegetation<8.tlkpLeafPhentblVegetation<8-tlkpLandformtblEnvironmentDetailsLH,tlkpHydrologytblEnvironment@<+tlkpHeightClasstblVegetationB>*tlkpGeologytblEnvironment<8)tlkpCowardintblEnvironment>:(tlkpCovertblVegetationDetailsD@'tlkpAlliancestblVegetation>:&tlkpAAVegAssociationtblAAVegAssociationXT%tblVegetationtblVegetationDetailsLH$tblPlotDetailstblVegetation@<#tblPlotDetailstblPhotos84"tblPlotDetailstblFuels62!tblPlotDetailstblEnvironmentB> tblNCPNPlantstblVegetationDetailsLHtblNCPNPlantstblFuelsDetailsB>tblNCPNPlantstblAAVegetationDetailsPLtblFuelstblFuelsDetails84tblEnvironmenttblEnvironmentDetailsPLPlot LocationPlot DescriptionD@MSysAccessStorageSTGREL84{F19E2E89-3A6C-4E78-86DD-7E9869ACEF43}VR{C9B8BF35-C256-4B7F-B478-A6CB03308F6A}VR{BEF08136-DBEE-4D0B-B67B-6239397FFBA6}VR{AF4F21DC-8C83-478D-9181-6F5CD20C6823}VR{AAA18348-FF53-42ED-9F0B-7EBF76EC1B08}VR{A5BA107D-12D5-4745-A428-131AF1F95A65}VR{8A48A9DE-9CC3-4E4D-A6E5-C1F6B5D0CA67}VR{82469702-159A-4B62-94D3-333C27377BF0}VR{7162FDF8-2224-40D6-9757-AC2AE25F2DE4}VR{1C5BE197-FE38-4E00-A5F0-CD7757344DEF}VRzLookupTables$ zLookupFields$ zFieldWidths" tlkpUTMZone tlkpUSGS_Quad$ tlkpTopography&"tlkpSurveyors$ ;=tlkpUTMZonetblPlotLocation>:>p,% u / k (  W  K -  ]%UCvLw5j%d!X s.tblVegetation.DwarfCovTot8 g s.tblVegetation.DwarfHt4 g s.tblVegetation.ShrubCovTot8 g s.tblVegetation.ShrubHt4 g s.tblVegetation.TallShCovTot9 g s.tblVegetation.TallShHt5 g s.tblVegetation.SubCovTot6 g s.tblVegetation.SubHt2 g s.tblVegetation.CanCovTot6 g s.tblVegetation.CanHt2 g s.tblVegetation.EmergCovTot8 g s.tblVegetation.EmergHt4 g s.tblVegetation.Physiognom7 g s.tblVegetation.Associations9 g s.tblVegetation.Alliance5 g s. !tblVegetation.ProvCommunityName> g s. tblVegetation.VegetationID9 g s. tblPlotDetails.PlotShape7 g s. B@  g s. tblPlotDetails.PlotDiam6 g s.tblPlotDetails.PlotWidth7 g s.tblPlotDetails.PlotAzimuth9 g s.tblPlotDetails.PlotLength8 g s.tblPlotDetails.SurveyDate8 g s.tblPlotDetails.PlotID4 g s.tblPlotLocation.UTMNorthing: g s.tblPlotLocation.UTMEasting9 g s.tblPlotLocation.PlotCode7 g ls.tblVegetationDetails999  ls.tblVegetation+++  ls.tblPlotDetails---  ls.tblPlotLocation///  s. G s. G ls.  s. G tblNCPNPlants.LatinName6 ' tblNCPNPlants.FamilyName7 ' tblNCPNPlants.FullName5 g tblNCPNPlants.Authority6 g tblNCPNPlants.LatinName6 g tblNCPNPlants.FamilyName7 g tblNCPNPlants.TSN0 g tblNCPNPlantstblVegetationDetailsX@ _S+  CountOfTSN!Count(tblVegetationDetails.TSN)R%% o tblNCPNPlants.FullName5 g tblNCPNPlants.Authority6 g tblNCPNPlants.LatinName6 g tblNCPNPlants.FamilyName7 g tblNCPNPlants.TSN0 g tblVegetationDetails999  tblNCPNPlants+++   G  G    G kptblPlotDetailstblVegetationX@ SG-  kptblPlotLocationtblPlotDetailsd@WK/  kp tblPlotLocation.BPUCode6 g kptblPlotDetails.Surveyors7 g kptblPlotLocation.[UTM Error]: g kptblPlotLocation.AerialPhotoNo< g#<|<t4 j ( ^  x  p R 4 @ w2e;j$Q 6rTT tblPlotDetailstblVegetationX@SG- !tblVegetation.ProvCommunityName> gtblPlotDetails.PlotShape7 gtblPlotDetails.PlotCode6 gtblPlotDetails.PlotID4 gtblVegetation+++ tblPlotDetails---  G G  GtblVegetationtblVegetationDetails|@_S+ tblPlotDetailstblVegetationX@SG- tblPlotLocationtblPlotDetailsd@WK/ !tblVegetationDetails.CoverClass> gtblVegetationDetails.TSN7 gtblVegetationDetails.Stratum; gtblVegetation.Physiognom7 gtblVegetation.Associations9 gtblVegetation.Alliance5 g !tblVegetation.ProvCommunityName> g tblVegetation.VegetationID9 g tblPlotLocation.UTMNorthing: g tblPlotLocation.UTMEasting9 g tblPlotDetails.PlotShape7 gB@ gtblPlotDetails.PlotDiam6 gtblPlotDetails.PlotWidth7 gtblPlotDetails.PlotAzimuth9 gtblPlotDetails.PlotLength8 gtblPlotDetails.SurveyDate8 gtblPlotDetails.PlotCode6 gtblPlotDetails.PlotID4 gtblVegetationDetails999 tblVegetation+++ tblPlotLocation/// tblPlotDetails---  G G  G s.tblVegetationtblVegetationDetails|@_S+  s.tblPlotDetailstblVegetationX@ SG-  s.tblPlotLocationtblPlotDetailsd@ WK/  s.,tblVegetation.EpiTotCov6 g s.+tblVegetation.EpiHt2 g s.*tblVegetation.VineTotCov7 g s.)tblVegetation.VineHt3 g s.(tblVegetation.NonvasCovTot9 g s.'tblVegetation.NonvasHt5 g s.&tblVegetation.SeedlCovTot8 g s.%tblVegetation.SeedlHt4 g s.$tblVegetation.FernCovTot7 g s.#tblVegetation.FernHt3 g s."tblVegetation.ForbCovTot7 g s.!tblVegetation.ForbHt3 g s. tblVegetation.GramCovTot7 g s.tblVegetation.GramHt3 g s.tblVegetation.HerbCovTot7 g s.tblVegetation.HerbHt3 g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lotCodeFinal NVC NameEVEYYYPlotCodePrimaryKeyv1 ?DS  J .  % -rEoN}BWARCH.0027Coleogyne ramosissima ShrublandVARCH.0026Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0025Coleogyne ramosissima ShrublandVARCH.0024Coleogyne ramosissima ShrublandVARCH.0023Coleogyne ramosissima ShrublandVARCH.0022Ephedra viridis / Pleuraphis jamesii ShrublandtARCH.0021Grayia spinosa ShrublandHARCH.0020Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri ShrublandARCH.0019Ephedra viridis / (Achnatherum hymenoides, Hesperostipa comata) ShrublandARCH.0018ARCH.0017Sarcobatus vermiculatus Disturbed ShrublandnARCH.0016Coleogyne ramosissima ShrublandVARCH.0015Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0014Pinus edulis - Juniperus osteosperma / Quercus havardii var. tuckeri Woodland ARCH.0013Atriplex confertifolia / Pleuraphis jamesii Shrubland ARCH.0012Leymus salinus Shale Sparse Vegetationd ARCH.0011Artemisia filifolia Colorado Plateau Shrublandt ARCH.0010Coleogyne ramosissima ShrublandV ARCH.0009Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0008Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0007Sarcobatus vermiculatus / Artemisia tridentata ShrublandARCH.0006Coleogyne ramosissima ShrublandVARCH.0005Pleuraphis jamesii Herbaceous VegetationhARCH.0004Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0003Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0002Coleogyne ramosissima ShrublandVARCH.0001Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandDBv z  # V ,H^7ARCH.0055Atriplex confertifolia / Pleuraphis jamesii Shrubland6ARCH.0054Coleogyne ramosissima ShrublandV5ARCH.0053Bromus tectorum Semi-natural Herbaceous Vegetation|4ARCH.0052Coleogyne ramosissima ShrublandV3ARCH.0051Coleogyne ramosissima ShrublandV2ARCH.0050Pleuraphis jamesii Herbaceous Vegetationh1ARCH.0049Bromus tectorum Semi-natural Herbaceous Vegetation|0ARCH.0048Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$/ARCH.0047Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$.ARCH.0046Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Shrubland-ARCH.0045Coleogyne ramosissima ShrublandV,ARCH.0044Bromus tectorum Semi-natural Herbaceous Vegetation|+ARCH.0043Coleogyne ramosissima ShrublandV*ARCH.0042Ephedra viridis / (Achnatherum hymenoides, Hesperostipa comata) Shrubland)ARCH.0041Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$(ARCH.0040Atriplex confertifolia / Pleuraphis jamesii Shrubland'ARCH.0039Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Shrubland&ARCH.0038Atriplex spp. Desert Pavement Sparse Vegetationv%ARCH.0037Ephedra viridis / Pleuraphis jamesii Shrublandt$ARCH.0036Atriplex confertifolia / Pleuraphis jamesii Shrubland#ARCH.0035Coleogyne ramosissima ShrublandV"ARCH.0034Pleuraphis jamesii Herbaceous Vegetationh!ARCH.0033Coleogyne ramosissima ShrublandV ARCH.0032Pleuraphis jamesii - Sporobolus airoides Herbaceous VegetationARCH.0031Leymus salinus Shale Sparse VegetationdARCH.0030Coleogyne ramosissima ShrublandVARCH.0029Coleogyne ramosissima ShrublandVARCH.0028Coleogyne ramosissima ShrublandVmDi S m c 6  tGoINARCH.0078Ericameria nauseosa Desert Wash ShrublandjMARCH.0077Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$LARCH.0076Atriplex canescens ShrublandPKARCH.0075Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri ShrublandJARCH.0074Pinus edulis - Juniperus osteosperma / Coleogyne ramosissima WoodlandIARCH.0073Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$HARCH.0072Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$GARCH.0071Pinus edulis - Juniperus osteosperma / Coleogyne ramosissima WoodlandFARCH.0070Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri ShrublandEARCH.0069Pleuraphis jamesii - Sporobolus airoides Herbaceous VegetationDARCH.0068Populus fremontii / Equisetum spp. Woodland [Provisional]CARCH.0067Pinus edulis - Juniperus osteosperma / Quercus havardii var. tuckeri WoodlandBARCH.0066Coleogyne ramosissima ShrublandVAARCH.0065Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$@ARCH.0064Coleogyne ramosissima ShrublandV?ARCH.0063Pinus edulis - Juniperus osteosperma / Coleogyne ramosissima Woodland>ARCH.0062Coleogyne ramosissima ShrublandV=ARCH.0061Juniperus osteosperma / Mixed Shrubs Talus Woodland~<ARCH.0060Pinus edulis - Juniperus osteosperma / Purshia stansburiana Woodland;ARCH.0059Leymus salinus Shale Sparse Vegetationd:ARCH.0058Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse Vegetation9ARCH.0057Pleuraphis jamesii Herbaceous Vegetationh8ARCH.0056Pleuraphis jamesii Herbaceous Vegetationh2Dt @ T ~  V.u"ZxjARCH.0106Eriogonum corymbosum Badlands Sparse VegetationviARCH.0105Atriplex gardneri Dwarf-shrublandZhARCH.0104Atriplex gardneri Dwarf-shrublandZgARCH.0103Atriplex corrugata Dwarf-shrubland\fARCH.0102Atriplex corrugata Dwarf-shrubland\eARCH.0101Atriplex gardneri Dwarf-shrublandZdARCH.0100Atriplex confertifolia / Pleuraphis jamesii ShrublandcARCH.0099Atriplex confertifolia / Pleuraphis jamesii ShrublandbARCH.0098Rhus trilobata - Ephedra (viridis, torreyana) Talus ShrublandaARCH.0097Sporobolus airoides Southern Plains Herbaceous Vegetation`ARCH.0096Atriplex corrugata Dwarf-shrubland\_ARCH.0095Atriplex confertifolia / Pleuraphis jamesii Shrubland^ARCH.0094Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Shrubland]ARCH.0093Poliomintha incana - Artemisia filifolia - Vanclevea stylosa Shrubland\ARCH.0092Coleogyne ramosissima ShrublandV[ARCH.0091Coleogyne ramosissima ShrublandVZARCH.0090Pinus edulis - Juniperus osteosperma / Coleogyne ramosissima WoodlandYARCH.0089Chrysothamnus viscidiflorus Shrubland AlliancetXARCH.0088Salix exigua / Barren ShrublandVWARCH.0087Sarcobatus vermiculatus Disturbed ShrublandnVARCH.0086Artemisia filifolia Colorado Plateau ShrublandtUARCH.0085Quercus havardii var. tuckeri ShrublandfTARCH.0084Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandSARCH.0083Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandRARCH.0082Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$QARCH.0081Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandPARCH.0080Coleogyne ramosissima ShrublandVOARCH.0079Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$eDu}   l ) k>$z"ARCH.0303Ephedra viridis / Pleuraphis jamesii ShrublandtARCH.0302Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse VegetationARCH.0301Pinus edulis - Juniperus osteosperma / Purshia stansburiana WoodlandARCH.0128Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0127Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Shrubland~ARCH.0126Artemisia filifolia Colorado Plateau Shrublandt}ARCH.0125Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$|ARCH.0124Sarcobatus vermiculatus / Sporobolus airoides Shrubland{ARCH.0123Hesperostipa comata Great Basin Herbaceous VegetationzARCH.0122Juniperus osteosperma - (Pinus 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hARCH.0332Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse VegetationARCH.0331Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0330Atriplex canescens / Sporobolus airoides Shrubland|ARCH.0329Pleuraphis jamesii Herbaceous VegetationhARCH.0328Artemisia filifolia Colorado Plateau ShrublandtARCH.0327Artemisia filifolia Colorado Plateau ShrublandtARCH.0326Ephedra torreyana / Pleuraphis jamesii ShrublandxARCH.0325Atriplex gardneri Dwarf-shrublandZARCH.0324Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0323Coleogyne ramosissima ShrublandVARCH.0322Leymus salinus Shale Sparse VegetationdARCH.0321Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0320Coleogyne ramosissima ShrublandVARCH.0319Coleogyne ramosissima ShrublandVARCH.0318Coleogyne ramosissima ShrublandVARCH.0317Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0316Pinus edulis - Juniperus osteosperma / Quercus havardii var. tuckeri WoodlandARCH.0315Ephedra viridis / Pleuraphis jamesii ShrublandtARCH.0314Coleogyne ramosissima ShrublandVARCH.0313Quercus havardii var. tuckeri ShrublandfARCH.0312Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri ShrublandARCH.0311Coleogyne ramosissima ShrublandVARCH.0310Atriplex gardneri Dwarf-shrublandZARCH.0309Coleogyne ramosissima ShrublandVARCH.0308Coleogyne ramosissima ShrublandVARCH.0307Coleogyne ramosissima ShrublandVARCH.0306Coleogyne ramosissima ShrublandVARCH.0305Pinus edulis - Juniperus osteosperma / Mixed Shrubs Talus WoodlandARCH.0304Pleuraphis jamesii Herbaceous VegetationhD5 ; 8 j %HARCH.0354Coleogyne ramosissima ShrublandVARCH.0353Leymus salinus Shale Sparse VegetationdARCH.0352Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0351Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0350Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0349Juniperus osteosperma / Mixed Shrubs Talus Woodland~ARCH.0348Artemisia bigelovii - Ephedra (viridis, torreyana) Talus ShrublandARCH.0347Coleogyne ramosissima ShrublandVARCH.0346Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0345Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0344Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0343Coleogyne ramosissima ShrublandVARCH.0342Coleogyne ramosissima ShrublandVARCH.0341Quercus havardii var. tuckeri ShrublandfARCH.0340Quercus havardii var. tuckeri ShrublandfARCH.0339Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0338Slickrock Fin Pocket [Park Special]^ARCH.0337Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri ShrublandARCH.0336Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0335Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0334Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0333Pleuraphis jamesii Herbaceous VegetationhDoO U k }  Y G ~um?ARCH.0379Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0378Populus fremontii / Ericameria nauseosa WoodlandxARCH.0377Achnatherum hymenoides Colorado Plateau Herbaceous VegetationARCH.0376Sarcobatus vermiculatus Disturbed ShrublandnARCH.0375Elaeagnus angustifolia Semi-natural WoodlandpARCH.0374Artemisia filifolia Colorado Plateau ShrublandtARCH.0373Artemisia filifolia Colorado Plateau ShrublandtARCH.0372Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0371Coleogyne ramosissima ShrublandVARCH.0370Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0369Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0368Quercus havardii var. tuckeri ShrublandfARCH.0367Ephedra viridis / (Achnatherum hymenoides, Hesperostipa comata) ShrublandARCH.0366Coleogyne ramosissima ShrublandVARCH.0365Pinus edulis - Juniperus osteosperma / Cercocarpus intricatus WoodlandARCH.0364Sarcobatus vermiculatus Disturbed ShrublandnARCH.0363Pleuraphis jamesii Herbaceous VegetationhARCH.0362Artemisia filifolia Colorado Plateau ShrublandtARCH.0361Coleogyne ramosissima ShrublandVARCH.0360Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0359Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0358Quercus havardii var. tuckeri ShrublandfARCH.0357Sarcobatus vermiculatus / Artemisia tridentata ShrublandARCH.0356Tamarix spp. Temporarily Flooded Semi-natural ShrublandARCH.0355Sarcobatus vermiculatus / Artemisia tridentata ShrublandD* ( " D  G [=cwsFFARCH.0621Sarcobatus vermiculatus / Artemisia tridentata ShrublandARCH.0620Populus fremontii / Salix exigua ForestfARCH.0619Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0618Atriplex spp. Desert Pavement Sparse VegetationvARCH.0617Juniperus osteosperma / Sparse Understory Woodland|ARCH.0616Leymus salinus Shale Sparse VegetationdARCH.0615Atriplex spp. Desert Pavement Sparse VegetationvARCH.0614Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0613Atriplex confertifolia - Picrothamnus desertorum ShrublandARCH.0612Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0611Atriplex gardneri / Pleuraphis jamesii Dwarf-shrublandARCH.0610Atriplex gardneri / Pleuraphis jamesii Dwarf-shrublandARCH.0609Sarcobatus vermiculatus / Artemisia tridentata ShrublandARCH.0608Atriplex spp. Desert Pavement Sparse VegetationvARCH.0607Leymus salinus Shale Sparse VegetationdARCH.0606Pleuraphis jamesii Herbaceous VegetationhARCH.0605Coleogyne ramosissima ShrublandVARCH.0604Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0603Coleogyne ramosissima ShrublandVARCH.0602Atriplex spp. Desert Pavement Sparse VegetationvARCH.0601Poliomintha incana - Artemisia filifolia - Vanclevea stylosa ShrublandARCH.0384Atriplex canescens ShrublandPARCH.0383Sporobolus cryptandrus Great Basin Herbaceous VegetationARCH.0382Krascheninnikovia lanata Dwarf-shrublandhARCH.0381Pinus edulis - Juniperus osteosperma / Purshia stansburiana WoodlandARCH.0380Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$MDt  w J   8  ARCH.0646Atriplex canescens ShrublandPARCH.0645Pinus edulis - Juniperus osteosperma / Coleogyne ramosissima WoodlandARCH.0644Juniperus osteosperma / Mixed Shrubs Talus Woodland~ARCH.0643Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0642Ephedra viridis / Pleuraphis jamesii ShrublandtARCH.0641Coleogyne ramosissima ShrublandVARCH.0640Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0639Coleogyne ramosissima ShrublandVARCH.0638Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0637Sarcobatus vermiculatus Disturbed ShrublandnARCH.0636Pleuraphis jamesii Herbaceous VegetationhARCH.0635Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0634Coleogyne ramosissima ShrublandVARCH.0633Atriplex confertifolia - Picrothamnus desertorum ShrublandARCH.0632Leymus salinus Shale Sparse VegetationdARCH.0631Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0630Ephedra viridis / (Achnatherum hymenoides, Hesperostipa comata) ShrublandARCH.0629Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0628Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0627Coleogyne ramosissima ShrublandVARCH.0626Ephedra viridis / (Achnatherum hymenoides, Hesperostipa comata) ShrublandARCH.0625Coleogyne ramosissima ShrublandVARCH.0624Coleogyne ramosissima ShrublandVARCH.0623Coleogyne ramosissima ShrublandVARCH.0622Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$Dt w   B yZ-b8ARCH.0671Leymus salinus Shale Sparse VegetationdARCH.0670Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0669Aquilegia micrantha - Mimulus eastwoodiae Herbaceous VegetationARCH.0668Atriplex confertifolia / Pleuraphis jamesii ShrublandARCH.0667Krascheninnikovia lanata / Pleuraphis jamesii Dwarf-shrublandARCH.0666Artemisia bigelovii - Ephedra (viridis, torreyana) Talus ShrublandARCH.0665Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$ARCH.0664Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse VegetationARCH.0663Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse VegetationARCH.0662Ephedra torreyana - (Atriplex spp.) / Nonvascular Gypsum Sparse VegetationARCH.0661Coleogyne ramosissima ShrublandVARCH.0660Ephedra torreyana - (Atriplex spp.) / 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Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$2ARCH.0694Poliomintha incana - Artemisia filifolia - Vanclevea stylosa Shrubland1ARCH.0693Poliomintha incana - Artemisia filifolia - Vanclevea stylosa Shrubland0ARCH.0692Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$/ARCH.0691Juniperus osteosperma - (Pinus edulis) / Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Wooded Shrubland$.ARCH.0690Rhus trilobata Intermittently Flooded Shrublandv-ARCH.0689Quercus havardii var. tuckeri Shrublandf,ARCH.0688Hesperostipa comata Great Basin Herbaceous Vegetation+ARCH.0687Pinus edulis - Juniperus osteosperma / Quercus havardii var. tuckeri Woodland*ARCH.0686Artemisia filifolia Colorado Plateau Shrublandt)ARCH.0685Coleogyne ramosissima - Purshia stansburiana - Quercus havardii var. tuckeri Shrubland(ARCH.0684Coleogyne ramosissima ShrublandV'ARCH.0683Pinus edulis - 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"\!#\"$\#%\$&\%'\&(\')\(*\)+\*,\+-\,.\-/\.0\/1\02\13\24\35\46\57\68\79\8:];]<]=]>]?]@]A]B]C] D] E] F] G] H]I]J]K]L]M]N]O]P]Q]R]S]T]U]V]W]X]Y]Z] []!\]"]]#^]$_]%`]&a]'b](c])d]*e]+f],g]-h].i]/j]0k]1l]2m]3n]4o]5p]6q]7r]8s]9t^u^v^w^x^y^z^{^|^}^ ~^ ^ ^ ^ ^^^^^^^^^^^^^^^^^^^ ^!^"^#^$^%^&^'^(^)^*^+^,^-^.^/^0^1^2^3^4^5^6^7^8^9__________ _ _ _ _ ___________________ _!_"_#_$_%_&_'_(_)_*_+_,_-_._/_0_1_2_3_4_5_6_7_8_9`````````` ` ` ` ` `````````````````` `  `! `" `# `$`%`&`'`(`)`*`+`,`-`.`/`0`1`2`3`4`5`6 `7!`8"`9#a$a%a&a'a(a)a*a+a,a -a .a /a 0a 1a2a3a4a5a6a7a8a9a:a;a<a=a>a?a@aAaBaCa Da!Ea"Fa#Ga$Ha%Ia&Ja'Ka(La)Ma*Na+Oa,Pa-Qa.Ra/Sa0Ta1Ua2Va3Wa4Xa5Za6[a7\a8]a9^b_b`babbbcbdbebfbgb hb ib jb kb lbmbnbobpbqbrbsbtbubvbwbxbybzb{b|b}b~b 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/c0c1c2c3c4c5c6c7c8c9dddddddddd d d d d ddddddddddddddddddd d!d"d#d$d%d&d'd(d)d*d+d,d-d.d/d0d1d2d3d4d5 d6 d7 d8 d9 eeeeeeeeee e e e e eeeee 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Da!Ea"Fa#Ga$Ha%Ia&Ja'Ka(La)Ma*Na+Oa,Pa-Qa.Ra/Sa0Ta1Ua2Va3Wa4Xa5Za6[a7\a8]a9^b_b`babbbcbdbebfbgb hb ib jb kb lbmbnbobpbqbrbsbtbubvbwbxbybzb{b|b}b~b 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/c0c1c2c3c4c5c6c7c8c9dddddddddd d d d d ddddddddddddddddddd d!d"d#d$d%d&d'd(d)d*d+d,d-d.d/d0d1d2d3d4d5 d6 d7 d8 d9 eeeeeeeeee e e e e eeeee e!e"e#e$e%e&e'e(e)e*e+e,e-e .e!/e"0e#1e$2e%3e&4e'5e(6e)7e*8e+9e,:e-;e.<e/=e0>e1?e2@e3Ae4Be5Ce6Ee7Fe8Ge9HfIfJfKfLfMfNfOfQfRf Sf Uf Vf Wf XfYfZf[f\f]f^f_fZt @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @`fbfcfdfefffgfhfifjfkf lf!mf"nf#of$pf%qf&rf'sf(tf)uf*vf+wf,xf-yf.zf/{f0|f1}f2~f3f4f5f6f7f8f9gggggggggg g g g g ggggggggggggggggggg g!g"g#g$g%g&g'g(g)g*g+g,g-g.g/g0g1g2g3g4g5g6g7g8g9hhhhhhhhhh h h h h hhhhhhhhhhhhhhhhhhh h!h"h#h$h%h&h'h(h)h*h+h,h-h.h/h0h1h2h3h4h5h6h7h8h9iiiiiiiiii i i i i  i i i i iiiiiiiiiiiiO YNwwY 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 WateraooSwSuaStawovHSuowDwYYZYYY.rDL{AAA18348-FF53-42ED-9F0B-7EBF76EC1B08}EnvironmentID PlotIDPrimaryKeywwv1bvmڶJDDTJ"%$%ILVAL< R N <r(The undulating slickrock makes measuring slope and aspect an educated guess. Plants are rooted in small pools of sand covered with biocrust.This is a large sand sheet that transitions to bare Navajo sandstone along Courthouse Wash.The wash bottom is cut down about a meter from the vegetated banks.This is a weedy area with silty soil.The badlands slope generally to the north. The clay soil is covered with pebbles and white crystals.A thick layer of sandy alluvium fills the valley floor.The eroded slope is littered with large rocks.The eroded hogback is mostly soil here, littered with large rocks.The top of the hogback is broken up here creating pockets of soil.This plot actually wraps clear over the top of the hogback - the slope given is for the majority of the plot.This dune has climbed the side of a Morrison hogback, making a fairly thick layer in this area. Many shrubs are dead - mostly Vanclevea.This is the lower slope of a Morrison hogback that is covered with a thin layer of blown-in sand.The broad wash bottom is cut down about a meter below the banks that hold the vegetation. The soil is all sand with no rocks at all.Plants are growing in cracks in the rocks and small pockets of soil.Lots of slickrock is exposed and there are mounds of sandy soil.Plants are growing in cracks in the slickrock and pockets of soil.A few Navajo domes poke up through the sandy soil.The slope is the average of undulating terrain. Plants are growing in cracks in the slickrock and pockets of soil.The terrain is ledgy with the larger ledges having substantial pockets of soil. The slope is averaged across the ledges.Soil is very sandy. Rocks are exposed only in the washes. Biocrust is well developed.The surface alternates between rocky ledges and sloping pockets of soil.The slope is the average of the steps and ledges. The plot varies from bare rock to deep soil because of the ledgy terrain. Junipers are mostly stunted.WvTV T e 60[@368High LevelGPS@zNavajo Sandstone1-b07T01-bBiocrustPP0T00T0000usqomkigeca_UPNLHC1% [0n/aLow levelGPS@zAeolian Sands2020PBiocrust400000T0000jhfdb`^\ZXVTJHFDB@1% h10160MidslopeGPS@xNavajo SandstoneT09T0PBiocrustTT0T0000000pnljhfdb`^\ZPNLJFD2&!~2199Low levelGPS@xAeolian Sands2P7001-a00T00T0000ca_][YWUSQOJJHFDB@1% 40n/aLow levelGPS@xNew Alluvium30300300T00T0000_][YWUSQOMKIIGECA?1% 50n/aLow levelGPSJ@xObscured by Soil04000PBiocrust0500000T0000qomkigeca_]YOMKIGC1% 6#20variableMidslopeGPS@xMancos Shale040000T00050000000igeca_][WUSQQOMKIE7+&%0n/aLow levelGPSn@xNew Alluvium040P000500000P0000ca_][YWUSQOKKIGEC?1% 19172MidslopeGPS\@xDakota Sandstone2P0001-a2040000000geca_][YWUSNNLJHFD2&!/7284Low slopeGPS@xMorrison Fm - Brushy Basin Member05P000P1-b030000000ywusqomkigb``^\ZXT1% K22177High SlopeGPS@ xMorrison Fm - Salt Wash Member1-b4000P30200T0000wusqomkigecaa_][YT4(# N23166High SlopeGPS@ xMorrison Fm - Salt Wash Member23000P20200T0000trpnljhfdb`^^\ZXVT4(# >21315MidslopeGPS@ xAeolian Sands00700300000T0000a_][YWUSQOMKKIGECA2&! 15310Low slopeGPS@ xAeolian Sands3P3003T0T00T0000b`^\ZXVTRPNLLJHFDB3'" 0n/aLow levelGPS @ xNew Alluvium0005000500000P0000ca_][YWUSQOKKIGCA?1%  a448High SlopeGPS@xNavajo Sandstone1-b08001-bBiocrustPT0T00T0000usqomkigeca_UPNLHC1% j3201High LevelGPS@xNavajo Sandstone0306T01-bBiocrustPT0T00T0000usqomkigeca_UPNLHD2&!m3168High LevelGPS@xNavajo Sandstone1-b08T01-bBiocrustPT0T00T0000vtrpnljhfdb`VQOMID2&!z0n/aHigh LevelGPSd@xNavajo Sandstone051-bP002Biocrust02T0T00T0000wusqomkigec_UQOMHD2&! 5239High SlopeGPS@xNavajo Sandstone1-b0700PBiocrustPP0P00T0000sqomkigeca_]SQOMID2&!n1276High SlopeGPS@xKayenta Formation304001-bBiocrustPP0P00T0000usqomkigeca_UPNLHF3'"]3155High LevelGPS@xNavajo Sandstone3TP03Biocrust1-bT0T00T0000qomkigeca_]XNLJHFD2&!Z2227High SlopeGPS@xKayenta Formation05020002BiocrustPP0P00T0000vtrpnljhfdb`VRPNJF3'"X1594High LevelGPS4@xKayenta Formation05020002BiocrustPP0P00T0000vtrpnljhfdb`VRPNJF3'"LVAL R ~ F ~2FA few dead branches are found in the blackbrush.A slickrock lump with potholes of happy plants and biocrust define this spot. Some of the Fraxinus branches are dead.Plot is on the edge of a very shallow basin with sandstone outcrops on the western flank & colluvial slopes to the east. Ephedra is growing in clumps, and all the plants are of equal height and distribution, giving the area a pleasing sense of symmetry. Blackbrush shrubs are growing on small mounds. Most litter has blown away.Plot is on a smooth, thick, bank of slickrock with very few pockets of soil & vegetation. Plants are also growing out of deep cracks in the rock.Soils are deep and the area is relatively level. Small pebbles are on the soil surface. Moss is mostly under the trees. Most shrub litter has blown away. Ephedra and Grayia are on sandier hummocks.This site is composed of ledge, lavender, broken bedrock. It is a relatively cooler site, supporting a diverse mix of shrubs. The trees are stunted, and the cliffrose, especially, displays many dead branches from past drought.This is an area of thick soil probably partly derived from the Dewy Bridge member. There is some Navajo bedrock exposed in the drainage bottoms. The surface is pebbly and the shrubs are politely spaced and well groomed.The surface is mostly bare sandstone with a few pockets of sandy soil holding some plants.The terrain is mostly bare rock although there are a few large collections of sandy soil in the area.The terrain is low undulating dunes partly stabilized by annual weeds. Lots of shrubs are dead in this area - mostly Artemisia filifolia.The gently undulating slickrock has many large pockets of sandy soil. Trees are mostly stunted.In this location a pour off on a high cliff drains onto a large dune and has created a wash through the deep sand. All the plants along this corridor are robust and happy. Many weedy annuals are in the understory.v_s / 4 #lWbx/315MidslopeGPS@}Obscured by Soil08000Pmoss1-a0000000000ljhfdb`^\ZXSMKIGEA/#.323MidslopeGPS@}Obscured by Soil080001-bmoss1-a0000000000omkigeca_][VPKIGEA/#-36MidslopeGPS@}Obscured by Soil0600003biocrust, moss1-a00000T0000vtrpnljhfdb]MIGEC?-!,+0n/aLow levelGPSV@}New Alluvium060P000400000T0000ca_][YWUSQOKKIGEC?1% +(0n/aLow levelGPS>@}Mancos Shale07000Pmoss1-bT01-b0000000mkigeca_ZXVQKIGEC?1% *' 0n/aLow levelGPSr@}Mancos Shale060T0Pmoss1-b00020000000ljhfdb`^ZXVQKIGEC?1% )#variablevariableInterfluveGPS$@|Mancos Shale0600001-aP0030000000zxvtrpnlhfd__][YWSE94(('248MidslopeGPS@|Morrison Fm - Brushy Basin Member04P000T020040000000xvtrpnljfd`^^\ZXVR/#'%22172Low slopeGPS@|Morrison Fm - Brushy Basin Member04000PbiocrustP030030000000~|zxtrnlb`^\ZV3'"& /32344MidslopeGPSR@|Morrison Fm - Brushy Basin Member40000P2040000000usqomkigeca__][YWU2&!%>5180MidslopeGPS.@|Morrison Fm - Salt Wash Member0204P0PBiocrust1-bP0P00T0000}{ywusqomh^\ZXTP0$$(22176High SlopeGPS&@|Morrison Fm - Salt Wash Member1-b0600PBiocrust1-a1-b0020000000}ywrmca_]YT4(##@F7131MidslopeGPS8@|Obscured by Soil08T001-aBiocrustPT01-a00T0000trpnljhfa_][QLJHFB0$"D75146High SlopeGPS@ zNavajo SandstoneP0900PBiocrustPT0T00T0000pnljhfdb`^\ZPNLJFD2&!!P1154MidslopeGPS\@|Obscured by SoilT00009biocrustP0000000000omkigeca_][YOKIGEC1%  O0n/aHigh LevelGPS@ zObscured by Soil080001-bBiocrust1-a00P00T0000vtrpnljhfdb]SNLJHD2&!F2110Step in slopeGPS$@zKayenta FormationP0900PBiocrustTT0T00T0000trpnljhfdb`^TRPNJH5)$C$273High LevelGPS@zObscured by Soil071-a001-bPT00200T0000mkigeca_[YWUUPNLGC1% A1454MidslopeGPS@zKayenta Formation0504000PP01-a00T0000kigeca_]XVTRRPNLHD1% 560Low slopeGPS@zNavajo Sandstone06PP0PBiocrustPT00200T0000pnljhfdb^\ZXNLJHFB0$23Low levelGPS@zNavajo SandstoneT09T0TBiocrustT0000000000ljhfdb`^\ZXVLJHFB@."25Low levelGPS@zNavajo Sandstone020700PBiocrustP00000T0000nljhfdb`^\ZXNLJHD@." 