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Y  Y  Y PlotCode ELCODEClassif_GK `Ѐ`E!FYY ELCODEPlotCodev1U)  j  >=<;dCEBR.0021CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0020CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0019CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0018Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0017Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0016Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0015CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0014Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0013Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0012CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0011Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0010CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0009CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0008CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0007CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0006CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0005CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0004CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0003CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0002Park Special5Elymus trachycaulus Herbaceous Vegetation [Park Special].CEBR.0001CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(qY  - V , S-EfCEBR.0042CEGL003485Deschampsia caespitosa - Polygonum bistortoides Herbaceous Vegetation(CEBR.0041CEGL002988Artemisia cana (ssp. bolanderi, ssp. viscidula) / Poa pratensis Semi-natural Shrubland(CEBR.0040Park Special6Ericameria discoidea Dwarf-shrubland Herbaceous Sparse Vegetation [Park Special].CEBR.0039CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0038CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0037CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0036Park Special13Pinus ponderosa / Cercocarpus ledifolius / Arctostaphylos patula Woodland [Park Special]0CEBR.0035CEGL000744Juniperus scopulorum / Cercocarpus ledifolius Woodland(CEBR.0034CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0033CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0032CEGL000867Pinus ponderosa / Purshia tridentata Woodland(CEBR.0031Park Special16Pseudotsuga menziesii / Ribes montigenum Forest [Park Special]0CEBR.0030Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0029Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0028CEGL000439Pseudotsuga menziesii / Juniperus communis Forest(CEBR.0027CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0026CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0025CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0024CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0023CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0022CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(`?/n 4 s  E !x ]L6uCEBR.0066Park Special8Eriogonum umbellatum - Potentilla hippiana Herbaceous Vegetation [Park Special].CEBR.0065CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0064Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0063CEGL001133Ribes montigenum Shrubland\(CEBR.0062Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0061Park Special3Carex egglestonii Herbaceous Vegetation [Park Special].CEBR.0060CEGL003485Deschampsia caespitosa - Polygonum bistortoides Herbaceous Vegetation(CEBR.0059Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0058CEGL003485Deschampsia caespitosa - Polygonum bistortoides Herbaceous Vegetation(CEBR.0057Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0056Park Special5Elymus trachycaulus Herbaceous Vegetation [Park Special].CEBR.0055Park Special7Eriogonum panguicense Herbaceous Vegetation [Park Special].CEBR.0054A.1601Ligusticum porteri Herbaceous Alliancel CEBR.0053Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0052Park Special17Salix arizonica Shrubland [Park Special]0CEBR.0051CEGL001133Ribes montigenum Shrubland\(CEBR.0050BRCA_NEW_1Achnatherum lettermanii Herbaceous Vegetation(CEBR.0049CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0048Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0047Park Special17Salix arizonica Shrubland [Park Special]0CEBR.0046CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0045Park Special5Elymus trachycaulus Herbaceous Vegetation [Park Special].CEBR.0044CEGL001133Ribes montigenum Shrubland\(CEBR.0043CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(S= j  X = qjCCEBR.0090A.1605Lupinus argenteus Herbaceous Alliancej CEBR.0088Park Special6Ericameria discoidea Dwarf-shrubland Herbaceous Sparse Vegetation [Park Special].CEBR.0087Park Special6Ericameria discoidea Dwarf-shrubland Herbaceous Sparse Vegetation [Park Special].CEBR.0086Park Special7Eriogonum panguicense Herbaceous Vegetation [Park Special].CEBR.0085Park Special7Eriogonum panguicense Herbaceous Vegetation [Park Special].CEBR.0084Park Special7Eriogonum panguicense Herbaceous Vegetation [Park Special].CEBR.0083Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0082Park Special4Carex scirpoidea Seasonally Flooded Herbaceous Vegetation [Park Special].CEBR.0081Park Special4Carex scirpoidea Seasonally Flooded Herbaceous Vegetation [Park Special].CEBR.0080Park Special17Salix arizonica Shrubland [Park Special]0CEBR.0079Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0078Park Special5Elymus trachycaulus Herbaceous Vegetation [Park Special].CEBR.0077CEGL005264Bromus inermis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0076CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0075Park Special10Lomatium minimum - Arenaria fendleri Herbaceous Vegetation [Park Special]0CEBR.0074CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0073CEGL005264Bromus inermis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0072CEGL001133Ribes montigenum Shrubland\(CEBR.0071CEGL002988Artemisia cana (ssp. bolanderi, ssp. viscidula) / Poa pratensis Semi-natural Shrubland(CEBR.0070BRCA_NEW_1Achnatherum lettermanii Herbaceous Vegetation(CEBR.0069Park Special18Solidago multiradiata Herbaceous Vegetation [Park Special]0CEBR.0068CEGL001133Ribes montigenum Shrubland\(CEBR.0067Park Special9Helianthella uniflora Herbaceous Vegetation [Park Special].\?| i =  p FgdaCEBR.0114CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0113Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0112Park Special14Populus angustifolia - Picea pungens / Acer glabrum Woodland0CEBR.0111Park Special1Acer glabrum Colluvial Slope Shrubland [Park Special].CEBR.0110Park Special2Calamagrostis scopulorum Herbaceous Vegetation [Park Special].CEBR.0109Park Special11Picea pungens / Salix brachycarpa Woodland [Park Special]0CEBR.0108CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0107CEGL000522Populus tremuloides - Abies concolor / Arctostaphylos patula Forest(CEBR.0106CEGL000919Abies lasiocarpa - Picea engelmannii / Juniperus communis Woodland(CEBR.0105CEGL000619Populus tremuloides / Thalictrum fendleri Forest(CEBR.0104CEGL000439Pseudotsuga menziesii / Juniperus communis Forest(CEBR.0103CEGL000919Abies lasiocarpa - Picea engelmannii / Juniperus communis Woodland(CEBR.0102Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0101Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0100Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0099CEGL000242Abies concolor / Arctostaphylos patula Forest(CEBR.0098CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0097CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0096Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0095CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0094BRCA_NEW_2Cercocarpus ledifolius / Arctostaphylos patula Woodland (Provisional)(CEBR.0093CEGL000209Pinus ponderosa - Pseudotsuga menziesii / Arctostaphylos patula Woodland(CEBR.0092CEGL005264Bromus inermis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(CEBR.0091CEGL005265Poa pratensis - (Pascopyrum smithii) Semi-natural Herbaceous Vegetation(^_ ? h \  OAMI5CEBR.0140Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0139CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0138Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0137Park Special1Acer glabrum Colluvial Slope Shrubland [Park Special].CEBR.0136Park Special1Acer glabrum Colluvial Slope Shrubland [Park Special].CEBR.0135CEGL000242Abies concolor / Arctostaphylos patula Forest(CEBR.0134CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0133Park Special13Pinus ponderosa / Cercocarpus ledifolius / Arctostaphylos patula Woodland [Park Special]0CEBR.0132Park Special2Calamagrostis scopulorum Herbaceous Vegetation [Park Special].CEBR.0131CEGL003900Salix exigua ShrublandT(CEBR.0130Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0129Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0128A.586Cercocarpus ledifolius Woodland AlliancenCEBR.0127Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0126CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0125CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0124Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0123Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0122CEGL000392Picea pungens / Juniperus communis Forestz(CEBR.0121CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0120CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0119CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0118CEGL000242Abies concolor / Arctostaphylos patula Forest(CEBR.0117CEGL000587Populus tremuloides / Juniperus communis Forest(CEBR.0116CEGL000587Populus tremuloides / Juniperus communis Forest(CEBR.0115CEGL000251Abies concolor / Mahonia repens Forestt(m/ A j \ 6 ] :uClfCEBR.0164CEGL000522Populus tremuloides - Abies concolor / Arctostaphylos patula Forest(CEBR.0163CEGL000780Pinus edulis - Juniperus spp. / Cercocarpus montanus - Mixed Shrubs Woodland(CEBR.0162CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0161CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0160CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0159CEGL005927Picea engelmannii / Equisetum arvense Forest(CEBR.0158CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0157CEGL000242Abies concolor / Arctostaphylos patula Forest(CEBR.0156CEGL000522Populus tremuloides - Abies concolor / Arctostaphylos patula Forest(CEBR.0155CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0154CEGL000919Abies lasiocarpa - Picea engelmannii / Juniperus communis Woodland(CEBR.0153CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0152Park Special12Pinus longaeva - (Pinus spp.) Sparse Woodland0CEBR.0151Park Special6Ericameria discoidea Dwarf-shrubland Herbaceous Sparse Vegetation [Park Special].CEBR.0150CEGL000251Abies concolor / Mahonia repens Forestt(CEBR.0149CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0148CEGL001133Ribes montigenum Shrubland\(CEBR.0147CEGL000533Populus tremuloides - Abies lasiocarpa / Tall Forbs Forest(CEBR.0146CEGL000331Abies lasiocarpa - Picea engelmannii / Ribes (montigenum, lacustre, inerme) Forest(CEBR.0145CEGL001133Ribes montigenum Shrubland\(CEBR.0144CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0143CEGL000744Juniperus scopulorum / Cercocarpus ledifolius Woodland(CEBR.0142CEGL000744Juniperus scopulorum / Cercocarpus ledifolius Woodland(CEBR.0141CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland( S X  CEBR.0172Park Special11Picea pungens / Salix brachycarpa Woodland [Park Special]0CEBR.0171CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0170CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0169Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0168CEGL000842Pinus ponderosa / Arctostaphylos patula Woodland(CEBR.0167CEGL000249Abies concolor / Juniperus communis Forest|(CEBR.0166Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0CEBR.0165Park Special15Populus angustifolia Temporarily Flooded Terrace Woodland0 @ @ @ @ @ @ @ @ @ @ @ @ @@ @ @ @ @ @@@@@@@@@@J8B68 J8B6@J@FB LiMJ+bQs+8LiMJ+bQs+8LiMJ+bQs+:MQU^666:6HMQU^666:>:MQU^666:>:MQU^666:>:MQU^666:>:MQU^666:>HMQU^666:>H MQU^666:>HMQU^666:>HMQU^666:>HMQU^666:>HMQU^666:@8MQU^666:@8MQU^666:@8MQU^666:@8 MQU^666:@8MQU^666:@8 MQU^666:@8MQU^666:@8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8 MQU^666<<8 MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8MQU^666<<8 MQU^666<<8MQU^666> MQU^666D>>MQU^666D>>MQU^666DF6MQU^666F>: MQU^666F>: MQU^666F>:MQU^666F>:MQU^666F>:MQU^666F>:MQU^666F>:MQU^666F>:MQU^666F>:MQU^666F>:MQU^666FBD MQU^666H8H MQU^666H8HMQU^666H8H MQU^6688<<MQU^6688<<MQU^6688<<MQU^6688<<MQU^6688<<MQU^6688<<MQU^6688<<MQU^66:HFFMQU^66:HFFMQU^66<>F@MQU^66<>F@MQU^66<>F@MQU^66MQU^66@:B> MQU^66@:B>MQU^66@:B@MQU^66@:B@MQU^66@:B@MQU^66@:B@MQU^66@:B@MQU^66@:B@MQU^66@:B@ MQU^66@:B@MQU^66@H:DfJi\kfQMYJ^8fJi\kfQMYJ^8fJi\kfQMYJ^8fJi\kfQMYJ^86fJi\kfQMYJ^88fJi\kfQMYJ^88fJi\kfQMYJ^8: fJi\kfQMYJ^8: fJi\kfQMYJ^8: fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8: fJi\kfQMYJ^8: fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8:fJi\kfQMYJ^8: fJi\kfQMYJ^8<fJi\kfQMYJ^8<fJi\kfQMYJ^8>fJi\kfQMYJ^8@fJi\kfQMYJ^8@ fJi\kfQMYJ^8@fJi\kfQMYJ^8@ fJi\kfQMYJ^8@ fJi\kfQMYJ^8@fJi\kfQMYJ^8@fJi\kfQMYJ^8@fJi\kfQMYJ^8B fJi\kfQMYJ^8DfJi\kfQMYJ^8D fJi\kfQMYJ^8D fJi\kfQMYJ^8FfJi\kfQMYJ^8F fJi\kfQMYJ^8FfJi\kfQMYJ^8FfJi\kfQMYJ^8FfJi\kfQMYJ^8FfJi\kfQMYJ^8FfJi\kfQMYJ^8F fJi\kfQMYJ^8FfJi\kfQMYJ^:fJi\kfQMYJ^:fJi\kfQMYJ^<fJi\kfQMYJ^>fJi\kfQMYJ^>fJi\kfQMYJ^@fJi\kfQMYJ^@fJi\kfQMYJ^@ fJi\kfQMYJ^@ fJi\kfQMYJ^BfJi\kfQMYJ^BfJi\kfQMYJ^BfJi\kfQMYJ^B fJi\kfQMYJ^D fJi\kfQMYJ^DfJi\kfQMYJ^DfJi\kfQMYJ^DfJi\kfQMYJ^FfJi\kfQMYJ^HpMQLi6668MQLi666:MQLi666<MQLi666>MQLi666@MQLi666BMQLi666DMQLi666FMQLi666HMQLi6686 MQLi6688 MQLi668: MQLi668< MQLi668> MQLi668@MQLi668BMQLi668DMQLi668FMQLi668HMQLi66:6MQLi66:8MQLi66::MQLi66:<MQLi66:>MQLi66:@MQLi66:BMQLi66:DMQLi66:FMQLi66:HMQLi66<6MQLi66<8 MQLi66<: MQLi66<< MQLi66<> MQLi66<@ MQLi666MQLi66>8MQLi66>:MQLi66><MQLi66>>MQLi66>@MQLi66>BMQLi66>DMQLi66>FMQLi66>HMQLi66@6MQLi66@8MQLi66@: MQLi66@< MQLi66@> MQLi66@@ MQLi66@B MQLi66@DMQLi66@FMQLi66@HMQLi66B6MQLi66B8MQLi66B:MQLi66B<MQLi66B>MQLi66B@MQLi66BBMQLi66BDMQLi66BFMQLi66BHMQLi66D6MQLi66D8MQLi66D:MQLi66D<MQLi66D>MQLi66D@MQLi66DB MQLi66DD MQLi66DF MQLi66DH MQLi66F6 MQLi66F8MQLi66F:MQLi66F<MQLi66F>MQLi66F@MQLi66FBMQLi66FDMQLi66FFMQLi66H6MQLi66H8MQLi66H:MQLi66H<MQLi66H>MQLi66H@MQLi66HBMQLi66HDMQLi66HFMQLi66HHMQLi6866 MQLi6868 MQLi686: MQLi686< MQLi686> MQLi686@MQLi686BMQLi686DMQLi686FMQLi686HMQLi6886MQLi6888MQLi688:MQLi688<MQLi688>MQLi688@MQLi688BMQLi688DMQLi688FMQLi688HMQLi68:6MQLi68:8MQLi68::MQLi68:<MQLi68:> MQLi68:@ MQLi68:B MQLi68:D MQLi68:F MQLi68:HMQLi68<6MQLi68<8MQLi68<:MQLi68<<MQLi68<>MQLi68<@MQLi686MQLi68>8MQLi68>:MQLi68><MQLi68>>MQLi68>@MQLi68>BMQLi68>DMQLi68>FMQLi68>HMQLi68@6 MQLi68@8 MQLi68@: MQLi68@< MQLi68@> MQLi68@@MQLi68@BMQLi68@DMQLi68@FMQLi68@HMQLi68B6MQLi68B8MQLi68B:MQLi68B<MQLi68B>MQLi68B@MQLi68BBMQLi68BDMQLi68BFMQLi68BHMQLi68D6MQLi68D8MQLi68D:1@A1 b D & R  s <  n 6  d  p_ l uD hP2xBAAIDtblAADetails.AAID8 wtblAAEnvironment111 tblAADetails))) GPS_Data_Download333  GtblAAEnvironment111 O  GGPS_Data_DownloadtblAALocation`@#YM3 SurveyorsGPS_Data_Download.SurveyorK# wSurveyDateGPS_Data_Download.GPS_DateM% wCameraUsedGPS_Data_Download.CameraK% wAACodetblAALocation.AACode? wtblAALocation+++ GPS_Data_Download333  GtblAADetails))) O  G  DiffCorrectedGPS_Data_Download.Corr_TypeT+ w  ParkCodeParkCode"CARE"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    G [PhotoFrame]+ '  [PhotoRoll]* ' 8@# '  [PhotoID]( g [PhotoFrame]+ g  [PhotoRoll]* g tblPhotos###     G aCount([BPUCode])>11 ' a [BPUCode]( g aNumberOfDupsCount([BPUCode])G)) o aBPUCode FieldFirst([BPUCode])I++ o atblBPU  a  a G R.0Z@# ' .0[PhotoFrame]+ g .0 [PhotoRoll]* g .0 [PlotCode]) g .0NumberOfDupsCount([PlotCode])H)) o .0PhotoFrame FieldFirst([PhotoFrame])R11 o .0PhotoRoll FieldFirst([PhotoRoll])O// o .0PlotCode FieldFirst([PlotCode])L-- o R.0Query3  R.0  .0 G"LVALnZ L > H D |$` .B@ltblPlotDetails.[PlotID] = tblPhotos.[PlotID]tblVegetation.VegetationID = tblVegetationDetails.VegetationIDtblPlotDetails.PlotID = tblVegetation.PlotIDtblVegetationDetails.ObsPointCoverClass((([tblPlotLocation].[IsObservationPt])=True))[tblPlotDetails].[PlotID]=[tblVegetation].[PlotID][tblVegetation].[VegetationID]=[tblVegetationDetails].[VegetationID][tblPlotLocation].[PlotCode]=[tblPlotDetails].[PlotCode]tblPlotLocation.PlotCode = tblISKY_UTMs_Import.PLOTCODEtblPlotDetails.PlotID=tblVegetation.PlotIDtblPlotDetails.PlotCode=Final_Classification_Import.PlotCodeFinal_Classification_Import.Classif_GKtblPlotDetails.PlotID = tblVegetation.PlotIDtblPlotDetails.PlotCode = Final_Classification_Import.PlotCodeFinal_Classification_Import.Classif_GKFinal_Classification_Import.PlotCodetblPlotDetails.PlotID = tblVegetation.PlotIDtblPlotLocation.PlotCode = tblPlotDetails.PlotCode(((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[PhotoRoll] In (SELECT [PhotoRoll] FROM [tblPhotos] As Tmp GROUP BY [PhotoRoll],[PhotoFrame] HAVING Count(*)>1 And [PhotoFrame] = [tblPhotos].[PhotoFrame])Count([PlotCode])>1 And Count([PhotoFrame])>1 <_S o Q  q 3 y  w ;  b  UqST2TZAs GlVtblPlotDetailstblVegetationX@ #SG- lVtblPlotLocationtblPlotDetailsd@ #WK/ lV tblPlotLocation.BPUCode6 glVtblPlotDetails.Surveyors7 glVtblPlotLocation.[UTM Error]: glVtblPlotLocation.AerialPhotoNo< glV!tblVegetation.ProvCommunityName> glVtblPlotLocation.SiteName7 glVtblPlotDetails.PlotID4 glVtblPlotLocation.Waypoint7 glVtblPlotLocation.PlotCode7 gblVtblVegetation+++ blVtblPlotDetails--- blVtblPlotLocation/// lV GlV GblV 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  GtblAADetailstblAAEnvironmentR@#UI) GPS_Data_DownloadtblAADetails^@#WK3 LandformGPS_Data_Download.LandformI! wEnvironmentID tblAAEnvironment.EnvironmentIDW+ wtblAAEnvironment111 tblAADetails))) GPS_Data_Download333  GtblAAEnvironmentDetails??? O  GtblAADetailstblAAEnvironmentR@#UI) GPS_Data_DownloadtblAADetails^@#WK3 ElevSourceElevSource@#E9% ElevationGPS_Data_Download.GPS_HeightM# wTopoPositionGPS_Data_Download.Topo_PositS) wAspectGPS_Data_Download.Aspect_DE wSlopeGPS_Data_Download.Slope_DB w/Y/ N$$&&////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 Y 4Y <Y DY LY TY \ Y  Y   Y  ! Y!! " Y"" # Y## AIDAA_Code 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&KACe&LYYAA_CodePrimaryKeyv1%  g 4  Y $^K@ @@4@??4&k C@OAo@ACEBR_AA.0187Olympus StylusMidslopecliffEvergreenNeedle-leavedSparsely Vegetated No 11:11:52amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsOtherCedar Breaks NMjVF.   ~f$]V@@`4@??4&k Cv5OAVժACEBR_AA.0158 No 11:53:04amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM* ~f$\E@o@ 1@  4&k CZdOAnACEBR_AA.0067Olympus StylusMidsloperavineEvergreenNeedle-leavedWoodland No AA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMiXN@<&~f$[A@q@ 1@  4&k COAhACEBR_AA.0048Olympus StylusHigh SlopecliffEvergreenBroad-leavedDwarf Shrubland No AA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMwf\NJ4  ~f$Z?@c@ 1@  4&k C`,OAACEBR_AA.0045Olympus StylusHigh SlopecliffEvergreenBroad-leavedDwarf Shrubland No AA_POINT.corBrian HeadIron CountyUtBruce CondieOtherCedar Breaks NMtc\NJ4  ~f$YV@@1@  4&k CI OAK7#ACEBR_AA.0019 No AA_POINT.corBrian HeadIron CountyUtBruce Condie Cedar Breaks NM~f$X1@  @ OAQ}ACEBR_AA.0399 AA399WNoGPS III+ Brian HeadIron CountyUtPete Williams Cedar Breaks NM~f$W1@  Ru{OAZd;_LACEBR_AA.0054 AA054WNoGPS III+ Brian HeadIron CountyUtPete Williams Cedar Breaks NM~f$V1@  `—OA#T~ACEBR_AA.0053 AA053WNoGPS III+ Brian HeadIron CountyUtPete Williams Cedar Breaks NM~f$U1@  סOA-|ACEBR_AA.0052 AA052WNoGPS III+ Brian HeadIron CountyUtPete Williams Cedar Breaks NM~f#% -  (=C$g2@r@ @1@  rG@ ~O?7A0OAF}ACEBR_AA.0005Olympus StylusMidslopecanyonEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMo^TFB,~f$f*@`s@@1@  +@ _cD?DOAGaACEBR_AA.0003Olympus StylusMidsloperidgeMixed Evgrn Cld DecdMixedForest YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$e1@q@`ff.@1@ "@ iq0'h?C@r@@4@??4&k COA7AACEBR_AA.0400Olympus StylusMidsloperidgeEvergreenNeedle-leavedWoodlandbinocular plotNo 11:11:52amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMp\L4& ~f$cA@(@@4@??4&k CBOA7A`fACEBR_AA.0397Olympus StylusMidsloperidgeEvergreenNeedle-leavedWoodlandbinocular plotNo 11:11:52amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMp\L4& ~f$bD@q@ 1@  4&k COAoACEBR_AA.0369Olympus StylusHigh SlopecliffHerb - PerennialForbHerbaceous No AA_POINT.corNavajo LakeIron CountyUtBruce CondieOtherCedar Breaks NMjYRD@*~f$aA@@o@`4@??4&k CHzjOAGaDACEBR_AA.0317Olympus StylusMidsloperidgeEvergreenNeedle-leavedForest No 11:18:01amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NM}njT>.~f$`B@ r@ 1@  4&k C'1OAC ACEBR_AA.0314Olympus StylusInterfluvebadlandsEvergreenNeedle-leavedWoodland No AA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$_A@X@`4@??4&k C OA$ACEBR_AA.0247Olympus StylusLow sloperavineEvergreenNeedle-leavedForest No 11:18:01amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NMrnXB2 ~f% V E /$p@Z@`ff@ 1@ wǨ@ g,{B?sh=KOAACEBR_AA.0017Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMrhZV@,, ~f$o@@u@@ 1@ '1ڨ@ KK?\COAףpACEBR_AA.0016Olympus StylusHigh LevelplateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$n@t@@33@ 1@ Mbƨ@ Tqs*9? \OA=ACEBR_AA.0015Olympus StylusMidslopeplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMndVR<((~f$m@v@@ 1@ MbȨ@ ]ݱ&U?|OAL7AeACEBR_AA.0026Olympus StylusMidslopehiloslope;plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjfP<<$$$~f$u@F@@ 1@ ffff@ m2;?9OAGᓢACEBR_AA.0024Olympus StylusHigh LevelplateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppCircularCedar Breaks NMq`VJF0~f$t@I@ @ 1@  r@ *31?sh-"OA(\ACEBR_AA.0023Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMrhZV@,, ~f$s@Y@`ff@ 1@ +Y@ m2K?%EDOA +JACEBR_AA.0021Olympus StylusHigh SlopeplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMrhZV@,, ~f$r@i@@ 1@ jt@ ~S?K OA(\]ACEBR_AA.0020Olympus StylusToe slopeplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppCircularCedar Breaks NMndXT>**~f$q&@r@@ 1@ ʡE@ RT:?fffXOAK7ACEBR_AA.0018Olympus StylusMidslopeplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMndVR<((~f% +u ,_>$A@g@@1@ o @ I?V}xOAo@zACEBR_AA.0040Olympus StylusHigh SlopebreaksEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~mcNJ4  ~f$:@ g@@1@ /$@  W`?`bnOAĠbwACEBR_AA.0038Olympus StylusHigh SlopebreaksEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~mcNJ4  ~f$@0s@@ 1@ )\5@  0=? ף`EOA-֩ACEBR_AA.0037Olympus StylusHigh SlopeplateauHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$@`q@@ 1@ K7IǨ@  W8?rh}OAnHACEBR_AA.0036Olympus StylusHigh Slopeplateau; hillslopeHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM{fbL88   ~f$~@33 @ 1@ #~j@  .V`J?xOAX9H ACEBR_AA.0035Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyoZV@,, ~f$}@p@@ 1@ FȨ@ $D2?OA ףpACEBR_AA.0034Olympus StylusLow slopedrainageHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyoZV@,, ~f$|@@u@@ 1@ 阮@  8KrB?333#OAjṯACEBR_AA.0033Olympus StylusMidslopehillslope;plateauEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMu`\F22 ~f${@.@@33@ 1@ Pn@ E&HR?Zd[OAoACEBR_AA.0032Olympus StylusMidslopehill slopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMngRN8$$   ~f$z&@Q@@ 1@ E}@ MPT?OAQACEBR_AA.0030Olympus StylusHigh Slopehillslope;plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMnjT@@(((~f% Q & UH$2@`h@@`1@  ڨ@ sIvC?E3OA;OACEBR_AA.0056Olympus StylusMidsloperidgeHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMq`VHD.~f$@D@@@1@ K@  fh>&&&~f$@i@@33@ 1@ oJ @  8KrB?I bOAOACEBR_AA.0047Olympus StylusLow slopevalley;hillslopeHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjfP<<$$$~f$@`r@@ 1@  ףp=1@ U+C?MbpNOAQ8ACEBR_AA.0046Olympus StylusHigh SlopehilllslopeHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMukVR<((~f$>@o@@1@ K7 D@  [O?OAO=ACEBR_AA.0043Olympus StylusMidslopemountainMixed Evgrn Cld DecdMixedForest YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMyh^PL6""   ~f$@t@ @ 1@ ٨@ 8fٓ?zOAM⃄ACEBR_AA.0069Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM01:50:04pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMt`P8* ~f$;@i@@4@B@B@ r(Ť@)@ @Xj@?