Bedrock geology and regional geologic setting of Coweeta Hydrologic Laboratory in the eastern Blue Ridge. Hatcher, R. D Pages 81-92 in W, 1988.
Bedrock geology and regional geologic setting of Coweeta Hydrologic Laboratory in the eastern Blue Ridge. [pdf]Paper  abstract   bibtex   
The Appalachian Highlands represent the last remnant of a more extensive mountain chain, which at one time was as lofty as many of the modern, less eroded chains of the world such as the Alps, Andes, and North American Cordillera. This chapter discusses the bedrock geology of Coweeta Hydrologic Laboratory and places it into the context of Blue Ridge geology. Control of topography by structure and the nature of the Quaternary deposits is discussed.

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