217MidslopeGPS@zAeolian Sands1-b040PBiocrust400000P0000kigeca_][YWUKIGEC>/#LVAL l F  X4A hilly area of grey and golden Mancos shale. Piles of sandstone blocks top some of the hills. The Eriogonum shrubs are struggling to leaf out. Dead stems and branches are in nearly all shrubs. The dried skeletons of desert trumpet rattle like wooden chimes in the wind.This plot is V-shaped. The upper, fan-shaped portion (s) is gravelly, & supports most of the vegetation, including all the ELYSAL. The lower, northern, part is a jumble of large sandstone blocks and barren, ball-bearing surface material, along with most of the shrubs. The Elymus clumps are struggling to come back to life, and a few are dead.Large sandstone rocks & boulders have tumbled down onto this clayey slope from above. Small rocks, too, are on soil surface. The lower (northern) end of plot has very little vegetation as it slopes into the wash bottom.The gravelly, shaly soil holds large sandstone blocks fallen down from above. The plants are evenly distributed across the slope. The odor of Selenium is overpowering.This is a fairly level site with slickrock exposures. The rock here is light-colored, fine-grained, and looks conglomerate. All the plants are stunted, growing in cracks or pockets of soil. The Cliffrose and Ash were especially hard-hit by drought displaying many dense stems.Coarse sandstone is fractured into large slabs of bedrock with large broken rocks scattered on top. Pieces of conglomerate and rounded pebbles are embedded into the surface. Plants are stunted where growing in cracks, and more robust in spots of increased soil development.The north end of plot spends a good part of the afternoon in the shade, so more mesic species are there. A few of the trees area dead, as are the Fraxinus.This plot occupies the gentle slopes below the cliff band and into the valley floor. The Atriplex has many dead stems and branches and many of the Sporobolus clumps are now low, grey mounds; dead. The soil surface is a near continuum of moss and biocrust, nearly obscured by the carpeting cheatgrass.6LVAL P d lXHXArea is highly disturbed with poor soil crust development and most of the bunchgrasses have been replaced by cheatgrass.A smooth slickrock expanse with pockets of soil where plants are growing. Soil must be fairly deep, as the plants are not very stunted.The soils here are fairly well-stabilized by biocrust and plants. Some dead stems are in the sand sage. Most shrubs are on small mounds.Death and dying in the shrubs, especially the saltbush. Salsola skeletons are the most prominent feature of this spot. This plot is hilly, with Salsola conventions meeting in the depressions.The southern 1/2 of this plot is quite hilly and supports most of the shrub species other than the saltbush & Ephedra. Most of the dead shrubs are just a pile of flattened, dead sticks & unidentifiable. Salsola skeletons are a prominent feature.At one time, there was probably a "P" of bunchgrasses here. Today I saw a couple bunches with green leaves. Most of the Atriplex shrubs are dead - about 60%. Old Salsola skeletons are the most visually prominent feature. It looks like there wasn't much sand sage here before the drought; only a couple of live ones now.This plot is on a hilly area of deep soils. About 80% of the Artemisia shrubs are dead, and about 50% of the Atriplex also dead. Visibly dominant are the large, tan skeletons of Salsola. Moss and small annuals are coloring the ground surface. Almost all the bunchgrasses are dead. Grasses would be 'present' if all were alive.A 2x2m arm of Salt Wash runs through plot, basically unvegetated. The cheatgrass is robust. The Tamarix has some dead branches. This area may be flooded intermittently.Most of the cheatgrass is growing in the shallow drainages that dissect this plot, as is the sagebrush. The greasewood has suffered some dieback from drought.This plot occupies a level area, with a 3 meter deep and wide wash running through it. The vegetation doesn't change at all in the wash. Pebbly rocks are embedded in the soil surface.pvX M ^ k P ZIJF \8113High SlopeGPS@Dakota Sandstone06PT00PP0030000000hfdb`^\ZVTRPPNLJHD2&!EH14118MidslopeGPS@Mancos Shale051-a000P1-a0030000000jhfdb`^\XVQOOMKID@2&!D S10175High SlopeGPS>@Cedar Mountain Sandstone04P00TMossPP0050000000xvtrpnljfdb`ZXVTRN4(#CM14120High LevelGPS@Aeolian Sands07P1-a01-bMoss, Cryptos1-a00000T0000{ywusqomkigbSNLGEA2&!BJ.3145High LevelGPS~@Aeolian Sands06PP003Moss, Cryptos1-a00000T0000wusqomkigec^OKIGEA2&!AL.variablevariableHigh LevelGPSL@New Alluvium021-a050PCryptos1-bT0T00T0000~|zxvtrmdb`\WSE94(@K?5267MidslopeGPS@Navajo Sandstone061-a0003CryptosPP0T0000000rpnljhfdb`^\SOMKFB0$?NN3238High LevelGPS|@Navajo Sandstone1-b05001-bCryptos1-aP01-b00T0000{ywusqomhfd_VQOMID2&!>Q2226Low levelGPS@New AlluviumPP020PWater07T0T00P0000jhfdb`^\ZXVRKIGCA?1% =W6153High LevelGPS~@Navajo SandstoneP0900PmossP1-a0P00T0000omkigeca_]XVPNLJFD2&!<b variablevariableHigh LevelGPS^@Aeolian Sands02TP005Moss, Cryptos0200000P0000}{ywuqb^\ZXTE94(;s494High LevelGPSx@Navajo SandstoneP08001-aCryptos, mossPP0P00T0000wusqomkigecaRMKIEC1% :R%3277High LevelGPS@@Aeolian Sands050P003Cryptos, mosses1-bP0T00T0000ywusqomkige`OKIGEA2&!91200Low LevelGPS@New AlluviumT0001-amoss090000000000jhfdb`^\ZXVRLGECA?1% 8variablevariableMidslopeGPS@Aeolian Sands00900P00000T0000rpnljhfdb`^\\ZXVTRC72(72230MidslopeGPS@Obscured by Soil6PP01-bbiocrust1-aT01-a00T0000usqomkigb`^YOJHFDB0$65351MidslopeGPS@ }Aeolian Sands06000PMoss, soil crust040000000000usqomkigeca]KIGEC?0$5792MidslopeGPS@Aeolian Sands1-a00700P1-a01-a00T0000igeca_][VTOMMKIEC>/#4339MidslopeGPS@Navajo Sandstone05P00PbiocrustPP00400T0000omkigeca][YWMKIGEA/#30n/aLow levelGPS@}Navajo Sandstone0206001-abiocrust, mossPT0P00T0000zxvtrpnljhfdTOMKGC1% 20n/aLow levelGPS`@ zObscured by Soil0600003biocrust, moss1-a0000000000zxvtrpnljhfaQMKIGC1% 111111MidslopeGPS@}Obscured by Soil0600002biocrust1-b0000000000usqomkigeca\RNLJHD2&!04360High SlopeGPS@}Obscured by Soil080001-amoss1-a0000000000rpnljhfdb`^YSNLJHD2&!fLVAL2Z D *rRolling badland hills bisected by many deep gullies lined with JUNOST. Soils stabilized by moss and scattered pebbles.Vegetation restricted to scattered soil pockets and cracks on this slickrock canyon rim. Soil pockets are stabilized by fairly well-developed cryptos. JUNOST cover too sparse to be a woodland. A township/range marker from 1924 is in NW corner of plot. Sparse community due to the significant exposure of bedrock.Rolling topography with stabilized and active dunes interspersed between petrified (Navajo bedrock) dunes. COLRAM becomes dominant here where soils are deeper. Plot encompasses a small wash where PURMEX and FRAANO occur. QUEWEL more representative of neighboring polygon to the SW, but some crosses over into this polygon. Consistent crypto cover (not well-developed) except on higher dunes. Plants pedestalled.Woody vegetation runs in strips between braided intermittent channels, now cloaked with cheatgrass. Last year's cheatgrass crop bent over by surface flow, and there is debris 1m high in the TAMCHI.Loose blowing sand mounded up into dunes. Many skeletons of shrubs that died in the drought; most shrubs stand up above the ground surface because of wind erosion. No biocrusts - too raw a surface.Plot is typical of this slope that drops from the main park road into Salt Valley. Trees are somewhat dwarfed over shallow bedrock. Surface undulates, but general trend is to the SW. Geology is a mess - all kinds of bedrock cropping out. Substrate is a red sand.This is not a true dune as there are pockets of soil development scattered throughout. The species distribution doesn't seem to be effected. Plants are growing on mounds or else pedestalled out. A rogue juniper found its way up here.A broken Navajo ledge runs through this plot. It looks like most of the bedrock is covered with a shallow layer of unconsolidated Dewey Bridge sandstone, the small rocks nearly creating a pavement. The ash all have dead branches.bLVAL $ | RVegetation is very dense near stream, less so in overflow channels. Vegetation occurs in belts that correspond to the banks of former or present flood channels.A very sandy wash bottom occurs here between the dunes. Lots of die-back on the JUNOST. Dunes less stabilized by moss and cryptos here. ATRCAN and ARTFIL appear to be associated with the wash, not the surrounding community.Small dunes and pedestalled plants mostly stabilized by moss, though some more active. A few Navajo bedrock exposures. Lots of die-back on the JUNOST. Surrounded by petrified Navajo dunes.Variable slope and aspect in this meandering wash with 2-5 meter tall banks on either side. Very sandy-bottomed wash with Navajo bedrock exposures on the wash sides.Pretty homogenous COLRAM community on a long ramp extending W from Navajo domes/petrified dunes. Soils seem pretty shallow, as there are patchy bedrock exposures. Crypto cover is continuous but not well-developed.Very shallow, scattered soil pockets atop fractured sandstone petrified dunes. Soils stabilized by well-developed cryptos. JUNOST mildly to severely stunted and COLRAM also short-statured.A narrow riparian corridor with mature, healthy POPFRE and a mixed shrub/herbaceous understory. Water at the surface in spots and others areas of the creek channel have moist soil. Hawk nest in one POPFRE tree.Fractured canyon rim of extensive Navajo exposure with small slot canyons draining towards the canyon below (to the SSE). Very few soil pockets in plot area and hence very sparse vegetation.A unique community occurring in a large depression surrounded by petrified Navajo dunes. Significant death and die-back on JUNOST, only those closest to bedrock domes (where run-off collects) have green on them. Hummocky dunes in depression, capped with QUEHAV or grass-like form of EPHVIR, are mostly stabilized, but a few are active. Significant moss cover in plant interspaces. FRAANO only occurs at bases of bedrock domes.dLVAL RPoint fell near the top of a badland hill that sloped in all directions. Large dry wash S of center point has PURMEX associated with it. Colorful pebbles, mostly pea-size, cover the ground. Plants slightly pedestalled and stabilized by moss. Geology may actually be gravel deposits.Slope and aspect are an average for plot area which has a variety due to badlands topography. Clay soils with scattered small rock cover. Except near drainages, SARVER and Atriplex shrubs are stunted.Clay soils with scattered fossilized shells on the surface. QUEHAV in plot associated with drainages N of logged point. Lots of die-back on the COLRAM. COLRAM may be transitional from polygon to the N.Soils have more clay in them here and are covered with polished black and grey pebbles (marble-size) and tiny conglomerate rocks. Odd occurrences of QUEHAV scattered about. Could be Dakota geology type here.A swath of grey-blue, small limestone rocks cover the SE quarter of plot, which is otherwise covered in multi-colored pebbles; so plot may capture two different geo types: Dakota and Mancos. COLRAM shrubland continuous in area, despite geology changes. Old road cuts through NE quarter of plot.Despite the diversity of geology types in this area, the COLRAM shrublands are continuous across different geo types. Soils deeper here and more loamy with a scattered coating of small rocks. Very odd small patch of QUEWEL in SE quarter of plot.Clay soils with large chunky and small round rocks on the surface. An old road runs through the NW quarter of point. COLRAM very small, JUNOST associated with gully that bisects the point. May be a geologic ecotone between Mancos and Cedar Mountain.Very diverse geology in not too large an area, and COLRAM shrubland crosses onto several geo types. Soils appear very shallow, as there is lots of bedrock (broken chunks) exposed and plants are stunted. Soil surface is covered in loose rocks (pea to plum-sized). Homogenous community. vOx W \ m*Zx ^^$1200Low LevelMap2@New Alluvium1-b01-a002Moss, biocrust0600000T0000ywusqomkigeaQMKFD?1% ]1210Low LevelMapB@New Alluvium0300201-bmoss/biocrust0400000T0000wusqomkigec_PKIEC?1% \%1848MidslopeMap@Moab Tongue - Curtis Fm04040001Moss, Soil crust010100100T0000~|zvtplZVTRNJ1% [^flatn/aLow levelGPS@New Alluvium0500000500000T0000igeca_][YWUQQOMKIE7+&Zfflatn/aLow levelGPS.@New Alluvium0008000200000P0000igeca_][YWUQQOMIGE7+&Ygflatn/aLow levelGPS:@New Alluvium090T0PWaterP00T0000000nljhfdb`^\ZXQOMKIE7+&Xk1138Low levelGPSF@New Alluvium070P0PWater0200P00P0000jhfdb`^\ZXVRKIGEC?1% Wd1168Low levelGPSL@New Alluvium000900P00000T0000a_][YWUSQOMKKIGCA?1% VY5233High SlopeGPSF@Aeolian Sands000900T00000P0000ca_][YWUSQOMMKIECA2&!Ul2158Low levelGPS@New Alluvium0600002moss020000000000kigeca_][YWSMIGEC?1% Tq2162Low levelGPS@New Alluvium04TP002Water03P0T00P0000ljhfdb`^\ZXTMIGEC?1% Sp5223Low levelGPSf@New Alluvium051-a0002moss02T0P00P0000nljhfdb`^\ZVPLJHC?1% Rr298Low levelGPSN@New Alluvium0400004Moss, Cryptos1-b00T0000000trpnljhfdb`[LHFDB>0$Q}2165Low levelGPS@New AlluviumP0080PWater1-b00P00P0000kigeca_][YWRKIGCA?1% P2122Low levelGPS@New Alluvium090001-amossP0000000000jhfdb`^\ZXVTNIGEC?1% O`1227MidslopeGPS@Obscured by Soil050P002Moss, Cryptos1-aP00200P0000{ywusqomige`QMKIGC1% N0|367Low levelGPS@New Alluvium0601-a003Moss, CryptosP00T0000000trpnljhfdb`^OKIDB>0$M7p3167Low levelGPS@Obscured by Soil07000Pmoss0200T0000000mkigeca_][YUOMKIGC1% L1OvariablevariableLow levelGPS @Older Alluvium0501-b003Moss, CryptosPP01-b0000000zxvtea_ZXTD83(K.QvariablevariableHigh LevelGPS<@Older Alluvium0401-a0Pmoss1-b04000000000}{ywusojdb`[YUE94(J K4185Toe slopeGPS@Mancos Shale080000PT0020000000ca_][YWUQOMKKIGEC?1% I!L2196Low slopeGPS@Mancos Shale09T000PT01-a0000000db`^\ZXVQOMKKIGEC?1% H[7331MidslopeGPS@Cedar Mountain Sandstone05P000PP0050000000nljhfdb`\ZXVVTRPNJ0$G\variablevariableHigh LevelGPSP@Dakota Sandstone05T000PP0040000000{ywusqomigecca_][WE94(LVAL L Sort of an alcove tucked back against an encircling sandstone wall of Entrada. JUNOST occur mostly at the base of the wall and out 30-40 meters. Diverse shrub mixture, due to proximity to wall and variable soil depths (one large bedrock exposure). Soils have light crypto development and some moss cover.SARVER cover in this polygon ranges from sparse to <10%. Soils are stabilized by a consistent cover of moss. Grass cover is patchy. Plants are somewhat pedestalled.Scattered POPFRE trees are a mix of young and mature, and their total cover along Courthouse Wash ranges from 5% to over 20%. Wash running through center of plot has running water 0.5 to 2" deep. Very sandy first terrace is intermittently flooded and dominated by SALEXI shrubs and a few scattered forb species. N of plot ~50 meters (same polygon) is a large area (~1 acre) where TAMCHI have been cut to the ground and slash piles burned, so the photo signature would look quite different now!A sparse shrubland on this high terrace/floodplain of Courthouse Wash. Closer to the terrace edge, SARVER really increases and is mixed with ARTTRI (different polygon). Soils somewhat stabilized by moss cover. Lots of weedy annuals popping up.A 20 meter wide lower terrace just above the sandy wash bottom is dominated by HILJAM and a mixture of forbs. Shrubs mostly on higher banks bordering the terrace. Soils stabilized by a consistent covering of mosses.N half of plot is somewhat ecotonal with the community to the N, increasing grass and ARTFIL cover in plot. Sandy soils are barely stabilized and there is pedestalling of plants. EPHVIR growing in large patches.Point fell in a wash bottom with 3-5 meter tall banks on either side and included the associated wash species: JUNOST, PURMEX, and ARTFIL. N side of wash has a rockier substrate, while S side (which is N-facing) has a moss-covered substrate and sparser COLRAM.RLVAL  8 `&rPolygon is a slab of Moab Tongue fallen from the roof of the Salt Valley anticline when it collapsed. The slab has weathered into a rounded joint pattern with patches of shallow soil. Trees are rooted in joints.A beautiful, thick SPOAIR grassland with scattered, mixed mesic tall shrubs and a fairly sparse but mature POPFRE canopy. Soils are clay and covered with grass litter. Far enough from the stream channel that the SALEXI have disappeared.Large overflow area cris--crossed with furrows. POPFRE all young or seedlings. Fine clay soils are cracked from drying out. Sparse weedy understory.A large disturbed overflow area of the main creek channel. Ground is divided like an agricultural field into furrows. Very weedy area with fine clay soils.On N edge of plot a swath of TAMCHI have been cut to the ground and slash piles burned. POPFRE all young here, many seedlings. Creek running through center of plot is a couple inches deep. Pretty bare understory, probably due to intermittent flooding, which would cover most of plot area.Very sandy and deep wash channel (8-12 m. deep by 6-10 m. wide). Very little growing in the wash bottom except STIHYM and ARTFIL coming down where banks have eroded.Rolling, active dunes with a general SW aspect, facing down-canyon. No crust development at all and litter has mostly all been blown out. Typical dune community.High bench/terrace 10-15 meters above Courthouse Wash that is dominated by SARVER. Lots of dead grass clumps, may be SPOAIR. A couple small surficial drainages cut through plot. Moss cover well-developed on mounds around the shrubs.Mixed age POPFRE stand (from seedlings to mature) with a couple large trees contributing most of the total cover. SALEXI growing in a narrow strip along the banks of the creek, which is several feet deep and ~4 meters wide here. Other shrubs are several meters back from the creek. Plot includes a large strip where TAMCHI have been cut to the ground and slash piles burned.LVAL L < HSite is at the foot of Turret Arch, somewhat shaded by it in the afternoon and also has a shallow drainage running through the point - thus the rich vegetation.What isn't salt encrusted is a silty alkaline sand. Plot is at the point where the valley floor begins to narrow to the entrance to Salt Wash Canyon.Ground is still wet from recent runoff. Plot includes the current active channel. Fine silty sand texture.Surface is silty, with polygonal cracking. Other than the clumping described above, the vegetation is not obviously organized along channels.Grasses occur mostly where Moenkopi washes over the Mancos. Most of soil surface covered by shale fragments.Several small ridges and gullies in plot. South- facing slopes are sparser, but composition is consistent throughout.Ground surface still wet from recent runoff. Phenology more advanced here than in drier parts of the floodplain ( e.g., 625).No obvious reason for change from SARVER to TAMCHI, on the same level, similar soils with polygonal cracks.Plot includes a flowing channel. This bank hasn't flooded this year, last year's leaves are still tightly clustered at the base of each shrub. Sand has been kept bare and mobile by wind.Although close to the current channel, this part of the floodplain feels older. Old, tall, dense TAMCHI form bands along old channels. There are patches of SALEXI also.Center is on the bank of the flowing channel. Wet spp. on/in the bank/channel, drier spp. on low terraces away from the water.Polygonal cracking indicates silty soil.This part of the floodplain is pretty dry. TAMCHI are older, and it has been a while since it has flooded here.This site hasn't flooded recently. There are old anthills in the plot, and widespread moss cover among the cheatgrass. This plot has some floodplain topography, with distinct channels lower than the terraces with the old TAMCHI. Channels here younger TAMCHI, SARVER, and ALLOCC.v` S Q  }J+4u_8298MidslopeGPS@ Navajo Sandstone04P0004biocrust1-a00T0000000sqomkigeca_ZPLJHFB0$t10254High LevelGPS8@Kayenta FormationP0500Pcrust/ mossPP00400T0000xvtrpnljfdb`SQOMIG4(#si5205High LevelGPS@Navajo SandstoneP0500PbiocrustPP00300T0000rpnljhfd`^\ZPNLJFD2&!r`2266High LevelGPS@Aeolian Sands040040TbiocrustP00P00T0000omkigeca_][YOMKGEA2&!qV 4126 high levelGPS@Aeolian Sands080P0Pbiocrust, mossP00T0000000trpnljhfdb`^NLJHFB3'"pU7312High LevelGPS@Aeolian Sands07PP0PbiocrustP00P00T0000mkigeca_][YWMKIGEA2&!oS480 high levelMapV@Navajo Sandstone05PT002biological soil crust1-aT0P00T0000~|zxvtrpniRNLJHD2&!nH%variablevariableMidslopeMapj@Aeolian SandsP0080Pbiological soil crust1-b00T00T0000~|zu^\ZVTRC72(mG4350 high slopeMap@Navajo Sandstone1-a030004biological soil crust1-aP0P00T0000~|zxvtrmVRPNJE3'"lB%1185MidslopeMap@Navajo Sandstone1-a04P01-abiological soil crust02P01-a00T0000}{ytrplUPNLHC1% k?.5330High LevelMap@@ Navajo Sandstone0202T002biological crust021-a01-a00T0000~|zxvqojfTPNLHD2&!j=1145Low LevelMap,@ New AlluviumT006000300000T0000ca_][YWUSQOKKIGCA?1% i<1165Low LevelMap@ New Alluvium0800000200000T0000ca_][YWUSQOKKIGEC?1% h;1165Low LevelMap@ New Alluvium060001-aMoss0300T00T0000ljhfdb`^\ZXTNIGEC?1% g:%variablevariableToeslopeMap@ Mancos Shale030000TT00700T0000usqomkigca_]][YWUQC72(f91variablevariable toeslopeMap@Mancos Shale02000PmossPT00700T0000|zxvtrpnjhfd^\ZXVRD83(e81168Low LevelMap@New Alluvium04000Psalt crust0600000T0000omkigeca_][WKIGEC?1% d31204Low LevelMap@New Alluvium0600000400000T0000ca_][YWUSQOKKIGEC?1% c21275Low LevelGPSx@New Alluvium0009001-a00000T0000db`^\ZXVTRPKKIGCA?1% b/1210Low LevelMapT@New Alluvium020P000800000T0000ca_][YWUSQOKKIGEC?1% a-1218Low LevelMap@New Alluvium020020Pwater0600000T0000ljhfdb`^\ZXTMKIEC?1% `,flatn/aLow LevelMapP@New Alluvium020P000800000T0000igeca_][YWUQQOMKIE7+&_)1170Low LevelMap@New Alluvium1-b0P0Pmoss0800000T0000jhfdb`^\ZXVRLJHFD?1% JLVAL^0 N 8 | j&ZzLots of broken slickrock exposure here, with COLRAM shrubs growing on soil pockets with good crypto development.Point encompasses both sides of a wash ~2m wide. Steeply sloping sides have bedrock exposure and areas of deeper soil covered by COLRAM. Awesome cryptos on the deep soil areas.Point is in a small wash ~2m wide, sandy-bottom with a lot of slickrock exposure on either side. Slope and aspect vary with the sides of the wash, but the wash drains to the west.Rolling slickrock with a scattering of shrubs and bonsai Junipers growing in cracks. Very few soil pockets, but where there is soil, the cryptos are doing great!Rolling domes of Navajo in the polygon, so slope and aspect are pretty variable. Shallow soil pockets have great crypto development and lots of COLROM.Sandy soils well-stabilized by cryptos. A small drainage through plot has a few JUNOST. Some sandier hillocks in the area have QUEWEL and VANSTYDune on the side of this canyon, stabilized somewhat especially on the upper part by crypto development.A few areas where bedrock is poking through, but soil is deep enough to support this sea of blackbrush. Great cryptos!Plot includes a small slickrock tributary canyon and both rims, which are very similar. CERINT are only closest to rim and typical of community in general.QUEHAV only where sand has managed to collect on this windswept bench. Everything else is rooted in bedrock cracks.Biocrust development in early stages in most of polygon. Lots of loose sand.Moss development under shrubs - only rudimentary biocrust development in most of polygon. COLRAM shrubs are robust- 1mm wide, >0.5m tall.This COLRAM field is tucked between long outcrops of Navajo sandstone.Shallow eolian sands over Navajo sandstone.Sand is a mix of loose, blowing and semi- stabilized.Rim of small canyon where soil thins over Navajo slickrock. Biological crusts are well-developed.Oak in pockets of deep sand - other shrubs and trees growing in bedrock crevices.vU[ ) & d_PET322Low levelGPS@Obscured by Soil0500003crypto1-b0000000000qomkigeca_]XPLJHFB0$0n/aLow levelGPS@Obscured by Soil1-b00007Biocrust0200000(t)0000wusqojhfdb`\RNLJHC1% "52124Low levelGPS~@New Alluvium1-a00800PT01-a00T0000geca_][YTRPNNLJFD?1% 73338Low slopeGPS*@Obscured by Soil0800001-b00T0000000hfdb`^\ZXVTOOMKIGC1%  C3104Low slopeGPSh@Morrison Fm - Brushy Basin Member07000Pcryptos1-b001-a0000000}{ywrpni`^\ZXT1% 97165Toe slopeGPS@Morrison Fm - Brushy Basin Member0800001-aT01-b0000000|zxvtrpnige``^\ZXT1% /9167MidslopeGPSN@ Morrison Fm - Brushy Basin Member080000P001-b0000000xvtrpnljeca__][YWS0$/4174Low slopeGPS*@Morrison Fm - Brushy Basin Member0800001-a001-b0000000|zxvtrpnige``^\ZXT1% 44249Toe slopeGPS$@Morrison Fm - Brushy Basin Member090000P001-a0000000ywusqomkfdb``^\ZXT1% 220204MidslopeGPSp@Morrison Fm - Brushy Basin Member080000P001-b0000000zxvtrpnlgecaa_][YU2&!&'3208Low levelGPS@New Alluvium0800001-bP0P0000000db`^\ZXVTRPKKIGEC?1% *,variablevariableLow levelGPSz@New Alluvium03P040Pcryptos1-aP01-a00T0000}{ywrpni`^\XVRD83(>variablevariableLow levelGPS@Navajo Sandstone03041-a01-acryptos1-bP0T00T0000~|zxsjec^ZVD83(E238High LevelGPS@Navajo Sandstone061-a0002biocrust1-bT0T00T0000wusqomkigec^TPNLGC1% ~I3259High LevelGPS6@Navajo Sandstone1007T01-acrypto1-a1-a0P00T0000ywusqomkigb]UPNLHD2&!}T5325High LevelGPS@Navajo Sandstone0502001-a1-aP01-a00T0000qomkigec^\ZUUPNLHD2&!|\h5181High LevelGPS:@Navajo Sandstone071-a001-acryptos1-aT01-b0000000{ywusqomhfd_VQOMHD2&!{c[variablevariableLow LevelGPSd@Navajo Sandstone0303P002biocrust1-aT0T00T0000}{ywupfb`^ZVD83(zeKvariablevariableLow levelGPSh@Navajo Sandstone031-a1-a002cryptos1-bP0P0000000~|zxsjfd_ZVD83(yxb5340High LevelGPSD@ Navajo SandstoneP0900PcryptosT00T0000000omkigeca_][YPNLJFD2&!x:8219High LevelGPS0@ Navajo Sandstone1-a0800Pcrypto1-a00T00T0000trpnljhfdb`[SQOMID2&!w_6248High SlopeGPS$@ Obscured by Soil0700002biocrust1-b00T0000000usqomkigeca\RNLJHD2&!v_16310High SlopeGPS@ Aeolian Sands000701-bbiocrust1-b0000000000usqomkigeca\RMKGEC4(#LVAL  @Broad bench above Courthouse Wash with small hilly microtopography. Cryptos are doing well here.Low, dry mud hills which are somewhat badland-like. A few gypsiferous crystals scattered around, and some small drainages running through where the SARVER congregate.Confusing area for geology, but in any case these hills are somewhat badland-like, very clayey and cracked-looking. Not many cryptos, but a few gypsiferous crystals scattered around. Slope and aspect vary here due to micro-washes- Overall slope and aspect of area are given.Not 100% sure of geology here, but it's clayey cracked/dry soils with an almost badland-like look. There area a few gypsiferous crystals present.Plot is in the clayey hills that scream "Brushy Basin"& or could it be Mancos? The layers are confusing here, but it is definitely the type of environment where you would expect these shrubs. Little gypsum pieces on lower part of slope here (with gray soil), but upper part of slope is tan and has shaly rocks.Broad sandy bench (~50m wide). Very weedy; lots of dead SALTRA around. Not much stabilization from cryptos here. Some of plot is rocky- line may have been poorly drawn here as polygon seems to include community from neighboring polygon.Sandy, wide wash bottom with some rocks scattered around. Bedrock outcrop here seems pretty anomalous. ARTFIL on banks are growing on somewhat dune areas, partially stabilized by cryptos.Shallow, sandy wash bottom with some of the banks made of slickrock and others are dune.Some bedrock exposure and lots of great cryptos. Most of the polygon made up of big ledgy Navajo outcrops.Large area of rolling, fractured bedrock. Soil pockets have well-developed cryptos and lots of COLRAM. Lots of micro-drainages running through the area.This part of polygon has more slickrock exposure and small rocks, and less cryptos than areas farther north. Rolling Navajo domes outside plot to the south.bLVAL (   0JUNOST are big and healthy here, kept happy by all the rain runoff from slickrock above. Cryptos are huge too. Lots of SALTRA litter around, marring an otherwise pristine-looking Woodland.Very wide terrace above and far away from Courthouse Wash. Cryptos are great here! Lots of tumbleweed litter. SARVER are giant and look pretty happyPoint/polygon are the wash banks of the stream, where lots of surface water is present right now. Lots of burned tamarisk stumps behind POPFRE (away from the stream). Area seems pretty disturbed.Sandy terrace high above Courthouse Wash, with great crypto development on the soil. Plot straddles an upper and lower terrace, but both are definitely SARVER.This is a very broad terrace far above and away from Courthouse Wash.. This particular area is pretty grassy and weedy, with not much crust development. Part of plot falls in a pretty bare, open area.Broad sandy terrace high above Courthouse Wash and at least 150m from the main channel, gently sloping towards the wash. Lots of cryptos here. ARTFIL shrubs look half-dead from drought stress.High terrace about 5 meters above Courthouse Wash, with amazing cryptos! Terrace is broad and flat, at least 50 meters wide here.Very wide, shallow wash here with some braided channels. Wash is 10-40m wide, varying through plot. CHRNAU growing mainly in the braided channel area, with PURMEX clinging to edges of wash.This part of the polygon is in a depression surrounded by low hills of Brushy Basin, but I don't think this spot could justly be called brushy basin.Plot is at bottom of Brushy Basin Hills- it also seems like old alluvial deposits here. More crypto development here than other areas with a similar geology that I've seen today.Polygon is on either Brushy Basin or Mancos clay (cracked, dry-looking and pebbly). Small drainage to the east (wash polygon- SARVER), and above me just outside plot to the North is a Dakota (?) sandstone ridge with COLRAM all over it.vV ]  f b l&v~G JvariablevariableLow levelGPS@New Alluvium1-aP02003Moss04P0T00P0000}{ywusqomic_]YWRD83(&2254Low levelGPS~@New Alluvium0P030PWater05T0P001-b0000mkige`^\ZXVRKIGCA?1% &2182Low levelGPSt@New Alluvium05000005T0T00T0000ca_][YWUSQOKKIGEC?1% -6512Low slopeGPS|@Mancos Shale08000TMossT00020000000hfdb`^\ZVTRPJHFDB>0$2<184Toe slopeGPS@Mancos Shale060000PT0040000000b`^\ZXVTPNLJJHFDB>0$,flatn/aLow levelGPS@New Alluvium0500002Moss, Cryptos0300000T0000zxvtrpnljhfbSOMKIE7+&0flatn/aLow levelGPS@New Alluvium0500003Moss, Cryptos0200000T0000zxvtrpnljhfbSOMKIE7+&1flatn/aLow levelGPS@New Alluvium0400002moss, cryptos0400000T0000zxvtrpnljhfbSOMKIE7+&61135Low levelGPS@New Alluvium050T01-bWater03P0P00P0000mkigeca_][YUNIGEC?1% >2155Low levelMap@New Alluvium05T1-a0pWater04P0p00T0000mkigeca_][YUNLJEC?1% =2146Low levelMapd@New Alluvium041-aP0PWater04P01-a00P0000pnljhfdb][YUNLJHC?1% t131Low levelGPSd@Obscured by Soil0300004Biocrust030000000000rpnljhfdb`^ZPLJHFB0$o267Low levelGPS@ Obscured by Soil0300004biocrust0200000P0000rpnljhfdb`^ZPLJHFB0$v0n/aHigh LevelGPS@Obscured by Soil070001-bcrypto0200000T0000sqomkigeca_[SNLJHD2&!y962High slopeGPS@Entrada Sandstone1-a08000TP01-a0000000ljhfdb`^YWUSSQOMID1% {variablevariableLow LevelGPS@Aeolian Sands020060Pcryptos1-b0000000000}{ywusqoja_]YWSD83(19Low levelGPS0@Obscured by Soil0201-a004biocrust0300000P0000sqomkigeca_[QMKFD@."217Low levelGPS@New Alluvium0201-a003crypto0300000P0000omkigeca_][WOKIDB>0$0n/aLow levelGPS|@ Obscured by Soil1-b00006cryptos0200000P0000sqomkigeca_[RNLJHC1% |220Lower MidslopeGPS.