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A" A#A$A%A&A'A(A)A*A+A,A-A.A/AA0A2A3A4A5A6A7BBBBB BA1BBB B B B B BBBBB B B B B BBBBBBBBBB B!B"B#B$B%B&B'B(BA1v1@(( @ @+ JS6HOJDM>:H>>M:>JQ@S>S @] Kҷ@yKҷ@qry_ht_DS_New_AA_Pts_@ @ bVVJJJJJJJH @Zҷ@Jҷ@@qry_ht_append_AA_Veg_Details@ |@ rffZZZZZZZX @/ҷ@Lҷ@@qry_ht_append_AA_Veg_Assoc@ |@ nbbVVVVVVVT @] ,8ӷ@̹8ӷ@@qry_ht_append_AA_PhotosY@ |@ h\\PPPPPPPN @~nҷ@wEnҷ@@qry_ht_append_AA_Loc0@ |@ bVVJJJJJJJH @JNҷ@E:ҷ@@qry_ht_append_AA_Env_Details@ |@ rffZZZZZZZX @=ҷ@7ҷ@@qry_ht_append_AA_Env@ |@ bVVJJJJJJJH @] =4m@4m@ MSysNavPaneObjectIDs4MR2KeepLocal  TJJJJJJJH @7=m@m@m@ MSysNavPaneGroupCategories4MR2KeepLocal  TVVVVVVVT @] 3n@<,f@ MSysAccessStorageDDDDDDDDDDB f;q @Րu@GPS_Data_Download .-PPPDDDDDDDB @U!Zq @z9#@@GPS_append_6#@ @ RFF:::::::8 @U!Zq @ 7#@@GPS_append_5@ @ RFF:::::::8 @]  `Yq @ĸ2#@@GPS_append_3@ @ RFF:::::::8 @ `Yq @ q@@GPS_append_2@ @ RFF:::::::8 @ IXq @[$q@@GPS_Append_1m@ |@ RFF:::::::8 @  `@v@$LU@AdminL3 -8,,,,,,,,,* .Dn@.Dn@frmCalcT@ <<<0000000. @\q @\q @frm_Import_GPST@ JJJ>>>>>>>< @] Ib u@Ib u@SysRel.........., Ib u@Ib u@Scripts0000000000. Ib u@Ib u@Reports0000000000. Ib u@Ib u@Modules0000000000. Ib u@Ib u@Forms,,,,,,,,,,* Ib u@Ib u@DataAccessPages@@@@@@@@@@> J u@J u@MSysRelationshipsDDDDDDDDDDB J u@J u@MSysQueries88888888886 J u@J u@MSysACEs22222222220 J u@J u@MSysObjects88888888886 J u@e@MSysDb(@<:::......., @J u@J u@Relationships<<<<<<<<<<: J u@J u@Databases44444444442 J u@J u@Tables.........., :9n.: ) 6 ? F j * N6^(VJ2Lt GPS_Data_DownloadtblAADetails^@WK3  LandformGPS_Data_Download.LandformI! w EnvironmentID tblAAEnvironment.EnvironmentIDW+ w tblAAEnvironment111  tblAADetails)))  GPS_Data_Download333   G tblAAEnvironmentDetails??? O    G tblAADetailstblAAEnvironmentR@UI)  GPS_Data_DownloadtblAADetails^@WK3  ElevSourceElevSource@E9%  ElevationGPS_Data_Download.GPS_HeightM# w TopoPositionGPS_Data_Download.Topo_PositS) w AspectGPS_Data_Download.Aspect_DE w SlopeGPS_Data_Download.Slope_DB w AAIDtblAADetails.AAID8 w tblAAEnvironment111  tblAADetails)))  GPS_Data_Download333   G tblAAEnvironment111 O    G GPS_Data_DownloadtblAALocation`@YM3  SurveyorsGPS_Data_Download.SurveyorK# w SurveyDateGPS_Data_Download.GPS_DateM% w CameraUsedGPS_Data_Download.CameraK% w AACodetblAALocation.AACode? w tblAALocation+++  GPS_Data_Download333   G tblAADetails))) O    G TMUGPS_Data_Download.MapUnit3? w SMUGPS_Data_Download.MapUnit2? w PMUGPS_Data_Download.MapUnit1? w  DiffCorrectedGPS_Data_Download.Corr_TypeT+ w  ParkCodeParkCode"CANY"E1!   PlotShapeGPS_Data_Download.PlotShapeL# w  UTMZoneUTMZone"12"?-   StateGPS_Data_Download.State@ w CountyGPS_Data_Download.CountyC w USGSQuadGPS_Data_Download.QuadNameI! w UTMEastingGPS_Data_Download.EastingL% w UTMNorthingGPS_Data_Download.NorthingO' w GPSFileNameGPS_Data_Download.DatafileO' w GPSUnitGPS_Data_Download.Rcvr_TypeH w PDOPGPS_Data_Download.Max_PDOPA w AACodeGPS_Data_Download.AA_CodeD w GPS_Data_Download333   G tblAALocation+++ O    GLVAL$< . x D  J|4d P zl&tblAAVegAssociation_DS.VegAssocCodetblAAVegAssociation_DS.VegAssocID(((tblAAVegetation_DS.AAID)=2285 Or (tblAAVegetation_DS.AAID)=2286 Or (tblAAVegetation_DS.AAID)=2287))tblAAVegetation_DS.PlantSpeciesCommentstblAAVegetation_DS.VineTotPercenttblAAVegetation_DS.NonvasCovPercenttblAAVegetation_DS.H4CoverPercenttblAAVegetation_DS.HTotalCoverPercenttblAAVegetation_DS.DwarfCovPercenttblAAVegetation_DS.ShrubCovPercenttblAAVegetation_DS.TallShCovPercenttblAAVegetation_DS.EmergCovPercenttblAAVegetation_DS.LeafTypeCommentstblAAVegetation_DS.ProvCommunityName(((tblAALocation_DS.AACode)="CANY_AA.0298" Or (tblAALocation_DS.AACode)="CANY_AA.0308" Or (tblAALocation_DS.AACode)="CANY_AA.0931"))tblAALocation_DS.ClassificationComments(((tblAAEnvironmentDetails_DS.EnvironmentID)=3602 Or (tblAAEnvironmentDetails_DS.EnvironmentID)=3603 Or (tblAAEnvironmentDetails_DS.EnvironmentID)=3604))tblAAEnvironmentDetails_DS.LandformtblAAEnvironmentDetails_DS.EnvironmentIDtblAAEnvironmentDetails_DS.EnvDetailID(((tblAAEnvironment_DS.AAID)=2285 Or (tblAAEnvironment_DS.AAID)=2286 Or (tblAAEnvironment_DS.AAID)=2287))tblAAEnvironment_DS.DarkCyanobacteriatblAAEnvironment_DS.LiveVegLittertblAAEnvironment_DS.EnvironmentalCommentstblAAEnvironment_DS.EnvironmentID(((tblAADetails_DS.AACode)="CANY_AA.0298" Or (tblAADetails_DS.AACode)="CANY_AA.0308" Or (tblAADetails_DS.AACode)="CANY_AA.0931"))(((GPS_Data_Download.New_Associ)="yes" Or (GPS_Data_Download.New_Associ)="no"))tblAADetails.AAID = tblAAVegAssociation.AAIDGPS_Data_Download.AA_Code = tblAADetails.AACodeGPS_Data_Download.AA_Code = tblAADetails.AACodetblAADetails.AAID = tblAAEnvironment.AAIDGPS_Data_Download.AA_Code = tblAADetails.AACodetblAADetails.AAID = tblAAEnvironment.AAIDGPS_Data_Download.AA_Code = tblAADetails.AACodeIIf((IsNull(GPS_Data_Download.GPS_Height)) Or (GPS_Data_Download.GPS_Height=0),Null,"GPS")GPS_Data_Download.AA_Code = tblAALocation.AACode:b&M @ \ > ?  c ' 7\> <O21D?LichentblAAEnvironment_DS.LichenE wRockstblAAEnvironment_DS.RocksB wLittertblAAEnvironment_DS.LitterE wOtherPctDesc"tblAAEnvironment_DS.OtherPctDescW) wOthertblAAEnvironment_DS.OtherB w MosstblAAEnvironment_DS.Moss? w SandtblAAEnvironment_DS.Sand? w BedrocktblAAEnvironment_DS.BedrockH w BareSoiltblAAEnvironment_DS.BareSoilK! w GeologytblAAEnvironment_DS.GeologyH wEnvironmentalCommentsR@ G; wElevSource tblAAEnvironment_DS.ElevSourceQ% wElevationtblAAEnvironment_DS.ElevationN# wTopoPosition"tblAAEnvironment_DS.TopoPositionW) wAspecttblAAEnvironment_DS.AspectE wSlopetblAAEnvironment_DS.SlopeB wAAIDtblAAEnvironment_DS.AAID? wEnvironmentIDB@ 7+ wtblAAEnvironment_DS777  GtblAAEnvironment111 O  GblV@  'lVCameraUsedtblAADetails_DS.CameraUsedM% wlVSurveyorstblAADetails_DS.SurveyorsJ# wlVSurveyDatetblAADetails_DS.SurveyDateM% wlVAACodetblAADetails_DS.AACodeA wlVAAIDtblAADetails_DS.AAID; wblVtblAADetails_DS/// lV GlVtblAADetails))) OblV lV G@  'tblAADetailstblAAVegAssociationX@[O) GPS_Data_DownloadtblAADetails^@WK3 NewNameGPS_Data_Download.New_AssociI wAAIDtblAADetails.AAID8 wtblAAVegAssociation777 tblAADetails))) GPS_Data_Download333  GtblAAVegAssociation777 O  GGPS_Data_DownloadtblAADetails^@WK3 PhysiognomGPS_Data_Download.PhysiognomO% wLeafTypeGPS_Data_Download.Leaf_TypeJ! wPhenologyGPS_Data_Download.Leaf_PhenoM# wAAIDtblAADetails.AAID8 wtblAADetails))) GPS_Data_Download333  GtblAAVegetation/// O  G tblAADetailstblAAEnvironmentR@UI) HY@xW@N''Y  Y d Y  Y  Y  Y d Y  Y  Y  Y  Y    Y    Y   Y  Y   Y   Y  Y  Y  Y Y  Y  Y  Y Y $Y , Y Y 4Y <Y DY LY TY  \ Y!! " Y"" # Y## $ Y$$ % Y%% & Y&& AIDAA_CodeMapUnit1MapUnit2MapUnit3 CameraNew_AssociRep_of_Pt_Rep_Assoc_Slope_DAspect_DTopo_PositLandformLeaf_PhenoLeaf_TypePhysiognom NotesMax_PDOPCorr_TypeRcvr_TypeGPS_DateGPS_TimeUpdate_StaDatafileUnfilt_PosFilt_PosData_DictiGPS_HeightVert_PrecHorz_PrecStd_DevNorthingEastingQuadName County StateSurveyorPlotShapePark`1ACe;YYAA_CodePrimaryKeyv1 ',)@~@$@$@;O@L9@*@Z@ ף2PAV-r!ACANY_AA.1078300GoodPoorLow levelterraceCold-deciduousBroad-leavedWoodlandYesJuno ST04:49:32pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NPvbL.  ~f'+@~@,@,@ClM@333333@gfffff@I,|}?V2PAp=&!ACANY_AA.1070300GoodPoorLow levelterraceCold-deciduousBroad-leavedWoodlandYesJuno ST04:32:26pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NPvbL.  ~f'*@~@*@*@Mb\@@@ȑ?7A2PAx&!ACANY_AA.1167130UnknownFairLow levelterraceCold-deciduousBroad-leavedShrublandYesJuno ST04:26:54pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NP~jT6(~f')?~@$@$@+_@333333@@52;?淪2PA+!ACANY_AA.1068300GoodPoorLow levelfloodplainCold-deciduousBroad-leavedWoodlandYesJuno ST03:48:15pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NP|hR4&~f'(@~@,@,@vm@333333 @gfffff@4s?;O5O3PA"۹/!ACANY_AA.1017100UnknownGoodLow levelterraceCold-deciduousNeedle-leavedShrublandYesJuno ST02:54:36pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadWayne CountyUtLiz BallengerCircularCanyonlands NPlV8*~f''@33@~@,@,@h|?V@gfffff@333333@c3?L5PAo!ACANY_AA.1088300GoodGoodLow levelfloodplainCold-deciduousBroad-leavedWoodlandYesJuno ST01:33:52pmUpdatedCANY_AA_PTS.corCANY_AA_ptsUpheaval DomeWayne CountyUtLiz BallengerCircularCanyonlands NPhR4&~f'&@~@(@(@Q_@@gfffff@U?QΧ5PAq= WB!ACANY_AA.1089300GoodGoodLow levelfloodplainCold-deciduousBroad-leavedWoodlandYesJuno ST01:14:12pmUpdatedCANY_AA_PTS.corCANY_AA_ptsUpheaval DomeWayne CountyUtLiz BallengerCircularCanyonlands NPhR4&~f '3&@`@@`~@O@O@V@gfffff!@@GY@K)>PA1J!ACANY_AA.40431100GoodGoodMidslopefalling duneEvergreenMicrophyllousShrub Herbaceousdone!YesJuno ST06:04:06pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesCircularCanyonlands NP~hJ<( ~f'2?`@`ff@`~@`@`@ ףp=z@333333%@@;ʃ @t?PA5^!ACANY_AA.40361800FairGoodLow levelalluvial terraceEvergreenBroad-leavedDwarf ShrublandNoJuno ST04:06:45pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesCircularCanyonlands NPxbD6"~f'1@~@4@4@K7 Y@@@c ?= 0PARE"ACANY_AA.1216100UnknownGoodLow levelterraceEvergreenMicrophyllousShrublandYesJuno ST10:33:10amUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadWayne CountyUtLiz BallengerCircularCanyonlands NPvbL.  ~f'0@i@`ff@~@$@$@Ca@@?14?"1PA1!ACANY_AA.11101800GoodGoodHigh LevelbenchCold-deciduousBroad-leavedShrublandYesJuno ST09:22:01amUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NPxdN0"~f'/@j@`ff @~@&@&@gfffc@ffffff@gfffff@3iSu?v1PAV-r)!ACANY_AA.1076300GoodPoorLow levelterraceCold-deciduousBroad-leavedWoodlandYesJuno ST08:57:51amUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadWayne CountyUtLiz BallengerCircularCanyonlands NPvbL.  ~f'.@~@$@$@/ݤQ@333333@@{\&?G=2PA#!ACANY_AA.1168100UnknownFairLow levelterraceCold-deciduousBroad-leavedShrublandYesJuno ST05:37:10pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NP~jT6(~f'-@~@&@&@gffffZ@@333333 @{c? y2PA+!ACANY_AA.10745000GoodPoorLow levelterraceCold-deciduousBroad-leavedShrublandYesJuno ST05:08:23pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtLiz BallengerCircularCanyonlands NPzfP2$~f/ K':@~@[@[@?5^Ie@@333333@Q0c ֘@ +_4PA|?*!ACANY_AA.1010210FairGoodLow levelalluvial terraceCold-deciduousMixedShrublandsubstitute for 1012 - inaccessibleYesJuno ST10:08:54amUpdatedCANY_AA_PTS.corCANY_AA_ptsUpheaval DomeSan Juan CountyUtJanet ColesCircularCanyonlands NPxjVHB~f'9@e@@33@~@I@I@oJ@333333@ffffff@]p?7AT6PA(\J!ACANY_AA.40803400GoodGoodLow levelbench, drainageEvergreenBroad-leavedDwarf ShrublandYesJuno ST06:13:01pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesCircularCanyonlands NPxbD6"~f'8?o@@~@N@N@x&@333333!@333333@$D?bX6PAK7 !ACANY_AA.40853400GoodGoodStep in slopebenchEvergreenBroad-leavedDwarf ShrublandYesJuno ST05:27:35pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesOtherCanyonlands NPlV8*~f'7@:@@~@I@I@m@gfffff@333333 @z>?Q-6PA+V)!ACANY_AA.40833400GoodGoodStep in slopebenchEvergreenBroad-leavedDwarf ShrublandYesJuno ST04:57:55pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesOtherCanyonlands NPlV8*~f'6@~@N@N@$F@)@333333@C·?X9L9PAuC!ACANY_AA.1023200GoodGoodLow levelterrace, floodplainCold-deciduousMicrophyllousShrublandYesJuno ST01:52:22pmUpdatedCANY_AA_PTS.corCANY_AA_ptsHorsethief CanyonWayne CountyUtJanet ColesCircularCanyonlands NP~hJ<(~f'5@33@~@I@I@^I f@@333333@H@= ׋@~@t@t@Zd;]@ @@)yu @!r3PAG!!ACANY_AA.1163320FairGoodLow levelalluvial terraceCold-deciduousBroad-leavedWooded ShrublandYesJuno ST04:08:46pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtJanet ColesCircularCanyonlands NPnPB. ~f'= @~@Q@Q@Zd;OK@'@gfffff#@9 ?#vh3PA!ACANY_AA.1164120GoodFairLow levelalluvial terraceCold-deciduousMicrophyllousShrublandYesJuno ST02:55:32pmUpdatedCANY_AA_PTS.corCANY_AA_ptsTurks HeadSan Juan CountyUtJanet ColesCircularCanyonlands NPxbD6"~f'< @~@N@N@'1r@ @@c{-轱@jt;5PA8 !ACANY_AA.1014100GoodFairLow levelalluvial terraceMixed Evgrn Cld DecdBroad-leavedShrublandYesJuno ST01:18:25pmUpdatedCANY_AA_PTS.corCANY_AA_ptsUpheaval DomeWayne CountyUtJanet ColesCircularCanyonlands NPlN@,~f';@~@`@`@QD@$@ffffff@;PMJbv+JJ868BMJbv+JJ868DMJbv+JJ86:<MJbv+JJ86BDMJbv+JJ86BFMJbv+JJ86D6MJbv+JJ86D>MJbv+JJ86D@MJbv+JJ86DBMJbv+JJ86DFMJbv+JJ86FFMJbv+JJ86FHMJbv+JJ86H>MJbv+JJ8886MJbv+JJ88B<MJbv+JJ88B>MJbv+JJ88BDMJbv+JJ88BFMJbv+JJ88DDMJbv+JJ8:8BMJbv+JJ>66><MJbv+JJ>6F6MJbv+JJ>6F<MJbv+JJ>6F@-  @ @ @&'()*+,-./0123456789:;<=>?@ RY%/2 N Y > Y  Y  Y  Y Y /Y /DateCreateDateUpdateIdLvNameParentIdType x`M &eM X'Mi $mM (rM ,Mv YYYYY.rEId.MSysAccessStorageSTGRELParentIdIdParentIdName. v `  L (@;3@ R 3 - H g $ U ERǮ9o,I-f@I-f@@ PROJECT840" I-f@I-f@e@ PROJECTwm<84" I-f@I-f@@!dir0,(" I-f@I-f@%\-_VBA_PROJECTB>:" I-f@I-f@#\-VJSBPSBZKGQIGERXVCDBHCKDMMBBb^Z" I-f@I-f@ @!ZGJXSAKSGQBRSDIEEDIFIXHHJTP_b^Z" I-f@I-f@ AcessVBADataNJF. s m@s m@]ImExSpecs0,( wq @q @<BlobDelta.0,( w\q @Z/q @1PropData.PLH8 \q @;9~q @0k@ TypeInfo.:62" \q @}q @/@ Blob.2.*" ni\q @cr}q @.1   w3n@3n@DataAccessPages<84 w3n@3n@CustomGroups62. w^3n@3n@MSysDbDirDataPLH8 ^3n@3n@Blob&" w^3n@3n@0  w^3n@3n@Databases0,( w^3n@ m@jiPropDataPLH8 ^3n@^3n@Scripts,($ w^3n@^3n@Reports,($ w^3n@^3n@Modules,($ w^3n@^3n@Cmdbars,($ w^3n@zbq @ 0CB0 1CB0PropData TPL< ^3n@_q @:frmCalc frm_Import_GPSDirData tpl\ ^3n@3n@0dhdhBlobDelta lhdR ^3n@3n@T@ TypeInfo :62" ^3n@3n@ PropData GC?/ ^3n@3n@@ Blob 2.*" ^3n@3n@ 0   w^3n@h`q @ Forms($  w 3n@I-f@VBA$  w 3n@I-f@VBAProject2.* w 3n@I-f@VBA$  wx3n@x3n@MSysAccessStorage_SCRATCHPLH wx3n@ m@MSysAccessStorage_ROOTJFB w\LVAL eǫǫǫF~FormID="{956DCFE3-4310-4E50-98FD-6C4049EBD851}" DocClass=Form_frmCalc/&H00000000 DocClass=Form_frm_Import_GPS/&H00000000 Name="CARE_Plots_be" HelpContextID="0" VersionCompatible32="393222000" CMG="C9CB20B024B024B024B024" DPB="2527CC4C74A975A975A9" GC="8183686D696D6992" [Host Extender Info] &H00000001={3832D640-CF90-11CF-8E43-00A0C911005A};VBE;&H00000000 [Workspace] Form_frmCalc=22, 29, 702, 514, Form_frm_Import_GPS=132, 174, 998, 659, Z Form_frmCalcForm_frmCalcForm_frm_Import_GPSForm_frm_Import_GPSͬ")J N+v)^٘Detaild Label0h ButtonImporth ButtonClose:028|=5B>a)b*e gh6iXjk ?l41L@x b*PZDagy  U @ Ariald2" @ Tahomahg#h%" @ Tahoma`,  Detailx  ~B.eHd5U`6ab@ c,d#e%  Label0 Import GPS Datax QN@|BABB%h1U`6 ac, ButtonImport Import GPS Data~ "[Event Procedure]x N+i=AQ1h1U`6 a0 b c,i ButtonClose Close Form~ "[Event Procedure]x ёAAEfͬ\fb9K~Detaild Label0h ButtonCalc08w=Babe ghij.k Dn@E4I@T  U Ariald2 Tahomahgh Tahoma`@  Detail'vJE(\}Td5U`ab cd Label06Calculate Total PercentagesUG ADOBo *\G{020 1-10-8 AA006D2EA4}#2.1#0#C:\Program Files\Common System\ado\ms21.tlb#Microsoft ActiveX Data Objects , Librar&yHyst dole>istdolje^h^^2P0430V0C^46^0^WINDOWS\sT32\22SOLE Automation0DAO>AJDAOA A5EC9A5. 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LL B@0'( !2a '$% Set Fields Index to thirteenth fieldb9K'& $ a $ %6$4 $ %6t $ %6(t) $ $ %6'* & * '&kx $ '$` B@8 & ): B@< ( '( B@> B@B ( Records Updated.A@@  BB@BD| F!H Record  (A@@DxophAttribute VB_Name = "Form_frmCalc" Bas0{665C8786-8C62-4B39-81C2-0E7EA419F7C0} |GlobalSpacFalse dCreatablTru PredeclaId"Expose_TemplateDerivCustomizD$Option Comp@ DT P&* Sub Button_Click() On Error GoTo_" Dim db As DAO.0 Env ir@Recordset TypeIndex Integer otPct !CCounQVa8lid ASet+= Curr`entDbE*=A.OpenF+(P"tblm "G .MoveFirs6'= 0 Do U ntil  EOF G@= 1@2 ' (F@ields Fto thirteh fHTG> 24 If Not IsNull( "( )) And  <> "t" (t) $17) Then& m=JN''T+jE`If=H/+ 1LoopS#5di: %!y al!S " Updjc+A& 1!HNexb Cl c MsgBox" & "s d.I DoCmd. 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LL B@0'( !2a '$% Set Fields Index to thirteenth field'& $ a% $ %6$4 $ %6t $ %6(t) $ $ %6'* & * '&kx $ '$` B@8 & ): B@< ( '( B@> B@B ( Records Updated.A@@ BB@BD| F!H Record  (A@@DxophAttribute VB_Name = "Form_frmCalc" Bas0{665C8786-8C62-4B39-81C2-0E7EA419F7C0} |GlobalSpacFalse dCreatablTru PredeclaId"Expose_TemplateDerivCustomizD$Option Comp@ DT P&* Sub Button_Click() On Error GoTo_" Dim db As DAO.0 Env ir@Recordset TypeIndex Integer otPct !CCounQVa8lid ASet+= Curr`entDbE*=A.OpenF+(P"tblm "G .MoveFirs6'= 0 Do U ntil  EOF G@= 1@2 ' (F@ields Fto thirteh fHTG> 24 If Not IsNull( "( )) And  <> "t" (t) $17) Then& m=JN''T+jE`If=H/+ 1LoopS#5di: %!y al!S " Updjc+A& 1!HNexb Cl c MsgBox" & "s d.I DoCmd. Ehxity: a ?z@ .Descricg(& [] Resu`R#5BLVAL\-$T(]}xME PS<S<S< .    @HP *X    R( (  H&X,  " @P &p & & & & &8 `h px "     xh Ptbl_GPS_Import BB@N1 Delete previous import table. R]@]X]x]]]]] j h%X.V7A=Declare a variable to contain the path of each selected item.] V(Please select a GPS data file to import.9nWUse the Show method to display the File Picker dialog box and return the user's action.#The user pressed the action button.m@5p l5rlIvrtSelectedItem is a String that contains the path of each selected item.HYou can use any file I/O functions that you want to work with this path.7This example simply displays the path in a message box.(MsgBox "The path is: " & vrtSelectedItem l'T lThe user pressed Cancel.dkq#Set the object variable to Nothing..V MsgBox FilePathL DoCmd.TransferText acImportFixed, "COOPSpec", "tblImportWork", FilePath vtbl_GPS_Import T BB@t Check for import errors.$,. f !x!z  f %x.b b!*Errors*"Import errors - check error table.A@@k f DoCmd.SetWarnings FalseqryClearGPSDownLoad BB@| BB@~qryAppGPSImport BB@| DoCmd.OpenQuery "GPS_Append_1" DoCmd.OpenQuery "GPS_Append_2" DoCmd.OpenQuery "GPS_Append_3" DoCmd.OpenQuery "GPS_Append_4" DoCmd.OpenQuery "GPS_Append_5" DoCmd.OpenQuery "GPS_Append_6"|R F!HA@@poh(X BB@B@|80 F!HA@@o LVAL" ǵAttribute VB_Name = "Form_fImport_GPS" " Bas0{298F9EF1-4AB6-4E09-96B0-2BB87629 5ED9} |GlobalSpacIFalse dCreatablTru Pre declaId"Expose_TemplateDerivCustomizD$Option Comp@ DT P&* Sub ButtonClick()On Error ResuNext DoCmd.DeleteObject acT=, "tbl_'" '  previous i B.4GoTo:_I @ Dim FilePath As Sngg%@&fdAADialoHstrBSourceA:UIndex Integ4er#TAGDefI Set @/= App@aao.A2(msoGAPjerj AF'DC a vari‚to contain the pMof @each s@pctitemaEWvrtSI@A*Vn@C*Wi^fd .Tit"PleC!@ data f@l #~. 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@@e`@>Bg@>DgB66z@!B68~#B6<y B6>z@ B88~"B8<z@B8>~%B8@`@B8B`B8FyJJ>>B<g`MJbv+JJ>>B>e MJbv+JJ>>B@e!MJbv+JJ>>BDe"MJbv+JJ>>BFe#MJbv+JJ>>D6e$MJbv+JJ>>D8e%MJbv+JJ>>D<e&MJbv+JJ>>D>e'MJbv+JJ>>D@g(MJbv+JJ>>DBg)MJbv+JJ>>DDe*MJbv+JJ>>DHe+MJbv+JJ>>F6e,MJbv+JJ>>F<g-MJbv+JJ>>F>e.MJbv+JJ>>F@e/MJbv+JJ>>FBe0MJbv+JJ>>FDe1MJbv+JJ>>FFe2MJbv+JJ>>H6e/MJbv+JJ>>H8e0MJbv+JJ>>H:g@1MJbv+JJ>>H<g 2MJbv+JJ>>HBg3MJbv+JJ>>HFg4MJbv+JJ>@68e5 { 52 }}}} } } } } }}}}}}}}}}}}}}}}}}} }!}"}#}$}%}&}'}(})}*}+},}-}. }/ }0 }1 }2 }3}4}5}6}7~~~~~~~~~~ ~ ~ ~ ~  ~!~"~#~$~%~&~'~(~)~*~+~,~-~.~/~0~1~2~ 3~!4~"5~#6~$7~%8~&9~':~(;~)<~*=~+>~,?~-@~.A~/B~0C~1D~2E~3F~4G~5H~6IJKLMNOPQR S T U V WXYZ[\]^_`abcdefghi j!k"l#m$n%o&p'q(r)s*t+u,v-w.x/y0z1{2|3}4~567      !"#$%&'()*+,-./01234567      !"#$%&'()*+,-./012345678           !"#$%&'()*+,- .!/"0#1$2%3&4'5(6)7*+,-./0123 4 5 6 7 89:;<=>?@ABCDEFGHIJ K!L"M#N$O%P&Q'R(S)T*U+V,W-X.Y/Z0[1\2]3^_`abcdefg h i j k lmnopqrstuvwxyz{|}~ !"#$%&'()*+,-./0123456      !"#$%&'()*+,-./01234      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             6374859:;<=>?@AB C D E F GHIJKLMNOPQRSTUVWXY Z!["\#]$^%_&`'a(b)c*d+e,f-g.h/i0j1k2l3m4n5o6p7q8rstuvwxyz{ | } ~   !"#$%&'()*+,-./0123456789:      !"#$%&'()*+,-./0123      !"# $ % & ' ()*+,-./012345678 "#$%()* + , - . /0123456789:;<=>?@A B!C"D#E$F%G&H'I(J)K*L+M,N-O.P/Q0R1S2T3U4V5W6X7Y8Z[\]^_`abc e f g h ijklmnopqrstuvwxyz{ |!}"~#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678      !"#$%&'()*+,-./0123456789           !"#$%&' (!)"*#+$,%-&.'/(0)1*2+3,4-5.6/708192:3;4<5=6>7?8@ABCDEFGHI J K L M NOPQRSTUVWXYZ[\]^_` a!b"c#d$e%f&g'h(i)j*k+l,m-n.o/p0q1r2s3t4u5v6w7x8yz{|}~     {                                                                                                                                                       !"#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678         ! 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" # $%&'()*+,-./0123456 7!"#$%&'()* + , - . /0123456789:;<=>?@A B!C"D#E$F%G&H'I(J)K*L+M,N-O.P/Q0R1S2T3U4V5WXYZ[\]^_` a b c d efghijklmnopqrswxz{ |!}"~#$%&'()*+,-./01234567      !"#$%&'()*+,-./012345678      { 52 }}}} } } } } }}}}}}}}}}}}}}}}}}} }!}"}#}$}%}&}'}(})}*}+},}-}. }/ }0 }1 }2 }3}4}5}6}7~~~~~~~~~~ ~ ~ ~ ~  ~!