Evolution-Siberian complex, 5 to 40 percent slopes

Evolution (33%)
Skeletal Valley Floor Till
Vitrandic Cryorthents
Moderately well drained
Hydric: No
PAWS: 5 cm
moraines / Footslope
glacial-valley floors
Siberian (25%)
Subalpine, sandy-skeletal, moderately steep slopes
Vitrandic Cryorthents
Well drained
Hydric: No
PAWS: 6 cm
moraines / Footslope
glacial-valley floors
McGee (10%)
Very Deep Skeletal Concave North Slopes
Vitrixerandic Dystrocryepts
Moderately well drained
Hydric: No
PAWS: 20 cm
moraines / Footslope
glacial-valley floors
Isosceles (10%)
Shallow Dry Bedrock Pockets
Lithic Humicryepts
Somewhat excessively drained
Hydric: No
PAWS: 4 cm
structural benches / Backslope
glacial-valley floors
Mendel (7%)
Steep subalpine, valley bottom riverine system
Vitrandic Cryofluvents
Somewhat poorly drained
Hydric: No
PAWS: 5 cm
glacial-valley floors
flood-plain steps / Toeslope
Ledumhill (5%)
Discharge slopes and moist toeslopes
Aquandic Cryaquepts
Poorly drained
Hydric: Yes
PAWS: 9 cm
glacial-valley floors
seeps / Footslope
Rockcreek (3%)
Subalpine Discharge Slopes
Histic Cryaquepts
Poorly drained
Hydric: Yes
PAWS: 17 cm
glacial-valley floors
seeps / Backslope
seeps / Footslope
Rock outcrop (3%)


Hydric: No
PAWS: NA
structural benches
glacial-valley floors
Glacierpoint (2%)
Subalpine Sandy Talus
Vitrixerandic Humicryepts
Somewhat excessively drained
Hydric: No
PAWS: 3 cm
glacial-valley floors
talus slopes / Backslope
talus slopes / Footslope
Water (2%)


Hydric: No
PAWS: NA
streams
SSAScalePublishedExport
ca7321:24,00019982024-09-10