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Florida's Hazelhurst terrace and shoreline : ウィキペディア英語版 | Florida's Hazelhurst terrace and shoreline
Florida's Hazelhurst terrace and shoreline (formerly the Brandywine) is an ancient relict shoreline or delta present in the southeastern United States's Atlantic seaboard dating from the Late Miocene to Early Pliocene (~11.0 to 7.0 Ma—3.6 to 2.88 Ma). ==Entomology== The name Hazelhurst was assigned by Dr. C. Wythe Cooke of the (Florida Geographical Survey ) after previously calling it the Brandywine after the Brandywine deposits in Prince George's County, Maryland.〔Cooke, C. W., and Mansfield, W. C., 1936, Suwanne Limestone of Florida (abstract): Geological Society of America Proceedings, 1935, p. 71–72.〕 and includes the geographic features of R. O. Vernon's Coastwise delta plain〔Vernon, R. O., 1951, Surface occurrences of geologic formations in Florida (geologic map): in Association of American State Geologists Forty-fourth Annual Meeting Field Trip Guidebook - A summary of the geology of Florida and a guidebook to the Cenozoic exposures of a portion of the State, 116 p., 5 plates.〕 as well as MacNeil's high Pliocene marine terrace. Deposits are found between 97 to 65.5 meters (320–215 feet) mean sea level.〔(Florida Department of State, Florida Geological Survey: Shorelines and terraces )〕
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