~"~#~$~%~&~'~(~)~*~+~,~-~.~/~0~1~2~ 3~!4~"5~#6~$7~%8~&9~':~(;~)<~*=~+>~,?~-@~.A~/B~0C~1D~2E~3F~4G~5H~6IJKLMNOPQR S T U V WXYZ[\]^_`abcdefghi j!k"l#m$n%o&p'q(r)s*t+u,v-w.x/y0z1{2|3}4~567      !"#$%&'()*+,-./01234567      !"#$%&'()*+,-./012345678           !"#$%&'()*+,- .!/"0#1$2%3&4'5(6)7*+,-./0123 4 5 6 7 89:;<=>?@ABCDEFGHIJ K!L"M#N$O%P&Q'R(S)T*U+V,W-X.Y/Z0[1\2]3^_`abcdefg h i j k lmnopqrstuvwxyz{|}~ !"#$%&'()*+,-./0123456      !"#$%&'()*+,-./01234      !"#$%&'()*+,-./0123456         !"# $!%"&#'$(%)&*'+(,)-*.+/,0-1.2/304152{                                                                                                                                                      }}}}}}}}}} } } } } }}}}}}}}}}}}}}}}}}} }!}"}#}$}%}&}'}(})}*}+},}-}. }/ }0 }1 }2 }3}4}5}6}7~~~~~~~~~~ ~ ~ ~ ~  ~!~"~#~$~%~&~'~(~)~*~+~,~-~.~/~0~1~2~ 3~!4~"5~#6~$7~%8~&9~':~(;~)<~*=~+>~,?~-@~.A~/B~0C~1D~2E~3F~4G~5H~6IJKLMNOPQR S T U V WXYZ[\]^_`abcdefghi j!k"l#m$n%o&p'q(r)s*t+u,v-w.x/y0z1{2|3}4~567      !"#$%&'()*+,-./01234567      !"#$%&'()*+,-./012345678           !"#$%&'()*+,- .!/"0#1$2%3&4'5(6)7*+,-./0123 4 5 6 7 89:;<=>?@ABCDEFGHIJ K!L"M#N$O%P&Q'R(S)T*U+V,W-X.Y/Z0[1\2]3^_`abcdefg h i j k lmnopqrstuvwxyz{|}~ !"#$%&'()*+,-./0123456      !"#$%&'()*+,-./01234      !"#$%&'()*+,-./0123456         !"# $!%"&#'$(%)&*'+(,)-*.+/,0-1.2/304152{                                                                                                                                                      6374859:;<=>?@AB C D E F GHIJKLMNOPQRSTUVWXY Z!["\#]$^%_&`'a(b)c*d+e,f-g.h/i0j1k2l3m4n5o6p7q8rstuvwxyz{ | } ~   !"#$%&'()*+,-./0123456789:      !"#$%&'()*+,-./0123      !"# $ % & ' ()*+,-./012345678 "#$%()* + , - . /0123456789:;<=>?@A B!C"D#E$F%G&H'I(J)K*L+M,N-O.P/Q0R1S2T3U4V5W6X7Y8Z[\]^_`abc e f g h ijklmnopqrstuvwxyz{ |!}"~#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678      !"#$%&'()*+,-./0123456789           !"#$%&' (!)"*#+$,%-&.'/(0)1*2+3,4-5.6/708192:3;4<5=6>7?8@ABCDEFGHI J K L M NOPQRSTUVWXYZ[\]^_` a!b"c#d$e%f&g'h(i)j*k+l,m-n.o/p0q1r2s3t4u5v6w7x8yz{|}~     {                                                                                                                                                       !"#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678         ! "#$%&'()*+,-./01234 5!6"7#8$%&'()*+,- . / 0 1 23456789:;<=>?@ABCD E!F"G#H$I%J&K'L(M)N*O+P,Q-R.S/T0U1V2W3X4Y5Z6[7\8]^_`abcdef g h i j klmnopqrstuvwxyz{|} ~!"#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678      !"#$%&'()*+,-./012345678           !"#$%&'() *!+",#-$.%/&0'1(2)3*4+5,6-7.8/90:1;2<3=4>5?6@7A8BCDEFGHIJK L M N O QRSTUVWXYZ[\]^_`abc d!e"f#g$h%i&j'k(l)m*n+o,p-q.r/s0t1u2v3w4x5y6z{|}~      !"#$%&'()*+,-./01234567      !"#$%&'()*+,-./0123456  { @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @      ! " # $%&'()*+,-./0123456 7!"#$%&'()* + , - . /0123456789:;<=>?@A B!C"D#E$F%G&H'I(J)K*L+M,N-O.P/Q0R1S2T3U4V5WXYZ[\]^_` a b c d efghijklmnopqrswxz{ |!}"~#$%&'()*+,-./01234567      !"#$%&'()*+,-./012345678     c Y1W@NY 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 WaterctatovvrnSSuuoeellYYYYY{.rEEnvironmentID PlotIDPrimaryKey8tblAADetailstblAAEnvironmentv1b|@noݶ[vڶm۶mm۶mֶkHD$$"ID$H$))$%I$I$$I$)I"LVAL  z Point is on a low level bench at the bottom of the Chinle toeslope. There are car sized boulders from Chinle slope above and high small rock cover and some shelving bedrock exposed. Big patches of cryptos abound.This point lies in the headwaters of a small ravine that drains an amphitheater of alcoves and Wingate cliffs. The ravine and surrounding hill slopes have very high boulder (car-sized) cover and shaley medium sized rocks, very jumbly. Some larger junipers for such a rocky place.This is a very bouldery, rocky steep hillside below the Wingate. The ground surface has very high cover of medium (hand sized) rocks to football to house sized boulders. This point lies at the top of a concave erosional gully system.The plot happened to land in a ravine that is in the plot. Some purple and gray Chinle dirt is showing in spots.This site is shaded by the high cliff above. Most of the slope is covered by Wingate talus. Some water probably pours into this area from above during rainstorms.Point fell on a narrow ledge above a small canyon or large drainage area. Ledgy areas above and below point have high crust cover and are dominated by COLRAM in the understory. PINEDU very tall and robust, and JUNOST more stunted with many dead branches. Large bedrock slabs have very little breakdown and pop up here and there mosaicked with crusty areas.Point is on white Moenkopi Badlands impossible to get to. High crypto cover - very very sparse vegetation.Very high crypto cover and low vegetation cover which is just Atriplex gardneri.Point is very very steep and has high crypto cover and Atriplex gardneri mostly in the drainage areas. Very sparse cover of Atriplex gardneri some larger boulders, throughout but mostly very light colored clayey soil.Point is on very steep Moenkopi Badlands right below Chinle layer. Has high crypto cover and low vegetation cover which is nearly all Atriplex gardneri.Y ` W Q [[Rm3135Step in slopeGPS@Moenkopi FmT03001-acryptoT030030000000sqomkigea_[YQLJHDB5)$3213Toe slopeGPS@Moenkopi FmT0300TcryptoT030030000000ljhfdb`^ZXTRJHFD@>1% 5174Step in slopeGPS@Moenkopi FmT0300TcryptoT030030000000pnljhfdb^\XVNLJHDB5)$flatn/aLow levelGPS@ New Alluvium000900T00T00T0000geca_][YWUSQQOMIGE7+&8205Toe slopeGPS@Talus/Colluvium/LandslidesT02001-bcryptoT020020000000~|zxvtrpljfd\WUSOM1% 3322High SlopeGPS@Talus/Colluvium/LandslidesT1-a000T0801-a00t0000wusqomkidb^\\ZXVQO3'"32360High SlopeGPS@Talus/Colluvium/LandslidesTP000P080P00P0000rpnljhfdb`\ZZXVTRP4(#1417MidslopeGPSN@Moenkopi FmTP0007cryptoT030T0000000jhfdb`^\ZXTRJFDB@>1%  flatn/aHigh LevelGPSn@Chinle FormationT1-bT004cryptoT020020000000{ywusqomigcaYUSQLJ8,'  flatn/aHigh LevelGPS@Chinle FormationT00007cryptoT1-b0020000000ywusqomkge`^VRPNLJ8,' flatn/aLow levelGPS@Aeolian SandsT00700T0000000000hfdb`^\ZXVTRRPNJHF7+& rollingn/aLow levelGPS8@Aeolian SandsT0090TcryptoT0000000000vtrpnljhfdb`XVTPNL=1,! rollingn/aLow levelGPS@Aeolian SandsT0090TcryptoP0000000000vtrpnljhfdb`XVTPNL=1,! 2164Low levelGPS@ Chinle FormationTP0005cryptoP020030000000qomkigec_]YWOKIGEC1% F15343High SlopeGPS2@Talus/Colluvium/LandslidesT1-b00PcryptoP0701-b00P0000~|zxvtrmkge][YWRP4(#3063High SlopeGPS@Talus/Colluvium/LandslidesT0T00T0800200T0000sqomkigea_[YYWUSQO3'"F33331Midslope1:24K Quad@Chinle Formation1-bP00PbiocrustP0500300T0000|zxvtrpnjhdbXVTRPK9-!x3326Midslope1:24K QuadH@Chinle FormationPP000P080P00T0000ljhfdb`^\ZVTTRPNLJ8, 4163High Level1:24K Quad@Kayenta Formation02040002Biocrust1-bP0P00P0000}{ywusqomkf\XVTPL9-!??High Slope1:24K Quad@Moenkopi Fm000009cryptoT1-a01-a0000000sqomkige`^YWOKIGEC6*8108Step in slopeGPS@Moenkopi FmT1-a0007cryptoT1-a01-a0000000usqomkigb`[YQMKIDB5)$??High Slope1:24K Quad@Moenkopi Fm0T0008cryptoT020T0000000omkigeca_]YWOKIGEC6*??High Slope1:24K Quad2@Moenkopi FmT020008cryptoT020T0000000qomkigeca_[YQMKIEC6*|LVAL  8 |&This area is intermittently flooded evidenced by deep channels, but mostly dry and evidence of aeolian depositing evidenced by small coppice mounding and some pedestalling - not many dunes though.This hillslope is in the Moenkopi geological layer and is covered with small rocks and good crypto cover. There are many car sized boulders scattered throughout, crumbly bedrock exposed too. Rocks are platey in nature. Moenkopi is white/grey.Point is 15 feet below Wingate cliffs in a very bouldery steep talus slope with some Chinle bedrock, exposed and fresh rock fall exposing bare soil. Very rocky. Junipers are fairly large for such a rocky area.Very bouldery hillslope that is concave in shape with shallow gullies draining this amphitheater of Wingate cliffs. Some bare soil exposed that is very pebbly and platey rocky. Point near apex of hillslope near Wingate cliff.This hillslope is deeply divided by narrow gullies and has very high crypto cover (lots of lichen and mosses) and boulders ranging from chair to house sized. Small pebbles on surface scattered about, soil is dark red. Point lies at the interface of Chinle and Moenkopi (more Moenkopi I think).This point falls directly in a small ravine on this high level bench below the Chinle slope going up to the Wingate cliffs above. Therefore the covers of sand and bedrock are higher.This bench has some undulations in topography but is generally flat with very high small rock and crypto cover with some house-sized boulders from the steep slopes above the bench going to the Wingate cliffs.Rolling dunes of sand evidenced by coppice mounds, pedestalled shrubs, blowing sand. Larger grained sand resting on top of finer sand.Rolling dunes of active sand evidenced by coppicing, pedestalling of shrubs and sand ripples. Some stability of soils evidenced by small patches of crypto.Rolling dunes of actively blowing sand evidenced by coppice mounding, pedestalling and ripples on ground surface.*LVAL N JThese are rolling, low hills of very developed crypto, with moss species throughout. The mot form of EPHVIR forms large clumps with the bunchgrass STIHYM growing in-between them.Deep sandy soil with crypto & small rocks covering the surface, some bedrock exposed but very little. Litter mostly under trees.Crypto cover and small rocks very high in this plateau woodland. Shallow gullies run throughout area and soil is light brown.This point is directly off of Hardscrabble Hill Road in the Moenkopi badlands. Area is riddled with deep gullies, soil is very light tan, far more crypto cover than small platey / shaley rocks. Bedrock which is shelving is exposed. Rocks mostly on extreme end of interfluve with crypto is on slope and benches.This is an alluvial terrace dominated by Sarcobatus vermiculatus and must get temporarily flooded on occasion (cracks in sand debris around shrubs, gullies) and has aeolian depositing forming ripples and SMALL mounding on surface.Point is on a step in slope of the Moenkopi badlands. Bedrock is very light, platey tan rocks completely cover the ground surface. Deep gullies bisect the badlands. Very sparse veg (except Atriplex gardneri - not much else)This point is on a lower step in slope in the Moenkopi badlands that have significant cover of shaley/platey rocks and patches of crypto. There are deep gullies throughout area. Point directly below Amasa Back cliff band in Chinle. Crypto has good lichen cover. Lighter colored Moenkopi bedrock exposed and rocks are tan/grey plates.Point is on toeslope within the shaley Moenkopi badlands below the Amasa Back member of the Chinle. Surface is covered with tan shaley rocks and toeslope divided into deep gullies, some light tan bedrock exposed.Point is on a step in slope in the Moenkopi badlands that is white / light grey in color. Point sits above the toeslope and has many gullies running throughout. Surface littered with tan platey hand-sized rocks (& smaller sized too). Very sparse vegetation.XK G D6,z o,W324High LevelGPS@Kayenta Formation1-a0800PBiocrust1-aP0P00T0000vtrpnljhfdb]SQOMID1% +h1313MidslopeGPS@Kayenta Formation0204001-aBiocrust1-aP01-b00T0000{ywusqomhfd_UPNLHD1% *t5258High LevelGPS @Kayenta Formation0502001-bBiocrust1-bP01-a00T0000|zxvtrpnige`VQOMIE2&!)3285High LevelGPS@Aeolian Sands06PP002biocrust1-b00T00T0000rpnljhfdb`^YOKIGEA2&!(3255High LevelGPS@Kayenta Formation051-a0003biocrust1-aT01-a00T0000|zxvtrpnige`VRPNIE2&!'3247High LevelGPS@Kayenta Formation1-a02P005Biocrust1-aP01-a00T0000|zxvtrpnige`VRPNJE2&!&3257High LevelGPSf@Kayenta Formation04PT005Biocrust1-a00T0000000vtrpnljhfdb]SOMKIE2&!%4294High LevelGPSr@Kayenta Formation05PT004Biocrust1-a00T0000000vtrpnljhfdb]SOMKIE2&!$9285MidslopeGPS@Kayenta Formation1-a03P004Biocrust02P0P00T0000vtrpnljhfdb^TPNLHC0$#`11286MidslopeGPS@Talus/Colluvium/LandslidesP01-a001-a0801-a00T0000ywusqomkfd`[[YWRPN2&!"[17242Low SlopeGPS@Talus/Colluvium/LandslidesP000PBiocrustP0600300T0000}{ywusqokiecYWUSQO3'"!0413Low LevelGPS@New Alluvium050001-bMoss02P01-b0000000nljhfdb`[YWSMHFDB>0$ .3298Low LevelGPS@New Alluvium070P002Biocrust1-aP0P0000000pnljhfdb`^\WMIGEC?1% 28345MidslopeGPS@Talus/Colluvium/LandslidesP0001-aBiocrust1-b0701-b00T0000}{ywupnje[VTRPN2&!-variablevariableHigh LevelGPS\@Obscured by Soil1-a1-a1-a007crypto1-aT0T001-a0000}{ytlhfa\WE94(-variablevariableHigh LevelGPS@Obscured by Soil1-aT1-a006crypto1-a001-a00P0000zxvqiec^\WE94(1variablevariableHigh LevelGPSd@Obscured by Soil0200008cryptoT0000000000}{ywusqomea_][WE94(variablevariableHigh LevelGPS@Obscured by SoilTTT003crypto1-a1-a003001-a0000}{wupkc_][YWE94(variablevariableHigh LevelGPS@Obscured by Soil1-aT0003crypto1-a1-a003001-a0000~zxsnfb`^\WE94(5126Step in slopeGPSp@Moenkopi FmT020005cryptoT020020000000rpnljhfd`^ZXPLJHDB5)$flatn/aLow levelGPS@New Alluvium0009001-a0000000000jhfdb`^\ZXVQQOMIGE7+&12231Step in slopeGPS@Moenkopi FmT03T0TcryptoT030030000000rpnljhfd`^ZXPNLJFD7+&LVAL@ <Loose, unstable talus slope with Wingate-derived soils. Some minor gullying across the plot, but vegetation remains homogeneous.Fairly shallow, rocky ravine filled with large colluvium chunks, but with intermittent sections of flat, sandy wash bottom. AMEUTA is clearly dominant, but may decrease upslope where JUNOST cover is higher.Extremely large colluvium (humvee-size) scattered throughout plot and polygon, but the majority of it is more like 1-2 square meters. One young PINEDU in plot. Hot, dry slope, but JUNOST are doing well on it.Weedy, disturbed low terrace with sparse shrub cover is in the floodplain; high terrace is 6-8 meters above low terrace and not in the floodplain. Rock cover is mainly concentrated on the slope (~23 degrees) between terraces. Portions of the high terrace outside plot to the N appear to be an ACHHYM grassland community; whereas, to the S it transitions to a clearer MU 15 community.Point captured the upper and lower terraces with two distinct communities. Upper terrace much less weedy and disturbed and probably very rarely flooded; lower terrace definitely in the floodplain. Mot form of EPHVIR present on low stabilized dunes on low terrace, but EPHTOR is the co-dominant shrub on the high terrace. Also, upper terrace much grassier and low terrace nearly devoid of grass.Mesic, N-facing talus slope with rocks ranging from baseball to truck-size. Saw FENRUP in polygon, but not in plot. Stable slope with crust development around plant bases, but regularly transected by rocky ravines and more active rock slides.Deep, sandy soils with good crypto crust cover; litter under trees mostly. Shrubs and grasses about equal in cover. More bedrock exposed here than at other points in polygon.Deep, sandy soils with developed crypto cover and attendant mosses; very little bedrock exposed. The microtopography is rolling hillocks, with some JUNOST at this point. There is more JUNOST than at AA0435, but less than 5%.LVAL @|"Shallow mounds of soil stabilized by cryptos in a mosaic with solid, and occasionally ledgy bedrock exposures. COLRAM dominates the understory.Area of stabilized dunes with small patches of active sands and spotty bedrock exposures. Cryptos are not well-developed, but cover the area. COLRAM shrubs are pedestalled, but doing well--quite robust. Many dead JUNOST skeletons.Pretty shallow soils with bedrock poking through here and there, and cryptos and moss stabilizing the soil. Small rocks lightly scattered across the soil. PINEDU and JUNOST co-dominate the overstory.Most of polygon is either a P-J/COLRAM or P-J/sparse understory woodland with extensive, well-developed cryptos dominating the understory. Wash cuts thru center of plot and is several meters wide, sandy-bottomed, with ledgy bedrock exposures along its banks. COLRAM cover much higher in areas of polygon surrounding plot. Tree cover ranges from 7-18%.Extensive COLRAM shrubland stabilized by well-developed and widespread crypto cover. Trees dotted throughout the polygon, as are small bedrock exposures in shallow wash channels.Lots of well-developed cryptos covering much of the soil. Robust PINEDU along edges of bedrock wash channel that cuts thru center of plot. ATRCAN in plot appears anomalous in polygon.Polygon is huge and, from what I've walked thru, varies from bedrock-dominated to P-J/COLRAM woodlands on deeper soils to areas more similar to this point. Still the polygon as a whole seems best described by MU 33 because bedrock exposures are ledgy and consistent throughout and soil development is shallow to moderately deep and has extensive cover over the bedrock. Very well-developed cryptos have consistently covered soil exposures. Plot has a real mixtures of shrubs, but polygon is more characterized by the dominance of COLRAM and PURMEX. PINEDU recruitment good, and overall are healthier-looking than the JUNOST.PLVAL l z*(pLow-growing, mot form of EPHVIR on microdunes stabilized by moss cover. Grass cover is equal to EPHVIR cover. Small gully (1-2 m. deep) cuts thru center of plot.Low-growing, mot form of EPHVIR is dominant and dense throughout area. This plot captures a transition from BOUGRA-dominance in the understory (to the SW) to Stipa-dominance (to the NE). Still a shrubland, but becoming more shrub-herbaceous near NE end of plot.Low-growing, mot form of EPHVIR has dense cover throughout this area. BOUGRA is the dominant understory, but doesn't have high enough cover to make this a shrub-herbaceous type.Deep soils with very little and light crust development. JUNOST presence due to being in/near an ecotone. Shrubs are pedestalled, possibly due to sheet erosion with water running downhill thru plot from the paved ISKY road, which is ~60 meters SW of plot.Tons of well-developed cryptos everywhere! Large trees have denser cover in this head drainage area, surrounded by small cliff bands. COLRAM dominates the understory.Old dune area, now very stabilized, with only one tiny patch of loose sands. Crypto cover is everywhere, but only lightly developed and much of it is moss-covered. Many dead trees (look long-dead). Mot form of EPHVIR caps the dunes and has significant cover.A meandering wash bottom with many large bedrock exposures in bottom and along banks. Very sandy wash with patches of small rock cover. TAMCHI have been sparsely scattered along wash, one by plot center. JUNOST are very robust. Wash varies from 6-10 meters wide with mostly <1 meter high banks.Out on a sandstone rim or point where bedrock is dominant. Very shallow soil pockets are mostly stabilized by cryptos. Many species are rooted in shallow joints. Several dead PINEDU in plot and area.Ledgy hillside with several large bedrock exposures supporting the rare occurrence of AMEUTA and CERMON. Below ledge in plot is an area of deeper soils, where COLRAM dominates. Crypto cover is patchy.X[  k  o &43@C2350Low levelGPS@New Alluvium0400002biotic soilPP00200T0000rpnljhfd`^\ZMIGEC?1% Bm3054MidslopeGPS@Talus/Colluvium/Landslides04000Tbiotic soilP0401-b0000000}{ywusnlhfYWUSQM1% A2334High LevelGPS@Obscured by Soil05000Pmoss040000000000nljhfdb`^\ZVPNLJHD2&!@p248MidslopeGPS0@Navajo SandstoneP0900TbiocrustPP0P00T0000mkigeca_][YWMKIGCA/#?'219High LevelGPS@New Alluvium03T1-b003biocrust1-bT01-b00T0000vtrpnljhca_ZPLJEC?1% >%1360High LevelGPS@New Alluvium02P02002biocrust03P01-a00T0000usqomkigb`^ZPLJFD@2&!=833High LevelGPSR@Kayenta Formation05P00PbiocrustPP0040000000pnljhfdb^\ZXNLJHFB/#<&5352High LevelGPSh@Kayenta Formation1-b06001-bbiocrust1-bP0P00T0000zxvtrpnljhfaWRPNJE2&!;*4250High LevelGPS@Obscured by Soil0500003biocrust1-a001-b0000000xvtrpnljeca\RNLJHD2&!:2270Low LevelGPS@New Alluvium1-a0P0PMoss0800000P0000jhfdb`^\ZXVRLJHFD?1% 9225High LevelGPS@Obscured by Soil060001-aMoss030000000000nljhfdb`^\ZVPKIGEA/#8+136High LevelGPS@Obscured by Soil0500002Moss030000000000omkigeca_][WQMKIGC1% 7/2208High LevelGPSz@Obscured by Soil07000PMoss030000000000nljhfdb`^\ZVPNLJHD2&!6,226High LevelGPS@Obscured by Soil050001-bMoss030000000000pnljhfdb`^\XRMKIGC1% 51541High LevelGPS@Kayenta Formation0204P003Biocrust1-bT0T0000000wusqomkigec^TPNLHD1% 4542MidslopeGPS@Obscured by Soil0202P003Biocrust02T0T00T0000sqomkigeca_[QMKIEA/#3 ,2208High LevelGPSF@Obscured by Soil0500002Moss030000000000pnljhfdb`^\XRNLJHD2&!2 &240High LevelGPS@Obscured by Soil0500002Moss030000000000omkigeca_][WQMKIGC1% 1 )242High LevelGPSd@Obscured by Soil0500002Moss030000000000omkigeca_][WQMKIGC1% 0 ,260High LevelGPS@Obscured by Soil08T00PBiocrust1-bT0T00T0000rpnljhfdb`^YOMKIGC1% / 5228Low levelGPSP@Kayenta Formation1-bP0006Biocrust1-bP01-b00T0000ywusqomkfdb]SOMKID1% .