@ Obscured by Soil0300004cryptos0300000T0000vtrpnljhfdb^UQOMKG5)$u0n/aLow levelGPS@New Alluvium040001-awater04P0p00T0000mkigeca_][YUNIGEC?1% w0n/aLow levelGPS@@Obscured by Soil0400004biocrust1-b0000000000trpnljhfdb`[QMKIGC1% 0n/aLow levelGPS@Obscured by Soil070001-abiocrust020000000000trpnljhfdb`\RMKIGC1% LVAL 8 DPoint fell on an island with flowing water, several inches deep, in the creek channels on either side. DISSPI growing in a strip right along the banks. Clay soils on the island are cracked from drying out. Diverse shrub mixture.Most of Salt Wash, including plot area, has had running water several inches deep. Lots of cat tracks in the moist sand! TAMCHI have been consistent along the banks with a weedy understory dominated by BROTEC.Salt Wash flows through center of plot and is several inches deep. A wall with several gushing seeps is ~100 meters N of plot. TAMCHI are consistent along the banks and low terraces and have a weedy understory dominated by BROTEC. East side of wash is mostly bare slickrock in this stretch of the creek.2/3 of plot at the edge on the high second terrace ~150m from Courthouse Wash. The other 1/3 of plot is ~6m lower, on the 1st terrace above the wash, and has all the ARTTRI TRI.Slightly rolling microtopography here, with overall area pretty flat. Area has stabilized dune-like appearance, with decent crypto development. Tons of SALTRA litter around. Lots of dieback on ATRCAN, and ARTFIL isn't looking too great either.Gentle dome of Entrada sandstone rising up in a rather odd place in the mouth of this giant alcove. There's a bunch of small rocks scattered around, and a decent soil pocket at the top of the hill deep enough to support a couple QUEHAV and COLRAM shrubs.Rolling duney area with very little cryptos stabilizing the soil. Most shrubs growing on little mounds with some cryptos at their bases.Plot straddles a small, shallow wash (~1m wide) which gently drains this N-facing alcove. Cryptos are large and abundant, and so is the Salsola litter.Wide, very sandy drainage that is so shallow that it's hardly distinguishable as a drainage. Crypto development on the sides of the drainage is great! Lots of SALTRA litter here, but otherwise the place seems very undisturbed.$LVAL  ( *>DExpansive and monotonous SARVER shrubland on this broad valley floor that is stabilized by well-developed cryptos and mosses.Polygon ends to the NW at a huge pour-off with mature POPFRE inhabiting the sandy alcove at the base. Point fell on a fairly steep NE-facing bank covered in mixed shrubs, carpeted with BROTEC, and stabilized by mosses. Wash runs mostly SE through plot, but turns S just outside plot. E side of wash has a much smaller and lower bank with sparser vegetation growing on it.Main wash channel is 2-5 meters below the terraces and has trickling water running, and the banks are mostly line with Muhlenbergia. Small SALEXI patch is unique for the polygon and sits next to a pool. Lots of downed POPFRE branches and trees. POPFRE are mature and have considerable die-back, but are regenerating.Very tall SARVER stand with lots of CHRNAU mixed in. Cover varies, as does litter, from fairly sparse to very dense. DISSPI patch is thick and homogenous, no bare ground exposed there.Clayey soils with scattered small rock cover, some look like gypsiferous crystals. Low hills intersected with drainage channels. Lots of variation in soil color (tan, blue, yellows, etc.).Rolling badland hills with variable cover of small, shaly rock chunks (tan to brown). Sparse shrubland on clayey soils. Hills are bisected by gully drainage channels, where the larger shrubs occur.Fairly dense mixed shrubland on this broad floodplain. Shrubs slightly pedestalled from sheet erosion. Fair amount of moss cover stabilizing soils in shrub interspaces. Plot captured one large TAMCHI situated near the polygon boundary to the N.Sparser mixed shrubland with shrub interspaces stabilized by mosses and covered with emerging BROTEC grasses. A small gully cuts through the W side of plot. One large TAMCHI in plot is invading from the TAMCHI shrubland to the west.Very dense mixed shrubland on this large floodplain. Shrub interspaces are fairly devoid of herbaceous but have well-developed moss cover.LVALVD R :Soils extremely shallow in this area stunting P-J to a height less than 2 meters, except in the wash to the E. Lots of bedrock exposure with scattered soil pockets stabilized by well-developed cryptos and mosses.N of rim was a community on shallower, tan, clayey soils atop fractured white bedrock. Soils pockets are stabilized by cryptos. Some die-back on JUNOST. PINEDU regenerating but not found in the canopy. S of the rim was a S-facing slope on red clayey soils with scattered truck-sized boulders and small rock chunks broken off the rim. Vegetation was very different from that on top of the rim and sparser. Deeper soils and hardly any cryptos on the slope.White slickrock ramp with fractures running E to W and shallow soil pockets stabilized by plants and moss cover. P-J mostly mature, healthy-looking individuals and regenerating nicely.Steep N-facing side of an Entrada dome with a few soil pockets to the E and a narrow band at the base (N), both vegetated with JUNOST/CERMON. Mostly bare sandstone!Very diverse understory! A N-facing alcove surrounded by bare Entrada domes. Duney microtopography with sandy soils and very light crust development in spots. EPHVIR have grass-like form. Vegetation covers are low because so much of plot is sandstone, except alcove bottom where it's all packed in.A large homogenous COLRAM shrubland on top of this plain with rolling microtopography. Scattered small rocks and moss cover stabilize the soils. Shrubs are pedestalled and tiny surficial drainages are common. JUNOST small-statured and look young.ARTFIL shrublands on either side of this broad wash are different polygons. Only vegetation worth noting for this polygon are the forbs.A small meandering wash with some bedrock exposures along the banks and scattered small rock cover in the sandy bottom. Moss cover significant on N-facing bank, which is steeper and less rocky than S-facing bank.Hv> S 4 | UI@o.2132Low levelGPSl@New Alluvium1-b00002Moss, cryptos0600P00T0000trpnljhfdb`\MIGEC>0$+266Low levelGPS @New Alluvium020001-aWater07T0P00P0000ljhfdb`^\ZXTMHFDB>0$+293Low levelGPSj@New Alluvium02000PWater08P0P00T0000igeca_][YWUQJHFDB>0$/296Low levelGPS@New Alluvium020T0PWater08T0T00P0000igeca_][YWUQJHFDB>0$83260Low levelGPS@Aeolian Sands0008001-b00000T0000eca_][YWUSQLLJHDB@1% 52295Low levelGPS@New Alluvium000900P00P00T0000a_][YWUSQOMKKIGCA?1% Cn/an/aLow levelGPS@New Alluvium03T1-b0PMoss, Dark cyano05P0P00T0000|zxvtrpnljhdRPNIGC5)$5variablevariableLow levelGPS @New Alluvium0601-b0PMoss, Cryptos0200T00T0000~|zxvtpa_]XVRD83(<2305Low levelGPS@New Alluvium04T0500PP0T00T0000ca_][YWUSQOMMKIEC?1% =2228Low levelGPSB@Aeolian Sands0P0900P001-a00T0000eca_][YWRPNLLJHDB@1% _25338MidslopeGPS$@Entrada Sandstone008P0PMoss, cryptosP1-a0P00T0000ywusqomkigb`QOMKGE2&!JrollingvariableHigh SlopeGPS@Aeolian Sands020202003moss, cryptos1-aT0P00T0000~|zxsd`^ZVRC72&648MidslopeGPS@Moab Tongue - Curtis Fm031-a0004Moss, Cryptos0200P00P0000~|zxvtrpnlhYUSQLH/#1029MidslopeGPS@Moab Tongue - Curtis Fm1-a07T01-aMoss, Cryptos1-b00T00T0000~|zxvtrpk\WUSOJ1% 528MidslopeGPS@Moab Tongue - Curtis Fm1-b05P002Moss, Cryptos1-b00000P0000}{ywusqomhYUSQMH/#967MidslopeGPS@Moab Tongue - Curtis Fm1-b06001-bMoss, Cryptos1-bT0P00T0000~|zxvtrpniZUSQMH/#n/an/aHigh LevelGPS@Morrison Fm - Salt Wash Member0202T01-bMoss, Cryptos1-b0201-b00P0000{vgb`^ZV6*%572MidslopeGPSr@Moab Tongue - Curtis Fm1-b06001-bMoss, Cryptos1-b00T00T0000~|zxvtrpniZUSQMH/#25354MidslopeGPSJ@Entrada SandstoneP09000P00T00T0000geca_][YWUSQQOMKGE2&!333High LevelGPS\@Entrada Sandstone00603001-a00T00P0000kigeca_][YWRRPNJFD1% 6123High SlopeGPS@Obscured by Soil070001-aMoss, CryptosP000200T0000zxvtrpnlhfdbSNLJHD2&!1225High LevelGPS@New Alluvium000800T00020000000db`^\ZXVRPNLLJHDB@2&!variablevariableHigh LevelGPS@Navajo Sandstone031-a02002Moss1-bP01-a00T0000~ywupjfd`[WE94(LVAL $z @znExtensive SARVER monoculture. Valley floor stabilized by well-developed cryptos and mosses.High terrace intersected by many big ravines (6-10 meters tall and wide). Ravine sides and bottoms are sandy and filled with ARTTRI and tumbleweed skeletons. Terrace community is lightly stabilized by cryptos and has a carpet of BROTEC under the SARVER shrubs.This area was obviously disturbed by historical grazing, evidenced by the abundance of BROTEC and presence of old cow pies. The ground cover values represent the more stabilized bank to the N and the sand dunes to the E and W.Very sandy, slightly duney wash with small rocks lining the main channel. N side of wash is a sheer rock face, while S side is a sand-dune bank 5-7 meters tall.Scattered soil pockets are sandy and downslope more duney (where QUEWEL occurs), but upslope are stabilized by mosses and dark cyano. Most of plot is an exposed bedrock canyon side with basketball to truck-sized boulders scattered about. Some of the CERINT are very large.Sort of a variable polygon, encompassing both active and stabilized dunes and some bedrock exposures. A few standing JUNOST skeletons. Diverse shrub mixture due to a mixture of substrates and proximity to the wash. Crust development is minor, more moss than cryptos.Soils a little deeper and bedrock exposure significantly less than in most of the polygon (from what I've seen of it). Very well-developed crypto cover holds the soils in place. A perfect example of this community type.Shallow soil pockets atop bedrock are stabilized by well-developed cryptos. More bedrock exposure and hence less plant cover, though P-J cover is still significant. JUNOST stunted in the shallowest soil pockets.Point fell near a slickrock wash bottom with sand deposits in grooves. Shallow soil pockets over bedrock are stabilized by well-developed cryptos, though near the wash have sand blown over them. JUNOST stunted in the shallowest pockets.xLVAL "  n 6*DTPolygon definitely covers a rolling, duney area with partial stabilization by light cryptos.Falling dune at the base of a ledgy valley side. Mostly an active dune, though some light moss cover around the shrubs.Extensive SARVER monoculture with understory of well-developed cryptos and mosses.SARVER less dense here, but still a monoculture. Well-developed cryptos and mosses cover most of the soil.Homogenous SARVER-ARTTRI terrace shrubland with a dense carpet of BROTEC and stabilized by moss cover. A couple deep gullies cut through plot, and the other shrubs line the gullies.Point fell at the confluence of Clover Canyon and a side canyon tributary, so there are more pools of water and moist banks. Water in creek is from 3 inches to 2 feet deep in pools. POPFRE mostly young, with a few mature ones intermixed. A lot of Juncus here!Narrow wash channel with water flowing 3-10 inches deep. Much of the EQULAE has not resprouted, so cover values are based on last year's skeletons. POPFRE still look pretty young.Bend in the canyon where the terrace is a little broader and drier. Creek flowing through plot is several to 1 foot deep in spots. POPFRE all young. JUNBAL just along banks, whereas EQULAE growing in thick patches on the terrace.Plot encompasses sandy wash filled with weedy forbs and grasses and the N-facing slope of a dune that rises 8-12 meters. Shrubs are fairly evenly scattered and quite diverse, though dune species are dominant.Very sandy meandering wash bottom sparsely vegetated with ARTTRI. JUNOST seem to be part of a separate polygon and so were not recorded.Narrow canyon bottom with a sandy wash channel 2-4 meters wide and densely vegetated terraces 2-4 meters above the wash. Seems an unusual mix of co-dominant shrubs, but obviously a mesic site with a fair amount of shading. Some of the oak are over 2 meters tall. Point fell at a fork in the canyon where side canyons come in flowing W and NW, then join flowing NW.`vVW  o  u eR3>)222Low levelGPS@Obscured by Soil07000PMoss0300T00T0000ljhfdb`^\ZXTNLJHFB0$(2320Low slopeGPS@Wingate Sandstone021-a0001-a0200400P0000qomkigec_]YTTRPNIE2&!"640Toe slopeGPSh@Obscured by Soil060T001-aT00300T0000igeca_][WUSNNLJHFB0$1076High SlopeGPS,@Aeolian Sands000801-aMoss, cryptos1-a00000T0000ywusqomkige`QLJFDB3'"645MidslopeGPS@ Aeolian Sands09000PMoss1-a0000000000igeca_][YWUPJHFDB>/#598Low levelGPS@Paradox Formation02T0006biological soil crust, moss1-aT01-b0000000~|wusnQMKIGC0$4100Low levelGPS2@Paradox Formation03P0003biological soil crust, moss1-aT0030000000~|xvtoRNLJHD1%  3123Low levelGPSV@Obscured by Soil0700002Moss, cryptosP001-a0000000ywusqomkfdb`QMKIGC1%  470Low levelGPS@Paradox Formation0300003cryptos, moss1-bT0020000000{ywusqomige`QMKIGC0$ 2324Low levelGPSt@Paradox Formation030001-bcryptos, moss1-aT0040000000}{ywusqokigbSNLJHD1% 448Low levelGPS@Paradox Formation03T0003Moss, cryptos1-aT0030000000{ywusqomige`QMKIGC0$3357MidslopeGPS@Entrada Sandstone0202P002Moss, cryptos03P01-a00P0000}{ywusqojhfbSOMKGC0$638MidslopeGPS@Obscured by Soil0500003moss, cryptos020000000000vtrpnljhfdb^OKIGEA/#-4108MidslopeGPS@Aeolian Sands01-a0601-bmoss02T0T00P0000omkigeca_][WQLJFA?0$ee25125High SlopeGPS^@Entrada Sandstone1-b07000P1-b0P00P0000omkigeca_]XVVTRPLG4(#D767High SlopeGPSN@Dewey Bridge Member - Entrada0500001-b1-a00300P0000zxvtrpnlhfa\\ZXVTP1% 53206Low levelGPS@New Alluvium08000002P0T00T0000ca_][YWUSQOKKIGEC?1% /1133Low levelGPS@New Alluvium0400003Moss, Cryptos0300000T0000trpnljhfdb`\MIGEC?1% U30204High SlopeGPS@Entrada SandstoneP08000P1-b01-a00T0000omkigeca\ZUSSQOMIG4(#*1163Low levelGPS@New Alluvium1-b00006Moss, Cryptos0300000T0000usqomkigeca]NJHFD?1% -1165Low levelGPS@New Alluvium0200006Moss, Cryptos0200000T0000trpnljhfdb`\MIGEC?1% /1168Low levelGPS@New Alluvium0200005Moss, Cryptos0300000T0000trpnljhfdb`\MIGEC?1% +1150Low levelGPS@New Alluvium0200005Moss, cryptos0300000T0000trpnljhfdb`\MIGEC?1% LVAL& &tVery duney area with almost no stabilization by cryptos. Microtopography very rolling, but overall area is flat.COLRAM and JUNOST invading from surrounding communities. About a 2-3 acre grassy opening with EPHVIR and HILJAM dominant, but high forb cover as well. Lots of browsing evidence on the grasses.Partially stabilized dune area at the base of fins and narrows. Soils are sandy and relatively deep, though strips of exposed bedrock occur in places. Many dead PINEDU, look beetle-killed, though some are long dead.Area of fins and deep narrows in between mostly filled with large rock jumbles and mesic shrubs and P-J. Aspect is more SE, which may be why no mesic tree species occur here.Red clay rolling hills covered with small shaly rocks and cris--crossed with many deep gullies/drainage channels. PURSTA and FRAANO occur along drainages only. JUNOST somewhat dwarfed, though soils are relatively deep, so probably no due to soil depth. Extensive, fairly homogenous community.Very weedy and sparse section of this extensive SARVER shrubland; also no biocrusts here. The dark band of vegetation that wraps around this alcove is a more mesic area where run-off collects and supports a JUNOST woodland with mesic shrubs in the understory. May not be MMU size, but it's very different than the SARVER shrubland it borders.Extensive homogenous SARVER shrubland with an understory of well-developed cryptos and mosses. Lower terrace has considerably less SARVER and crypto cover, and more of a mixture of shrubs with ARTTRI dominant.A few shallow soils pockets atop bedrock PURSTA and CERINT. Otherwise, most of the vegetation in plot is growing on a steep rock slide strewn with large (truck-sized) and small rocks, and is quite a mixture with nothing clearly dominant. Some old seep activity at the base of the Moab Tongue on the E side of plot. Vegetation limited by the availability of soil.fLVAL   z $Sort of a stabilized dune area, though soils more loamy than sandy, and a physical crust keeps soil from blowing around. Small rock coating consistent throughout polygon. Many of the shrubs look stunted and area N of point is sparsely vegetated. JUNOST invading from polygon to the S on ledgy valley side.Dune at the base of a ledgy valley side with more characteristic dune species on the steeper slope (E side) and lots of COLRAM on the flatter area on top. Very light crusting and moss cover around plants, otherwise looks like an active dune. Slope is an average for plot area.Tan and yellow clay soils stabilized by a diversity of colorful, well-developed lichens and scattered small rock cover. Some Paradox outcroppings in large gully/wash that bisects plot and scattered gypsum crystals. Plants pedestalled.Yellow clay soils stabilized by well-developed cryptos and shaly small rock chunks. An outcropping of Paradox near the wash channel, which bisects plot.Sandier soils with considerably less small rock cover and crypto (barely developed) cover. Plants pedestalled. COLRAM is clearly dominant. One small gully bisects plot.Yellow clay soils stabilized by well-developed cryptos and mosses and small rock cover. Some gypsum crystals scattered about. Plants pedestalled. A couple surficial drainage channels cut through plot.Soils vary in color from red to tan to yellow. Plants slightly pedestalled. Much higher small rock cover and less crypto cover here. A couple deep gullies intersect plot. Clay soils.Yellowish clay soils on badland hills stabilized by well-developed cryptos and an even coating of shaly small rock chunks. Plants are pedestalled. Many small to large gullies cris-cross the area.Sandy wash bottom 2-4 meters wide with banks 4-6 meters tall that have exposed bedrock with moss-covered soil on top. PURSTA is clearly dominant along the banks, but just above the banks the community transitions to one with more COLRAM and QUEHAV.$LVAL $$\6DSandy, somewhat duney area between low Entrada slickrock "hills." Good cryptos in areas where there is soil exposure. QUEHAV growing on Aeolian mounds, and COLRAM gravitating to shallow soil pockets between mounds where there's slickrock exposure.Rolling, duney area with some cryptos stabilizing the sands. Bedrock (Entrada) outcrops at the edges of the dunes- probably in next polygon over.Rolling, duney area with lots of big, healthy QUEHAV and bit, healthy JUNOST. A few little wash channels run through point. Some nice crypto development stabilizing a few of the dunes.Point is mostly slickrock with a few shallow, sandy soil pockets that support vegetation. A couple duney areas with QUEHAV in these soil pockets- no crypto development.Very rocky- lots of chunky bedrock exposures and broken off large (hand-sized) and small rocks. Looks like bonsai-land! Everything is miniature, most of the PJ is under 2 meters tall. COLRAM cover would be higher if individual plants weren't so dwarfed.Rolling topography bisected by gullies, which have outcrops of bedrock (Paradox?). South half of plot especially is covered with diverse, colorful gypsiferous biocrusts. Slope and aspect are an average for the area.Rolling topography bisected by gullies. Slope and aspect are an average for the area. Crypto cover not well-developed, especially compared to areas in South part of this polygon. Plants slightly pedestalled. One half-dead JUNOST in plot. Geology may be Paradox.Some physical crusting, but no real biocrust cover here. An old holding pen and cans and bottles near W edge of plot. HILJAM doing really well here. A couple ATRCAN skeletons in plot. Also many weedy forbs not listed, though total herbaceous cover is still "02."Ledgy canyon side of broken-down bedrock exposures and small cliffy outcrops of bedrock. Lots of shaley small rocks on the ground. Understory fairly sparse and a mixture of species. Trees and tall shrubs are a little stunted. Lots of browsing on ELYSAL.OvA 7 D = >:5($V234MidslopeGPS@Mancos Shale09000PcryptoP0000000000geca_][YWUSQIGECA=/#'PvariablevariableLow levelGPS\@Obscured by Soil080001-acrypto1-a00T0000000~|zxvtrme`^\ZVD83(%g16206MidslopeGPSj@Cedar Mountain Sandstone02T000P1-a0060000000sqomkigea_ZXXVTRPL2&!Ct4256High LevelGPS"@ Aeolian Sands1-aP070Pcryptos1-a00T00T0000rpnljhfdb`^YPNLHFA2&!Dh3244High LevelGPSN@ Moab Tongue - Curtis Fm1-a0800PcryptoPT0T00T0000xvtrpnljhfdbZXVTPK2&!IZ3194High LevelGPS@Moab Tongue - Curtis FmP04040Pcrypto1-aT0T00T0000zxvtrpnljhfaYWUQMK2&!Jl5199High LevelGPS@Aeolian SandsP1-a070Pcrypto1-a00T00T0000qomkigeca_]XPNLHCA2&!H7136Step in slopeGPSb@Entrada Sandstone1-a08P0TwaterPT0T00T0000trpnljhfdb`^WUSQMH5)$GvariablevariableHigh LevelGPS@Entrada SandstoneP09000PT0000T0000zxvtrpnljhfddb`^ZXE94(E4222High LevelGPS@Obscured by Soil0501-a0Pcrypto1-b00P00T0000trpnljhfdb`[SQOJHD2&!B0n/aHigh LevelGPS@Obscured by Soil070001-acrypto020000000000sqomkigeca_[SNLJHD2&!A2330High LevelGPS@Aeolian Sands0500301-acrypto1-b0000000000sqomkigeca_ZRMKGEA2&!?1247High LevelGPS@Obscured by Soil0600201-acryptos1-b0000000000wusqomkigec^UPNJHD2&!b218High LevelGPS@Moab Tongue - Curtis Fm03P020Pcrypto0300000T0000xvtrpnljhfd`XVTPNJ1% a318High LevelGPS@Moab Tongue - Curtis Fm041-b020Pcryptos0200T00T0000|zxvtrpnljhd[YWSNJ1% ^246High LevelGPS&@Aeolian Sands02T070Pbiocrust1-a0000000000qomkigeca_]XNLJFD@1% _0n/aHigh LevelGPS@Aeolian Sands02T070TcryptoP0000000000mkigeca_][YWOMKGEA2&!`839High LevelGPS@ Entrada Sandstone02T060Pcrypto1-a00000T0000sqomkigeca_ZRPNJHD1% c4344High LevelGPSt@Aeolian Sands05T030Pcryptos1-b00T00P0000qomkigeca_]XOMKGEA2&!d679High LevelGPST@Entrada Sandstone1-a08000PT01-a00T0000ljhfdb`^YWUSSQOMID1% 5213MidslopeGPS@Navajo Sandstone030300Pmoss1-b1-a00200T0000trpnljhfb`[VPNLJFB0${46Low levelGPS@Paradox Formation04P0004biological soil crust, moss1-bT01-a0000000~|zusqlOKIGEA."728Low levelGPS@Obscured by Soil0500003biological soil crust, moss1-b001-a0000000}{vtrmPLJHFB0$8LVAL L  8 t~^Deep soils here with very little crypto, and a lot of dead ATRCAN shrubs. Grasses seem to be doing well, though. Lots of SALTRA litter around.Rolling, blowing dunes with only a few patches of slickrock (Moab tongue) peeking through. Very few cryptos here; lots of SALTRA litter around.Rolling, fractured slickrock with veg. growing in joints and shallow soil pockets. Good cryptos where they can get a foothold. JUNOST very stunted here/ bonsai-like.Swells of Moab Tongue with sandy, almost duney areas in between. Very few cryptos.Some good outcroppings of Moab Tongue here and there, but polygon is trying to capture the duney area here it seems. Dunes partially stabilized by some cryptos at their bases and in between dunes.Point falls on the NW side of a shallow slickrock wash that has a few pools of water in it at present. Area slopes gently to wash, and is mainly rolling, unvegetated slickrock.Swirling/ sloping Entrada sandstone here- plot straddles a wash and some Entrada domes, so slope and aspect are variable.Fairly sandy area with most of COLRAM showing slight to moderate pedestalling from wind erosion. A few sandier/ dunier mounds have QUEHAV, and a few JUNOST skeletons around. Odd scattering of small rocks on the soil surface.Lots of dieback on larger bunchgrasses here, and some young shrubby JUNOST scattered about, looking invasive.1/3 of plot has dunes that are 1-2m higher than the lower, flat part of the plot. Surprisingly nice cryptos in the interspaces between dunes; flat part of plot is trashed and weedy-looking with old cow pies around.Weedy sand sheet stabilized by a decent amount of young cryptos. Lots of dead shrubs and bunchgrasses around- drought stress? A few areas of plot have very small dunes with EPHVIR clumps on top.Polygon is long and narrow, between low "hills/cliffs" of slickrock. There are duney areas where QUEHAV is growing, but also lots of slickrock exposure. Decent cryptos where soil is exposed. Old cow pies are around.LVAL : , zN&Lots of small, rough, reddish and white rocks on the surface. Plot covers all slopes and aspects of a series of small hills that have an almost badland-like appearance, with many small drainage channels in between. There may be several geologies mixed together here0 geo map indicates Paradox? Possibly Chinle as well. Cryptos are patchy, but where they exist, they're the crunchy, gypsiferous type.Soils appear deep here, with a scattering of pebbly rocks on the surface. Big, healthy COLRAM here with grass-like clumps of EPHVIR scattered around.Mancos is rockier here than other parts of the polygon. Several small drainages bisect these badland-like hills. It's possible that this could be Morrison- Brushy Basin- Geology is very confusing here.Plot straddles a rocky drainage channel 1-2m wide between steep tan hills of Mancos clay. Plot is near junction with the next polygon, which has a very rock geology type. Lots of dieback on shrubs in the area.Plot straddles the wash, which is wide, braided and shallow here, with a very sandy bottom. The whole area drains gently to the E/SE.Very sparsely vegetated, badland-looking tan clay hills. A few small sandstone and shaley rocks scattered around. Lots of skeletons from Eriogonum inflatum here.Tan, clayey soil here of gently-sloping Mancos hills. A few drainages run through the area, and a few gypsiferous crystals are scattered around.Geology could also be Morrison- Brushy Basin, and there are gray and red areas NW or plot that definitely look like Brushy Basin, but this area is tan clay. Point wraps around this hill so aspect varies, but slope and aspect given above are for majority of plot.Point encompasses the south terrace and low hills on the south side of a wash. Good cryptos on lowest terrace near wash, but very sparse cryptos higher up farther from wash.Geology is confusing here, but Cedar Mountain is my best guess. There's a band of Moab Tongue just above plot to the north. Many 1-2cm sized quartz rocks mixed into the soil here.vh9 E 9 :jm]Nk3266MidslopeGPS8@Moab Tongue - Curtis Fm0207001-abiological soil crust1-bT0T00T0000~|zxvqZUSQMI0$K4278High SlopeGPS @Moab Tongue - Curtis Fm060400Pbiological soil crustPT0T00T0000~|zxvtrpYWUSOK2&!L3206High LevelGPSv@Moab Tongue - Curtis FmP080Pbiological soil crustTP0P00T0000~|zxvtrpnlUSQQMK2&!]i0n/aHigh LevelGPS@Entrada SandstoneT0900PwaterTP0T00T0000nljhfdb`^\ZXQOMKGE2&!\i0n/aHigh LevelGPSL@ Entrada SandstoneP09T0Pbiological soil crustTP0T00T0000~|zxvtrpnljhQOMKGE2&!.33275 midslopeGPSN@ Entrada Sandstone1-aP0001-a0600200T0000pnljhfdb^\XSSQOMKF3'"20n/aLow levelGPS@New Alluvium03000Pmoss0700T00P0000igeca_][YWUQKIGEC?1% -0n/aLow levelGPS@New Alluvium0400002biological soil crust, moss040000000000~|zxvtrpnjMIGEC?1% 10n/aLow levelGPS@New Alluvium050P000500T00T0000ca_][YWUSQOKKIGEC?1% '0n/aLow LevelGPS@New Alluvium000000900000P0000a_][YWUSQOMIIGECA?1% 0n/aLow LevelGPS@New Alluvium05P00Pwater0500T00P0000jhfdb`^\ZXVRKIGEC?1% 1085MidslopeGPS@Obscured by Soil0300501-bcryptosP0000000000sqomkigeca_]TOMIGC1%  z192Low levelGPSz@New Alluvium050020Pcrypto0200P0000000ljhfdb`^\ZXTLJHDB>0$uvariablevariableLow levelGPS<@Obscured by Soil0800001-a001-a0000000~|zxvtrpkigbb`^\ZVD83(#69Low slopeGPS@Obscured by Soil0300005cryptos1-b00P0000000pnljhfdb`^\WNJHFD@."+272Low levelGPS @ Obscured by Soil08000Pcryptos020000000000omkigeca_][WNLJHFB0$*vvariablevariableToe slopeGPS(@ Paradox Formation1-bT001-acryptos1-bT0060000000}ywupgb`^\WD83(6186Low slopeGPS,@Obscured by Soil07000Pcrypto1-b001-a0000000sqomkige`^\WOMKIGC1% 15200MidslopeGPS@Mancos Shale080000PT01-a0000000eca_][YWRPNLLJHFD@2&!xvariablevariableLow levelGPS@Mancos Shale080000P1-a01-a0000000zxvtrpnlge`^^\ZXVRD83(s2120Low LevelGPS @New Alluvium000900PT0P0000000a_][YWUSQOMKKIGCA?1%  n27268MidslopeGPSF@Mancos Shale090000P00P0000000b`^\ZXVTRPNLLJHFD@2&!!q143MidslopeGPS"@Mancos Shale0900001-a0000000000b`^\ZXVTRPNIIGECA=/#LVAL B  ><&This is a rolling duney area, with oak atop the stabilized dunes and the rest of the plants well-distributed.Here, atop the Great Wall, smooth sandstone is interrupted by potholes of vegetation, and the occasional crack-dwelling plant. About half the grass bunches are dead.Huge blocks of sandstone, probably from the Moab Tongue, provide a home for a variety of shrubs and several juniper trees. Several dead stems can be seen in the oak.This plot, near the head of a canyon, consists of a narrow, deep (two meter) drainage and the terrace above. The terrace does not flood, and is infested with cheatgrass. Very old cow pies are around.This area has been disturbed by cows in the past and, more recently, by drought. Most of the shrubs have dead stems, there are a few fatalities, and the understory is dominated by annual weeds.Deep alluvial deposits have turned to annual weeds, mostly cheatgrass. The Juniper and barberry sit close to the monolith base.The litter layer is thick here from all the old grasses and leaves. Many dead stems are in the Tamarisk.This plot includes the water course and the terrace above, and the bare alluvial terrace which is about 12 feet tall above me. The salt cedar is scattered and the shrubs are large. I suppose this first terrace could be flooded occasionally.Plot borders the Salt Valley Road. Has well-developed cryptos in places, and other areas that are more sandy and loose. Some shrubs growing on mounds, whereas others show pedestalling from wind erosion.Point falls in the wide, braided wash area, but is undisturbed enough to have some decent crypto development in places. ERINAU shrubs look healthy, but there is some dieback on the ARTFIL.Point falls in the middle of some low hills which drain into Salt Valley Wash, so slope and aspect vary. Soils have an almost chemical crusting look to them.Really nice cryptos throughout this area, covered with gray lichens, with some yellow and pink.LVAL z ^This plot is in an area where the sandstone ledge is breaking off into large boulders on the slope below, and with soil accumulating on the flats where the slickrock shows through. The aspects are mainly SW & W, with one section of the plot sloping gently NE.Highly dissected hilly slopes are sparkling with glassy mica rock fragments. Many of the Eriogonum shrubs are dead nor have dead branches in them.The Mancos hills have gypsum rocks embedded in the soil.This site experiences rapid runoff from rain, which is caught in pockets of soil in the slickrock, making for exuberant plant growth in these areas. Most ash shrubs have dead tops. A few CERINT shrubs are also dead.Most of the bunchgrass had died. There was 2 -3 percent previously. The sand sage is growing next to the road only. Ephedra is mounded. The blackbrush is large and healthy looking.Large expanse of slickrock on the east side of plot. Plants are growing in patches of soil. The polygon taken as a whole probably has more vegetation than this plot reflects.This plot has areas of blown - up sand mounds, supporting the oak, alternating with more level areas where soil has stabilized, and supporting the trees and blackbrush. Small pebbles dot the soil surface in the low - lying areas.More or less parallel banding of slickrock with plants growing in soil between. Biocrust is well-developed and litter is mostly under the oak and junipers.Slabby slickrock exposures with mounds of soil where plants are growing. Some of the trees are stunted. Some dead branches in the tall shrubs.About half the plot is barren slickrock. The other half is broken slickrock with shallow potholes and cracks where plants are growing. Many ash have dead tops and a few trees have died.Atop the Great Wall, slickrock is the name of he game. This plot has some large broken rocks, shallow potholes with developing cryptobiotic crust and one larger deep pothole with standing water.