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example 6 Eutrocryept-glacial
till
landscape - Valley Co., ID
This landscape resulted from the activity of localized glaciers
at higher elevations in central Idaho. The large boulders in the
foreground were deposited by these glaciers. The soils formed in
this glacial till landscape have a low water holding capacity due
to the large percentage of rock fragments in the subsoil. This limits
the use of these landscapes for timber or crop production. As a
result, the primary uses are pasture and grazing land.
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