24 Geologic Maps, Geophysical Maps, and Derivatives from Geologic and Geophysical Maps (Posters)
Sunday, 14 March 2010
1:30 PM - 4:15 PM
International ABCDF
GEOLOGIC MAP ILLUSTRATING THE STRATIGRAPHY AND STRUCTURAL GEOLOGY OF THE BURNT HICKORY RIDGE, GEORGIA, 7.5-MINUTE QUADRANGLE
Paper number: 24-24
Program: Theme Sessions
Time: 1:30 PM – 4:15 PM
Authors
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Thomas J. CrawfordUniversity of West Georgia, Carrollton, GA
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Randy KathUniversity of West Georgia, Carrollton, GA
Abstract
Of particular significance on the Burnt Hickory Ridge quadrangle is a chloritic and calcareous schist-metagraywacke lithologic unit, consisting of: feldspar-quartz-muscovite schist and muscovite-quartz-feldspar metagraywacke, both of which are chloritic and calcareous, and contain thin well-layered quartzites. An abundance of quartz pods gives the rock a “rolling” texture, and the unit weathers brownish red to dark reddish brown. This distinctive lithologic unit extends across the Burnt Hickory Ridge quadrangle near the Emerson-Talladega Fault in broad open folds; and continues across the northwest corner of the Acworth quadrangle and to near the middle of the Allatoona Dam quadrangle, where it is in fault contact with the Corbin Metagranite, emphasizing the overriding relationship of the Emerson-Talladega Fault with the Great Smoky (Cartersville) Fault and the Allatoona Dam Fault.