08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Argiborolls component makes up 85 percent of the map unit. Slopes are 10 to 25 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from metasedimentary rock and/or colluvium derived from basalt and/or residuum weathered from metasedimentary rock and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 7 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931556"|"29603916"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 45 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931557"|"29603917"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Calciborolls component makes up 40 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931558"|"29603918"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 50 percent of the map unit. Slopes are 10 to 40 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931559"|"29603919"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Calcic Cryoborolls component makes up 35 percent of the map unit. Slopes are 10 to 40 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931560"|"29603920"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Calcic Cryoborolls component makes up 80 percent of the map unit. Slopes are 10 to 25 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931561"|"29603921"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 40 percent of the map unit. Slopes are 40 to 60 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931562"|"29603922"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931563"|"29603923"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 30 percent of the map unit. Slopes are 40 to 60 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931564"|"29603924"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 50 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931565"|"29603925"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 40 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931566"|"29603926"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 85 percent of the map unit. Slopes are 25 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931567"|"29603927"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 80 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931568"|"29603928"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 65 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931512"|"29603872"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Aquolls component makes up 25 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain slopes. The parent material consists of alluvium derived from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 0 inches during April, May, June, July, August. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the R043BP801MT Bottomland Group ecological site.      "|"26931513"|"29603873"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 65 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931510"|"29603870"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryoborolls component makes up 25 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes.  Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931511"|"29603871"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 85 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931569"|"29603929"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryoborolls component makes up 50 percent of the map unit. Slopes are 25 to 40 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931570"|"29603930"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 40 percent of the map unit. Slopes are 25 to 40 percent. This component is on mountain slopes.  Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931571"|"29603931"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrpets component makes up 50 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931572"|"29603932"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 40 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes.  Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931573"|"29603933"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 85 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931574"|"29603934"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 45 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931508"|"29603868"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Calcic Cryoborolls component makes up 40 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 0 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931509"|"29603869"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 85 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931507"|"29603867"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryorthents component makes up 100 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain slopes, mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931506"|"29603866"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 55 percent of the map unit. Slopes are 25 to 40 percent. This component is on mountain slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931575"|"29603935"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 45 percent of the map unit. Slopes are 25 to 40 percent. This component is on mountain slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931576"|"29603936"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 85 percent of the map unit. Slopes are 25 to 50 percent. This component is on mountain slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931577"|"29603937"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Dystric Cryochrepts component makes up 85 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from rhyolite and/or residuum weathered from rhyolite. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931578"|"29603938"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 55 percent of the map unit. Slopes are 25 to 50 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931579"|"29603939"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 85 percent of the map unit. Slopes are 10 to 25 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931514"|"29603874"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 35 percent of the map unit. Slopes are 10 to 25 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931555"|"29603915"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 55 percent of the map unit. Slopes are 10 to 25 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931554"|"29603914"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 85 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP903MT Shallow Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931553"|"29603913"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Eutroboralfs component makes up 30 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931516"|"29603876"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 60 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, paralithic, is 20 to 40 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931515"|"29603875"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 80 percent of the map unit. Slopes are 10 to 25 percent. This component is on dip slopes on mountains. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 10 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931517"|"29603877"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 35 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931552"|"29603912"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 55 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931551"|"29603911"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Eutroboralfs component makes up 90 percent of the map unit. Slopes are 10 to 40 percent. This component is on landslides. The parent material consists of complex landslide deposits. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931518"|"29603878"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 90 percent of the map unit. Slopes are 10 to 40 percent. This component is on landslides. The parent material consists of complex landslide deposits. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP917MT Subirrigated Cool Moist Woodland Group ecological site.      "|"26931550"|"29603910"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 90 percent of the map unit. Slopes are 10 to 40 percent. This component is on intermontane basins, toes on mountains. The parent material consists of colluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931549"|"29603909"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 90 percent of the map unit. Slopes are 10 to 25 percent. This component is on intermontane basins, toes on mountains. The parent material consists of colluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP917MT Subirrigated Cool Moist Woodland Group ecological site.      "|"26931548"|"29603908"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 90 percent of the map unit. Slopes are 10 to 40 percent. This component is on intermontane basins, toes on mountains. The parent material consists of colluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931547"|"29603907"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 90 percent of the map unit. Slopes are 25 to 50 percent. This component is on intermontane basins, toes on mountains. The parent material consists of colluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP917MT Subirrigated Cool Moist Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931546"|"29603906"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 90 percent of the map unit. Slopes are 10 to 25 percent. This component is on moraines, glaciated mountain ridges. The parent material consists of glacial till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931545"|"29603905"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 100 percent of the map unit. Slopes are 25 to 50 percent. This component is on moraines. The parent material consists of glacial till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931544"|"29603904"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Andic Cryochrepts component makes up 80 percent of the map unit. Slopes are 15 to 40 percent. This component is on moraines. The parent material consists of glacial till. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931543"|"29603903"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 45 percent of the map unit. Slopes are 25 to 40 percent. This component is on moraines. The parent material consists of glacial till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931542"|"29603902"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 55 percent of the map unit. Slopes are 25 to 40 percent. This component is on moraines. The parent material consists of glacial till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931541"|"29603901"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 85 percent of the map unit. Slopes are 10 to 25 percent. This component is on moraines. The parent material consists of glacial drift. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931540"|"29603900"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 45 percent of the map unit. Slopes are 25 to 50 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931580"|"29603940"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 90 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931581"|"29603941"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 65 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931582"|"29603942"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 25 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931583"|"29603943"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931584"|"29603944"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 75 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931585"|"29603945"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryoborolls component makes up 80 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931505"|"29603865"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931502"|"29603862"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 55 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 20 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931503"|"29603863"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 20 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 10 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP902MT Shallow Cold Woodland Group ecological site.      "|"26931504"|"29603864"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land is a miscellaneous area."|"26931500"|"29603860"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 60 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931501"|"29603861"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land is a miscellaneous area."|"26931586"|"29603946"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 65 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931587"|"29603947"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land is a miscellaneous area."|"26931588"|"29603948"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 65 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931589"|"29603949"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Andic Cryochrepts component makes up 85 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from rhyolite and/or residuum weathered from rhyolite. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931499"|"29603859"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts, channery component makes up 55 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931590"|"29603950"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts, extremely cobbly component makes up 45 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931591"|"29603951"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Andic Cryochrepts component makes up 80 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931592"|"29603952"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931593"|"29603953"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 65 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent.  "|"26931594"|"29603954"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryumbrepts component makes up 80 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931595"|"29603955"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 80 percent of the map unit. Slopes are 25 to 50 percent. This component is on glaciated mountain slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931596"|"29603956"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 90 percent of the map unit. Slopes are 10 to 25 percent. This component is on glaciated mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931597"|"29603957"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 45 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931598"|"29603958"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 40 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP902MT Shallow Cold Woodland Group ecological site.      "|"26931599"|"29603959"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 75 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931600"|"29603960"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryoborolls component makes up 15 percent of the map unit. Slopes are 10 to 25 percent. This component is on mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931601"|"29603961"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 85 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931602"|"29603962"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 80 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931603"|"29603963"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 50 percent of the map unit. Slopes are 10 to 25 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931604"|"29603964"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 40 percent of the map unit. Slopes are 10 to 25 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931605"|"29603965"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Cirqueland is a miscellaneous area."|"26931606"|"29603966"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931497"|"29603857"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 50 percent of the map unit. Slopes are 60 to 90 percent.  The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931498"|"29603858"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931607"|"29603967"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 50 percent of the map unit. Slopes are 60 to 90 percent.  The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931608"|"29603968"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931609"|"29603969"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 45 percent of the map unit. Slopes are 60 to 90 percent.  The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931610"|"29603970"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Andic Cryochrepts component makes up 70 percent of the map unit. Slopes are 60 to 90 percent.  The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931611"|"29603971"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 15 percent of the map unit. Slopes are 60 to 90 percent.  