7 Geologic Maps, Digital Geologic Maps, Geophysical Maps, and Derivatives from Geologic Maps (Posters)
Thursday, 12 March 2009
8:30 AM - 12:30 PM
GEOLOGIC MAPS OF THE GRANT, LANGSTON, HOLLYWOOD, SCOTTSBORO, STEVENSON, SWEARENGIN, AND WANNVILLE 7.5-MINUTE QUADRANGLES, NORTHEAST ALABAMA
Paper number: 7-13
Program: Theme Sessions
Time: 8:30 AM – 12:30 PM
Authors
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G. Daniel IrvinGeological Survey of Alabama, Tuscaloosa, AL
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Dorothy E. RaymondGeological Survey of Alabama, Tuscaloosa, AL
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W. Edward OsborneGeological Survey of Alabama, Tuscaloosa, AL
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Willard E. WardGeological Survey of Alabama, Tuscaloosa, AL
Abstract
The structure of the area is dominated by the northwest-verging Sequatchie anticline, which shares a gently dipping common limb with the Sand Mountain syncline to the southeast. The steeply dipping northwestern forelimb of the anticline is cut by the southeast-dipping Sequatchie fault. Significantly, the new mapping has demonstrated the presence of northwest-dipping thrust faults (backthrusts) and associated southeast-verging folds in the hanging wall of the Sequatchie fault in this area. Additionally, a klippe of Fort Payne Chert structurally overlying the Monteagle Limestone northwest of the Sequatchie fault in the Wannville quadrangle is reminiscent of klippen mapped along strike near the Alabama-Tennessee state line (Milici and Finlayson, 1983).