Caddo Archeology Journal




In the wildly rugged hills near Canyon Springs, in southeastern Pontotoc County, Oklahoma, a unique sandstone formation has produced evidence of once sheltering a prehistoric people.

Technically, the sandstone is of the Wilcox series, and is faulted to a position above the McLish limestone beneath which it normally lies. The fault line runs from the north southward a distance of 25 yards, then runs at right angles to the east for 40 yards. The sandstone ranges from 6 feet in height on the northern extremity to 35 feet along the southeastern portion. Multiple fractures, generally parallel to the fault lines, have been recemented with dissolved siliceous material to make a highly resistant formation. Erosion takes place by exfoliation, giving to the rock mass, at a distance, a granitic appearance. Because of slanting fracture lines, the foot-wall of the fault, overthrust as it is, has broken off in places to form huge over-hangs that afford plentiful protection from the weather. It was in such an area evidence of a prehistoric habitation was found.

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Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.



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