DGS Geologic Map No. 18 (Bethany Beach and Assawoman Bay Quadrangles) Dataset
This vector data set contains the rock unit polygons for the surficial geology in the Delaware Coastal Plain covered by DGS Geologic Map Series No. 18 (Bethany Beach and Assawoman Bay Quadrangles). The geologic history of the surficial units of the Bethany Beach and Assawoman Bay Quadrangles is that of deposition of the Beaverdam Formation and its subsequent modification by erosion and deposition related to sea-level fluctuations during the Pleistocene. The geology reflects this complex history onshore, in Indian River Bay and Assawoman Bay, and offshore in the Atlantic Ocean. Erosion during the late Pleistocene sea-level lowstand and ongoing deposition offshore and in Indian River Bay during the Holocene rise in sea level represents the latest of several cycles of erosion and deposition. An additional dataset of datapoints used to generate rock unit polygons for the surficial geology in the Delaware Coastal Plain covered by DGS Geologic Map Series No. 18 (Bethany Beach and Assawoman Bay quadrangles) exists for use in conjunction with this dataset.
- alluvial deposits
- alluvium and swamp deposits
- Assawoman Bay
- barrier washover deposits
- beach deposits
- Beaverdam Formation
- Bethany Beach
- Bethany Formation
- Carolina Bay deposits
- coastal geology
- dredge disposal deposits
- dune deposits
- dune washovers
- Fenwick Island
- fill
- finger shoal deposits
- lagoon deposits
- Lynch Heights Formation
- marine deposits
- marsh and tidal deposits
- marsh deposits
- nearshore deposits
- Quaternary Period
- sheet sand deposits
- shoreline deposits
- Sinepuxent Formation
- STATEMAP
- surficial geology
- Shapefile
GM18 Geologic Map of the Bethany Beach and Assawoman Bay Quadrangles
The geologic history of the surficial units of the Bethany Beach and Assawoman Bay Quadrangles is that of deposition of the Beaverdam Formation and its subsequent modification by erosion and deposition related to sea-level fluctuations during the Pleistocene. The geology reflects this complex history onshore, in Indian River Bay and Assawoman Bay, and offshore in the Atlantic Ocean. Erosion during the late Pleistocene sea-level lowstand and ongoing deposition offshore and in Indian River Bay during the Holocene rise in sea level represents the latest of several cycles of erosion and deposition.
- alluvial deposits
- alluvium and swamp deposits
- Assawoman Bay
- Atlantic Coastal Plain
- barrier washover deposits
- beach deposits
- Beaverdam Formation
- Bethany Beach
- Bethany Formation
- Carolina Bay deposits
- coastal geology
- dredge disposal deposits
- dune deposits
- dune washovers
- Fenwick Island
- fill
- finger shoal deposits
- lagoon deposits
- Lynch Heights Formation
- marine deposits
- marsh and tidal deposits
- marsh deposits
- nearshore deposits
- Quaternary Period
- sheet sand deposits
- shoreline deposits
- Sinepuxent Formation
- STATEMAP
- surficial geology
Assawoman Bay Group
The Assawoman Bay Group consists of the well-sorted sands, silts, and clays of the Omar, Ironshire, and Sinepuxent Formations found adjacent to and inland of the Atlantic Coast of Delaware and Maryland. These deposits in Delaware and Maryland were named from oldest to youngest: the Omar Formation (Jordan, 1962, 1964), the Ironshire Formation (Owens and Denny, 1979a), and the Sinepuxent Formation (Owens and Denny, 1979a).



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