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Home > Explore! > Bedrock Geology > Two Lights and Crescent Beach > Glaciation > Table 3
TABLE 3: Surficial Sediments of the Cape Elizabeth Area*
| Type of Deposit | Characteristics |
| Swamp and tidal marsh |
Peat and organic muck; some interstratified silt, clay, and sand. |
| Beach and dune |
Fine, well-sorted sand of coastal beaches, and windblown sand of associated dunes adjacent to beaches. |
| Marine |
Dark blue-gray silt, clay, and fine sand, occasionally with marine fossils. The Presumpscot Formation of Bloom (1959, Late Pleistocene changes of sea level in southwestern Maine: Maine Geological Survey, 143 p.). Deposited in marine waters during deglaciation, when the terminus of the retreating ice sheet stood in the sea. |
| Glacial outwash |
Stratified deposits of sand and gravel deposited by meltwater from retreating ice sheet. |
| Till |
Unsorted and unstratified mixture of clay, silt, sand, pebbles, cobbles, and boulders. Forms a variable thickness cover over bedrock. |
| * Adopted from Prescott, Glenn C., Jr., 1976, Ground water favorability and surficial geology of the Portland area, Maine: U.S. Geological Survey, map HA-561. |
Last updated on January 16, 2008
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