-OOAuACEBR_AA.0068Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM10:35:44amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMt`P8* ~f$.@l@@4@G@G@ +l@ffffff@@d< H?QiOAw3ACEBR_AA.0066Olympus StylusToe slopestream terraceCold-deciduousBroad-leavedWoodland YesGeoXM11:15:15amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|hX@2 ~f$ @r@`ff@`1@ ʡ@ nYk(W?"ٻOAB`PԭACEBR_AA.0065Olympus StylusHigh SloperidgeCold-deciduousBroad-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NM}lbTP:&&~f$@D@@@1@ S@ E&H2?WOAZdIACEBR_AA.0061Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppCircularCedar Breaks NMpfZV@,, ~f$@M@@33@@1@ %@ R\U]1?nOAjACEBR_AA.0060Olympus StylusHigh Levellow ridge, plateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMxn`\F22 ~f$@I@@33@@1@ ">ި@ 3/0?d;OAp=FACEBR_AA.0059Olympus StylusLow levelplateau, basinHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppCircularCedar Breaks NM}lbVR<((~f$"@h@@@1@ li@ 1{vQ?)\"fOAkACEBR_AA.0058Olympus StylusMidslopeslope, plateauHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieOtherCedar Breaks NMohZV@,, ~f%" h Z$@@ q@@`1@ +C@ H[@?X9[OAMhACEBR_AA.0082Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$?@e@@33@`1@ `"[Ȩ@ ZQfC?VOAZd;vACEBR_AA.0081Olympus StylusStep in slopehill slopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM{q\XB.. ~f$2@q@@`1@ /$@ UZ N?WOAvֳACEBR_AA.0079Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$.@`q@@`1@ 9v@ X%C?= s OA5^IACEBR_AA.0078Olympus StylusLow slopeswaleEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$*@m@@@1@ $U@ 6w\&?CeOA5^IACEBR_AA.0076Olympus StylusHigh SlopedrainagewayHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppOtherCedar Breaks NMve^RN8$$   ~f$@ c@@@1@ X9Hڨ@ PۆQ0?sh}OAQACEBR_AA.0075Olympus StylusMidslopeslope, plateauHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMrhZV@,, ~f$=@r@@4@>@>@@333333"@ffffff@J4A?%UOAvACEBR_AA.0073Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM01:09:09pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMt`P8* ~f$<@@q@@33-@4@M@M@m1@ffffff-@ffffff*@Za/d?POA%ACEBR_AA.0071Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM12:19:55pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMt`P8* ~f % ?  e-$?@\@@33@4@@@@@\(*@@333333@RTJ?7A`OA;O (ACEBR_AA.0095Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM02:11:12pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$,@a@`ff@4@A@A@S# @333333@ @mON?jtSWOAˡEހACEBR_AA.0093Olympus StylusLow slopevalley sideEvergreenNeedle-leavedWoodland YesGeoXM02:49:03pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMnZJ2$~f$?@v@`ff@@1@ rhΨ@ u69?OAVACEBR_AA.0092Olympus StylusHigh LevelplateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppCircularCedar Breaks NMq`VJF0~f$@@1@ 1Ҩ@ | E?`BDOA/݀ACEBR_AA.0091Olympus StylusLow levelbasin, plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NM~tfbL88   ~f$ @t@`ff)@`1@ @ uy?NbXpOAQαACEBR_AA.0090Olympus StylusMidslopehill slopeEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~mcNJ4  ~f$$@ p@@`1@ 1Z@ F̱N?MBVOAxACEBR_AA.0088Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$5@0s@@`1@ jtب@ #fF?Z?qOAJ +бACEBR_AA.0087Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$(@s@@`1@  0ݨ@ K8@_@ @4@7@7@v @ffffff@ffffff@ՔdM?-ͷOAI &ACEBR_AA.0113Olympus StylusToe slopecanyonsideEvergreenNeedle-leavedWoodland YesGeoXM10:31:55amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NMlXH0"~f$V@?`ff@4@.@.@sh<>@ffffff@@mrS?A`OADl:ACEBR_AA.0111 YesGeoXM11:09:25amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$V@?@4@(@(@VNl@@333333@d?H2?V-OAtACEBR_AA.0109 YesGeoXM11:35:10amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$;@h@ @4@B@B@~j@ffffff@@)qH? +OAˡEsACEBR_AA.0107Olympus StylusMidslopehillsideEvergreenBroad-leavedWoodland YesGeoXM01:21:41pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM~zdP@(~f$@`e@ @4@4@4@+NF@@ffffff@WY?'1,OAV-2AACEBR_AA.0101Olympus StylusLow slopehill;terraceEvergreenNeedle-leavedWoodland YesGeoXM12:08:38pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMp\L4&~f$@@m@@33@4@@@@@(\B@ffffff@333333@1{vA?Mbp*OAFesACEBR_AA.0099Olympus StylusMidslopecolluvial slopeEvergreenBroad-leavedWoodland YesGeoXM12:58:00pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMr^N6( ~f$@p@@33@@1@ +Ϩ@ A3?$OAˡE:ACEBR_AA.0098Olympus StylusMidslopeknollCold-deciduousBroad-leavedShrub Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppOtherCedar Breaks NMsl`\F22 ~f$@@s@ @@1@  Ԩ@ {8?L7OA!r蓷ACEBR_AA.0097Olympus StylusHigh LevelplateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieOtherCedar Breaks NMp_XJF0~f$V@?1@4@1@1@|?5@%@@b)r?SOA|?ACEBR_AA.0096Olympus Stylus YesGeoXM11:12:04amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NMXG=.*~f%  /5$.@p@@4@9@9@{G!ʣ@333333@333333@kHcCG?\_OAʡE2vACEBR_AA.0125Olympus StylusLow slopehillsideEvergreenNeedle-leavedWoodland YesGeoXM03:35:06pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM~hTD, ~f$=@f@@4@5@5@ʡz@@@-C6Z?x$OAq= הACEBR_AA.0124Olympus StylusMidslopehillEvergreenMixedWoodland YesGeoXM11:51:08amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM}hdN:*~f$?@k@)@4@L@L@vɤ@@ @i:M?}?5iOA ACEBR_AA.0123Olympus StylusMidslopehillEvergreenBroad-leavedWoodland YesGeoXM11:16:07amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMvr\H8 ~f$V@?`ff@4@(@(@NbX@@@V_]5?POA"KACEBR_AA.0121 YesGeoXM12:25:41pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$9@r@@4@;@;@v@ffffff+@@uR?^IlDOA"ĂACEBR_AA.0119Olympus StylusLow slopevalley sideEvergreenNeedle-leavedWoodland YesGeoXM03:23:37pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMnZJ2$~f$:@p@3@@4@x@x@E{@&@&@͐*WY{?L7`OAGaēACEBR_AA.0118Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM12:26:01pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$@?@33 @@4@D@D@-'j@@@Tb.A?Zd;/OA/ACEBR_AA.0115Olympus StylusLow slopewash channel Sparsely Vegetatedthis polygon has no plant communityYesGeoXM11:11:52amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsOtherCedar Breaks NM|dVB82~f$A@i@@4@D@D@V.@ffffff @@9̗7?T{OA~j^{ACEBR_AA.0114Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM04:56:24pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMt`P8* ~fd%( G fx*$@]@`ff@`1@ Q@ 1zn+A?COA(\ACEBR_AA.0137Olympus StylusLow slopehillEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMq`VHD.~f$V@? @4@.@.@x.@ffffff @ @4LmN?!rOA(\RACEBR_AA.0135 YesGeoXM11:59:51amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$(@q@0@@4@D@D@VNz@!@@kHcCW?V-r'OAGzSACEBR_AA.0134Olympus StylusToe slopehillsideEvergreenNeedle-leavedWoodland YesGeoXM01:22:10pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM~hTD, ~f$@i@'@@4@:@:@= ף0(@@@ٓDOAGACEBR_AA.0132Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM12:49:32pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$2@r@&@4@I@I@Pn@-@@yxee?NbOAWuACEBR_AA.0130Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM02:43:07pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$;@u@@4@;@;@ffffr@@@e3F?C >OA tsACEBR_AA.0128Olympus StylusLow slopenarrow valley sideEvergreenNeedle-leavedWoodland YesGeoXM04:03:33pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|hX@2 ~f$<@ t@@4@D@D@^I ߣ@@@pDkL?SOA +~sACEBR_AA.0127Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM02:01:30pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f(%Xw #F$:@t@`ff$@4@4@4@+@333333@333333@u):\?jtOAVEACEBR_AA.0147Olympus StylusLow slopehillEvergreenNeedle-leavedForest YesGeoXM12:36:14pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMvr\H8 ~f$:@`u@@33+@@4@7@7@bX94i@ffffff!@@Btl?T{rOAGzXACEBR_AA.0145Olympus StylusMidslopehillslopeMixed Evgrn Cld DecdMixedForest YesGeoXM02:56:34pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjVF.  ~f$@j@@@4@4@4@S@ffffff@@D6.6D?OAxoACEBR_AA.0144Olympus StylusLow slopedrainageeCold-deciduousBroad-leavedWoodland YesGeoXM04:23:02pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMr^N6( ~f$`ff@`1@ u@ 8ӅXA? " OA;ACEBR_AA.0143Olympus StylusHigh LevelplateauEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$>@@o@@33@@4@?@?@X9ȶʤ@ffffff@333333@rrg&H?p=OAjtACEBR_AA.0141Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM03:43:33pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$A@@t@`ff@@4@A@A@w @$@@MqJ?'1OA( ACEBR_AA.0140Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM02:20:16pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$A@0@ @@4@>@>@Cl'@ffffff@ @/PR`LI?'1OA`Т"ACEBR_AA.0139Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM03:02:42pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$@W@@33@`1@ E@ z?ZOAS~ACEBR_AA.0138Olympus StylusLow slopehillEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMq`VHD.~f%> U t$@o@`ff @4@E@E@jt@ffffff@ffffff@a@?333s(OAbX9"ACEBR_AA.0157Olympus StylusLow levelwash channel/terracesCold-deciduousBroad-leavedWoodland YesGeoXM04:21:13pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsOtherCedar Breaks NMvfN@," ~f$.@`d@@33@@4@5@5@)\u¤@333333@ffffff @ҏS[?HzHOAGa֓ACEBR_AA.0156Olympus StylusLow slopehillslopeEvergreenBroad-leavedWoodland YesGeoXM01:03:34pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~hTD, ~f$@m@@@4@4@4@rhc@333333@333333@V@g@`ff@4@?@?@(֣@@333333@g 2*\?q= DŽOAZd;sACEBR_AA.0153Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM03:01:27pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$>@2@@33@4@9@9@w/9@ffffff@333333@30&F?TOAʡEcACEBR_AA.0151Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM12:59:55pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$@@D@@33@@4@5@5@QԤ@@333333@[~l_?KJOA`ТqACEBR_AA.0150Olympus StylusHigh SlopehillslopeEvergreenNeedle-leavedForest YesGeoXM03:41:15pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~hTD, ~f$A@`v@ @4@7@7@C,p@333333@@H}=?QeOAjACEBR_AA.0149Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM12:55:16pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f$A@u@`ff @4@4@4@A`P@@@[[%X\?DOAd;jACEBR_AA.0148Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM12:14:24pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM|fRB*~f%  )J $@n@ @4@&@&@/ݤ^@ @ffffff@)O?= OANzACEBR_AA.0170Olympus StylusLow levelcreekCold-deciduousBroad-leavedWoodland YesGeoXM12:12:17pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerOtherCedar Breaks NMjVF.  ~f$V@?@4@H@H@h|@ @ffffff@t u?zOAh|ACEBR_AA.0169Olympus StylusLow slopehillEvergreenNeedle-leavedForest YesGeoXM09:23:31amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMvr\H8 ~f$V@?@4@0@0@DlG@ @? 0=?nOAHzACEBR_AA.0168 YesGeoXM10:42:34amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$4@r@@33 @4@@@@ @333333@ nU?"+OAd;OwACEBR_AA.0167Olympus StylusMidslopehillEvergreenNeedle-leavedWoodland YesGeoXM03:21:33pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMxt^J:"~f$@`1@ Cl @ d< X?MbOAnGACEBR_AA.0165Olympus StylusHigh LevelplateauHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$6@i@@4@6@6@QE@@ffffff@@RGN?#/OAvACEBR_AA.0164Olympus StylusLow slopehillEvergreenNeedle-leavedWoodland YesGeoXM10:04:55amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMzv`L<$~f$(@@$@@4@>@>@'1\֤@0@,@$>w?\5=OAYACEBR_AA.0163Olympus StylusLow slopehiillslopeMixed Evgrn Cld DecdMixedForest YesGeoXM12:24:35pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMnZJ2$~f$@p@/@@4@9@9@v_ɤ@%@@(p?|1OA`ТACEBR_AA.0162Olympus StylusLow slopedrainageEvergreenNeedle-leavedForest YesGeoXM01:26:27pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~zdP@(~f$V@?`ff@4@*@*@Rk@@@: vA?ʑOATACEBR_AA.0159 YesGeoXM09:20:19amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f%%F m $5@p@`ff@4@A@A@K7AΤ@@ffffff@y&1L?\uOA#~ACEBR_AA.0183Olympus StylusMidslopehillEvergreenNeedle-leavedWoodland YesGeoXM11:09:25amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMxt^J:"~f$>@`p@@33/@4@E@E@T㥛@333333,@"@pY?hL?OAEs4ACEBR_AA.0181Olympus StylusHigh SlopehillEvergreenNeedle-leavedForest YesGeoXM12:40:40pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMxt^J:"~f$<@c@`ff@4@.@.@l)@@ffffff@vA]PF?/$*OA"yACEBR_AA.0180Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedWoodland YesGeoXM12:33:44pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NMlXH0"~f$B@p@3@4@5@5@I +@2@fffff1@Xۼqr?7A@OAˡEmACEBR_AA.0178Olympus StylusHigh SlopehillEvergreenNeedle-leavedForest YesGeoXM12:13:57pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMxt^J:"~f$@4@>@>@7A`?@333333 @333333@MP?OAR(xACEBR_AA.0176Olympus StylusLow levelterraceEvergreenNeedle-leavedForest YesGeoXM04:43:02pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM|xbN>&~f$<@o@ @4@&@&@\@ffffff@@W>?"۩LOAjtACEBR_AA.0175Olympus StylusLow sloperidgeEvergreenNeedle-leavedForest YesGeoXM03:13:18pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NMxt^J:"~f$?@p@@33%@4@&@&@J +ܣ@ffffff/@ffffff@?{&:?bXy(OAS㓂ACEBR_AA.0173Olympus StylusHigh SloperidgeEvergreenNeedle-leavedWoodland YesGeoXM02:30:46pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NM~zdP@(~f$<@n@@4@C@C@㥛`@ffffff@ @vk I?-,OAuACEBR_AA.0171Olympus StylusMidslopehillEvergreenNeedle-leavedForest YesGeoXM12:58:06pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMtpZF6~fs% ;\$6@@k@@33@4@B@B@K7I@@@*Ŏơ~G?{OAd;ϸACEBR_AA.0194Olympus StylusMidslopehillEvergreenMixedForest YesGeoXM01:52:22pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyd`J6&~f$8@g@@33%@4@4@4@Sc~@@ @*T7C?rhOA+Y͉ACEBR_AA.0193Olympus StylusLow slopehillEvergreenBroad-leavedWoodland YesGeoXM02:24:08pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMxt^J:"~f$5@j@@4@K@K@ d@333333@ffffff@t ;G?/OAQbACEBR_AA.0192Olympus StylusMidslopehillEvergreenMixedForest YesGeoXM02:47:14pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyd`J6&~f$@pp@`ff@4@$@$@S[$@@333333?A#?FݺOAusACEBR_AA.0191Olympus StylusLow levelcanyon bottomCold-deciduousBroad-leavedWoodland YesGeoXM12:46:34pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerOtherCedar Breaks NMzfV>0  ~f$8@@m@@4@:@:@y&1:@ @ffffff@%F?\OA1ACEBR_AA.0189Olympus StylusMidsloperidgeEvergreenNeedle-leavedWoodland YesGeoXM11:02:59amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NMzv`L<$~f$:@@`@@4@6@6@ffff$@@333333@Owx@?jtOAACEBR_AA.0188Olympus StylusHigh SloperidgeEvergreenNeedle-leavedWoodland YesGeoXM10:44:06amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM~zdP@(~f$@o@@33@4@&@&@$@@ffffff@1zn+1?Q>OANbX~ACEBR_AA.0186Olympus StylusLow levelcanyonCold-deciduousBroad-leavedForest YesGeoXM03:53:33pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NM~hTD, ~f$V@?@33@4@$@$@bX9@@@t^c*?Q"OA ACEBR_AA.0185 YesGeoXM02:45:48pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f%(P Dg$@[@@@1@ +Y@ &"dTI?Ga3OAl{cACEBR_AA.0205Olympus StylusHigh LevelplateauHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$6@`q@@4@6@6@Q@ffffff@ffffff@FSwe7?DlWIOAK7ACEBR_AA.0204Olympus StylusMidslopehilllEvergreenNeedle-leavedForest YesGeoXM01:14:58pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMvr\H8 ~f$ @@1@ 7A`%@ Udt@R?`_OA&18ACEBR_AA.0203Olympus StylusMidslopeplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMukVR<((~f$`ff@@1@ "@ QTU?OAl{ACEBR_AA.0201Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyoZV@,, ~f$`ff@@1@ )\µԨ@ &5P?OA$޳ACEBR_AA.0200Olympus StylusHigh Leveldrainage;plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMlhR>>&&&~f$@@j@@@1@ ~j@ 4aO?QOATACEBR_AA.0199Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMvoZV@,, ~f$@`s@@4@&@&@p= ׿@@ffffff@! _B7?n5OAVACEBR_AA.0198Olympus StylusToe slopevalletEvergreenNeedle-leavedForest YesGeoXM10:58:58amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerOtherCedar Breaks NMzv`L<$~f$@q@@4@&@&@NbXy@333333@333333 @t|8c3?KiOA%ACEBR_AA.0197Olympus StylusToe slopevalleyEvergreenNeedle-leavedForest YesGeoXM10:23:28amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerOtherCedar Breaks NMzv`L<$~f% ?T o 3P#$@@e@#@`1@ /̨@  X4m?(zACEBR_AA.0214 YesGeoXM04:34:42pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$@@l@@33"@@1@ +@ E|'fX?X9OAlVACEBR_AA.0213Olympus StylusHigh Slopehillslope;plateauMixed Evgrn Cld DecdMixedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjfP<<$$$~f$8@B@`ff@4@6@6@SP@ @333333@%IDW?V=wOAyACEBR_AA.0211Olympus StylusMidslopehillslopeEvergreenNeedle-leavedForest YesGeoXM03:22:07pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~zdP@(~f$"@0@@33@4@&@&@Q8@ffffff@ @.H? OAh wACEBR_AA.0209Olympus StylusHigh Slopecanyon sideEvergreenNeedle-leavedWoodland YesGeoXM10:43:11amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtLiz BallengerCircularCedar Breaks NMp\L4&~f$@33 @@1@ t@ oӟHI?C,GOA$ACEBR_AA.0206Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMyoZV@,, ~f%@  "k$`ff@@1@ Zd;@ &OYMc?M>OAX9HACEBR_AA.0228Olympus StylusHigh LevelplateauEvergreenBroad-leavedShrub Herbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM}s^ZD00~f$@l@"@`1@ -'@ HPsR?"OAxACEBR_AA.0227Olympus StylusHigh SlopeplateauEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMoePL6""   ~f$? e@`ff@@1@ Dl统@ صݒ@F@@33@`4@&@&@h|?m@ffffff @333333@:8؛H?I OA?5^VACEBR_AA.0250Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedForest YesGeoXM02:16:30pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NMjTD, ~f$ >@pu@ @`4@6@6@`"(@@!@a`?`OAL~ACEBR_AA.0249Olympus StylusHigh SloperidgeEvergreenNeedle-leavedForest YesGeoXM03:27:05pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NM|xbL<$~f$ >@u@@33@`4@&@&@ףp=ʦ@ffffff@ffffff @5z5@iq? ף0kOAjtACEBR_AA.0246Olympus StylusToe sloperavineEvergreenNeedle-leavedForest YesGeoXM03:27:08pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NM|xbL<$~f$ 9@C@@33@`4@(@(@/G@@@K8@p@@33@`1@ Q^@ óE?z~#OA`" ACEBR_AA.0242Olympus StylusHigh SlopecliffCold-deciduousBroad-leavedDwarf Shrubland YesGeoXMAA_POINT.corBrian HeadIron CountyUtBruce CondieCircularCedar Breaks NMzpb^H44  ~f$ V@?@4@3@3@(@333333@ffffff??6?B`bOAJ9ACEBR_AA.0241 YesGeoXM01:37:56pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$ `ff@@1@ Zd@ y7D? +'4OAvACEBR_AA.0240Olympus StylusHigh Leveldrainage;plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMlhR>>&&&~f %%J w *$ @Pv@@@1@ ףp=J@ t>9?pOATACEBR_AA.0258Olympus StylusMidslopecanyyon sideEvergreenNeedle-leavedForest YesGeoXM02:00:13pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NMlVF.  ~f$ @8@@`4@*@*@GA@@@$xCE?OAT㥛OACEBR_AA.0257Olympus StylusLow slopecanyonEvergreenNeedle-leavedForest YesGeoXM04:24:39pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NM|xbL<$~f$ 8@B@@33 @`4@(@(@wo@@@N ^5?= ׃+OATACEBR_AA.0256Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedForest YesGeoXM01:50:00pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NMjTD, ~f$ @@C@@4@*@*@L7A@@333333@8CY?*OAPn~ACEBR_AA.0254Olympus StylusMidslopehillEvergreenNeedle-leavedForest YesGeoXM04:07:07pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NMtpZF6~f$ $@9@@33 @`4@*@*@nn@@@'4?aOA~ACEBR_AA.0252Olympus StylusHigh SloperidgeEvergreenNeedle-leavedForest YesGeoXM02:42:22pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NM|xbL<$~f$ .@$@@`4@$@$@$d@@@#-#6?fffOAKACEBR_AA.0251Olympus StylusHigh SloperidgeEvergreenNeedle-leavedForest YesGeoXM03:04:10pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NM|xbL<$~f}%/ : Q l}$ >@g@@33@4@.@.@x愤@@@Xj@?~OAVACEBR_AA.0274Olympus StylusMidslopehillEvergreenNeedle-leavedWooded Shrubland YesGeoXM10:56:18amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickOtherCedar Breaks NMnZJ2$~f$ @`4@8@8@ˡEsţ@333333@333333@NwxF?COAjACEBR_AA.0273Olympus StylusLow levelterrace;drainageCold-deciduousBroad-leavedWoodland YesGeoXM04:32:58pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerOtherCedar Breaks NMl\D6"~f$ @s@@4@2@2@J +Gۣ@!@@_% d?HzDOAl{AsACEBR_AA.0271Olympus StylusStep in slopehillslopeEvergreenNeedle-leavedForest YesGeoXM12:42:25pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMnZJ2$~f$ <@t@@33@4@*@*@wo@@333333@VF?8? OA rACEBR_AA.0268Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedWoodland YesGeoXM11:42:19amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NMlXH0"~f$ 6@j@@4@C@C@7A`@333333@@6pd?T㥋OAoirACEBR_AA.0267Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXM02:18:15pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~hTD, ~f$ V@?@33@4@(@(@x&V@ @ffffff@Nwx6?Zd;OAfff?ACEBR_AA.0266 YesGeoXM03:10:16pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$ A@g@ @4@&@&@n@ffffff@ffffff@DXP8?333(OA"ACEBR_AA.0265Olympus Stylus YesGeoXM01:00:38pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickOtherCedar Breaks NMSB;.*~f$ @u@ @@1@ q= 㵨@ ǜgK6N?!r(OARACEBR_AA.0263Olympus StylusMidslopehillslope;plateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjfP<<$$$~f%* 5 $( @@`ff@4@*@*@K-@333333@@\4 o?WOAˡE6}ACEBR_AA.0284Olympus StylusLow slopecanyonMixed Evgrn Cld DecdBroad-leavedForest YesGeoXM03:11:59pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NMt`P8* ~f$' V@?`ff@4@&@&@/$F1@ @@מY2?5^OAw|ACEBR_AA.0283 YesGeoXM03:49:13pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy Tendick Cedar Breaks NM4#!~f$& <@ t@`ff@4@&@&@+َL@333333@ffffff@k$ 5?R5OA|~ACEBR_AA.0282Olympus StylusMidslopehillEvergreenNeedle-leavedWoodland YesGeoXM03:33:22pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NMxt^J:"~f$% 6@@e@0@`1@ 㥛 ܨ@ D0  ~f$, >@pp@`ff @`4@&@&@K7I@@@c#7?P^OAX9ÅACEBR_AA.0289Olympus StylusHigh SloperidgeEvergreenNeedle-leavedForest YesGeoXM11:18:01amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NM|xbL<$~f$+ 5@k@`ff@4@5@5@ ףpW@333333@@VSbR?7AOACtwACEBR_AA.0287Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXM01:43:59pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NM~hTD, ~f$* &@@@33@4@,@,@jt.@@333333 @&:,BU?K7OAV-B}ACEBR_AA.0286Olympus StylusLow slopecanyonEvergreenNeedle-leavedWoodland YesGeoXM02:38:52pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickCircularCedar Breaks NM~zdP@(~f$) @E@@4@&@&@Gzw@ffffff@@MP4?%OA-zACEBR_AA.0285Olympus StylusHigh LevelridgeEvergreenNeedle-leavedWooded Shrubland YesGeoXM01:34:24pmUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtAmy TendickOtherCedar Breaks NMt`P8* ~f%, I Xq$8 ?@K@@33@4@(@(@ޤ@@@8fٓ@@j@@`4@9@9@B`@@ffffff@_F??5^ZOAMuACEBR_AA.0298Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM02:53:17pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NMv`P8* ~f$3 >@ q@@`4@D@D@/$פ@333333@@_vj.7H?1:OA,ACEBR_AA.0297Olympus StylusMidslopehillsideEvergreenNeedle-leavedWoodland YesGeoXM03:26:25pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NM~hRB*~f$2 4@s@`ff @`4@9@9@(@ffffff@@k$ E?;O-OAWACEBR_AA.0296Olympus StylusLow slopehillsideEvergreenNeedle-leavedWoodland YesGeoXM01:44:06pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NMjTD, ~f$1 @@l@`ff@`4@=@=@ +@@333333@ fh@ q@@33(@`4@@w@@w@(@333333#@"@aE| v?V-OA+ٖACEBR_AA.0312Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedWoodland YesGeoXM12:33:31pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NMv`P8* ~f$> 9@o@@`4@D@D@ffff@@ffffff@'eRC;? +OAjt!ACEBR_AA.0311Olympus StylusMidsloperidge sideEvergreenNeedle-leavedWoodland YesGeoXM11:28:59amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NMlVF.  ~f$= V@?@`4@&@&@NbXs@@333333 @Xj@?'1L0OAV-ACEBR_AA.0310 YesGeoXM03:54:17pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy Tendick Cedar Breaks NM6%#~f$< $@t@@33@`4@4@4@ףp=J;@@333333@P?u4OA^IACEBR_AA.0309Olympus StylusMidslopehillslopeMixed Evgrn Cld DecdMixedForest YesGeoXM01:20:02pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtStephanie ShoemakerCircularCedar Breaks NMlVF.  ~f$; 2@t@@33+@`4@;@;@%@&@@XWj1xh?(\.OAPnACEBR_AA.0308Olympus StylusMidslopehillslopeEvergreenNeedle-leavedForest YesGeoXM02:28:21pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtStephanie ShoemakerCircularCedar Breaks NM|fP@(~f$: :@2@@`4@5@5@ rh@ffffff@333333@&|g?jtOAqACEBR_AA.0307Olympus StylusHigh SlopehillslopeEvergreenNeedle-leavedForest YesGeoXM01:53:55pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjTD, ~f$9 2@Q@.