{4311MidslopeGPS @Aeolian Sands0T05004Biocrust1-b00000T0000pnljhfdb`^\WMIGCA?0$-L2257Low LevelGPST@New Alluvium002040PBiocrust02P01-b00T0000rpnljhfd_][WMKIEA?1% LVAL H 0 vA very sparse, mostly biotic soil or pebbly soil environment.Shrubs are slightly pedestalled and soils around shrubs are stabilized by crypto cover. Lots of EPHTOR mixed in with the COLRAM. An extensive, homogeneous community stretching north and east of the plot.An extremely dense FORPUB community transitioning to a MAHFRE shrubland outside polygon to the SW and into an OSTKNO woodland inside polygon to the S. POPFRE limited to edges of wash that runs adjacent to bare slickrock ramp on N end of polygon. Quite a unique and anomalous "green spot" in the midst of so much rock and sparse vegetation.Low-growing, mot form of EPHVIR has very dense cover in this area, far higher than the grass species combined. Moss cover is light and patchy, but soils stabilized by plant cover. Old road cuts through center of plot.Low-growing, mot form of EPHVIR co-dominates with several grass species. Unlike most of the polygon I've seen, HILJAM is the dominant grass in this area. Soils are stabilized by moss and very lightly developed cryptos.`Low-growing, mot form of EPHVIR co-dominates with several grass species. Soils much sandier here, with very little moss cover or stabilization, but don't appear to be loose, blowing sands.Several very robust JUNOST scattered in plot and area. Low-growing, mot form of EPHVIR dominates, but several grass species contribute significant cover. Crust development is light and patchy, mostly moss.Shallow soils extensively covered by well-developed cryptos in a mosaic with rolling bedrock exposures. JUNOST appear stunted, but PINEDU fairly tall. Several large, dead PINEDU in polygon. Lots of die-back on CERINT.COLRAM cover in the polygon as a whole is probably twice as high as it is in this plot. Undulating low hills transected by gullies with some bedrock exposures in the bottoms of them. Crypto cover is fairly well-developed and extensive throughout polygon.:LVAL F v0XThe trees are concentrated along the southern edges of this polygon, where bedrock outcrops are more common.The plot is in a rolling terrain of small hills. Vegetation density varies a bit with the local slope and aspect, but the plot is still similar to the rest of the polygon on average. Weedy with annuals.A very grassy shrub-herbaceous type, with grasses having 3x the cover of EPHVIR. Moss cover is very patchy and not very extensive. EPHVIR occurs as scattered mots and not as the grass-like form typical of this area.A steep Navajo dome that ramps down to a vertical cliff below (north of point). Plants are growing in cracks in the slickrock, or in tiny and sparsely scattered soil pockets stabilized by plants and some crypto cover. CERINT is the predominant plant found throughout this polygon.A very sandy, narrow (2-3 meters wide) wash dominated by PURSTA in the understory; but very ecotonal, with surrounding wooded COLRAM shrublands. Banks are well-stabilized by cryptos. COLRAM shrubland has cryptos and small rocks co-stabilizing the soils.A very narrow wash community, with the actual wash channel only 1-2 meters wide and sandy-bottomed with scattered small rocks and bedrock exposures. High COLRAM cover due to the whole wash community being ecotonal along its banks with a JUNOST/COLRAM Wooded Shrubland (MU10T) surrounding it. JUNOST have lots of die-back and dead branches.A huge, homogeneous polygon of COLRAM, stretching west from the plot. EPHTOR cover is consistently one-fourth to one-sixth the cover of COLRAM. Very little crust development here, and soils are instead stabilized by an extensive coating of very rough, marble-sized rocks half-embedded in the soil.A real melting pot, one of each kind of shrub. JUNOST are stunted, but CERINT are robust, with some as tall as the JUNOST. Soil pockets are shallow, are scattered across the bedrock in depressions, and are stabilized by cryptos. The vegetation is dense, considering how limited the available soil niches are.LVAL Relatively lush, with weedy annuals, but the perennials are sparse. PLEJAM occurs in limited small clumps, mostly near a shallow drainage transecting the plot.Plot is in an area with some variety of slope. About half of the plot is similar to AA0773, but the other half is an extremely steep, eroding area with less (though similar species) vegetation density. Less steep areas have a consistent ATRGAR cover.Polygon and plot are steep, bouldery talus, with lots of huge Wingate house-sized boulders. Soil areas are limited and tend to be rocky. Large boulders probably create shadier areas than aspect would imply. The western half of the polygon is drier, with smaller boulders and more southerly aspect--ATRGAR is the only shrub there. Other shrubs concentrate on east edge of polygon.Some soils are fine sands with a duney topography, although surfaces are generally vegetated. Some small blowout areas do occur. The area and polygon are also transected by multiple shallow drainage channels, and a large one transects the plot--with a different species list. Also included in the plot is a platey-pebbled area with high soil rock content--where the EPHTOR dominates.Plot and polygon are characterized by flat alluvial surfaces composed of materials transported from the canyon walls--this is not a stream terrace! Many superficial, braided run-off channels transect the area. One larger such channel crosses the plot, increasing the large rock content above the norm for the polygon, and contributing to the CHRNAU density--it's missing from much of the polygon.Occasional outcrops of Chinle here and there, but most of the slope in the plot is soils and rock of Wingate origin. The plot is in an area with significant gullying, but the microtopography doesn't seem to affect vegetation density or composition. Soils tend to be deep, and often protected by very large talus blocks. I would definitely not characterize this community as "sparse.".W 7 $ w  qcnvjZ4S4318Toe slopeGPS@Chinle Formation03T0006biotic soilPT0P00t0000trpnljhfdb`^QMKIGC1% Y330350MidslopeGPS@Talus/Colluvium/Landslides03000Pbiotic soilP0300300T0000}{ywusomigZXVTRN2&!X219340MidslopeGPS@Aeolian Sands0600003biotic soil1-aP0P00T0000usqomkigeca\OKIGEA2&!W11250Low levelGPS@New Alluvium080T001-aT01-a00T0000geca_][YTRPKKIGEC?1% V0220High LevelGPS@Chinle Formation020001-abiotic soilTP00600020000ywusqmkieca_RMKIGC1% U/5252MidslopeGPSZ@Chinle Formation1-bP00Pbiotic soilP0300500T0000vtrpnljhdb^\OMKIGB0$T.4262High SlopeGPS6@Chinle FormationPP00Pbiotic soilP0400400T0000usqomkigca][NLJHFD2&!S-3300Low levelGPS@Chinle Formation06T000PP00300T0000geca_][YUSQOOMKIGC1% R,2330Low levelGPSL@Chinle Formation1-b00005biotic soilTT0040000000wusqomkieca_RNLJHC1% Q+10160Toe slopeGPSz@Chinle Formation02P02003biotic soilTP00500020000|zxvtpnlhfdbUQOKIE3'"P*5250MidslopeGPS@Chinle Formation04PT01-abiotic soilTP00400T0000vtrpnljhdb`^QLJHFB0$O)3190Low levelGPS>@Chinle Formation04TP01-abiotic soilP1-a00400T0000zxvtrpnlhfa_RMKIGC1% N(5298MidslopeGPS@Chinle Formation03T0003biotic soilPP0030000000usqomkigca_]PLJHFB0$M'3324Low levelGPS@Chinle Formation03T0002biotic soilPP00300T0000vtrpnljhdb`^QMKIGC1% L&2342Low levelGPS@Chinle Formation02T0002biotic soilP1-a0050000000ywusqomkge`^QMKIGC1% K%1094MidslopeGPS@Chinle Formation1-aP00Pbiotic soilT020070000000wusqomkiec_]PNLJHC1% J$350Low levelGPSP@Chinle Formation1-bP001-abiotic soilTP0070000000wusqomkieca_RMKIGB0$I#2678MidslopeGPS@Talus/Colluvium/Landslides02000Pbiotic soilP0600200T0000~|zxvtrnlhfYWUSQM1% H"17330MidslopeGPS@Chinle Formation03P00Tbiotic soil1-a0200400T0000zxvtrpnlhfb]PNLJHD2&!G!18348Low slopeGPS2@Talus/Colluvium/Landslides1-a002001-a0501-a00T0000|zxvtrpnigc^^\ZVTO3'"F 35148MidslopeGPS@Talus/Colluvium/Landslides02000Tbiotic soilT050030000000}{ywusomigZXVTRN2&!E833168MidslopeGPS@Talus/Colluvium/Landslides02000Tbiotic soilT050030000000}{ywusomigZXVTRN2&!D2244Low levelGPS@Aeolian Sands030020Pbiotic soilPP00300T0000sqomkigea_][NLJFD@1% LVAL v\Very weedy, with annuals--makes photo appear lush! However, the perennials are quite sparse--and much of the Atriplex is quite small in stature. PLEJAM only occurs in a couple small patches. Collema dominates bio soils here.Lots of weedy annuals here, but perennials are sparse. Biotic soil is about evenly mixed between Collema and moss. Atriplex is very sparse in most of plot, but is concentrated along a superficial drainage- where the only rare clumps of PLEJAM also occur.Shallow, superficial drainage runs throughout the plot, but it doesn't affect the vegetation. Lots of annuals are growing here, but the perennial cover is sparse. Biotic soil is about evenly mixed Collema and moss.Plot includes a very small "ridge" of bedrock outcrop on the larger bench--thus increased slope over AA0741 (nearby). Vegetation seems unchanged, though biotic crusts are less present. Density of vegetation is decreased somewhat, though the variety is slightly greater.The plot is on a broad bench formed by the Mossback member of the Chinle. Soils are sandy but quite thin, with lots of platey small rock. Lots of weedy annuals present.The plot is an a lower-angle "bench" above Mossback cliffs, but most of the polygon is steeper-sloped, with a wide spectrum of aspects. West-facing and northeast-facing parts of the polygon are quite different, community-wise. The plot is in a transitional area, but more closely fits the northeast-facing community. (The west-facing area is an ATRCON/LEYSAL community in a limited area.)Plot is a narrow ~20-25m) drainage ravine descending from an overhanging pouroff, bounded by steep talus slopes. The terrain is characterized by very large boulders with small sand areas between them. Vegetation tends to be concentrated on the margins of the wash, between large boulders (protection from flash flooding). North of plot, polygon loses the large shrubs and becomes an open desert sand wash.LVAL $  FDuney tomography with stabilized soils. Mots form dune tops.Stabilized soils with a duney topography. The soils are deep (except in a small area of bedrock).Soils are rockier here than in AA746 and 748. Several recently dead pinyons reduce PINEDU cover relative to juniper in the plot.Sandy soils with some larger cobbles SARVER is often slightly pedestalled from wind blow-outs of surface, but those aren't dunes.Lots of platey, small, silty sandstone pebbles on the surface. Some areas in the plot have significant biotic soil patches--though it's probably at least as much moss as lichen. Other areas are just small rock on a silty, buff-colored soil. Weedy annuals make the place look a bit more lush than the perennial cover suggests.The plot is on the top of a bench formed by Mossback member of Chinle. Soil surfaces are very rocky with pebbles. Soils are a buff color with gray-brown rock. Biotic soils are significant in small patchy areas, but much of the plot is just small rock cover, composed of silty-sandstone-platey-pebbles.The plot is on a low mound or "hill" on the bench comprising this polygon. Soils are very rocky, with platey sandstone surfaces, and only traces of biotic soils. PLEJAM is concentrated around bedrock and areas of larger surface rocks. Lots of weedy annuals in some areas of the plot.The plot is the entirety of a small bench created by the Mossback (on top of Mossback) member of the Chinle. As such, it is really a small inclusion in the polygon, more closely resembling the nearby polygon that includes points 647, 642 and 676. Soils are silty sand, gray in color, and have lots of small rock. No biotic soil.A high degree of biotic soil crusting here. Weedy annuals contribute to a "more lush" look, but the perennial community is quite sparse. The only PLEJAM in the plot, and apparently the polygon, occurs near small rocky outcrops--but most of the polygon is a platey pebble or biotic soil surface.LVAL T >XAn anomalous patch of slickrock exposed in a blow-out, but otherwise a typical weedy EPHVIR/grass plateau.A very flat bench on a maroon sandstone member of the Chinle. Very shallow soils. ARTCON % was once higher, perhaps even 3%, but it's now mostly drought-killed in the plot. The southeast areas of the polygon have slightly deeper soils and more live ATRCON.Steep, bouldery, north-facing talus and soils derived from the Wingate. The plot appears to be in a slightly lusher area compared to the surrounding areas of talus--but has the same community.As with AA0577, this plot is located at the "back" of this broad Mossback bench, where the slopes are slightly steeper and more eroded than on and near the rim (where the biotic soil rules). COLRAM generally only occurs in the plot on the upslope areas without biotic soil. PLEJAM is concentrated in the areas of COLRAM, and is relatively sparse in the pure ATRCON areas.Gray soils. The plot is close to the back of the bench composing the polygon, and has some slightly steeper, less-developed slopes, but down slope portions are very well-developed biotic soils. COLRAM only occurs on upslope areas of the plot without the biotic soils.Steep talus below the Mossback layer. Lots of sandy conglomerate rock. Very diverse community! These are soils derived from the sandstone and conglomerate layers of the Mossback--NO gray clay soils here.This is an intriguing plot with a mix of environments. About two-thirds of plot is the primary association--in a curious mix of stabilized sands (old dune?) with layers of rock likely deposited from down slope erosion. The remaining one-third is on native Moenkopi on the west edge of the polygon--not representative of the majority of the polygon (which continues the primary association to the east). Note that the very northeast areas of the polygon are an EPHTOR/ATRCON community, however! A very heterogeneous polygon.T^  c  m #mp%CFrL2330High LevelGPS@Obscured by Soil0600002crypto1-b00P0000000sqomkigeca_ZRNLJHD2&!qK2342High LevelGPS@ Obscured by Soil0600002cyrpto1-b00P0000000sqomkigeca_ZRNLJHD2&!pJ24High LevelGPS@Obscured by Soil08T001-bDark cyano1-a00T0000000usqomkigeca\PKIGEA/#oI7270High LevelGPS@Kayenta Formation1-b0700PCryptosPP01-a00T0000vtrpnljhca_]TRPNJE2&!nH2219Low levelGPS"@New Alluvium0200600PP0020000000eca_][YWSQOMMKIEC?1% mG2212Low levelGPS@@New Alluvium0200600PP0020000000eca_][YWSQOMMKIEC?1% lF3202High LevelGPS@Chinle Formation031-aP002BiocrustP1-a0020000000zxvtrpnlhfa_UQOMHD2&!kE3185Low levelGPS@Aeolian Sands000900T001-a0000000eca_][YWRPNLLJHDB@1% jDflatn/aLow levelGPS@New Alluvium1-aP1-a00T1-b0060000000pnljhfdb^\WUUSQLJE7+&iCz2932MidslopeGPS@Talus/Colluvium/LandslidesP000TCryptosT0700200T0000zxvtrpnlhfb`WUSQOM1% hBN5331Toe slopeGPS@Older Alluvium050P003Cryptos1-bT0T0000000qomkigeca_]XOKIGEA1% gA24329High SlopeGPST@Talus/Colluvium/Landslides1-a000PCryptosP0600200P0000~|zxvtrnlhf][YWUP4(#f@8330Low LevelGPST@New Alluvium1-a01-b00P0701-a00T0000jhfdb`^\WUQOOMKFD?1% e?2212Low levelGPS@Aeolian Sands0501-a003Biocrust1-a00000T0000trpnljhfdb`[QMKFD@1% d>3276Low levelGPSz@Aeolian Sands070001-amoss020000000000mkigeca_][YUOJHFD@1% c=2288Low levelGPS@Aeolian Sands05P0002biotic soil030000000000sqomkigeca_[NJHFD@1% b<598MidslopeGPS@Navajo Sandstone04T0003biotic soilP000200T0000trpnljhfb`^\OKIGEA/#a;5140MidslopeGPS@Navajo Sandstone04P0004biotic soil1-a00000T0000vtrpnljhfdb]PLJHFB0$`:5154MidslopeGPS6@Aeolian Sands030050Tbiotic soil1-b00000P0000sqomkigeca_ZMKIEC?0$_9K14Low levelGPSR@New Alluvium02T001-bbiotic soilPT0060000000pnljhfdb^\ZXKFDB@<."^81174High LevelGPS@Chinle Formation1-b1-a000P1-a00800T0000omkigeca][VTTRPNID2&!]7374MidslopeGPS@Talus/Colluvium/Landslides020000T0400400T0000qomkigec_]YWWUSQOK/#\6T4312Low slopeGPS@Chinle Formation04P00Tbiotic soilTP00400T0000trpnljhfb`^\OMKIGC1% [5Q4314Toe slopeGPS@Chinle Formation03P0002biotic soilPP00300T0000vtrpnljhdb`^QMKIGC1% LVAL x j PApparently deep soils stabilized by mostly cryptos--typical ISKY mesa top Mormon-tea environment.Pebbly wash with sandy banks and a few shaley outcrops. Trickling water in some areas of wash, may just be from rainfall yesterday.Steep, very bouldery slope with deeper erosional gullies and a little crypto crust development. Surface has high small rock cover.Broad, sloping terrace below colluvial slope and above wash. Terrace has good crypto development. Channel with a couple large rocks and anomalous shrubs (CHRNAU, RHUARO) runs through plot, but we did not include this on the veg. list.This NW-facing slope is convex in shape, therefore a little drier than typical. Good cryptobiotic soil for a talusy slope. Giant (~ 4 m. wide) boulders littering slope.Moderately steep, talusy wash with giant car-sized boulders. Some water trickling through parts of the canyon (not here), but this may be from rain in the last 24 hours.The soil is sandy and mostly stabilized, but there are isolated spots in the plot and polygon where the sand is loose and blowable. Lower parts of the plot could flood, but most of it is above the high water mark. Biocrust is extensive, but much of it has sand on it.Much more stabilized, though still sandy soils than AA748. Biotic soil is extensive and dominates all areas of soil except under trees.The polygon and plot have duney topography with some blowout areas. COLRAM is often on pedestal roots. Trees are denser on the west side of the polygon, where the plot is located. Ephedra is mot form, but is limited in forming large mats. Sand movement is active on most of the plot.This is another bench formed on top of the Mossback member of the Chinle. However, soils here are sandy and buff-colored, and I suspect much of it is derived from the weathered Wingate talus covering most of the steep slopes to the south (below Wingate cliffs). Soils are relatively deep in areas.nLVAL * V 44lSoil well-stabilized with crust here. Shrubs are big and happy here. DESPIN is all clustered under the trees.Flat bedrock peeking through crust-covered soils, and one bedrock scarp just northeast of the point.A fairly steep, but very stable slope between large Kayenta outcrops. PINEDU is abundant and healthy-looking; the shrub understory is pretty sparse, but diverse. Tall, well-developed, lichen-covered cryptos stabilize the soil well.Deep soils with lumpy-moss-crypto stabilizing the surface. Not as much dark crypto evident here.Apparently deep soils with mossy cryptos stabilizing the surface. A few shrubby junipers are invading the area.Seemingly deep soils with mossy cryptos stabilizing the surface. DESPIN in full bloom now, so has high cover at the moment.Huge sandstone shelves with smaller areas of soil collected on the steps. A few pockets of soil with really well-developed cryptos, other pockets are more pebbly. A few big soil/veg. potholes are here too.Many very shallow, sandy wash channels are braiding down the canyon floor here, but overall the polygon is more reminiscent of an upland terrace.Very shallow, sandy wash channels braid through this area. Some areas of wash are pretty pebbly. The area overall seems very dry and sands are not stabilized.Point falls on broad bench between steep talus Chinle slopes above and Moenkopi slopes below. Numerous outcroppings of very rough-textured, but flat (Mossback?) bedrock, and large slabby rocks in plot. Some small platey rocks made of the same stuff litter the area too. Well-developed, black lichen-covered (but not gypsiferous) cryptos cover soil where it is stable enough for cryptos. Soils are tan in color, and are somewhat clayey though very gritty.Slightly rolling terrace about 5 feet above the wash. Soil has very little cryptobiotic crust development with some small rocks scattered throughout; and shrubs pedestalled throughout and mounding (coppicing) denote aeolian influence.fX M L C J>><c$280High LevelGPSX@Kayenta Formation0000000000000000db`^\ZXVTRPNNLJHFD1% b(3342High LevelGPS@Kayenta Formation05P00PcryptoPP00400T0000qomkigec_][YQOMKIE2&!a2287High LevelGPS@Kayenta Formation031-b1-a003biocrust1-b00T00T0000|zxvtrpnljhcYUSNIE2&!