Mancelona sand, 6 to 12 percent slopes
Mancelona
(90%)
Rich Sandy Drift
Alfic Haplorthods
Somewhat excessively drained
Hydric: No
PAWS: 12 cm
stream terraces / Summit
stream terraces / Shoulder
stream terraces / Backslope
stream terraces / Footslope
stream terraces / Toeslope
glacial drainage channels / Summit
glacial drainage channels / Shoulder
glacial drainage channels / Backslope
glacial drainage channels / Footslope
glacial drainage channels / Toeslope
Klacking
(4%)
Arenic Glossudalfs
Well drained
Hydric: No
PAWS: 16 cm
glacial drainage channels / Summit
glacial drainage channels / Shoulder
glacial drainage channels / Backslope
glacial drainage channels / Footslope
glacial drainage channels / Toeslope
stream terraces / Summit
stream terraces / Shoulder
stream terraces / Backslope
stream terraces / Footslope
stream terraces / Toeslope
Graycalm
(3%)
Lamellic Udipsamments
Somewhat excessively drained
Hydric: No
PAWS: 11 cm
glacial drainage channels / Summit
glacial drainage channels / Shoulder
glacial drainage channels / Backslope
glacial drainage channels / Footslope
glacial drainage channels / Toeslope
stream terraces / Summit
stream terraces / Shoulder
stream terraces / Backslope
stream terraces / Footslope
stream terraces / Toeslope
McGinn
(3%)
Haplic Glossudalfs
Well drained
Hydric: No
PAWS: 24 cm
glacial drainage channels / Summit
glacial drainage channels / Shoulder
glacial drainage channels / Backslope
glacial drainage channels / Footslope
glacial drainage channels / Toeslope
stream terraces / Summit
stream terraces / Shoulder
stream terraces / Backslope
stream terraces / Footslope
stream terraces / Toeslope
SSA
Scale
Published
Export
mi007
1:12,000
1998
2024-08-26