The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931612"|"29603972"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931613"|"29603973"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931614"|"29603974"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 55 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931615"|"29603975"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931616"|"29603976"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 55 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP903MT Shallow Cool Woodland Group ecological site.      "|"26931617"|"29603977"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931618"|"29603978"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 55 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP903MT Shallow Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931619"|"29603979"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 65 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931494"|"29603854"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931495"|"29603855"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Cryochrepts component makes up 20 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931496"|"29603856"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 80 percent of the map unit. Slopes are 60 to 90 percent. This component is on structural breaks. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931493"|"29603853"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Borolls component makes up 90 percent of the map unit. Slopes are 0 to 10 percent. This component is on stream terraces, flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 30 inches during April, May, June, July. Organic matter content in the surface horizon is about 3 percent. This component is in the R043BP801MT Bottomland Group ecological site.      "|"26931620"|"29603980"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Aquolls component makes up 90 percent of the map unit. Slopes are 0 to 10 percent. This component is on flood plains, stream terraces. The parent material consists of alluvium and/or glacial outwash. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 0 inches during April, May, June, July. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the R043BP801MT Bottomland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 28 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931488"|"29603848"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Argiborolls component makes up 55 percent of the map unit. Slopes are 10 to 25 percent. This component is on alluvial fans. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931621"|"29603981"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 45 percent of the map unit. Slopes are 10 to 25 percent.  The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931622"|"29603982"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 45 percent of the map unit. Slopes are 10 to 25 percent. This component is on glaciated mountain slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931491"|"29603851"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 35 percent of the map unit. Slopes are 10 to 25 percent. This component is on glaciated mountain slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931492"|"29603852"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 60 percent of the map unit. Slopes are 10 to 40 percent. This component is on moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931623"|"29603983"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 30 percent of the map unit. Slopes are 10 to 40 percent. This component is on moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931624"|"29603984"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Aquolls component makes up 65 percent of the map unit. Slopes are 0 to 10 percent. This component is on moraines. The parent material consists of glacial drift. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 0 inches during April, May, June, July. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 28 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931625"|"29603985"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 35 percent of the map unit. Slopes are 0 to 10 percent. This component is on moraines. The parent material consists of glacial drift. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931626"|"29603986"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 65 percent of the map unit. Slopes are 10 to 40 percent. This component is on landslides. The parent material consists of complex landslide deposits. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931627"|"29603987"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 25 percent of the map unit. Slopes are 10 to 40 percent. This component is on landslides. The parent material consists of complex landslide deposits. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931628"|"29603988"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 60 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931489"|"29603849"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 30 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP912MT Limy Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931490"|"29603850"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Haploborolls component makes up 45 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, paralithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931486"|"29603846"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 35 percent of the map unit. Slopes are 10 to 40 percent. This component is on rolling upland slopes. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, paralithic, is 20 to 60 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931487"|"29603847"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lithic Ustochrepts component makes up 65 percent of the map unit. Slopes are 10 to 30 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 4 to 20 inches.   Water movement in the most restrictive layer is high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 0 percent. This component is in the R043BP823MT Shallow Alpine Group ecological site.      "|"26931484"|"29603844"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 25 percent of the map unit. Slopes are 10 to 30 percent. This component is on structural benches. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931485"|"29603845"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Calcic Cryoborolls component makes up 55 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 50 percent.  "|"26931629"|"29603989"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 25 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from limestone and/or residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931630"|"29603990"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 50 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931631"|"29603991"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 35 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from granite and/or residuum weathered from granite. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931632"|"29603992"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Eutroboralfs component makes up 50 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931633"|"29603993"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Argiborolls component makes up 35 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931634"|"29603994"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 80 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.      "|"26931635"|"29603995"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Haploborolls component makes up 65 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931636"|"29603996"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Eutroboralfs component makes up 25 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 60 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931637"|"29603997"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 55 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931482"|"29603842"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 35 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931483"|"29603843"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Ustochrepts component makes up 50 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  "|"26931638"|"29603998"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 35 percent of the map unit. Slopes are 40 to 60 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931639"|"29603999"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 45 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges, mountain slopes. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931480"|"29603840"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 40 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain slopes, mountain ridges. The parent material consists of colluvium derived from basalt and/or residuum weathered from basalt. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.      "|"26931481"|"29603841"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 90 percent of the map unit. Slopes are 25 to 50 percent. This component is on mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931479"|"29603839"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Argic Cryoborolls component makes up 55 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent. This component is in the R043BP821MT Upland Alpine Group ecological site.     There are no saline horizons within 30 inches of the soil surface. "|"26931477"|"29603837"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Mollic Cryoboralfs component makes up 35 percent of the map unit. Slopes are 10 to 40 percent. This component is on mountain ridges. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 40 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BP910MT Upland Cool Woodland Group ecological site.    The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931478"|"29603838"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryochrepts component makes up 55 percent of the map unit. Slopes are 25 to 40 percent. This component is on glaciated mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock and/or till. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931640"|"29604000"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Typic Cryoboralfs component makes up 25 percent of the map unit. Slopes are 25 to 40 percent. This component is on glaciated mountain slopes. The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 40 to 80 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 50 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931641"|"29604001"
03/27/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931642"|"29604002"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Andic Cryochrepts component makes up 75 percent of the map unit. Slopes are 25 to 40 percent.  The parent material consists of colluvium derived from metasedimentary rock and/or residuum weathered from metasedimentary rock and/or till. Depth to a root restrictive layer is greater than 60 inches.   Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group ecological site.      "|"26931643"|"29604003"
05/20/2020 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Water is a miscellaneous area."|"26931476"|"29603836"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Worock soil is a minor component."|"26931644"|"29604004"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Bordengulch family soil is a minor component."|"26931645"|"29604005"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Risingwolf component makes up 35 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of mixed volcanic ash over colluvium and/or till derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931646"|"29604006"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Sherlock family component makes up 25 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of mixed volcanic ash over colluvium and/or till derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931647"|"29604007"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Kegsprings family, stony component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of colluvium and/or till derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931648"|"29604008"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Whitore family soil is a minor component."|"26931649"|"29604009"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Skaggs family, very stony soil is a minor component."|"26931650"|"29604010"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Risingwolf family component makes up 35 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of mixed volcanic ash over colluvium and/or till derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  "|"26931651"|"29604011"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Sherlock family component makes up 30 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of mixed volcanic ash over colluvium and/or till derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931652"|"29604012"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Helmville family component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of colluvium and/or till derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BD901MT Lower Subalpine Coniferous Subalpine fir / twinflower, Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931653"|"29604013"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop, metasedimentary soil is a minor component."|"26931519"|"29603879"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land, talus, metasedimentary soil is a minor component."|"26931520"|"29603880"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Scalplock, stony soil is a minor component."|"26931521"|"29603881"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Risingwolf component makes up 35 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of mixed volcanic ash over colluvium derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP916MT Ashy Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931522"|"29603882"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Nooney, stony component makes up 25 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 39 to 79 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931523"|"29603883"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lonniebee family component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 39 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the R043BP818MT Upland Cold Woodland Group, Upland Grassland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931524"|"29603884"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land, talus, metasedimentary soil is a minor component."|"26931654"|"29604014"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931655"|"29604015"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Risingwolf soil is a minor component."|"26931656"|"29604016"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Scalplock, very stony soil is a minor component."|"26931657"|"29604017"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Nooney, very stony component makes up 40 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 39 to 79 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931658"|"29604018"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Lonniebee family component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 20 to 39 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the R043BP818MT Upland Cold Woodland Group, Upland Grassland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria.   "|"26931659"|"29604019"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Tropal family, very stony soil is a minor component."|"26931660"|"29604020"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop, limestone soil is a minor component."|"26931661"|"29604021"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land, talus, limestone soil is a minor component."|"26931662"|"29604022"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Risingwolf family, stony component makes up 35 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of mixed volcanic ash over colluvium derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 3 percent. This component is in the F043BP916MT Ashy Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  "|"26931663"|"29604023"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Helmville family component makes up 30 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931664"|"29604024"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Skaggs family, stony component makes up 15 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium derived from metasedimentary rock and/or limestone over residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 39 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 5 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 25 percent.  "|"26931665"|"29604025"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Tropal family, extremely stony soil is a minor component."