Typic Cryorthents, warm-Rock outcrop, granitic-McGee complex, 5 to 60 percent slopes

Typic Cryorthents (26%)
Subalpine Sandy Talus
Typic Cryorthents
Excessively drained
Hydric: No
PAWS: 2 cm
mountain slopes
talus slopes / Backslope
Rock outcrop (25%)


Hydric: No
PAWS: NA
structural benches
mountain slopes
McGee (15%)
Very Deep Skeletal Concave North Slopes
Vitrixerandic Dystrocryepts
Moderately well drained
Hydric: No
PAWS: 20 cm
ground moraines / Footslope
ground moraines / Toeslope
mountain slopes
Ledumhill (14%)
Discharge slopes and moist toeslopes
Aquandic Cryaquepts
Poorly drained
Hydric: Yes
PAWS: 9 cm
seeps / Footslope
mountain slopes
Benchlake (9%)
Shallow Dry Bedrock Pockets
Lithic Cryorthents
Well drained
Hydric: No
PAWS: 1 cm
structural benches / Backslope
mountain slopes
Rockcreek (9%)
Subalpine Discharge Slopes
Histic Cryaquepts
Poorly drained
Hydric: Yes
PAWS: 17 cm
mountain slopes
seeps / Backslope
Water (2%)


Hydric: No
PAWS: NA
mountain slopes
streams
SSAScalePublishedExport
ca7921:24,00020182024-09-05