` 1285High LevelGPST@Aeolian SandsP00801-abiocrust1-a00T00T0000sqomkigeca_ZPKIECA2&!_flatn/aLow levelGPS@New Alluvium1-a01-a0PWater07T0P001-a0000wusqojhfdb`\USQLJE7+&^=3251High SlopeGPS@Navajo Sandstone04031-a0Pbiocrust1-aT0P00P0000xvtrpnljhfd_USQLHD2&!]6flatn/aHigh LevelGPS@Obscured by Soil080P001-a0000000000omkigeca_][VVTRPNJ8,'\)flatn/aHigh LevelGPS@Aeolian Sands040040Pmoss1-b0000000000trpnljhfdb`[USQMKG8,'[-flatn/aHigh LevelGPS@ Obscured by Soil0801-a0Pbiocrust1-a00000T0000|zxvtrpnljhcYWUPNJ8,'Z/flatn/aHigh LevelGPSR@Obscured by Soil0701-a0Pcrypto1-b00000T0000zxvtrpnljhfaYWUPNJ8,'Y02252High LevelGPSJ@Obscured by Soil070P01-abiocrust1-b00T00T0000vtrpnljhfdb]SNLJHD2&!~X47High LevelGPS@Kayenta Formation04PP002biocrust1-bT01-a00T0000vtrpnljhca_ZPLJHFB/#}W,1270High LevelGPSR@Obscured by Soil05004001-a00000T0000kigeca_][YWRRPNJHD2&!|V5238High SlopeGPS@ Kayenta Formation04T0004biocrust1-bT0T00T0000vtrpnljhfdb]SOMKIE2&!{U5290High LevelGPSR@Kayenta Formation02P02004crust1-bP01-a00T0000xvtrpnljeca\UQOKIE2&!zTd4211High SlopeGPSn@Kayenta Formation1-b050002biocrust1-aT0P00T0000ywusqomkige`VRPNJE2&!yS865High SlopeGPSH@Kayenta Formation041-a000P1-b0030000000nljhfdb`\ZUSSQOMHD1% xRs62High SlopeGPS@Kayenta Formation03030002biocrust1-bT0T00T0000usqomkigeca\RNLJFB/#wQt4106High SlopeGPSl@Kayenta Formation021-bP003crust1-b1-a01-b00T0000|zxvtrpnigb]VRPNIE2&!vPi7160High slopeGPS@ Kayenta Formation02020003biocrust1-b1-a0P00T0000{ywusqomkid_UQOMIE2&!uO20331MidslopeGPS@Kayenta Formation02P0003biocrust1-b1-a00200P0000{ywusqomigb]SOMKIE2&!tN158High LevelGPS@Obscured by Soil080001-bcrypto1-a00T0000000sqomkigeca_ZRMKIGC1% sM2320High LevelGPS@Obscured by Soil0500003crypto0200T0000000rpnljhfdb`^ZRNLJHD2&!&LVAL  Z fHSlightly rolling, microdune topography with more loose, blowing sand in the ARTTRI community and a few cryptos (mossy) in the EPHVIR community.Slightly rolling, micro-dune topography with more loose, blowing sand in the ARTTRI shrubland; and more stabilized substrate (with some cryptos) in the EPHVIR shrubland.There is a definite boundary between these two shrublands with almost no transition, but I'm not sure what environmental factors are making the difference. The ARTTRI community has micro-dunes with some loose sand, whereas COLRAM shrubland has soils stabilized with bio- and physical crusting.Extensive biocrust and physical crusting has the soil well stabilized in the plot, except for one drainage channel that cuts through the middle of the plot. Many small, chunky rocks are scattered over the soil surface.Undulating microdunes with a lot of loose sand. Interdune areas are mostly stabilized, with what looks more like a physical than a biological crust (no filaments in it).A few Kayenta outcrops peeking through the nicely crypto-stabilized soil. Lots of die-back on JUNOST, and dead trees around. PINEDU, though less abundant, looks happier.Shelfy, solid bedrock with thin soil pockets on top. Most of the soil is covered with nice crypto, although there are areas outside of the point with thin aeolian dunes over the rock.Plot wraps up over a small ridge to the southwest of plot center, where soils seem more clayey and ATRCON & EPHTOR occur. The area is very shelfy, but deeper soils cover the shelves than in other areas of the polygon, and soil surface seems too clayey and rock-covered for crypto development.Well-developed, licheny cryptos stabilize the thin soils here--other areas of the polygon look like they have more aeolian influence. Weedy forbs and Festuca are clustered under the PINEDU here.Thin soils with well-developed cryptos cover the vast majority of this AA point. Pebbly and platey rocks are scattered over the surface. Bedrock exposure is no greater than 15% here.LVAL    h BThis slope is covered with giant boulders that came from the Wingate above. There might be a little Chinle soil showing through in spots. Some of the colluvium looks pretty recent.A few plants grow in the cracks of this huge Navajo ledge.One piece of bedrock is exposed in a blowout--otherwise, this area appears to have deep soil and is very crust-stabilized.The point falls on a largely unvegetated Navajo outcrop, with most of the plot falling on the north-facing side, where there are some soil shelves and potholes with vegetation.Very rolling, duney area with soils mostly stabilized by cryptos (dark cyano and some moss). A lot of JUNOST skeletons in the area.Dark cryptos cover the soil where it is stabilized, and a few areas have loose, blowing sand on small dunes. There are lots of weedy annuals here, despite the crypto cover.Dark red soil with lots of pebbly rocks scattered over the surface.Kayenta bedrock poking through mostly well-stabilized aeolian deposits. One large dune falls in the plot.Rolling topography in definite duney area. EPHVIR is growing on sand mounds in a mostly grasslike form. Some stabilization of a few areas with bio- and physical crusting.Very mesic, sheltered, narrow canyon bottom. Wash runs due west and has 1/4 to 1/2 inches of trickling water in it. Lots of limb fall from POPFRE littering the ground, and leaf litter everywhere. Thick, mesic tall shrubs dominate the understory.The polygon appears to delineate an area with broken Navajo outcrops protruding through the soil (see photo 1), but also includes lesser areas of small dunes collected between outcrops (see photo 2).Soil seems mainly stabilized by a physical crust, but there is a bit of loose sand in small depressions as well. The area seems pretty thrashed--the only thing that looks happy here is the EPHVIR.Low, rolling dunes with a lot of loose sand and only a few patches of moss and physical crusting to stabilize soil.MB O  u  } .8Am#{2249Low levelGPSV@Moenkopi Fm020P00TT0070000000b`^\ZXVTPNLJJHFDB>1% z8190Low slopeGPS@White Rim Sandstone - Cutler GpP09T0TbiocrustTT0T0000000~|zxvtrpnljh^\ZXTR1% y6324Toe slopeGPS@ Moenkopi FmPP000PP0080000000`^\ZXVTRNLJHHFDB@>1% x4204Toe slopeGPSV@ Moenkopi FmPPP00TP0080000000`^\ZXVTRNLJHHFDB@>1% wJ2038MidslopeGPS@Chinle Formation03T000T020040000000igeca_][WUQOOMKIGC1% vW2172MidslopeGPS@Chinle Formation02P000P030040000000igeca_][WUQOOMKIGC1% u935258MidslopeGPS~@Chinle FormationPP000T090P0000000fdb`^\ZXVTPNNLJHFD2&!t3333Low levelGPS@Aeolian Sands020070PBiocrustP00000T0000nljhfdb`^\ZXNLJFD@1% svariablevariableLow levelGPS@Aeolian SandsP007002BiocrustP0000000000}{ywusqomka][WUSD83(r7190InterfluveGPSJ@Moenkopi FmPP00PBiocrustTT0080000000kigeca_]YWUSIGECA?2&!q16208Low slopeGPS@Moenkopi Fm03P00PBiocrustT1-b0040000000qomkigec_]XVLJHFD@3'"p2311Step in slopeGPS@Chinle Formation02TT006BiocrustTt01-b0000000xvtrpnljeca_UQOMKG5)$oB30237MidslopeGPS@Chinle Formation02P000T050020000000jhfdb`^\XVRPPNLJHD2&!nS2595MidslopeGPSl@ Talus/Colluvium/LandslidesP000PbiocrustT090P0000000ywusqomkigcaWUSQOM1% m18230MidslopeGPSt@ Navajo SandstoneP090000T0T00T0000fdb`^\ZXVTRPPNLJFD2&!l+450Low levelGPS@Talus/Colluvium/Landslides02PP0Pbiocrust03030p00P0000|zxvtrpnljfbXVTRPL0$kflatn/aLow levelGPS0@New Alluvium08000Pbiocrust1-b00000T0000trpnljhfdb`[QOMKIE7+&j65Toe slopeGPSH@Moenkopi FmPP001-abiocrustPP0070000000jhfdb`^\XVTRHCA?=;."i1237Low levelGPS@Aeolian Sands060030P1-a00000T0000geca_][YWUSNNLJFD@1% h6234Low slopeGPS<@Moenkopi Fm021-aT0PP020040000000geca_][YUSOMMKIGB>1% gJ25248MidslopeGPS@Talus/Colluvium/LandslidesPT00PT090T00T0000pnljhfdb`^ZXXVTRPN2&!f4336High LevelGPS@ Obscured by Soil05T0004crustP0000000000omkigeca_][YRNLJHD2&!e821High SlopeGPS`@ Navajo Sandstone1-a0900TbiocrustTP0P0000000rpnljhfdb`^\RPNLHC1% d!variablevariableHigh LevelGPS@Obscured by Soil02T03003crypto1-b00000T0000~|zxvtogca][WE94(LVALj . dThe slope is down the canyon. The steep, nearby sides of the canyon are Chinle, but the bottom is full of alluvium and colluvium. There is water flowing in the stream and the lush vegetation makes me think this is a perennial flow.This is a large flat area of deep, silty soil. Some areas show signs of water running or pooling. The north side of the plot is a little sandier and holds most of the sand sage and a little biocrust. The south, silty side is dominated by annual weeds - especially cheat grass.The terrain is a series of low toeslope ridges alternating with small washes - two of which cross the plot. The surface is covered with limestone rocks and pebbles. A mound of biocrust covered, gypsiferous soil is also partly in the plot. The plants are well spaced and seem to be stunted.The sand here is mostly stabilized by plants and young biocrust, however, significant areas in the plot and polygon are not stabilized and the vegetation is different in these areas. It looks like flood waters have flowed through here beyond the wash banks. Annual weeds carpet some areas. There was no room on the species list for all the weeds present.Map unit 37 best fits the vegetation here, but the geology is wrong. Map unit 15 is a good fit for the part of the plot outside the ravine and probably represents the polygon better. The first association choice is for the ravine. Many more species not listed are present in trace amounts. The second association choice is for the part of the plot outside the ravine and probably better represents the polygon.Giant boulders fill this polygon and completely cover the underlying Chinle bedrock. Plants are growing between the boulders and in tiny accumulations of soil. Some of the boulders are house-sized and many are car-sized. The polygon is in a ravine and is much more shady and moist than some neighboring slopes in other polygons.vLVAL @ n z`fThis is a vast, gently rolling plain. The soil is sandy, well-stabilized by fairly thick vegetation.This is the last toeslope of the Moenkopi, transitioning into the nearby White Rim. A few shallow drainage channels cross the plot, but don't affect the vegetation. A little bedrock is exposed, but the surface is mainly this soil covered with pebbles.This is the last toeslope of the Moenkopi before it peters out on the White Rim Sandstone. There's a little bedrock showing, but the plot is mostly thin soil covered with little rocks. A couple of shallow, sandy drainage channels meander through the plot, but they don't seem to affect vegetation.A few big boulders from the Wingate have landed on the plot. Most of the rocks are from the Chinle and some purple and gray dirt is showing. A couple of erosion gullies go through the plot but don't seem to affect the vegetation.This is a steep rocky slope with some purple and gray soil showing in some spots. Most of the colluvium is Chinle-derived.Much of the Chinle slope is covered with colluvium from the Wingate above. Boulders range from major appliance sized to small house sized. Plants are growing in small accumulations of soil.Parts of these active dunes have been stabilized by biocrust and plants.Some of the dunes are up to 10 feet high and active. Some flatter areas are stabilized by biocrust and vegetation.The plot includes three gullies and three interfluves, but the vegetation isn't much affected. The surface is almost completely covered with flat rocks and pebbles.The terrain is a series of ledges about 20 feet high with sloping piles of soil filling in between the ledges. The surface is light-colored with a good coverage of flat rocks and pebbles. A few gypsum crystals decorate the scene.This is the bottom of the Chinle where the toeslope flattens out on the Moenkopi bench below.This slope has a lot of colluvium from the Wingate on it. However, much Chinle soil is exposed.LVALd This is the relatively flat plateau area by the NPS entrance sign. The microtopography has variable slope / aspect as it is rolling small hills with shallow small drainages through and very high crypto cover with some lichen and mosses as well. Stable, deep, soil with little bedrock exposed.*Note: Environmental Data from SS. SS: A very bouldery ravine at the bottom of a tight canyon. Boulders collect smaller rocks and debris around them. Many pour-offs in this canyon. Some puddling of water possibly from downpour two days ago. PW: Wash is very narrow, bounded by slickrock and colluvial toe slopes. The wash bottom is bouldery, and has frequent sections with little vegetation. POPFRE was in one clump of several crowns, bounded by Rhus and Amelanchier.This area of Gray's Pasture is a little weedy. The sandy soil is well-stabilized by plants and biocrust.This is the gently rolling Gray's Pasture. The sandy soil is well-stabilized by plants and biocrust. The Ephedra is the "mot" type here.This community owes its vigor to the slickrock outcrop on the east side that shelters it and concentrates precipitation. Big trees and shrubs seem quite happy here.This is classic Moenkopi terrain with thin-rock ledges and red dirt covered with pebbles. This aspect has more dense vegetation than sunnier sites, but the species present are about the same. The plot is in a concave bowl with several erosion gullies running through it.This is a nice little valley in the lower Moenkopi. The plot is right in the drainage bottom, but the vegetation and soil surface is not much different than the surrounding desert. There's a little coarse red sand where water rarely flows, but that's the only suggestion that this might be a wash.The White Rim slopes gradually down to the river here and the plot landed in a concavity that collects a little soil and channels water. There might be a few more plants here than other areas of White Rim.dx [  h "~0|]i3303MidslopeGPS@Aeolian Sands02002004biocrust1-aP01-b0000000usqomkigb`^YOKIEC?0$3127High LevelGPS@White Rim Sandstone - Cutler Gp0402P00TT0020000000ywusqomkgecaa_][WS2&!4variesHigh SlopeGPSl@Moenkopi Fm04000PbiocrustPT0060000000pnljhfdb^\ZXNLJHFB5)$4317Step In SlopeGPS@Moenkopi Fm04P0001-aP0040000000igeca_][WUSNNLJHFB5)$4127Toe SlopeGPS@White Rim Sandstone - Cutler Gp06P00PbiocrustPT00300T0000~|zxvtrnljh^\ZXVR1% 4320Low LevelGPS@White Rim Sandstone - Cutler GpP0900PbiocrustPT0P0000000~|zxvtrpnljh^\ZXTR1% 4144InterfluveGPS(@ White Rim Sandstone - Cutler GpP09T0PbiocrustTT0T0000000}{ywusqomki_][YUS2&!475High LevelGPS@White Rim Sandstone - Cutler GpT0900TbiocrustTT0T0000000~|zxvtrpnljh^\ZXTR1% '4150High SlopeGPSV@Aeolian Sands050001-amoss040000000000nljhfdb`^\ZVPKIGEA2&!(5152High SlopeGPSV@Aeolian Sands060001-bbio & moss030000000000trpnljhfdb`\PKIGEA2&!)1186High LevelGPSP@Aeolian Sands060001-amoss030000000000nljhfdb`^\ZVPKIGEA2&!/2328High LevelGPS@Aeolian Sands060001-amoss030000000000nljhfdb`^\ZVPKIGEA2&!4300Toe slopeGPS@Moenkopi Fm03000PbiocrustP00060000000ljhfdb`^ZXVTJHFDB>1% f656High SlopeGPSx@Kayenta Formation1-b04P001-a1-b00200T0000qomkigec_]XSSQOMID1% 2199Low levelGPS@Aeolian Sands06002002biocrustP0000000000pnljhfdb`^\ZPLJFD@1% 12109MidslopeGPS@Moenkopi FmTP00Tbiotic soilT030060000000pnljhfdb^\XVIGECA?2&!variablevariableHigh LevelGPSL@Obscured by Soil1-aTT004crypto1-a1-a004001-a0000~zxsnfb`^\WE94(8314Low slopeGPS@Talus/Colluvium/LandslidesP01-a00P0601-b00P0000usqomkigb`\ZZXVQOM1% (flatn/aHigh LevelGPS@Aeolian Sands0400003biocrust0200000T0000wusqomkigec_UQOMKG8,'%2353High LevelGPS@Aeolian Sands0500002biocrust020000000000qomkigeca_]YOKIGEA2&!~010278MidslopeGPSJ@Navajo Sandstone0205P0Pbiocrust0200000P0000trpnljhfdb`\RPNLHD2&!}2330High LevelGPS@ Aeolian Sands070000020000000000eca_][YWUSQMMKIGEA2&!|10309MidslopeGPS @Moenkopi Fm1-aP000T020060000000fdb`^\ZXTRNLLJHFD?2&!LVAL   ~.pHMore pavement-like small rock on deep soils.This site has sloping, linear lumps of bedrock perpendicular to a large, sandy-bottomed wash just to the southeast of plot. Plants are growing happily in the linear, soil-filled cracks and pockets between the lumps. Biocrust is well-developed also in these soil-filled cracks.This plot has a little step in it that accounts for the slope listed. The actual slope of the flat areas is about 2 degrees. Very little soil has accumulated here. The plants are mostly growing in cracks. The large shrubs are growing in the shelter of the step.The plot is at the upper (north) end of Gray's Pasture. Soil is deep and stabilized by moss and vegetation. Ephedra exhibits some clumpiness, but sprigs pop up everywhere.The plot is at the upper (north) end of Gray's Pasture. Soil is deep sand stabilized by crust, moss and vegetation. Ephedra tends to be clumpy, but sprigs pop up all over.Soil is deep and sandy; well-stabilized.Soil is deep, sandy and stable. Ephedra is clumpy, with scattered sprigs.This toeslope is on the terrace above the riparian river corridor. The surface is gently undulating and mostly covered with pebbles. The biocrust is mostly in one patch and not throughout the plot.Broken shelves of sandstone are more like large humps cascading down the side of the dunes. There are many loose rocks around, so there is little chance for crypto buildup on soil surface.Plot/polygon is located on a broad, low wash terrace with significant areas of active dunes. Other areas in polygon are less duney and have stabilized soils. The vegetation is quite weedy with annuals. Biotic soils occur regularly in the stabilized areas.Area has a very high rock content, with platey rock on surface. Lots of low ledges and shallow transecting gullies. Grayer clay toeslopes around west perimeter of plot are essentially barren. The grey clays are the only areas with biotic soil.LVAL & HArea is mostly stabilized sand, with one large dune (1/4 of plot) at plot center. The alluvium is influenced strongly by the Moenkopi at the upper half of the plot as it creates fingers of harder, rocky soil and rocks dribbling down. Most of the Stipa is restricted to the dune, and the Hilaria is well-distributed everywhere also.Area is a well-stabilized sand sheet with one large dune in the SE side of plot. Biocrust is extensive everywhere else; moderately well-developed. Hilaria is evenly distributed everywhere except on the dune. Ricegrass is also evenly distributed. Rumex is confined to the dune. Artemisia filifolia is mainly along a narrow drainage at the NE edge of plot.This area has a thin layer of soil mostly covering the underlying White Rim sandstone. The soil is sandy, with many small pebbles decorating the surface. A few shallow erosion channels meander through the plot.This anomalous pile of dirt on the White Rim consists of fine-textured soil with a layer of pebbles and rocks on the surface, creating a desert pavement-like cap. Nearly all of the rocks are smooth with rounded edges, suggesting old alluvium, although the soil underneath is sticky when wet, like the Moenkopi.This expansive area is characterized by gently-sloping benches, cut with narrow, rocky erosion channels where the Stanleya grows. Soil surface is capped with flat, platey rocks and pebbles. Biocrust is practically non-existent.This site is very close to the Moenkopi geologic layer and there's even a little red Moenkopi dirt in the plot. Some areas of the plot have a little bedrock showing, and the soil is probably fairly thin. Many multicolored pebbles decorate the surface.This is a beautiful spot on the White Rim, characterized by slopey ledges and lumps with nearly parallel cracks heading toward the river. Vegetation is growing in cracks and on flat spots wherever shallow soil has developed sufficiently. Tall shrubs are not so tall here.