@4@?@?@`"[$@ @@.c}k?I eOAB`wrACEBR_AA.0304Olympus StylusMidslopehillslopeEvergreenNeedle-leavedWoodland YesGeoXM12:23:17pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtStephanie ShoemakerCircularCedar Breaks NMjTD, ~fv%u /{$H =@@@`4@0@0@(\إ@ffffff@ffffff@Iطc?$OA"ACEBR_AA.0327Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedWoodland YesGeoXM12:35:15pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NMnXH0"~f$G @M@@`1@ Kv@ PۆQ0?R%OAA`eACEBR_AA.0326Olympus StylusMidslopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NM}lbVR<&&~f$F @[@@`1@ Vm@ HSȕz6?ٮOA333YACEBR_AA.0325Olympus StylusMidslopevalley sideEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NM{j`RN8""   ~f$E A@@q@@33@`4@P@P@X96-@ffffff@ffffff@@mX?mwOA{GێACEBR_AA.0324Olympus StylusMidslopecolluvial slopeEvergreenNeedle-leavedSparsely Vegetated YesGeoXM12:57:35pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtPete WilliamsCircularCedar Breaks NMtdL>* ~f$D 5@t@@33@4@.@.@ηޤ@ffffff@ffffff@d7iJ?jOAbX9 zACEBR_AA.0321Olympus StylusMidslopecanyon sideCold-deciduousBroad-leavedForest YesGeoXM11:30:16amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NMr\L4&~f$C 2@e@ @`1@ fffff@ m2;?vOA ףpACEBR_AA.0320Olympus StylusLow sloperidgeMixed Evgrn Cld Decd Forest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NMm\RFB,~f$B 2@@i@@33@`1@ /$@ @fg;e?+IOATȱACEBR_AA.0319Olympus StylusLow sloperidgeMixed Evgrn Cld Decd Forest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMo^TFB,~f$A @@@r@`ff"@`4@&@&@v_Ȥ@ffffff$@333333!@}EJ?POARACEBR_AA.0316Olympus StylusMidslopecanyon sideEvergreenNeedle-leavedForest YesGeoXM12:41:50pmUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtLiz BallengerCircularCedar Breaks NMjTD, ~fI% b <i$Q @c@@33@`1@ zZ@ :`4?OAQaACEBR_AA.0350Olympus StylusMidslopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NM}lbVR<&&~f$P @_@ @`1@ v3@ GR{Q?eOA ףpACEBR_AA.0349Olympus StylusLow slopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMpfXT>((~f$O @@_@ @`1@ 7A`%E@ RG?333COA+©ACEBR_AA.0348Olympus StylusMidslopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NM}lbVR<&&~f$N @@e@@`1@ G@@ ܂I?OAʡEACEBR_AA.0346Olympus StylusMidslopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieOtherCedar Breaks NM|kdVR<&&~f$M @d@@`1@ jt3@ {gUId??9FtOAz.0ACEBR_AA.0345Olympus StylusLow slopevalley sideHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NMndXT>((~f$L @g@ @`1@ J +<@ ZQf3?O7OAbX9ACEBR_AA.0344Olympus StylusMidslopevalley sideHerb - Perennial Herbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMyh^PL6  ~f$K (@p@@@1@ C,@ sIv3?/"OAx饧ACEBR_AA.0343Olympus StylusHigh SloperimCold-deciduousBroad-leavedDwarf Shrubland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMxn`\F00~f$J @^@`ff@`1@ Rkh@ O'3?o4OAACEBR_AA.0331Olympus StylusLow levelswaleCold-deciduousBroad-leavedShrubland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieOtherCedar Breaks NM|kdVR<&&~f$I @@D@@33@`4@*@*@ʡE4@@ffffff@Tqs*9?xOA= #ACEBR_AA.0328Olympus StylusHigh Slopecanyon sideEvergreenNeedle-leavedWoodland YesGeoXM11:53:04amUpdatedAA_POINT.corAA_PointNavajo LakeIron CountyUtAmy TendickCircularCedar Breaks NMr\L4&~f% J T R$Z 8@k@&@@1@ d;OMB@ )u?bXOA1{ACEBR_AA.0363Olympus StylusHigh SloperimEvergreenMicrophyllousWoodland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$Y 3@r@1@ 1@ h|@ p'vu?~jOAўACEBR_AA.0362Olympus StylusMidsloperidgeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$X (@u@@@1@ E@ IVO?/OA}?5PACEBR_AA.0360Olympus StylusLow slopevalleyEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$W &@s@@33 @@1@ zǀ@ {GzD?hOAB`_ACEBR_AA.0359Olympus StylusHigh SlopeknollEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMwf\NJ4~f$V 9@@t@@33@ 1@ (\@ !'*K?uOA/$ՇACEBR_AA.0358Olympus StylusMidsloperidgeEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$U *@n@@ 1@ !@ "ACEBR_AA.0375Olympus StylusHigh SlopevalleyHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMrhZV@**~f$` @c@@`1@ Hz'@ &5@?/mOArhACEBR_AA.0373Olympus StylusLow slopevalley, plateauHerb - Perennial Herbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtSarah ToppCircularCedar Breaks NMpfZV@**~f$_ @Y@@`1@ ηU@ fLg1?MtOAvACEBR_AA.0372Olympus StylusHigh Slopevalley sideHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NM|rd`J44  ~f$^ "@h@`ff@ 1@ "yO@ W>?xvOAHzEACEBR_AA.0371Olympus StylusMidslopeswaleHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NM}lbTP:$$   ~f$] @s@@@1@ Gz~@ Q+2?TKOAiACEBR_AA.0368Olympus StylusHigh LevelrimHerb - PerennialForbHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMsbXJF0~f$\ @@p@`ff@ 1@ x&17@ )[$F_?}?5OA ACEBR_AA.0365Olympus StylusLow slopegorgeEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMq`VHD.~f$[ 4@g@`ff@ 1@ lħ@  XrD?7OANbІACEBR_AA.0364Olympus StylusMidsloperidgeEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMo^TFB,~ft% H $ hL$l @@q@@@1@ %@ +4?rh:OA$ACEBR_AA.0387Olympus StylusHigh SlopeswaleHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMpfXT>((~f$k "@`e@`ff@@1@ Ө@ 'eRCK?B`zOA)\wACEBR_AA.0386Olympus StylusMidslopehillHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NM{j`RN8""   ~f$j @`i@?@1@ L7A@ g,{2?Zd{;OAm,ACEBR_AA.0385Olympus StylusLow slopeswaleHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMndVR<&&~f$i @ c@?@1@ /$A@ !*?jpOAlACEBR_AA.0384Olympus StylusLow slopehillHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NM}lbTP:$$   ~f$h @d@@@1@ Y@ 1{vA? ף`IOAbXACEBR_AA.0382Olympus StylusHigh LevelplateauHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMtj\XB,, ~f$g $@c@@@1@  rh@ IӠh.?9OA\ACEBR_AA.0381Olympus StylusHigh SlopehillHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMndVR<&&~f$f (@c@@@1@ {Gᥨ@ iUMu/?ʡOA-ACEBR_AA.0380Olympus StylusHigh SlopehillHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMndVR<&&~f$e @?@ 1@ Zd{0@ 3.L?#OA{GjACEBR_AA.0379Olympus StylusLow slopevalleyHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMpfXT>((~f$d @Q@`ff@ 1@ J +@ -H?y&aOAZd;nACEBR_AA.0378Olympus StylusLow levelvalleyHerb - PerennialGraminoidHerbaceous YesGeoXMAA_POINT.corNavajo LakeIron CountyUtBruce CondieCircularCedar Breaks NMpfXT>((~f%V  "g$t 1@q@`ff$@4@8@8@d;OM@ @@ W`?O',OAPnڏACEBR_AA.0398Olympus StylusHigh SloperidgeEvergreenNeedle-leavedWoodland YesGeoXM09:08:32amUpdatedAA_POINT.corAA_PointBrian HeadIron CountyUtPete WilliamsCircularCedar Breaks NM~zdP@(~f$s @@e@@1@ G)@ | L?333CMOAd;zACEBR_AA.0395Olympus StylusMidslopebreaksEvergreenNeedle-leavedWoodland YesGeoXMAA_POINT.corBrian HeadIron CountyUtStephanie ShoemakerCircularCedar Breaks NMzi_JF0~f$r @h@`ff@1@ ˡE3ǧ@ {gUIdO?|?OA- ACEBR_AA.0394Olympus StylusStep in slopeplateau breaksEvergreenNeedle-leavedForest YesGeoXMAA_POINT.corBrian HeadIron CountyUtSarah ToppOtherCedar Breaks NMsl`\F22 ~f$q 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(? )@ *@ +@ ,@ -@ .@ /@ 0@ 1A 2A 3A 4A 5A 6A 7A 8A 9B :B ;B <B =B >B ?B @B AC BC CC DC EC FC GC HC ID JD KD LD MD ND OD PD QD RE SE TE UE VE WE XE YE ZE [F \F ]F ^F _F `F aF bF cF dG eG fG gG hG iG jG kG lG mH nH oH pH qH rH sH tH uI vI wI xI yI zI {I |I }J ~J J J J J J RY%NNN Y Y Y  Y  Y Y eY DateCreateDateUpdateIdLvNameParentIdTypeolPtNVerhoaNWPhtNNaNXeINYMYYMYY.rEId.MSysAccessStorageSTGRELParentIdIdParentIdNameNN6 vh# T  @;M3@ R 3 - H g $ U ERǮ9o,ʛ @ʛ @@ PPROJECT840" ʛ @ʛ @e@PPROJECTwm<84" ʛ @ʛ @@Qdir0,(" ʛ @ʛ @UW _VBA_PROJECTB>:" ʛ @ʛ @SW JZBELIMWUDDIZDLJFLPQJEYAXUULb^Z" ʛ @ʛ @ @QDOPVQYIAFRRSXDGEJEWWLSZODRIGb^Z" ʛ @ʛ @ AcessVBADataNJF. w@w@ZImExSpecs0,( w0Q6@X` 6@<BlobDelta00,( wQ6@X` 6@3PropData0PLH8 Q6@ ` 6@2k@PTypeInfo0:62" Q6@X` 6@1@PBlob02.*" )Q6@k_ 6@01   w$=Xs@$=Xs@DataAccessPages<84 w$=Xs@$=Xs@CustomGroups62. w$=Xs@$=Xs@MSysDbDirDataPLH8 $=Xs@$=Xs@Blob&" w$=Xs@$=Xs@0  w$=Xs@$=Xs@Databases0,( w$=Xs@x@jiPropDataPLH8 $=Xs@$=Xs@Scripts,($ w$=Xs@$=Xs@Reports,($ w$=Xs@$=Xs@Modules,($ w$=Xs@$=Xs@Cmdbars,($ w$=Xs@Q6@ 0CB0 1CB0PropData TPL< $=Xs@Q6@:frmCalc frm_Import_GPSDirData tpl\ $=Xs@$=Xs@0dhdhBlobDelta lhdR $=Xs@$=Xs@T@PTypeInfo :62" $=Xs@$=Xs@ PropData GC?/ $=Xs@$=Xs@@PBlob 2.*" $=Xs@$=Xs@ 0   w$=Xs@Q6@ Forms($  w$=Xs@ʛ @VBA$  w$=Xs@ʛ @VBAProject2.* w$=Xs@ʛ @VBA$  wPa)b*e gh6iXj.k ?l41L@x !l,^3;M3nvBy  U @ Ariald2" @ Tahomahg#h%" @ Tahoma`,  Detailx ez˭V~Hƶ?Ld5U`6ab@ c,d#e%  Label0 Import GPS Datax "SsD"@50N!h1U`6 ac, ButtonImport Import GPS Data~ "[Event Procedure]x DK@tߨh1U`6 a0 b c,i ButtonClose Close Form~ "[Event Procedure]x b*zG*yYgͬ\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. OJSh ared\\dao360.dllR 3.6PO~OWC10~OWC1*0.-.E55N1~*Office\12\OFF.DLL,C XP Web @ponen|ts"C|C|ODf@icB| [2DF8D04C-5BFA-101B-BHDE5442GH|[@.ICE0MSO/10.0]"}­Form_frmCalcG  FXrmF_CaZcDOPVQYIAFRRSXDGEJEWWLSZODRIG28!OPVQY"IQFR SX{GEJ`W=LSZ`"DIG H  A(,~6""(+`%_Import_GPSG& _mpUtGSJZBELIMWUDDIZDLJFLPQJEYAXUULJB@LMUD`ZLFL QYXU Lkw8}~6xME PS<S<S<<<<<<Xe"dN0{665C8786-8C62-4B39-81C2-0E7EA419F7C0} + Xe\ % xC.%`$`&1`(0[xB`*b9K%- "  (08@  H"X   4 \Xp     " 0 @H P"X xh]@]`]]]] ,.hartblEnvironment %.. LL B@0'( !2a '$% Set Fields Index to thirteenth field'& $ a% $ %6$4 $ %6t $ %6(t) $ $ %6'* & * '&kx $ '$` B@8 & ): B@< ( '( B@> B@BA ( 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#5B LVAL0* pHd CARE_Plo@ts_be@T@ = +x grH J< ADODB> 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. OJSh ared\\dao360.dllR 3.6PO~OWC10~OWC1*0.-.E55N1~*Office\12\OFF.DLL,C XP Web @ponen|ts"C|C|ODf@icB| [2DF8D04C-5BFA-101B-BHDE5442GH|[@.ICE0MSO/10.0]"}­Form_frmCalcG  FXrmF_CaZcVIKWRHJBFSDKLTHSVGIFANIVH28!IK9ByERHJBFS KLT SVGFUNV` @ A@,~6"(J+`%_Import_G`PSG& _QmptG PRAQYBD_BGDVCPDRFDBIBJOMDOLCMER@QY@DU`BDC`DUFB BOMO@C kw8}~6xME PS<S<S<<<<<<Xl"aN0{665C8786-8C62-4B39-81C2-0E7EA419F7C0} + X % x%`$ts`&`(8`*pl%- "  (08@  H"X   4 \Xp     " 0 @H P"X xh]@]`]]]] ,.hartblEnvironment %.. LL B@0tsi'( !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#5BLVALW TT(]}kwxME 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.Vield=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.pe#The user pressed the action button._3"5ppe l5rpeIvrtSelectedItem 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.$,.mk f !x!z R f %x.b> b!*Errors*"Import errors - check error table.A@@4&k fvkiQ^ DoCmd.SetWarnings FalseqryClearGPSDownLoad BB@|OJ BB@~MQkkqryAppGPSImport BB@| DoCmd.OpenQuery "GPS_Append_1"e DoCmd.OpenQuery "GPS_Append_2"`k DoCmd.OpenQuery "GPS_Append_3"Q DoCmd.OpenQuery "GPS_Append_4"m DoCmd.OpenQuery "GPS_Append_5"i` DoCmd.OpenQuery "GPS_Append_6"|R F!HA@@&poh(X BB@B@ʣ@|80 F!HA@@io LVAL" ǵAttribute VB_Name = "Form_fImport_GPS" " Bas0{8FFAD4A9-EDBB-4CC4-92B5-944DBF84 E12B} |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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88<4!88>4"88@4@#88F4@$88H4%8:84&8:<4'8:>4(8:@4)8:D4*8:F4+8<64,8<:4@-8<<4@.8<>4@/8<@40864@48>84@58><1`68>>4@78>@4@8>D48>F48>H48@64@8@848@<48@>4@8@@4@8@B4@8@D48@F4` 8@H4 8B848B:4@ 8B<4@ 8B>4 8B@1` 8BD48BF48BH48D648D848D<48D@48DB48DD48DF48F648F848F<48F@48FB48FD4@ 8FF48FH48H848H:48H<4 8H>4!8HD4"8HF4#8HH1@$:661@%:681@&:6<1@':6>4(:6@1@):6B1@*:6D4:6H4+:884,:8<1@-:8>4.:8@4/:8D1`0:8F1`1:8H1`2::643::844:::1@5::<1@::@4::B1@::D1`::F1@::H1@:<81@:<:4:<<4:<@4 :61@ :>84:>:1`:><4:>>1@:>@4`:>B4`:>D4` :>H4`:@64`:@84`:@:4`:@>4:@B4`:@D4`:@F4`:B64`:B:1@:B<1@:B@4:BB4                                                   MQLi+JJ666:166<166@166B166D166H1686168:168>1 68@1 68B1 68D1 68F1 6:61 6:81 6::1 6:<1 6:>1 !6:B1 "6:D1 #6:F1 $6:H1 %6<61 &6<:1 '6<<1 (6<>1 )6<@1 *661.6>81/6>:1 06><116>@1 6>B1 26>D1 36>F1 6>H1 46@61`56@:16@<16@>16@@1@66@B1`6@F1@6@H1@6B61@6B81@6B@1`6BB46BD1 6BF46BH46D846D<4 6D@1@ 6DB1@ 6DF1` 6DH1` 6F81`6F:1`6F<1`6F>1`6FD1`6FF1`6H61`6H81@6H:1@6H<46H@46HB46HD1@6HF1@6HH4868486>486D486H488648884 88<4!88>4"88@4@#88F4@$88H4%8:84&8:<4'8:>4(8:@4)8:D4*8:F4+8<64,8<:4@-8<<4@.8<>4@/8<@40864@48>84@58><1`68>>4@78>@4@8>D48>F48>H48@64@8@848@<48@>4@8@@4@8@B4@8@D48@F4` 8@H4 8B848B:4@ 8B<4@ 8B>4 8B@1` 8BD48BF48BH48D648D848D<48D@48DB48DD48DF48F648F848F<48F@48FB48FD4@ 8FF48FH48H848H:48H<4 8H>4!8HD4"8HF4#8HH1@$:661@%:681@&:6<1@':6>4(:6@1@):6B1@*:6D4:6H4+:884,:8<1@-:8>4.:8@4/:8D1`0:8F1`1:8H1`2::643::844:::1@5::<1@::@4::B1@::D1`::F1@::H1@:<81@:<:4:<<4:<@4 :61@ :>84:>:1`:><4:>>1@:>@4`:>B4`:>D4` :>H4`:@64`:@84`:@:4`:@>4:@B4`:@D4`:@F4`:B64`:B:1@:B<1@:B@4:BB4 u @ @ @ @ @ @ @ @ @ @ @ @ @MQLi+JJ6:BD4!MQLi+JJ6:BF4"MQLi+JJ6:D84#MQLi+JJ6:D<4`$MQLi+JJ6:D>4%MQLi+JJ6:D@4&MQLi+JJ6:DB4`'MQLi+JJ6:DD4`(MQLi+JJ6:DH1`)MQLi+JJ6:F81`*MQLi+JJ6:F:4+MQLi+JJ6:F<4,MQLi+JJ6:F>4-MQLi+JJ6:F@4.MQLi+JJ6:FB4/MQLi+JJ6:FD40MQLi+JJ6:FH4`1MQLi+JJ6:H64`2MQLi+JJ6:H843MQLi+JJ6:H:44MQLi+JJ6:H>45MQLi+JJ6:H@4`6MQLi+JJ6:HB4`MQLi+JJ6:HD4`MQLi+JJ6:HF4`MQLi+JJ6:HH4MQLi+JJ6<684`MQLi+JJ6<6:4MQLi+JJ6<6<4MQLi+JJ6<6>4MQLi+JJ6<6D4`MQLi+JJ6<6F4` MQLi+JJ6<6H4` MQLi+JJ6<864` MQLi+JJ6<884` MQLi+JJ6<8:4` MQLi+JJ6<8>1 MQLi+JJ6<8@4`MQLi+JJ6<8B4`MQLi+JJ6<8D4` MQLi+JJ6<8H1`MQLi+JJ6<:61`MQLi+JJ6<:84MQLi+JJ6<:<4`MQLi+JJ6<:>4`MQLi+JJ6<:@1`MQLi+JJ6<:B1`MQLi+JJ6<:D4`MQLi+JJ6<:F4`MQLi+JJ6<<64`MQLi+JJ6<<81`MQLi+JJ6<<:4`MQLi+JJ6<><1@MQLi+JJ6<>>1`MQLi+JJ6<>@1`MQLi+JJ6<>B1`MQLi+JJ6<>F1`MQLi+JJ6<>H1`MQLi+JJ6<@61`MQLi+JJ6<@81` MQLi+JJ6<@>1 !MQLi+JJ6<@@1@"MQLi+JJ6<@B1 #MQLi+JJ6<@F1 $MQLi+JJ6<@H1@%MQLi+JJ61 )MQLi+JJ61@7MQLi+JJ61MQLi+JJ6664@MQLi+JJ6>684 MQLi+JJ6>6>4 MQLi+JJ6>6@4 MQLi+JJ6>6B4MQLi+JJ6>6F4y @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @       ! "!#"$#%$&%'&(')(*)+*,+-,.-/.0/10213243546576879:;<=>@ABC D E F G HIJKLMNOPQRSTUVWXYZ [!\"]#^$_%`&a'b(c)d*e+f,g-h.i/j0k1l2m3n4o5p6qrstuvwxyz { | } ~  !"#$%&'()*+,-./012345      !"#$%&'()*+,-./0123456      !"#$%&'()* + , - . /01234567  ! " # $%&'()*+,-./0y @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @ @       ! "!#"$#%$&%'&(')(*)+*,+-,.-/.0/10213243546576879:;<=>@ABC D E F G HIJKLMNOPQRSTUVWXYZ [!\"]#^$_%`&a'b(c)d*e+f,g-h.i/j0k1l2m3n4o5p6qrstuvwxyz { | } ~  !"#$%&'()*+,-./012345      !"#$%&'()*+,-./0123456      !"#$%&'()* + , - . /01234567  ! " # $%&'()*+,-./0O Y/0N//////Y Y  Y d Y d Y dY  Y d Y  Y  Y    Y    Y    Y   Y   Y   Y   Y   Y  Y  Y  Y  Y  Y  Y  Y  Y EnvironmentIDAAID Slope AspectTopoPositionElevationElevSource*EnvironmentalCommentsGeologyBareSoilBedrockSandMoss OtherOtherPctDesc Litter Rocks Lichen GravelLiveVegLitterLiveVegWoodWoodLichenRocksLichenGround"DarkCyanobacteria WatervrnCCaaoeebHoSCPtYYYYY.rEL{1F99A0EE-346B-4DD3-9A47-C9D4CDA58DBF}EnvironmentID PlotIDPrimaryKeyv1b@ ֶm-)I$LVALX : X JHuge amount of dead PICENG from beetle outbreak, many trees standing and lying dead. Many live trees have broken tops or are leaning.This area alternates openings with clumps of trees. Several dead spruce are in the plot and there are plenty of logs on the ground.Site funnels snowmelt from below road to edge of breaks, creating a meadow condition which is xeric overall.This point is in a gently sloping meadow below a low ridge of volcanic gravels. The gravels are exposed at the soil surface in the upper (N) end of the plot, but most of the plot has developed soil at the surface. A shallow gravelly gully runs through plot. Burrowing evident.Talus/colluvium derived from Pink Claron. Entire plot is subject to surface runoff during flash flood conditions.Talus/colluvium derived from the Pink Claron.Colluvium is derived from Pink Claron. Plot is transected by steep, shallow gullies; surface gets rinsed in flash flood events.Bedrock and source of talus is Pink Claron.Plot is located on what is both a high terraces of the main Adams Canyon drainage and the outwash area of a steep gully descending the colluvial slopes to the east of the drainage. This gully has recently flash flooded, dumping lots of mud and rock into the plot.This area alternates between small forb meadows and dense trees.Plot is on the gentle slope above a basin, and is also a meadow. Vegetation is dense, sod-forming. Tunnels and piles of bare soil bear witness to underground burrowing activity.This point fell on a low ridge overlooking two meadows. The ridge summit consists of gravelly volcanic tuff, and soil becomes more fine sediment away from the summit.Plot is in a low-lying meadow which has filled in with sediment. Some gravelly rocks are on soil surface.Plot is on a slope of ashflow tuff above a low-lying meadow. Soil surface is covered with volcanic gravel and scattered larger rocks. Aspen seedlings and clumps of Ribes are coming in from nearby forested clumps.G`| A 3 ;PKc 14140Low slopeGPS@ alluviumP0000061-a00200P0000db`^\ZXVRPKGGECA?=3'"g 1356High LevelGPS@Brian Head Formation0300000700T0000000ljhfdb`^\ZXTTRPNLH2&!i 0n/aLow levelGPS@Brian Head Formation1-b0000080000000000ljhfdb`^\ZXTTRPNLG1% r 8335MidslopeGPS@Brian Head FormationT00000800000020000jhfdb^\ZXVTPPNLJHF0$W 10258MidslopeGPSD@Brian Head Formation000000800000020000ljhfd`^\ZXVRRPNLJH2&!l 21307MidslopeGPS@Brian Head FormationT000008001-a001-b0000pnljhca_ZXVRRPNLJH2&!o 12312MidslopeGPSl@Brian Head FormationT00000800000020000ljhfd`^\ZXVRRPNLJH2&!M 3350Step in slopeGPSV@Brian Head FormationT0001-awater08000001-b0000zxvtrmkigec_XSQOMK5)$" 32274MidslopeGPS@Claron Formation, White MemberT1-a00008001-a001-b0000}{ywupnlgec__][YTR2&!d 1170Step in slopeGPS@Brian Head Formation000000800000020000omkigca_][YUUSQOMK5)$ 18285MidslopeGPS @ Brian Head Formation1-b00000700000020000omkigca_][YUUSQOMH2&! ] 15278Low slopeGPS@ Brian Head FormationP000009T0T00P0000kigeca_][YWSSQOMKI3'" ] 13236High SlopeGPS@ Brian Head Formation02000006P01-a00P0000qomkigec^\ZVVTRPNJ4(# m 6153MidslopeGPS(@ Brian Head Formation02000006T01-b0000000mkigeca_ZXVRRPNLJF0$ u 29302MidslopeGPS@ talus/ colluvium/ landslide1-a0000020400300P0000xvtrpnljfd`\\ZXVTO2&! H 28276MidslopeGPSZ@talus/ colluvium/ landslide020000020300300P0000wusqomkiec_[[YWUSO2&!3 32288MidslopeGPS@talus/ colluvium/ landslide1-a0000030300300P0000xvtrpnljfd`\\ZXVTO2&!c 27206MidslopeGPSV@talus/ colluvium/ landslide1-a020000203002001-a0000}{ywupnlhfb^^\ZXTO2&!6 15230Toe slopeGPS@alluvium070000P1-b01-b00T0000eca_][YWRPKIIGECA=3'"` 8289High SlopeGPS@Brian Head FormationP00000800000P0000jhfdb`^\ZXVRRPNLJH2&!t 340High LevelGPSb@Brian Head Formation02000007T0P00P0000kigeca_][YWSSQOMKG1% s 258High LevelGPSL@Isom Formation020000041-a0040000000jhfdb`^\XVQMMKIGEA1% o 250Low levelGPS@Brian Head Formation04000005T01-a0000000mkigeca_ZXVRRPNLJF0$v 9196MidslopeGPS@Isom Formation1-a0000021-a00600P0000jhfdb`^\XVQMMKIGE@0$LVAL < J \tlGravels of substrate are derived from Pink Claron and have probably arrived here as much from water as gravity.Point is in a dry meadow. A shallow swale runs through plot and has most of the Deschampsia. Soil is free of rocks. Underground animal tunneling evident on soil surface. Veg and litter cover most of soil surface.This point is in a low-lying meadow, in an area with a high water table. Edges of the point are slightly higher with a mix of drier-site species. Majority of plot is a thick carpet of Carex with some Juncus patches. Elk or deer bedding sites are found here.This point's centroid is directly on the Alpine Pond Trail. There are many broken top trees, dead standing PICENG and downed logs and stumps. Ground is covered with forbs and litter, very little soil exposed.This forest has many standing dead and down PICENG from the spruce beetle outbreak. The herbaceous and shrub layer are very thick and there are many young PICENGMost of the canopy PICENG has been killed in the spruce beetle outbreak. PICENG returning in subcanopy and many seedlings of both species. ABILAS seedlings forming circle around canopy trees.Many standing dead PICENG from beetle outbreak. Ground difficult to walk through from so many dead lying trees. Trees have broken tops or are leaning. Herbaceous layer very thick.This point is very boggy with standing water with associated mesic species. Most of PICENG canopy is dead from the beetle outbreak, and many dead trees are on the ground.This point is below a scenic overlook and adjoining a trail. Most of PICENG canopy is dead but there is a good subcanopy of ABILAS and PICENG. Many dead and down trees and some White Claron rocks on ground.This point is on a flat area in the middle of a forest hill slope near the breaks. Most mature PICENG are dead from the spruce beetle outbreak and there is high cover of dead and down trees and stumps, and broken-topped trees.LVAL   >NSteep hillside with lots of tree cover and duff. Substrate could possibly be colluvium derived from Wahweep and Claron.An active flash flood channel composed of gravels and boulders. Steep, cut channel banks forming boundaries of polygon can have upland species in the process of being eroded into the channel.Very steep, eroding slopes. Lots of downed trees in area, not sure whether from wind or water. Quite a few tall standing dead (ABICON, PINPON, esp.) are in area, as well.Plot wraps across creek (which has flowing water) to the other bank. Slope and aspect given are for the majority of the plot on the SE-facing slope.Dense CERLED Woodland with some PJ mixed in and scattered emergent PINPON's. Dense ARCPAT where the canopy opens. Small wash with scattered Claron boulders cuts through plot center.Dense mat of ARCPAT along this ridgeline with a dense, short-statured CERLED canopy (a few are barely 2m tall, mostly less) with scattered emergent PINPON. Lots of canopy openings for ARCPAT to fill in.Occasional Red Claron rocks on surface suggest subsurface is a red Claron-derived colluvium.Point directly above drainage on a terraced low slope. Trees very tall.Very steep, active talus slope of red Claron origin.Point is on the side of a rocky knoll. Soil surface is covered on top with gravelly rocks. The knoll has large, rectangular volcanic rocks on it; the sides transitioning into more sedimentary soils. Two clumps of standing dead and live trees are on the plot.Area of consideration is in a large meadow at the forest's edge. Soil surface is free of rocks and covered with herbaceous vegetation and litter. Some animal burrowing and bedding happens here.Giant white Claron boulders and smaller pink rocks scattered around. Trees are tall and beanpole-like.Lots more soil on the surface on this side of the canyon than the south side (N-facing), but the substrate is still Red Claron-derived colluvium.eM `  } H I `*EQ00= 12280Toe slopeGPSv@ talus/ colluvium/ landslideT0000081-b0T001-a0000xvtrpkigec^ZZXVTRP3'"// 5205Low levelGPS@ new alluvium0031-a001-a03003001-a0000nljhfa_]YWSNNLJEA?1% ..8 25214MidslopeGPS@obscured by soils1-a0000071-b0P001-a0000pnljhca_][VRRPNLJE2&!-- 18288MidslopeGPS@talus/ colluvium/ landslideP0000081-b0P00P0000trpnljhfdb]YYWUSQO2&!,, 27350Low slopeGPS,@obscured by soilsP00000900T001-a0000kigec^\ZXVTPPNLJHF3'"++ 28322MidslopeGPSH@obscured by soilsP000009T0T001-a0000jhfdb][YWUSOOMKIGE2&!** 15264Low slopeGPS|@obscured by soils1-a000008P0P001-a0000nljhfa_][YWSSQOMKF3'"))= 29176MidslopeGPS@WahweepTT000071-a01-a00020000eca_]YWUPNIEECA?=;2&!((e 31220MidslopeGPS@WahweepT1-a00006T002001-a0000eca_]XVTPNLHHFDB=;2&!'' 23210MidslopeGPS@Straight Cliffs Formation03000006P01-b00P0000trpnljhfa_]YYWUSQM2&!&& 25288Low slopeGPS@obscured by soils1-a000008000001-b0000nljhfa_][YWSSQOMKF3'"%%> 26268MidslopeGPS@ obscured by soils0000000000000000eca_][YWUSQOOMKIGE2&!$$5 41Low slopeGPS@ new alluviumT1-a0000500500T0000a_][YWUSOMIGGEC><<."## 35200MidslopeGPSX@ talus/ colluvium/ landslide1-b00000302003001-b0000{ywusnljfd`\\ZXVTO2&!"" 30127Toe slopeGPS*@ Claron Formation, Red Member1-a000Pwater030200400P0000}{ywusomie^\ZXVQ3'"!! 16195MidslopeGPSn@Wahweep1-a0000081-a0P00P0000ca_][YWUSQLHHFDB@;2&! 6 18189High SlopeGPS@Wahweep020200007P01-a00T0000fdb`^\ZXSQOKKIGEA=4(#A 27196MidslopeGPS@obscured by soilsT000009T0T00P0000geca_][YWUSOOMKIGE2&!