Author: Ramsey, K.W.; Tomlinson, J.L.
Citable URI: http://udspace.udel.edu/handle/19716/12960
Publisher: Newark, DE: Delaware Geological Survey, University of Delaware
Date Issued: 2014-04
Abstract: The geological history of the surficial units of the Millsboro Quadrangle and Delaware portion of the Whaleysville Quadrangle was the result of deposition of the Beaverdam Formation during the late Pliocene and its subsequent modification by erosion and deposition related to sea-level fluctuations during the Pleistocene and late Pleistocene upland swamp and bog deposition. The geology at the land surface was then further modified by periglacial activity that produced dune deposits and Carolina Bays in the map area. Surficial geologic mapping was conducted using field maps at a scale of 1:12,000 with 2 foot contours. Stratigraphic boundaries drawn at topographic breaks reflect detailed mapping using contours not shown on this map.
URI: http://udspace.udel.edu/handle/19716/12960
Series/Report no.: Geologic map;
geomap20.pdf | Size: 26.29Mb | Format: PDF |
Geologic Map of the Millsboro and Whaleysville Quadrangles, ... |
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