<Q R  w 5 AebLz\12196MidslopeGPS@Moenkopi FmPP000T0200700T0000ca_][YWUQOKIIGECA?2&!35340MidslopeGPSR@Moenkopi Fm031-a000P0300300T0000hfdb`^\ZVTPNNLJHC?2&!x2300Low levelGPSj@Moenkopi Fm0400001-aP00400T0000eca_][YWSQOJJHFDB>1% 30240MidslopeGPSt@Talus/Colluvium/Landslides03P00Pbiotic soil1-a0300200T0000~|zxvrplgZXVTRN2&!\302Midslope1:24K Quad@Talus/Colluvium/Landslides031-b000P1-b00300T0000|zxvtrpnjhcaa_][VR6*B2330Low LevelGPS@New Alluvium05P1-b0Pbiocrust1-aP01-b0000000trpnljhfa_]XNLJEC?1% 26270MidslopeGPS@Talus/Colluvium/Landslides1-b1-b000P030050000000xvtrpnljfd`^^\ZXSN2&!62326Low LevelGPS@New Alluvium1-b01-b005bio & moss1-b1-a00200T0000{ywusqomigb]QMKFD?1% 1226Low LevelGPS@New Alluvium07PP01-bbiocrustPT0P0000000nljhfdb`^\ZXNIGEC?1% 1212Low LevelGPSp@New Alluvium0800000200000T0000ca_][YWUSQOKKIGEC?1% 1210Low LevelGPS@New Alluvium0601-a002bio & mossP0000000000rpnljhfdb`^\PLJEC?1% 1240Low LevelGPS@New Alluvium06002000200000T0000eca_][YWUSQMMKIEC?1% 1210Low LevelGPS@New Alluvium070030PbiocrustP0000000000mkigeca_][YWMKIEC?1% 21354High SlopeGPS@Chinle Formation02P00PmossP1-a0070000000sqomkigea_ZXRPNLJF4(#1200Low LevelGPSx@New Alluvium050P003bio & moss1-b0000000000rpnljhfdb`^YMIGEC?1% 1194Low LevelGPS@New Alluvium0500301-abiocrust1-a00000T0000sqomkigeca_ZPKIEC?1% 16Low SlopeGPS@New Alluvium000400T1-b00400T0000ca_][YWUQOJHHFD@><."3269Toe SlopeGPSJ@Moenkopi Fm070P0Pbiocrust1-aP0020000000omkigeca][YTJHFDB>1% 1277Low LevelGPS&@Aeolian SandsP009001-aT0P00T0000eca_][YWUSQLLJHDB@1% 1286Low LevelGPSb@Aeolian Sands0009001-a00T00T0000eca_][YWUSQLLJHDB@1% 3266MidslopeGPS@Aeolian Sands050P004biocrust1-a00T0000000pnljhfdb`^\WMIGEC?0$3250High LevelGPS@Aeolian Sands0401-b002biocrust1-a1-a0020000000zxvtrpnlhfa\RNLGEA2&!4247High SlopeGPS,@Moenkopi Fm030P0Pbiocrust1-b1-a0030000000sqomkigea_ZUKIGEC?2&!3331MidslopeGPS@Aeolian Sands0301-a003biocrust1-a1-a01-a0000000ywusqomkfd_ZPLJEC?0$LVAL j 8These slopes are mostly colluvium from the Mossback Rim upslope, with occasional small outcrops of Moenkopi bedrock.Point is not homogenous from a geological point of view. Plot center fell at the very tip of a low finger of Moenkopi, where below (west) the substrate is sandy alluvium. If the Atriplex confertifolia hadn't dribbled out onto the alluvium, I would have split the plant list. Nearly all the weeds and Sarcobatus are on the alluvium. Most, but not all the Hilaria is on the Moenkopi rise. PLOT IS MORE OR LESS ECOTONAL.Area is a broad, flat terrace that floods in high water, and is subjected to wind and blowing sand otherwise. Plants all have debris and mounds of sand in and on them. The sand has that platey- look it gets where the water ran and then dried out. Looks like sheet erosion.Area is a broad, flat terrace/sand sheet that floods in heavy rainfall and withstands blowing sand and high winds. Debris and mounding around shrubs. Looks like sheet erosion.Site consists of deep, stabilized sand with one small dune at the SW edge of plot. Biocrust is extensive, and moderately well-developed. Hilaria is evenly distributed, and by far the most conspicuous plant component. Shrubs are widely scattered.THIS AREA IS ECOTONAL, with Moenkopi to the uphill (E) and alluvium terrace down slope (W). A significant rocky, sandy wash runs through plot (Chrysothamnus nauseosus, Artemisia filifolia), plot center is on a dune, and the only consistent plant components are the Ephedra and Hilaria. Species-wise, I couldn't see splitting the plant list as there is no clear dividing line.This area is highly consolidated, firm; heavily influenced by the rock layers above (east). Soil surface is littered with Wingate boulders and covered with coarse limestone and sandstone and conglomerate rocks and pebbles. Biocrust is found mostly along the small drainage on the north side of plot, and is also underneath shrubs. Soil lacks the bright red color of Moenkopi, but exhibits its character.LVAL   The area is described by the wash terrace, which is lined by Tamarisk. The terrace is about 1.5 meters above the wash, where the edge may flood occasionally. A large inland-growing line of Tamarix is included in the plot/polygon. Many annual weeds are found growing in-between these two groupings of Tamarix. The soil is deep sand, with little to no crust development.The area is a flat terrace about 2 meters above the wash. Shrubs are large, but widely scattered, with the forb layer dominant. Loose sand covers the entire site, with very little biocrust development, although there is a thin crust just beneath the sand which may be preventing any dune formation. Some random-appearing mounding exists.The point fell at the base of the Mossback cliff, so the plot shape was skewed down and across the slope below that. The terrain falls off sharply to either side of this high ridge, with very little vegetation on the steep west-facing slope. The soil surface is embedded with rough, irregularly-shaped pieces of sandstone conglomerate; however, farther down slope and to the north, the rocks are platey mudstone with extensive hard, gypsiferous lichens.Area is a rolling, stabilized sand sheet with deep soil and extensive crust and moss development; although somewhat patchy with some dunes in spots. The herbaceous layer is well-developed.This area has undulating, deep, sandy soils close to the Taylor Canyon wash, with a minor drainage in it. The soils closest to the wash are more loose, with little to no crust development, while the area further away from the wash is more stabilized by crust. Shrubs are scattered and the herbaceous layer is well-developed.Site is characterized by a braided wash terrace about .5m high. All plants show signs of being in the flood zone, with debris packed around their bases and by having soil washed away beneath them. Gravel and sand, with large rocks typify site.*LVALn $ FSteep, north-facing colluvium derived from the White Rim. Plot does include some Cutler bedrock--reducing species density a bit. Shrubs are also much denser along the base of the White Rim, at the upslope edge of the polygon.The wash terrace is generally sloping in nature, with the lower potions probably flooding occasionally. The vegetation is predominantly herbaceous, with a scattered shrub layer. The trees visible in photo #10 to the northwest are NOT part of this polygon.A hot, west-facing slope with thin soil, littered with rocks and Wingate boulders, with the occasional bedrock outcropping. Shrubs are stunted and widely spaced. Smaller rocks are mostly sandstone plates.The polygon consists of the wash and the terrace just above it. The terrace averages about 1 meter high, and is quite weedy, with scattered shrubs (including the tall shrub, Tamarix). Most of the rabbitbrush is confined to the wash edges, with a few on gravel bars in the wash. It appears that the wash terrace does not flood, but instead gets washed away with each flood episode. Black moss is extensive, forming a conspicuous ground surface feature.This is a relatively stable, deeply sandy plain, with some dunes in the southern edge of the point. Biocrust is rather weakly developed in most areas. Bunchgrasses are restricted to a shallow depression running through the western edge of the plot. The area is very weedy. The Ephedra is growing on a small rocky mound of Moenkopi at the northwest edge of the plot.These clumps of Tamarix are well away from the wash, in deep alluvial soil. Annual weeds do a great job of filling in the spaces. Biocrust is poorly developed, with just a thin crust under the loose sand at the soil surface. I did not include the wash in my observation, since it is wide and has zero vegetation.This site is a rolling, mostly stabilized, sandy area, with deep soil and some slightly duney spots. Shrubs are widely scattered; biocrust and moss are patchy, but significant. The area is quite weedy.LVAL" L Very pebbly maroon Moenkopi soils, very scattered junipers occur mostly where shallow drainage channels transect area.Area is the gray clay band of Moenkopi below the Mossback member of the Chinle--very xeric badlands and toeslopes. Grass only occurs in the wash/trough bottoms between steep interfluve ridges. Slope is actually quite variable, with lots of steeper sides to minor ridges. Sphaeralcea was also mostly in one dense clump, although it can occur anywhere. Most of the plot is sparse ATRGAR and Ephedra.Deep soils with a high pebble content on surface. Minor surficial flow areas have some sandier spots. COLRAM is dribbling in from higher bluffs outside polygon.SPOAIR is limited to sandier soils in the low areas of the plot, where surface runoff has occasionally occurred. Higher mounds in the plot have rocky pavement-like soil cover and Atriplex & Ephedra. HILJAM is lush throughout the area.Both ATRCON & COLRAM are dominant in various aspects throughout this large polygon. ATRCON seems to dominate the interfluve tops and south-facing slopes, while COLRAM dominates the north- and west-facing slopes. Hilaria is limited to the bottom edges of the plot in flatter drainage areas. The soil is a pavement of flat pebbles on all aspects.Steep, rugged terrain in the gray band of clays at the top of the Moenkopi. Some small areas in plot included small colluvial slides from the Chinle above. Lots of variation in aspect in this terrain--340 degrees is an average. Colluvium has the diversity--gray shales are generally sparse ATRGAR.Deep soils with a pebbly surface on very weathered Moenkopi. The polygon is very homogeneous. Both plot and polygon lie on a high area of remnant alluvium between two gully systems.A moderately steep talus slope, with Wingate-derived soils and large blocks that create lots of relatively level microclimates. Occasional small outcrops of Chinle bedrock occur in area.[X% , V  u:D7F7112High LevelGPS>@ Kayenta Formation0400003biotic soilP000200T0000wusqomkieca_RNLJHD1% 3144Low levelGPSR@Kayenta Formation07P000TT00300T0000hfdb`^\ZVTRPPNLJHD1% 132Low levelGPS@Chinle Formation05P00Tbiotic soilPP00400T0000sqomkigea_][NLJHFB0$34138MidslopeGPSr@Talus/Colluvium/Landslides030000P0300300T0000trpnljhfb`\ZZXVTRN2&!4184Low slopeGPS@Talus/Colluvium/Landslides03000Tbiotic soilP0300300T0000~|zxvtrnlhfYWUSQM1% 2218Low levelGPSl@Talus/Colluvium/Landslides03000Tbiotic soilP0300300T0000~|zxvtrnlhfYWUSQM1% 2350Low levelGPS@Moenkopi Fm04P050PcryptosP00P00T0000kigeca_][YWULJHDB>1% 2312MidslopeGPS@Talus/Colluvium/Landslides1-b000Pbiotic soil020400300T0000~|zxvtpnjfYWUSQL0$25230MidslopeGPS@Chinle Formation02P0000040040000000jhfdb`^\XVRPPNLJHD2&!625270MidslopeGPS@Moenkopi Fm021-a000P0300400T0000hfdb`^\ZVTPNNLJHC?2&!526Toe slopeGPS@Moenkopi Fm040000PP0040000000a_][YWUSOMKIIGECA=0$118Low levelGPS@Moenkopi Fm04000Pbiotic soilPP0040000000nljhfdb`\ZXVIGECA=0$2276MidslopeGPS@Moenkopi Fm031-a000T0300300T0000geca_][YUSOMMKIGB>1% 304MidslopeGPS@Talus/Colluvium/Landslides021-a000P0300400T0000trpnljhfb`\ZZXVTOK/#6282MidslopeGPS@Moenkopi Fm02T000P1-a00600T0000db`^\ZXVRPKIIGECA=0$d3308Low levelGPS@Moenkopi Fm060000TT00400T0000b`^\ZXVTPNLJJHFDB>1% 20244MidslopeGPSb@Moenkopi Fm041-a000T1-a0040000000igeca_][WUPNNLJHC?2&!~20260MidslopeGPS@Moenkopi Fm1-a1-b000T020060000000igeca_][WUQOOMKID?2&!35180MidslopeGPS@Talus/Colluvium/Landslides02020000030030000000vtrpnljhdb^\\ZXVRN2&!]15176MidslopeGPSd@Moenkopi Fm1-aP00Tbiotic soilT0200700T0000sqomkigea_[YLJHFD?2&!J15180MidslopeGPS@Moenkopi Fm09000Pbiotic soilTT0P0000000nljhfdb`^\ZXKIGEC?2&!412Low slopeGPSX@ Moenkopi Fm1-b00001-aT00900T0000eca_][YWSQOJJHFDB=0$3334Low levelGPS@@Moenkopi Fm040000PP00600T0000b`^\ZXVTPNLJJHFDB>1% 3278Low levelGPS@Moenkopi Fm020P0Tbiotic soil1-a000700T0000rpnljhfd`^\WJHFDB>1% LVAL ^PRelatively deep, stable soils with a pebbly surface. A superficial drainage has occurred in areas of plot, leaving shallow braided channels, but not affecting the vegetation composition or density.A large (~ 40 feet high) cliff bisects the plot--but the slope, aspect, and vegetation are similar above and below. The slope is of the vegetated surfaces above and below, and ignores the cliff.Rocky maroon Moenkopi soils in a shallow drainage. Lone JUNOST is anomalous--the only one I've seen in the entire polygon. Rhus is also a small, discrete patch in a shallow drainage transecting the plot, and does not characterize the community.Relatively deep soils from weathered Moenkopi just above the White Rim in the stratum. Lots of pebbles on surface. Very little under shrubs--it blows a lot here. No evidence of dunes--the soil just blows away.This plot is on the gray shale band of the Moenkopi, located just below the Mossback member of the Chinle. Most of the plot is extremely sparse, but areas do occur with colluvium from the Chinle upslope--these more closely resemble the red Moenkopi community documented in AA0293--more diverse and denser.Plot and vicinity are red Moenkopi sandstones and flakey pebble soil surfaces, heavily transected by steep heads of wash channels. Vegetation is slightly denser on the wash channel floors, but otherwise it's the same community. Lots of small cliffs everywhere.This plot and polygon are quite homogeneous, and are composed of very steep colluvial slopes of Wingate-derived talus and soil, with large areas of exposed Chinle bedrock. The community is the same everywhere--extremely sparse ATRGAR.The plot is in the most upslope (northern) edge of polygon, where Mossback-derived talus intrudes on a more sandstone/platey pebble area of the uppermost gray band of Moenkopi. Rocky soil surfaces, large boulders, and more flat, benchy areas contribute to a more diverse community than down slope in AA427.<LVAL R\ J r  `JbLarge areas of fine soils intermixed with small patches of slickrock bedrock. Trees may be rooted in fractures, but they all have soil cover around their bases. PINEDU, especially, have large crown areas.Plot is in an area with more exposed bedrock and thinner soils--thus, less COLRAM than in neighboring areas. But the COLRAM is still consistently here as an understory.Deep, pebbly soils--perhaps as influenced by eroded Navajo as the Kayenta that underlies the soils and appears to be responsible for the bench-like topography.Relatively deep soils in an area are frequently transected by minor, shallow washes, exposing more rock/bedrock. The trees are generally denser along the rock exposures.Deep pebbly soils. Trees are sparse but common along the occasional shallow drainage channel, where bedrock or large rock outcrops a bit.Steep, blocky, Wingate-derived talus on a xeric exposure.Similar to AA0077, but perhaps with less shrub diversity and density. Huge talus boulders and relatively flat rocky soil areas create a more sheltered but similar environment to the steeper slopes to the north.This benchy area bears a close resemblance to the steep colluvial slopes to the N (upslope), but here the Wingate-derived colluvium has collected on a flatter spot of limited extent.Purshia, EPHVIR, SYMLON and majority of juniper in this plot actually are located in a shallow drainage area (with the exposed bedrock), and don't characterize the community in general. Lots of PLEJAM even in sandy, almost duney areas.A lot of flat areas behind boulders and more sandy soils (Wingate-derived) makes the ELYSAL happy in this distinctive area of lush grass.Lots of Wingate boulders on this slope, but the soils tend to be weathered Chinle, with extensive Chinle bedrock exposures.Plot is on a steep, bouldery colluvial slope with many small cliff bands. A steep drainage transecting plot probably slightly increases tree and Rhus cover, but veg variety is the same as elsewhere on these slopes.ZY[ ^  R Pj3b2250Toe slopeGPS@ Moenkopi Fm050P0041-a00P0000000db`^\ZXVTRPKKGECA=0$11110Low slopeGPS@Moenkopi Fm02P000TT0070000000db`^\ZXVRPNLLJHFD@3'"3245Toe slopeGPS@Moenkopi FmPT000PP00800T0000`^\ZXVTRNLJHHFDB@>1% 37190MidslopeGPS@Moenkopi FmPP000T090P0000000a_][YWUSQOKIIGECA?2&!38338MidslopeGPS@Moenkopi Fm1-aP000P0801-a00T0000geca_][YTRNLLJHFD?2&!40338MidslopeGPS6@Moenkopi Fm1-aT000T0801-a00T0000geca_][YTRNLLJHFD?2&!2040High SlopeGPSh@Moenkopi FmPT000T020070000000db`^\ZXVRPLJJHFDB@3'"12277MidslopeGPSl@Moenkopi Fm1-bT000T1-b0070000000geca_][YUSNLLJHFD?2&!j34210InterfluveGPS@Moenkopi Fm0402001-abiocrust0P0020000000trpnljhfb`^\RMKIEA4(#U4228InterfluveGPS,@Moenkopi Fm1-aP000P1-a0080000000geca_][YUSNLLJHFD?2&!39335MidslopeGPS@ Moenkopi Fm021-a00001-b0060000000igeca_][WUPNNLJHC?2&!f15333Toe slopeGPS @ Moenkopi Fm03PT005biocrustTT0020000000pnljhfdb^\ZXNJHFD@3'"2254High LevelGPSR@ Chinle Formation05P001-abiocrustP1-b0020000000xvtrpnljfd_]SNLJHD2&!10308Toe slopeGPS0@Chinle Formation02PP01-abiocrustP030020000000xvtrpnljfd`^TOMKIE3'"flatn/aHigh Level1:24K Quad@Kayenta Formation1-a07000T020P00T0000ywusqomkigcaa_][WR?3'2732MidslopeGPS@Talus/Colluvium/Landslides060001-bbiotic soil1-aP0T00P0000~|zxvtrpni\WUSQM1% 436MidslopeGPS@Aeolian Sands08000Pbiotic soil0200000T0000omkigeca_][WJHFDB>/#6184MidslopeGPS@Navajo Sandstone020600Pbiotic soil1-aP0T00T0000vtrpnljhfdb]PNLJFB0$3166Low levelGPSL@Navajo SandstoneP0900Tbiotic soilP00000T0000rpnljhfdb`^\OMKIEC1% 322Low levelGPS@@Aeolian Sands04P040Pbiotic soil1-a00000P0000sqomkigeca_ZMKIEC?0$4310MidslopeGPS@Kayenta Formation06PT0Pbiotic soilPT00300T0000trpnljhfb`^\OMKIGC0$338Low levelGPS@Obscured by Soil05000Pbiotic soilPT00400T0000sqomkigea_][NLJHFB0$1302Low levelGPS@ Kayenta Formation06P00Pbiotic soilP000300T0000usqomkigca_]PNLJHD1% 120Low levelGPSP@ Kayenta Formation06P00PbiocrustPT00300T0000qomkigec_][YOMKIGC0$LVAL jt4 DJFThis steep hillside is eroding fast into less steep badlands below. Shale plates cover gypsum soil.The slope listed is an average between 25 and 5 degrees. Part of the plot is up on a ledge to the south. Biocrust is dense and thick.This is the well-defined bench at the bottom of the Chinle and is free of colluvium at this location. The soil is pebbly and quite a few flat rocks decorate the surface.A lot of giant boulders have rained down on this slope from the Wingate above. In spots it's obvious that the soil has been altered by the reddish colluvium, but most of the soil has the distinctive Chinle gray and green color. Biocrust is thriving in patches on the lighter soil.This bench is mostly solid rock, although a little colluvium has accumulated on the north side, where the trees are a bit thicker.Colluvial slope is composed of weathered Navajo, and is mostly a sandy soil with some smaller rocks. Heavy crust development.The area has a very duney topography, but soil surfaces are quite stabilized with physical crusting.The plot and polygon are on a canyon rim area with lots of exposed slickrock and weathered Navajo soils collected in fractures or grooves. Some soils are relatively deep, though not extensive. Coleogyne is creeping in from nearby polygon.Vegetation--except for CERINT--is generally in potholes and joint patterns. The vegetation is dense in these areas of soil, but most of the plot/polygon is slickrock.This plot shares much with the next polygon east of this one--sandy dunes and the accompanying grasses and Ephedra--except that bedrock is occasionally exposed from a small Navajo hogback to the west, and the trees are present as a result. An ecotonal area. Pinyon crowns are quite large.The plot landed on a wash bank--thus the exposed bedrock and the tall shrubs, which are not typical of the plot or polygon.Soils are likely derived from a mix of Kayenta and Navajo. Deep and pebbly.LVAL 8 xThe soil is sandy. A little bedrock is exposed through the thin soil. Many multicolored pebbles decorate the surface.The sand is mostly stabilized by biocrust and vegetation. The terrain is gently rolling low dunes.This point landed in a small flat basin surrounded by low dunes. The sand is very fine- almost silty, annual weeds inhabit the understory.This site has areas where sand has blown in covering parts of the Moenkopi soil. Mature biocrust occupies these sandy areas.A few thin bedrock ledges are exposed in spots. The surface is mostly covered with flat rocks and pebbles.The surface is