Interior Alaska Mountains-Boreal Upland and Subalpine-Glaciated Plains and Hills, Ash Influenced

E28-boreal forest-ashy till slopes (45%)
Typic Humicryods
Well drained
Hydric: No
PAWS: 10 cm
hills / Shoulder
hills / Backslope
plains
E28-boreal forest-ashy wet till slopes (22%)
Thaptic Cryaquands
Very poorly drained
Hydric: Yes
PAWS: 27 cm
depressions
hills / Footslope
till plains
E28-boreal subalpine scrub-meadow-ashy till slopes (18%)
Andic Humicryods
Well drained
Hydric: No
PAWS: 20 cm
mountains / Backslope
E28-boreal forest-loamy high flood plains (5%)
Typic Cryofluvents
Well drained
Hydric: No
PAWS: 6 cm
flood plains
E28-boreal scrub-gravelly flood plains (4%)
Oxyaquic Cryorthents
Somewhat poorly drained
Hydric: Yes
PAWS: 3 cm
flood plains
E28-boreal taiga/tussock-ashy frozen slopes (3%)
Typic Histoturbels
Very poorly drained
Hydric: Yes
PAWS: 36 cm
plains
E28-boreal wet meadow-gravelly pond margins (1%)
Histic Cryaquepts
Very poorly drained
Hydric: Yes
PAWS: 23 cm
depressions
stream terraces
E28-Boreal alpine scrub-gravelly till slopes (1%)
Andic Dystrocryepts
Well drained
Hydric: No
PAWS: 10 cm
hills / Backslope
till plains
E28-Boreal water, fresh (1%)


Hydric: No
PAWS: 0 cm
lakes
streams
rivers
SSAScalePublishedExport
ak7791:250,0002024-09-05