# 5171Low slopeGPS@obscured by soilsT000008T0T00020000hfdb`\ZXVTRNNLJHFD1%  33232MidslopeGPSh@talus/ colluvium/ landslide1-a0000P40500T0000rpnljhfdb`^\\ZXVTO2&!h 5270MidslopeGPS @Brian Head Formation20000320300P0000fdb`^\ZXVTRPPNLJHF0$j 2308High LevelGPS@Brian Head Formation030000070000000000ljhfdb`^\ZXTTRPNLH2&! 28170Toe slopeGPS@Claron Formation, White MemberPP000020200500P0000ywusqomkgea]][YWUS3'" 31112MidslopeGPS"@talus/ colluvium/ landslide1-a0000061-b01-a001-a0000}{ywupnlge`\\ZXVTO2&!tLVALLh & xjThis spot had some logging and burning done after the beetle kill. The plants are responding happily.This site near the park road has some logging and burning done since the spruce beetle kill. The Sambucus and tall forbs seem to love it. Seedlings are growing profusely.Dense ARCPAT shrubland with an open, mixed canopy of JUNSCO and CERLED and emergent PINPON.Colluvium from Red Claron. Lots of house-sized boulders in plot area. Area appears to have had a lot of treefall sometime in the past, and there are now lots of small trees in clusters.This point is in a drainage that has large boulders and smaller rocks and logs throughout. Much of the area has been scoured out from previous flooding. The banks are actively eroding away and trees and shrubs from adjacent hillsides are invading the banks.More rock cover, less duff than in nearby AA 118. Lots of Red Claron colluvium on surface.Lots of soil and a fairly stable slope to be considered talus or landslide, but the substrate is obvious Red Claron colluvium. Lots of large boulders on surface and an erosional channel from cliffs above transects plot. Exceptionally tall trees in this area.Plot is located at the bottom of steep slopes, with a narrow drainage on the downslope edge. Substrate is likely Wahweep or Straight Cliffs colluviumSubstrate likely Red Claron derived.Rock on surface suggests Pink Claron colluvium as a substrate.This point is midway downslope from massive Red Claron cliffs formations. The CERLED and ARCPAT are very thick, and PINPON forms a canopy.This point is on a steep hillside below a massive Red Claron cliffs formation. The CERLED and ARCPAT are very thick throughout, with a sparse mixed conifer canopy. Bands of bedrock forming short cliffs are present.Rolling hills with higher evergreen cover in the swales and higher CERLED, JUNSCO, and ARCPAT cover on the ridges.Substrate is likely residuum/ colluvium from the Wahweep formation, which outcrops nearby.fy F b  Y.ABIIX 3512Midslope1:24K Quad@Claron Formation, Red Member040000PT00500P0000zxvtrpnlhfdbb`^\ZV8, HHV 40286High SlopeGPS:@Claron Formation, White Member050000000050000000xvtrpnljfdb``^\ZXT4(#GG 35250Midslope1:24K Quad@WahweepP000061-b01-a001-a0000kigec^\ZUSNLLJHFDB9-!FF 36290InterfluveGPST@Claron Formation, Red Member520000T0300T0000rpnljhfdb`^\\ZXVTR4(#EE\ 3598Low slope1:24K Quad@Wahweep1-b00003203001-a0000hfdb`[YWUSQOOMKIGB9-!DD 548Midslope1:24K Quad@Wahweep28000TP0P00T0000_][YWUSQOMKIIGECA?6*CC 37225Midslope1:24K Quadv@ Claron Formation, Red Member040000P0300300P0000}{ywusqokiecca_][W9-!BB 43252Midslope1:24K Quad@ Claron Formation, Red Member0402000TP00400T0000}{ywusqokigeeca_[W9-!AAq 34280High SlopeGPS@ Claron Formation, White Member090000T00000T0000vtrpnljhfdb``^\ZXT4(#@@Q 31157High SlopeGPSj@ Claron Formation, White Member080000000020000000xvtrpnljfdb``^\ZXT4(#>>9 13270Midslope1:24K Quadf@ Claron Formation, Red Member1-a000003P00400P0000~|zxvtrpljhddb`^\W9-!==r 20270Midslope1:24K QuadDense duff in this plot.Claron Formation, Red MemberT00000900000P0000{{ywusqS-!<<f 18236Midslope1:24K Quad@Claron Formation, Red MemberT000009P0000P0000ywusqomkigeaa_][YW9-!;;V 15204Midslope1:24K QuadN@Claron Formation, Red Member020000021-a01-a001-a0000~|wusnlgcca_][W9-!:: 26330Low slopeGPS.@obscured by soilsT000008T0T00020000jhfdb^\ZXVTPPNLJHF3'"995 26342MidslopeGPS@WahweepT0000051-a003001-b0000eca_]XVTPNIEECA?=;2&!88 3208Low slopeGPSn@alluvium1-a01-a001-a03004001-b0000kigec^\ZVTPKKIGB@;1% 77 0n/aHigh LevelGPSh@Brian Head Formation1-a000007001-b00020000rpnljfdb][YUUSQOMH2&!66e 30250MidslopeGPSN@WahweepPP00008P0P00P0000][YWUSQOMKIEECA?=;2&!55 35324MidslopeGPS@obscured by soilsT000009P0T001-a0000jhfdb][YWUSOOMKIGE2&!44q 3516MidslopeGPST@obscured by soilsP0000081-a0T001-a0000ljhfd_][YWRNNLJHFD1% 33s 795Low slopeGPS@ Brian Head Formation06000TAsh03T0P00T0000omkigeca_][WRPNLJF0$22 5116Low slopeGPSX@ Brian Head Formation02000Pash0700T00P0000pnljhfdb`^\XSQOMKG1% 11 26151MidslopeGPS@ Wahweep1-a0020007P00200T0000db`^\ZXVRPNJJHFB@;2&!(LVAL, "jVVSteep-sides ravine with water flowing in the bottom and a mixture of sandstone boulders and Claron rocks rolling down the sides.Plot/polygon is a steep, eroding cliff face with only scattered vegetation on the occasional ledge.Very steep talus area on Claron breaks with a sparse mixed tree canopy and a JUNCOM-dominated understory. Large Claron boulders scattered in large gully that cuts through center of plot.This super steep ravine shelters a few brave trees and shrubs. The surface is ball-bearing limestone gravel.The site is the narrow steep slope above the first cliffs of the breaks. The soil is white clay. A few unlucky trees are trying to grow there, but are tumbling due to rapid erosion. The site is practically non-vegetated.This site is the high slope at the top of the first cliff of the breaks. The soil is gravelly white clay. It looks like the Elymus was planted fro revegetation around the viewpoint.Much more open canopy than nearby plots #52, 53, 54Several recently dead trees - PSEMEN and PINFLE - can be found in plot.Plenty of duff cover in the understory.This point is on a low slope above a drainage and its adjacent terrace. There are many standing dead POPTRE and a thick understory of subcanopy trees.This point is midway up a steep slope above the main drainage (Ashdown Creek). There are small grey and pink rocks throughout. This area seems to have every kind of conifer in park, good regeneration of young trees as well.This point is in a drainage that has a high cover of boulders and variable sized rocks. The banks are actively eroding and there is a high cover of dead and downed trees in drainage.This point is in a woodland that extends past the NPS boundary and has meadow areas interspersed throughout. The trees are thick in areas and there are open grassy areas in point.Exposed bedrock is a whitish sandstone.Pink Claron boulders occur in plot, likely the substrate is Claron colluvium. Extremely steep slope.Substrate is likely Pink Claron colluvium.8LVALz  R LHH0dPlot is on a gentle, windswept, high-elevation slope. Soil is gravelly and compacted with plant roots.Plot is in a high, windswept, gently sloping, dry meadow. Mature spruce are beetle-killed, standing dead, but have krummholz live bases which are growing into new trees. Soil is compacted with plant roots. A shallow drainage through plot supports a group of monkshood.This is a mixed open forest of large trees. Some boulders and bedrock are exposed, but it's mostly wood and duff on the surface.Very thick litter with rotting logs throughout. Many ABICON seedlings carpeting ground, some moss and mushrooms - more mesic area.Lots of wood is on the ground. A thick layer of duff covers the surface.This is a thick forest of young trees. Some of the aspen are dead. Logs, litter and duff cover the surface.Lots of down wood here - mostly aspen, but some fir also. A thick layer of litter and duff covers the ground. A couple of large Engelmann spruce are still alive.This is a thick forest of young trees. No much is growing in the understory. A continuous layer of duff about three inches thick covers the surface. Most of the aspen is dead.The aspen trees are mature, large-diameter, and overtopping the fir. Lots of Abies coming into the understory. Most of the down wood is old aspen logs. A thick layer of duff and litter covers the ground.Aspens here are large-diameter, mature and over-topping the Abies. Most of the down wood is aspen. Litter and duff form a continuous, deep layerNo litter or ground cover visible in majority of plot, but small amounts of litter occur on downslope edges.No litter or ground cover to speak of in visible (majority) parts of polygon.This site is a narrow slope at the top of a high cliff. The limestone has crumbled to a gravelly soil. Most of the plants are only a couple of inches tall.Large chunky gray sandstone rocks and boulders embedded in the slope, and lots of pine litter here with no evidence of fire.Only the Bristlecone could love this site.AO Q  b  q ,CWiaa^ 615MidslopeGPSB@Brian Head FormationT00000800000020000igeca][YWUSOOMKIGE/#``Y 1168High SlopeGPS@Brian Head Formation030000031-b0020000000rpnljhfd`^YUUSQOMI3'"__Y 250High LevelGPSn@Brian Head Formation03000004000300T0000mkigeca_[YWSSQOMKG1% ^^S 3245High LevelGPS@ Brian Head Formation020000031-a0030000000qomkigec_]XTTRPNLH2&!]]a 156High LevelGPS@Brian Head Formation05000003P01-b0000000nljhfdb`[YWSSQOMKG1% \\\ 2169MidslopeGPS@Brian Head Formation02000008T01-a00T0000mkigeca_ZXVRRPNLJF0$[[Y 244High LevelGPS@Brian Head Formation03000003P0030000000mkigeca_[YWSSQOMKG1% ZZ[ 550High LevelGPS@Brian Head Formation030000030200200P0000omkigeca][WSSQOMKG1% YY` 7100High SlopeGPSB@Brian Head Formation02000004T0040000000nljhfdb`\ZXTTRPNLH2&!XXW 4200Toe slopeGPSf@Brian Head Formation0604000000P0000000kigeca_][YWUUSQOKG1% WW[ 11296MidslopeGPS@Brian Head Formation04000004P0020000000nljhfdb`\ZXTTRPNLH2&!VVd 2106High LevelGPS@Brian Head Formation05000003T0020000000nljhfdb`\ZXTTRPNLH2&!UUm 3340High LevelGPS@Brian Head Formation05000004P0P00P0000ljhfdb`^\ZXTTRPNLH2&!TTc 5332MidslopeGPS"@Brian Head Formation04000005P01-b0000000mkigeca_ZXVRRPNLJF0$SSd 4353High LevelGPS@ Brian Head Formation02000007T0P00P0000ljhfdb`^\ZXTTRPNLH2&!RRx 22273MidslopeGPS@ Brian Head FormationTP00007P0T001-a0000mkige`^\ZXVRRPNLJH2&!QQ5 15338MidslopeGPS@ Claron Formation, White MemberT00000800T00020000vtrpnjhfdb`\\ZXVTR2&!PP 19314High SlopeGPS@ obscured by soils000000800000020000kigec_][YWUQQOMKIG4(#OO' 18256MidslopeGPS@ Brian Head Formation0000008T0000020000ljhfd`^\ZXVRRPNLJH2&!NN 18276MidslopeGPSB@Claron Formation, White MemberP000008P0P00020000vtrpnjhfdb`\\ZXVTR2&!MM$ 18303MidslopeGPS^@Brian Head Formation0000008T0000020000ljhfd`^\ZXVRRPNLJH2&!LL 13310MidslopeGPS@Claron Formation, White MemberP000008P0T00020000vtrpnjhfdb`\\ZXVTR2&!KK 17282MidslopeGPS @Claron Formation, White MemberP000008P01-a001-b0000zxvtrmkidb`\\ZXVTR2&!JJf 30302Midslope1:24K Quad@Claron Formation, Red Member040000TT00500T0000{ywusqomigecca_][W9-! LVAL  P  0 BPlot center fell in a shallow draw which has many large, rectangular tan (volcanic?) rocks in it. A few are scattered away from the draw. Most of the Asters are found in the draw. Soil surface is also very gravelly, especially in the draw.Plot is in a high-elevation, windswept, dry meadow. Soil is gravelly, with some white limestone rocks also. Vegetation is primarily graminoids. There are some animal burrows and tunnels at soil surface.This point is on a gentle slope within a large dry meadow grassland. There is some evidence of gopher or vole activity.This plot encompasses two geology types which run in 5 alternating strips following the slope. Three strips are Brian Head, where the Poa pratensis and Elymus are found. The other 2 strips are Claron limestone, supporting those distinctive species. Gopher activity is evident throughout the plot, mostly by holes in the ground.Plot fell in an anomalous area with a steep-sided drainage near plot center and a rocky knoll with clumps of fir and Ribes. Delphinium is in the draw. Large white limestone rocks are on the soil surface, and lots of gravelly rocks as well.Plot is in a gently sloping, high-elevation, windswept meadow. Soil is very gravelly, with gray rocks. Most of the Poa fendleriana is growing on the upper slope.This plot is near the bottom of a slope, in a high-elevation, windswept, dry meadow. There are many piles of bare, loose soil and evidence of tunnels from burrowing small mammals.Plot is in a high-elevation, windswept, dry meadow. Soil is gravelly-rocky with lots of surface disturbance from small burrowing rodents.Plot is in a high-elevation, gently-sloping, windswept dry meadow. Four clumps of mature subalpine fir harbor most of the Ribes and Ligusticum, although the Ligusticum is also scattered in the open. Soil is somewhat pebbly/rocky. Forbs vie with grasses for dominance.Plot is in a high-elevation, windswept, sloping dry meadow. Soil is slightly pebbly-rocky. Bromus inermis forms a near carpet of vegetation here.LVAL  | J <This point is near the rim of the breaks and mixed conifer forest about 30m to the north of point. Ground is pinkish Claron soil with small White Claron rocks scattered throughout. ARCPAT growing under trees. Healthy trees and cushion plants.This point is between two fair-sized tree islands within this meadow. There is a tiny amount of bedrock exposed and evidence of vole/gopher activity.This forb-dominated meadow is part of a larger meadow that has shrubs, grasses and Carices. Fair amount of barren ground with small rocks evident and some vole/gopher use. Meadow between island pockets of trees.This point lies in an polygon that is a mix of POTFRU shrubs and various Carex species and grasses. It is relatively flat area with a few barren patches (where water collects?). Grasses are taller than POTFRU.This point is in a gently sloping meadow with very thick CARAQU and SALARI throughout. To the northern edge of the point there is more dry meadow species and less SALARI. No bare ground is visible, only litter. Moist area but no standing water apparent.This point lies in a large spruce-fir forest area on the large plateau of CEBR. Nearly all of the tall, mature PICENG are dead but younger, smaller trees seem healthy. The ground is nearly covered with shrubs, forbs and heavy dead and downed trees.Most of the tall canopy is dead PICENG from the previous beetle outbreak. Subcanopy is healthy ABILAS and PICENG. Dead and downed logs abundant with very high forb cover and litter. Centroid of point is on forest meadow edge so made plot shape more of an oval going back into the woodland.This point lies on a drier hill slope above a meadow. The ground is drier with more bare soil and white limestone rocks scattered throughout. Grass varies from sparse cover to dense cover with less bare ground exposed and more litter.This point is off of the main park road just south of the northern park boundary. There is fairly high bare ground cover with some small rocks scattered throughout and copious litter.I]x  b  b YzG a(yy 2254Low levelGPS@alluviumP0P0TWater0203004001-a0000kigec^\ZVTPLECA?=;1% xxa 15163Low slopeGPS@WahweepT1-a00008T0T001-b0000db`^\WUSQOMIIGEC><3'"ww2 7237Low slopeGPS@obscured by soilsT000008000001-b0000igeca\ZXVTRNNLJHFD1% vv 30184MidslopeGPS@Straight Cliffs Formation1-b000007T0T00P0000rpnljhfdb`^ZZXVTRM2&!uu 3018MidslopeGPS@obscured by soilsT000009000001-a0000igeca\ZXVTRNNLJHFD1% ttj 3241High SlopeGPSb@ Wahweep01-a000031-a004001-b0000igeca\ZXTRMIIGEC><3'"ss8 35358MidslopeGPSJ@ WahweepPP00008P0P00P0000][YWUSQOMKIEECA?=;2&!rrL 34336MidslopeGPSD@ obscured by soilsP000009000001-a0000jhfdb][YWUSOOMKIGE2&!qqm 18195MidslopeGPS@ Brian Head Formation03000003T00300P0000nljhfdb`\ZXTTRPNLH2&!pp~ 340High LevelGPS@Isom Formation1-b000002T0070000000hfdb`^\ZVTRNNLJHFA1% ooz 15308MidslopeGPS@obscured by soils000000900000P0000geca_][YWUSOOMKIGE2&!nn 3191Low slopeGPS@Brian Head Formation020000051-a00200T0000pnljhfdb^\WSSQOMKG1% mm 5200Low slopeGPS@Claron Formation, White Member020000041-a00300T0000zxvtrpnlhfa]][YWUQ1% ll 7294High SlopeGPS@Claron Formation, White Member031-a000T0200300030000}{ywuqomigcaa_][VR2&!kk 30254MidslopeGPS@Claron Formation, White MemberT000008T0T001-a0000wusqojhfdb`\\ZXVTR2&!jjm 2320Low levelGPS@Brian Head Formation020000080000000000kigeca_][YWSSQOMKG1% iiM 0n/aHigh LevelGPS @Claron Formation, White Member0400001-a0004001-a0000|zxvtomkgec^^\ZXVR2&!hhK 35190High SlopeGPS@Claron Formation, White MemberT1-b0001-a1-a007001-a0000~|zusqmkfaa_][VT4(#ggD 26185High SlopeGPS@Claron Formation, White Member0200001-a1-a007001-a0000}{ytrplje``^\ZXT4(#ffp 5307High SlopeGPS*@Brian Head Formation021-b0000400020000000qomkigec_][WWUSQLH2&!eed 2278High SlopeGPS@Brian Head Formation0200000600020000000nljhfdb`\ZXTTRPNLH2&!ddV 0n/aHigh LevelGPS@Brian Head Formation020000080000000000ljhfdb`^\ZXTTRPNLH2&!ccd 2268Low slopeGPS@Brian Head FormationT00000900000T0000igeca_][YWUQQOMKIG1% bb} 3340MidslopeGPS@Brian Head Formation1-a00000800000020000mkigea_][YWSSQOMKF0$LVAL J> .n$This point is near the crest of a very steep hillside. The trees are tall and robust with high diversity. The ground has a high cover of small, gray and pink rocks throughout.Steep, with exposed bedrock outcrops.Substrate likely Wahweep residuum.Rhyolitic boulders and volcanic glass are scattered over the surface. Several dead spruce are in the plot.Plot is in an opening surrounded by scattered clumps of trees and forest on one side. Soil surface is covered with volcanic gravel.Thigh-high forbs create jungle-like conditions. Many dead spruce are in the plot.This point is on a low slope within a broad meadow off of the east park boundary. Slopes are gradual with a few large stones randomly scattered throughout. There are some vole burrows and tunnels in point and scattered small rocks.This point is on a low slope within a broad meadow that is on either side of the main park road adjacent to the east park boundary. A few large rocks are scattered about, but the ground has high cover of small rocks and bare ground.This point is on a sloping meadow between dense patches of spruce-fir. The ground has scattered large rocks but is mostly covered with small rocks, bare ground and litter with a little bedrock exposed. Some RIBMON within the otherwise forb-dominated meadow.This area is a little more open than the surrounding forest. A great mix of trees is present.This point is in a lower seepage area or drainage within a broad meadow. The SALARI is very short and in large clumps within the dense CARAQU patch which follows this drainage/seep area. Taller grasses above the CARAQU.Very white Claron soils with gravelly white Claron rocks. Dead trees and branches litter the ground. Some standing dead trees as well.Point is directly below a White Claron cliff band; the slope below is very steep and covered with small and medium-sized Claron rocks. Trees are very larger; some have dead tops and a few large dead trees on the ground.jLVAL t L \ FfThis point is midway downslope from massive cliffs of Red Claron. Large boulders are scattered throughout.This point is midway downslope from a massive Red Claron Cliffs formation. There is a small anomalous patch of POPTRE just outside of point but in polygon. ARCPAT is a carpet.This point lies directly off of the main CEBR road. The meadow lies next to a tree island to the north. Some dead and downed trees in point.This point is low on a slope that has a lot of barren ground covered with small rocks and large patches of ARCPAT. Point is directly above small drainage hence the high PICPUN.This point is on a low slope directly above the small side drainage off of Ashdown Creek. The ground is covered with dead wood, litter and mosses and lichens. A few large blocks of bedrock are in the point.This point lies in a narrow drainage inundated with boulders, medium and small rocks. There are pools of standing water from the recent rains. PICPUN are very large and robust, understory is diverse but dominated by JUNCOM.Very steep Claron barrens with scattered tree cover dominated by tall and fairly robust (for the species) PINLON. Many ridges and ravines make the slopes have an undulating topography. Flowing creek at base of slope.Most of polygon is scoured stream channel, but the terraces captured in this plot are typical of the broader wash areas.This point is on a hillside clearly dominated by CERLED and ARCPAT. Downslope, near drainage, there is more diversity in trees and shrubs. Some blocky bedrock is at point but ground is otherwise covered by litter.This point is on the low slope of a hill slope that abuts a small drainage. This is a fairly mesic forest with moss and lichen growing between the litter and dead/down trees. Aspen stand is uniform in height at around 35 feet tall and fairly young.Geology could possibly be Wahweep. Very large JUNSCO in this area.Substrate is likely Wahweep. Lots of juvenile trees in this vicinity.rSh ( | # EE c$K? 24190Low slopeGPSN@Wahweep1-aT00051-a02001-a0000eca_]XVTRPKIIGECA<3'"2 21215MidslopeGPS<@Wahweep1-a000071-a01-a001-a0000geca_ZXVQOJHHFDB@;2&! 2263Low levelGPS$@alluvium1-a000pWater1-a50200P0000hfdb`^\ZXVTOHFDB@;1%  24234MidslopeGPSJ@ obscured by soilsT00009T0T001-a0000hfdb`[YWUSQOOMKIGE2&! 26130High SlopeGPSJ@ obscured by soils1-b00000800P00P0000ljhfdb`^\ZXTTRPNLG4(# 2252Low levelGPS"@obscured by soilsT000061-a0P0020000geca_][YWUPNNLJHFD1% Y 15225MidslopeGPS"@Claron Formation, Red MemberT00009T0P00P0000pnljhfdb`^\ZZXVTRP2&!g 21270MidslopeGPSV@ Wahweep1-a00007001-a001-a0000db`^\WUSNLJHHFDB@;2&!{ 30262High SlopeGPSD@Wahweep1-a1-a00071-a01-a001-a0000ljhfd_][VTOMMKIGB=4(#r 28152MidslopeGPS@Claron Formation, Red MemberP000071-b01-a00p0000vtrpnljhca\ZZXVTRP2&! 36266High SlopeGPSR@Wahweep1-a1-b000051-a01-a001-b0000nljhfa_]XVQMMKIGB=4(# 0n/aLow levelGPS @talus/ colluvium/ landslide01-a000040201-b00020000zxvtrnljec_[[YWUPN1%  28255Low slopeGPS8@obscured by soilsP0000051-a0T00030000mkigea_][YTPPNLJHF3'" 31257High SlopeGPS@WahweepP0000061-b00200P0000db`^\ZXVRPKGGECA?=4(#W 28246MidslopeGPS@ Wahweep1-a1-a000061-a01-a00020000kigec_][VTOKKIGE@;2&! 3240Low levelGPSn@new alluvium1-b000Pwater1-a0500200P0000pnljhfdb^\XSLJHFD?1% ] 8255Low slopeGPS\@Claron Formation, Red MemberT1-a000071-a01-a001-b0000}{ywupnlge`\\ZXVQO1%  25225MidslopeGPSD@Claron Formation, Red Member03000004P00200P0000vtrpnljhdb`\\ZXVTP2&!` 20300MidslopeGPSb@ WahweepT000007T01-a00020000b`^\ZVTRMKIEECA?=;2&!~~ 0n/aHigh LevelGPS@ Brian Head Formation02000007001-a001-a0000rpnljeca\ZXTTRPNLH2&!