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Science 26 July 1985:
Vol. 229. no. 4711, pp. 379 - 381
DOI: 10.1126/science.229.4711.379

Articles

Paleoseismic Evidence for Recurrence of Earthquakes near Charleston, South Carolina

PRADEEP TALWANI 1 and JOHN COX 1

1 Department of Geology, University of South Carolina, Columbia 29208

A destructive earthquake that occurred in 1886 near Charleston, South Carolina, was associated with widespread liquefaction of shallow sand structures and their extravasation to the surface. Several seismically induced paleoliquefaction structures preserved within the shallow sediments in the meizoseismal area of the 1886 event were identified. Field evidence and radiocarbon dates suggest that at least two earthquakes of magnitudes greater than 6.2 preceded the 1886 event in the past 3000 to 3700 years. The evidence yielded an initial estimate of about 1500 to 1800 years for the maximum recurrence of destructive, intraplate earthquakes in the Charleston region.

Submitted on January 30, 1985
Accepted on May 17, 1985


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