Osage Plains

Coordinates: 36°N 96°W / 36°N 96°W / 36; -96
Source: Wikipedia, the free encyclopedia.
U.S. states
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The Osage Plains are a

Blackland Prairies and Cross Timbers. This vegetatively complex region of intermixed prairie and scrubby juniper-mesquite woodland extends into north-central Texas. Bluestem prairies and oak-dominated savannas and woodlands characterize the natural vegetation in the Cross Timbers. Much of the area has been converted to agriculture, although expanses of oak
forest and woodland are still scattered throughout the eastern portion of the subregion.

Birds in the Osage Plains include the threatened greater prairie-chicken, Henslow's sparrow, dickcissel, loggerhead shrike, field sparrow, scissor-tailed flycatcher, Bell's vireo, painted bunting, and Harris's sparrow. Wildfire suppression, overgrazing, and the spread of exotic plants are the factors most negatively affecting priority bird habitat. The area now is managed almost exclusively for beef production with annual burns and intensive grazing practices that provide little of the habitat structure required to support many priority bird species.

Historically, fire, drought, and

corn and soybeans, or has been converted to non-native grasses for pasture and hay. Large expanses of tallgrass prairie
remain in the Flint Hills, where relief is greater than in the Osage Plains subregion and the land less suitable for cropping.

Geology

The Osage Plains are underlain by soft

Mississippian to Pennsylvanian ages. Some of the rocks prevalent in the Osage Plains are Mississippian limestone, limestone shale, Ordovician dolomite, and Pennsylvanian coal. Also, clay and shale are found within the Pennsylvanian bedrock.[3]

The area contained two major mining areas. The biggest was the Tri-State lead and zinc region, consisting of nearly 2,000 sq mi (5,200 km2). This was the largest concentration of zinc deposits anywhere in the world. Most mining sites have closed, mainly due to health and other environmental issues. More than $1 billion worth of lead and zinc were extracted from the area during the active mining days. The other major mining was for bituminous coal. Due to air quality standards, this region's coal is in low demand due to its high sulfur content.[4]

References

  1. ^ "Physiographic divisions of the conterminous U. S." U.S. Geological Survey. Retrieved 2007-12-06.
  2. ^ "Osage Plains". Oklahoma Historical Society. Archived from the original on 2014-11-04. Retrieved 2007-12-28.
  3. ^ Adamski, James C.; James C. Petersen; David A. Freiwald; Jerri V. Davis (1995). Environmental and Hydrologic Setting of the Ozark Plateaus Study Unit, Arkansas, Kansas, Missouri, and Oklahoma (PDF). U.S. Geological Survey, Water-Resources Investigations Report 94-4022. p. 14.
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36°N 96°W / 36°N 96°W / 36; -96

Public Domain This article incorporates public domain material from Osage Plains. Bureau of Land Management.