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

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

By D. Gordon Bennett, Jeffrey C. Patton

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Precipitation from these thunderstorms can be very intense, but usually of short duration. Thunderstorms are essential in sustaining agricultural crops during the summer when temperature and evaporation rates are high. During some years, the Bermuda 36 High moves westward, establishing itself over the Southeast. When this happens, drier air develops, vertical lifting weakens, and clouds and precipitation are suppressed. In some summers, this latter process results in drought which damages crops.

New York: Macmillan Publishing Co. Smosma, R. A. 1977. Geological Facts about the New River. Mountain State Geology, December: 51. Soller, D. R. 1988. Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina. U. S. Geological Survey, Professional Paper 1466-A. _____ and H. H. Mills. 1991. Surficial Geology and Geomorphology. In The Geology of the Carolinas: Carolina Geological Society Fiftieth Anniversary Volume, eds. W. Horton and V. A. Zullo, Knoxville: University of Tennessee Press, 290-308.

Triassic Basins Eventually, Gondwanaland and Laurentia sutured together, forming the great supercontinent Pangea III. Pangea III lasted some 100 million years and then began to split apart, starting some 250 million years ago during the Triassic Age. As it did, the crust near the split or rift was stretched and thinned. This crustal extension would have been similar to what is occurring in the Great Rift Valley of eastern Africa today. From outer space, the African Rift Valley appears as a 4,000-mile long scar on the continent’s surface.

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