|"26931666"|"29604026"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land, talus, limestone soil is a minor component."|"26931667"|"29604027"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931668"|"29604028"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Risingwolf family soil is a minor component."|"26931669"|"29604029"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Skaggs family, very stony component makes up 45 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 39 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 5 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 25 percent.  "|"26931670"|"29604030"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Helmville family, stony component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BP909MT Upland Cold Woodland Group, Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock's smooth woodrush-beargrass/yellow avalanche lily. ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931671"|"29604031"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931672"|"29604032"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Tropal family, extremely stony soil is a minor component."|"26931673"|"29604033"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Risingwolf family soil is a minor component."|"26931674"|"29604034"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land is a miscellaneous area."|"26931675"|"29604035"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Skaggs family, very stony component makes up 20 percent of the map unit. Slopes are 35 to 60 percent. This component is on ridges, mountains. The parent material consists of colluvium over residuum weathered from limestone. Depth to a root restrictive layer, bedrock, lithic, is 20 to 39 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 5 percent. This component is in the R043AP809MT Upland Alpine Group, Upland Cold Woodland Group ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 25 percent.  "|"26931676"|"29604036"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Sherlock family soil is a minor component."|"26931677"|"29604037"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Whitore family component makes up 45 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of colluvium and/or till derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 2 percent. This component is in the F043BD900MT Lower Subalpine Dry Coniferous Subalpine fir/ Beargrass, Subalpine Coniferous Cool Moderately Dry subalpine fir (Abies lasiocarpa) / Engelmann spruce (Picea engelmannii) ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 25 percent.  "|"26931678"|"29604038"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Risingwolf family soil is a minor component."|"26931679"|"29604039"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Skaggs family, very stony soil is a minor component."|"26931680"|"29604040"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Helmville family, stony component makes up 30 percent of the map unit. Slopes are 35 to 60 percent. This component is on mountain slopes, mountains. The parent material consists of colluvium and/or till derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 1 percent. This component is in the F043BD900MT Lower Subalpine Dry Coniferous Subalpine fir/ Beargrass, Subalpine Coniferous Cool Moderately Dry subalpine fir (Abies lasiocarpa) / Engelmann spruce (Picea engelmannii) ecological site. Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent.  "|"26931681"|"29604041"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Water soil is a minor component."|"26931525"|"29603885"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Poso family soil is a minor component."|"26931526"|"29603886"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Jonescreek family, occasionally flooded soil is a minor component."|"26931527"|"29603887"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Riverwash soil is a minor component."|"26931528"|"29603888"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Parkcity family component makes up 52 percent of the map unit. Slopes are 0 to 8 percent. This component is on stream terraces, valleys. The parent material consists of alluvium derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 5 percent. This component is in the F043AX959MT Montane Warm Dry Coniferous Douglas fir/white spirea-common snowberry/pinegrass ecological site. Nonirrigated land capability classification is 6e. Irrigated land capability classification is 6e. This soil does not meet hydric criteria.   "|"26931529"|"29603889"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Pippin family component makes up 25 percent of the map unit. Slopes are 0 to 8 percent. This component is on stream terraces, valleys. The parent material consists of alluvium derived from metasedimentary rock. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is excessively drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 5 percent. This component is in the R043AP802MT Bottomland Group ecological site. Nonirrigated land capability classification is 7s. Irrigated land capability classification is 7e. This soil does not meet hydric criteria.   "|"26931530"|"29603890"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rock outcrop is a miscellaneous area."|"26931531"|"29603891"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Rubble land is a miscellaneous area."|"26931532"|"29603892"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Scalplock soil is a minor component."|"26931533"|"29603893"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Piegan soil is a minor component."|"26931534"|"29603894"
08/07/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Nooney family, very bouldery component makes up 40 percent of the map unit. Slopes are 60 to 80 percent. This component is on cirque headwalls, mountains. The parent material consists of colluvium over residuum weathered from metasedimentary rock. Depth to a root restrictive layer, bedrock, lithic, is 39 to 79 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches (or restricted depth) is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043AX958MT Alpine Krummholtz Coniferous subalpine fir-whitebark pine/grouse whortleberry Abies lasciocarpa-Pinus albicaulis (Picea engelmannii)/Vaccinium scoparium ecological site. Nonirrigated land capability classification is 8.  This soil does not meet hydric criteria.   "|"26931535"|"29603895"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Helmville family soil is a minor component."|"26931536"|"29603896"
05/22/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"Generated brief soil descriptions are created for major soil components.  The Babb soil is a minor component."|"26931537"|"29603897"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Levengood family component makes up 50 percent of the map unit. Slopes are 2 to 15 percent. This component is on stream terraces, valleys. The parent material consists of alluvium derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches (or restricted depth) is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 5 percent. This component is in the F043BD908MT Lower Subalpine Cool Dry Coniferous subalpine fir- Engelmann spruce/ Sitka alder/ thinleaf huckleberry/ common beargrass, Montane Dry Coniferous Douglas fir / common snowberry ecological site. Nonirrigated land capability classification is 6e. Irrigated land capability classification is 6e. This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 21 percent.  "|"26931538"|"29603898"
08/06/2025 00:00:00|"Nontechnical description"|"GENSOIL"|"generated"|"The Poso family component makes up 30 percent of the map unit. Slopes are 0 to 15 percent. This component is on stream terraces, valleys. The parent material consists of alluvium derived from metasedimentary rock and/or limestone. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high. Available water to a depth of 60 inches (or restricted depth) is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 75 percent. Below this thin organic horizon the organic matter content is about 4 percent. This component is in the F043BD908MT Lower Subalpine Cool Dry Coniferous subalpine fir- Engelmann spruce/ Sitka alder/ thinleaf huckleberry/ common beargrass, Montane Dry Coniferous Douglas fir / common snowberry ecological site. Nonirrigated land capability classification is 6e. Irrigated land capability classification is 6e. This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent. There are no saline horizons within 30 inches of the soil surface. "|"26931539"|"29603899"