}} 22200Low slopeGPSb@Claron Formation, Red MemberT0000030200300020000ywusqmkiec_[[YWUSQ3'"||k 122Low slopeGPS@WahweepT1-a00008T0T001-b0000a_][YTRPNLJFFDB@;90${{e 6264Low slopeGPS@alluvium1-a031-b001-a1-b01-b001-a0000omkigb`^YWRMMKID@;1% zzq 352MidslopeGPS@Claron Formation, Red Member0400001-a1-a00400P0000wusqomkiec^YYWUSQM/#LVAL ` p 8.:V Substrate is likely Wahweep residuum.Substrate is likely Wahweep residuum.This point is off of a small ridge off of the main Chessman Ridge. There is a diversity of healthy conifers and thick cover of ARCPAT interspersed with bare rocky ground.This point is below some massive Red Claron cliffs with a few boulders and dead/downed trees collecting rocks and litter on their uphill side. Trees are healthy.Fairly steep, S-facing slope with a dense ARCPAT shrub layer and an open canopy co-dominated by PINPON and PSEMEN. Several large Claron boulders strewn about. Litter layer fairly deep under trees and shrubs.This point is directly below a cliff band of Claron (red). The slope is very steep, with boulders and rocks collecting on the uphill sides of trees and larger boulders.There are many large rocks and small pebbles throughout this large flat terrace area near the confluence of Adams and Ashdown Creeks.Soils are probably Wahweep or Straight Cliffs- derived here, but can't tell for sure. There are some car-sized tan sandstone boulders at the base of the slope though. A spring at the base of this slope is flowing into the creek here, which explains the Juncus, Equisetum and Betula.Claron rocks which have rolled down from above are all over this slope, but a big tan sandstone outcropping is in plot (Wahweep?) Ridgetop is definitely Claron, but mostly covered with litter.Rocky/ bouldery wash with large logs lying about that have been washed down- evidence of violent flooding. Water flowing about 2 ft wide and a couple inches deep in the channel now.This point is low on a steep slope above a small drainage. Most of the PICPUN are near the drainage while upslope there is more of a mix of conifers. Lots of dead and down.Mixed evergreen stand on Claron slopes. Openings in the canopy expose Claron rolly rocks, bare soil, and forbs. Trees are very tall. Many downed trees in area.pLVAL \  \2NThis point is directly off of the main CEBR road and is surrounded by a spruce-fir woodland.Exposed ground is covered with small rocks. This meadow point is surrounded by trees.This point is by a tree island but is a wetter, lower area (dominated by Carex species) than the rest of the dry grass and forb meadow. There is some standing water. Polygon includes drier areas with vegetation like AA201. The ELYTRA and STILET are coming in from dry meadow areas.This polygon encompasses the meadow area closest to and between tree islands. Ground has been disturbed by gopher/vole activity. Small rocks cover the bare ground. Some random RIBMON from the tree islands in point are anomalous.Mesic swale with graminoids and forbs doing well here. No evidence of fire anywhere in the area.Mesic swale with large, healthy POPTRE and JUNCOM shrubs seem large here too.This point is on a hill slope off of a small drainage and below a minor ridge in the vicinity of Chessman Ridge. POPTRE is present but not dominant. ARCPAT forms thick patches with bedrock boulders and rock between.This point is lower on the same slope as AA194. The ARCPAT is thick in patches with small rocks, boulders, and litter in interspaces. Some burned out stumps present.This point has large PINPON and an understory of CERLED and JUNSCO. Litter is thick under trees and barren patches between shrubs have high small rock cover.Big, bouldery alluvium from the Claron jumbles up the wash. A small pond with JUNARC is in the plot, probably gets scoured out frequently though.Point falls on a terrace near the wash/creek but high above it, so is probably not receiving water from it. Tons of downed wood and litter here.A lovely park-like woodland of decadent (and a younger subcanopy) PINPON and PSEMEN with a dense ARCPAT understory. Gentle slope (comparatively) above steep "barrens" with litter carpeting the ground. ARCPAT shrubs are close to 1 meter tall! I would love to linger here.u_z % < Vp+L]P 1169High SlopeGPS`@Brian Head Formation1-a000081-a01-b001-a0000trpnlgec^\WUUSQOMH2&!! 33209MidslopeGPS@Claron Formation, Red MemberP000041-a0400p0000sqomkigeca\ZZXVTRP2&!f 4165MidslopeGPS@ Brian Head Formation1-a00008001-a0000000ljhfdb`^YWUSSQOMKF0$b 2250High SlopeGPS@Brian Head Formation1-b00007001-b0000000nljhfdb`[YWUUSQOMH2&! 2230Low levelGPS@obscured by soils1-a00007P0P001-a0000jhfdb][YWUSQQOMKID1%  167High SlopeGPSN@obscured by soils1-a00007T01-a00P0000jhfdb`^\WUSQQOMKID1% f 7170MidslopeGPS@Brian Head Formation2000051-a030000000igeca_][YWRPPNLJHF0$z 5240MidslopeGPS@Brian Head Formation2000051-a02001-b0000ljhfd_][YWRPPNLJHF0$x 3195Low slopeGPS@Brian Head Formation1-b00008001-b0000000mkigeca_ZXVTTRPNLG1%  2291Low levelGPS@obscured by soilsP000PMoss8T0P001-b0000mkige`^\ZXVTNLJHFD1%  3325Low levelGPS0@alluvium06000pWaterP0301-b00P0000igeca_][VTPNGECA?;1% z 7226High SlopeGPS@Brian Head Formation1-b000021-b020020000nljhfdb`^\WUUSQOMH2&!( 2436MidslopeGPS^@obscured by soils1-a00007T01-a0020000jhfdb`^\WUSQQOMKID1%  916High SlopeGPS@obscured by soils02000007T0P001-a0000kigec^\ZXVTPPNLJHD1% } 0n/aHigh LevelGPS@ Brian Head Formation02000007001-a0000000omkigeca\ZXTTRPNLH2&!x 2108High LevelGPSP@Brian Head Formation030000061-a01-b00T0000rpnljhfd_]XTTRPNLH2&!G 22278MidslopeGPSn@WahweepT1-a000071-a01-a00020000hfdb`\ZXSQLHHFDB=;2&! 3193MidslopeGPS@ Brian Head Formation1-a000006000300T0000mkigeca_[YWSSQOMKF0$t 0n/aHigh LevelGPS@Brian Head Formation020000061-a01-a0000000rpnljhfd_]XTTRPNLH2&!j 0n/aHigh LevelGPS8@ Brian Head Formation1-b0001-awater08t0t00T0000wusqomkigec_XSQOMH2&![ 2210High LevelGPS@Brian Head Formation1-b000005T00400T0000omkigeca][YUUSQOMH2&! 3310Toe slopeGPS@obscured by soilsP000PMoss8000001-b0000mkige`^\ZXVTNLJHFD1%  7272Toe slopeGPS@obscured by soilsP00008000001-a0000geca_ZXVTRPNNLJHFD1% ] 22218MidslopeGPS@Wahweep1-a1-a000061-a01-a00020000kigec_][VTOKKIGE@;2&!LVAL & h &DPThis is a grass-dominated meadow that also has high forb cover. Point is directly off main CEBR road.This open woodland is directly off of the main CEBR road. There are small rocks scattered through. Some standing dead trees and high dead and down logs and stumps throughout. There is more POPTRE in polygon than in point.A few rocks from the Wahweep/Straight Cliffs (?) and Claron formations scattered through the soil.A narrow terrace ~2 meters above flowing Ashdown Creek. POPANG have skinny canopies, but are evenly scattered on terrace. Many evergreen seedlings. Most of terrace has exposed alluvially-deposited soils with strips of boulders from flash floods along the middle of the terrace.This point is in a tree island within a large meadow on a broad plateau. The dead and down tree cover is very high with a few open spots. Many trees have broken tops, leaning over, some standing dead. The ABILAS seedlings form round mats.This point is just east, midway downslope from Shooting Star Ridge. The ARCPAT forms a thick blanket of shrub cover with exposed areas filled with litter and few small rocks.Open-feeling woodland with what appears to be young, healthy trees. Shrubs are healthy too, waist-high in places.This is a drier meadow, forb-dominated area, directly off of the main CEBR road. To the east there is a wetter, lower, Carex-dominated polygon (also very small). There is a fair amount of barren ground due to gopher/vole activity. An isolated patch of LUPARG to west end of point is anomalous.This area is midslope down from a massive Red Cliffs formation. The trees are robust, the ARCPAT is in thick patches with bedrock and bare ground covered with small rocks in between.This polygon basically encompasses the meadow around the spruce-fir aspen forest that abuts the large meadow. The point is relatively flat, but there are small slopes of varying slope and aspect. Some medium, grey, square rocks around.$LVAL ,2 D ,dF&JPlot wraps over both sides of this pink rock-covered, narrow ridge, bur majority of plot falls on the SW side.This point is directly off of the main CEBR road. Some exposed dirt from vole/gopher activity.This polygon of DASFRU should run NE to SW in a fairly narrow rectangle. Some soil exposed with small rocks scattered throughout.This point is directly off of main CEBR road. ARTCAN is varying in cover across point and polygon. Vole/gopher activity making bare ground in areas. Small rocks throughout.This is a tree island within the large meadow of Chessman Overlook. There are many small rocks on the surface and some larger blocky rocks, as well. Some anomalous POPTRE within the ABILAS and PICENG woodland tree island.This point lies in a broad flat plateau. This polygon is dominated by ARTCAN and generally POAPRA but some areas have good cover of native grasses. Some gopher/vole activity.Slope is covered with golf ball and marble-sized pink/orange rocks. A few big boulders are present.This point is in the meadow along the main CEBR road near a tree island. Some bare ground is exposed with small rocks scattered throughout.Not sure of the geology here, since both Claron and Straight Cliffs (or Wahweep?) rocks are present. Point is on a fairly broad, flat terrace high above the creek. No sign that fire ever touched this place.It looks like there are rocks from both the Claron and Wahweep/Straight Cliffs layers here, so not sure about geology. Soils seem sandy though. ARCPAT is giant here.This tree island is fairly large and directly off a main CEBR road and within the Chessman Overlook area meadow. There are open areas within the woodland that have short forbs where shrubs and tall forbs are by trees. Large and small rocks throughout.This point is in the fairly dense tree island of POPTRE-ABILAS within the large meadow of the Chessman Overlook area. Plenty of downed logs and stumps and thick carpets of ABILAS seedlings. Dense litter and some rocks on the ground.C_} - J L[i|&! 624Low slopeGPS@obscured by soilsT0001-aMoss8P0p001-a0000omkigb`^\ZXVPKIGEC0$ 2437MidslopeGPS@Claron Formation, Red MemberP000061-b0200P0000rpnljhfdb`[YYWUSQO1%  3338MidslopeGPS@Straight Cliffs Formation1-ap001-aMoss8P0P00P0000xvtrpnljhfdb\WUSQL1%  1025High SlopeGPSF@Wahweep1-b00006p0200P0000_][YWUSQOMKIIGECA<3'" 1510High SlopeGPS@Claron Formation, Red Member1-a000061-a02001-a0000zxvtrmkige`^^\ZXVQ3'" 3044MidslopeGPS@Claron Formation, Red MemberP000061-b0200P0000rpnljhfdb`[YYWUSQO1%  30343High SlopeGPS@obscured by soilsP00009P0P00P0000geca_][YWUSQQOMKIG4(#S 30337Low slopeGPS@ Claron Formation, Red Member1-a00003203001-a0000wusqojhfdb`^^\ZXVQ3'" 2538MidslopeGPS@ Claron Formation, Red MemberP000061-b0200P0000rpnljhfdb`[YYWUSQO1% U 2348High SlopeGPS @ Brian Head FormationT000031-b060000000kigeca_][YTRRPNLJH2&!N 33253MidslopeGPS@Claron Formation, Red Member30000PP0600P0000pnljhfdb`^\ZZXVTRP2&!_ 30268High SlopeGPS@Claron Formation, White Member7P0000T020000000trpnljhfdb`^^\ZXVT4(#Z 32323MidslopeGPS0@Claron Formation, Red Member300001-a1-a0500P0000vtrpnljhfd_ZZXVTRP2&!P 0n/aHigh LevelGPS@Brian Head Formation20001-awater41-a01-a00T0000xvtrpnljec^\UPNLJH2&!S 3165High SlopeGPS@Brian Head Formation1-a00008T01-a00T0000nljhfdb`[YWUUSQOMH2&! 3348MidslopeGPS8@obscured by soilsT00006T01-a0030000geca_][YTRPNNLJHFD1%  2323Low levelGPS@obscured by soilsT000pMoss70000030000jhfdb`^\ZXVTNLJHFD1% L 28176High SlopeGPSz@obscured by soilsTT00061-a01-b001-b0000pnljhca_ZXSQQOMKIG4(#y 32166High SlopeGPS2@Wahweep1-a1-a00071-a01-a001-a0000ljhfd_][VTOMMKIGB=4(## 32237High SlopeGPS@ Claron Formation, Red Member1-a000031-a0500P0000xvtrpnljhfa__][YWR4(#i 0n/aHigh LevelGPS@ Brian Head Formation20000800T0000000hfdb`^\ZXVTRRPNLJH2&!W 131High SlopeGPS@ Brian Head Formation1-a00009001-a00T0000mkigeca_ZXVTTRPNLG1% [ 0n/aHigh LevelGPS^@Brian Head Formation200007001-a0000000kigeca_]XVTRRPNLJH2&!q 5231High SlopeGPS@Brian Head Formation1-b00005T040000000kigeca_][YWUUSQOMH2&!LVAL T l<rWater flowing through the bottom of this deep, narrow ravine. Lots of large boulders and talus from the Claron above. Plot falls on both steep slopes of this ravine, but slope and aspect given are for the majority of plot.Mixed conifer stand with ABICON and PSEMEN co-dominant and JUNCOM abundant in the understory. Many Claron boulders strewn about.There are large rocks scattered throughout this small polygon and most of ground is covered with small rocks. Shrubs are low growing.Very steep Claron barrens slope with a sparse mixed canopy dominated by PINLON and a sparse shrub understory dominated by ARCPAT. A few PINLON are very tall and robust. Rollly rocks cover most of the ground.This is the narrow slope at the top of the first big cliff of the breaks. The soil is gravelly clay.Steep Claron barrens with sparse tree cover due to the short, narrow canopies of the mixed trees found here. Many small gullies incise the rocky slope.This point is shapes to follow a drainage or seep with some standing water in which CARAQU is dominant with other mesic species present. Bedding sites (deer?) present. Some large rocks throughout.This point is on a gently sloping hill on the relatively flat, large plateau of CEBR. This polygon is extensive and ARTCAN cover varies throughout. Some bare ground exposed and small rock scattered around.This area has thick tree cover, very high 100 hour fuel loading, and thick dead and downed trees (1,000 hour fuels). Some stumps in area and standing dead.Dense forest with an amazing amount of downed wood and deep litter.This point is directly off of Shooting Star Ridge. The ARCPAT crosses over the ridge and down the opposite slope. PINPON dominates, but there are many different tree species on the ridge.There is some exposed bedrock and many small rocks in the barren shrub interspaces, which makes me think this Wahweep. The trees are diverse and robust..LVAL :" @ x|JTVery steep south-facing slope of Claron rolly rocks and a dense ARCPAT shrub layer with a sparse but diverse canopy layer. Some large Claron boulders scattered about. A dense little stand (5-6 trees) of PINLON just outside plot boundaries to the NW.Gopher / vole activity exposing barren ground with few scattered small rocks. Some dean and downed trees from tree islands within large meadow on plateau.This point is in a gently sloping dry meadow with much soil exposed with small rocks throughout. Some vole / gopher activity.Many basketball and larger sized Claron rocks on the slope.Rocks from both Wahweep and Claron are scattered on the slope here.Dense mixed canopy with ABICON dominant. Rock-lined wash runs through plot. Lots of moss covering areas where litter is not as thick. POPTRE presence due to cooler air sink in this drainage.ABICON-dominated, fairly open woodland with PICPUN nearly co-dominant. Large gully in plot has lots of boulders in it. Much less PSEMEN and more PICPUN than in last plot (#245) in this polygon.Very steep, sheltered, cool slope with a PICPUN-dominated canopy and JUNCOM-dominated understory. Lots of moss. Large landslide area in plot exposes some bare soil, otherwise litter and branches and trees cover the ground.Mixed open woodland with ABICON dominant and JUNCOM-ARCPAT co-dominant in the understory. Trees look fairly young (not very tall). Narrow ridge runs from S to N.Narrow ridgeline running S to N with a very mixed and open tree canopy. Here PINFLE is dominant, but all the trees have fairly low cover. Understory is typical of the polygon (ARCPAT-JUNCOM co-dominance).Very mixed open woodland dominated by PICPUN, ABICON, and PINLON. Large gully runs through plot. Trees appear fairly young, not very tall.Mixed canopy with ABICON clearly dominant and many younger ones regenerating in the subcanopy. Cooler aspect may explain the presence of POPTRE here and the absence of ARCPAT. Steep slope seems less so because it's not rocky.Vcx  u 5 NY `-4C 20210High SlopeGPS@Wahweep1-a0000031-a003001-b0000jhfdb][YUSNJJHFDB=4(#q 30263High SlopeGPS@Claron Formation, Red Member03000003P00300P0000xvtrpnljfdb^^\ZXVR4(#, 21220MidslopeGPS@obscured by soils1-a0000071-a01-b001-b0000sqomkfdb][VRRPNLJE2&! 115Low slopeGPS\@obscured by soilsT0002moss6000001-a0000ljhfd_][YWUSMKIGEC0$< 842High LevelGPS@Wahweep31-a0003P0300P0000][YWUSQOMKIGGECA<:1%  84Low slopeGPS@obscured by soilsT000Pmoss9000001-a0000jhfdb][YWUSQKIGECA." 36210MidslopeGPS@talus/ colluvium/ landslide31-b000T401-b00P0000usqomkigb`^\\ZXVQO2&!& 28322MidslopeGPS@Straight Cliffs FormationT00009P0P00P0000mkigeca_][YWWUSQOM2&!n 22170MidslopeGPS@Claron Formation, White Member200005T04001-b0000usqomhfdb`^\\ZXVTR2&!' 35282High SlopeGPS@ Claron Formation, White MemberT0000800T0020000trpnljhfdb`^^\ZXVT4(# 8329Step in slopeGPS@obscured by soilsT000080000020000hfdb`^\ZXVTRRPNLJH5)$ 31330MidslopeGPSd@obscured by soils1-a0001-amoss41-a01-b0020000wusqomkidb][UPNLJE2&! 850Low slopeGPS|@obscured by soilsT000PMoss8000001-b0000ljhfd_][YWUSMKIGEC0$B 30191MidslopeGPSz@Claron Formation, Red Member200006P0200P0000pnljhfdb`^\ZZXVTRP2&! 0n/aLow levelGPS.@alluviumT01-a001-b1-a007001-b0000igeca\ZXTRMHHFD?=;1%  5305Step in slopeGPS@obscured by soilsT000006T0T00040000ljhfd`^\ZXVRRPNLJH5)$^ 28330MidslopeGPSD@Wahweep02P000041-b01-a001-b0000hfdb`[YWRPKGGECA?;2&! 22215MidslopeGPS@obscured by soils1-a0000071-a01-a00020000rpnljfdb][VRRPNLJE2&!+ 30230MidslopeGPS@Claron Formation, Red Member02000005P00300P0000vtrpnljhdb`\\ZXVTP2&! 35189MidslopeGPS@ Claron Formation, Red Member020000041-a00300P0000ywusqomkge`\\ZXVTP2&![ 2345MidslopeGPS6@ Brian Head Formation200007T01-a00T0000igeca_][VTRPPNLJHF0$R 2357High SlopeGPS@ Brian Head Formation4000040020000000hfdb`^\ZXVTRRPNLJH2&!Z 3240Low slopeGPSv@talus/ colluvium/ landslide1-a000Pmoss220400P0000xvtrpnljhfdb\ZXVTO2&! 3359MidslopeGPS@obscured by soilsP00008P0p001-b0000geca_ZXVTRPNNLJHFD1% LVAL n  lI'm surprised anything can grow on this steep slope. Trees that couldn't hang on are tangled on the ground. A few bare spots are showing where it was just too steep. There is 6% dead PICENG cover in plot.This point is in a step in slope that collects and holds runoff (more mesic species). There is a lot of dead and downed trees.This point is on a steep slope off of a ridge above Cresant Hollow. The ground has small rocks, moss, lichen, and dead logs throughout. The PINPON are on upslope side of point.A mix of evergreens and aspen with horsetail dominant in the understory. Downed wood everywhere! Litter layer is very thick. ABICON is the predominant tree regenerating in the understory.Steep, S-facing slope with a dense, nearly impenetrable ARCPAT shrub layer and scattered, mixed trees, with PSEMEN the largest (hence highest cover) trees. Lots of JUNSCO in the subcanopy.This point is at the confluence of a small drainage and the upper section of Ashdown Creek. The ground is covered with small rocks, boulders and logs.This point is near a small tributary off of Shooting Star Ridge. The area is relatively flat, with lots of dead and downed trees and few standing dead. Here are a lot of young trees and seedlings.Cool north facing slope with some seepage areas and a couple large gullies that are boulder-strewn. Mixed tree canopy is Picea pungens dominated, but understory is a diverse mix of shrubs. Lots of dead trees and limbs on the ground. Pink Claron cliffs about 100 meters (or less) upslope.This point is below Shooting Star Ridge on a beautiful, open, sunny PINPON/ARCPAT hillside. Interspaces between shrubs are filled with small rocks, bare ground and POAFEN, Carex rossii and litter.Steep south-facing slope of Claron rolly rocks and a dense, nearly impenetrable ARCPAT shrub layer. Lots of young (large saplings) PINPONs creeping into polygon from the more wooded polygon downslope.LVAL H D n z$This point is about 50m downslope from Shooting Star Ridge. The trees are robust, tall. There are some standing dead trees, grey-pinkish bedrock and blocky rocks around.This point is directly off of a ridge between Crescent Hollow and upper Ashdown Creek. The ARCPAT forms clumps with fairly large rocky barren patches in between. Diverse tree species here, but PINPON dominates.Plot wraps over both sides of a steep ridge covered with pink pebbly rocks. No evidence of fire here.This point is on a hill slope just below Shooting Star Ridge. The area is open sunny, with tall trees and a blanket of ARCPAT with interspaces of blocky rocks, CARROS, downed trees and litter.Very open woodland of PICPUN with an extremely dense mesic herbaceous understory. Soils are permeated with water and many areas have active water seepage at the surface and lots of moss. Ground is nearly entirely covered with a mix of grasses, sedges, and forbs. Lots of downed wood. A lovely spot!Narrow exposed ridgeline with scattered mixed trees (PINPON dominant) and dense ARCPAT cover.A forest of extremely dense, young (DBH=2-6 inches) PSEMEN and POPTRE. Nothing worth noting in the understory, maybe 3 individuals of MAHREP, but otherwise very sparse and with a very thick litter layer. Many downed trees.Extremely steep, unstable rock and landslide area with many Populus spp. recolonizing it, but overall vegetation is, not surprisingly, very sparse. Cliffy bedrock exposures are actively crumbling and littering the slope with basketball-size boulders. CALSCO doing quite well despite the hot exposure and lack of seepage.Very open woodland of decadent PINPON, mixed trees in the subcanopy, and lots of ARCPAT in the understory. Few shorter POPTRE scattered in plot, but not sure if that's typical of the polygon.This point is directly off of the main CEBR road. There are many White Claron rocks throughout the heavy litter accumulation. Shorter forbs and seedlings dominate the understory and there is a good mix of tree species.lH Q D g =Q*7R 35276MidslopeGPS@ talus/ colluvium/ landslide1-a0000230400P0000rpnljhfdb`^\\ZXVTO2&!o 21321MidslopeGPS@obscured by soilsT000Pmoss9P0T00P0000kigeca_][YWUOMKIGE2&!H 18174Low slopeGPSV@Brian Head Formation200006P01-b001-b0000omkigb`^YWUSSQOMKI3'"M 18202Low slopeGPS$@Brian Head FormationP00008P0P0020000igeca_][YWUSSQOMKI3'"d 32292MidslopeGPS@WahweepP000Pmoss61-a0P001-b0000geca_ZXVTRMKECA?=;2&!g 36279High SlopeGPS@Claron Formation, Red Member1-a0000320400P0000usqomkigeca__][YWR4(# 30274MidslopeGPSx@talus/ colluvium/ landslide300004201-a001-a0000usqomhfd_][YYWUSQO2&!~ 25252MidslopeGPS@WahweepP00008P0P00P0000[YWUSQOMKIGEECA?=;2&!: 3682MidslopeGPS@Wahweep61-a000T1-a0300P0000`^\ZXVTRPNIGGECA<:1%  10330MidslopeGPS@obscured by soilsT000070000030000eca_][YWUSQOOMKIGE2&!E 18328MidslopeGPSx@ obscured by soilsTT0007T01-a0030000hfdb`^\ZUSQOOMKIGE2&!B 2618High SlopeGPSF@ obscured by soilsTT001-amoss, lichen41-a01-b0030000}{ywusqojhcaSNLJHF3'" 1870MidslopeGPS@ obscured by soilsT000070000030000db`^\ZXVTRPNNLJHFD1% o 3154MidslopeGPST@ Wahweep300004P0300P0000ZXVTRPNLJHFDDB@><:1% H 9350Low slopeGPS@obscured by soilsT000PMoss9T00001-a0000mkige`^\ZXVTNLJHFD1% 8 25232MidslopeGPS@obscured by soilsT00009T0000T0000eca_][YWUSQOOMKIGE2&! 14305MidslopeGPS.@obscured by soilsTT00007T0T00030000igeca][YWUSOOMKIGE2&! 30210MidslopeGPSF@talus/ colluvium/ landslide0300001-a0300300P0000xvtrpnljfd`[[YWUSO2&!l 30274MidslopeGPS@talus/ colluvium/ landslide030000041-a01-a00P0000ywusqomkfd_[[YWUSO2&!Y 20304Low slopeGPS@talus/ colluvium/ landslide020000061-a0P001-a0000zxvtrmkige`\\ZXVTP3'"} 32224MidslopeGPSH@talus/ colluvium/ landslide0200001-b0300300P0000xvtrpnljfd`[[YWUSO2&!/ 1658Low slopeGPS0@obscured by soilsT000Pmoss0900T001-a0000pnljhca_][YUOMKIGE2&! 