March 7, 2017

A Geography of the Carolinas by D. Gordon Bennett, Jeffrey C. Patton

By D. Gordon Bennett, Jeffrey C. Patton

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Sample text

Located on the Piedmont are numer- ous remnants of the greater mountains that once existed there. These monadnocks exist because they are composed of rock that is harder or less fractured than the surrounding rock. The Coastal Plain—that broad relatively flat surface—has been the recipient of the sediment eroding off of the highlands to the west and of deposits laid down when the sea has periodically covered it. More or less of the Coastal Plain has been exposed, in recent geologic history, as world sea levels rose or fell—dependent on the degree of the thermal expansion of ocean water and the amount of water held in the earth’s glacial ice caps.

Cabe, S. and R. Reiman. 1996. Sandhills of the Carolinas. In Snapshots of the Carolinas: Landscapes and Cultures, ed. D. G. : Association of American Geographers, 83-86. Conley, J. F. and G. L. Bain. 1965. Geology of the Carolina Slate Belt West of the Deep River Wadesboro Triassic Basin, North Carolina. Southeastern Geology 6: 117-118. Corbett, J. 1989. Our Mysterious Bays, Their Origin and History. Bladen Weekly, 13 December, 1. Fisher, J. J. 1962. Geomorphic Expression of Former Inlets along the Outer Banks of North Carolina.

The deltas, tidal inlets, barrier islands, and beaches comprise a distinctive physical landscape. Distance to the sea is responsible for most variation in this landscape. We use Beaufort County, South Carolina to illustrate this coastal setting. Climate The proximity of the Atlantic, and especially the Gulf Stream, moderates the daily and seasonal temperature range in Beaufort County. Warm coastal waters buffer the region from low minimum temperatures during the winter months. The average minimum January temperature is warmer than inland locations at the same latitude.

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