*vK  V " Q | iasAf14130Low slopeGPSp@New Alluvium0501-a000400000T0000fdb`^\ZXVTRNNLJEC?1% 90n/aLow levelGPS@New AlluviumT00000900000P0000a_][YWUSQOMIIGECA?1% P8280High SlopeGPS@Entrada Sandstone1-a05P001-a0201-a00P0000rpnljhfd_]YTTRPNJE2&!?0n/aLow levelGPS@New Alluvium050P000400000P0000ca_][YWUSQOKKIGEC?1% ?0n/aLow levelGPS@New Alluvium0400000600000T0000ca_][YWUSQOKKIGEC?1% I2236Low levelGPS\@New AlluviumP0001-amoss0800000P0000jhfdb`^\ZXVRLGECA?1% K0n/aLow levelGPS@New AlluviumP007000300P00P0000ca_][YWUSQOKKIGCA?1% F3192Low slopeGPS@New Alluvium0200201-abiological soil crust0400T00P0000}{ywusqomkgPKIEC?1% B4178Low levelGPSZ@New Alluvium020P0pbiocrust0700000P0000mkigeca_][YUKIGEC?1% 331MidslopeGPSD@Morrison Fm - Salt Wash Member04PT003biocrust1-aP00200T0000~|zxvtpnlg]YWUSO/#450MidslopeGPS@Obscured by Soil031-aP003biocrust02P01-b00T0000wusqomkidb`\RNLJEA/# 37MidslopeGPS@Morrison Fm - Tidwell Member040P01-abio-moss1-aT00300T0000}{ywusqmkidZUSQOK-! 0n/aLow levelGPS@Obscured by Soil030T003moss0400T00P0000omkigeca_][WQMKIGC1%  7288High SlopeGPS@Morrison Fm - Tidwell Member030001-abiocrust02T00400T0000}{ywuqomi_ZXVTP2&! variablevariableHigh SlopeGPS&@Morrison Fm - Salt Wash Member1-b04001-bbiocrust1-a1-b00200T0000wrpnjeE94( variablevariableHigh SlopeGPS@ Morrison Fm - Salt Wash Member030300Pbiocrust1-b1-a00200T0000}sqomieE94(/#2225Low slopeGPS&@ Mancos Shale090000PT0P0000000b`^\ZXVTRPNLLJHFD@2&!.22246High SlopeGPSp@Mancos Shale080000PT01-b0000000fdb`^\ZXSQOMMKIGEA3'"@10210High SlopeGPS@Navajo Sandstone1-a070PBiological soil crust1-bT0T00T0000}{ywusqojSQOOKF4(#F231High LevelGPSp@Obscured by Soil0500004biological soil crust, moss1-a0000000000}{ywusnQMKIGC1% U}5280MidslopeGPS`@Moab Tongue - Curtis Fm0207P0PBiological soil crust1-aT0t00T0000}{ywusnWUSQMI0$P3222High SlopeGPS@ Obscured by Soil070P01-aBiological soil crust and moss1-a00T00T0000~|zxsSNLJHD2&!O0n/aHigh LevelGPS@Obscured by Soil02P080Pbiological soil crustP00P00P0000}{ywusqomkiRPNJHD2&!LVAL   @The terrace is quite sandy. The small rocks are in the wash bottom. The terrace is subject to periodic flooding.This plot includes a high wash terrace and a lower one, across the wash. The vegetation doesn't change much, except the ATRCAN is on the high terrace. A lot of sand has been deposited on the wash bend. Many dead grass bunches are on the terrace.Plot landed on a high terrace (15') with the main wash on the east side and an old meander to the west. The drainage so far seems to have many of these high terraces jutting into it. The greasewood and sage are mainly on these terraces, with the cottonwood, willow and rabbitbrush in the wash below.Most of the geology is obscured, with only a few patches of sandstone showing. Soil crust is well developed on deeper soils. A small drainage runs through plot.Limestone exposures are on the south side of wash; sandstone on the north side. Purshia is restricted to the wash edges and sandstone side, as are most of the trees. Shallow gullies lead into the wash. Soil crust is well-developed.About 1/2 of plot is desert pavement with lots of limestone chunks; the rest is obscured by soil with cryptobiotic soil developing. The plant composition doesn t' change, but juniper increases and blackbrush decreases in the pavement area.Plot occupies a shallow basin which has filled in with soil. Many old cow pies and annual weeds attest to past grazing activity. Tall, yellow sticks from last year's annual mustards masquerade as bunchgrasses. A couple of shallow drainages run through plot.The plot encompasses the flat blackbrush plain where soil obscures geology, and the slope below, where the small rocks cover the soil surface. Biocrust is restricted to areas underneath the shrubs. Many dead sticks are in the blackbrush.Broken slabs of sandstone provide pockets of soil for plants, and on the edges of this ridge boulders have broken off and landed on the soil below.LVAL V rv"~Slickrock exposure alternate with areas of soil and biocrust development.This plot occupies a lower terrace above the wash. Biocrust is nearly continuous.This plot occupies the terrace above the main wash. Soils are deep and a narrow gully runs through plot. There is an exceptional amount of dead and down sagebrush stems right at plot center, which are very old. Almost as if an area were cleared intentionally; about a 10 meter by 5 meter circle.Deep soils grow tall shrubs. This terrace is above floodline.Deep soils with lumpy biocrust developing. The ash is growing at the edges of the slickrock exposure and has dead tops. Shallow gullies run through the plot. Soil harbors many chert pieces.The plot encompasses the sandy wash, the level terrace and the sloping bank up to the next terrace. The sloping bank, of shifting sands probably never floods, as the low terrace does.The soil is obscured by cheatgrass and litter. This was a favorite cow hang-out, with all the shade trees. Salsola skeletons and cow pies have gathered together for some unknown purpose. These plants must be enjoying the extra moisture at the monolith base on this NW aspect and in the protected alcove in the northern part of the polygon.This area receives a lot of afternoon sun. The oak is growing where sand and soil have accumulated.This plot represents the community hugging the monolith base on the north and west sides of this side canyon. A convention of Salsola skeletons is meeting here. This area was heavily grazed in the past.This is a very Tall greasewood terrace, well above flood line. Many old cow pies are here.This side canyon was heavily grazed in the past, as evidenced by an abundance of cheatgrass and old cow pies. The trees and tall shrubs cling to the monolith base for the most part, with the short shrubs dispersed throughout the central canyon. Area does not flood. Several big sage shrubs are dead..vE : C ) j3Pzj/RY2276Low levelGPSf@Moab Tongue - Curtis Fm004030Pbiocrust0200000T0000zxvtrpnljhfbXVTPLJ1% .TO6352Low slopeGPS @Moab Tongue - Curtis Fm0203030Pbiocrust0200T00T0000|zxvtrpnljhdZXVRNJ1% -SB357Low levelGPSh@Moab Tongue - Curtis Fm1-b08T0PbiocrustP00T00T0000xvtrpnljhfdbXVTRNI0$,M;2272High LevelGPS@Aeolian Sands00700200T00T0000a_][YWUSQOMKKIGECA2&!+V/3275High LevelGPS@Moab Tongue - Curtis FmP9T0PbiocrustP00000T0000usqomkigeca_USQOMK2&!*WF610MidslopeGPS@ Aeolian Sands00900P00000T0000^\ZXVTRPNLJHHFDB@>/#)[=3265High SlopeGPS$@Moab Tongue - Curtis Fmp09T0TbiocrustTt0t00T0000wusqomkigecaWUSQMK2&!(hn5128Low slopeMapz@ Entrada Sandstone45000PT0T00T0000db`^\ZXVTRPNNLJHFD1% ',0n/aLow levelGPS@ New Alluvium00005water50000000000fdb`^\ZXVTRPIGECA?1% &432MidslopeGPS@Moab Tongue - Curtis Fm0204T002biological soil crust02T0P00T0000}{ywusoXTRPLH/#%332MidslopeGPSj@Moab Tongue - Curtis Fm1-a1-b0004biological soil crust03T0P00P0000}{ywuqZVTRMH/#$731MidslopeGPS&@Moab Tongue - Curtis FmP020005biological soil crust0300T00P0000}{ywusqmVRPNJH/## 431MidslopeGPS8@Moab Tongue - Curtis Fm1-a05T0Pbiological soil crust021-a0P00P0000}{ywrnWUSQMH/#"348Low levelGPS@Moab Tongue - Curtis Fm1-b04P01-bbiological soil crust02P01-a00P0000zxvr[VTRNI0$!520MidslopeGPS@ Moab Tongue - Curtis Fm1-a020004biological soil crust03T0T00P0000~|zxvtpYUSQMH/# +0n/aLow levelGPS@New Alluvium070P000300T00P0000ca_][YWUSQOKKIGEC?1% (0n/aLow levelGPS@ Obscured by SoilP00007biological soil crust0300000T0000~|zxvtrpnljfOKIGEC1% R16112High SlopeGPS^@Obscured by SoilP0000081-b0P00T0000kigeca_][YTPPNLJHF4(#J1200Low levelGPS@Obscured by Soil040020003T01-a00T0000ljhfdb`^YWUQQOMIGC1% A0n/aLow levelGPS@New Alluvium000000900000T0000a_][YWUSQOMIIGECA?1% <1164Low levelGPST@Obscured by Soil040T01-abiological soil crust0600T00P0000}{ywusqomiRMKIGC1% @2206Low levelGPS|@Obscured by Soil050001-abiological soil crust, moss0400T00T0000}{ywusoRMKIGC1% 94200Low slopeGPS@Obscured by Soil071-aT01-abiological soil crust1-aT0T00T0000}{ywusqlUPNLGC1% BLVAL b 4 d,2hThis sandy area has sand actively blowing in or out. Some small mounds are stabilized by vegetation.Deep slots in sandstone fins create a semi-mesic environment.Beavers have flooded this section of the wash. The cattails look dead, but it's possible they just haven't started growing for this season.Ledgy bedrock outcrops ease into a more level area. The serviceberry is restricted to the sandstone ledges.Slickrock exposures are being gobbled up by biocrust.The biocrust is so aggressive here, someday there may be no bedrock exposed at all. The trees and shrubs are somewhat stunted due to shallow soil.Fractured slickrock and large boulders broken away from ledges characterize this spot. Plants are growing in the fractures and wherever soil has developed.This four meter wide wash is scrubbed clean. All the plants are growing at the edges and in cracks in the fractured sandstone above the wash.This plot encompasses the lowest wash terrace and the wash and part of the second terrace on the east. Most of the cheatgrass is below the trees and shrubs. The cottonwoods occupy the wash edge and the first terrace.This slope may be composed of alluvium piled up from below, or eroded Entrada sandstone from above. In either case, the slope has large white blocks on it now, and a draw running down the center. Cheatgrass and sagebrush grow wherever soil is deep enough. Among the boulders the tall shrubs flourish.This plot is in the area leading into Cottonwood Wash, where the stream channel is braided and not so well defined. Tamarix clumps are widely scattered with a good shrub layer below. The evil cocklebur lines the braided channels.The soil is saturated here and I'm thankful for the mounds of dried rush stems to walk on. The Juncus is just beginning to green up, but it forms a continuous carpet here - 100 percent cover. The litter layer is about one half to one foot thick. The tall grasses and willows are growing in clumps and the trees are well-distributed.LVAL 4 :j|lLBedrock exposures alternate with large areas of pebbly soil.Slope and aspect refer to the wash channel. The banks of the wash are sandy and slope gently to the channel. Only a little bedrock is exposed.The terrain is mostly pebbly dirt with just a few bedrock exposures.The surface is mostly pebbly with a few pockets of sand in the area.The soil is covered with coarse angular stones.The slope and aspect are measured down the wash channel. The wash bottom has sandy sections and exposed bedrock. The banks are sloping sandstone. Plants are growing mainly in cracks in the bedrock.Some large pockets of soil have collected in this area, but most of the surface is bedrock and boulders.Giant boulders, tilted bedrock and deep cracks hint at the titanic geological processes that occurred here. Plants are growing in cracks and tiny pockets of soil.The terrain is rugged with giant boulders, cracks, and much bedrock exposed. Plants are growing in cracks and pockets of soil of various sizes.This area is decorated with large sandstone domes - widely spaced. Deep piles of sand have collected between - they are mostly stabilized by plants and biocrust.Sand is actively moving in and out of this area although some spots are stabilized by plants and biocrust.Considerable sand has blown in partially covering the bedrock.Sandy soil covers most of the bedrock in this area.Sand has been blowing in here, covering the slickrock in places. Also, the northerly aspect may be allowing more plant density here.This slickrock area has large pockets of sandy soil.The sand here is pretty well stabilized by plants - especially the Oak that makes large rounded mounds.Slope and aspect are averaged across the undulating slickrock. Plants are growing in cracks and small collections of sandy soil.The slope and aspect are an average of the undulating slickrock. Plants are growing in cracks in the bedrock and small collections of sandy soil.vQ U b  v +X$RfG264Low levelGPSx@ Entrada Sandstone05400PT0T00T0000ca_][YWUSQOMMKIGEC0$F5352MidslopeGPS@ Moab Tongue - Curtis FmP0900PbiocrustPT0T00T0000usqomkigeca_USQOKI0$E0n/aLow levelGPS@ New Alluvium20001-bbiocrust600000T0000ljhfdb`^\ZXVLGECA?1% D$2180Low levelGPS@New Alluvium2000Pbiocrust700000T0000igeca_][YWUSIGECA?1% C0n/aLow levelGPS@New Alluvium20300500000T0000_][YWUSQOMKIIGECA?1% B 189Low LevelGPS@New AlluviumP000Pbiocrust900000T0000hfdb`^\ZXVTRHFDB@>0$A0n/aLow levelGPS@New Alluvium9000TbiocrustP00000T0000igeca_][YWUSIGECA?1% @0n/aLow levelGPSH@New Alluvium90000P00000T0000_][YWUSQOMKIIGECA?1% ?0n/aLow levelGPS6@New Alluvium8000Tbiocrust200000T0000igeca_][YWUSIGECA?1% >!0n/aLow levelGPS@New Alluvium40001-bbiocrust400000P0000ljhfdb`^\ZXVLGECA?1% =0n/aLow levelGPSF@New Alluvium40000500000P0000_][YWUSQOMKIIGECA?1% <0n/aLow levelGPS@New AlluviumT0T0Pwater900000T0000fdb`^\ZXVTRPIGECA?1% ;75172MidslopeGPSx@Navajo Sandstone0503T0PbiocrustPT0P00T0000pnljhfdb`^\ZPNLJFB0$:9[165Low levelGPS @Navajo Sandstone1-bT60Pbiocrust2T0T00T0000omkigeca_][YOMKIGB0$9:v5330MidslopeGPS@Navajo Sandstone6PT0PbiocrustPP0200T0000ljhfdb`^\ZXVLJHFDB0$8<357MidslopeGPS@Obscured by Soil4T20PbiocrustPT0400T0000kigeca_][YWUKIGECA/#7;l14345MidslopeGPS^@ Kayenta Formation04000PbiocrustPT0050000000sqomkigea_][QOMKIE2&!68Y297Low levelGPS@ Kayenta Formation007020TbiocrustPT0T00T0000qomkigeca_][QOMIEC0$5511219MidslopeGPS@ Kayenta Formation1-b0600PBiocrustP0201-a00T0000ywusqomkfd`^TRPNJE2&!4413193High SlopeGPSF@ Wingate SandstoneT6000T40T00T0000geca_][YWUSQQOMKIG4(#3312180High SlopeGPS @ Wingate Sandstone1-b06000P0201-b00T0000qomkigec^\XVVTRPLG4(#2Z0n/aHigh LevelGPSD@Moab Tongue - Curtis Fm003030Pbiocrust0200000T0000{ywusqomkigcYWUQMK2&!1Xg5273High SlopeGPS@Aeolian Sands00601-abiocrust200000T0000nljhfdb`^\ZXNIGECA2&!0Qu4222High LevelGPS|@Moab Tongue - Curtis Fm004040Pbiocrust2T0t00T0000ywusqomkigecYWUQMK2&!TLVAL l $ "4$~PZThis low area is surrounded by dunes and little hills and could possibly have intermittent standing water.This rocky hill seems anomalous in this otherwise sediment-filled valley. The vegetation changes dramatically on the hill.The slickrock fins are widely spaced with large areas of soil between.This site is mostly solid rock with a few opportunistic plants growing in cracks.The sandstone fins have accumulated fairly deep pockets of sandy soil between them.The low, rounded Entrada fins have large pockets of sandy soil between them.The slope was measured down the wash channel. Steep, high canyon walls make this a shady site. The wash bottom is sand in this location. A few small terraces support most of the plants.The terrain is sloping bedrock with fractures running perpendicular to the slope. Plants are growing in the fractures.The silty terrace is eroding into numerous channels in this area. Annual weeds rule the understory.This is the upper terrace of the valley, about 30 feet above the bottom of the wash. The soil is silty. Cheat grass rules the understory.The wash is wide and deep at this site. A few minor terraces are within the main wash.This site is shaded in the afternoon by a tall cliff. The soil is sandy. The understory is carpeted with annual weeds.This area has silty soil eroding into deep, vertical-sided gullies.This silty area is almost a hardpan.This terrace has been eroded with many gullies in the area. Most of the plants are in the gullies. The soil is silty with patches of salt on the surface.This terrace has silty soil and is about 15 feet above the level of the stream channel. Salt deposits are visible on the surface.This large flat terrace is about 20 feet above the stream channel. The soil is silty, drying into geometric patterns. Patches of salt are visible on the surface.The creek channel is about a meter below the vegetated terraces. Part of the plot is a large pond created by industrious desert beavers.Pv\m ) D  o1e0^,`30n/aLow levelGPS@New AlluviumT0T0Pwater900000P0000fdb`^\ZXVTRPIGECA?1% _2192Low levelGPS@New AlluviumP0P0Pwater9T0T00P0000eca_][YWUSQOHFDB@>0$^A322Low slopeGPS,@New AlluviumP1-bP009T0P00T0000a_][YWUSQOMKKIGE@>0$]?0n/aLow levelGPS:@New Alluvium50T00400T00P0000_][YWUSQOMKIIGECA?1% \<0n/aLow levelGPS@New Alluvium20003Biocrust300000T0000igeca_][YWUSIGECA?1% [:0n/aLow levelGPS@ New Alluvium0000PWater0900000T0000hfdb`^\ZXVTPIGECA?1% Z?0n/aLow levelGPS@ New Alluvium50002biocrust300000T0000igeca_][YWUSIGECA?1% Y70n/aHigh LevelGPS\@ New Alluvium70000200000T0000`^\ZXVTRPNLJJHFDB@2&!X,2206Low levelGPS@ New Alluvium50000400000T0000_][YWUSQOMKIIGECA?1% W&0n/aLow levelGPSf@ New Alluvium30004biocrust200000T0000igeca_][YWUSIGECA?1% V#0n/aLow levelGPSX@New Alluvium1-b0800P00000P0000b`^\ZXVTRPNLLJHFD?1% U&2187Low levelGPS^@New Alluvium30003biocrust300000T0000igeca_][YWUSIGECA?1% T)0n/aLow levelGPSP@New Alluvium20005biocrust200000T0000igeca_][YWUSIGECA?1% S(2228Low levelGPS|@New Alluvium30003biocrust200000T0000igeca_][YWUSIGECA?1% R,290Low slopeGPS@New Alluvium22P01-abiocrust2P0T00P0000kigeca_][YWUKFDB@>0$Q)0n/aLow levelGPSh@New Alluvium50000400000T0000_][YWUSQOMKIIGECA?1% P(0n/aLow levelGPSh@New Alluvium30003biocrust300000T0000igeca_][YWUSIGECA?1% O+0n/aLow levelGPS|@New Alluvium30003biocrust300000T0000igeca_][YWUSIGECA?1% N06180MidslopeGPS@Entrada Sandstone06000Tbiocrust0300T00T0000qomkigeca_]YOMKIGC0$M-0n/aLow levelGPS@New Alluvium2000080000000000_][YWUSQOMKIIGECA?1% L26298MidslopeGPS@Entrada Sandstone0202001-abiocrust02P01-a00P0000ywusqomkfdb^TOMKGC0$K57342High SlopeGPS@Entrada Sandstone33001-bbiocrust2T0T00P0000rpnljhfdb`^\RMKIGE2&!JiJ25334High SlopeGPS@Entrada SandstoneP9000T00T00T0000geca_][YWUSQQOMKIG4(#Ij 4138Low slopeGPS@ Entrada Sandstone1-b600Pbiocrust1-bT0T00T0000trpnljhfdb`[QOMKID1% Hg/63MidslopeGPS@ Entrada Sandstone040500PbiocrustPT0T00T0000nljhfdb`^\ZXNLJHD@-!LVALz. 2 , 8 X~l Part of this point is a terrace about six feet high that includes some upland plants.The wash is about 100 feet wide here but still looks like it floods wall to wall.The aspect is down the wash channel. Many of the understory plants aren't doing anything yet, but in season, this should be a lush site.This site is against a north-facing cliff with piles of soil ramping up the side in spots. The site is quite lush and I suspect moisture is seeping into the ground from the cliff. This is an archeological site with a big cave, metates, petroglyphs, and a few cowboy artifacts.This point landed on the edge of a gulley that is cut down 15 feet below the rest of the valley floor. The vegetation is distinctly different in the gulley.This area of the valley is cut by deep gullies. The soil is silty. There aren't too many weeds here.The water table is at or above the surface here, giving the data collector wet feet.This area seems more moist than sites observed south of here. A flowing spring is nearby and water flows in the wash to the west. Plant growth is lush. Many signs of cow activity are present.The soil is sandy and the understory is weedy.This area has sandier soil and is not as flat as the rest of Salt Wash.Cheat grass and biocrust crowd the understory here.The wide sandy wash has steep sloping banks.Biocrust and annual weeds cover the silty soil.The silty soil is covered with biocrust.The soil is silty with patches of salt visible on the surface.This site gets afternoon shade from encircling cliffs that are lined with hanging gardens and springs. All this makes for big happy plants here. The soil is sandy. The Quercus is tree-like.Cheat grass and annual weeds inhabit the understory.The silty soil is full of annual weeds and biocrust.The soil is silty with patches of salt visible on the surface.This sandy hill rises to about 20 feet above the flat valley floor._vd# % > 84KZxn/an/a 0000000000000000;97531/-+)'%%#!?ww0n/aLow LevelGPSf@New Alluvium1-a00301-awater0400000P0000pnljhfdb`^\XQLJFD?1% vv0n/aLow LevelGPS@New Alluvium1-b00301-awater0500P00P0000pnljhfdb`^\XQLJFD?1% uu0n/aLow levelGPS(@New Alluvium0400004Biocrust0200000T0000omkigeca_][WMIGEC?1% tt0n/aLow levelGPS4@New Alluvium1-a1-a020Pwater05P0P00P0000pnljhfdb`^\XQOMID?1% ss0n/aLow levelGPSx@New Alluvium1-bP0401-awater02P0T00P0000pnljhfdb`^\XQLJFD?1% rr0n/aLow levelGPSt@New Alluvium1-aP0401-bwater0300T00P0000pnljhfdb`^\XQLJFD?1% qq0n/aLow levelGPS@New Alluvium1-aP1-a01-awater0600000P0000qomkigeca_]YRMKFD?1% pp0n/aLow levelMapz@New Alluvium1-bP03000400T00P0000fdb`^\ZXVTRNNLJFD?1% oo26298MidslopeGPS@ Navajo Sandstone1-a03001-acrypto1-a0301-a0000000|zxvtrpnigc^VQOMID2&!nn28211MidslopeGPS@ Navajo Sandstone0204001-aP020P0000000mkigeca_][WUUPNLHD2&!mm497Step in slopeGPSv@ Obscured by Soil031-a0003cryptos1-bP0P0000000ywusqomkige`WSQOJF4(#llvariablevariableLow levelGPS@ New Alluvium1-bP0401-bwater0300000T0000}{ywusqokd_]YWRD83(kk0n/aLow levelMap@ New Alluvium1-b0P0pwater0700000P0000kigeca_][YWSLJHFD?1% j946MidslopeGPS@Moab Tongue - Curtis FmP0600Pbiocrust02T0T00P0000vtrpnljhfdb^TRPNJH/#iU55High SlopeGPS@Moab Tongue - Curtis Fm020300Pbiocrust03T0P00P0000xvtrpnljhfd`VTRPLH/#hfl14341MidslopeGPS@Entrada SandstoneP900TbiocrustPT0T00T0000omkigeca_][YOMKIGE2&!gq103MidslopeGPS@Aeolian SandsP0600300T00P0000^\ZXVTRPNLJHHFDB@>/#f,617MidslopeGPS@Moab Tongue - Curtis Fm031-bP003biocrust0200000P0000{ywusqomkigcYUSQLH/#e1023MidslopeGPS@Moab Tongue - Curtis FmP0700Pbiocrust02T0T00T0000xvtrpnljhfd`VTRPLJ1% d70n/aLow levelGPS@New Alluvium40002biocrust300000T0000igeca_][YWUSIGECA?1% c-0n/aLow levelGPS@New AlluviumP000Pbiocrust7000001-b0000ljhfd_][YWUSIGECA?1% b70n/aLow levelGPST@New AlluviumP0005biocrust400000T0000igeca_][YWUSIGECA?1% a,0n/aLow levelGPS@New AlluviumP0T0Pwater800T00P0000fdb`^\ZXVTRPIGECA?1% LVAL h <Narrow, somewhat slotty side canyon of Courthouse Wash. No water flowing here, but sand in the wash is quite damp. ACENEG and CELRET doing well in this cool, sheltered, moist environment.Point falls in an area with lots of large talus, but this canyonside in general is a series of ledges and vertical drop-offs, with some breakdown in between. Cryptos doing well on some of the ledges here.Plot captures part of wash terrace and ledgy bedrock outcroppings with big drop-offs and some large boulders scattered around. Slop gives the overall picture, but canyonside here is more vertical with horizontal shelves.Terrace high above Courthouse Wash, with part of plot falling on a weedy SARVER area and 1/3 of plot falling on a higher slope with ledgy bedrock exposures and a very different community.Gently sloping, sandy terrace with a little slow-moving water in the wash. ELEANG and TAMCHI seem to be choking out all the natives here.It's a jungle in here! Definite bushwhack, and lots of litter so it's hard to see your footing.Shallow pools of sandy soil cover a significant amount of bedrock here.Most of the bedrock here is covered with a varying thickness of sandy soil.The slots and cracks between the fins are fairly deep here with significant soil accumulation. The rare Lomatium latilobum grows here.This duney area is partly stabilized by vegetation. Some spots are blown off exposing red soil - probably Entrada based.This site has quite a bit of sandy soil accumulated. Not much bedrock is exposed.The bedrock here is fractured, but there aren't large slots between the slabs. Plants are rooted in the cracks and shallow pockets of soil.The silty soil is drying into geometric shapes. Large spots of hardpan, possibly compacted by cows, alternate with biocrust.This point is on a terrace about six feet above the wash channel. The trees are large and old. All the plants seem robust.The silty soil encourages biocrust growth.LVAL< P   " This is an area of duney sand, mostly stabilized by vegetation.This is an area of deep sandy soil with no bedrock exposures nearby.This is an area of deep, sandy soil with an occasional outcrop of Moab Tongue bedrock - widely spaced.The terrain is extremely lumpy. Plants are growing between the lumps in pockets of soil. The troughs between the lumps are 10-20 feet deep and 20-30 feet wide.The terrain is mostly solid rock. Plants are growing in pools of sandy soil of various sizes.Large boulders litter the slope. The soil is more clay-like at this site. The junipers are stunted.Large boulders litter the undulating terrain. The soil is pebbly.This is the cliff by the highway where the bighorn sheep hang out - and I'm no bighorn sheep! The site was viewed from below. It is steep to vertical colluvium with small to huge boulders.Nothing too remarkable here- water flowing in the sandy wash, terrace sloping up on either side of it until it is 1-2m above the wash. Lots of leaf litter under the cottonwoods.Stream channel is wide and divides in several places here. Corresponding terraces are also very wide, and pretty weedy.Polygon barely excludes the POPFRE trees lining the wash. Cryptos are doing well on both terraces, but are particularly giant on the upper terrace.Slabs of bedrock exposed in and around the wash. Surface water trickling in some places. QUEGAM stands clinging to the base of the N-facing cliffs here.Outcroppings of slabby slickrock in and around the creek here, but most of the area is deep sand. Terraces are a little higher up from the water here (1-2m), and support a lot of exotics.A few cut tamarisk stumps here and trails runs through plot. Slickrock walls rise up 8-10m on either side- beginning to turn into a canyon here. Lots of POPFRE saplings line the creek.Lots of cut tamarisk stumps around, and quite a few dead CHRNAU and SALEXI. Area seems disturbed.Jvee  p  ^ k*6g!0n/aLow levelGPSr@Obscured by Soil6000040000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPSThe soil is sandy.Obscured by Soil6000040000000000wusqomkigecaa_][YWE% 0n/aLow levelGPSR@ Obscured by Soil6000040000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPSf@ Obscured by Soil7000030000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPSn@ Obscured by Soil0600000300P00t0000geca_][YWUSOOMKIGC1% 2202Low levelGPS4@ Obscured by Soil600003P000000000ca_][YWUSQOMMKIGEC1% 1841MidslopeGPSb@ Wingate Sandstone1-a600Pbiocrust1-a20P00P0000trpnljhfdb`[QOMKID1% 4145MidslopeGPS@Entrada Sandstone04PP00020301-a00T0000ljhfdb`^YWSOOMKIGC0$4206MidslopeGPS@Navajo Sandstone05PP0Tbiocrust02020P00T0000rpnljhfdb`\XNLJHFB0$5202MidslopeGPSt@Entrada SandstoneP0800PbiocrustPT0P00T0000omkigeca_][YOMKIEC0$3179Low slopeGPS@Entrada Sandstone007300P00000T0000fdb`^\ZXVTRPPNLJFD1% 4309Low slopeGPS@@Entrada SandstoneP0800pbiocrustPT0T00T0000pnljhfdb`^\ZPNLJFD1% 5210MidslopeGPS@Entrada SandstoneP08000PT0P00T0000eca_][YWUSQOOMKIEC0$5158High SlopeGPSV@Morrison Fm - Salt Wash Member03060001-a1-a0P00T0000|zxvtrpnlje``^\ZVR2&!3240High SlopeGPS @Morrison Fm - Salt Wash Member040400Pbiocrust02P0T00P0000~|zxvtrpnj`^\ZVR2&!0n/aLow levelGPSX@Morrison Fm - Salt Wash Member06000TbiocrustP030P00T0000}{ywusqomig][YWUQ1% 0n/aHigh LevelGPS~@Aeolian Sands00060Tbiocrust0300000T0000omkigeca_][WMKIECA2&!2147High LevelGPS@ Obscured by Soil06000Pbiocrust0200000T0000rpnljhfdb`^ZPNLJHD2&!~ 4200High LevelGPS@ Obscured by Soil050200002T0T00P0000jhfdb`^\ZXVRRPNLHD2&!}5225High SlopeGPSB@ Moab Tongue - Curtis FmP08T0PbiocrustP00000T0000wusqomkigecaWUSQMK2&!|r7204MidslopeGPS@ Moab Tongue - Curtis FmP08T0TbiocrustP00000T0000usqomkigeca_USQOKI0${%23341MidslopeGPS@ Morrison Fm - Tidwell Member2P000T4030000000pnljhfdb`^\ZZXVTRP2&!z!1078MidslopeGPS@Morrison Fm - Tidwell Member3200PbiocrustP2020000000ywusqomkigecYWUSQO1% ye40149MidslopeMap|@Kayenta Formation04000050P0000000eca_][YWUSQOOMKIGE2&!LVAL 2 L   ( \The soil seems a little more silty here than points south.The soil is sandy. Lots of new grass is popping up here.The soil is sandy with many annual weeds.The soil is sandy here with some immature biocrust.The soil seems loamy with a few pebbles on the surface.Many rodent burrows are in this area. A lot of old tin cans and cowboy litter decorate the site. The soil seems loamy with a few pebbles on the surface.The bedrock here is mostly shattered by the collapse of Salt Valley. The terrain is ledgy and bouldery with random pockets of soil on the ledges. The trees are mostly stunted.Deep gullies snake through this area. Most of the bedrock looks shattered.A little bedrock is exposed here. The soil is sandy. A dry wash bottom about four feet wide snakes through the plot.These fins have cracks 10-15 feet deep but only 2-10 feet wide. Some soil has accumulated in small pools outside the cracks. Peculiar spherical nodules of sandstone litter the surface.Soil has accumulated in this canyon in the form of a climbing dune. Otherwise the plot is solid rock.This site is mostly bare sandstone, but nevertheless some deep soil has accumulated in some areas. This creates a variety of habitats that encourage diversity.Some Moab Tongue sandstone covers part of this plot. The slickrock fins range from being low and mellow to abrupt and lumpy. Soil accumulations range from narrow pockets in crevices to fairly large flat areas.The terrain is a series of ridges formed by eroding hogbacks with much bedrock exposed. Plants are growing in cracks and accumulations of soil. The junipers are stunted.The plot is on the nearly flat top of a of a large hogback. Lots of bedrock is exposed. The plants are growing in accumulations of sandy soil.The terrain is generally flat, but small hogbacks protrude from the valley floor. So the habitat is a mixture of flat deep soil and large boulders piled in tilting slopes.vc' \ c 1 5[ip24257Low slopeGPSN@Moab Tongue - Curtis Fm09P000T0T0000000jhfdb`^\ZXVTTRPNLJ1% /3247Low levelGPS@Moab Tongue - Curtis Fm009P00TP0T0000000ljhfdb`^\ZXVVTRPLJ1% 8,5186High SlopeGPS@Moab Tongue - Curtis FmT0900TbiocrustTT0T0000000wusqomkigecaWUSQMK2&!730n/aHigh LevelGPSt@Morrison Fm - Tidwell Member0400500P00T0000000trpnljhfdb`^^\ZVTP2&!