Interior Alaska Mountains-Boreal Upland and Subalpine-Mountain Valleys, Ash Influenced

E28-boreal taiga-silty frozen till slopes (22%)
Typic Historthels
Poorly drained
Hydric: Yes
PAWS: 27 cm
mountains / Footslope
mountains / Toeslope
E28-boreal forest-silty till slopes (13%)
Typic Humicryods
Well drained
Hydric: No
PAWS: 10 cm
mountains / Backslope
E28-boreal forest-silty wet till slopes (12%)
Thaptic Cryaquands
Very poorly drained
Hydric: Yes
PAWS: 32 cm
mountains / Footslope
E28-boreal subalpine scrub-silty till slopes (11%)
Andic Dystrocryepts
Well drained
Hydric: No
PAWS: 11 cm
mountains / Backslope
E28-boreal rock outcrop and rubbleland (10%)


Hydric: Unranked
PAWS: NA
mountains
mountain slopes
E28-boreal subalpine scrub-silty spodic till slopes (8%)
Andic Humicryods
Well drained
Hydric: No
PAWS: 20 cm
mountains / Backslope
E28-boreal taiga/tussock-silty frozen till slopes (8%)
Typic Histoturbels
Very poorly drained
Hydric: Yes
PAWS: 27 cm
mountains / Toeslope
E28-boreal scrub-gravelly low flood plains (6%)
Oxyaquic Cryorthents
Somewhat poorly drained
Hydric: Yes
PAWS: 3 cm
flood plains
E28-boreal alpine dwarf scrub-gravelly colluvial slopes (5%)
Typic Dystrocryepts
Well drained
Hydric: No
PAWS: 9 cm
mountains / Summit
mountains / Backslope
E28-Boreal water, fresh (3%)


Hydric: No
PAWS: 0 cm
rivers
lakes
streams
E28-boreal wet meadow-gravelly pond margins (2%)
Histic Cryaquepts
Very poorly drained
Hydric: Yes
PAWS: 23 cm
stream terraces
depressions
SSAScalePublishedExport
ak7141:250,0002024-09-05