DGS Geologic Map Series
Permanent URI for this collection
Browse
Browsing DGS Geologic Map Series by Subject "Carolina Bay Deposits"
Now showing 1 - 3 of 3
Results Per Page
Sort Options
Item Geologic Map of the Millsboro and Whaleysville Quadrangles, Delaware(Newark, DE: Delaware Geological Survey, University of Delaware, 2014-04) Ramsey, K.W.; Tomlinson, J.L.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.Item Geologic Map of the Sharptown, Laurel, Hebron, and Delmar Quadrangles, Delaware(Newark, DE: Delaware Geological Survey, University of Delaware, 2014-09) Ramsey, K.W.; Tomlinson, J.L.The geological history of the surficial geologic units in western Sussex County is that of deposition of the Beaverdam Formation and its subsequent modification by erosion and deposition related to the sea-level fluctuations during the Pleistocene. The geology reflects this complex history by the cut and fill geometry of the middle and late Pleistocene deposits into the Beaverdam Formation. The geology is further complicated by periglacial activity that produced dune deposits and Carolina Bays in the map area, which modified the land surface. Mapping was conducted using field maps at a scale of 1:12,000 with 2-ft contours. Stratigraphic boundaries drawn at topographic breaks reflect detailed mapping using contours not shown on this map.Item Geologic Map of the Trap Pond and Pittsville Quadrangles, Delaware(Newark, DE: Delaware Geological Survey, University of Delaware, 2014-06) Tomlinson, J.L.; Ramsey, K.W.The geological history of the surficial units of the Trap Pond and the Delaware portion of the Pittsville Quadrangle was the result of deposition of the Beaverdam Formation and its subsequent modification by erosion and deposition related to the sea-level fluctuations during the Pleistocene. The geology reflects this complex history by the cut and fill geometry of the Middle and late Pleistocene deposits into the Beaverdam Formation. The geology is further complicated by periglacial activity that produced dune deposits and Carolina Bays in the map area, which modified the land surface. 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.