well-covered with flat rocks. A little bedrock is exposed in places.Giant boulders litter this slope and provide shelter for plants. A fair amount of soil has accumulated.This very steep slope has accumulated enough soil to support a variety of plants, including the biggest Ephedra I've ever seen (see photo).This steep slope has a surrounding amount of soil between the boulders. The plants look happy in their sheltered locations. The slope really is 40 degrees.The slope and aspect listed is for the majority of the plot. Part of the plot goes to the top of the ridge and a bit down the other side. The surface is well-covered by flat rocks.This point landed in a concave bowl that seems more sheltered and a little more moist than other areas of the polygon. The surface is well-covered with little flat rocks and pebbles.These steep badlands are eroding fast--too fast for anything to grow on them. The soil has gypsum crystals and a physical crust on the surface. One part of the plot that is less steep has a nice patch of lichen-crusted biocrust.These badlands are broad and rolling. The slope and aspect listed describe the general lay of the land. The actual slope and aspect are highly variable. The soil is almost completely covered with little flat rocks. The vegetation isn't much affected by the variations in aspect.To  f  f rz(~%+2126High LevelGPS@Aeolian Sands06000Pbiocrust030000000000omkigeca_][WMKIGEA2&!285High LevelGPS@Aeolian Sands05000Pbiocrust040000000000nljhfdb`^\ZVLJHFD@1% 918344MidslopeGPS@Navajo Sandstone1-a04T002biocrust02T0T00T0000wusqomkigec_UQOMID2&!:20115MidslopeGPS<@Navajo Sandstone0203P002biocrust02T0T00P0000vtrpnljhfdb^TPNLHD2&!N5214High SlopeGPS@Navajo Sandstone05PT002biocrust02T0T00P0000trpnljhfdb`\RNLJHD2&!LvariablevariableLow slopeGPS@Aeolian Sands060P0Pbiocrust0300000P0000}{ywusqomi_][YWSD83(M9172High SlopeGPS@Aeolian Sands0600000300000T0000eca_][YWUSQMMKIGEA2&!84115High LevelGPS@Aeolian Sands06000Tbiocrust030000000000omkigeca_][WMKIGEA2&!,2142High LevelGPS@ Aeolian Sands06000Tbiocrust030000000000omkigeca_][WMKIGEA2&!flatn/aHigh LevelGPSd@ Aeolian Sands060001-abiocrust0300000T0000xvtrpnljhfd`VQOMKG8,' 2245Low slopeGPS@ Aeolian Sands070P0Pbiocrust0200000T0000nljhfdb`^\ZVLJHFD@1%  236Low slopeGPS@Aeolian Sands03PP005biocrust1-aT0t00P0000pnljhfdb`^\WMIGEC?0$ 5334MidslopeGPSh@Kayenta Formation06PP003biocrust1-bT0T00T0000trpnljhfdb`[QMKIGC0$ flatn/aLow levelGPS@Kayenta Formation07T0002biocrustP00T00T0000xvtrpnljhfdbXTRPNJ7+& 5233High SlopeGPS@Kayenta Formation1-a07T0TbiocrustPT0T00P0000trpnljhfdb`^TRPNJE2&!15High LevelGPS@Kayenta Formation020400PbiocrustPT00200T0000rpnljhfd`^\ZPNLJFB/#[31224MidslopeGPS@Moenkopi Fm1-aP000T060020000000fdb`^\ZXTRNLLJHFD?2&!3231Toe slopeGPS@White Rim Sandstone - Cutler Gp07TT0TbiocrustTT0020000000~|zxvtrnljh^\ZXVR1% 3189Toe slopeGPS@ White Rim Sandstone - Cutler Gp08TT0PbiocrustTT01-b0000000}{ywusnljh^\ZXVR1% 2188High LevelGPS@Moenkopi Fm060T00T00030000000ca_][YWUQOMKKIGEC?2&!2150High LevelGPS@Moenkopi Fm040T0PbiocrustT020040000000omkigeca][WUKIGEC?2&!2126High LevelGPS@ Aeolian Sands03004003biocrustP00000T0000qomkigeca_][QMKGEA2&!flatn/aLow levelGPS@ Aeolian Sands0500003biocrust020000000000vtrpnljhfdb^TPNLJF7+&pLVAL 2@ < d N H>This is an area of deep, sandy soil. A small amount of biocrust is scattered around.Thick vegetation covers this area of deep soil. The plot is in a slight depression that probably collects more than its share of water. The biocrust is scattered--not continuous.These dunes are mostly stabilized by vegetation and a little biocrust. The trees are some of the largest PJ's I've seen in the park.The terrain is low, rolling dunes of an apparently thick layer of sand, well stabilized by biocrust. An erosion channel wanders through the plot without any effect on vegetation. The trees are big and puffy.There are a couple of ledges on one side of the plot, but most of it appears to be deep, sandy soil. A small erosion channel goes through the plot without affecting the vegetation.At this site, the soil seems deep and the plants are robust. Biocrust is scattered across the sandy soil.The terrain is broad ledges of sandstone, with significant accumulations of soil on the flat spots and in potholes. The soil is a little pebbly and some biocrust lives in isolated patches. A couple of sandy runnels cross the plot.This plot has thin soil, with several flat bedrock exposures. The soil has a pebble surface where it's not covered with litter or biocrust.This steep slope has accumulated a fair amount of soil and the big boulders provide shelter for a few plantsThe soil is thin and looks like a mixture of Moenkopi and White Rim. A little bedrock is exposed. Many pebbles litter the surface.Sand has mixed with the Moenkopi soil here, giving it a lighter color. Many small pebbles decorate the surface. The soil is getting thinner as I approach the white rim, but the blackbrush grows pretty thickly right up to the edge (see second photo).The soil is getting thinner here as I approach the White Rim. A fair amount of sand is mixed in with the Moenkopi dirt, giving it a lighter color. Many small pebbles decorate the surface. The blackbrush looks a little stunted here.LVAL z  fp4Sparsely vegetated, cool aspect talus slope on an area of Wingate cliffs that is not too steep, so that some soil with boulder overlay has collected on it. Very active, steep slope that hinders plant development, though some hardy individuals are persisting on it. Slope is estimated.A cool, sheltered short talus slope below Kayenta rim, but above Wingate cliffs. Amelanchier and Elymus co-dominate the understory. Pines near the base of the Kayenta are very tall (~8m+) and robust. Some dieback on Amelanchier, but most are robust and full of flowers. Shaley, platey rocks comprise the talus substrate.Very steep rockslide area on Wingate cliff band that is a very active slope, leaving little area for plants to root and establish. Shaded, cool aspect, but lots of bedrock exposure, keeping plant cover low.This is an area of deep, sandy soil. There are some annual weeds and a little biocrust in the understory.This is an area of deep, sandy soil. Immature biocrust is scattered around the plot.This mesa has eroded to a smooth slope with considerable sandy soil accumulated. Mature biocrust abounds.The terrain is an eroded sandstone mesa with rounded slopes and ledges. Sandy soil has accumulated in the flat spots. Patches of mature biocrust dot the plot.The sandy soil is a little thinner here, with bedrock exposures. Many Pinyon trees have died in the last few years. Small pebbles and rocks decorate the surface. Biocrust is in thick patches and seems to be trying to fill all available space.This duney area overall is mainly flat, but the rolling dunes are up to six feet high. Most of the sand is stabilized by physical crust, biocrust, and a few plants, but there is also some actively blowing sand.This is an area of sandy soil that has accumulated in a wide notch in a cliff band. The understory is dominated by annual weeds. Most of the blackbrush and Atriplex is dead or nearly dead. A giant stinkbug tried to crawl into my pants.This is an area of deep, sandy soil and sparse, scattered biocrust.FJ 2 ! } $ u~ a c&.R28275Low slopeGPS@Chinle Formation031-a000T030030000000nljhfdb`\ZVTTRPNIE3'"-X26340Low slopeGPS@Chinle Formation03P000T0300400T0000kigeca_]YWSQQOMKIE3'",11216MidslopeGPS@Moenkopi Fm1-aP000P020070000000fdb`^\ZXTRNLLJHFD?2&!+flatn/aLow LevelGPS@New Alluvium01-a05001-a1-a00300T0000rpnljhfd`^YTTRPLGE7+&*`2228High LevelGPSP@Aeolian Sands0P0600PT0030000000eca_][YWSQOMMKIECA2&!)W3307High LevelGPS8@White Rim Sandstone - Cutler Gp1-a07P0PbiocrustPT01-b0000000}{ywrpnlb`^\XS2&!(V37314MidslopeGPS@Talus/Colluvium/Landslides020000P0500300T0000trpnljhfb`\ZZXVTRN2&!'1288High LevelGPS@Chinle Formation040P01-bbiocrustP1-a0030000000xvtrpnljfd_]SNLJHD2&!&variable144Toe slopeGPS@Talus/Colluvium/Landslides1-b0T0Pbiocrust1-a0400300T0000}{wrhfdb`[?3.#%%3174High LevelGPS8@Aeolian Sands1-a00900P001-a00T0000igeca_][VTRPPNLHFA2&!$3306High LevelGPSn@Aeolian Sands00100TbiocrustT00T0000000mkigeca_][YWMKIECA2&!#4287High LevelGPS@White Rim Sandstone - Cutler GpT09T0PbiocrustTT0T0000000}{ywusqomki_][YUS2&!"91112High LevelGPSt@Kayenta Formation04TT01-bbiocrust1-aP00400T0000ywusqomkgec^TOMKIE2&!!9197High LevelGPS@Kayenta Formation05P00Pbiocrust1-aP00400P0000usqomkigca_ZPNLJHD1%  B2247High LevelGPS@Kayenta Formation020400Pbiocrust02P01-b00P0000xvtrpnljeca]SQOMIE2&!G2255High LevelGPSJ@Kayenta Formation03020001-bP00300P0000nljhfdb`\ZXSSQOMIE2&!E2294High LevelGPSJ@Kayenta Formation041-bT0002T00200P0000nljhfdb`\ZXTTRPNIE2&!27103Midslope1:24K Quad6@Talus/Colluvium/Landslides03000PbiocrustT030030000000}{ywsqmka_][YU9-!36320Midslope1:24K Quad@Talus/Colluvium/Landslides1-b0000P0400400T0000|zxvtrpnjhdbb`^\ZU9-!3622Midslope1:24K QuadP@Talus/Colluvium/Landslides1-a1-b0001-b0300400P0000}{ywusomiddb`^YT8, 32292Midslope1:24K Quad<@ Talus/Colluvium/Landslides1-b02000P0300300P0000~|zxvtrpljfddb`^ZU9-!:285MidslopeGPS@ Talus/Colluvium/Landslides1-b1-b000020300200P0000wusqomkiec_[[YWUPK/#35345Midslope1:24K Quad@Wingate Sandstone1-b0400PbiocrustP0301-a00T0000~|zxvtrmkge[YWUQL9-!fLVAL   @pA very narrow PJ community that wraps around the base of a Navajo dome understory. Vegetation is diverse but sparse.Very shallow joints and scattered potholes stabilized by crypto cover characterize this polygon, which is 90% or more White Rim bedrock. Soil pockets support a couple individuals each of a variety of grasses and forbs and stunted COLRAM. CERINT limited to bigger joints.Slightly rolling terrain intersected by shallow runnels. Crypto cover is patchy and mainly around the bases of shrubs, which are pedestalled. Small rock cover is consistent everywhere.Flat bench just above Wingate cliffs covered in PJ and blackbrush. Crust cover is very patchy, mainly around the bases of shrubs and small rock cover is stabilizing the soils. Blackbrush is pedestalled.Small broken ledges of Kayenta and larger flat expanses of bedrock in a mosaic with shallow soils lightly covered by pebbly rocks. Lots of die-back on the Purshia and Fraxinus and one recently dead pine in plot.Very shallow soils atop bedrock stabilized by pebble-sized rock cover. PJ and blackbrush are dwarfed and blackbrush is pedestalled. Lots of dieback on the Purshia.Very shallow soils covered in pebble-sized rock chunks with bedrock exposures in shallow washes favoring Purshia and Fraxinus. Blackbrush are dwarfed and pedestalled. PJ also dwarfed, though some larger individuals are around. Die-back on Purshia and dead Pinus trees and seedlings in plot.Slope was estimated. A hot aspect, sparsely vegetated talus slope with very sparsely scattered Rhus, Juniper and (surprise!) tamarisk in the many drainage channels dissecting the slope. Boulders from Wingate scattered around and some bluish Chinle clay exposures on the low slopes.A very steep, active slope, covered in large and small pieces of Wingate colluvium.We viewed entire polygon. Long, ovalish point on a steeper bench above the Wingate cliffs and below Kayenta. Large rocks resting on bench and large bedrock exposures.NLVAL Z j 2LnRolling badland hills of the Moenkopi formation covered in pebble- to hand-sized platey rocks. COLRAM, EPHTOR and ATRCON are all characteristic of this extensive community, with COLRAM more dominant on north-facing slopes and in drainages.A meandering, sandy wash channel, where ERINAU is the dominant vegetation. TAMCHI also scattered in wash bottom. Up wash of plot in the wash polygon the SPOAIR cover is much higher (1-5%) and the ERINAU/SPOAIR association name is a better fit.Shallow, sandy soils that have blown in over White Rim bedrock. Shrubs are pedestalled on mini sand dunes, and a coating of tiny rock fragments covers much of the sand.Very shallow soils in linear depressions on the White Rim sandstone are stabilized by cryptos and small rock cover. COURAM is the dominant species out here.A very steep, active slope with lots of rocks and soil mounded on upslope sides of plants. Plot fell next to a major drainage/ravine that has lots of Rhus and CHRNAU along its course. Evidence of landslides and rockslides everywhere.A broad bench covered in COLRAM. Substrate is dominated by rough, pebbly rocks, but patches of well-developed cryptos are common. Shrubs are slightly pedestalled. A very shallow, broad (~4 meters wide) wash cuts through the center of plot.Polygon and plot both capture a fairly large bench/toeslope (6 degree slope), as well as the steep talus slope (34 degrees) below the bench. The community is pretty much the same throughout, but JUNOST and COLRAM only occur on the bench/toeslope. Boulders are everywhere, and range from basketball- to half-car-sized. Some small patches of biocrust where slope is more level.Aeolian sand on entire surface of this sandsheet with mainly blackbrush, but a diversity of other shrubs at low cover as well. Some small dunes throughout.Large sandsheet covered in COLRAM, but this small polygon captures an area of looser sands as small dunes, and has more shrub diversity and decent grass/forb cover, especially STIHYM.LVAL x n f Very rocky slope below the Wingate cliffs. Car-sized boulders and large rocks throughout area. Sparsely vegetated steeper slope with little erosional gullying.Narrow FRED community following base of Navajo dome. High shrub density, all with low cover. Crypto cover is patchy and not that well developed.Steep Chinle badland hills have an undulating terrain at the base of the Chinle talus slopes below the Wingate. Huge Wingate boulders cover the slopes, but areas of clay are also exposed, sometimes as spires supporting balanced Wingate rocks. Vegetation is very sparse. Clay color is bluish purple.Undulating terrain of steep Chinle badland hills dissected by ravines and coated with large pieces of colluvium from both the Wingate and the Mossback (which has a long, linear protrusion of bedrock just upslope of plot center). Diverse shrub and grass mixture, all with trace cover.A gently sloping bench with scattered Wingate boulders, one the size of a mobile home, and a coating of small rocks. Crypto cover is patchy. Shrubs are slightly pedestalled and PJ cover is denser in plot than in most of the polygon.Gradually sloping bench with large chunks of Wingate colluvium scattered about. Shrubs are slightly pedestalled and community looks lush compared to the surroundings.Low hills dissected by shallow gullies with some bedrock exposure along the banks. Dark gray Chinle soils are stabilized by cryptos and small rock cover.Steep Chinle badland hills below talus slope that have been covered in large chunks of Wingate colluvium. Vegetation is extremely sparse and has lots of rock and soil mounded upslope of plant bases.It looks like Mars here, with some vegetation. Steep Chinle clay hills are carved open by deep gullies and covered with large (car-sized) chunks of Wingate colluvium. Some rocks are balanced atop Chinle spires--quite amazing! Vegetation is very sparse, and plants have lots of soils and rocks mounded on their upslope sides.S H 8 > $qdeKE@2240High LevelGPSn@Kayenta Formation021-b0003biocrust03P01-a00P0000{ywusqomhfd`VRPNIE2&!DJ3244High LevelGPS@Kayenta Formation03PP003crypto1-bT0P00P0000trpnljhfdb`[SOMKIE2&!CZvariablevariableHigh LevelGPS:@Kayenta Formation051-a0002crypto0200P00P0000}{ywuqieca\XE94(Bj2200High LevelGPSn@Aeolian Sands0500201-abiocrust1-b00T00P0000usqomkigeca\RMKGEA2&!AS348High LevelGPS@Aeolian Sands021-a1-a003biocrust0300000P0000vtrpnljhfdb^TPNID@1% @]3168High LevelGPS@Aeolian Sands0301-a003crypto0200000P0000rpnljhfdb`^ZRNLGEA2&!?R1188High LevelGPSf@Obscured by Soil08000Pmoss020000000000nljhfdb`^\ZVPNLJHD2&!>15348Midslope1:24K Quad@Talus/Colluvium/Landslides0300001-a0300300T0000~|zxvtrpljfaa_][YU9-!=28160Midslope1:24K QuadB@Talus/Colluvium/Landslides1-b00001-a0400300T0000}{ywusqmkgbb`^\ZU9-!<15260High SlopeGPS @Navajo Sandstone041-b0002biocrust1-aP01-b00P0000}{ywusqojhfaWSQOJF4(#;3245High LevelGPS@ Obscured by Soil031-a0002biocrust1-aP00300P0000zxvtrpnlhfd_UQOMHD2&!:26308MidslopeGPS@Navajo Sandstone021-a0002biocrust1-b0200200P0000|zxvtrpnjhd_UQOMHD2&!928334MidslopeGPS@Talus/Colluvium/Landslides02P0002biocrust020200200P0000~|zxvtpnjf\XVTRN2&!815296MidslopeGPS@Kayenta Formation031-b001-abiocrust1-a1-b00300T0000}{ywusqmkfaWRPNIE2&!7g790High LevelGPS@Kayenta Formation0303P001-bP00200P0000mkigeca_[YWRRPNLHD1% 61796MidslopeGPS@Chinle Formation0200001-a0300400T0000ljhfdb`^ZXTOOMKIGC1% 5|variablevariableToe slopeGPS@Chinle Formation1-b000pbiocrustP030060000000}{yusomca_][VD83(4lvariablevariableHigh LevelGPSb@Chinle Formation05P000P020030000000}{ywusqokiecca_][WE94(3 o2547Low slopeGPSZ@Chinle Formation020000T050030000000jhfdb`^\XVRPPNLJHD2&!2 n15348Low slopeGPS8@Chinle Formation020200PBiocrustP0501-b0000000xvtrpnljec_]SQOMIE3'"1 Z7288High LevelGPS@Chinle Formation03000Pbiocrust1-a0300300P0000wusqomkiec_ZPNLJHD2&!0 [8270High LevelGPSL@Chinle Formation050001-abiocrust1-a0200200T0000zxvtrpnlhfb]SNLJHD2&!