\<396High LevelGPSD@Navajo Sandstone0206T01-abiocrustP00000T0000trpnljhfdb`^TOMKGC1% ^Q1084MidslopeGPS@Navajo Sandstone04P0002biocrustPP00200T0000sqomkigea_][QMKIGC1% cu12192High SlopeGPS<@Navajo Sandstone1-a6000P20P00T0000igeca_][YWUSSQOMKF4(#b2121Low levelGPS@New Alluvium00004asphalt02P0P0000000jhfdb`^\ZXVRIECA??1% d2143Low levelGPS@ New Alluvium040030Pbiocrust02T0T00T0000omkigeca_][WMKIEC?1% f0n/aLow levelGPS@ New AlluviumT0000900T00P0000_][YWUSQOMKIIGECA?1% 0n/aLow levelGPS@ Obscured by Soil5000050000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPSThe soil is sandy and weedy.Obscured by Soil50000500000T0000}{ywusqomkkigecaO% 3242Low slopeGPSx@ Kayenta Formation205001-abiocrust1-aT0T00P0000vtrpnljhfdb]SNLJFD1% 0n/aLow levelGPSR@ Obscured by Soil6000040000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPS@Obscured by Soil5000050000000000ca_][YWUSQOMMKIGEC1% 2191Low slopeGPS@Navajo Sandstone06P00Pbiocrust0200000T0000qomkigeca_]YOMKIGC1% 4222Low slopeGPS@Kayenta Formation303P0Pbiocrust021-a0P00P0000usqomkigec^ZPNLJFD1% 2218Low slopeGPS@Obscured by Soil060T0Tbiocrust03T0T00P0000qomkigeca_]YOMKIGC1% 0n/aLow levelGPSh@Obscured by Soil6000040000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPS@Obscured by Soil60000300t00T0000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPS`@Obscured by Soil4000060000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPST@Obscured by Soil5000050000000000ca_][YWUSQOMMKIGEC1% 0n/aLow levelGPS^@Obscured by Soil6000Tbiocrust40000000000mkigeca_][YWMKIGEC1% 0n/aLow levelGPSt@Obscured by Soil060000040000000000geca_][YWUSOOMKIGC1% LVALN@   r :This site has some bedrock exposures but also some large accumulations of deep soil. The soil is sandy with a lot of sandstone pebbles.The terrain is rough with tilted bedrock and giant boulders. Plants are growing in cracks and small collections of sandy soil. The trees are mostly stunted.This plot has the paved park road running through it, so a good portion of this site is disturbed. Some native plants have been seeded along the roadside to compete with the weeds. These include ricegrass and Sphaeralcea. A lot of Salsola tragus is on the right of way too. Away from the road the soil is sandy and the normal vegetation is intact.This site is a sandy area with a wash running through it. The wash bottom is about three feet lower than the terraces on each side.This site is on two river terraces; one a few feet above the river and another one a few feet above that.The soil is sandy but not too weedy. Lots of dried sticks from last years annual mustards litter the site.The terrain is ledgey bedrock with significant soil accumulation depending on the size of the ledge. This is the first large ledge, just above the valley floor. The soil is coarse sandy.The soil is sandy. The plants are weedy.The soil is sandy and a little more coarse than other sites in the valley.This site is mostly sandy soil with a few bedrock exposures. There's quite a bit of dieback on the blackbrush here.The terrain here includes bedrock ledges and boulders but also large areas of deep soil. Several small drainages meander through the area.This area gets a little moisture from the nearby cliff to the east. The soil is sandy with a few pebbles.The soil is sandy with a smattering of annual weeds.The soil is silty with a few small pebbles. The site is less weedy than others nearby.The soil is silty and hosting many annual weeds.The soil is fine sand with a lot of weeds.The soil is silty here with a hint of biocrust.LVAL H V pHeterogeneous area, seems transitional. Shrubs are pedestalled. Crust development is minor.Fin area with strips of vegetation growing on deep, sandy soils deposited as dunes, which are stabilized by oak cover and trace amounts of cryptos. More PINEDU than JUNOST in the larger area, some very dwarfed, as they are in shallow soil pockets atop bedrock. Plot fell atop a fin, so it captured a lot of bedrock as well as the dunes in between, so it is a good representation of the polygon.Meandering sandy wash bottom lined with JUNOST and a mixed shrub understory. Many rock chunks in the wash. Some parts of the bank are stabilized by moss and cryptos.This site is at the junction of the Moab Tongue and the Entrada and there is water seeping out of the cliff creating jungle-like conditions. Plants are going crazy in size and diversity.This wash is from 20-30 feet deep and from 20-50 feet wide. The bottom alternates between rounded slickrock and sand. Most of the plants are on the sloping sides in cracks and piles of sand.This is a broad shallow wash whose bottom alternates between slickrock and sand. I suspect water flows here rarely since a fair amount of vegetation is established in the bottom.This is an extremely sandy, active dune area. A couple of small spots have some pebbles showing where the sand has blown away. Some of the oak are tree sized.This slickrock wash has a rounded bottom and is about 15-20 feet deep and 40-50 feet wide. What plants there are cling to the sides in cracks or little piles of sand.This wide wash has a slickrock bottom. It is 4-6 feet deep and 20-40 feet wide.This site is mostly solid rock. Plants are growing in cracks and small collections of sandy soil.The Tidwell dirt has a little sand blown in to top it off.This is a most beautiful site comprised of a vast area of gently undulating sandstone with perfect circular pools of sand cradling gardens of pristine vegetation.JvVm 5 |  Q6o2%3157Low levelGPS@Entrada SandstoneP0900Pmoss, cryptosP1-a0T00T0000xvtrpnljhfa_PNLJFD1% $variablevariableHigh LevelGPS @Entrada SandstoneP0900Pmoss, cryptosPT0T00T0000}{ywusdb`^ZXE94(#variablevariableHigh LevelGPS@Obscured by Soil021-a040Pmoss, cryptos02T01-a00T0000}{whfd`[WE94( 2247High LevelGPS^@Navajo Sandstone041-b1-a002moss, cryptos1-bT0P00T0000~|zxvtrpnlgXTRMHD2&!!23High LevelGPS@Aeolian Sands0500003moss, cryptos0200T0000000sqomkigeca_[LHFDB>/#"4167High LevelGPS@Dewey Bridge Member - Entrada051-a00PMossPP00400T0000~|zxvtrpljhf`^\ZUQ2&!n/an/aLow levelGPS@Paradox Formation1-b00007moss, lichens1-bT01-a0000000~|zxvtomkfWSQOMH5)$5165Low levelGPST@Paradox Formation0300003moss, cryptos1-b00030000000|zxvtrpnjhfaRNLJHD1% 4228Low levelGPS@ Obscured by Soil050001-amoss, cryptos0200020000000{ywusqomigeaRMKIGC1% variablevariableLow levelGPS@New Alluvium0500201-amoss1-bT01-a00T0000}{ywrpnic^\XVRD83(3239Low levelGPS@Paradox Formation02T001-abiocrusts1-bT0060000000ywusqomkgec^SNLJHD1% variablevariableLow levelGPSL@Paradox Formation1-a00008lichensP001-a0000000~|zusqofb`^\WD83(8239Low slopeGPSj@Navajo Sandstone0302001-bmoss, cryptos021-a01-a00T0000}{ywusnlgcTOMKGC1% 8266MidslopeGPS@Navajo Sandstone0302001-amoss, cryptos021-b01-b00T0000~|zxvtrmkfbSNLJFB0$7242High SlopeGPS@Navajo Sandstone0303001-bMoss, Cryptos1-b1-a01-b00P0000}{ywupnidUPNLHD2&!+5210High SlopeGPS2@Dewey Bridge Member - Entrada041-b00PMoss, Cryptos1-bP00300P0000~|xvto`^\ZUQ2&!jK9132MidslopeGPS@ Entrada Sandstone006020PMoss, Cryptos1-bP0P00P0000ywusqomkige`QOMIEC0$UvariablevariableLow levelMapN@ Entrada Sandstone03T1-b01-bMoss, cryptos031-b0P00T0000|xidb][WD83(,W22220MidslopeGPSv@Entrada SandstoneP330pbiocrust3T0t00P0000omkigeca_][YOMKIGE2&!-M3241Low levelGPS@Moab Tongue - Curtis Fm06300PT0T00T0000jhfdb`^\ZXVTTRPNLJ1% .&2258Low levelGPSf@Moab Tongue - Curtis Fm0070300PT0T00P0000nljhfdb`^\ZXXVTPLJ1% 62variablevariableHigh SlopeGPS@@Aeolian Sands00900P00T00T0000trpnljhfdb`^^\ZXVTE94(LVAL H 695% of plot is slickrock and the few shallow soil pockets are scarcely vegetated and are near the edge of the polygon.Rolling microtopography on clay soils stabilized by small rock and biocrust cover. Several surficial drainages cut through plot and join in a small gully just S of plot.Meandering wash channel with a low terrace partially stabilized by moss and covered with a mix of typical wash shrubs. Hills beyond low banks are 3-5 meters high. Scattered small rocks in the sandy wash bottom.Rolling microtopography and soil coated with small rocks. Deep wash that bisects plot has an exposure of Paradox bedrock and the banks are stabilized by gypsiferous biocrusts. JUNOST associated with the wash channel.Very diverse, well-developed, gypsiferous biocrusts cover the soil. EPHTOR monoculture with plants pedestalled. Badland topography on this part of the valley floor.Rolling microtopography intersected by small drainages and interspersed with chunky bedrock exposures. Anomalous patch of ARTFIL. A few PINEDU regenerating but none in the canopy.Colorful plot area, geologically-speaking. Small wash that bisects plot has a steep hill to the N with broken-down exposures of tan Navajo bedrock and purple. clayey-looking bedrock exposures below (Chinle?). S half of plot has red, sandy soils somewhat stabilized by crypto cover. May be some Entrada and Dewey Bridge exposures here also.Plot bisected by a fairly deep wash. Geology looks like a mix between Navajo and Kayenta, as there are both white and brick-red exposures of bedrock and soil cover varies between small rocks and cryptos. Lots of die-back on the PURMEX.Mixed geology on this valley side. Most of plot area encompasses broken-down Dewey Bridge formation, but there are several long exposures of Navajo sticking up, and outside plot to the NE ~100 m. are Entrada fins. Red soils with lots of small rock cover. Plants are pedestalled.LVAL  P H(Old cattle fence (JUNOST logs) cuts across canyon through the center of plot. Stabilized dune area on this high terrace above the wash channel in the canyon bottom. JUNOST cover is high in this part of the polygon. PURMEX growing in and along the wash.Stabilized dunes capped with oak on this high terrace (~4 meters tall) above the wash channel. JUNOST and PURMEX mostly along the wash channel. Some die-back on the JUNOST. Cliffy Entrada exposure N of point center.Small canyon between Entrada domes/fins that has a few shallow soil pockets and a couple small dunes stabilized by cryptos and plant roots. The majority of plot and area is Entrada sandstone.Depression area with shallow soils stabilized by cryptos and fairly dense grass cover. Most of plot and area/polygon is Entrada domes and fins.Meandering sandy wash bottom with duney banks to 8 meters high covered with oak. Spotty JUNOST form the canopy and PURMEX growing right along the banks. Some bedrock exposures on sides of wash look like Entrada.Sandy wash bottom with gradually sloping banks stabilized by crypto cover with Navajo exposures intermittently. Mixed shrubs with a spotty JUNOST canopy along the wash banks.Stabilized dune area with lots of moss cover around the shrubs and dunes capped with EPHVIR. Sort of weedy, fair amount of prickly pear and Plantago cover. Soils deep and sandy. Sparsely wooded, but individual trees are large.Slightly sloping area intersected by multiple drainages, along which the majority of PURSTA are located. Ground covered in small rocks. Bedrock exposures along drainages are both Dewey Bridge and Navajo. JUNOST somewhat stunted.Half of plot (S) covered with well-developed gypsiferous lichens, while the other half has more moss and dark cyano cover. PLEJAM patchy in area, which varies between the two association names. A couple large gullies bisect the plot. Slightly undulating topography.0v; 3 r = cH2w%jvariablevariableHigh LevelGPS2@ Obscured by Soil08PT01-aMoss1-b00T00T0000}{ywusqlfa_][WE94(7152MidslopeGPS@Entrada Sandstone020700PMossPp0P00T0000mkigeca_][YWQOMKGC0$4207MidslopeGPS@Aeolian Sands0P0701-aMoss, cryptos1-b001-a00T0000ywusqomkfdb]NIGCA?0$ variablevariableHigh LevelGPSP@Aeolian Sands0601-a01-bMoss1-b00P00T0000}{ywusqlfa_ZXTE94( 3185MidslopeGPS@Aeolian Sands06000PMoss, dark cyano0300T00T0000usqomkigeca]KIGEC?0$5224MidslopeGPS@Obscured by Soil060P01-aMoss, dark cyano1-bT00200T0000~|zxvtrpljhcQLJHFB0$221Low slopeGPS@Moab Tongue - Curtis Fm1-a05P002Moss, cryptos02P0T00P0000}{ywusqomiZVTRNI0$723MidslopeGPS@Moab Tongue - Curtis Fm1-b04P003Moss, cryptos1-b00T00P0000}{ywusqomhYUSQMH/#675High SlopeGPS@Moab Tongue - Curtis Fm1-a0700PMoss, cryptos1-bP0P00P0000}{ywusqomkfWUSQMH/#4325Low slopeGPS@Entrada Sandstone05P0003Moss, cryptos0200T00T0000ywusqomkigeaRNLJHD1% '6318MidslopeGPS@Entrada Sandstone0402001-bMoss, cryptos02T0P00P0000{ywusqomkigcTOMKGC0$-13344MidslopeGPSB@Entrada Sandstone0203001-bMoss, cryptos02P01-b00P0000~|zxvtrmkieVQOMIE2&!6109High SlopeGPS@Moab Tongue - Curtis Fm1-b0500PMoss, cryptos03P01-a00P0000}{ywupnlhYWUSOJ1% n/an/aLow levelGPS@Obscured by Soil02P03002Moss, dark cyano02P01-a00T0000~|zxvqomiWSQMKG5)$85MidslopeGPSl@Moab Tongue - Curtis FmP050003moss, cryptos0200T00P0000{ywusqomkigcTPNLHF-!|3150High SlopeGPS@Morrison Fm - Salt Wash Member03020002Moss, cryptos1-bP01-b00T0000zxvqb^\ZVR2&!z104MidslopeGPSD@Morrison Fm - Salt Wash Member040300PMoss, cryptos1-b1-a01-a00P0000}xvql][YWSO/#y107MidslopeGPS@Morrison Fm - Salt Wash Member0402001-bMoss, cryptos1-bP01-b00P0000}xvto`[YWSO/#x547Low slopeGPS$@Morrison Fm - Brushy Basin Member05P00Pmoss1-a1-a00300T0000}{ywuqoje_][YWS0$(17302High SlopeGPS@Entrada SandstoneP09000TP0T00T0000igeca_][YWUSSQOMIG4(#'3246Low levelGPS@Entrada Sandstone05TP01-bmoss, cryptos03T0T00P0000zxvtrpnljhfbSNLJHD1% &variablevariableLow levelGPS@Entrada Sandstone031-bP003moss, cryptos02T0T00P0000}{whdb`[WD83( LVAL ( ( &>x,Very narrow canyon bottom community and very mesic. JUNBAL forms a dense carpet in patches and oak and Rhus dominate. POPFRE are mature. Some small pools of water.Slightly rolling microtopography of soils atop intermittent bedrock exposures. Soils are somewhat stabilized by cryptos. PINEDU more dominant than JUNOST, though some have die-back. PURSTA and FRAANO also with some die-back.Ledgy hillside below a small cliff band of Entrada. Soils are fairly shallow atop bedrock and stabilized mostly by plant cover and some light crust development.Ledgy hillside with lots of bedrock exposure and fairly shallow soil pockets that support mixed shrubs and mature P-J. Crust development is minor but consistent in soil pockets. Dead PINEDU look beetle-killed.Small wash polygon that captures the dense patches of oak along the banks. ARTFIL and the grasses may be invading from neighboring polygons. Steeper bank (>3 m. high) is stabilized by dark cyano cover.Shallow soil pockets atop bedrock are stabilized by plant cover and well-developed cryptos. Dead PINEDU may have been beetle-killed. PURSTA are large, some more than 2 meters tall.Ledgy Salt Wash exposures on this gentle hillside. Shallow soils are stabilized by well-developed cryptos. Plants are pedestalled. PINEDU in area are all seedling/sapling or otherwise young. Lots of die-back on FRAANO.Small hill with lots of Salt Wash bedrock exposure. Lots of die-back on the FRAANO and PURSTA, and couple young PINEDU look beetle-killed. Soils appear shallow.Broken ledgy hillside with moderate exposure of Salt Wash bedrock. Soils fairly shallow and stabilized by intermittent crypto and small rock cover. JUNOST somewhat stunted. Lots of die-back on the FRAANO and PURMEX.Deep clay soils of the Morrison (blue-grey and tan) are interrupted by small exposures of the Salt Wash, mostly broken down, and small rocks cover parts of the ground, also Salt Wash-derived. Sort of a badland topography. A diverse shrub mixture with 2 clear co-dominants.LVAL * $jRolling microtopography and moss cover around shrub bases. A couple small outcrops of clumpy Navajo bedrock in plot. Few surficial drainages are sandy.Mostly bedrock with plants growing in fractures, except for a couple large soil pockets where most of the vegetation is growing. Soils are sandy and pretty shallow, with some moss around plant bases.Rolling dunes, mostly active, though some are partly stabilized by moss cover. Small bedrock exposure in a wash. Area is full of chipping beds/chert flakes. JUNOST are mature and evenly scattered about.Meandering wash bottom with a steep S bank and low N bank, both stabilized by moss cover. A real mix of shrub species along the wash with a disturbed weedy understory.Pretty much a homogenous COLRAM shrubland except for a component of ARTFIL invading from the dune community nearby. A few large JUNOST are scattered about. Slightly rolling microtopography and no real crust development.Badland-type hills intersected by many surficial drainages. PURMEX and JUNOST occur along the small washes. Crypto cover is light. Soils a little clayey and deep. Die-back on the PURMEX. Geology may be Dewey Bridge.A ravine cuts through center of plot with a sandy wash bottom and some oak along the banks. Most of plot is a mosaic of bare bedrock and shallow soil pockets on top that are stabilized by well-developed cryptos and plant cover.Micro-dunes atop bedrock are stabilized by well-developed cryptos. PURSTA and EPHVIR are both tall and co-dominate the understory.Mainly bedrock with plants growing in the cracks or joints and in the narrow pockets of shallow soil that are somewhat stabilized by cryptos. Oak and CERINT are tall (average = 1-1.5 meters).Rolling microtopography of small dunes stabilized by light crypto development. PINEDU mostly young. Healthy patches of grass invading from the community to the W and SW. A few bedrock exposures, but soils seem fairly deep otherwise.LVAL B "* Sort of a depression area on this high terrace. Very disturbed understory (possibly due to past grazing) dominated by prickly pear. Little moss cover. Salsola skeletons in plot.Canyon side with large bedrock exposures and car to truck-sized boulders scattered about. Soils stabilized by well-developed cryptos and moss.Point fell on a high, sloping terrace 10 or more meters above the wash. A couple deep pools of water in the wash here. POPFRE are mature, but plot captured a more open canopy area. Very disturbed understory, lots of BROTEC. Polygon to the S is in a sheltered alcove and has lots of QUEGAM, some ACENEG, POPFRE, and ARTTRI.Plot captures first and second high terraces 50 meters from the wash channel. SARVER mostly over 2 meters tall. Soils stabilized by moss. Disturbed understory dominated by BROTEC.Broad high terrace with dense tall shrub cover and a disturbed understory. Soils stabilized by extensive moss cover. Wash channel sandy with scattered large boulders and soils are moist at the surface. POPFRE young in plot, but mature individuals are just outside plot.Looks like an abandoned prairie dog town with hardpan silty soil. AT and LB comments: In the middle of Salt Valley in a large playa that is patchily vegetated with ugly weedy annuals. Clay soils have hexagonal cracks. Not sure why this area is so different from its surroundings, could be the basin/low point for Salt Valley where all the salts drain to.Rocky area, lots of bedrock exposed and soils pockets on top are shallow and covered with many small rocks. JUNOST are very dwarfed, many less than 1 meter tall and COLRAM are also dwarfed. Die-back noted on the PURMEX.Beautiful representative of the homogenous COLRAM shrubland. Pavement-like coating of small rocks is evenly spaced. Shrubs are slightly pedestalled. No slope or aspect since this community inhabits a depression area 8-10 acres or more in size. Great views of Salt Valley from here!vU [  g ' v * o*4q288Low levelGPS@Entrada SandstonePPP0Pwater08P0T00T0000ljhfdb`^\ZXTMKIGEC0$c12278MidslopeGPS@ Entrada SandstoneP070001-a020P00T0000ljhfdb`^\ZVQQOMKGE2&! Y2360Low levelGPSb@ Entrada Sandstone02PP0Pwater07P0T00T0000omkigeca_][WPNLJHD1% 2270Low levelGPS(@ Obscured by Soil050020PMoss021-a0P00T0000rpnljhfdb`[WQOMIGC1% flatn/aLow levelGPS@ Obscured by Soil08000TMoss0200T0000000sqomkigeca_[USQOMI7+&128Low levelGPS@Obscured by Soil08000PMoss0200T0000000ljhfdb`^\ZXTNLJHFB0$2353Low levelGPS@Obscured by Soil08000TMoss020000000000mkigeca_][YUOMKIGC1% 2122Low levelGPS@Obscured by Soil0800000200T00T0000geca_][YWUSOOMKIGC1% 43165MidslopeGPSj@Navajo Sandstone1-a040003Moss, cryptos1-bT01-a00P0000~|zxvtrpkigbSOMKGB0$variablevariableMidslopeGPSz@Navajo Sandstone1-b05T01-bMoss, cryptos02P01-a00T0000~|zvgb`^ZUC72(1122Low levelGPS@Obscured by Soil08000TMoss020000000000mkigeca_][YUOMKIGC1% 1142Low levelGPS@Obscured by Soil07000Tmoss030000000000mkigeca_][YUOMKIGC1% Qflatn/aLow levelGPS@New Alluvium080001-aMoss1-a00000T0000sqomkigeca_ZTOMKIE7+&R30323MidslopeGPS<@Entrada SandstoneP0700PCryptos, mossP0201-a00T0000{ywusqomhfb`QOMKGE2&!L220Low levelGPSL@ New Alluvium0TP0PWater09P0T00P0000geca_][YWUSOHFDB@>0$In/an/aLow levelGPSh@New Alluvium08000PMoss02P0000T0000mkigeca_][YUOMKIGC5)$E203MidslopeGPS@Entrada Sandstone02020003Moss, cryptos1-a020P00T0000|zxvtrpnljfaRNLJFB/#@168MidslopeGPS@New Alluvium0301-b002moss0300T00P0000ljhfdb`^\ZXTNJHCA=/#<236Low levelGPSl@New Alluvium0300003moss04T0T00P0000jhfdb`^\ZXVRLHFDB>0$;flatn/aLow levelGPS @New Alluvium1-bP1-a003Moss041-a0T00P0000xvtrpnljhfa]WSQLJE7+&flatn/aLow levelGPS@Obscured by Soil0800000200T0000000mkigeca_][YUUSQOMI7+&"3231High SlopeGPS@Navajo Sandstone030300PMoss1-aP00300T0000sqomkigea_]XRPNLHD2&!/n/an/aHigh LevelGPS:@Obscured by Soil06000PMoss1-a00030000000usqomkigca_ZTRPNLH6*%LVAL@ 6  d This steep-sided, narrow slot provides a home for many plants, all reaching for the sun.This slickrock slope is littered with boulders from the Moab tongue above, which have helped to create pockets of soil for plants to grow.It looks as though periodic flooding occurs here.A small section of the valley floor protected by surrounding Navajo cliff faces. Sandy wash channel cuts through center of plot and is filled with dry tumble weeds. Large ATRCAN are growing mostly near the wash channel and the understory is a disturbed mix of weedy annuals.Extensive grassland on this valley floor with scattered shrubs and deep, fine soils.Extensive grassland on this valley floor with scattered shrubs and deep, fine soils. Anomalous 1-2 acre patch of COLRAM (with KRALAN mixed in) ~200 meters E of here, near the road, but in the same polygon.Extensive grassland on this valley floor with scattered shrubs and deep, fine soils.Extensive grassland on this valley floor with scattered, low cover of shrubs. Deep, fine soils.A mosaic of bedrock exposures and shallow soil pockets that are stabilized by well-developed and diverse cryptos. JUNOST are fairly stunted, especially compared to the tall PINEDU.Ledgy and ramped bedrock exposures with vegetation growing in cracks in the bedrock and on shallow, linear soil pockets atop the bedrock. Soils stabilized by fairly well-developed cryptos. Sort of a depression where point fell, with a small surficial drainage channel separating this polygon from the one to the SW.Extensive grassland on this valley floor, but more weedy here than much of the surroundings. Deep, fine soils.Extensive grassland on this valley floor with sparse scattered shrubs. Fine, deep soils.Extensive terrace with low shrub cover and a disturbed understory.Steep canyonside rockslide area. Rocks range from hand to truck-sized. Sparse JUNOST canopy with a mixed shrub and grass understory, but QUEWEL is dominant.LVAL  R & ,zShallow drainage channels dissect this plot. Biocrust and rocks cover the soil surface.This plot has a small drainage running through and gypsiferous crust on the west facing slopes, which is probably anomalous to this polygon. Many of the smaller grass bunches are dead.Very hard biocrust and colorful lichens cover the soil surface. Small grey (limestone?) rocks are mixed in.Very hard lichens and crust cover the soil surface. Small grey rocks are mixed in.Blown sand has created a duney look to this area woven between the slickrock fins. Most of the plants, esp. the oak, are on top of the mounds. Most litter has blown away. Someone rode their motorcycle through here.Sand has blown into this pocket at cliff base, and is being stabilized by oak and mahogany. This association continues onto the more open area to the NE where slickrock slabs are exposed, although more sparse and with some blackbrush.This shallow and wide wash supports vegetation on its mounded, sandy banks, most litter has blown away, and oak is helping to stabilize the banks.The sandstone stretches away from the cliff to the west, forming parallel fractures and level areas where shallow soils have stunted trees and shrubs.Slickrock fins tower over and fall away from this relatively open garden pocket.The lumpy, ledgy Dewey Bridge slickrock harbors a few plants on the east side of plot, while most of the plants prefer the eroded, western half of plot where there is more soil development. Slabs of Navajo are exposed in this area as well.This plot includes the Tidwell and Salt Wash geologic formations. The Purshia, Fraxinus and Rhus are restricted to the fractured slickrock exposures. Several large chunks of white and grey petrified wood are here.The canyon is very narrow here, about five meters wide, between the slickrock to the north and the colluvial slope to the south. Soil is saturated in places and there are pools of water also.%v4 ( f ` :(BZavariablevariableHigh SlopeGPSv@ gravel deposits04000Pmoss02P0040000000~|zxvtpnlhb`^\ZVE94(2108Low levelGPS0@ Obscured by Soil0800000200P0000000geca_][YWUSOOMKIGC1% 2284Low levelGPS`@Obscured by Soil08000Pmoss1-b00T0000000nljhfdb`^\ZUOMKIGC1% 2288Low levelGPS@Obscured by Soil07000Pmoss0300T0000000mkigeca_][YUOMKIGC1% 296Low levelGPSB@Obscured by Soil08000Pmoss0200T0000000ljhfdb`^\ZXTNLJHFB0$2115Low levelGPS@Obscured by Soil08000Pmoss0200T0000000mkigeca_][YUOMKIGC1% 2161Low levelGPS @Obscured by Soil070P0Pmoss0200P00T0000mkigeca_][YUOMKIGC1% 0n/aLow levelGPS@Obscured by Soil08000Pmoss0200T0000000mkigeca_][YUOMKIGC1% 0n/aLow levelGPS@New Alluvium08000Pmoss1-b00T0000000jhfdb`^\ZXVQKIGEC?1% 362Low slopeGPS@Obscured by Soil04T001-bbiological soil crust02P0020000000~|zxvtpnlhQLJHFB0$375Low slopeGPSP@New Alluvium070001-amoss0200P0000000kigeca_][YWSMHFDB>0$3133Low slopeGPS@ Paradox FormationP00008biological soil crust1-bP01-b0000000}{ywupnlgPLJHFD1% 0n/aLow levelGPSr@ New Alluvium0500003moss, biological soil crust02T0P0000000~|zxvtrpnjMIGEC?1% 0n/aInterfluveGPS@ Paradox FormationP00009biological soil crustP00P0000000~|zxvtrpnljhQMKIGE2&!0n/aInterfluveGPS@Paradox Formation1-a00008biological soil crustPT01-a0000000~|zxvqomkTPNLJE2&!4320Low slopeGPS@Aeolian SandsP050400PT0P00T0000db`^\ZXVTRPNNLJFB@1% 0358Low levelGPS@Obscured by Soil08P00Pbiological soil crust02T0T00T0000~|zxvtrpnljfOMKIGC1% 1262Low levelGPS$@Aeolian Sands1-aP0701-abiological soil crustPT01-a00T0000~|zxvtomkiRMKGE@1% 8198MidslopeGPS,@Dewey Bridge Member - Entrada020600Pbiological soil crustPT00200T0000~zxvt][YWSO0$k0n/aLow levelGPS@Entrada Sandstone1-b07T0Pbiological soil crust1-bP0T00P0000}{ywusqojSQOMID1% 13262High SlopeGPS@Dewey Bridge Member - Entrada1-b060001-aP01-b00T0000~|zxvtrpkigbb`^\XS4(#l0n/aLow levelGPS@ Entrada Sandstone1-b08T00PT0P00T0000igeca_][YWUSSQOMID1% 3207High LevelGPS@Morrison Fm - Salt Wash Member1-b0600Pbiological soil crust1-a1-a00200P0000}xa_][WR2&!LVAL F  f:fH2@Abundant regeneration in the winterfat. Lots of old Descurainia sticks are trying to look like old grass inflorescences.Small pebbles and chunks of chert and larger rocks are on soil surface. Much of the litter has blown away and some shrubs are pedestalled.Lots of cheatgrass here, and Descurainia masquerading as old grass inflorescences. Most of the shrubs are on the north half of plot. Ephedra patches are short and hiding among the herbs.There are several burrows at this site. Many very old dead bunchgrass clumps here.This area is riddled with small to medium - sized burrows. It appears that many very old dead bunchgrass clumps are here. Who knows which beauty they once were?Deep, sandy soils here. A few dead grass bunches, probably ricegrass.This spot has experienced some disturbance between cowboy activities and burrowing animals.Deep and rocky soil makes up this rocky hill in the valley.An area about six meters round was disturbed by a medium-sized burrowing group of animals at one time. Deep soils. Several bunchgrass clumps are dead.Many dead bunchgrasses here- probably ricegrass.Deep soil and a sort of gently rolling terrain in this wide valley. There are a few dead bunchgrasses around, but most are doing well.All the plants look healthy here.Bunchgrasses are doing really well here. Blackbrush is sneaking in from polygon to the west.A shallow, broad, sandy wash runs through plot, varying from three to ten meters wide. This is where the sand sage and Purshia live.This area is uniform in its patchiness of species, not too many dead bunchgrasses here.The annual weeds try to fill up the spaces between shrub patches. A few Sporobolus bunches have died, but most are doing alright.Small drainages dissect west side of plot. Small rocks are embedded in soil. Salsola skeletons are caught in the shrubs.The terrain is rolling here. Nearly all the larger bunchgrass clumps are dead- ricegrass and dropseed. The Hilaria is doing well. Small annual weeds are greening up.