Preliminary report on the geology of the Arbuckle and Wichita mountains in Indian Territory and Oklahoma
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Abstract
The Arbuckle Mountains consist of a moderately elevated table -land or plateau in the east-central part of the Chickasaw Nation, Indian Territory. The plateau ranges in elevation from 1,300 feet above sea, in its contracted western part, to 750 feet, at the east end, where it coalesces with the bordering plain. Geologically the Arbuckle Mountain region consists of a great thickness of rocks, composed chiefly of limestones, which range in age from middle Cambrian to Devonian, and which are succeeded on the borders by an almost equal thickness of Carboniferous conglomerates, shales, and sandstones. In the central part of the district, unconformably beneath the Cambrian strata, there is a mass of granite, granite-porphyry, diabase, and associated crystalline rocks. The uplifting and folding of the region occurred previous to the deposition of the Permian "Red Beds," which were deposited across it on the' west. The bearing of the Arbuckle uplift is approximately N. 70° W.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Preliminary report on the geology of the Arbuckle and Wichita mountains in Indian Territory and Oklahoma |
| Series title | Professional Paper |
| Series number | 31 |
| DOI | 10.3133/pp31 |
| Year Published | 1904 |
| Language | English |
| Publisher | Government Printing Office |
| Publisher location | Washington, D.C. |
| Description | 97 p. |
| Country | United States |
| State | Oklahoma |
| Other Geospatial | Arbuckle Mountains, Wichita Mountains |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |
| Google Analytic Metrics | Metrics page |