/ <3346High LevelGPS2@Chinle Formation04PT002biocrustP1-a0030000000wusqomkiec^\RNLJHD2&!LVAL &pOpen PJ woodland with a LEYSAL-dominated understory on a steep slope below a Navajo dome. More of a shaley slope than a talus slope.A narrow, mesic PJ community around the base of a Navajo slickrock dome with a cool aspect and steep slope. Slope is a mix of soil, rock, and crypto cover; all about equal. High shrub diversity, but LEYSAL is dominant in the understory. AMEUTA and CERINT shrubs are some of the tallest I've ever seen; nearly as tall as the trees.Point is on a small bench below a steep slope that has broken, ledgy bedrock exposures down slope and solid bedrock cliffs upslope. Crypto cover is patchy. The area is ecotonal between a narrow pour-over slope community and wooded blackbrush flats to the northwest.Ledgy Kayenta bedrock exposures with shallow soils on top that support a typical FRED community, though PINEDU is co-dominant with JUNOST. Lots of dieback on shrubs (especially FRAANO) and dead PJ snags around.Plot center fell on a bench, but also captured the steep talus slope below the bench. Juniper, Ephedra torreyana and Stipa comata are the dominant species. Wingate boulders strewn about plot. Polygon has had an undulating appearance, whereas plot is more of a bench and slope, less hilly than much of polygon. Slope is an average.Point fell on a low Chinle hill between two steep talus slopes, so slope and aspect vary greatly, but general aspect of area is E-facing. Vegetation is mixed and very sparse. Area/polygon definitely has an undulating moraine appearance.Point fell on top of a small hill, so slope is variable throughout polygon, pretty flat around and on top of hill and hillslope about 15 degrees. Undulating moraines in plot as well as flat wash channels between hills with some bedrock exposures. Wingate colluvium cover much of plot, but there are also large exposures of purple-blue grey Chinle clay hills. Very diverse mix of shrubs all with trace cover, but adding up to 2-3%.LVAL x>FA PINEDU-dominated woodland with a homogeneous COLRAM understory. Crust cover is consistent throughout area, and there are ledgy bedrock exposures on rises and in minor wash channels.Old, low, well-stabilized dunes with a well-homogenized PJ/COLRAM community. Scattered bedrock & small rock throughout area.Point fell in a large, depressed area with a wide bedrock exposure and extensive cover of lightly-developed cryptos. Rolling microtopography of low stabilized dunes. Many dead JUNOST snags lying around. Aspect and slope vary all around us, since we are in the bottom of the depression.Partially stabilized dunes with some active blowing of sand and pedestalling of shrubs. Very little cryptobiotic crust cover, with some moss associated. Some dunes fairly tall (~2 m).Rolling dunes with some bedrock exposures in small drainages between dunes, with slight but consistent crust development, keeping them stabilized. A few areas of blowout sands. Dunes are 2-3 meters tall. A lot of die-back on the JUNOST and some large snags around.Stabilized dunes with some moss cover and lightly-developed cryptobiotic crust cover. More trees (JUNOST & PINEDU) throughout area, and large dead JUNOST wood on ground. Higher, rolling hilly dunes throughout.Very little crust development, probably due to close proximity of sand dune N of point. Point captures a small stand of Atriplex canescens, which is unusual in the polygon. Ephedra viridis growing in mots and grass-like form. Stipa hymenoides the only grass we can see, other than some Festuca octoflora.Slope was estimated, and some species with trace cover were unidentifiable from this distance. Definitely a cool aspect slope with a sparse but regular cover of PJ, mainly Juniper. A large area of the polygon ESE of plot, and near the base of the cliff, is covered with Elymus and little else. Many huge boulders 1/2 car size are scattered across slope. Old road cuts through plot.LVAL  8 lP<Small rocks scattered on surface, shallow, smaller gullies throughout.On the White Rim by Candlestick Campground. Bedrock which has joints, and many potholes that have heavy biocrust development and vegetation. Crust is very black, tall and supports lichens.This hillslope has a surface littered with small rocks and some larger (bowling ball sized) rocks & boulders (1/2 car sized).Relatively flat mesa top with some exposed bedrock, small rocks scattered throughout surface, small mounding around some shrubs from aeolian sand, some pedestalling around shrubs but pretty much stable soil.Rolling, taller dunes with aeolian sand between dunes as well. Litter accumulation mostly below trees. Trees very robust with larger crowns.Some bedrock exposed and some more duney aeolian areas in SE edge of plot. More shrub species diversity in this plot than in other areas of polygon, but still good representation.More bedrock exposed here than in other areas of polygon. Deeper soils beneath trees and shrubs.Flat area of deeper sandy soils with small rocks littering surface. Some small accumulation of aeolian sand around clumping, pedestalled shrubs (very small dunes) throughout area but area generally very flat.Duney area with aeolian deposits around dunes. Shrubs are pedestalled and small areas of bedrock exposed with small, sometimes platey rocks on surface. Litter mostly under trees.Thick shrubland of COLRAM with some large crown PINEDU & JUNOST throughout. Shallow rolling dunes with good crypto cover and small gullies running between dunes.An extensive, fairly homogeneous COLRAM shrubland, dotted with PJ, mainly JUNOST. Crust cover is also extensive and fairly well-developed. Microtopography is rolling and area is dissected by many small drainage channels.PINEDU/JUNOST woodland with a sparser understory of a mix of shrubs (COLRAM, RHUARO, EPHVAR and PURSTA) with bedrock exposed. Trees have larger crowns and trail runs through plot.QVa ; 3 w<ps9\6flatn/aLow levelGPS@New AlluviumP1-a040PcryptoP020030000000vtrpnljhdb^\TRPLGE7+&[5h1192High LevelGPS(@Aeolian Sands000700T00030000000eca_][YWSQOMMKIECA2&!Z45188Step In SlopeGPS@Moenkopi FmT1-b000T030040000000igeca_][WUQOOMKIDB5)$Y3iflatn/aLow levelGPS@ New Alluvium1-a003001-b00030000000omkigeca][YTTRPLJE7+&X28267Toe slopeGPS*@Moenkopi Fm1-a1-b0001-b1-b0070000000ljhfdb`^ZXSNNLJHC>1% W1flatn/aStep in slopeGPS@Chinle FormationT1-aT003biocrust02T0030000000~|zxvtrnljf\XVTOM;/*V0 flatn/aStep in slopeGPS@Chinle Formation0000000000000000mkigeca_][YWWUSQOM;/*U/flatn/aStep in slopeGPS@Obscured by SoilTT0003crypto021-b0030000000~|zxvtrpljeaYUSQOM;/*T.c30346MidslopeGPS@Talus/Colluvium/Landslides1-aTT0Tbiocrust1-a05002001-a0000}xvtpnje[YWUSN2&!S-flatn/aStep in slopeGPS@Obscured by Soil1-a00004biocrust1-b1-b0040000000~|zxvrpkf\XVTRM;/*R,15356MidslopeGPS@Moenkopi FmTT000T050050000000ca_][YWUQOKIIGECA?2&!Q+flatn/aHigh LevelGPS^@Aeolian SandsT00900T001-a00T0000ljhfdb`^YWUSSQOKIG8,'P*flatn/aHigh LevelGPS|@ White Rim Sandstone - Cutler GpT09001-acryptoT00T00T0000~|zxvtrphca_[Y8,'O)@8155Low slopeGPS@ Obscured by Soil1-bT0001-aP00700P0000kigeca_]YWUPPNLJHC1% N(62111High SlopeGPS@Kayenta Formation031-bP0Pcrypto021-a01-b001-a0000}{ywupnlge`\TRPNIE2&!M'NvariablevariableHigh LevelGPS@Aeolian Sands1-a0070002000001-b0000~|zxvqomkigcca_[YTE94(L&Rflatn/aHigh LevelGPSh@Kayenta Formation021-a1-a01-acrypto021-a002001-a0000{ywsqlh`[YTOK8,'K%Jflatn/aHigh LevelGPS@Kayenta Formation021-b1-a00021-a01-b001-a0000~|zxvqomhfa]][YTOK8,'J$Xflatn/aHigh LevelGPS@Obscured by Soil0201-a0Tcrypto020002001-a0000~|zxvqomigeaYWUPNJ8,'I#e3218High SlopeGPSh@Aeolian Sands03P030002T00300P0000igeca_][WUSOOMKGEA2&!H"U4324High LevelGPSB@Obscured by Soil0502P003crypto1-b00P00T0000usqomkigeca\TPNLHD2&!G!L4275High LevelGPS@Kayenta Formation03P0005biocrust02T0P00P0000usqomkigeca]SOMKIE2&!F 63220High LevelGPSf@Kayenta Formation02031-a01-a02P0P001-a0000trpnlgeca_]YYTRMIE2&!pLVAL  6 P&This slightly sloping bench of Moenkopi sits above the White Rim and is sparsely vegetated. The ground surface is covered with small and large platey red-brown rocks. A ledgy layer of bedrock is exposed.Moenkopi toeslope that has a ground surface covered with small, platey, red-brown rocks. Some ledge bedrock exposed, and some pedestalling of shrubs.Some Chinle-derived bedrock is exposed, but ground cover is dominated by small rock and biocrust. Few JUNOST in point, but more to the east of point. Well-developed crust with lichens abundant.Ground is covered with small rocks, biocrust & litter under shrubs, as well as a trace amount of bedrock. Biocrust is tall, pinnacled, and black with lichens. Expansive flat bench with a low, rolling microtopography with some shallow, sandy, small drainages throughout and some deeper sandy pockets of bare ground. Bench between Chinle slope and Moenkopi badlands.Ground covered with small rocks, platey larger rocks, and ledgy bedrock scattered throughout. Good black biocrust with lichens throughout. Microtopography of low, rolling hillocks on an otherwise flat, expansive bench between Chinle slopes and lower Moenkopi badlands. Deeper, sandier, light-tan soil close to point to south.This Chinle-derived slope has car-sized and smaller boulders throughout, some sand accumulations in pockets and some biotic crust development. Deep erosional gullies throughout. Junipers are stunted in growth.Ground surface covered with small rocks and biocrust cover with good lichens developed. Microtopography of bench has low rolling hills but bench itself is extensive and is below Chinle slope and above Moenkopi Shale barrens.Ground surface covered with medium (hand) sized platey rocks with some bedrock ledges throughout, deep erosional gullies in point.Flat sandsheet with aeolian derived sand on ground surface forming very low mounds on the microtopography. Some blackbrush are pedestalling. Blackbrush is healthy and happy.LVAL , Steph: Large, flat mesa which is definitely COLRAM dominated except at point which has more ATRCON. Pete: Deep, pebbly soils.The ground surface of this Moenkopi toeslope is completely covered with medium to small flat, platey rocks. At the bottom of the slope is a drainage with a small pour-off. Bedrock is exposed to the northeast of the point. Tall shrubs and trees are in the drainage area only.This is a bench off of the Chinle toeslope and is very expansive and flat bench with deep and sandy soils (almost plateau-like). There is aeolian deposition forming small undulations in the microtopography, and some pedestalling of shrubs. Scattered small rocks on surface.This toeslope is very bouldery and jumbly and has small rocks on entire ground surface and cryptobiotic crust as well. Crypto is well developed in areas. Some standing dead JUNOST. More grass here than in other areas of polygon but otherwise good fit to rest of polygon.Point is right off a light foot trail in deeper light tan color sandy soil with very large (car-sized and smaller) boulders, and very light, shaley bedrock. Chinle exposed. JUNOST stunted and some standing dead throughout. Bench is at bottom of Chinle talus slope.This point is on the toeslopes that come off of the Moss Back member of the Chinle and extend out to the low-level dry washes throughout this area. Some steeper slopes are very barren and rocky, while the flatter tops and gullies have higher shrub covers. Soil seems sandy and deep, but completely covered with rocks and crypto.Fairly wide wash, with high cover of medium- & small-sized rocks. Terraces are low and still have good cryptobiotic crust cover and larger boulders on them. Ledgy bedrock is exposed on the west bank of the wash. The more upland-type shrubs are on the banks of the wash.Shallow, sandy soils that have blown in over White Rim bedrock. Shrubs are pedestalled on mini-dunes, and tiny rock fragments coat the soil surface.RY <  a -#v@;rL12116Step In Slope1:24K Quad@Kayenta Formation0204000P0200200T0000ywusqomkgea__][YUQ>2&߿qK7311MidslopeGPS@Kayenta Formation02030002biocrust02P0T00P0000usqomkigeca]SOMKGC0$pJ7293MidslopeGPS@Kayenta Formation031-a0004biocrust02T0P001-a0000ywusqljhfdb^TPNLGC0$oI2220High LevelGPS@Obscured by Soil060001-bbiocrust030000000000usqomkigeca]SNLJHD2&!nH7263High LevelGPS@Kayenta Formation031-aP003biocrust1-bP00200P0000{ywusqomige`VRPNIE2&!mGvariablevariableStep in slopeGPS@Navajo Sandstone1-a031-a003crypto1-b1-b01-a001-a0000{vnjhc_ZH<7(lFzflatn/aHigh LevelGPSt@Kayenta Formation0203001-bcrypto02T002001-a0000}{ytrpljhd\WUSOK8,'kE|1278High LevelGPSZ@Kayenta Formation031-bT0Tcrypto1-bT00300T0000wusqomkieca\TRPNIE2&!jDLflatn/aHigh LevelGPS"@Kayenta Formation1-a06T01-acryptoT1-b01-b00T0000}{ywusnlge]XVTPK8,'iC1360Low levelGPS@Obscured by Soil0200003cypto1-b00030000000sqomkigea_]XQMKIGC1% hB169Low levelGPSb@Moenkopi Fm041-a001-bbiocrust1-aP0040000000trpnljhfb`^YOJHFA=0$gAflatn/aStep in slopeGPS@Talus/Colluvium/LandslidesTT001-acrypto1-a0400400T0000}{wuqld_][YW;/*f@}2969Toe slopeGPSh@Talus/Colluvium/LandslidesTT00Tcrypto1-a0500500T0000}{ywusqokie`XVTRPN2&!e?cflatn/aStep in slopeGPS@Talus/Colluvium/LandslidesT1-b001-bcrypto1-a030030000000~zxtogb`^YW;/*d>1528Toe slopeGPS6@Talus/Colluvium/LandslidesTT001-acrypto1-a0400400T0000~|zxvtrnlhc[VTRPN2&!c=tvariablevariableStep in slopeGPS@Talus/Colluvium/LandslidesP1-a00PcryptoP0300400P0000{yqomkfdH<7(b<1292High LevelGPS@White Rim Sandstone - Cutler Gp1-a07001-abiocrust1-aT01-a00T0000}xvtoe`^\XS2&!a;15228Toe slopeGPS$@Moenkopi FmT0000T1-a0090000000eca_][YWSQLJJHFDB@3'"`:-flatn/aStep in slopeGPS"@Obscured by SoilT007000200020000000sqomkigea_]YYWUQOM;/*_988186Toe slopeGPS"@Talus/Colluvium/LandslidesPT00PcryptoP0400500P0000ywusqomkgea_WUSQOM1% ^8+2191Step in slopeGPS@Talus/Colluvium/Landslides1-a1-b1-a01-acrypto1-a02004001-a0000~zxtogb`[VQ5)$]73168Toe slopeGPS@Moenkopi FmTT001-bcrypto1-a1-a0070000000qomkigec_]XSKFDB@>1% dLVAL d . 6. fBig shelves of slickrock with thin soils covering and very little crypto. A perfect fit for environment of MU33.Ledgy, large alcove with thin soils and various-sized rocks covering the sandstone.The point is on a high level plateau that is long and narrow, running mostly northwest and southeast. Ledgy Kayenta bedrock is exposed and has high cover. JUNOST is very stunted, as are the tall shrubs. Some very developed crypto in-between bedrock outcrops. Shallow soils.A broad, homogeneous valley filled with COLRAM. Crypto cover is patchy, but well-developed. Plot captured an unusually large patch of bedrock with some PURMEX growing around it.This is a bench at the base of the Wingate/Chinle Scarp of Junction Butte. JUNOST is stunted, large boulders everywhere; there are more grasses than at other points in polygon, but it's still very good example.This is a steeper talus toeslope off of the Wingate/Chinle scarp. Talus is large (RV- or car-sized) and erosional gullies run throughout it. JUNOST stunted & mainly on bench below.This flat bench is off the Wingate/ Chinle scarp and has a lot of Chinle bedrock exposed and large car-sized boulders throughout. JUNOST are stunted and there is more COLRAM here than in other areas.This is a steeper toeslope off of the Wingate/Chinle scarp, which has a high degree of erosional gullies throughout. Very large boulders in point, and shallow gullies on a bench below the toeslope (in point as well). JUNOST is stunted. Higher crypto cover on bench; none on slopes.This bench is bisected on both sides by Chinle toeslopes & has a rolling moraine microtopography. Large Chinle boulders ranging from RV to basketball size and stunted JUNOST. Mossback member bedrock exposed.Rolling White Rim bedrock outcrops forming mini-domes and small valleys in between with shallow soils stabilized by small rock and crypto cover. High shrub diversity and all are doing well. JUNOST not doing as well, some dieback and dead snags abound.LVAL 2 F TdThe surface is covered with pebbles.This is a large, nearly flat area. The soil is pebblyLow, undulating hills with broad outcrops of bedrock, mostly flat with some broken ledges; and areas in-between are stabilized by extensive and well-developed cryptos. PINEDU-dominated canopy. Many small surficial drainages dissect the plot.Low undulating hills dissected by shallow wash channels and stabilized by extensive and well-developed cryptos. Scattered bedrock exposures in area increase the PURMEX and FRAANO cover where they occur. Lots of downed wood and dieback on the shrubs and JUNOST.A broad EPHVIR/grassland community east of the plot transitions to a COLRAM shrubland with scattered PJ as you approach a small drop-off, where soils are shallower and there's more exposure of bedrock and small rock to the west. It's hard to put a good line on the map here, because the transitional zone is ~80 meters wide or more.Several drainages in the plot have bedrock exposures and probably contribute to the higher tree cover. Substrate of scattered small rocks and small bedrock shelves, but is dominated by fairly well-developed crusts. Tree cover is dominated by JUNOST.The point lies half on a Navajo slope to the lower bench (step in slope) to another Navajo slope. Very high crypto development and vegetation on the bench. Navajo slope and dome have little to no vegetation on them, except in cracks and potholes.Bedrock is exposed and is ledgy Kayenta; significant amounts of aeolian sand deposited around trees and shrubs to form an undulating, almost duney microtopography. Some crypto developed.A large plateau that has Navajo domes and Kayenta ledgy bedrock exposed. The plateau is relatively flat, but has shallow undulations in the microtopography. The surface of deeper, sandy soil has high small rock cover, some shallow aeolian-derived mounding around shrub clusters, and some pedestalling.\& ] - < Rnr kdTflatn/aLow levelGPS@Aeolian Sands1-a008001-b001-a0000000qomkigec^\ZUUSQMKF7+&c<1250Toe slopeGPS@Moenkopi Fm1-a02T001-a1-b0070000000ljhfdb`^ZXSNNLJHD?2&!bflatn/aHigh LevelGPS@Cedar Mesa SandstoneT09T00TT0T00T0000pnljhfdb`^\ZZXVTPN8,'avariablevariableStep in slopeGPS:@Cutler Group (undiff)T04T001-a1-a0040000000}{wupkkigea_H<7(`/flatn/aLow levelGPS@Aeolian Sands1-b01-b000300030000000pnljhfdb^\ZVVTRMKF7+&_2202Step in slopeGPSr@Cutler Group (undiff)T03T00TT0050000000pnljhfdb^\ZXXVTRNL5)$^Wflatn/aLow levelGPS@Aeolian Sands1-a1-a040Tcrypto0200030000000zxvtrpnlhfd`XVTPKF7+&]U3318Low levelGPS@Moenkopi FmT02000TT00800T0000b`^\ZXVTPNLJJHFD@>1% \s846MidslopeGPS@ Moenkopi FmT1-b000T1-b00800T0000db`^\ZXVRPKIIGEC></#[31318MidslopeGPS@ Talus/Colluvium/LandslidesTT00Tcrypto020500200T0000|zxvtrpnjhd`XVTRPN2&!Zflatn/aLow levelGPS@ New AlluviumT0020TcryptoT040030000000sqomkigea_[YQOMIGE7+&Yflatn/aLow levelGPS,@ New AlluviumTT020Tcrypto020200300T0000usqomkigca]YQOMIGE7+&~XL2156Toe SlopeGPS@Moenkopi FmPTP00TT00800T0000`^\ZXVTRNLJHHFDB@>1% }WM2170Toe SlopeGPS@Moenkopi Fm030T00T00060000000b`^\ZXVTPNLJJHFDB>1% |VP1251High LevelGPS@White Rim Sandstone - Cutler Gp0206000TT0020000000ywusqomkgecaa_][WS2&!{U31118InterfluveGPS@Moenkopi Fm02P0003biocrust01-b0030000000trpnljhfb`[YOKIGEA4(#zT/322Low SlopeGPS@Aeolian SandsP00800P00T00T0000a_][YWUSQOMKKIGCA?0$ySs58High SlopeGPS@Moenkopi Fm020000T1-b0070000000ca_][YWUQOJHHFDB@</#xR42295Toe SlopeGPS@Moenkopi Fm0500300TT01-b0000000eca_][YWRPNLLJHDB>1% wQ22313Toe SlopeGPS@Moenkopi Fm0400500T00P0000000b`^\ZXVTRPNLLJHDB>1% vPM3155Toe SlopeGPSH@Moenkopi FmPTT00TT0080000000`^\ZXVTRNLJHHFDB@>1% uOM2206Toe SlopeGPSl@Moenkopi Fm040T00T00050000000b`^\ZXVTPNLJJHFDB>1% tN2842MidslopeGPS@Kayenta FormationPP000P020070000000hfdb`^\ZVTPNNLJHFD1% sMS442High LevelGPS@ Kayenta Formation1-a04000P1-b00300T0000nljhfdb`\ZUSSQOMID1% 2LVALr  Z*\Plot is on lower slopes of this canyon, with Cutler soils and occasional blocks of White Rim fragments.This mudslide point is entirely covered with small, platey and shaley rock. Some Moenkopi ledgy bedrock is exposed, forming sloping benches throughout this hill. Many large boulders lie throughout, as well.This is a talus-filled slope in the Wingate/Chinle scarp. The Wingate is in the form of a half-circle, with many deep gullies running through the talus slope. Talus is RV- and car-sized and smaller; small rocks and bare soil collect on the uphill side of boulders.This wash has high boulder cover and small rocks. Many of the trees and shrubs in the wash have roots exposed. Areas further south of the point have puddling from recent rains, but not at point.This point is in a tributary wash of Musselman Canyon, and includes the wash and shorter terraces. A high cover of small rock in wash and on terraces.Lots of pebbles cover the surface of this broad, almost flat toeslope.This is a broad, almost flat toeslope. The soil is typical pebbly Moenkopi.There are a few patches of thin, pebbly soil in the plot, but most of the area is solid White Rim sandstone.These steep badlands seem to be eroding fast and discouraging much growth; however, where the slope mellows a little, the surface is covered with thick biocrust. A few gypsum crystals decorate the site.A little bit of Moenkopi soil is showing through in spots, but this site is mostly active sand.This is classic Moenkopi, with rolling hills and occasional bedrock outcrops. The surface is nearly covered by little flat rocks.A thin layer of sand has blown in, partially covering the pebbly Moenkopi soil.A thin layer of sand has blown in, partially covering the pebbly Moenkopi soil.Talus slope with many small rocks and a few scattered boulders. Many undulations and ravines across the slope, so there is a variety of warm and cool aspects here. Vegetation is moderately dense here, but species fit MU30 better than MU29 for sure.LVAL D 4 f0>4Pebbly soils, less compacted than AA0261 in same polygon.Classic White Rim slickrock with trace soils in low spots and joints.Very small dunes forming around EPHTOR clumps. Active sand blowing; ground cover nearly all sand. Grasses taller while shrubs are shorter. Patches of small rocks throughout. Some pedestalling.This sandsheet is directly off of the main road and has an undulating microtopography, due to aeolian-derived sand mounds and some pedestalling of shrubs. Grasses are very healthy and tall, while EPHTOR is shorter. Patches of small rocks throughout.This point lies on the toeslope of the Moenkopi ledgy bedrock scarp. The ground surface is completely covered with small, platey rocks, and bedrock is exposed in places. It lies about 30 meters from the White Rim road.This is a very sparsely vegetated, flat bedrock outcrop above the river and below the Cutler layer. Vegetation is growing in potholes only with developed cryptos covering the soil in potholes.This bench is fairly level with an undulating microtopography due to water erosion gullying. High cover of bedrock exposed at ground level and canyon sides.This is an extensive bench that is directly below the Cutler bedrock