^vZ  3 f  ^*mn@2184Low slopeGPSh@Obscured by Soil07000PCryptos020000000000pnljhfdb`^\XOMKIGC1% +p6240MidslopeGPS,@Obscured by Soil06T00Pbiological soil crust02T01-b00P0000~|zxvtrmkieNLJHFB0$3,26148High SlopeGPS"@Morrison Fm - Salt Wash Member1-a1-a000P0701-b0000000}{ywusqljfddb`^YT4(#4 5106High SlopeGPS@Morrison Fm - Tidwell Member04T00Pbiological soil crustP0300300T0000{yus\ZXVTP2&!51170MidslopeGPS@Morrison Fm - Tidwell Member04T000P1-a0040000000vtrpnljhdb][[YWUSO1% 12154MidslopeGPS@ Obscured by Soil05PT003biological soil crust02T0T0000000}{ywusqomkgPLJHFB0$00n/aLow levelGPS@ Obscured by Soil080P001-bT0T00T0000hfdb`^\ZXVTOOMKIGC1% :(2300High LevelGPS@Moab Tongue - Curtis FmP08P0Pbiological soil crust1-a00T00T0000}{ywusnWUSQMK2&!Z53105MidslopeGPS8@Navajo Sandstone1-b03P003biological soil crust1-aT01-b00P0000~|zxsqojSOMKGB0$Y)1090MidslopeGPSt@Dewey Bridge Member - Entrada031-b00Pbiological soil crust1-a1-a00300T0000{v_][YTP1% X 15116MidslopeGPS@Dewey Bridge Member - Entrada041-a000PP00400T0000xvtrpnljfdb``^\ZUQ2&!`0n/aLow levelGPS@Obscured by Soil0701-a0Pbiological soil crust02T0T00T0000}{ywusqomiRPNIGC1% _0n/aLow levelGPS0@Obscured by Soil0800000200T00T0000geca_][YWUSOOMKIGC1% ]0n/aLow levelGPSN@Obscured by Soil00080Pbiological soil crust02T0T0000000~|zxvtrpnljfOMKGEC1%  g0n/aLow levelGPS\@New Alluvium08000002T0P00P0000ca_][YWUSQOKKIGEC?1%  h0n/aLow levelGPS(@New Alluvium00P000900P00T0000a_][YWUSQOMIIGECA?1%  0n/aLow levelGPS@Obscured by Soil0800000200P0000000geca_][YWUSOOMKIGC1%  variablevariableHigh SlopeGPS@gravel deposits0500001-bP0030000000}{ywusqokigbb`^\ZVE94( 1116Low levelGPSx@Obscured by Soil0700000300T0000000geca_][YWUSOOMKIGC1% 1235Low levelGPS@Obscured by Soil0800000200T0000000geca_][YWUSOOMKIGC1% 0n/aLow levelGPSH@ Obscured by Soil0700000300T0000000geca_][YWUSOOMKIGC1% 0n/aLow levelGPS@ Obscured by Soil0700000300T0000000geca_][YWUSOOMKIGC1% 2282Toe slopeGPS@ Obscured by Soil070001-amoss02T0P0000000pnljhfdb`^\XRMKIGC1% TLVAL | . (xxThe wash running through this plot has some bedrock and all rocks and the big sage in it. Some spots are hardpan on the terrace. Lots of Salsola and cheatgrass litter here, along with past grazing.This tiny polygon is on a stream terrace that has experienced erosion, cows and weeds.This huge expanse of fairly level, lumpy slickrock has pockets of soil for plants and biocrust. Trees are stunted due to shallow soil depth.Large slabs of slickrock are exposed near the edge of the dry sandy wash which runs through plot. Biocrust is well developed wherever soil has accumulated.This upper slope below the cliff receives lengthy afternoon shade. Still, many dead stems are seen in the tall shrubs and trees. This area has ledges and drainageways. Soil is pebbly.Most of the juniper here is dead or has many dead branches. Soil is pebbly with ledges of bedrock and shallow drainages. Most of the blackbrush is on the gentle slope below the ledges (which are at the cliff base).A sandy wash runs through plot, where the Chrysothamnus and Purshia live. Some Ephedra and oak are sneaking in from adjacent polygon. Many grass bunches are dead (SPOCRY and STICUM ?) Many dead stems in shrubs and a few dead shrubs.This plot is on the west side, next to the new highway. It is in the Park! It is a stabilized sand sheet with plenty of Salsola and cheatgrass litter.This plot lies between the old entrance road (ortho photo) and the new one. It is very sandy here, but more or less stabilized by vegetation and some biocrust, many old Salsola and skeletons abound. More sand sage is found in the northern part of plot and polygon where a giant culvert drains.This high terrace burned several years ago, but the Tammy's didn't care and have returned. This particular spot has several campsites and an unpaved road running through it.A veritable carpet of Cyperus litter covers the ground. The tamarisk is young and well-spaced. On high runoff years, this terrace probably floods.LVALb Z tLow rolling hills of Paradox Formation covered with lovely gypsiferous crusts that make me feel guilty for being here!Wide-open, windswept valley floor which was obviously grazed in the past. Cryptos starting to recover a bit.Gently sloping hills of Paradox formation, covered with lovely, crunchy crust. I feel bad for walking through it!Gently sloping hills of Paradox formation covered with crunchy, gypsiferous crusts.Low, rolling Paradox hills which gently slope toward Salt Valley Wash. Crusts are big and crunchy here.Low, rolling hills covered with obviously gypsiferous crusts. Small drainages bisect the area.Plot gently slopes toward a wash, which runs through the N end of plot. Area made up of low, rolling hills.Plot mainly falls on sandy (though not very duney) areas with very little crypto development. ~1/3 of plot is on a rockier hillslope, with no cryptos and many pebbly rocks covering the surface.Duney area sloping toward a wash that drains into Salt Valley. Pretty good cryptos stabilizing most of the dunes here.Fairly unremarkable COLRAM community. A few invading JUNOST are scattered around, but most are in neighboring polygons. Robust COLRAM shrubs and stumpy, almost grass-like EPHVIR.This sand sheet slopes down to Willow Springs and the canyon head. Soils are deep and plants are mounded. Cottonwood is sneaking up from the canyon.Huge sandstone blocks intermixed with smaller pieces define this slope. Plants are growing in cracks and wherever the rocky soil is more stable.This plot is at the juncture of the Tidwell and Salt Wash. Huge blocks of sandstone are jumbled on the soil surface. The ash and skunkbrush are only growing out of sandstone cracks. Soil is very rocky with small rocks.Hot, dry and rocky soil best describes this strip of red soil. Large boulders from the Salt Wash Sandstone and pretty chert chunks are scattered throughout the area. A few shallow gullies run through plot.vW ` ^ ` z8DE>42231High LevelGPSL@Obscured by Soil070001-bcrypto1-a00P0000000trpnljhfdb`[SNLJHD2&!33318High LevelGPS@Entrada Sandstone1-b1-a040Pcrypto1-aP01-b00T0000{ywusqomhfd_WUSOJE2&!21278High LevelGPSL@ Obscured by Soil0701-b0Pbiocrust1-a00000T0000vtrpnljhfdb]SQOJHD2&!15200High SlopeGPS@ Entrada Sandstone06PP0Pcryptos1-b00P00T0000sqomkigeca_ZQOMKIE2&!03243High LevelGPST@ Entrada Sandstone051-a1-a0Pcrypto1-b00P00P0000xvtrpnljhfd_WUSNIE2&!/3205High SlopeGPSd@ Obscured by Soil070P0Pcryptos1-a00P0000000rpnljhfdb`^YPNLJHD2&!.5191High SlopeGPS@Aeolian Sands1-b007001-b00P00T0000igeca_][YWUPPNLHFA2&!-variablevariableLow levelGPS@New AlluviumP0070Pcryptos1-a001-a0000000}{ywupnlg^\ZVTRD83(,6125High LevelGPS@Aeolian SandsP008001-a00P00T0000fdb`^\ZXVTRMMKIECA2&!+0n/aLow levelGPS@Obscured by Soil0700000200P0000000geca_][YWUSOOMKIGC1% *3255Low slopeGPS@Obscured by Soil06000Pcrypto0300P0000000omkigeca_][WOMKIGC1% )0n/aLow levelGPS@Obscured by Soil0700000200P0000000geca_][YWUSOOMKIGC1% (2202Low levelGPS@Obscured by Soil0800001-b00P0000000hfdb`^\ZXVTOOMKIGC1% '3232Low slopeGPS@Paradox FormationP00006biocrust02001-b0000000usqomkigb`^ZPLJHFD1% &4255Toe slopeGPS@Paradox FormationP00006Biocrust02001-b0000000usqomkigb`^ZPLJHFD1% %2152Low slopeGPS@ Paradox FormationPT0007biocrust1-b001-a0000000vtrpnljhca_ZPLJHFD1% $ 121Low levelGPS@ Obscured by Soil08000Pbiocrust1-b0000000000qomkigeca_]XNLJHFB0$#3171Toe slopeGPS@ Paradox Formation1-a00007Biocrust1-b001-a0000000ywusqomkfdb]SOMKID1% "4139Low slopeGPS@ Paradox Formation1-a00007Crusts1-b00P0000000trpnljhfdb`[SOMKID1% !5175Low slopeGPS@ Paradox FormationPT0008BiocrustP001-a0000000sqomkige`^\ZPLJHFD1%  5167Low slopeGPS@Paradox Formation1-aTT007biocrustP001-b0000000vtrpnljhca_]SOMKID1% 35Low levelGPS@Obscured by Soil0401-b01-bCryptos02001-b0000000vtrpnljhca_[RMKFD@."7186Low slopeGPS@Aeolian Sands04002001-aT0030000000igeca_][WUSNNLJFD@1% 7122Low slopeGPS@Aeolian Sands0300401-bCryptos1-b0000000000sqomkigeca_ZQLJFD@1% LVAL b~  @ H x$>JUNOST are pretty shrubby and invasive-looking. Some areas are small Aeolian deposits, others are stabilized by crusts. Area has a slightly rolling microtopography.A bit of slickrock poking through in a wash, but most of plot is Aeolian deposits or soil stabilized by cryptos. QUEHAV growing up on mounds, while some of the COLRAM shows pedestalling from wind erosion.Gently rolling duney areas- some places with cryptos- straddling a broad shallow wash with lots of slickrock showing through. Slope and aspect are of the overall area.This part of polygon not as sandy as the area by point 566- stabilized here by some cryptos but mostly a grayish physical crust. A few small drainage channels run through area.Very sandy area- almost no cryptos- with many shrubs growing up on mounds and other shrubs showing pedestalling from wind erosion. Pebbly rocks scattered around on spaces between mounds. Shrubs big and healthy here.Plot is very long and narrow, straddling a very shallow sandy wash which is ~2-3m wide. Community surrounding wash looks about the same as the adjoining communities, except for a few more PURSTA shrubs and some ARTFIL.Rolling duney area with QUEWEL congregating up on big mounds. Slope and aspect vary on the small scale, but overall slope and aspect of area are given above. A few small pebbly rocks in interspaces b/w dunes, but no stabilization of dunes by cryptos.Kind of weedy, trashy valley bottom. No recovery of cryptos here yet. Plot bordered by road on north side.Weedy, trashed-looking wide open area with a bit of crypto recovery here.Wide-open, windswept, weedy floor of Salt Valley. Trashed-looking, with very little crypto recovery here.Big weed patch out in the middle of Salt Valley. Lots of dead Streptanthella longirostris stalks standing aroundCrunchy, gypsiferous crusts here, and many small shaley rocks mixed in with the soil.Point is at edge of the polygon, where soils and crusts aren't quite as gypsiferous. Small shaley rocks scattered around.LVAL   <f@Shallow wash 1-2 meters wide with bedrock showing through in places and eolian deposits along the sides.Slabby slickrock slope with vegetation growing in cracks and shallow soil pockets.Point has a big cliffy bedrock exposure, with large boulders as well, and also some flatter slickrock areas. Vegetation growing in joints and shallow soil pockets, with lots of cryptos on soil.Fractured slickrock has vegetation growing in cracks and very shallow soil pockets with lovely, licheny cryptos covering the soil.Lots of slickrock showing through in shallow wash channel that runs through plot, and a couple mounds of bedrock outcroppings. Otherwise, substrate is mainly eolian deposits partially stabilized by cryptos.Plot straddles a joint, not really a wash, 5-10 meters wide with walls 4-6 meters tall and varying degrees of slope. The sheltered nature of this spot and increased run-off from the surrounding slickrock makes this community possible.Rolling slickrock exposures which overall gently slope towards a deep side canyon of Courthouse Wash. Vegetation growing in shallow soil pockets; QUEWEL growing on a few sandy humps.Rolling hills of slickrock with vegetation growing out of joints and pockets of soil. Poor crypto development, and a few old cow pies around.Big, swirling domes of Entrada with canyon-like fractures and joints, making navigation difficult.Rolling, duney deposits with cryptos stabilizing them in some places.Chunky-looking, rough outcroppings of Navajo throughout plot. All the veg. looks dwarfed here.Dirt road runs through west end of plot, and Navajo sandstone upwelling borders plot to the E (photo 2). Plot area is mainly soil stabilized by pretty nice cryptos.Pieces of Entrada showing through in places, but otherwise the plot is mainly covered with Aeolian deposits and some soils stabilized by cryptos. Plot straddles a rocky/bedrocky wash, and surrounding area has gently rolling microtopography.vQA  k ?I7CMK9n/an/aLow levelGPS@Obscured by Soil060P01-aCryptos02T0T00P0000wusqomkigec_VQOMKG5)$J44Toe slopeGPS@Obscured by Soil0800001-b0000000000eca_][YWUSQLLJHFD@."I16231MidslopeGPS@ Navajo Sandstone1-b0600PCryptos1-a1-a0P00T0000xvtrpnljhfa\SQOMID2&!H262Low slopeGPS @Aeolian SandsP007001-b001-a00T0000geca_][YTRPKKIGCA?0$GvariablevariableLow levelGPS@ Entrada SandstoneP1-a050002P0P00T0000~|zxvtrpnljffdb^YWD83(F18247MidslopeGPS@ Kayenta FormationP07000P1-a01-a00T0000mkigeca_ZXSQQOMKGE2&!E0n/aLow levelGPSp@Obscured by Soil0601-a01-aCryptos1-b00P00T0000wusqomkigec^UPNIGC1% DvariablevariableLow levelGPS@Aeolian SandsP007001-bT01-a00P0000{ywusqomhfd__][WUSD83(CvariablevariableLow levelGPSz@Aeolian Sands01-a07001-aT01-a00T0000~|zxvtrpkigbb`^ZUSD83(B15229MidslopeGPSb@Navajo SandstoneP0800PCryptosPP0P0000000omkigeca_][YPNLJFD2&!A2211High LevelGPS@Obscured by Soil070P00P001-b00T0000igeca_][VTRPPNLJHD2&!@107Low slopeGPS@Moab Tongue - Curtis Fm0204P0PCryptos1-a1-a0P00P0000|zxvtrpnlje`WUSQMI0$?.22335MidslopeGPS@Moab Tongue - Curtis Fm1-bP001-aCryptos1-b0400200T0000}{ywusomid[VTRPK2&!>i(variablevariableLow levelGPSl@Entrada SandstoneP06P01-aBiocrust1-bT0T00P0000}{ywupfa_]YWD83(=~'831MidslopeGPS@ Moab Tongue - Curtis Fm1-a07001-aBiocrust1-a1-a0P00P0000~|zxvtrpnidZUSQMH/#<{$950MidslopeGPS@ Moab Tongue - Curtis Fm1-a040002Biocrust02P0T00T0000{ywusqomkigcYUSQMH/#;Sw114High LevelGPS@Moab Tongue - Curtis Fm061-aP01-aCryptos1-a00P00T0000~|zxvtrpnlje\WUSNJ1% :[variablevariableLow levelGPS@Moab Tongue - Curtis Fm1-a03P00020201-a00P0000}{vtplljhfb]D83(9V2358High LevelGPSn@Moab Tongue - Curtis Fm1-a07P0PCryptos1-aT0T00T0000|zxvtrpnljhcZXVTPK2&!8WvariablevariableHigh LevelGPS@Moab Tongue - Curtis Fm030500PCryptos1-a00T00T0000~|zuljhfb^E94(7)8148MidslopeGPS@Entrada SandstoneP0800PcryptoPP0P0000000mkigeca_][YWOMKIEC0$6*34High LevelGPS@Aeolian Sands1-a00701-abiocrust1-a00000T0000sqomkigeca_ZPKIEC>/#53268High LevelGPS@Navajo Sandstone040200Pcrypto1-a1-a01-b0000000ywusqomkfd_ZRPNLHD2&!v `yyyyyyy y y y y y y yyyyyyyyyy{{{{{{{ {!{"{ #{ ${ %{ &{ '{({){*{+{,{-{.{/{0~1~2~3~4~5~6~7~8~9~ :~ ;~ <~ =~ >~?~@~A~B~C~D~E~F~GHIJKLMNOP Q R S T UVWXYZ[\]^_`abcdefgh i j k l mnopqrstuvwxyz{|}~              !" # $ % & '()*+,-./0123456789 : ; < = >?@ABCDEFGHIJKLMNOPQ R S T U VWXYZ[\]^_`abcdefghij k l m n opqrstuvwxyz{|}~                                         !"#$%& ' ( ) * +,-./0123456789:;<=> ? 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 s V 9  p U : } f P 9 " v _ H 0   tU7sX=tU6y_E-oW9  tV=eE# s[Cplain bench sand sheet sand sheet bench mesa mesa bluff bluff Colluvial Slope Alluvial flat Alluvial flat Alluvial flat terrace Wash valley  wash  valley  valley side  valley  valley side valley side hill drainage Wash hill hill hill valley valley side plain plain plain plain shelf rim plain plain plain plain plateau plateau plateau plateau plateau plateau Bench valley side valley floor valley floor valley floor ledge valley side falling dune falling dune badlands badlands valley floor badlands badlands badlands wash valley dunes fins hill alcove terrace canyon side valley floor valley floor valley floor valley floor terrace wash wash wash dunes wash wash terrace wash wash canyon side dunes ramp ramp ramp ramp rim ramp dome alcove hill wash wash wash wash terrace badlands badlands plain plain plain island wash wash dFloodplain cFloodplain bFloodplain aFloodplain ]Floodplain `Floodplain _Floodplain 9Floodplain ^Floodplain 1sandsheet [wash terrace Xcanyon bottom WGully Vcanyon bottom Ucanyon bottom Tcreek terrace SFloodplain Rcanyon bottom Qfirst terrace Ohills <petrified dunes sandsheet CWash >Wash \Hogback terrace terrace bench hill dunes drainage drainage plateau terrace wash terrace Plain LVAL  Swirling rounded hills of slickrock rise abruptly here out of the valley below, making a big rolling ramp. Soils shelves host COLRAM, most of the P-J and other shrubs growing out of cracks/joints.Duney area at the base of some Entrada cliffs, with lots of small pebbly rocks on interspaces between dunes. No cryptos to speak of.Sandy 4WD road and braided wash channels run through plot. Vegetation is above on gently rolling, sandy/duney terrace. Wash channels are deep (1-2 meters) and wide (3-5 meters) here.Plot straddles the sandy 4WD road, which is also a wash. Very duney area with big clonal clumps of QUEHAV on wash banks and dunes.Plot/polygon straddles the sandy 4WD road, which is also a wash here. Thick mounds of QUEHAV line the wash banks, with the occasional PURSTA and FRAANO hanging out by the bedrock outcrops.Geology could also be Kayenta (it's reddish-brown), not sure. Big rounded slabs of sandstone make up this slope, with vegetation growing out of cracks and shallow soil pockets.Dark red soils (derived from Dewey Bridge) with lots of little pebbly rocks and almost no cryptos. Shallow wash 1-2 meters wide runs through point. This is where all the PURSTA and many of the JUNOST occur.Ledgy bedrock exposures with some big rocks and boulders. Vegetation growing in cracks and shallow soil pockets. Moderate cryptos here.One meters to car-sized boulders make up most of this ledgy bedrock outcrop. Some talusy breakdown between boulders and many small rocks are mixed in with the soils, making crypto development a challenge. Not much flat bedrock exposure here.Plot lies in between and on some fins/spires that are 8-10 meters high. Soils very sandy and joint/micro valley has a very rolling microtopography. Mesic shrubs hug the walls of the joint, while QUEHAV dominates the rolling sandy exposures. Vegetation growing densely and robustly in areas that it can grow.LVAL LJ 2JStand is at least 30 to 40 meters from wash channel, so would only receive flood disturbance during major events. Lots of litter and dead TAMCHI branches- mature TAMCHI stand in full bloom. Some moss-dominated cryptos along outside of stand.Point is on east terrace of wash, about 40 meters from wash channel, so would only receive flood disturbance during major events. Thick leaf litter from all the major species and lots of dead twigs mixed in.Very sandy terrace, almost beach like, with a good flow of water in the wash channel. SALEXI concentrated close to water- a few large ELAANG around but luckily not taking over yet.Big mature Tamarisk are choking out the POPFRE-many have lost the battle already as evidenced by some scattered POPFRE skeletons. Moss-dominated cryptos on some of the spaces between TAMCHI.A little stagnant water in the wash channel here, with vegetation growing on a broad terrace one to two meters above the channel. Some cut tamarisk stumps in plot and some resprouts. Plot bounded on one side by steep canyon walls, and another side by wall of the second wash terrace which is about six meters higher than the first.Fairly narrow first terrace here, with very steeply sloping banks beyond that which are covered with ARTTRITRI. Huge car to truck-sized boulders scattered about the area, and a big stagnant pool of water in wash channel here.Plot falls mainly on lowest part of canyon, where wash channel is divided here. ~1/4 of plot is 8-10 m. above primary community on a high wash terrace between these two channels. Some cut TAMCHI stumps on first terrace.Point encompasses high and low terraces of this canyon floor, with SALEXI lining the water's edge (small trickle of water), ARTTRITRI farther out on first terrace (with POPFRE), and ATRCAN dominating second terrace. Many cut TAMCHI stumps on first terrace.Area of apparently deep soils, but not eolian. Very weedy and little crust recovery here..vZ A  O  r @ m#jldL1026High SlopeGPS@Obscured by Soil0500001-aT0040000000ljhfdb`^ZXVQQOMKIE3'"cC1169High LevelGPS@Navajo Sandstone061-a001-abiocrust1-aT0P00P0000ywusqomkige`VQOMHD2&!bG0n/aHigh LevelGPS>@Navajo Sandstone040300Pcryptos1-aT01-b00P0000wusqomkidb`[RPNLHD2&!a;3358High slopeGPS:@Navajo Sandstone041-a0003biocrust1-a00P00T0000xvtrpnljhfd_UQOMHD2&!`:5276High SlopeGPS@ Dewey Bridge Member - Entrada041-a00Pcrypto1-a1-a00200T0000~|zxtrmh`^\ZUQ2&!_B2286High LevelGPS@ Navajo Sandstone061-a001-bcryptos1-bT0T00T0000xvtrpnljhfd_VQOMHD2&!^4232Step in slopeGPS@ Navajo Sandstone05P000PP0030000000kigeca_]YWUSSQOMKG5)$]26188Step in slopeGPS@ Wingate Sandstone02030001-a0201-b00T0000vtrpnljhca]XXVTRNJ7+&\1155Low levelGPS@Obscured by Soil0800001-b0000000000hfdb`^\ZXVTOOMKIGC1% [0n/aLow levelGPS@Obscured by Soil0800001-b0000000000hfdb`^\ZXVTOOMKIGC1% ZO0n/aLow levelGPS@New Alluvium0201-a000600000P0000fdb`^\ZXVTRNNLJEC?1% YN0n/aLow levelGPS@New Alluvium060P000300000P0000ca_][YWUSQOKKIGEC?1% XM0n/aLow levelGPS@New Alluvium0300000600000P0000ca_][YWUSQOKKIGEC?1% WK0n/aLow levelGPS@New Alluvium0300000600000P0000ca_][YWUSQOKKIGEC?1% VJ0n/aLow levelGPS @Obscured by Soil02000007000001-a0000jhfdb][YWUSOOMKIGC1% UH0n/aLow levelGPS@New Alluvium020001-awater0600P00P0000mkigeca_][YUNIGEC?1% TG0n/aLow levelGPSz@New AlluviumP008001-b00000T0000db`^\ZXVTRPKKIGCA?1% RF0n/aLow levelGPS@New Alluvium1-b000Pbiological soil crust07000001-a0000~|zxvqomkigcLJHFD?1% QC0n/aLow levelGPS@New AlluviumP000008000001-b0000db`^\WUSQOMIIGECA?1% PB0n/aLow levelGPSj@New AlluviumP00601-awater1-bT0P00P0000nljhfdb`^\ZUNIGCA?1% OA0n/aLow levelGPS~@New Alluvium020001-abiological soil crust0700000P0000}{ywusqomkieNIGEC?1% N?0n/aLow levelGPS@New Alluvium03PP0Pbiological soil crust04P0P00P0000zxvtrpnljhfbKIGEC?1% M>variablevariableLow levelGPS@New Alluvium020P0PWater041-b0P00P0000~|zxvtrpnie^\ZXVRD83(L=0n/aLow levelGPS@New Alluvium031-a00PWater031-b0P00P0000pnljhfdb`^YUNLJHC?1% LVAL  v z HjChunky bedrock outcroppings scattered around, and lots of small rocks on the soil surface.Sandstone poking out in a few places, but for the most part, the substrate is sandy soils stabilized by cryptos.Plot is on a nearly level shelf between Navajo drop-off and Kayenta cliff. Slickrock is poking through soil in a few places, and a few bedrock ledges exposed, but for the most part the soil obscures the geology here. Lots of small platy rocks scattered around on the surface. Everything looks pretty dwarfed here, but happy.Steep, ledgy slope with lots of broken, vertical bedrock exposure and some soily horizontal shelves as well where ATRCAN is perched. Plot may be partially in Kayenta (?) Right at juncture between rock layers.Not too weedy here- bunchgrasses have a good foothold. No crypto development though.Wide-open, weedy valley bottom. No crypto development at all here.Broad terrace which has the wash of a side canyon bisecting it- lots of litter from POPFRE and TAMCHI.Very wide terrace-hard to believe SALEXI would do so well this far from the flowing stream, but they seem happy.Very wide terrace, almost floodplain-like, where the weeds are taking over. Soil has a cracked mud-like appearance in places.Very broad terrace-point is at lest 50 meters from the flowing stream, but SALEXI seems pretty happy growing on this seemingly dry floodplain.This point is as far back (east) on the terrace as you can get while still being on floodplain level. It is somewhat sheltered by the high Entrada walls that are just outside plot to the NE, E and SE. POPFRE litter is pretty deep here, and lots of downed wood.Lovely shallow stream flowing in the drainage- JUNARC clustered along the edges. POPFRE litter is quite thick here.Main wash channel (where water is flowing) is about thirty meters from the point- Wash is very broad here, and dry across this wide terrace, but obviously enough moisture to support SALEXI.jLVAL   L xLSlabby slickrock exposures with shallow soil covering most of the slickrock, and lovely cryptos covering most of the soil.Slabby, broken slickrock exposures with very shallow soil. Lots of cryptos. Healthy-looking community, although P-J is a little stunted.Plot is in a valley ~80 meters wide between two steeply-sloping outcroppings of Moab Tongue. Some old cow pies around under the trees.Big steeply-sloping, broken slabs of slickrock in plot with vegetation growing on shallow soil pockets. Not sure why oak is doing so well here, except maybe it's a N-aspect? Cryptos doing pretty well here too.Somewhat weedy, sandy-soiled area with some old cow pies around. Cryptos are starting to make a comeback though. Only a couple spots where Moab Tongue is peeking through. Otherwise soils appear deep.Plot is in a gently rolling, yet low-lying area between parallel outcrops of Moab Tongue and Entrada. There's only a few places in plot where slickrock is showing through, plot also has some duney areas.Very weedy area, with lots of Salsola litter caught in all the shrubs. No crypto development to speak of.Plot partially falls on some cliffy/ ledgy areas of bedrock outcrops and broken-down bedrock, while other part falls on a wide shelf (~60m wide?) on the valley side with seemingly deep soils. Slope given is that of the broad shelf.Polygon seems to capture a little hill with lots of gray, white, and blackish rocks everywhere (gravel deposits?) Blackbrush is thick here, but small. PJ are young and look kind of invasive.Fairly flat bedrock poking through in many places. Soil looks to be pretty shallow here. Decent crypto development.Plot slopes gently off both sides of the ridge that separates Salt Valley and Eagle Park. Lots of bedrock exposure and soils that probably vary in depth here.Sandstone peeking through in places (especially in small drainage channels). Lovely crypto development on the sandy soils here. Very healthy-looking stand.LvV M @ = KZSJ{{variablevariableLow levelGPS@Obscured by Soil0301-b01-bCryptos02T01-a00P0000~ywuqhca\ZVD83(zzvariablevariableLow levelGPS@ Obscured by Soil02PP002Cryptos0300P001-a0000{ywusqmd`^\ZVD83(yy889High SlopeGPSn@ Entrada Sandstone0203001-acryptos02T0P001-a0000ywusqljhfdb^UPNLHD1% xx!368Low slopeGPS@ Obscured by Soil0600000400000T0000fdb`^\ZXVTRNNLJHFB0$ww4520MidslopeGPS@ Dewey Bridge Member - Entrada070T0Pbiocrust0200T00T0000|zxvtrpnljhdZXVTRN/#vv:442MidslopeGPSH@ Navajo Sandstone1-a030003biocrust02T0T00P0000trpnljhfdb`\RNLJFA/#uu0735MidslopeGPSl@Navajo SandstoneP1-a0006biocrust02T01-a00P0000usqomkigb`^ZPLJHCA/#tt:867MidslopeGPS@Entrada Sandstone07PP0Pbiocrust02P0P00P0000pnljhfdb`^\XNLJHFB/#ss'378MidslopeGPSr@Navajo Sandstone070T0Tbiocrust02T0T00T0000omkigeca_][WMKIGEA/#rr338Low slopeGPSf@Obscured by Soil05000Tbiocrust0400000T0000pnljhfdb`^\XNLJHFB0$qqB736MidslopeGPS<@Navajo SandstoneT1-bP006biocrust02T0T00P0000rpnljhfdb`^ZPLJHCA/#pp4154MidslopeGPSV@Obscured by Soil6000Pbiocrust40000000000ljhfdb`^\ZXVLJHFDB0$ooM68MidslopeGPS(@Navajo Sandstone051-a0003biocrust02T0T00P0000rpnljhfdb`^ZPLJHC?-!nn224Low levelGPS\@Obscured by Soil5000050000000000b`^\ZXVTRPNLLJHFDB0$mm9742MidslopeGPSR@Dewey Bridge Member - Entrada1-aP0006biocrust02P01-a00P0000~|zxvtomkg]YWUSN/#l})7355LowslopeGPS@ Moab Tongue - Curtis Fm1-a03P004Biocrust1-a00T00T0000}{ywusqomkidZVTRNI0$k41ToeslopeGPS@ Moab Tongue - Curtis Fm1-b04T002Cryptos1-a00P00P0000ywusqomkige`WSQOKF-!jv3324Low LevelGPS@ Obscured by Soil04P0004Cryptos1-a00P00T0000sqomkigeca_ZQMKIGC1% i02220MidslopeGPS@Moab Tongue - Curtis Fm1-a05001-bBiocrust1-bP0P00P0000}{ywusqomkf\WUSOJ1% hH4350High SlopeGPS@Obscured by Soil07P001-aCryptos1-a00T00T0000usqomkigeca\SNLJHD2&!gRvariablevariableLow LevelGPS@Obscured by Soil061-a001-aCryptos1-b00000P0000~|zxvqhca_ZVD83(f<1156Low LevelGPS@Obscured by Soil0800001-b0000000000hfdb`^\ZXVTOOMKIGC1% e)2209Step in slopeGPS@Kayenta Formation041-a0001-a0200200T0000trpnljhfb`\WWUSQLH5)$LVALR * 2 >rGently rolling microtopography in a wide area (valley-like) between tall Entrada outcroppings. Tall cryptos in many places, and P-J is very thick and robust here. Shallow wash ~2 meters wide runs through plot.Small fins of Entrada slope down towards a wash, with areas in between somewhat valley-like. Some slickrock showing through soil in places- may help explain the abundance of PURSTA.The terrain is low rolling mounds of sandy soil. Gentle swales lead to the ultimate drainage of the valley.The soil is sandy here; probably some of it is blown-in sand. There are a few dead junipers in the area.Dead pinyon and juniper are scattered around. Biocrust is well-developed and extensive in between the sandstone exposures. There are quite a few young trees here.Well-developed biocrust is the prominent feature here. Not so much bedrock exposed. Lots of trees are young. Several larger trees have died. Dead stems in the ash and blackbrush.The deep, sandy soil is furrowed with numerous sinuous drainages.Shallow drainages snake through low mounds of sandy soil.The terrain is gently rolling mounds of sandy soil.Small sandy drainages cross the plot. Many of the older trees are dead. Biocrust is extensive and well-developed. Lots of dead Yucca harrimaniae here also.Soils are deep and sandy. There are many long-dead bunches of grass (not Hilaria). Area was heavily grazed in the past, evidenced by the many weedy species present here.Several trees are dead, both young and old. The pines may have a beetle problem. Most of the yucca are dead. Soils are relatively deep and sandy.This is a broad drainage in the bottom of this large valley. There is no well-defined channel, just a big, wide (up to 100 meters) rounded valley bottom. The soil is sandy.A very old two track (with biocrust) runs near plot center. Baby blackbrush shrubs are filling in. Soils are deep and rocky. Biocrust is well-developed and extensive.hLVAL v : h  ,h|COLRAM invading from neighboring community. Soil surface is stabilized by a light, but continual cover of dark cyano.Colluvial slope with lots of huge boulders near the band of Salt Wash bedrock near the crest of the hill, and small rocks covering the rest of the hill.White slickrock ramp with long thin fractures and linear strips of vegetation (growing NW > SE) growing on shallow soil deposits. Soils are stabilized by well-developed cryptos.Rolling red clay hills with lots of small chunks of chert.Rocky area-low bedrock exposures, scattered large rocks, and high small rock cover on soil areas. Soils obviously shallow, evidenced by the dwarfed stature of both JUNOST and COLRAM.Small, narrow canyon in the Moab Tongue, where there is water at the surface in parts of the wash. POPFRE are mature with some die-back. Understory is a dense and diverse mix of shrubs.Rolling dunes, mostly active though some moss around the bases of the shrubs. EPHVIR is dominant.Narrow, more mesic community (due to run-off) at the base of Entrada domes. Lots of old dead JUNOST trees lying around.Cliffs and ledges of bedrock in many places broken down into large rock chunks. Mini canyon drainage cuts through plot, soil development is shallow atop the bedrock.Area of Moab Tongue with small fractures and linear bands of vegetation growing on fairly shallow soil pockets. Soils are stabilized by well-developed cryptos. Anomalous willow in plot is near a small pothole with some water in it.Near polygon edge and near the border of the Tidwell and Salt Wash members, though community doesn't seem to change much. Salt wash mostly broken down into large rock chunks.Polygon follows this shallow, sandy wash which is ~2 meters wide and has bedrock outcrops along one side of it.Plot includes a broad sandy wash and straddles both terraces, which are mostly QUEHAV-dominated in the understory. Lots of small rocks in the wash and good crypto development between shrub mounds. vO : 9 [ 9NkC52MidslopeGPS@ Morrison Fm - Tidwell Member080001-aMoss, cryptos1-a00P0000000~|zxvtrpniZUSQOK-!8138High SlopeGPSl@Morrison Fm - Salt Wash Member04P001-aMoss, cryptosP1-b00300T0000}ywrpa\ZXVR2&!561MidslopeGPS0@Moab Tongue - Curtis FmP0900PMoss, cryptosP00T00P0000ywusqomkigecTRPNJH/#860MidslopeGPS@Moab Tongue - Curtis FmP0900PMoss, cryptos1-a00T00P0000|zxvtrpnljhcTRPNJH/#z2142MidslopeGPS@Morrison Fm - Tidwell Member07T001-bMoss, cryptosPP01-b0000000}{ywrpnl]XVTRN0${5243MidslopeGPS@Morrison Fm - Tidwell Member06T00PMoss, cryptosPP0030000000}{ywusomkiZXVTRN0$710High SlopeGPS@Morrison Fm - Salt Wash Member03040002Moss, cryptos1-aP0P00T0000}{ywupa][YUQ1% 872MidslopeGPS@ Obscured by Soil0800002Moss, Dark cyanoP0000000000wusqomkigecaOKIGEA/#0n/aLow LevelGPS@Aeolian SandsP008001-b0000000000eca_][YWUSQLLJHDB@1%  140Low levelGPS@Obscured by Soil08000Pmoss1-b00000T0000mkigeca_][YTNLJHFB0$p260Low levelGPSl@New Alluvium040P0TMoss0600000P0000hfdb`^\ZXVTPJHFDB>0$16333MidslopeGPS0@ Morrison Fm - Salt Wash Member031-a00PMoss, cryptos1-a0300200T0000{yupa_][VR2&!458Low slopeGPSd@ Moab Tongue - Curtis FmP0800Pbiological soil crust, moss1-bT0T00P0000}{ywrUSQOKI0$variablevariableMidslopeGPSt@ Morrison Fm - Tidwell Member050001-amoss, biological soil crust1-aP0030000000pkigeaC72(4180MidslopeGPSn@Kayenta Formation0203T0Tmoss, biological soil crust1-a1-b00300T0000~zxsnQOMKGC0$e150Low levelGPSv@New AlluviumP0P0TWater0900000T0000geca_][YWUSOHFDB@>0$383Low slopeGPS@Aeolian Sands070001-bmoss020000000000ljhfdb`^\ZXTNIGEC?0$0n/aLow levelGPS@Obscured by Soil03PT003moss, biological soil crust0300T001-a0000|zxvtrnQMKIGC1% Q14144MidslopeGPSL@Navajo Sandstone1-a06P0Pmoss, biological soil crust1-a1-b01-a00P0000|zupSQOMID2&!