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WEATHER
Pleistocene Sand Dunes
Ecoregion
on
Great Plains
in
OK
,
KS
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Active, barren, or stabilized Pleistocene Sand Dunes are found along, and usually to the north of, most major rivers in the Central Great Plains (27); they lack well developed drainage networks and are physiographically and lithologically unlike the rest of Ecoregion 27. Deep, loose, permeable to rapidly permeable, sandy soils are characteristic. They widely support sand sagebrush – bluestem prairie, but where moisture is sufficient, oak savanna stabilizes dunes. Small interdune wetlands occur where the water table is high; they are important habitat for migrating shorebirds and waterfowl. Grazing is the most common land use, but irrigated cropland is found on soils that can retain sufficient moisture. Local overgrazing has occurred, promoting wind erosion. Springs are abundant, especially at the contact between sand and the underlying Permian redbeds. Ecoregion 27l consistently supports large populations of rodents, rabbits, and birds; it is one of the most important areas for game in Ecoregion 27. During prolonged cold and wet periods, the Pleistocene Sand Dunes (27l) ecoregion provides important shelter to wildlife.
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