canyon sides, but the ground cover has high sand cover and small rocks. There are shallow gullies throughout. Soil is deep on benchPoint is on a bench with Cutler Canyon sides and boulders throughout. Surface covered with platey rock and shelfy boulders and some shallower gullies throughout. Sand in gullies only.This area has a little White Rim bedrock exposed, but most of the ground cover is small rocks, sand, and bare soil. Some small mounds are forming via aeolian sand deposition. Shallow soils (bedrock exposed).This is a low level bench completely covered with small, platey, shaley rocks. Some ledgy Moenkopi bedrock is exposed, and some car-sized boulders lie throughout bench (although far fewer boulders than the opposing slope).Y _  b D +w.'z26326MidslopeGPSx@Organ Rock Shale - Cutler Gp1-a0300Pbiotic soilT0200400T0000~|zxtrnl_][YUP2&!y&550High SlopeGPS@Cutler Group (undiff)0202000T1-a00500T0000qomkigec_]XVVTRPLH1% x20108MidslopeGPS@Cutler Group (undiff)021-aT00T020050000000rpnljhfd`^ZXXVTRMI2&!w4146Step in slopeGPS@Cutler Group (undiff)1-a031-a0Tbiotic soilP1-b0040000000~|zxtrmk^\ZUQL5)$v15184Step in slopeGPS@Moenkopi Fm031-a000P0200400T0000mkigeca_[YUSSQOMHD7+&u27358MidslopeGPSMostly sandy, pebbly soils.Talus/Colluvium/Landslides03T00Tbiotic soil1-a0300300T0000wusqokO&!t2520Toe slopeGPS@Talus/Colluvium/Landslides040P0Tbiotic soil1-a0300200P0000~|zxvrplgZXVTRN2&!s1484MidslopeGPS|@Talus/Colluvium/Landslides030P0Tbiotic soil020300200P0000~|zxvtpnjfYWUSQM1% r30128Midslope1:24K Quad@Talus/Colluvium/Landslides03P0001-a0300300P0000~|zxvtrpljfaa_][YU9-!q15352Midslope1:24K Quad@ Organ Rock Shale - Cutler Gp03P000P0200400T0000}{ywusqokiecca_][W9-!p20340Midslope1:24K Quad@Organ Rock Shale - Cutler Gp03P000P0300300T0000}{ywusqokiecca_][W9-!o2086Midslope1:24K Quad@Organ Rock Shale - Cutler Gp061-a000TP00300T0000}{ywusqokigeeca_ZV8, n308Midslope1:24K Quadf@Organ Rock Shale - Cutler Gp03P000020300200P0000|zxvtrpnjhd``^\ZXT6*m1520Toe slope1:24K Quad4@Organ Rock Shale - Cutler Gp021-a000P0200500T0000~|zxvtrnlhffdb`[W9-!l20350Midslope1:24K Quad4@Organ Rock Shale - Cutler Gp02P0001-b0300200P0000~|zxvtrnlhcca_][W9-!k1510Toe slope1:24K Quad@Cedar Mesa Sandstone06P0003biotic soilTT01-a00T0000}{ywupnlj]YWUSO9-!j3680MidslopeGPSt@Talus/Colluvium/LandslidesT0000T060040000000qomkigec_]YWWUSQOM1% if32135High SlopeGPS@Moenkopi FmT03000T030030000000geca_][YUSOMMKIGCA4(#hBflatn/aLow levelGPS@Moenkopi FmT000002020070000000jhfdb`^\XVRNNLJHFD7+&g3710MidslopeGPS@Talus/Colluvium/LandslidesT00001-a0500500T0000trpnljhfb`\WWUSQOM1% fvariablevariableHigh LevelGPS@Moenkopi FmT1-a0001-a00090000000zxvtrpnlhfd__][YTRE94(e`flatn/aLow levelGPS@Aeolian Sands1-a008001-b001-a0000000qomkigec^\ZUUSQMKF7+&LVAL . N ~Another sheltered, north-facing slope below the White Rim with Cutler soils but lots of big blocks of the White Rim scattered about. Rhamnus betulifolia and Ostrya tend to stay at the tops of the slopes where its likely more mesic and certainly shadier. Aquilegia is only at seep line under the White Rim.Cutler soils with occasional blocks of White Rim - concentrated in the gully areas of this polygon. Amelanchier the clear dominant in this small polygon.Soils are Cutler with large blocks of White Rim strewn about. This polygon gets mesic help from drainage off the rim, as well as from the seeps below it.Plot is on a relatively deep soiled slope along a wash channel. Soils appear rocky where bare, but there is lots of biotic soil development. Soils appear to be weathered from a band in the Cedar Mesa more closely resembling undifferentiated Cutler.This talus slope is made up of Wingate-derived boulders that are RV- to car-sized, with smaller boulders and rocks piled on the uphill sides. A mine entrance is directly below the point.This point lies directly below a cliff band of Moenkopi bedrock. The ground cover is entirely shaley/platey rocks and boulders. Deep erosional gullies bisect the hillslope and the vegetation is sparse.This is a low level area between Moenkopi slopes off of the White Rim. The ground is covered with small rocks, and large boulders are scattered throughout. There are slight undulations in the microtopography.This talus-filled hillside is nearly completely covered with rocks. Small and medium rocks are piled on the uphill sides of huge boulders. JUNOST are stunted. Talus is Wingate-derived rock lying on the Chinle scarp.Point lies exactly on top of a small ridge, about 10 meters wide, with steep slopes on either side. The ground is completely covered with small, platey rocks. Ledgy bedrock cliffs are below on hillsides and above on next ridge level. LVAL6 & D(Plot is in a highly transected area of cliffs and minor drainages with the vegetation growing on the "steps" between the short cliffs. Plot is in an area with slightly more extensive flat surfaces, but the vegetation is consistent with the more cliffy areas of polygon.The "step" in this slope is a toeslope-like less steep area between two cliff bands. Lots of large boulders from the Mossback member upslope litter the area, as well as exposed Moenkopi shaley bedrock exposures. What soil there is very pebbly or rocky. Trees are generally stunted and concentrated at bedrock exposures along cliff rims.The steep wash in 522 is lower angled here, and it's really the steep N-facing talus slope above the wash that consistently represents the community. Shrubs are not as dense, but they're the same species. No Populus fremontii here. The slopes may be getting more hydration from the slickrock above, but mostly they're just a cooler, wetter exposure.Despite the fact that this is a steep wash draining slickrock above, the vegetation is primarily among the talus boulders at the toe of the steep colluvial slopes on either side of the drainage - thus the call on the geology. The boulders are large, and protect the shrubs, which are equally large. See also AA 0524.Plot is located in huge boulders of Wingate, in a steep "V" head to Buck Canyon. Areas up slope of plot are slickrock slabs of Wingate contributing to the runoff fostering this localized community.North-facing slopes of Cutler bedrock and soils with chunks of broken White Rim caprock here and there. Evidence of seeping water at the base of the White Rim overhangs all along the top of the slopes of this polygon. Tall shrubs and trees are concentrated on upper slopes, with Aquilegia just under White Rim overhangs.Plot is in an extensive area of steep, soil-covered ledges and slopes extending down slope from the White Rim. Blackbrush dominates bench areas down slope of plot, and blackbrush in plot in invading from there (outside polygon).LVAL \ ^ |\vP*Steep Wingate derived colluvium thinly distributed over the Chinle - there are areas of Chinle bedrock in plot, mostly a dark, thin sandstone band.Platey Moenkopi soils with lots of minor bedrock ledges and cliffs. These slopes are heavily transected by minor gullies, creating lots of variability in aspect.Plot is on uneven terrain, with species list #1, pertaining to a west facing steep slope with ledgy terrain, and list #2 the flatter, deeper soils on top, with a variable aspect generally trending more southward than aspect listed indicates.Plot is on the edge of toeslopes at the base of a small ridge, but is consistent with the extensive bench areas around the head of Little Bridge Canyon. Chrysothamnus does seem limited to the toeslopes, and doesn't occur on the flatter areas.Deeper, pebbly soil. Hilaria is much lusher here than I've generally encountered in other Atriplex confertifolia - Hilaria jamesii communities.Plot is in an area of rocky north-facing Moenkopi soils. Snakeweed is mostly along the edge of the toeslope, at its most down slope areas, on flatter ground. More runoff there, perhaps.Plot is on a low wash terrace, with deep sandy soils. Tamarisk has been cut and sprayed in the plot and its vicinity. The stumps and dead stems are still here. Very disturbed area.Very rocky, pebbly soil with a northern exposure, below a short caprocked cliff. Down slope are extremely sparse slickrock slabs of the Cedar Mesa - plot doesn't include that environment.Plot is located on the edge of where the Cutler is beginning to differentiate between the Cedar Mesa and Organ Rock members. Portions of the plot lap off a large cliff to Cedar Mesa-like sandstone slickrock, and these parts are unvegetated. Areas E of plot should actually be a different polygon - as unvegetated geology.Plot (naturally) landed on the cliffy side of a shallow canyon, but the ledge areas, canyon floor and rim areas (all included in plot) all have the same vegetation. Vegetated surfaces are closer to 0-5% slope.T : A .JN6194Low levelGPS@Moenkopi Fm08000TBiotic soilP001-b00T0000omkigeca\ZXVIGECA=0$328Low levelGPSb@Moenkopi Fm07P00PBiotic soil1-a000200T0000qomkigec_][VIGECA=0$124Low levelGPS@ Moenkopi Fm08P00TBiotic soil1-a001-a00T0000rpnljhfd_][VIGECA=0$134Low levelGPS@ White Rim Sandstone - Cutler GpP0800PBiotic soilTP0P0000000~|zxvtrpnlj][YWSQ0$132Low levelGPS@White Rim Sandstone - Cutler Gp020500Tbiotic soilTT0030000000~|zxvrpnl_][YUQ0$e2538MidslopeGPSn@Talus/Colluvium/Landslides03000Pbiotic soil020300200T0000~|zxvtpnjfYWUSQM1% 156Low levelGPS@Moenkopi Fm03PP001-b0200300T0000fdb`^\ZXTRNIIGECA=0$3140Low levelGPS@Moenkopi Fm02000Tbiotic soilP1-b0060000000rpnljhfd`^YWJHFDB>1% 342Low levelGPS@New Alluvium02P02001-a0300200T0000igeca_][WUQLLJHDB>0$3104Low levelGPS,@New Alluvium02P02001-a0300200T0000jhfdb`^\XVRMMKIEC?1% {176Low levelGPSr@ Moenkopi Fm0400002cryptos1-a00030000000omkigeca][YTKGECA=0$1104Low levelGPSVery compacted, pebbly soilsMoenkopi Fm1-b0000P1-a0080000000~|zxvrpkiigeca\O% z1100Low levelGPS@New Alluvium1-a020200P1-b00300T0000kigeca_]YWRPPNLHD?1% p2136Low levelGPS@ White Rim Sandstone - Cutler GpP0900Pbiotic crustP00T00T0000~|zxvtrpnl^\ZXTR1% 178Low levelGPS\@New Alluvium021-a0300T0200300T0000igeca_][WUQOOMKGB>0$ 25166MidslopeGPS @Talus/Colluvium/Landslides02P0001-a0300400T0000wusqomkiec_ZZXVTRN2&!32144MidslopeGPS&@ Talus/Colluvium/Landslides021-a000P030040000000wusqomkiec_]][YWRN2&!f20190MidslopeGPSD@Moenkopi Fm1-b1-b000P0300400T0000igeca_][WUQOOMKID?2&!15296High SlopeGPS@Chinle Formation061-a000P1-b00200T0000pnljhfdb^\WUUSQOJF4(#~g78Toe slopeGPS@Moenkopi Fm020000P020060000000a_][YWUSOMIGGECA?;."}W3120Low levelGPS @Moenkopi Fm03000Tmoss1-aT0060000000kigeca_]YWUPJHFDB>1% |B1050Toe slopeGPSt@Moenkopi Fm1-aP000T1-b0070000000geca_][YUSNLLJHFD?2&!{flatn/aLow levelGPSn@New Alluvium07000Pbiotic soil0300000P0000vtrpnljhfdb^QOMKIE7+&NLVAL h < b.rPlot is on thin but consistent soils with a small rock content (not sands) over the White Rim.Classic White Rim slickrock, vegetation in joints and shallow depressions.Much of plot is barren of vegetation, but has a very thin pebbly soil in what is probably an outwash area from a drainage upslope. Otherwise, it fits the 10a description - blackbrush in thin soils in joints.Wingate-derived soils and huge boulders on slopes not quite as steep as usual, due to the band of Mossback down slope of plot area. Trees and shrubs are dense and happy in this area.This wash, in vicinity of plot, is actually a set of very shallow, very narrow braided channels with native Moenkopi rocky soils forming small island/terraces as banks. Vegetation tends to be on the southeast low terrace/bank/island features, and is a mix of wash-specific vegetation and upland species from the surrounding community (blackbrush dominated).Plot includes a shallow, surficial drainage area that increases grass (galleta) cover. Platey pebble covered soils.Narrow sand and large rock channel, minimal or no terraces. No pinyon in plot. Less evident ERINAU than in AA0219. PURMEX and Rhus co-dominate tall shrubs, and Juniper seems a bit more significant here than in AA0219.Narrow, gullied wash with sparse vegetation in the channel itself. Channel is mostly large rock and sand. Trees are sparse, but unique to wash area.Wash bottom in much of plot is actually White Rim bedrock. Otherwise, a very low sandy terrace in or on the sides is where vegetation occurs.Dry, open wash, with sparse vegetation. Chrysothamnus is the common denominator along the wash banks, with occasional Rhus and juniper, rarely also tamarisk and Amelanchier.Bouldery, generally steep Wingate - derived talus. Rhus and trees are denser on the lower slopes. Areas across this canyon facing north (in same polygon) appear to be Amelanchier (up to 10%) with an herbaceous understory - no trees except at the bottoms of those slopes. LVALD 8 N .6:Plot is in a shallowly depressed area that appears to have deep, fine soils, and less rock than surrounding areas with COLRAM.Plot is in an area with greater winterfat cover than most of the polygon, possibly because it's a lower, shallow depression.Vegetation is on flat surfaces, but cliffs give overall plot as steep slope. Vegetation is in cracks and joints, or thin soils on ledges. Most of plot is slickrock - very sparse.Slope is average of steps and small cliff bands in plot. Very thin soils in cracks and joints, or depressions on ledges. This is a relatively lush spot compared to much of polygon.A very sparse, mostly bedrock plot and polygon. A major drainage transects plot, but the vegetation isn't much affected because it's mostly on thin soils in cracks and shallow depressions on ledges.This plot is 99% bare slickrock. See AA #41 for discussion.Slickrock ledges with thin soils. Most of plot and vicinity is bare rock. Vegetation is on surfaces averaging about 10% slope, but whole plot, including cliff bands is represented by slope given.Flakey- pebbly soils with areas of well-developed biotic crusts. The community here is fairly extensive, as the ledge areas are broader, and the species diversity is notably homogenous throughout the area. Way cool spot.Lots of narrow ledges w/thin, flakey soils on the Organ Rock just above its contact with the Cedar Mesa. Species here are typical of this type of terrain.A bit of a mish-mash here, upland species on banks straddling a more or less bedrock wash.A dry, sandy wash with very sparse vegetation.Deep, sandy but stabilized soils.Deep, sandy soils. Slight pedestalling of some shrubs.Very fine, deep soils with no rock, but no evidence of dunes. Very slight pedestalling on some shrubs.Deep, sandy soils, possibly once of aeolian source, but there are no dunes here and soils are quite stabilized.Deep, pebbly soils. Slightly undulating surfaces, slight blowout areas here and there.Slightly deeper, still pebbly soils than AA #139.4Q J ; 7 fx-p12358MidslopeGPS@Talus/Colluvium/Landslides1-bT0001-a0701-b0000000ywusqomkfd`[[YWUSN2&!flatn/aLow levelGPS@Obscured by Soil030T0Tcrypto03T0040000000wusqomkieca]USQOMI7+&flatn/aLow level1:24K Quad@Obscured by Soil020T0Tcrypto0300050000000~|zxvtrpljhd\ZXVTP>2&flatn/aLow level1:24K Quad@New Alluvium0008001-a1-a01-a0000000wusqomkidb]XXVTPNL>2&߿3150Low levelGPSPebbly soils.Moenkopi Fm07P000TT0030000000qomkigec_][YYWUSQM@% 142Low levelGPSD@Moenkopi Fm08000PBiotic soil020000000000nljhfdb`^\ZVIGECA=0$258Low levelGPSV@Moenkopi Fm08000PBiotic soil020000000000nljhfdb`^\ZVIGECA=0$230Low levelGPS@Moenkopi Fm08000PBiotic soil020000000000nljhfdb`^\ZVIGECA=0$276Low levelGPS@Moenkopi Fm0600002Biotic soilP00020000000pnljhfdb^\ZXKGECA=0$ 4290MidslopeGPSPebbly soils are deep.Moenkopi Fm070000T00030000000ywusqomkgecaa_][YUH$x25180Step in slopeGPSh@Cedar Mesa Sandstone1-a0800Pboitic soilT1-a01-a00T0000}{ywrpki\ZXVRM7+&1576Step in slopeGPSl@ Cedar Mesa Sandstone020400Pbiotic soil1-a0201-b00T0000}{ywrplgZXVTPL6*%Y2010MidslopeGPS@ Cedar Mesa SandstoneP09p0Tbiotic soilTP0P00T0000vtrpnljhfdb`SQOMIG1% 5030MidslopeGPSx@ Cedar Mesa SandstoneT09000TT0P0000000igeca_][YWUSSQOMIG1% 35174Step in slopeGPS@ Cedar Mesa Sandstone1-a05000T0200300T0000vtrpnljhdb^\\ZXVRM7+&1530High SlopeGPS@ Organ Rock Shale - Cutler GpT1-b001-bcryptoT020040000000}{ywuqokia\ZXSQ3'"L25334MidslopeGPS6@Organ Rock Shale - Cutler Gp1-a03000P0200400T0000ywusqomkgea__][YUP2&!10144Toe slopeGPS@Organ Rock Shale - Cutler Gp021-bP00T1-b0050000000{ywusqomigb``^\ZUQ3'":180Low levelGPS\@Organ Rock Shale - Cutler Gp021-a0300P0200200T0000ywusqomkgea__][WRN0$1352Low levelGPSB@Obscured by Soil080001-aBiotic soil1-a00000T0000xvtrpnljhfd_RMKIGC1% 1294Low levelGPSn@Obscured by Soil08000PBiotic soil1-b00000T0000usqomkigeca\OMKIGC1% 1340Low levelGPS@Obscured by Soil080001-aBiotic soil1-a00T00T0000xvtrpnljhfd_RMKIGC1% 2348Low levelGPS@Obscured by Soil080001-aBiotic soils1-a00T00T0000ywusqomkige`RMKIGC1% $LVAL f 4 Dz&FHTypical Moenkopi hillslope with ledgy bedrock exposed and ground covered with shaley, platey rocks that are hand-sized and smaller. COLRAM is dominant and more than 9%, so I chose COLRAM name.Areas of White Rim bedrock exposed through the shallower sandy soils of this point. Ground covered with small rocks, bare soil, and some cryptos. Slight mounding on the microtopography scale.There are large areas of White Rim bedrock exposed at this point which has shallower, sandy soils with high cover of small rocks on surface and is adjacent to the White Rim. Vegetation is predominantly COLRAM.This is a triangular polygon formed by the saturation of the talus slope by the pour-off from the White Rim. Dense vegetation formed by the abundance of water.This talus slope is directly below the White Rim and has large boulders resting on the Cutler-derived slope (some ledges bedrock exposed). Vegetation is sparse and mixed.This point is midslope and in a gully. The talus are large and is both Cutler- and White Rim-derived.This is a large bench with the ground covered with small rocks and shallow gullies running throughout. The soil seems deeper here. There is little mounding or pedestalling. It could be considered a stabilized sandsheet perhaps, but very stabilized.This very large bench is between the Moenkopi toeslopes and the White Rim. The surface is covered with small rocks and has patches of PLEJAM herbaceous vegetation mixed into the pure COLRAM/PLEJAM shrubland.Point is at the bottom of a huge pouroff in a dry, sandy flat wash which is about 10m wide and has small and medium rocks throughout but is mostly sand. There is a definite channel in which most water flows, but the wash terrace is so low as to be flooded easily. Trees are mostly under pour offs and on western terrace of wash.Deep, fine soils. No aeolian or alluvial qualities stand out here, likely both wind and water have collected, the finer particles of soil here from nearby areas.See comments for AA #75. Deep, fine soils.OP $ .  teq'flatn/aLow levelGPSh@Aeolian Sands0000000000000000fdb`^\ZXVTRPPNLJHF7+&flatn/aLow levelGPS.@Obscured by Soil0200000200060000000omkigeca][YUUSQOMI7+&flatn/aLow levelGPS@Obscured by Soil0200000200050000000omkigeca][YUUSQOMI7+&flatn/aLow levelGPSt@Aeolian Sands02000Tcrypto0200060000000trpnljhfb`^ZRPNLJF7+&flatn/aLow levelGPS@Obscured by Soil0200000200050000000omkigeca][YUUSQOMI7+&flatn/aLow levelGPS@Obscured by Soil02000002T0060000000omkigeca][YUUSQOMI7+&flatn/aHigh LevelGPS@White Rim Sandstone - Cutler Gp1-a090001-a00T0000000}{ywusqomhhfdb^Y8,'3844High SlopeGPS@Talus/Colluvium/LandslidesT0000T0800200T0000sqomkigea_[YYWUSQO3'"flatn/aLow levelGPS@New Alluvium1-a1-a1-a001-b1-b005001-a0000ywusqljhdb]XXVTOJE7+&flatn/aLow levelGPSL@Moenkopi Fm03T000021-b00300020000omkigca_[YTPPNLJHD7+&flatn/aHigh LevelGPS@Obscured by Soil061-a00Tcrypto02001-a0000000|zxvtrpnigeaYWUSNJ8,'flatn/aLow levelGPS@Obscured by Soil051-a001-acrytpo02001-a0000000~|zxvtrpkigc[VTRMI7+&flatn/aLow levelGPS@Moenkopi Fm03TT0002000600T0000jhfdb`^\XVTPPNLJHD7+&flatn/aHigh LevelGPS@White Rim Sandstone - Cutler Gp1-a090001-a001-a00T0000~|zxvqomhhfdb^Y8,'variablevariableLow levelGPS@Moenkopi FmT0200002T00700T0000wusqomkieca]][YWSQD83(flatn/aLow levelGPS@Moenkopi Fm1-a1-a0001-b1-b00700T0000rpnljhfd`^YTTRPNID7+&flatn/aLow levelGPSx@New AlluviumTT03001-a03003001-a0000qomkidb`\ZVQQOMIGE7+&]28350High SlopeGPS~@Talus/Co