~~753MidslopeGPS@Moab Tongue - Curtis FmP08001-amoss, biological soil crust1-b00T00P0000}{ytWRPNJH/#}}10273MidslopeGPS^@Morrison Fm - Salt Wash Member03P00Pmoss, biological soil crust1-a0300300T0000{^\ZXVR2&!||variablevariableLow levelGPS@New Alluvium02P03001-bP00200T0000{ywusqomige``^\XVRD83(pLVAL  Some rough-looking parallel lines of bedrock exposures with soil in between the rows of exposures that appear deep. Not very good crypto development here.Lumpy sandstone exposures with pockets and fractures of soil and plants step down to the canyon rim.Low hills just above the rim of upper Clover Canyon. Some chunks of chert scattered about. Light crypto development.Broken ledges of bedrock between terraces that are covered in small rocks and cryptos. COLRAM and EPHTOR are co-dominant. Soils seem deeper here than in other parts of the polygon.The majority of polygon and plot is a ramp of bedrock with narrow, linear fractures and soil pockets (all shallow) running NW to SE. CELRET is unique and growing in a slot canyon. Soils are stabilized by well-developed cryptos. Vegetation cover is limited by soil availability.Polygon (and plot) is a ramp of bedrock with linear fractures and shallow, linear soil pockets (running NW to SE) that are stabilized by well-developed cryptos. Total plant cover is limited by soil availability.Slightly rolling microtopography and scattered chunks of chert. Soils stabilized by light crypto development and some small rock cover.Slightly rolling microtopography. A scattered coating of small rocks on the soil surface and a couple small piles of chert.Rolling exposures of bedrock in a mosaic with large, shallow soil pockets mostly stabilized by cryptos.Overall area is flat, but microtopography is very rolling and duney. JUNOST trees scattered throughout the area look young and invasive.Understory seems pretty weedy here- a fair amount of live BROTEC and lots of dead BROTEC from last year. Gently rolling, sandy and somewhat duney area, with moss crytpo stabilizing some of it (though in general, cryptos not doing well here).Canyon is shallower and drier here, much more bare ground exposed than in nearby deeper canyons. P-J experiencing some die-back. POPFRE are mature and oak dominates the understory.OvN E L G FQBA5155Low levelGPS0@Obscured by Soil1-a020002Moss, cryptos020201-a00P0000~|zxvtrmkgcTPNLHC1% 3150High SlopeGPS@@Morrison Fm - Salt Wash Member0303T00P0201-a00T0000{ywusqomhfb``^\ZVR2&!2128Low levelGPS@Obscured by SoilP000009P0000P0000eca_][YWUSQMMKIGEC1% 487MidslopeGPS@Moab Tongue - Curtis FmP08001-aMoss, cryptos1-aT0T00T0000}{ywusqomkfWRPNJH/#3102High SlopeGPS6@Moab Tongue - Curtis FmP08001-bMoss, cryptos1-a00P00P0000~|zxvtrpniZUSQMK2&!889High SlopeGPS@Moab Tongue - Curtis Fm071-aP01-bMoss, cryptos1-a00P00P0000~|zxvtrpk\WUSNJ1% '379High LevelGPS@Obscured by Soil0700000200000T0000geca_][YWUSOOMKIGC1% %variablevariableMidslopeGPSp@ Aeolian Sands0060Pbiocrust300000T0000|zxvtrpnljhf\ZXVTRC72(!3103MidslopeGPS@ Aeolian Sands00800200000T0000_][YWUSQOMKIIGECA?0$7286High LevelGPS @ Kayenta Formation04P00PCryptos1-a1-a00300P0000xvtrpnljfd_ZQOMKIE2&!346MidslopeGPS@ Moab Tongue - Curtis FmP050002Biocrust02T0T00P0000xvtrpnljhfd`VRPNJH/##variablevariableMidslopeGPS@ Aeolian Sands00900P00000P0000rpnljhfdb`^\\ZXVTRC72(3120MidslopeGPSJ@Moab Tongue - Curtis FmT0900PBiocrustPT0P0000000usqomkigeca_USQOKI0$366MidslopeGPS@Moab Tongue - Curtis FmT08P01-aBiocrust1-aP0P00P0000zxvtrpnljhfaWRPNJH/#235High LevelGPS@Obscured by Soil070001-bMoss0200T0000000pnljhfdb`^\XRMKIGC1% 13248High SlopeGPSf@Navajo Sandstone030400PCryptos1-b1-a0P00P0000ywusqomkigb]TRPNJF4(#69MidslopeGPS@Moab Tongue - Curtis FmP0800PbiocrustPT0T00T0000rpnljhfdb`^\RPNLHF-!815154MidslopeGPS@Aeolian Sands000900P0000000000ca_][YWUSQOMMKIECA2&!6274MidslopeGPS@Morrison Fm - Tidwell Member05P00PBiocrust1-a1-a00300T0000~|zxvtpnidZXVTRN0$637MidslopeGPS@Moab Tongue - Curtis Fm1-a07001-abiocrust1-a00000P0000}{ywusqomkidZUSQMH/#743MidslopeGPS@Moab Tongue - Curtis FmP900PbiocrustP00000T0000rpnljhfdb`^\RPNLJH/#%4196High SlopeGPS6@ Navajo Sandstone051-b001-aCryptos1-b00000P0000xvtrpnljhfd_VQOMHD2&!q4330High SlopeGPS@ Moab Tongue - Curtis Fm1-a0700PBiocrust02T0T00T0000|zxvtrpnljhdZXVTPK2&!LVALJXx  <The surface is bedrock and boulders with pockets of coarse sandy soil.Some flat bedrock exposures between mostly stabilized dunes. Soils vary from shallow to fairly deep.The soil is fine sand. A surprising number of rabbit droppings decorate the site.These dunes are partly stabilized by all the vegetation.This is pretty beach sand, actively blowing in and out of the area. Many of the plants are on mounds or pedestals.Dark red soils with lots of dark red rock. Some whiter sandstone outcrops at lower end of plot, may be Navajo. Lots of die-back on the PURMEX.Bedrock exposures with islands of vegetation where soil has accumulated. Biocrust is well developed here.The sand is not well-stabilized at this site. Many of the shrubs are on pedestals.This plot is nearly all bare rock. Plants are found living in cracks and where soil from the nearby Tidwell has accumulated. White chert chunks decorate the area.A small sandy wash runs through plot. The Moab Tongue is lumpy and expansive here, with plants and well-developed biocrust in the fractures. Trees are mostly about 3 meters tall. Many chert chunks are scattered around, suggesting the nearby Tidwell layer.Deep soils here. Plants are all growing on small mounds. Much of the Ephedra is dead.Shelf-like outcroppings of rough, tan sandstone here, with veg growing in cracks and shallow soil pockets. Lots of dead P-J standing (from long ago) and lots of dead wood around.The sandstone here forms big rounded lumps. Soil of varying depth has collected between the lumps.Very duney area, not stabilized by cryptos at all. Most of dunes are 1-2 meters high here.The soil has pretty cherty rocks embedded in it. Shallow gullies run through plot. Trees are widely scattered.The terrain is rounded lumps of Moab Tongue with collections of soil in between. The slots are not especially deep here.This site is mostly bedrock with plants occupying available cracks and collections of soil.LVAL  B  H&Point fell next to a micro canyon that has some small sandy dune areas and a pool of water below a rockslide. TAMCHI is anomalous in polygon and occurs in the wash. The rest of plot is more typical: petrified dune bedrock exposures with scattered pockets of shallow soil.Boulders, bedrock exposures, and a fair amount of soil make up the surface here.Lots of bedrock along with boulders and a little soil make up the surface here.Very duney area between fins on the outskirts of Fiery Furnace. Runoff from the walls are keeping JUNOST, PURMEX, and RHUARO happy along the edges.This site is the top of a rugged hogback with giant boulders, bedrock exposures, and not much soil. The rock is a durable coarse sandstone or conglomerate.Petrified dune-like exposures of bedrock with shallow bands of soil in between that are stabilized by cryptos.The terrain is a series of eroding hogbacks with bedrock exposures, boulders, and areas of deeper soil. The trees are somewhat stunted.Tiny polygon that captures the small community in this narrow side canyon. Soil development is ramped along the canyon sides and stabilized by cryptos.The terrain is a series of ridges formed by eroded hogbacks. Bedrock, boulders and patches of deeper soil characterize this area. The trees are a bit stunted.Small polygon that encompasses this narrow side canyon (~20 m. wide) that is a dense monoculture of tall Gambel oak (3-5 m.). Some seep areas underneath overhanging Entrada canyon walls. Can't see any bare ground from above.Petrified dune-like exposures of bedrock dominate the area. Shallow, linear soils pockets are stabilized by cryptos and are often densely vegetated. All 3 oak species here, though some could be hybrids instead of true forms.Vegetation cover is limited by the amount of soil deposits. Petrified dune-like bedrock exposures with patchy areas of shallow soil stabilized by cryptos.vO E 7 ! (8{#dbvariablevariableToe slopeGPS|@Obscured by Soil0500003moss, biological soil crust1-aT01-a00P0000d`^\ZVD83(1510MidslopeGPSX@ Wingate Sandstone04T00TMoss, CryptosP1-b00400T0000zxvtrpnlhfa_PNLJHD1% 512Toe slopeGPS@ Chinle Formation05T00Pmoss, biological soil crust1-a1-a00300T0000}{wupkNLJHFB0$1variablevariableHigh LevelGPS>@ Obscured by Soil070001-aMoss0200P0000000~|zxvtrplfa_][WE94(g3298Low LevelGPS$@Obscured by Soil0800001-b00P0000000hfdb`^\ZXVTOOMKIGC1%  282Low levelGPSDisturbed, weedy area.Obscured by Soil05000PMoss04001-a0000000}{ytrplfdb`^ZH$0flatn/aLow levelGPS8@Obscured by Soil070P01-bMoss1-b00T00T0000wusqomkigec^XSQOMI7+&3167Low slopeGPS@Mancos Shale08000PMossP00020000000igeca_][WUSQKIGEC?1% n/an/aLow levelGPS@@Mancos Shale09000TMossPT01-a0000000nljhfdb`[YWUOMKIGC5)$3191Low slopeGPS@Mancos Shale07000PMossPT0030000000igeca_][WUSQKIGEC?1% P26291MidslopeGPSv@Morrison Fm - Brushy Basin Member02000PMoss, cryptosT030040000000~|xvrpa_][YU2&!t3135High SlopeGPS@Mancos Shale080000PT0020000000db`^\ZXVRPNLLJHFD@2&!uvariablevariableHigh SlopeGPS@Mancos Shale06P000T1-a0030000000zxvtrpnlhfa__][YWSE94(V4110High SlopeGPS@Morrison Fm - Brushy Basin Member080000P001-b0000000zxvtrpnlgecaa_][YU2&!m6128MidslopeGPS"@ Moab Tongue - Curtis FmP081-a0PMoss, cryptos1-aT0P00T0000~|zxvtrpnlgXVTOKI0$4232Low slopeGPS@ Morrison Fm - Salt Wash Member040300Tbiocrust021-a0P00P0000~|zxvtrmi_][YUQ1% 4218Low slopeGPS@ Morrison Fm - Salt Wash Member020600PbiocrustP1-a0T00T0000~|zxvtrpki_][YUQ1% 17102MidslopeGPS(@Aeolian SandsP008001-bT0T00T0000fdb`^\ZXVTRMMKIECA2&!10210High SlopeGPS8@Morrison Fm - Salt Wash MemberP4000P50P00T0000trpnljhfdb`^^\ZXVT4(#5129MidslopeGPS@Moab Tongue - Curtis FmP08P01-bMoss, cryptosPT0T00T0000}{ywusqomkigXSQOKI0$5207Low slopeGPS@Morrison Fm - Salt Wash Member0204000P030P00T0000wusqomkigea__][YUQ1% 5135High SlopeGPS@Morrison Fm - Salt Wash Member03050001-a020P00T0000{ywusqomkie``^\ZVR2&!LVAL V F  zLumpy slickrock expanses with pockets of soil where plants are growing.Rolling hills on this valley side are intersected by drainages/gullies usually filled with rock fall. JUNOST cover is spotty. An old road cuts through the center of plot.Rolling microtopography on these toeslope hills that are intersected regularly by gullies.On the crest of a hill, so slope and aspect are variable. Disturbed understory with ARTFIL the dominant shrub, and COLRAM invading from neighboring community.Half of plot falls on flat area with more sandy soils (ARTFIL) and half of plot falls on lower sloping area, badland-like, with more clayey soils.Depression area with a couple sandy wash channels running through it. Main park road cuts through plot. ARTFIL dominant with a disturbed weedy understory.Rocky hillslope and low-lying area of clay soils. A few good-sized patches of HILJAM.Very sparse vegetation cover on clayey soils with scattered small rock cover. Plot captured a side of a hill, but mostly a flat area at the bottom of the hill.Slightly rolling microtopography of low clay hills with consistent but scattered small rock cover.Steep slope of blue clay soils covered in cello-sized rock chunks from the Salt Wash layer above and blue small rocks from the Brushy Basin. Vegetation is sparse, but evenly distributed.Plot falls on low rolling hills with the overall slope and aspect given above. Very clayey soils with many small rocks scattered about.Just crossed over into this geology type, but veg didn't change, COLRAM just looks a little more stressed. Plot straddles several small hills and drainages. Rocks of varying sizes scattered over the gray, clayey soils.Plot straddles three different substrates (and elevations). S side of plot is in a lower-lying "valley", with alluvial fill. Middle of plot is a hill running E to W of gray clay. N side of plot is a rockier hill with a slightly talusy appearance.lLVAL  d~Big cliffy outcroppings rising above the COLRAM and huge Entrada boulders adjoining the outcroppings. Area seems fairly protected by these outcroppings. Lots of small shaley rocks in some areas.The wash is dry now, but there are recent debris piled four feet high in the trees. The wash is from 20-30 feet wide. Vegetation is found on the sandy sloping banks. A small sinuously sculpted section of slickrock makes up part of the wash in the plot.Rolling microtopography with some broken-down bedrock exposures on top of the small hills. One anomalous patch of blue clay soils in plot. Several small drainages cut through plot.Rolling microtopography of hills stabilized by light cryptos and intersected by gullies. Outcrops of bedrock, especially near gullies, but soils seem pretty deep otherwise.Active dune area, though some shrubs have moss cover around their bases and there's scattered cover of small rocks between the dunes. JUNOST are large, but spaced out. Lots of die-back on the oak.Big, healthy COLRAM shrubs. A few well-developed cryptos in places, but mostly there are a lot of rough, white small rocks mixed in with the soil.Large, sloping exposure of white bedrock is eroding into small, shaley rocks. Rolling microtopography intersected by several surficial drainage channels. COLRAM look very healthy.Shaley small rocks and large rock-fall cover much of the soils on this valley side slope. A few exposures of bedrock are mostly broken-down. A fairly thick swath of ELYSAL along the old road-cut near center of point and in the rocky gully that cuts through the center of plot.Badland-type topography with colorful hills (yellow, purple, peach, red) covered in small rocks and intersected with deep gullies. A few small pancake-like exposures of bedrock.Rolling microtopography on the toe slopes of the valley side with multiple drainages cutting through the small hills. ARTFIL does not seem continuous in this community as far as I can tell.TvR J  h V'd/9204High SlopeGPSh@Navajo Sandstone051-a000PP00300T0000kigeca_]YWUSSQOMHD2&!8227High SlopeGPS@Navajo Sandstone0304001-bbiological soil crust1-aP0T00T0000}{ywusqlUPNLHD2&!variablevariableHigh LevelGPSD@ Aeolian Sands000901-bMoss, Dark cyanoP00000T0000}{ywuc^\XVTE94(27330MidslopeGPS@Kayenta Formation1-bPT0Pbiological soil crust06P00200T0000}{ywuqomiRPNLJE2&!2355MidslopeGPS@Obscured by Soil05PT01-abiological soil crust02T00200P0000~|zxvtpnlhQLJHFB0$266MidslopeGPS@Kayenta Formation021-aP0Pbiological soil crust061-a00200P0000}{ywsqlhQOMKFB/#879High SlopeGPS@Obscured by Soil0600003Biocrust1-b0000000000trpnljhfdb`[QMKIGC1% 524High SlopeGPS@Kayenta FormationP1-aP0Twater08P0P00P0000pnljhfdb`^\XQOMKFD1% 3494MidslopeGPSl@Kayenta Formation02PT0Pbiological soil crust05P00200P0000}{ywusomkgPNLJHD1% 10118Step in slopeGPS@Kayenta Formation04PP0Pbiological soil crust021-a00300T0000~|xvqmVTRPNJ7+&jvariable144MidslopeGPS @Moab Tongue - Curtis Fm1-a071-a001-bT0T00T0000~|zxvtrpniige`\W>2-#6174High SlopeGPS@Aeolian Sands03P040PCryptos1-bT0T00T0000qomkigeca_]XOMKGEA2&!4317High SlopeGPS@ Entrada Sandstone041-b00Pcryptos1-aT00300T0000xvtrpnljfdb]TRPNIE2&!4208MidslopeGPS@ Moab Tongue - Curtis Fm020600Pbiological soil crust1-bT0T00P0000}{ywusnWUSQMI0$z3190Low slopeGPS@Entrada SandstoneP2700PT0T00T0000db`^\ZXVTRPNNLJHFD1% variablevariableMidslopeGPSl@Navajo Sandstone051-a0003Moss, cryptos1-a1-a0P00P0000zufb`^YUC72(6327High SlopeGPSZ@Dewey Bridge Member - Entrada041-bP003Moss, cryptos1-aP0P00T0000~|zxvqb^\ZUQ2&!variablevariableHigh LevelGPS@Aeolian Sands000801-aMoss, cryptos1-aT0P00T0000}{ywrc^\XVTE94(8255High SlopeGPS&@Obscured by Soil06000PCryptos1-b000200T0000trpnljhfb`^YPNLJHD2&!6176High SlopeGPSj@Navajo Sandstone041-b001-aMoss, cryptos1-aP00300T0000~|zxvtrnljeVQOMHD2&!n19348Low slopeGPS,@Wingate Sandstone031-a0001-a0200400T0000rpnljhfd`^ZUUSQOJF3'"r10357Toe slopeGPSd@Chinle Formation06P00TMoss, cryptosPP00300T0000xvtrpnljfdb`QOMKIE3'"PLVAL $J <d`tBig, rolling exposures of slickrock, plus some flakey layers of bedrock jutting out, with a lot of platy rocks around.Partly stabilized, partly active dune area, with some dark cyano and moss cover around the bases of shrubs. Quite a few tumbleweed skeletons are scattered about.This slope is adjacent to the headwall of a side canyon. Slope is steep with loose, rocky soil.Soils are deep with small rocks above the bedrock floor of this narrow wash.This plot represents the gulch leading out of three adjacent alcoves. It is steep-sided with a combination of colluvium and bare sandstone. Whenever it rains, water flows here, although it is dry now.Crust here seems almost more chemical than biological, it's not very dark and has no lichens, but is pretty tall. Most areas in this polygon I've seen don't have much crust at all. Big, healthy COLRAM throughout.This alcove has moisture seeping out at points along the rocky wash bottom. A vanguard of poison ivy prevented me from walking clear to the back wall. The grass is growing on the drier slopes above the wash.This is a strange place. A seep near plot center on the canyon side supports a healthy population of Phragmites and salt grass. Also, on the canyon side facing east, is a mixture of short shrubs and Elymus salinus. On the west facing slope the Serviceberry is dominant. Soils are rocky and loose and steep.There must be a spring in the draw, and the vegetation associated with that constitutes approximately one quarter of plot. The remainder is ledgy colluvium below the cliff, and the drier wash bottom. The oak and serviceberry are less than two meters tall and the oak may be a hybrid, although it tends more toward Gambel in form and one foot size.This site has lumpy bedrock exposures and is very sandy otherwise. Plants are growing on humps of sand and rippled sand speaks of blowing sand.Rolling, duney area between tall, rounded-cliffy Entrada outcrops. A few cryptos stabilizing dunes in places.LVAL N 2 This plot occupies the high terrace above the wash. It looks as if it never floods here. Leaf litter covers much of the soil surface.This site is a real jungle. A big slope of dirt has accumulated against the side of the cliff wall right where water is seeping out.The wash is quite wide here with a jungle of vegetation growing on terraces 3-4 feet high. Some dried salt is visible on the surface.The spring at the canyon head keeps water flowing here perennially (I think). The rest of the wash is subject to periodic flooding. The poison ivy and box elder are on the next terrace higher and probably do not flood.The wash is about 100 feet wide here, bordered by cliffs about 60 feet high. All the vegetation is on low terraces - one or two feet high. Flood debris are stacked about four feet up the trees. Tent caterpillars are doing a lot of damage to the cottonwood trees.Rolling Navajo sandstone with slabs sloughing off in places. Good crypto development on the soil pockets. Lots of die back on CERINT and JUNOST.Vast expanses of rolling Navajo slickrock, with some scattered small and large pockets. A few good cryptos are around, but not many here.Fin area with linear, shallow soil pockets in between that are somewhat stabilized by moss and cryptos. Vegetation is pretty thick in these small soil pockets.Dark red soils with some chunky brown rocks around, and what looks like Navajo slickrock showing through in the wash. JUNOST and FRAANO are pretty much clustered around the wash and side channel that run through plot.Navajo slickrock showing through in places with Dewey Bridge talus and soils over the top of it from some cliffs to the north. A few small eolian deposits where QUEHAV is growing.Smooth, slightly domed outcrops of slickrock and many flat outcrops in the "valleys" between domes as well. Soils appear shallow- COLRAM and JUNOST are pretty dwarfed, but good crypto development on some of the soil.Pv8v G w - >@FQvariablevariableLow levelGPS@ Obscured by Soil1-a0060PMoss, cryptos02T01-a00T0000|zxteca][VD83(3259High LevelGPS@ Navajo Sandstone03020003biocrustPT0T00T0000trpnljhfdb`^TPNLHD2&!3350MidslopeGPS@ Obscured by Soil060020Pbiocrust0200000T0000rpnljhfdb`^ZPNLHFB0$0n/aLow levelGPS>@ Obscured by Soil60002biocrust20000000000mkigeca_][YWMKIGEC1% 2102Low slopeGPSh@Obscured by Soil701-a0Pbiocrust20000000000pnljhfdb`^\ZPNLGEC1% 196High LevelGPS@Obscured by Soil8000Pbiocrust1-a0000000000pnljhfdb`^\WMKIGEC1% 2284High SlopeGPS@Obscured by Soil0600002moss, biocrust200000T0000xvtrpnljhfdbRNLJHD2&!1155Low levelGPSL@New AlluviumP0030006T0T00P0000ca_][YWUSQOKKIGCA?1% 950High SlopeGPS^@Dewey Bridge Member - Entrada050P00PP00300T0000trpnljhfb`^\\ZXVTP1% 686High SlopeGPSh@Obscured by Soil060001-abiological soil crust1-a001-b0000000}{ywrpniRMKIGC1% variablevariableMidslopeGPS*@Dewey Bridge Member - Entrada1-b1-a1-a0003T00300P0000}{yuusqlgbC72(0n/aLow levelGPS@New Alluvium60000300000P0000_][YWUSQOMKIIGECA?1% 0n/aLow levelGPS2@New Alluvium2000050000030000_][YWUSQOMKIIGECA?1% 0n/aLow levelGPS@ New Alluvium03000Pbiological soil crust0700000P0000zxvtrpnljhfbKIGEC?1% 15306MidslopeGPS @ Obscured by SoilT0000900000P0000db`^\ZXVTRPNNLJHFD2&!144Low levelGPS @New Alluvium40P00500000P0000^\ZXVTRPNLJHHFDB@>0$1185Low levelGPS@New Alluvium00040Pwater0600000P0000jhfdb`^\ZXVRKIGCA?1%  1126Low levelGPS@New Alluvium0040Pwater400000P0000fdb`^\ZXVTRPIGECA?1% 8195High SlopeGPS@ Navajo Sandstone1-b040001-a1-a00200T0000qomkigec_]XSSQOMID2&!variablevariableHigh SlopeGPS$@Navajo Sandstone1-b06001-abiological soil crust1-aP0T00T0000idb`\WE94(4190High SlopeGPS@Navajo Sandstone1-b0600Pbiological soil crust1-aP0P00T0000}{ywusqojSQOMID2&!variablevariableHigh LevelGPS@@Entrada SandstoneP0900PMoss, cryptos1-a00P00T0000~|zxsdb`^ZXE94(3169High SlopeGPS@Dewey Bridge Member - Entrada051-b001-abiological soil crustPT0020000000~|zc^\ZUQ2&!`LVAL  P R4A very sandy wash bottom and side terraces. Very diverse shrub mixture and all shrubs are pretty tall. Light crypto development in places.This site has a few bedrock exposures and sandy soil with robust biocrust.A lumpy sand dune rises up, interrupting the homogenous sand sheet. Several dead bunchgrasses are here, as well as blown-in Salsola skeletons.This low-lying weedy area has a large space with no shrubs, just Salsola. To the NW, within plot, the land rises slightly to a more duney area (outside plot).This point fell on the low slope of a rising dune to the west and a sand sheet to the east. Both are included in the plot. The Vanclevea is restricted to the dune and Atriplex to the sand sheet. Soils are deep. Annual weeds and little speak of past disturbance. There are several old dead grass bunches.Soils are deep and sandy. Most yuccas are dead. There is plenty of Salsola litter. Biocrust is mostly not well-developed.An area with undulating topography and deep, sandy soil with moss and biocrust development.This steep-sided canyon has a spring at the head of it, about 100 meters from plot. Wash bottom is unvegetated. The species are more dry-site farther from the wash.Dark red soils with many red and white rocks on top. Several channels run through plot and drain into a little larger wash, also in plot, where mesic shrubs are concentrated.Pretty unremarkable COLRAM shrubland, with lots of SALTRA litter hung up in the bushes. Crusting seems more physical here than bio- it's same color as soil and no visible lichens.Plot encompasses a wash one to three meters wide and both banks, which are very steeply sloping broken-down Dewey Bridge / red soils and small rocks.Part of the plot is on a stream terrace about four feet above the stream channel - the rest is about four feet higher.This site is on a terrace about eight feet above the bottom of the wash. Some Tamarix removal has been done in this area, but there's still a lot to do.LVAL N L & *H@In this area the potholes are small (under 20 feet) and widely spaced. It appears that the soil accumulated is not especially deep.The potholes in this area are about 50 feet in diameter and appear to have collected a fairly deep layer of soil.Plants are growing in collections of soil in the undulating sandstone surface.Some of the potholes here are large - 1/2 acre or more, while others can be as small as a bathtub. A few plants are growing right out of the rock, rooted in the rare crack.Half the plot is solid rock - mostly unvegetated. The other half is sandy soil with a few pebbles.This site is in the crotch of a bunch of big slickrock domes. The plants seem to be benefiting greatly from their lucky location. Everything is big and happy.Exposures of bedrock alternate with pebbly soil at this site. The trees are somewhat stunted.Gradually sloping canyon side with fingers of bedrock spreading out over the Navajo-exposed wash channel below. A line of short cliff bands runs through center of plot with large rock chunks eroding off and some large rocks from the Entrada cliffs above.Small slickrock exposures and ledges interrupt the deeper pebbly soil. Many dead stems are in the ash.Most of plot and polygon is on a large, sloping exposure of bedrock with a mosaic of shallow soils pockets stabilized by cryptos. Plot also captured an area of deeper soils where COLRAM and EPHTOR dominate.This plot fell alongside a rocky, sandy, wide wash , which is mostly bare rock. The sides are sandier than the tops above the wash. Many oak shrubs are dead.The pebbly surface includes several bedrock exposures.The pebbly soil has a few bedrock exposures.The surface is pebbly with a few bedrock exposures.A lot of bedrock is exposed alternating with pockets of pebbly soil. The trees are stunted. There are a few dead CERINT shrubs here.I'm on the edge of a big basin with a lot of bedrock exposed and many boulders. There are good accumulations of soil on the ledges and at the top of the slope.vd(} 4  ]  ^ ep+variablevariableMidslopeGPS@Dewey Bridge Member - Entrada1-b03000P0200300P0000}ywsqqomkgbC72(9128High SlopeGPS@Entrada Sandstone020600pcryptos1-aT0T00P0000usqomkigeca\SQOMIE2&!%1841Low slopeGPS@Entrada Sandstone1-a0403000200000P0000nljhfdb`^\ZVVTRNJE2&!F15164Step in slopeMap@Navajo SandstoneT09000TT0T00T0000kigeca_][YWUUSQOKI7+&s1010High SlopeGPS@Navajo SandstoneT0900TbiocrustTT0T0000000qomkigeca_][QOMKGE3'"f326High SlopeGPS@Navajo Sandstone007020TbiocrustP00000T0000qomkigeca_][QOMIEC1% E1033High SlopeGPS@Navajo SandstoneP0900PbiocrustP00000T0000qomkigeca_][QOMKGE3'"-2292High LevelGPS@Navajo SandstoneP0600Pbiocrust0200T00T0000rpnljhfdb`^ZPNLJFD2&!A3273High LevelGPS@ Navajo SandstoneP0800PbiocrustP00T00T0000pnljhfdb`^\ZPNLJFD2&!+4284High SlopeGPSZ@ Navajo Sandstone020600Pbiocrust1-a00T00T0000usqomkigeca\RPNLHD2&!S3260High SlopeGPS@ Navajo Sandstone1-a07001-abiocrustTP0P00T0000vtrpnljhfdb`VQOMID2&!E5250Low slopeGPS@@ Navajo Sandstone0205T0Pbiocrust1-aT0T00T0000trpnljhfdb`[QOMKGC1% [4231Low slopeGPS@ Navajo Sandstone03040002biocrustPT0P00T0000sqomkigeca_]SOMKGC1% 12333MidslopeGPS@Dewey Bridge Member - Entrada031-a00PMoss, cryptosP0200400T0000}{wuqo`^\ZUQ2&!214MidslopeGPS@Navajo Sandstone06020001-aP00200T0000jhfdb`^\XVTOOMKIEA/#|5322High SlopeGPS"The soil here is deep and sandy.Navajo Sandstone060020PbiocrustP00000T0000~trpljfT&!430MidslopeGPS@Navajo Sandstone1-a08001-aMoss, cryptosTT0P00T0000xvtrpnljhfdbSNLJFA/#24MidslopeGPS>@Navajo Sandstone04021-a001-aP00200T0000kigeca_]YWUPPNLGC?