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Thickness of sediments above Cape Charles erosion surface, based on seismic tracks of Colman and Halka (1989)

Figure 4.2. Thickness of sediments (meters) above Cape Charles erosion surface, based on seismic tracks (dashed or solid lines) of Colman and Halka (1989). In areas where subbottom methane gas bubbles obscure the erosion surface, the isopachs are conjectural (dashed lines).


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U.S. Department of Interior, U.S. Geological Survey
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