16280MidslopeGPS@obscured by soilsT000008T01-a001-b0000mkige`^\WUSOOMKIGE2&!3 24308High SlopeGPSV@ obscured by soilsT1-a00Tmoss/ lichen051-a01-a00020000~|zvtrmkfbTRPNIG4(#DLVAL < \*lThis point is midway down a slope that has high dead and down trees, stumps, branches and litter. Small rocks are scattered throughout. So many 1000 hour fuels that walking is difficult.This point is just off a ridge between Crescent Hollow and Ashdown Creek. There are many conglomerate, blocky rocks throughout area and large dead and down trees.This point is on a hill slope, off of a small tributary drainage off of shooting star ridge. There are very large logs on the ground and a blanket of ARCPAT. The PINPON are very tall and robust.Very steep canyon side with a mixed open woodland and a mixed shrub understory. Abies and JUNCOM are dominant. More ARCPAT and PINPON upslope in polygon near the ridge.Pretty homogenous forest of giant Spruce on this fairly flat bench with a sparse understory. Litter layer consistent except for spots of moss. Lots of downed wood and half a dozen standing dead PICPUN.The limited rock exposed on surface suggests substrate is residuum / colluvium from the Wahweep.This point is midway downslope from Shooting Star Ridge near a small tributary drainage. The trees are healthy and tall with only a few standing dead.Colluvium derived from Pink Claron.Colluvium is derived from Pink Claron. Lots of areas with soil rather than just talus, but still not much development of an understory.Plot is located at the toe of a colluvial slope, but it's a narrow one, and plot lops onto Wahweep residuum areas.Steep, actively eroding loose talus.This spot has very dense trees (trunks spaced 1-3 feet apart on average), but because the canopies are narrow, tree cover is much lower than it looks like it should be. Understory is sparse. Thick littler layer everywhere and lots of downed wood. PSEMEN (dead tree cover) is 3%.This point is on a more open, sunny area of the ABICON forest in which the ARCPAT cover is particularly high. There is a mix of conifers with some very large PINPON. Looks like a PINPON/ ARCPAT but with high cover of ABICON.LVAL n . $ lzzRLots of dead spruce characterize this area. Spruce and fir seedlings and saplings enthusiastically fill the understory.Site is in a gently sloping, dry meadow with clumpy trees. There is some gopher activity here. The Ligusticum is mainly within the tree clumps; the Erigeron and Poa are found in the openings.Site is in a gently sloping meadow, with clumps of trees having a Ligusticum-dominated understory. The other forbs and the Poa are in the openings.Steep, active talus slope. The ASTKEN is quite common on sheltered or protected parts of this slope - perhaps even close to 1%.Thick stand of POPTRE with some PSEMEN mixed in and sapling ABICON regenerating in the understory. Thick litter layer carpets he ground except for some mossy spots. Lots of dead Aspen poles on the ground.Most of the dead and down wood is Aspen. Live Aspen are large diameter, >10 inches, and are overtopping the fir. The understory is a very homogenous layer of Ligusticum.Aspen trees are large diameter, mature, and mostly overtopping the fir. Many down logs, mostly old Aspen. Understory is dominated by Ligusticum.Lots of deadfall and no evidence of fire. Trees seem fairly young though.Part of the plot is quite open with a lot of Claron exposure (see photo).Colluvium from pink Claron. Area is transected by multiple, steep erosional runnels and gullies. Trees show damage from rock fall. Some dead PINPON trunks occur in plot, but none alive.Rock cover is higher in plot than much of polygon because of the proximity to ridge crest.Large landslide area that now supports a sparse mix of grass, shrubs, and tree seedlings. Very steep with scattered rocks but mostly bare soil exposed. Some seepage areas at the base of the slide.This point is west of a ridge west of upper Ashdown Creek. The slope is more gentle in this area and litter accumulation is high. Lots of dead and downed trees on ground and some standing dead trees.^p " A R ]dXM  ? 2316High LevelGPS@Claron Formation, White Member080000T00P0000000trpnljhfdb`^^\ZXVR2&! 5260Low slopeGPS@Claron Formation, White MemberP000Pwater08T0T001-a0000}{ywupnljhfb[YWUSQ1%  20190MidslopeGPS@Claron Formation, White Member030200006T0P00P0000xvtrpnljhfd``^\ZVR2&! 24223High SlopeGPS@ Claron Formation, Red Member1-a000008T0P00P0000wusqomkigec__][YWR4(# 19302MidslopeGPS@Claron Formation, Red Member02000005T00200P0000vtrpnljhdb`\\ZXVTP2&! 12345Low slopeGPS@Claron Formation, Red MemberT000Pwater09000001-a0000}{ywupnljhfb[YWUSQ3'"@ 11318High SlopeGPS@Claron Formation, White MemberT00000900000P0000vtrpnljhfdb^^\ZXVT4(#@ 25324MidslopeGPS:@Brian Head FormationT00000900000P0000jhfdb`^\ZXVRRPNLJH2&! 13246High SlopeGPS@ Claron Formation, Red Member1-a00000800000P0000wusqomkigec__][YWR4(# 15240High SlopeGPST@Claron Formation, Red Member02000005000200P0000xvtrpnljfdb^^\ZXVR4(#N 2664MidslopeGPS@Brian Head FormationP00000800000P0000igeca_][YWUQQOMKIG1% 2 5202MidslopeGPS@Brian Head Formation030000031-a003001-a0000rpnljeca][VRRPNLJF0$- 5157MidslopeGPS,@Brian Head Formation030000021-a00400P0000omkigeca][VRRPNLJF0$ 4124Low slopeGPST@Brian Head Formation030000021-b01-b001-a0000trpnlgec^\WSSQOMKG1% # 6125MidslopeGPS,@Brian Head Formation05000005P0P0000000jhfdb`^\ZXVRRPNLJF0$ 3170MidslopeGPSj@Brian Head Formation02000003P00300P0000ljhfdb`^ZXVRRPNLJF0$ 4167Low slopeGPS@Brian Head Formation2000051-a02001-a0000mkige`^\ZXSQQOMKIG1%  4190MidslopeGPS&@Brian Head Formation600002T0200T0000fdb`^\ZXVTRPPNLJHF0$D 12271High SlopeGPS2@Claron Formation, White Member80000P00000T0000trpnljhfdb`^^\ZXVT4(#4 2122Low levelGPS@Brian Head FormationP000Pwater90000000000nljhfdb`^\ZXQOMKIG1%  3341High SlopeGPS@Claron Formation, Red Member1-b0000P40400T0000trpnljhfdb`^^\ZXVQ3'" 297MidslopeGPS@Claron Formation, Red Member200001-b40200P0000pnljhfdb`^\WWUSQOM/#; 658MidslopeGPS@ Brian Head Formation500004T0P001-a0000hfdb`[YWUSQOOMKIGE/#@ 5110MidslopeGPS(@ Brian Head Formation400004001-b001-a0000ljhfd_][VTRPPNLJHF0$TLVAL :( p > ftThis site is a small swale that is relatively dry. A few limestone boulders decorate the surface. The soil is gravelly.Plot is in a gently sloping, dry meadow. A narrow drainage runs through, exposing volcanic rocks and pebbles. Gophers are running amok under ground.Plot is in a gently sloping dray meadow with shallow drainageways where Poa is most common. Anomalous clumps of trees and Ribes dot the meadow; an especially large one comprises about 10% of plot. Soil is gravelly with volcanic rock. Several dirt piles from burrowing animals are here. Dead PICENG is 5%Site is in a dry meadow, near valley bottom. Clumps of trees and Ribes interrupt the herbaceous layer. Soil is volcanic-gravelly, with a few large rocks and a smattering of white Claron rocks. This meadow was probably grazed in the past. Gophers have been busy here.Site is a gently-sloping, dry meadow. It's likely this entire meadow was grazed at some time previously - dandelion and yarrow are conspicuous. Soil is somewhat gravelly. Burrowing small animals are quite active here. An anomalous patch of trees and Ribes is in the plot.This site is right next to the edge of the breaks. The soil is white clay. The vegetation has elements of the cushion plant community and of the forest.This site is a low-lying mesic meadow with surface water in channels only. Soil surface is not saturated. Willow forms a dense thicket, with Carex occupying all openings. The mentioned forbs are found under the willow.Large rock / land-slide area with sparsely scattered mature trees and lots of seedlings / saplings regenerating. Claron cliff band is within 100 meters upslope. Many large boulders and gullies regularly incise the slope. Great views of the whole park from here!Steep, cool aspect slope with many active land / rock slide areas and deeply incised gullies strewn with boulders. Many dead PICPUN here (still have brown needles on them). Rocks piled upslope of tree bases is a common sight.LVAL  * This site is near the edge of the breaks. The understory is open. The surface has a thin layer of duff over gravelly soil. There are few dead trees and not much litter on the ground. The bristlecones are growing tall and straight like regular trees.This area was hit hard by the spruce beetle. The understory isn't quite as dense as other areas nearby. The surface is gravelly red soil.This is a little forested valley with a fairly broad bottom. Plenty of dead spruce dot the area. Many logs are on the ground. Vegetation and duff cover the surface. A perennial stream flows through the plot.All the mature spruce trees are dead. The understory is choked with vegetation. The surface is covered with a thick layer of duff.This is an area of heavy beetle kill on the sad spruce. Most of the dead wood is standing. Thick forbs fill the understory. Thick duff covers the surface.This site is right on the edge of the breaks. The understory is open with a lot of gravelly soil showing. It looks like mistletoe is attacking some of the bristlecones.Lots of standing and reclining dead trees (mostly spruce) litter at this site. Many forbs fill the understory thickly. The surface is covered with a few inches of duff. Mistletoe is infecting the subalpine fir.This site is in a gently sloping, dry meadow. There is an anomalous patch of trees w/Ribes underneath. Soil is volcanic-gravelly, with larger rocks scattered around. Some mounds of dirt point to gopher activity.Plot is in a gently sloping dry meadow with shallow drainage channels converging downslope. Soil is gravelly with volcanic rocks and many larger rocks are scattered around. A small clump of dead spruce is on plot where the Ribes and Ligusticum are found. PICENG (dead) is 2%.Site is in a dry, gently sloping meadow. A narrow, rock-lined ravine runs along. Trees with Ribes are in clumps. Soil is moderately gravelly. Gophers are active here.LVAL l |  L FpOn this high slope, shrubs begin to invade the meadow. The soil looks deep and rich.Some ryolitic boulders, volcanic glass, pumic and white limestone pebbles decorate the surface. Shrubs are invading the meadow in this area.This is a broad, gently sloping meadow that is mostly dry. The soil is mostly gravel-free. A few anomalous trees are included in the polygon.This point fell right in the bottom of the valley. The drainage is seasonal and not too moist at this time. The Bromus is in the bottom of the drainage and the Poa pratensis is on the gently sloping sides.Point is on the top of an interfluve within a fairly wide, shallow drainage. Many dead and down trees and grey cobble-sized rocks scattered throughout point. Some standing dead trees. Center of point has a few anomalous trees that are inclusions. There is a wet drainage to the north side of plot that has Carex praegracilis and other mesic species.This is a dry meadow. Soil is fine textured. A few white limestone pebbles are scattered on the surface.This is a large, dryish meadow that is quite homogenous.Soil here is reddish, not gravelly at all. Forbs and grasses are mixed here. Lots of gopher activity.Point is in a meadow below the picnic area, adjacent to Campground. Nothing looks trampled today. Soil has a lawn aspect from the Poa pratensis. Some gopher holes are around.This plot is right next to the edge of the breaks. The soil is white clay with a few pebbles. The site is inhabited mostly by cushion plants.This point fell at the bottom of a gorge with a flowing stream. This puts some surprising aquatic species in a small part of the understory. Slope and aspect were shot down the drainage. The plot includes both sides of the stream.This bristlecone forest has an open understory and a thin layer of duff covering the surface. A fair number of dead logs are on the ground. These bristlecones are straight and tall like regular trees.Te  Y k .F\cX!! 26358MidslopeGPS@Claron Formation, Red Member1-a00001-a0400400P0000zxvtrpnlhfb]][YWUP2&!   17280High SlopeGPS@ Claron Formation, Red MemberP000009T0P00P0000trpnljhfdb`\\ZXVTR4(# 33168MidslopeGPS@ Claron Formation, White MemberTT000061-a00200020000{ywusomkge`\\ZXVTR2&! 5198Step in slopeGPST@ Claron Formation, White Member03000007P0T00P0000ywusqomkigeaa_][YU5)$ 12155MidslopeGPS@ Wahweep1-a1-a000051-a01-a001-a0000ljhfd_][VTOKKIGE@;2&!= 159Low slopeGPSR@Claron Formation, Red MemberTT00008T0T00020000rpnljfdb`^\XXVTRPN0$8 5228High LevelGPS@Brian Head Formation07000002P0P0000000ljhfdb`^\ZXTTRPNLH2&!4 5214High LevelGPS<@Brian Head Formation07000002T0P0000000ljhfdb`^\ZXTTRPNLH2&!; 1255High SlopeGPS@Brian Head FormationT000006P003001-b0000pnljhca_[YWSSQOMKI3'"L 6276High SlopeGPST@Claron Formation, Red Member0600000300P00T0000trpnljhfdb`\\ZXVTP2&!T 9171MidslopeGPS@obscured by soils060000040000000000geca_][YWUSOOMKIGC0$G 6203Low slopeGPS@Brian Head Formation06000002T0P0000000kigeca_][YWSSQOMKG1% N 5153Low slopeGPS,@obscured by soils050000050000000000hfdb`^\ZXVTPPNLJHD1% J 3166High LevelGPS@obscured by soils060000030000000000igeca_][YWUQQOMKIE2&!^ 10156High SlopeGPS@ obscured by soils050000050000000000kigeca_][YWSSQOMKG4(#S 12152High SlopeGPS@ Brian Head Formation05000004T01-a0000000qomkigec^\ZVVTRPNJ4(# 81Low slopeGPS@ Claron Formation, Red Member0600000300T00T0000pnljhfdb`^\XXVTRPL." 470Low levelGPS@Claron Formation, Red Member07002000200P0000000trpnljhfdb`\\ZXTRN0$7 10119InterfluveGPS@Claron Formation, White Member1-a0000041-b004001-b0000}{ytrpljeaa_][YT4(#L 349High LevelGPS@Claron Formation, White Member0700000200T0000000usqomkigeca]][YWUQ1%   C 4107High SlopeGPSp@obscured by soils03000006001-a0000000ljhfdb`^YWUQQOMKIE2&!   3152Low slopeGPS@Claron Formation, White Member05000005T0P00T0000usqomkigeca]][YWUQ1%   + 4100High SlopeGPSb@Brian Head Formation02000008T0T00P0000ljhfdb`^\ZXTTRPNLH2&!  ( 9192MidslopeGPS@Claron Formation, White Member04000002P0040000000vtrpnljhdb`\\ZXVTP0$tLVAL F & V FA few standing dead - of all species, but in general his is a healthy patch of trees.This point is on the break below a cliff band of White Claron. The ground has pink Claron soils and white, small rocks. Many downed trees and branches litter the ground. Thick carpet of ARCAT.Plot is located on the plateau, at the edge of the breaks. This site has a moist ravine running through, with many wet-site understory species. Even away from the ravine, Smilacina is found. Several Picea engelmanii are thriving here. The bristlecone and limber pine are restricted to the edge.This point lies on a large hill slope downslope from a large Red Claron Cliffs formation between two small ridges.This is on a slope above a small drainage. On the ridge above the point is barren red Claron. The trees are tall, robust and healthy (except the standing dead PICENG).Boulders of rhyolitic tuff decorate this plot. The soil is gravelly loam.Rhyolitic boulders dot the surface. A few chunks of volcanic glass are present. A dry, shallow drainage snakes through the plot. The soil is gravelly loam.Area is an open woodland with clumps of trees and a forb understory. Over 1/2 the spruce trees are beetle-killed, standing dead. Soil surface is covered with white limestone rocks and litter.A few clumps of shrubs and trees are invading the meadow in this area. Patches of forbs alternate with patches of grass. A few white limestone rocks are on the surface.This is an area of apparently deep soil and thick, dry meadow vegetation.A gully about eight feet deep goes through the plot and has a few moisture loving plants in it. A few rhyolitic boulders and some volcanic glass are on the surface. Some sheep poop is in the plot.The contour of the terrain focuses a little more moisture here making this site a little more densely vegetated than other areas of this large meadow.This part of the large meadow is quite homogenous. The soil appears deep and free of gravel.LVAL  @ D r ( zr this is a moderately steep hill slope nearly covered with ARCPAT excepting the PINPON and litter-filled areas beneath. There are some standing dead trees and huge fallen dead trees on ground.This point is off of the main ridge near the massive Chessman Ridge. The ARCPAT forms a near blanket, but in the interspaces there is barren ground covered with small rocks.Amazing amounts of downed wood (from big logs to lots of tiny sticks).A few Claron rocks have rolled down from above, but for the most part the tan sandstone rocks in the plot look like Straight Cliffs.This point is midway up a hill slope off of a small drainage off of the main Ashdown Creek. There are a few bedrock blocks exposed, one anomalous PINLON subcanopy tree within the mix of conifers and POPTRE.Very dense woodland of JUNSCO and CERLED with emergent PINPON and PSEMEN here and there. ARCPAT fills in the sunnier openings in the canopy, where there is also some bare soil and rocks exposed. Many sapling JUNSCO filling in the understory.This point is just up from drainage. The tree cover is high, and there is high dead/ downed trees, branches and stumps. ARCPAT is thick in patches.Substrate is likely Wahweep residuum.Plot is located on a narrow terrace between two major stream channels, just upstream of their confluence.Plot is at the base of a steep, sheltered canyon slope. Trees are tall and bean-pole form. Creek is running on edge of plot.Plot includes barren ridgetop where PINLON are concentrated, and more forested N-facing hillside where PINFLE and PSEMEN dominate. Ground is hard-packed Claron on ridge and softer on N-facing slope.Talus/colluvium derived from Pink Claron.Plot is very similar to a "barrens" topography, but the surface has generally larger rocks and is more colluvial in nature. (i.e. this isn't a thin roller-bearing surface over bedrock, but rather deeper material gradually moving downslope).)T W  i  q @U00U 350High LevelGPS@Brian Head Formation030000041-b01-b0000000qomkigec^\WSSQOMKG1% // 30336High SlopeGPS@Wahweep01-a001-amoss, lichen41-a01-a0030000wusqomkidb][MHFD?=4(#.. 16326MidslopeGPS@WahweepT1-a0008T0T001-b0000a_][YTRPNLJHHFDB=;2&!-- 21191MidslopeGPS@ obscured by soilsT000080000020000eca_][YWUSQOOMKIGE2&!,,D 25175High SlopeGPS\@ WahweepT00006001-b0020000`^\ZXVTRMKIGGECA?=4(#++ 32298MidslopeGPS@ Straight Cliffs Formation1-a000005P0P00030000trpnlhfdb`^ZZXVTRM2&!** 5235Low levelGPS@ Straight Cliffs FormationT0000081-a0P00P0000qomkigeca_ZVVTRPNL1% ))R 21261MidslopeGPS@WahweepT1-a00Tmoss, lichens07T0T00020000qomkieca_][WHFDB=;2&!(( 28202MidslopeGPS@Straight Cliffs Formation1-a000008P01-a00T0000usqomkigb`^ZZXVTRM2&!'' 11190Low slopeGPS*@obscured by soilsT0000061-a01-a00030000pnljhdb`[YTPPNLJHF3'"&& 20310MidslopeGPSJ@obscured by soilsT00000900000P0000geca_][YWUSOOMKIGE2&!%% 1204Low levelGPS@alluvium030000030200300P0000ca_][YWUQOKGGECA?;1% $$ 25183Toe slopeGPS@Claron Formation, Red Member1-a00000302003001-b0000}{ywupnlhfb^^\ZXVQ3'"## 26339High SlopeGPS@Claron Formation, Red Member030000031-a00300P0000{ywusqomigb^^\ZXVR4(#"" 32300MidslopeGPSR@talus/ colluvium/ landslideP00001-a0500400P0000vtrpnljhdb^YYWUSQO2&!P LVAL^~ d This point is directly off of the main park road. There is a fair amount of barren ground with some larger rocks and many smaller rocks scattered throughout. The microtopography undulates into very small rolling hills, but it is a generally flat dry grassland meadow.This point is high up on a steep hill slope above upper Ashdown Creek. There are some standing dead trees within this forest and many wind thrown trees. The ground is heavy with litter and there is a band of bedrock cliff (short) exposed.This slope is midway down slope off of the ridge west of Ashdown Creek. The POPTRE are healthy and of uniform height. The ground is covered in litter and dead / downed trees. 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"!#"$#%$&%'&(')(*)+*,+-,.-/.0/102132435465768798:9;:<;=<>=@>A?B@CADBECFDGEHFIGJHKILJMKNLOMPNQORPSQTRUSVTWUXVYWZX[Y\Z][^\_]`^a_b`cadbecfdgehfigjhkiljmknlompnqorpsqtrusvtwuxvywzx{y|z}{~|}~ۀہۂۃۄۅۆۇۈۉۊۋیۍێ      !"#$%&'()*+,-./0123456789:;<=>?@ABCDEFGHIJKLMNOPQRSTUVWXYZ[\]^_`abcdefghijklmnopqrstuvw x y z { |}~܀܁܂܃܄܅܆܇܈܉܊܋܌܍܎ !"#$%&'() * + , - ./0123456789:;<=>?@ A!B"C#D$E%F&G'H(I)J*K+L,M-% Y/$N///// Y D Y 9 Y t Y A Y cd Y  Y td Y h2Y Y   Y  r Y t Y e Y nd Y  i Y   Y  e Y a Y a Y  Y  Y  Y  Y  AACodeSiteNameUSGSQuad State CountyParkCodeGPSFileNameGPSUnitUTMEastingUTMNorthingUTMZoneDiffCorrected DatumPDOPUTM Error InParkGPSCommentsRepresentPWPRepresentATD,ClassificationCommentsPlotShapePMUSMUTMUYYYY.rDParkCodePlotCodePrimaryKeyv1b@ Zk+PI)LVAL L 2 \The Elymus and the Poa pratensis have about equal cover and are mixed together fairly evenly, so I listed both names as possibilities. The forb mix fits the primary name best and it seems as though this site was probably never mesic, considering its topographic position. The also abundant Poa fendleriana is restricted to the highest part of the slope.Keys easily as P. pratensis is the dominant grass by far, although there is a fair amount of P. fendleriana in the NE section of the plot.Although Poa pratensis appears to be the dominant grass here, there is a nearly equal amount of Poa secunda.This was a tough call between forest or herbaceous types as tree cover is only about 7% and Ribes and Ligusticum both have high cover. The herbaceous layer is dominant. I guess I would weight the forest type as higher priority.Site keys easily to the association.Keyed easily to association. There is a fair amount of Elymus trachycaulus here, but Bromus is the overwhelming dominant species.I haven't toured much of this large polygon. AT note: Added ABILAS name because there is ABILAS present, and it is such a strong indicator that it trumps the ABICON.Good fit for both. AT note: Added ABILAS name because there is ABILAS present, and it is such a strong indicator that it trumps the ABICON.This plot represents the polygon well, as far as I have seen it.The aspen here deserves mention, thus the second name. There are no tall forbs here.Site keys easily and is similar to other points I've visited in this polygon.I can't see much of the polygon in the thick forest. AT note: Added ABICON-POPTRE alliance name because there was 10% dead POPTRE in plot, which was live POPTRE when aerial photos were flown.There is not quite as much tall forb cover in this plot as what I can see in surrounding areas.About half the herbaceous layer here is Bromus ciliatus, perhaps due to the large openings the forest canopy at this spot.s'Nu  8 \[(֟?CEBR_AA.0024North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372FairFair@Circularvoie^PJ=9- ?(D?CEBR_AA.0023North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.59999990463257FairGood@Circularvoie^PJ=9- ?(w?CEBR_AA.0022North Boundary CEBRBrian HeadUTIron CountyCEBRAA_POINT.corGeoXM12SNAD83GoodGoodD@Circular}wqqqqjje^PJ=9- )?CEBR_AA.0021North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628FairFair@ Circularvoie^PJ=9- ?)?CEBR_AA.0020North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372GoodGoodThis site keys easily.Circularvoie^PJ=9- ?()?CEBR_AA.0018North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372GoodGood@ Circularvoie^PJ=9- ?'?CEBR_AA.0017North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.29999995231628UnknownFair@ Circularvoie^PJ=9- ?&?CEBR_AA.0016North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.90000009536743GoodFair@ Circularvoie^PJ=9- ?&?CEBR_AA.0015North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743GoodGoodH@ Circularvoie^PJ=9- ?]&g?CEBR_AA.0014North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.90000009536743GoodGood@Circularwpjf_QK>:. ?G ƞ?CEBR_AA.0012North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.79999995231628UnknownGoodL@Circularqjd`YKE84( ??CEBR_AA.0010North Boundary CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257GoodGood@Circularwpjf_QK>:. ?=!8?CEBR_AA.0009North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodGood@Circularqjd`YKE84( ?z?CEBR_AA.0007North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.69999980926514UnknownFair@Circularqjd`YKE84( ?!7?CEBR_AA.0006Rattlesnake TrailBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodGood@Circulartmgc\NH;7+ ?s2?CEBR_AA.0005North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.59999990463257UnknownGood@Circularqjd`YKE84( ?"