Rain Water Basin
, region (
c.6,000 sq mi/15,540 sq km), S central
Nebr. Also called the Loess Plain, the basin is roughly triangular in
shape, with its base in the E overlooking the valley of Big Blue R.,
and extending to the low terraces of the Platte R. in the N and above
the Republican Valley at the SW. The land generally slopes gradually to
the SE. Much of the Loess Plain has no surface drainage; instead the
moderate amount of precipitation is disposed of by evaporation and
infiltration through the thick, silty soil. Water may remain on the
land in shallow, wind-carved depressions; where the basins are deeper
and infiltration slowed by nearly impentetrable claypan, rainwater
basins such as ponds, lagoons, and marshes result. They are common in
the more humid E part of the Loess Plain, esp. in Clay and Fillmore
cos. The wetlands have been reduced from c.100,000
acres/40,470 ha to c.21,000 acres/8,499 ha
through drainage and road building. Much of the wetland remaining is
managed by the U.S. Fish and Wildlife Service, esp. for wildfowl. The
Neb. Game and Parks Commission controls a smaller acreage.
Capital city or county seat is shown by the symbol
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