Hydrology of the Arbuckle Mountains area, south-central Oklahoma

Roy W. Fairchild; Ronald L. Hanson; Robert E. Davis

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USGS · 70046124

Hydrology of the Arbuckle Mountains area, south-central Oklahoma

Roy W. Fairchild·Ronald L. Hanson·Robert E. Davis

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Abstract

Rocks that make up the Arbuckle-Simpson aquifer crop out over ~500 mi 2 in the Arbuckle Mountains province in south-central Oklahoma. The aquifer consists of limestone, dolomite, and sandstone of the Arbuckle and Simpson Groups of Late Cambrian to Middle Ordovician age and is about 5,000-9,000 ft thick. The rocks were subjected to intensive folding and faulting associated with major uplift of the area during Early to Late Pennsylvanian time.

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Source-reported bounding extent: 33.6192° to 37° latitude; -103° to -94.4312° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

Roy W. Fairchild, Ronald L. Hanson, Robert E. Davis. 1990. Hydrology of the Arbuckle Mountains area, south-central Oklahoma. https://pubs.usgs.gov/publication/70046124

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