?CEBR_AA.0003Rattlesnake TrailBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.69999980926514GoodGood@Circulartmgc\NH;7+ ?!z?CEBR_AA.0002Rattlesnake TrailBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8315.1999998092651FairFair@Circulartmgc\NH;7+ LVAL  T 6 H "TZ$tGood fit to both; even though there is a high cover of SALARI, the vegetation is dominated by CARAQU.This is only a pretty good fit to primary name because though it is dominated by LIGPOR, there are no other tall forbs present, only short forbs (SOLMUL). The rest of the polygon lacks the density of LIGPOR that this point has, so it is only a fair representative. The rest of the polygon is SOLMUL Herbaceous Vegetation mixed with some LIGPOR.Fits well to both name and fairly well to polygon. This plot has high cover of SOLMUL. Polygon has pockets of high LIGPOR and ACOCOL near the tree islands.The cover of DASFRU and CARSCI are close in value so I added both names. Primary name is good because of CARSCI cover and it mentions DASFRU as being present but few. Secondary name has shrub and mentions Poa pratensis but not the other grasses present.Good fit to both - has most of the species mentioned, though definitely dominated by CARAQU and SALARI.The name is good because it mentions that the RIBMON is often patchy (like here) and that herb cover is typically 10-50% (like here). Other shrubs mentioned are present as well. Very sparse tree cover since I did not add dead PICENG and forest is recovering from beetle kill.Good fit to both even if RIBMON cover is low and the herbaceous cover is very high (as described for this association).Good fit to both for species present and abundance, but description does not mention the drier, rocky ground cover with high bare soil exposed.With the exception of the anomalous draw, the Poa is the dominant vegetation here.With the Claron exposures in this meadow come the distinct species associated with the secondary name. The primary name describes the polygon vegetation overall, as well as its geology (see Environmental Comments).This anomalous area was probably too small to map separately. The remainder of the plot fits the primary named association well (about 40%).Good fit to both name and polygon.D N x (_*T,?CEBR_AA.0046East Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.09999990463257GoodFair@Circularunhd]OI<8, ?(Y?CEBR_AA.0045North View PointBrian HeadUtIron CountyCEBRAA_POINT.cor 12NoNAD830GoodGood@Otherztnnnlea][MG:6* ? ?CEBR_AA.0043North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodFair@Circularqjd`YKE84( ?+?CEBR_AA.0042East BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.20000004768372GoodGood@ Otherpic_XJD73' ?X؞?CEBR_AA.0041North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.20000004768372FairGood|@Circularqjd`YKE84( ??CEBR_AA.0040North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.90000009536743FairFair@Circularqjd`YKE84( ?ݞ?CEBR_AA.0038North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.40000009536743GoodGood Good fit.Circularqjd`YKE84( ?v*?CEBR_AA.0037North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372FairFair@ Circularqjd`YKE84( ?*?CEBR_AA.0036North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5FairGood6@ Circular|vvvqjd`YKE84( ?C)?CEBR_AA.0035North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodFair@Circularqjd`YKE84( ?+?CEBR_AA.0034East Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5GoodGood@Circularzzzunhd]OI<8, ?s,?CEBR_AA.0033East Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.40000009536743GoodFair&@Circularunhd]OI<8, ?*ǟ?CEBR_AA.0032North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743GoodGood@Otherqjd`YKE84( ?)?CEBR_AA.0030North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodFair@Circularqjd`YKE84( ?)?CEBR_AA.0029North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743GoodGood Good fit to both - easy to keyCircularqjd`YKE84( ?(m?CEBR_AA.0028North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743FairGood@Circularvoie^PJ=9- ?'(?CEBR_AA.0027North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372GoodGoodKeys easily to association.Circularvoie^PJ=9- ?)%?CEBR_AA.0026North BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodGoodGood fit to both.Circularqjd`YKE84( ?LVAL * &I'm wondering if this shouldn't key to PSEMEN / ARCPAT; it's on Claron, but there's significant duff and the canopy is not particularly sparse.This site would fit the description better is the dead spruce were alive.The primary name is a good fit due to the high cover of ACHLET but key does not mention the forbs ERIUMB and POTHIP which are abundant; therefore, I added the second name.The trees don't really want to be here. They seem like an ecotonal intrusion. If they are to be considered, my third choice, the made-up name, could include the trees and the sparse herbaceous plants found in this habitat.The point is representative of the polygon but it could really fit into either name since ACHLET, ERIUMB, POHIA are the dominant species throughout.This point represents the gently sloping meadow area between tree islands well. There is a fair amount of ground exposed in the dry meadow and forbs dominate (ERIUMB, POTHIP). Some RIBMON is within the plot but not enough to be named that. Diverse grasses as well here. AT note: Added Ribes name because of Environmental comments about other areas in the polygon having Ribes scattered in them.A narrow plot was used to fit the polygon. The Ericameria comes and goes in clumps in this polygon. This point happened to include a clump.This polygon is a real jumble but the Abies concolor is scattered throughout. AT note: Added ABILAS name because there is ABILAS present, and it is such a strong indicator that it trumps the ABICON.This primary name is good for the rim of the breaks and the high slope off of the breaks, but downslope and south in the polygon it is New: PICPUN / ARCPAT Forest, with high cover of PICPUN.Some areas of this polygon are PINLON / Sparse and some are the primary name, and some are the primary name with large areas with little ARCPAT (patchy). AT note: Added PINLON name because of comments about other areas in the polygon.&g / k )JV-!!7?CEBR_AA.0069Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8313.6999998092651FairGoodZ@Circularohb^WIC62& ?`!!?CEBR_AA.0068Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.69999980926514FairPoor@Circularohb^WIC62& ?*R?CEBR_AA.0067North BreaksBrian HeadUtIron CountyCEBRAA_POINT.cor 12NoNAD830GoodGood@Circularvpjjjha]YWIC62& ? !Ԛ?CEBR_AA.0066Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834FairGood^@Circular}wqqqohb^WIC62& ?u+x?CEBR_AA.0065North EntranceBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.59999990463257GoodGoodThis spot fits like a glove.Circularqjd`YKE84( ?R-Û?CEBR_AA.0061Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372FairGood@CircularzsmibTNA=1 ?-p?CEBR_AA.0060Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743FairFair@CircularzsmibTNA=1 ?R-?CEBR_AA.0059Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.30000019073486FairGood\@CircularzsmibTNA=1 ?-̜?CEBR_AA.0058Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.90000009536743GoodFair@OtherzsmibTNA=1 ?k+?CEBR_AA.0056North EntranceBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodFair|@Circularqjd`YKE84( ?-?CEBR_AA.0055Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5GoodFairF@CircularzsmibTNA=1 ??CEBR_AA.0054Adams BarrierBrian HeadUtIron CountyCEBRAA054WGPS III+12YesNAD8307GoodGood@Circular}wqqomf`\RJD73' 0?CEBR_AA.0053Adams BarrierBrian HeadUtIron CountyCEBRAA053WGPS III+12YesNAD8308GoodGood@Circular}wqqomf`\RJD73' ?D?CEBR_AA.0052Adams BarrierBrian HeadUtIron CountyCEBRAA052WGPS III+12YesNAD8308GoodGood@ Circular}wqqomf`\RJD73' ,A?CEBR_AA.0050North EntranceBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.20000004768372GoodFair@Circularqjd`YKE84( ? .ϝ?CEBR_AA.0049East Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.59999990463257GoodFairV@Circularunhd]OI<8, ?*\?CEBR_AA.0048North EntranceBrian HeadUtIron CountyCEBRAA_POINT.cor 12NoNAD830FairFair@Circularxrllljc_[YKE84( ?.3?CEBR_AA.0047East Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743GoodFair(@Circularunhd]OI<8, ?LVAL ,j$ v2At this point, fobs have about 2x the cover of grasses, with Solidago and Penstemon rydbergii as co-dominants, and Poa pratensis following close behind.Areas to north in same polygon have dominant PICPUN.This point is somewhat anomalous to the polygon and non-homogenous itself. The geology is volcanic gravel as opposed to lake sediments like most of polygons, causing different vegetation. The point itself has characteristic soil of both types, so the Poa pratensis is found off the ridge summit where soil is better developed. Potentilla is a conspicuous species throughout point. AT note: Added two names because this point is borderline between a native and non-native herbaceous dry meadow.This point keyed fairly easily, although the nearly equal cover of Poa pratensis gave me pause momentarily. Poa pratensis is the dominant grass in some areas of this polygon.I'm not sure there is enough Ribes here for a shrubland. The herbaceous layer has about 4x more cover. Also, the Ribes description doesn't mention any herbaceous species at all as associates. The primary name is probably more accurate.This site doesn't fit the description perfectly - some of the associated species listed in the key aren't present and some clumps of trees are invading, but this seems to be the best choice.This point did not key easily. Poa fendleriana is the main grass, but shares dominance with Eriogonum umbellatum. Grasses and forbs have about equal cover, so I keyed both ways. I ended up adding a new name to include the Poa fendleriana. AT note: Added Ribes name because of the presence of Ribes in plot, and it was clear that the mapper was pulling out the Ribes signature from an otherwise herbaceous surroundings.Really PSEMEN / JUNCOM? AT note: Added secondary name because of species list and above comment.Really a PSEMEN woodland/forest? AT note: Added secondary name because of species list and above comment.LVAL( :Lots of PINLON here - if given the priority in the tree species hierarchy, this could easily be keyed as a PINLON / ARCPAT (if such an association existed). But this is not a "barrens" community, although it is on talus derived from the Claron. AT note: Added PINLON and ABICON names because of above notes and fairly equal tree cover among species (all low).A tossup between the spruce and white fir for dominance here. AT note: Added 3rd name because ARCPAT is present here also, and both JUNCOM and ARCPAT have really low cover.Plot is on the bottom edge of an active colluvial slope, and has fewer trees, more shrubs, and more rock cover that the majority of polygon. Areas in polygon downslope of plot probably include a higher percentage of PINLON and continue to have more PICPUN than ABICON. The ARCPAT appears to be dominant throughout area. AT note: Added PINLON and ABICON names because of above comments describing other areas in the polygon (higher up the slopes) as being dominated by these tree species.I had to binocular this plot from 70m above. The 43degree slope alternating with cliff bands is way beyond my comfort level. Nevertheless, I 'm confident in this call. The bristlecone trees are distinctive and in plain view.The majority of this long, skinny polygon is scoured wash channel, with small terraces similar to plot occurring irregularly and sparsely along the edges. This plot is exception for an area so far up the drainage system, in that it is quite extensive and has a large number of the characteristic POPANG.Although Elymus trachycaulis has a good showing here, Poa pratensis is by far the dominant in this plot. Other areas of polygon have Elymus as the main grass. AT note: Added ELYTRA name because of the comment above and the species list shows this polygon is a toss-up to call either a native or non-native-dominated meadow, when you add up all the native species.~ . _ Mz0\G+%?CEBR_AA.0096Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8317.6000003814697GoodGood@ Circularslfb[MG:6* ?J k?CEBR_AA.0095Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.80000019073486FairGood@ Circularohb^WIC62& ?8 ?CEBR_AA.0093Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257GoodGood@ Circularohb^WIC62& ?l-?CEBR_AA.0092Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.29999995231628GoodGood&@ CircularzsmibTNA=1 ?-?CEBR_AA.0091Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372FairGood@ CircularzsmibTNA=1 ?t,?CEBR_AA.0090Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8312.6999998092651GoodGoodGood fit to both.Circularnga]VHB51% ?+?CEBR_AA.0088Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.19999980926514GoodGood`@Circularnga]VHB51% ?t,?CEBR_AA.0087Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD837.69999980926514GoodGood@Circularnga]VHB51% ?+0?CEBR_AA.0084Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodGoodr@Circularnga]VHB51% ?+?CEBR_AA.0083Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8315.3000001907349GoodGood@Circularnga]VHB51% ?)?CEBR_AA.0082Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodGood@Circularnga]VHB51% ?+ ?CEBR_AA.0081Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.80000019073486GoodGood@Circularnga]VHB51% ?,=?CEBR_AA.0079Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.90000009536743GoodGoodZ@Circularnga]VHB51% ?,?CEBR_AA.0078North EntranceBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832GoodFairn@Circularysssqjd`YKE84( ?-ʚ?CEBR_AA.0076Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5FairGood@OtherzsmibTNA=1 ?-?CEBR_AA.0075Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.09999990463257GoodGood2@CircularzsmibTNA=1 ?j!?CEBR_AA.0073Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.40000009536743FairGoodh@Circularohb^WIC62& ?2 ?C"Ә?CEBR_AA.0123North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8312.5GoodFairJ@Circular{tnjcUOB>2 ?!Ɨ?CEBR_AA.0121East of Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628GoodGoodr@Circularwpjf_QK>:. ? ?CEBR_AA.0119Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835UnknownGoodv@Circularzqqqohb^WIC62& ?$?CEBR_AA.0118Ashdown Creek- North ForkBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8319.6000003814697Difficulty getting satellites.UnknownGoodd@Circular|uokdVPC?3 ?$.?CEBR_AA.0115North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodPoor@Other{tnjcUOB>2 ? ?CEBR_AA.0114The QuarryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372FairFair<@Circularmf`\UGA40$ ?*p?CEBR_AA.0113Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD838.39999961853027GoodGood^@Circularslfb[MG:6* ?!?CEBR_AA.0111East of Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.09999990463257GoodGoodPerfect fit.Circularwpjf_QK>:. ? ?CEBR_AA.0110East of Adam's CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12NoNAD834.59999990463257GoodFair@Circularvokg`RL?;/ ?B!:?CEBR_AA.0109East of Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodGoodPerfect fit.Circularwpjf_QK>:. ?2 ?P#?CEBR_AA.0101North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.70000004768372GoodGoodGood fit to both.Circular{tnjcUOB>2 ?U?CEBR_AA.0099Spring Creek HeadwatersBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.30000019073486GoodGood@CircularzsmibTNA=1 ?-J?CEBR_AA.0098North Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743FairFair|@Othervoie^PJ=9- ?-?CEBR_AA.0097Northeast Park BoundaryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.5FairFair@OtherzsmibTNA=1 ?pLVAL z02&Plot may have slightly less canopy cover than rest of polygon, with open areas filled in with possibly slightly more CERMON than usual.Good fit. Huge Picea are limited to the drainage bottom and sides; they don't represent upslope areas of polygon.Good fit. Understory varies a bit in polygon- some areas have JUNCOM dominance.Lots of POPTRE here- a couple open areas in canopy have POPTRE stands, and they've also invaded the conifer understory. Canopy in general is more open than usual in polygon. A number of dead trunks are standing or on the ground, of several species of conifer.Good fit to both. AT note: Added 2nd name because CERLED is the dominant tree, even though evergreen cover is higher than 10%.I like first name because both trees are dominant, but description caps shrub layer at 6%, whereas point has 33% ARCPAT, so secondary name could fit really well too.Plot appears a good representation, but I haven't walked through upslope areas of polygon. The POPTRE, however, are clearly limited to the downslope portions close to the drainage floor.Point shaped to fit polygon. This polygon is essentially devoid of vegetation, and is regularly scoured by flash flooding. The entire sum coverage of vegetation within the plot is perhaps three square feet- amounting to very occasional herbaceous erratics on temporary terraces of limited extent. Note that this polygon is detached from main drainage polygon.The Pinus longaeva is not present in much of the polygon, but a large percent of the plot. The variety and quantity of tall conifers in this polygon seems unusual for the JUNSCO-CERLED association, but it seems to fit the key. The area appears to have once had a higher percent of tall conifers to the juniper and CERLED, but no longer& AT note: Added 2nd name because this plot could key to this name, given the dominance of CERLED over any individual conifer species. Believe this was a missed secondary call by the person in the field.r.\ 0 P s'Oo["˖?CEBR_AA.0149North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.70000004768372FairGood@ Circular{tnjcUOB>2 ?["?CEBR_AA.0148North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.29999995231628FairGood Good fit.Circular{tnjcUOB>2 ?Q";?CEBR_AA.0147N. Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8310.1999998092651UnknownFairF@Circularxqkg`RL?;/ ?V#?CEBR_AA.0145Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8313.6000003814697FairGood@Circularslfb[MG:6* ?!2?CEBR_AA.0144Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.09999990463257GoodGoodR@Otherslfb[MG:6* ?-?CEBR_AA.0143E. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.29999995231628GoodFairt@Circulartmgc\NH;7+ ?$?CEBR_AA.0141North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.30000019073486FairFair@Circular{tnjcUOB>2 ?C&Ǘ?CEBR_AA.0140North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.09999990463257GoodFair@Circular{tnjcUOB>2 ?I%?CEBR_AA.0139North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.5GoodGood Good fit.Circular{tnjcUOB>2 ?`-?CEBR_AA.0138Alpine Pond TrailheadBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743GoodPoor6@Circularxqkg`RL?;/ ?e-?CEBR_AA.0137Alpine Pond TrailheadBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628UnknownPoorN@Circularxqkg`RL?;/ ?U!?CEBR_AA.0135East of Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.5GoodFair@Circular|||wpjf_QK>:. ?%O?CEBR_AA.0134North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8316FairGood4@Circular{tnjcUOB>2 ?$ŗ?CEBR_AA.0133Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8311.5GoodGoodGood fit to both.Otheryyyslfb[MG:6* ?%?CEBR_AA.0132North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372FairGood@Circular{tnjcUOB>2 ?V?CEBR_AA.0130The QuarryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8311FairGood Good fit.Circular}wqqqmf`\UGA40$ ?|?CEBR_AA.0128The QuarryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.09999990463257PoorFair@Circularmf`\UGA40$ ?3?CEBR_AA.0127The QuarryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.90000009536743FairGood@Circularmf`\UGA40$ ?TLVAL . X,vGood fit. Open spot in canopy (exposed bedrock) reduces average % over plot of tree cover.There are patches of POPTRE throughout polygon like at this point. There are also large areas without POPTRE, therefore I added secondary and tertiary names. I used both secondary and tertiary names because the shrubs were co-dominant.Good fit to both. Plot follows drainage.Good fit to both though most of the PICENG canopy is dead.Areas of polygon upslope have denser trees, and likely more % ABICON cover. Plot captures an area with likely thinner soils (some exposed bedrock) and thus thinner trees in general, and more ARCPAT. ARCPAT is probably still the dominant in the rest of the polygon, however. Nearby areas with bedrock exposure are really more of PINPON/ARCPAT association without significant ABICON. AT note: Added 2nd name because of above notes about nearby areas in polygon being more PINPON-dominated.Primary name is an okay fit, but the presence of the ACEGLA is actually what appears definitive of the understory. There is an ABICON/ACEGRA association in key, but I'm quite sure that the species here is glabrum. Perhaps the association should be Acer spp.?It's a stretch to call this a forest, but there are too many trees to call it a meadow. With all the baby trees growing, maybe this is more of a prophecy.The beetle kill, logging and burning have altered this site enough to make it a poor fit to the association description, although it still seems to be the best choice.A combination of all three names would be the best fit here. Not enough PINPON to call that the canopy dominant, and too much ARCPAT to feel good about secondary name. AT note: Replaced tertiary call of field person (PINPON/CERLED/ARCPAT) with ARCPAT shrubland because of notes and high ARCPAT cover to the relatively low tree cover.Seems a fair representation of this part of polygon. Shrub understory is a mix, but JUNCOM seems the most dominant. The maple appears limited in extent.NLVAL  4 h>rr.rI think primary name is best fit, but if PSEMEN cover is too low, then secondary name is best.Good fit to both for primary name.Viewed point within same polygon I'm in, ~270 meters away at 64 degrees, but was easily done with binoculars because it is on the opposite slope facing me. Good fit with name.Plot shaped to fit polygon. Good fit. Populus is dense on terraces, but % appears lower over whole plot.Good fit to both, description says that other trees may be present with generally less than 10% cover.There are areas within this polygon that have a much higher POPTRE cover. This point has more mixed conifers and less ARCPAT. JUNCOM is dominant in the shrub layer and description states that both ARCPAT and JUNCOM can dominate.This is definitely a polygon drawn around the POPTRE dominated woodland. The amount of ABICON seedlings and subcanopy make me think this will eventually be a POPTRE-ABICON/ARCPAT forest. The ARCPAT is nearly as abundant as the JUNCOM which is mentioned in the secondary name.The Cedar Breaks key takes me to couplet 30 in the Woodland section (PJ woodlands), where 30b suggests that the association for this plot is not described for CEBR. The key refers me to the BRCA key - where the above association is also missing. What the BRCA key does offer is a PINEDU - JUNOST/CERLED association - but the Juniper here is all scopulorum.Good fit. I haven't seen much of this polygon, but it appears similar to its neighbor where I just did two plots.Neither of the shrubs are dominant, so I added both names. This is a diverse forest with ABICON, having slightly more cover and is a more diagnostic species. Areas within polygon have higher cover of POPTRE.The primary name fits fairly well though JUNCOM is not abundant but does dominate this sparse understory. The conifers are very mixed, I chose an ABICON name since it is so diagnostic and fairly abundant. The POPTRE may be anomalous in rest of polygon, I haven't walked through much of it.(Es  5 L Bl$(?CEBR_AA.0169Chessmen RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD837.90000009536743UnknownFair@Circularqjd`YKE84( ?(ϕ?CEBR_AA.0168North of Chessmen RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.90000009536743GoodFair@CircularzsmibTNA=1 ?^"?CEBR_AA.0167Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodGood@ Circularqjd`YKE84( ?-?CEBR_AA.0165Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.19999980926514GoodGoodGood fit to both.Circularnga]VHB51% ?'_?CEBR_AA.0164Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.19999980926514GoodFair@Circularqjd`YKE84( ?$z?CEBR_AA.0163Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8310.3000001907349FairFair@Circularslfb[MG:6* ?F%d?CEBR_AA.0162Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8315.8999996185303GoodGoodD@ Circularslfb[MG:6* ?!v?CEBR_AA.0161North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8327.3999996185303GoodGood Good fit.Circular{tnjcUOB>2 ?)