Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma

John S. Havens

doi:10.3133/ofr82760

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Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma

John S. Havens

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Abstract

During 1978, the U.S. Geological Survey began a 5-year study of the High Plains regional aquifer system to provide hydrologic information for evaluation of the effects of long-term development of the aquifer and to develop computer models for prediction of aquifer response to alternative changes in ground-water management (Weeks, 1978). This report is one of a series presenting hydrologic information of the High Plains aquifer in Oklahoma. The 1980 saturated thickness of the High Plains regional aquifer in Oklahoma is shown for the eastern area (plate 1), consisting of Harper, Ellis, Woodward, Dewey, and Roger Mills Counties, and for the Panhandle area (plate 2), consisting of Cimarron, Texas, and Beaver Counties.

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Source-reported bounding extent: 35.38457160381764° to 37.00255267215955° latitude; -103.0078125° to -99.151611328125° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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John S. Havens. 1982. Saturated thickness of the High Plains regional aquifer in 1980, northwestern Oklahoma. https://doi.org/10.3133/ofr82760

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