-!2168High LevelGPSl@Navajo Sandstone050300PbiocrustP00P00T0000rpnljhfdb`^\RPNLHD2&!2148High LevelGPSX@Navajo Sandstone05P001-abiocrust0200P00T0000usqomkigeca]SNLJHD2&!3208High LevelGPSf@Navajo Sandstone06P000PT00200T0000hfdb`^\ZVTRPPNLJHD2&!7225High SlopeGPS @Navajo Sandstone0207000PP0P00T0000hfdb`^\ZXVTRRPNLHD2&!15217High SlopeGPS@@Navajo SandstoneP6000P30P00T0000fdb`^\ZXVTRPPNLJHF4(#:LVAL  h N 2tLbPlot encompasses a couple fins and the rolling eolian areas on either side of them. Very weedy understory, with lots of dead cheatgrass covering the more stabilized areas.The fins are eroded to low lumps at this site.Fin area with sections of small stabilized dunes in between the fins.The fins are about half gone from erosion and closely spaced.The fins in this area are eroded to low rounded lumps and don't offer much shade to the soil collected between them.The fins are quite tall here and would offer some shade to the plants growing near them. Some of the oaks are tree-like and may be a hybrid with Quercus turbinella.Point fell in a mini-canyon between fins. Lots of bedrock exposure with shallow soil development on top. Soils are somewhat stabilized by cryptos.Plot is right at the junction between Dewey Bridge and Entrada, and has both types of sandstone in plot. Lots of breakdown here, with slopes looking fairly talusy. Plot covers several steep slopes at a variety of aspects.Steep fins of slickrock with deep chasms between- the chasm next to me is full of poison ivy! Sloping pockets of soil have vegetation and cryptos stabilizing soil. Slope given is for overall area, but slope of the community between the fins here actually faces north.Aeolian deposits between these fins that are ~40m apart here. Some bedrock showing through the sand in places. Slope and aspect given for the duney area between fins (where veg is growing), but plot also includes vertical sandstone walls and gently sloping slickrock.This site is on an inaccessible ledge on the side of the Navajo sandstone cliff. It's mostly solid rock with a few plants growing in cracks.This plot is mostly solid rock. Only a few small potholes are included.This plot includes just one big pothole. Deep piles of sand have collected here and the vegetation is thriving. The sand is partly stabilized by plants. The Live Oaks are tree sized and appear to be hybridizing with the smaller Quercus welshii.vB N 1 > H06166LowslopeGPS@ New Alluvium020P0005P00200P0000db`^\ZXVRPNJJHFDB>0$22160LowslopeGPSf@ Talus/Colluvium/Landslides020000P050030000000trpnljhfb`\ZZXVTRN2&!2160Low LevelGPS@ New Alluvium00P0009P000000000a_][YWUSQOMIIGECA?1% 0n/aLow LevelGPS This area is flooded annually.New Alluvium03000007P000000000}{ywusqokkigec_Q% 11125LowslopeGPS@New AlluviumP000009P0T00T0000b`^\ZXVTRPNJJHFDB@2&!5227LowslopeGPS|@New Alluvium040P000500000T0000b`^\ZXVTRPNJJHFDB>0$8359LowslopeGPS@New Alluvium030P0005T0T00P0000b`^\ZXVTRPNJJHFDB>0$2143LowslopeGPS&@Talus/Colluvium/Landslides1-a000Pbiocrust04050P00T0000~|zxvtrpnlhdZXVTRM1% 1273LowslopeGPS@New Alluvium04000005T0T00P0000ca_][YWUSQOKKIGEC?1% 22134LowslopeGPS@Talus/Colluvium/LandslidesT1-aT00P070P0000000sqomkigeca][[YWUPN2&!4150High SlopeGPS@Entrada Sandstone020500PMoss, cryptos1-aT00200P0000}{ywusqokigbSQOMIE2&!  10212LowslopeGPS@Entrada SandstoneP9T00TT0T00T0000eca_][YWUSQOOMKIGE2&!  :10167MidslopeGPS@Entrada SandstoneP800PbiocrustPT0T00T0000omkigeca_][YOMKIGE2&!  variablevariableHigh LevelGPSX@ Entrada Sandstone020302000200000T0000~|zxvtrpnlhhfd`\XE94(  5284High SlopeGPS\@ Entrada SandstoneP0900PbiocrustP00000P0000qomkigeca_][QOMKGE2&!  V0n/aHigh LevelGPS@ Entrada Sandstone1-b0800Pmoss, biological soil crust1-a00T00P0000~|zxvqTRPNJE2&!7322MidslopeGPSz@ Entrada SandstoneP08T0PbiocrustPT0T00P0000omkigeca_][YOMKIEC0$7147MidslopeGPS@Entrada SandstoneP09T0PbiocrustPT0T00T0000omkigeca_][YOMKIEC0$5180Step in slopeGPSJ@Entrada SandstoneP09T0PbiocrustTT0T00T0000trpnljhfdb`^TRPNJH5)$f8144MidslopeGPS(@Entrada Sandstone1-a0800PMoss, biological soil crustPP01-a00P0000~|zusqoRPNLHC0$LVAL ^ $ H8The stand probably floods annually. The association above (to the north) never does.A hot, dry rocky slope with large Wingate boulders.This low terrace is flooded annually. Some beach sand and river rocks are exposed now.The river floods the lowest portion of this polygon annually, where the Salix is growing.The gently sloping bank encourages a thick growth of tamarisk.Here the bank is more sandy and less muddy than other nearby shores.Lots of boulders have landed here from the Wingate, Chinle, and Moenkopi. A fair amount of soil has also accumulated. The grass looks pretty dry.The bank starts out wet and muddy next to the river and dries out rapidly upslope. Rocky colluvium makes up the upper part of the plot.This is a steep, cliff-sided ravine full of huge boulders. Plants are growing in a few small collections of sandy soil.On the edge of a large area of fins. Soils are shallow over bedrock. Some die-back on the FRAANO and PURMEX.The terrain is a jumble of huge slickrock fins. The main drainage for this area passes through here and into a little slot. The slope and aspect given are for plot center. Part of the plot has the opposite aspect.The terrain is a rough jumble of slickrock fins with plants growing between them.v `yyyyyyy y y y y y y yyyyyyyyyy{{{{{{{ {!{"{ #{ ${ %{ &{ '{({){*{+{,{-{.{/{0~1~2~3~4~5~6~7~8~9~ :~ ;~ <~ =~ >~?~@~A~B~C~D~E~F~GHIJKLMNOP Q R S T UVWXYZ[\]^_`abcdefgh i j k l mnopqrstuvwxyz{|}~              !" # $ % & '()*+,-./0123456789 : ; < = >?@ABCDEFGHIJKLMNOPQ R S T U VWXYZ[\]^_`abcdefghij k l m n opqrstuvwxyz{|}~                                         !"#$%& ' ( ) * +,-./0123456789:;<=> ? @ A B CDEFGHIJKLMNOPQRTUV W X Y Z [\]^_`v                                                                                                                                                      yyyyyyyy y y y y y y yyyyyyyyyy{{{{{{{ {!{"{ #{ ${ %{ &{ '{({){*{+{,{-{.{/{0~1~2~3~4~5~6~7~8~9~ :~ ;~ <~ =~ >~?~@~A~B~C~D~E~F~GHIJKLMNOP Q R S T UVWXYZ[\]^_`abcdefgh i j k l mnopqrstuvwxyz{|}~              !" # $ % & '()*+,-./0123456789 : ; < = >?@ABCDEFGHIJKLMNOPQ R S T U VWXYZ[\]^_`abcdefghij k l m n opqrstuvwxyz{|}~                                         !"#$%& ' ( ) * +,-./0123456789:;<=> ? @ A B CDEFGHIJKLMNOPQRTUV W X Y Z [\]^_`v @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @abcdefghijklmn o p q r stuvwxyz{|}~                                        v _ ~~~{ { { { y ~ ~ {y y y y ~y ~ y !"#{$%y& '{({)* +{,-./01234y5y6y789:; < = > ? @{ A{B C{D{ E F{GHIJ~K~L~M~N~O{P{Q~R~ STUVW~ XyYZy[y\]y^_`ayb~ cdefghyijyklmynyo p q r s~ t uv wxyzy{|} ~yy y{{{~~~~{~~{{{                            !"#$%&'()*+,-./01234567 89 : ;<= > ? @A B CDE FGHIJKLMNOPQRSTUVWXZ[\]^_`ab cdefghijk l m n opqrstuvwxyz{|}~                                           !"#$%&'()*+,-./0123456789:;<=>?@ABCEFGHIJ K LM N O Q R SUVWX Y Z[\] ^_ v                                                                                                                                                      ~~~{ { { { y ~ ~ {y y y y ~y ~ y !"#{$%y& '{({)* +{,-./01234y5y6y789:; < = > ? @{ A{B C{D{ E F{GHIJ~K~L~M~N~O{P{Q~R~ STUVW~ XyYZy[y\]y^_`ayb~ cdefghyijyklmynyo p q r s~ t uv wxyzy{|} ~yy y{{{~~~~{~~{{{                            !"#$%&'()*+,-./01234567 89 : ;<= > ? @A B CDE FGHIJKLMNOPQRSTUVWXZ[\]^_`ab cdefghijk l m n opqrstuvwxyz{|}~                                           !"#$%&'()*+,-./0123456789:;<=>?@ABCEFGHIJ K LM N O Q R SUVWX Y Z[\] ^_ v @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @` bcdefghi jklmn o p q r stuvwxyz{|}~                                        oW?'}dK3 t R 3  q Z <  i O 5   r Z A ' x _ G )  }fM4jS:# zaH,eK-lU;% eN1lL4kK+canyon bottom canyon bottom canyon bottom Terrace Ravine canyon bottom Canyon Floodplain canyon bottom Plain canyon bottom  structural bench Wash Stream terrace Alcove Bank Floodplain Floodplain Floodplain Wash canyon bottom canyon bottom vCanyon Side Beach Bench sBench rPlateau qRim wTerrace vWash uterrace tcanyon floor swash rcanyon qterrace pcanyon bottom ocanyon side ncanyon side mterrace lcanyon floor kcanyon bottom janticline iridge hslickrock fins gdune fanticline ~eanticline }dvalley |cvalley {bvalley zawash y`wash x_wash w^valley v]valley u\valley t[wash sZvalley rYhill qXvalley pWvalley oVwash nUvalley mTvalley lSvalley kRbox canyon jQvalley iPvalley hOvalley gNhill fMvalley eLhill dKvalley cJslickrock dome bIslickrock slot aHslickrock fins `Gslot canyon _Fridge ^Evalley ]Dvalley \Cwash [BValley ZAvalley Y@valley X?terrace W>terrace V=terrace U<valley T;ridge S:vallley R9ridge Q8ridge P7ridge O6valley N5ridge M4ridge L3ridge K2plateau J1plateau I0plateau H/plain G.basin F-basin E,plain D+canyon rim C*blowout B)slickrock domes A(slot canyon @'wash ?&anticline >%anticline =$anticline <#anticline ;"wash :!anticline 9 wash terrace 8wash terrace 7colluvial slope 6canyon wash 5canyon wash 4canyon 3canyon 2canyon 1wash terrace 0canyon /Ledge .canyon -canyon ,canyon bottom +wash terrace *wash terrace )point bar (bench 'bench & bench % basin $ plain # finger ridge " finger ridge !badlands  badlands cliff base dD$rS5"  | d L 3  w ^ E # t [ B )  z b I 0  z ] <   cE' vW=# |eN7  hQ:" ~dJ0aC$qX@~W<;badlands :slickrock fin pocket 9monolith base 8wash terrace 7bench 6slick rock fin pocket! 5rock fall 4slickrock fin pocket 3bluff 2canyon 1canyon side 0canyon .valley floor -valley floor ,valley floor +valley floor *valley floor )valley side (valley side 'plain &plain $terrace #canyon side "wash !terrace  ledge terrace terrace terrace playa mesa mesa plain fins dunes wash plain hill ramp ramp ramp hill hill hill  ramp  wash  ramp  hill  hill hill hill dome canyon canyon canyon dome wash wash plateau plateau valley floor valley floor valley floor wash valley floor valley floor valley side valley side valley side valley side fin wash canyon wall slickrock wash wash dune slickrock wash slickrock wash canyon rim bench slickrock plateau basin ridge canyon wash terrace valley valley ledge valley valley valley valley valley valley valley valley valley valley valley valley valley valley valley valley valley colluvial slope valley valley slickrock fins slickrock canyon slickrock canyon slickrock fins hogback hogback valley plain plain ~plain }slickrock badlands |slickrock dome {ridge zridge ycliff x Valley side Valley floor Valley floor Valley floor Anticline Anticline Anticline canyon bottom canyon bottom canyon bottom Valley floor Valley floor ramp Wash Plain Plain hO6rY@' l J (  y W ? !  | c J 1  l P 8  y a K 3   iR;}^E,u[A' eG/}dK2lR6lT: z[=hValley side Valley floor Valley floor Plain canyon bottom Canyon Side Wash Plateau Plateau Plateau Ridge Anticline Anticline Valley side Valley side Valley side Anticline Anticline Anticline Plateau Plateau Fin Badlands dunes side canyon bottom Valley floor Valley floor luplift kuplift jValley iuplift huplift gValley fValley evalley side dridge cridge bridge avalley side `plateau _plateau ^valley side ]valley side \valley [valley floor Zterrace Yterrace Xterrace Wterrace Vterrace Uterrace Tfloodplain Rterrace Qterrace Pcanyon Ocanyon Ncanyon Mcanyon Lcanyon floor Kcanyon Jvalley side Imonocline Hvalley Gwash Fmonocline Ewash terrace Dwash Cwash Bmonocline Aplateau @uplift ?uplift >joint =uplift <uplift ;Plain :joint ~9rim }8plain |7hill {6dunes z5plain y4plain x3plain w2plain v1plain u0plain t/plain s.sandsheet r-wash q,dunes p+valley o*valley n)valley m(valley l'valley k&valley j%valley i$valley h#valley g"valley f!valley e valley side dvalley cvalley side bvalley side avalley side _bench ^colluvial slope ]knoll \pediment [stream terrace Zstream terrace Yslickrock bench Xbench Wcolluvial slope Vcolluvial slope Uvalley Tvalley Svalley R river terrace Q river terrace P valley O hill N valley Mvalley Lvalley Kvalley Jhill Ihill Hvalley Gvalley Fvalley Evalley Dvalley Cvalley Bvalley Avalley @valley ?valley >valley =valley <badlands jS5zcK2 } d J 3   j S 1   u ^ G 0  r T = !  r V ? (  w_E+sT;sU> w_C% kQ7 hG&cG+eM5_plain ^bench ]plateau \plateau [plateau Zbasin Ybasin Xwash Wplateau Vdune Usandsheet Tsandsheet Ssandsheet Rsandsheet Qcanyon Pplateau Oplateau Nwash banks Mstream terrace Lstream terrace Kstream terrace Jcanyon side Iwash Hcanyon wash Gwash Fplateau Eplateau Dplateau Cfins Bplateau Aplateau @plateau ?dunes >canyon side =wash terrace <gulch ;plateau :alcove 9canyon side 8colluvium 7bench 6plateau 5plateau 3bench 1wash 0hill /hill .dunes -valley side ,hill +valley side *valley side )valley side (valley side 'valley side &hill %Valley $valley bottom #valley "Valley floor !valley bottom  hill colluvial slope hills hills hills ramp hogback hogback Dunes hogback ramp hogback hogback canyon hogback canyon ramp ramp anticline  Plateau  Dune  Dune  Plain  anticline Dune anticline anticline rise Valley side Anticline Dunes rise Anticline Anticline Valley side canyon rim hill hill ramp ramp hill hill hill hill valley valley wash colluvial slope ramp hill valley side wash dunes valley valley side ~ramp }hill |wash {terrace zvalley yvalley xswale wanticline vbench ubench tanticline santicline rvalley qbench prise obench nvalley mbench LInterfluve KTerrace EInterfluve <Valley side =Valley side >fins ?Valley side @Valley side lValley side iValley side kValley side Dv\8lU>' w ` ?   y ] D +  { b D "  e E '  y Z ;   lTerrace -aeolian deposits Canyon Rim mCanyon stabilized dune iFloodplain hFloodplain ggully system fgully system eFloodplain Canyon $Bench #Bench %Bench &Bench !Bench Canyon Side River terrace Colluvial Slope river terrace river terrace river terrace River bank River gorge Colluvial Slope River gorge Ravine Fins {Wash Plateau Plateau Plateau Plateau Plateau Canyon Canyon Anticline ~Anticline }Anticline |Anticline {Plain zColluvial Slope yfins x Slickrock Fins w Slickrock Fins v fins u slickrock fins t fin sslickrock fins rslickrock fins qslickrock fins pfin ofins nfins mfins lcliff kslickrock plateau jslickrock plateau islickrock plateau hslickrock plateau gslickrock plateau fslickrock plateau eplateau dslickrock domes cbasin bcanyon side abench `plateau  _#    ! 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"!#"$#%$&%'&(')(*)+*,+-,.-/.0/102132435465768798:9;:<;=<>=?>@?A@BACBDCEDFEGFHGIHJIKJLKMLNMONPOQPRQSRTSUTVUWVXWYXZY[Z][^\_]`^a_b`cadbecfdgehfigjhkiljmknlompnqorpsqtrusvtwuxvywzx{y|z}{~|}~ƀƁƂƃƄƅƆƇƈƉƊ  !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz { | } ~ ǀǁǂǃDŽDždžLJLjljNJNjnjǍǎǏ !"#$%&'( ) * + , -./0123456789:;<=>? @!A"B#C$D%E&F'G(H)I*J+K,L-M.N/O0P1Q2R3S4T5U6V7W8X9Y:Z;[<\=]>^?_@`AaBbCcDdEeFfGgHhIiJjKkLlMmNnOoPpQqRrSsTtUuVvWwXxYyZz[{\|]}^~_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[ \ ] ^ _ `abcdefghijklmnopqr s!t"u#v$w&x'y(z){*|+},~-.0123456789:;<=>?@ABCDE F G H I JKLMNOPQRSTUVWXYZ[\ ]!^"_# @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @a$b%c&d'e(f)g*h+i,j-k.l/m0n1o2p3q4r5s6t7u8v9w:x;y<z={>|?}@~ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvwxyz{|}~      !"#$%&'()*+,-./0123456789:; < = > ? @ABCDEFGHIJKLMNOPQR S!T"U#V$W%X&Y'Z([)\*]+^,_-`.a/b0c1d3e5f6g7h8i9j:k;l<m=n>o?p@qArBsCtDuEvFwGxHyIzJ{K|L}M~NOPQRSTUVWXYZ[\]^_`abcdefghi j k l m nopqrstuvwxyz{|}~ !"#$%&'()*+,-./0123456789:;<=>?@ABC pY$N Y 3 Y F Y td Y A Y cd Y  Y nd Y I2 Y u Y P Y - Y b Y o Y rd Y  Y  Y e Y n Y i Y  Y t AACodeSiteNameUSGSQuad State CountyParkCodeGPSFileNameGPSUnitUTMEastingUTMNorthingUTMZoneDiffCorrected DatumPDOPUTM Error InParkGPSCommentsRepresentPWPRepresentATD,ClassificationCommentsPlotShapenau yasbsiszocioul~ fYZYYY.rDParkCodePlotCodePrimaryKeyv1b< UmjmmkmkkR)R$%%LVAL  <tPretty good representation of FRED here, though not much QUEWEL and it's more of a woodland than a wooded shrubland. Next polygon N is either COLRAM or P-J/COLRAM. Plot warped S to stay in polygon.Primary name not a great fit because it's not dominated by GRASPI. Secondary name not great because of all the P-J. This seems like a weird spot. Looking E, I can see that COLRAM takes over the understory and it looks that way from the photo as well. Made plot ~60 meters wide to stay in polygon.Primary name a good fit here, PURSTA is definitely dominant, no COLRAM in sight, and one QUEHAV outside plot. Polygon is huge though, so not sure if other areas could be more FRED-like. Not sure what ATRCAN is doing here?!This area has a lot of FRAANO and not much of the FRED components, compared to the rest of the polygon. Also, this is definitely a woodland, not a wooded shrubland. Either primary or secondary name could work here.Just not enough other ingredients for this to be a FRED. This place fits primary name much better. Not sure about rest of this polygon, but PURSTA is the big dominator as far as I can see. Plot warped N to stay in polygon.Good fit with primary name, though COLRAM is definitely dominant and shrub mixture is more diverse than just the named shrubs. Most of the polygon I've seen has been dominated by PURSTA with only trace cover of COLRAM and no oak, so this is clearly different.Polygon appears pretty homogenous, although some areas have very little QUEHAV and no COLRAM. PURSTA is dominant understory throughout. Either primary or secondary name could work, but this spot has a little too much QUEHAV for secondary name to work well.The co-dominance of Grayia here led me to think the secondary name could work, but it didn't mention any P-J or say that Grayia could be co-dominant with COLRAM. That's why I'd like to call it P-J/COLRAM-GRASPI, which describes this area much better.'$ = W *VolARCH_AA.0024Eagle ParkKlondike BluffsUTGrand CountyARCH Garmin GPS III+613963.934299637.6412NoNAD8304UnknownGood@Circular~wsocXGE?1-ARCH_AA.0023Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615342.924299719.1512YesNAD832GoodGood@Circular|vrf[TE?1-ARCH_AA.0022Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615585.284299802.8812YesNAD832.79999995231628GoodGood$@Circular|vrf[TE?1-ARCH_AA.0020Eagle ParkKlondike BluffsUTGrand CountyARCH Garmin GPS III+613971.254299970.5912NoNAD8304UnknownPoor@Other~wsocXGE?1-ARCH_AA.0018Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615261.734300040.7312YesNAD832.09999990463257GoodGoodKeyed easily - perfect fit!Circular|vrf[TE?1-ARCH_AA.0017Long ValleyKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613722.614300124.2012YesNAD834.59999990463257GoodGood(@Circular}wsg\UF@2.ARCH_AA.0016Long ValleyKlondike BluffsUTGrand CountyARCH Garmin GPS III+613887.714300210.5412NoNAD8304UnknownGood>@OtherxtpdYHF@2.ARCH_AA.0015Long ValleyKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613642.824300207.7612YesNAD834.5GoodGood@Other}wsg\UF@2.ARCH_AA.0014Long ValleyKlondike BluffsUTGrand CountyARCH Garmin GPS III+614139.194300273.7012NoNAD8304UnknownFairX@OtherxtpdYHF@2.ARCH_AA.0013Long ValleyKlondike BluffsUTGrand CountyARCH Garmin GPS III+613971.874300380.8612NoNAD8304UnknownGood@CircularxtpdYHF@2.ARCH_AA.0012Long ValleyKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613076.254300365.5212YesNAD833FairFair@Circular}wsg\UF@2.ARCH_AA.0010Long ValleyKlondike BluffsUTGrand CountyARCH Garmin GPS III+613636.614300445.1112NoNAD8304UnknownGood@OtherxtpdYHF@2.ARCH_AA.0008Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615669.064300530.2712YesNAD832.29999995231628PoorGood@Circular|vrf[TE?1-ARCH_AA.0007Long ValleyKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM612912.534300530.3812YesNAD833.40000009536743GoodGood@Circular}wsg\UF@2.ARCH_AA.0003Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615503.354300608.0512YesNAD832.59999990463257GoodGoodKeyed easily - perfect fit!Circular|vrf[TE?1-ARCH_AA.0002Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615423.064300610.0312YesNAD834GoodGoodKeyed easily - perfect fit!Circular|vrf[TE?1-ARCH_AA.0001Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615263.114300611.6912YesNAD831.79999995231628GoodFair@Circular|vrf[TE?1-LVAL This is the phase CERINT of primary name association name. Environmental description matches but species not as well. Oak is dominant, there is no COLRAM, canopy cover is high enough to call this a woodland and PINEDU has higher cover than JUNOST. No other name in the key fits.Made plot a rectangular shape to stay within the narrow wash polygon. Keyed easily and fit primary name description well.Primary name a perfect fit, except no mention of oak, which is co-dominant here, hence the new secondary name. Other parts of this polygon had little to no CERINT and oak and more COLRAM and especially PURSTA, neither of which occur here.Polygon large and winding, so not sure how representative this spot is. It fits primary name very well, however.Either name could work here, but secondary may actually be better since COLRAM and QUEHAV have only trace cover.Matches primary name perfectly! May be less PINEDU here than is representative of the polygon, which has a more even mix of the 2 canopy species.Really weird community and not sure why polygon was drawn this way because eastern side of polygon is clearly Moab Tongue and probably has P-J/PURSTA or FRED (but I haven't had time to go look). Primary name is the best I could come up with for this end of the polygon, but it is such a weird mix of shrubs that nothing from key fits. Plot made narrow NE to SW to stay in plot.Except for being a pretty sparse understory (and more of a woodland), this fits primary name well. Polygon to the N is either COLRAM or P-J/COLRAM.This place is definitely not a FRED, and as far as I can see in this long, narrow polygon, QUEHAV is about the only shrub in the understory! Fits description well except for habitat. QUEHAV is pretty big here, with fairly deep lobed leaves, so could be a Q. gambelii hybrid? Polygon stops abruptly at valley floor where COLRAM or P-J/COLRAM stand is growing. Made plot ~40 meters wide E to W to stay in polygon.7R l  !;b|ARCH_AA.0042Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM618180.164298588.0412YesNAD835.19999980926514FairGood@ Circularyui^WHB40ARCH_AA.0041Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615669.734298588.0412YesNAD837.80000019073486GoodGood@ Circular|vrf[TE?1-ARCH_AA.0040Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615912.384298669.1712YesNAD833.09999990463257GoodGoodL@ Circular|vrf[TE?1-ARCH_AA.0039Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614859.224298665.3912YesNAD834GoodGoodd@ Circular|vrf[TE?1-ARCH_AA.0038Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613561.544298752.7712YesNAD833.20000004768372FairGood@Circular|vrf[TE?1-ARCH_AA.0037Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614454.714298832.4912YesNAD832.5GoodGoodL@Circular|vrf[TE?1-ARCH_AA.0035Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613318.874298829.8412YesNAD834.19999980926514GoodGood\@Circular|vrf[TE?1-ARCH_AA.0034Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM617044.174298907.3612YesNAD833.29999995231628UnknownGood@Circularyui^WHB40ARCH_AA.0033Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615264.914298990.0212YesNAD832.09999990463257GoodGood8@Circular|vrf[TE?1-ARCH_AA.0032Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614778.134298995.0412YesNAD832.59999990463257GoodGoodCircular|vrf[TE?1-ARCH_AA.0031Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615424.914299075.1912YesNAD832.59999990463257GoodFair|@Circular|vrf[TE?1-ARCH_AA.0030Eagle ParkKlondike BluffsUTGrand CountyARCH Garmin GPS III+614049.814299073.8112NoNAD830?PoorGood:@Circular~wsocXGE?1-ARCH_AA.0029Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM613158.954299071.7012YesNAD836.59999990463257GoodGoodH@Circular|vrf[TE?1-ARCH_AA.0028Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615022.754299153.1812YesNAD832.59999990463257PoorGood@Circular|vrf[TE?1-ARCH_AA.0027Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615587.074299315.212YesNAD832.40000009536743GoodFair4@Circular{uqf[TE?1-ARCH_AA.0026Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615470.924299500.2812YesNAD831.89999997615814GoodGood@Other|vrf[TE?1-ARCH_AA.0025Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615019.164299558.0812YesNAD831.79999995231628PoorGood@Circular|vrf[TE?1-LVAL x V |F<0.There is a lot more blackbrush than either Purshia or Quercus.There is only about 2% blackbrush here, so I added the second name.Some spots in this polygon key to P-J/PURSTA woodland.This area has significant blackbrush cover, but only a couple of Purshia shrubs.This site fits the description perfectly!This site fits the description well. Due to the serviceberry, this may be a "phase CERINT".The Purshia and oak cover is a little skimpy for the second choice.The Purshia listed was just one plant.A case should be made for either of these choices.In this case the Cercocarpus is codominant with blackbrush and Ephedra.Fits the description and polygon well.This area fits the description well. One other plot in this polygon has Cercocarpus intricatus as a codominant shrub (#38). Soils are deeper here with less exposed bedrock.The cliffrose only has about 3 percent cover in this spot, probably not enough for the second name. I spied a small patch of oak nearby.Keyed easily and matched primary name description well, though COLRAM has only trace cover here. Included secondary name because oak is the dominant shrub.Matches primary name description well, except no mention of other shrubs. Could fit the secondary name if it was phase CERMON, though no COLRAM here and PINEDU is more dominant than JUNOST.Polygon is huge and I haven't seen all of it, but this spot seems anomalous to me. Plot happens to fall in the only COLRAM clump that I can see from here. KRALAN seems to dominate the rises in this valley, whereas the lowest areas appear to be filled with cheatgrass and other weeds.This area fits the description well.Point fell near an ecotone of P-J/COLRAM and Ephedra/grassland, so grass cover and that of EPHVIR are higher than is representative of the majority of this polygon (to the SE). Fits primary name description well (minus the grass cover) except no PURSTA here.1H _ .KbZlARCH_AA.0061W of Devil's GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM617451.884297856.5112YesNAD832FairFair@ Other{od]NH:6%ARCH_AA.0060Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614700.324297855.4412YesNAD832.5GoodGood*@Circular|vrf[TE?1-ARCH_AA.0059W of Devil's GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM616883.524297938.612YesNAD833.20000004768372GoodFairP@Circular~zod]NH:6%ARCH_AA.0058N of Devil's GardenMollie HogansUTGrand CountyARCHAA_POINTS.corGeoXM619395.484298021.9412YesNAD832.70000004768372GoodGoodEasy to key, perfect fit!Circular}ymb[LF84%ARCH_AA.0057Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM618911.434298017.5912YesNAD833.40000009536743GoodFair@Circularyui^WHB40ARCH_AA.0056Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615750.844298019.3912YesNAD834.80000019073486FairGoodj@Other|vrf[TE?1-ARCH_AA.0055Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614698.414298015.8712YesNAD832.59999990463257GoodGoodB@Circular|vrf[TE?1-ARCH_AA.0054N of Devil's GardenMollie HogansUTGrand CountyARCHAA_POINTS.corGeoXM619955.504298184.3312YesNAD832.79999995231628GoodFair@Circular}ymb[LF84%ARCH_AA.0052Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM618337.744298181.1012YesNAD835.80000019073486FairFair @Circularyui^WHB40ARCH_AA.0051Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM617774.704298260.2712YesNAD835.19999980926514UnknownGood@Circularyui^WHB40ARCH_AA.0050Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614938.914298264.1112YesNAD835GoodGoodX@Circular|vrf[TE?1-ARCH_AA.0049Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM618018.834298342.7312YesNAD832.29999995231628FairFair|@Circularyui^WHB40ARCH_AA.0048Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM615909.224298342.7912YesNAD834GoodGoodCircular|vrf[TE?1-ARCH_AA.0047Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614289.984298342.7312YesNAD834.80000019073486UnknownFair@Circular|vrf[TE?1-ARCH_AA.0045Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM618096.604298422.4912YesNAD834.59999990463257FairGoodl@Circularyui^WHB40ARCH_AA.0044Eagle ParkKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM614047.814298510.1312YesNAD833.29999995231628FairFair@Circular|vrf[TE?1-ARCH_AA.0043Devils GardenKlondike BluffsUTGrand CountyARCHAA_POINTS.corGeoXM617790.384298519.4812YesNAD835.09999990463257UnknownGoodR@ Otheryui^WHB40XLVAL   nZr|Good fit here! Polygon is large though and I'm not sure how homogenous it is. Lots of PINEDU around (relative to JUNOST).Made plot a long rectangle to stay within narrow wash bottom polygon, and viewed an area mostly S of point to avoid overlapping with polygon to the N. Primary name a good fit here, except that COLRAM and QUEHAV have more than trace cover, and PINEDU has higher cover than JUNOST. Secondary name describes community to the E and W of polygon, but also works for this one.Nice homogenous polygon- primary name is good fit, although COLRAM is so overwhelmingly dominant in the understory that secondary name can work too.Primary name has the right mix of species, but environmental comments don't match as well. Included secondary name because QUEHAV is dominant and this is a duney area.There are enough trees here to be a woodland rather than a wooded shrubland.Pretty good fit for association and polygon, although other areas SE of here had more oak. Also, this is a pretty pine-dominated woodland. Warped plot to south to stay in polygon.Polygon is pretty small, so plot evaluates most of it. Nice, homogenous COLRAM shrubland with some scattered PJ. Barely enough trees to justify secondary name.Point fell on a rim that separated two Morrison types (Tidwell and Salt Wash) and 2 communities, all in one polygon. Primary name was a good fit for the community on the rim (N). But no name in the key fit for the S-facing slope below the rim so I had to give this a new name. I made two species' lists for these 2 unique communities.Even though there is no black brush on this plot, it does occur nearby. The cliffrose is the dominant shrub and one large patch of oak is here.This spot seems to fit the description pretty well. The tree cover is about equal to the shrub cover.The Ephedra occupies a south aspect on a mound of soil in the plot - a pattern I see repeating across the polygon. The Plantago and other weeds fill the flat swale bottom.! K n c z  ARCH_AA.0081NE of Devils GardenMollie HogansUTGrand CountyARCHAA_POINTS.cor