?CEBR_AA.0159N. of Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.09999990463257Offset point 68 meters at 80 degrees because of dangerously steep slope. I am in polygon now with a good view of point.GoodGoodKeyed easily, good fit.Circular>>>>4 wpjf_QK>:. ?*l?CEBR_AA.0158N. of Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.cor 12NoNAD830Marked as updated, but not logged.GoodGood`@Circularrrpiea_QK>:. ?Q?CEBR_AA.0157Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.29999995231628GoodGood@Otherohb^WIC62& ?$?CEBR_AA.0156Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743GoodGood@Circularslfb[MG:6* ?x$?CEBR_AA.0155Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12NoNAD8317.5FairGood@Circular}wwwqjfb[MG:6* ?0$?CEBR_AA.0154Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.5GoodGood*@Circular~xxxslfb[MG:6* ? ?CEBR_AA.0153The QuarryBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257GoodPoor@Circularmf`\UGA40$ ?" ?CEBR_AA.0151North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.80000019073486UnknownGood@Circular{tnjcUOB>2 ?#?CEBR_AA.0150Columbine CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.80000019073486FairFair@Circularslfb[MG:6* ?LVAL. f It's hard to decide what the dominant tree is here. PICPUN is congregating on the flatter terrace near the creek (w/ Equisetum, birch and JUNCOM), whereas there's more of a mix upslope. SYMORE is definitely the dominant shrub in the area, and since there's a fair amount of ABICON, secondary name could work.Polygon includes Claron exposure on the top of this ridge which should be part of the neighboring polygon (PINPON/ ARCPAT). Ridge is very different from 2/3 of the plot which falls on the steep, west-facing slope and is mixed conifer with very little ARCPAT. A split plot form was done to show this. PICPUN is congregating on the lower parts of this polygon near the creek. Secondary name fits ridgetop well, but that's only 1/3 of the plot.Healthy-looking community making a go of it on the less-disturbed rocky terraces of the canyon bottom. Name fits great! Warped plot long and narrow to stay in polygon.This is a confusing plot and none of these names are great fit, therefore I added them all.Included both names because neither is a perfect fit. PINLON too diagnostic to ignore and nearly co-dominant with PICPUN, so it probably should be the primary name. However, I made PICPUN primary only because it has slightly more cover.I added primary name because there is so much of this diagnostic species but really it is a mix of conifers and not sparse. ARCPAT dominates, not JUNCOM, so secondary name is not the best either. Both names are only an OK fit.This polygon varies in the cover of POPTRE, some areas are dominated by it whereas other areas are a mix. This is only a fair representative because PSEMEN cover is quite high relative to both POPTRE and ABICON. The shrub layer is low whereas primary description states moderate to high cover for ARCPAT or JUNCOM. AT note: Added 2nd name because POPTRE cover is described as patchy, and rest of polygon could be more ABICON/(PSEMEN)-dominated and ABICON is more diagnostic than PSEMEN.1/Qo  5 Ka|9cs"E?CEBR_AA.0193Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8310.6000003814697FairFair@Circularqjd`YKE84( ?"n?CEBR_AA.0192Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372FairGood@Circularqjd`YKE84( ?v?CEBR_AA.0191Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.29999995231628GoodGood@Otherohb^WIC62& ?&!~?CEBR_AA.0189North of the MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257FairPoorV@Circularwpjf_QK>:. ? ?CEBR_AA.0188North of the MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.09999990463257UnknownGoodt@Circularwpjf_QK>:. ??CEBR_AA.0187North Fork Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.cor 12NoNAD830Point checked as updated, not logged. Actual point is inaccessible.GoodGood@OthervvtmiecUOB>2 ??CEBR_AA.0186Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743FairPoor@Circularpic_XJD73' ?"F?CEBR_AA.0185Chessman CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743GoodGoodPerfect fit.CircularrkeaZLF95) ?D"?CEBR_AA.0183Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.09999990463257GoodGoodGreat fit to both!Circularqjd`YKE84( ?"?CEBR_AA.0181Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8315.6000003814697GoodGoodGreat fit to both.Circularqjd`YKE84( ?)$U?CEBR_AA.0180Chessman CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.09999990463257GoodGoodPerfect fit.CircularrkeaZLF95) ?#>?CEBR_AA.0178Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8319.5GoodGood6@Circular}wwwqjd`YKE84( ?O?CEBR_AA.0177Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12NoNAD8366.3000030517578FairPoor@Circularngc_XJD73' ? k?CEBR_AA.0176Meadows Hill/ ConfluenceBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodGood@Circular{tnjcUOB>2 ?> ?CEBR_AA.0175Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.20000004768372UnknownPoorl@Circularpic_XJD73' ? Q?CEBR_AA.0173Meadows Hill- south endBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD8310.6000003814697UnknownPoorz@CircularzsmibTNA=1 ?"Z?CEBR_AA.0171Chessmen RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.19999980926514GoodGoodGreat!Circularqjd`YKE84( ??CEBR_AA.0170Adams CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.59999990463257GoodGoodR@Otherohb^WIC62& ?LVAL & 48XGood fit to both. AT note: Added 2nd name because it seemed like a reasonable fit here.Warped plot long and narrow to stay in polygon. Name fits perfectly!Neither association fits well. The POPTRE in plot can be ignored, they're invading polygon from downslope and do not characterize anything upslope of plot. This is closer to an ARCPAT shrubland such as described in the BRCA key, with some emergent trees. Upslope areas have fewer trees than plot.Plot is a good representation of this vicinity. Good fit.Plot shaped to polygon. POPTRE are mostly seedlings on the lower edge of polygon. Most of polygon is bare rock or steep bare mud. Vegetation is limited to a small area of ledges. This polygon should really be included with the major polygon upslope of it (to the S), it's a bedrock outcrop in that mixed conifer forest. AT note: Added 2nd name because all tree species have trace cover, so this name is just as reasonable a choice as primary name.This polygon has been a real mixture of trees, dominance changes rapidly in here, so almost any point is a fair representation. This spot is anomalous because the point landed in a patch of POPTRE. Most of the area outside plot would better fit with secondary name. Unfortunately nothing from the key can be stretched to fit around here.Great fit to both, even though PINFLE cover is relatively high (although PSEMEN does dominate). PINFLE is not mentioned in diagnostic ranking of conifers.Secondary name is a stretch here, but it's the only one from the key that remotely works. Understory definitely has more SYMORE than JUNCOM, and the overstory is nearly co-dominated by PSEMEN and POPTRE. Other areas in the polygon don't have so much POPTRE though.Good fit to both: PICPUN far more diagnostic than PINPON, which is co-dominant. AT note: Added 2nd name because PINPON is the dominant tree, even though PICPUN is more diagnostic. Could get to this name the way the key is written now.LVAL 8T z 4 ".TViewed entire linear terrace polygon. Perfect fit with name.Good fit to polygon. Name is best fit but there are not as many tall forbs present as listed in description.Due to the high cover of POAPRA I decided on that primary name but there is a fair mix of native grasses with ELYTRA being fairly dominant, so I added secondary name. It truly is a mix of grasses here.This point is anomalous with the rest of the polygon, which is a drier grassland meadow without Carex species or standing water. Point is a good representation of description.Good fit to both. This point is best representative of name, while AA201 had more native grasses (could be called ELYTRA name) and AA200 was an anomalous CARAQU point within the polygon.Plot falls right next to anomalous clearing at western edge of polygon, so I warped plot slightly east. JUNCOM is clearly the dominant understory, but it's clear from place to place what the dominant tree is. It's a real conifer mix. Right here, PICPUN is definitely most abundant but at eastern edge of plot, there is more ABICON.Point fits description well and understory is definitely JUNCOM-dominated, though there's a lot of grass here as well. Warped plot to the west to stay in polygon.Fair fit to primary name and rest of polygon is a combination of primary name and JUNSCO-CERLED woodland (which states shrubs <6%, whereas in polygon ARCPAT is 25-35%). Only a fair fit because there is so much POPTRE and other conifers.This is only a fair representation to name because description states shrubs can only be up to 6%, whereas throughout polygon ARCPAT is ~30%. PINPON and POPTRE had high cover to the east of point (AA194), but not here (but they are present).This is a good fit to primary name because PINPON dominates despite the relatively high cover of JUNSCO (secondary name was therefore added). Secondary name caps shrub cover at 6% though, whereas ARCPAT cover in polygon is ~30%.*Z  9 W ~Kx,)?CEBR_AA.0218Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD839.69999980926514GoodGoodt@Circulartmgc\NH;7+ ?+,?CEBR_AA.0217Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.19999980926514GoodFairj@Circulartmgc\NH;7+ ? (?CEBR_AA.0215The MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD837.69999980926514GoodPoor2@Circularnga]VHB51% ?E?CEBR_AA.0214Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5GoodGoodz@ Other{uuupic_XJD73' ?--?CEBR_AA.0213S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD839.10000038146973GoodFair@Circulartmgc\NH;7+ ?B?CEBR_AA.0211Shooting Star Ridge (east)Brian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257GoodGoodGood fit to both.Circular}vpleWQD@4 ??CEBR_AA.0209Shooting Star RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.80000019073486FairFair&@Circularvoie^PJ=9- ??CEBR_AA.0207Shooting Star RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12NoNAD834.09999990463257GoodGoodd@Circulartmie^PJ=9- ?&,?CEBR_AA.0206S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodGoodGood fit to both.Circulartmgc\NH;7+ ?,g?CEBR_AA.0205S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372GoodFairf@Circulartmgc\NH;7+ ?e"?CEBR_AA.0204Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodGood Great fit!Circularqjd`YKE84( ?N,?CEBR_AA.0203S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.59999990463257GoodGood@Circulartmgc\NH;7+ ?,0?CEBR_AA.0201S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.59999990463257GoodFair@Circulartmgc\NH;7+ ?,ӓ?CEBR_AA.0200S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257PoorGood`@Othertmgc\NH;7+ ?,&?CEBR_AA.0199S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5GoodGoodv@Otheryyytmgc\NH;7+ ?B k?CEBR_AA.0198The MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.69999980926514FairFair@Othernga]VHB51% ?d Ҕ?CEBR_AA.0197The MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.19999980926514GoodGoodF@Othernga]VHB51% ?"r?CEBR_AA.0194Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.80000019073486FairFair@Circularqjd`YKE84( ? LVAL 6  t|>Polygon looks like it captures an area with dense ARCPAT and few trees, plot shape was molded to stay in polygon. It includes flatter area at top of slope (primary name) where PSEMEN and PINPON dominate, as well as the incredibly steep slope (north) where ABICON dominates and there's very little understory. AT note: Added ARCPAT name because of the incredibly high ARCPAT cover to the relatively low tree cover.Good fit to both even though there is a higher cover of RIBMON than described for primary name and in open areas there are more short forbs than tall, where the trees are, there are tall shrubs.Good fit to both, although more seedlings than tall forbs.This is only a fair representative of description because it does not mention RIBMON which is present but it does mention the tall forbs and co-dominant nature of POPTRE and ABILAS.Nothing from the key fits here. There is a lot of ABICON, but most of it is still quite young and PICPUN trees tower above them. There is not an ARCPAT shrub in sight either, so I wasn't tempted by the POPTRE/ABICON/ARCPAT name. JUNCOM is the overwhelmingly dominant understory.This is a giant polygon, so not sure how about the whole thing, but there are large areas with different tree species dominant. Here on the flatter area, PINPON and PSEMENT dominate. On the steep slope to the north, ABICON takes over, and toward the bottom of the slope (near the creek), PICPUN is dominant. This shouldn't all be part of the same polygon. Too much JUNCOM for names to be a good fit.Higher up on the ridge there is more PSEMEN and less ABICON, but name fits great here. I haven't seen the whole polygon, but it seems like ABICON is at least present everywhere.This point is a mixture of SOLMUL, PENRYD, and POTHIP as dominants, so I listed both names. Primary name is good because it mentions more of the species present like PENRYD, ACHLET, and ELYTRA. Secondary name is for the abundance of POTHIP here, but point lacks ERIUMB which should be present or dominant."Jx  A h,X,?CEBR_AA.0239S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.5GoodGoodT@Circularyyytmgc\NH;7+ ??CEBR_AA.0238Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.59999990463257GoodGoodV@Circularpic_XJD73' ?!>?CEBR_AA.0237The MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628GoodPoor@Circularnga]VHB51% ?"6?CEBR_AA.0236Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12NoNAD835.59999990463257GoodGood(@Circularohd`YKE84( ?K?CEBR_AA.0235Shooting Star RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.90000009536743GoodGood@Circularvoie^PJ=9- ?"?CEBR_AA.0233Chessman RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.29999995231628GoodGood @Circularqjd`YKE84( ? z?CEBR_AA.0232Meadows HillBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.29999995231628GoodGood@Otherohb^WIC62& ?)J?CEBR_AA.0231Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD835.30000019073486GoodGood Good fit.Circulartmgc\NH;7+ ?2+ۑ?CEBR_AA.0229S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.90000009536743PoorGood@Othertmgc\NH;7+ ?*}?CEBR_AA.0228S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.59999990463257GoodGood@Circulartmgc\NH;7+ ?{+?CEBR_AA.0227Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD839.39999961853027GoodGood@Circulartmgc\NH;7+ ?,?CEBR_AA.0226S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628GoodGoodx@Circulartmgc\NH;7+ ?`!?CEBR_AA.0225The MeadowsBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628GoodFair@Circularnga]VHB51% ?*?CEBR_AA.0223Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628FairGood@Circulartmgc\NH;7+ ?*}?CEBR_AA.0222Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.79999995231628FairGood@Circulartmgc\NH;7+ ?)ݓ?CEBR_AA.0221Ashdown CreekBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.40000009536743GoodPoor@Otherpic_XJD73' ??CEBR_AA.0220Shooting Star RidgeBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodFair>@Othervoie^PJ=9- ?,?CEBR_AA.0219Chessman Overlook AreaBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD839.89999961853027GoodGood@CircularyrlhaSM@<0 ? LVAL  P H ..Good fit to both because even though there is not DESCAE, description mentions disturbed sites without DESCAE but having POAPRA.Viewed entire small, irregularly-shaped polygon. Keyed easily, good fit except no mention of ARCPAT in the description.Had to make plot long and narrow to stay in polygon. Pretty homogenous polygon except area to the SE has no CERLED. PINPON is clearly more dominant than ABICON, but I felt obligated to give secondary name because of ABICONs indicator value.This point is a good representative of primary name but rest of polygon is the ARTCAN name. Made plot an oval shape, from centroid stretching NE to SW. AT note: Added ARTCAN name because of above note, stating it as being more common in rest of polygon.Good fit to both. AT note: Added 2nd name because of high POAPRA cover, this plot could've been called either name.Good fit to both, fits into the cover % listed in description. Has some open areas which lack RIBMON and is dominated by short forbs, but where trees are there is RIBMON and tall forbs. AT note: Added 2nd name because plot fell in a less representative part of polygon where conifer cover was high relative to POPTRE cover. Most of polygon captured higher POPTRE cover.Good fit to both. At point there is a high cover of STILET.It was difficult to decide between primary and secondary name, both could work here. Trees are pretty sparse on this slope and it's tricky to say if PINPON is truly dominant. AT note: Added ARCPAT name because of low tree cover relative to high ARCPAT cover.Polygon grades from ELYTRA to ACHLET-dominated grassland. Forbs have high cover throughout polygon.Good fit to primary name even if POAPRA is relatively high. The polygon grades from ACHLET-dominated to ELYTRA-dominated.Polygon is fairly small and plot covers most of it. POPTRE and ABICON are nearly co-dominant, and JUNCOM and SYMORE are co-dominant in the understory. Nothing from the key fits. I didn't feel comfortable trying to stretch an Abies or Populus name.LVAL 2A narrow plot was used to fit the polygon. I don't know that the Ericameria occurs throughout the polygon. It looks like some of the polygon might key to Eriogonum panguicense Sparse Vegetation. AT note: Added 2nd name because of above comment.Made plot a narrow oval shape to stay within polygon boundaries. Keyed easily, pretty good fit with name except that there's twice the PICPUN cover as PINLON and ARCPAT is not mentioned in the description.Good fit to both. Cover of ARTCAN varies throughout point and polygon. AT note: Added wet Poa pratensis association to MU 36 and it was a reasonable call for this plot.This is the best fit for the point and polygon. POPTRE-ABICON/ARCPAT would be the closest name in the key, but not a good fit since PSEMEN has far more cover than ABICON.This is a ridiculous mix of trees to try to tell what's dominant! The only thing I'm really sure of is the understory! Either name could work here, but neither is very satisfying because of the tree mix.Great fit to both. AT note: Added ARCPAT name because polygon is so small that field person might have added in tree cover that was actually outside polygon boundaries. Polygon clearly captures an ARCPAT-dominated area and high ARCPAT cover given by field person shows that.Good fit to both. AT note: Added ARCPAT name because point fell in a more ecotonal (heterogenous) part of polygon, where tree cover was generally higher than in most of polygon. Environmental comments describe more ARCPAT cover in other parts of polygon.This point has a diverse mix of conifers with ABICON being the most diagnostic and slightly more abundant therefore I went with primary name. AT note: Added ARCPAT name because polygon was so small, it was easy for field person to add tree cover in that was actually outside polygon. Polygon really captures ARCPAT-dominated area and high cover of ARCPAT given by field person shows that.'<` 9bEY+l?CEBR_AA.0262S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.59999990463257GoodGoodGood fit to both.Circulartmgc\NH;7+ ? ?CEBR_AA.0260Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.80000019073486FairPoorV@ CircularrkeaZLF95( ?!?CEBR_AA.0258Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743GoodFair@CircularrkeaZLF95( ? ?CEBR_AA.0257Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.19999980926514GoodGood@CircularrkeaZLF95( ?) W?CEBR_AA.0256Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodGoodv@CircularrkeaZLF95( ?V?CEBR_AA.0254W. of Cresant HollowBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.90000009536743GoodGoodPerfect fit.Circularwpjf_QK>:. ?Î?CEBR_AA.0252Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD833.40000009536743GoodGood@CircularrkeaZLF95( ??CEBR_AA.0251Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.20000004768372GoodGoodT@CircularrkeaZLF95( ?6?CEBR_AA.0250Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743GoodGood@CircularrkeaZLF95( ??CEBR_AA.0249Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD838.39999961853027GoodGoodx@CircularrkeaZLF95( ?n L?CEBR_AA.0247Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.cor 12NoNAD830GPS quit working right as I got here, but I'm sure I'm in the right spot.FairPoor@Circularmmkd`\ZLF95( ? ֎?CEBR_AA.0246Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.80000019073486FairGood8@CircularrkeaZLF95( ? ?CEBR_AA.0245Cresant HollowNavajo LakeUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.90000009536743GoodGoodGood fit, easy to key.CircularrkeaZLF95( ?+U?CEBR_AA.0244S. of Alpine MeadowBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD836.59999990463257GoodGood@ Circularvoie^PJ=9- ?9"?CEBR_AA.0243N. of Chessman CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD834.5GoodGood@ Other}}}xqkg`RL?;/ ?*G?CEBR_AA.0242Chessman OverlookBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.40000009536743UnknownGood@Circulartmgc\NH;7+ ?"Ē?CEBR_AA.0241N. of Chessman CanyonBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.70000004768372GoodGood@Otherxqkg`RL?;/ ?,h?CEBR_AA.0240S. of Alpine PondBrian HeadUtIron CountyCEBRAA_POINT.corGeoXM12YesNAD832.29999995231628GoodGoodGood fit for both.Othertmgc\NH;7+ ?.LVAL  2TViewed entire small, oval polygon. No name in the key for this community type, so I had to make a new name. Included secondary name because it has the right mix of species, but this is not a woodland and only a sparsely wooded shrubland.Good fit even though there is a fair bit of POAPRA.Plot falls near an open area of Claron which is dominated by spruce and scattered JUNCOM. Plot is definitely Picea-dominated, though I walked through areas east of here and upslope which had more ABICON. Acer glabrum is definitely the most abundant understory species, so nothing from the key fit.Hard to tell whether JUNCOM or MAHREP is more dominant, so either name could work here. PINLON tree seems anomalous here.Good fit with either name since the two shrubs are co-dominant in the understory.Good fit, easy to key; though lots of PICPUN mixed in here.Good fit with either name. Plot captures E and W-facing slopes (~22-25 degrees) on either side of this ridge, with ARCPAT more dominant where tree canopy is open and JUNCOM dominant where tree canopy is more closed.Either name could work since the two shrubs are co-dominant in the understory. PINFLE is the dominant, but since the key doesn't care about it I was forced to ignore it.Either primary or secondary name could work since these two tree species are co-dominant (PINLON nearly co-dominant as well). Included tertiary name because ARCPAT cover is nearly co-dominant in the understory.Good fit, easy to key. Denser canopy on this cooler aspect.PICPUN is dominant on the lower parts of plot (near creek) but ABICON dominates the slopes higher up. ACEGLA is creeping up the slope from the creek, but ABICON forest looks like it has a mostly JUNCOM understory.Lower areas of this polygon (by creeks) are very Picea-dominated, whereas higher up on the slopes, there's more ABICON. Here, primary name fits well. AT note: Added 2nd name because the above comment describes ABICON as more dominant on the slopes above the PICPUN-dominated ravine.4`  @ e,Z