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A Transgressive Sequence of Late Holocene Epoch Tidal Environmental Lithosomes Along the Delaware Coast

  • John C. Kraft
  • Elizabeth A. Allen
Conference paper

Abstract

Studies of Holocene coastal sedimentary environments provide a direct key to the interpretation of sediments deposited in coastal and nearshore marine environments of the Atlantic continental shelf during the past 100,000,000 years (Fig. 5-1). Sequences of sediments and patterns and distributions of sedimentary structures can be used to form models for the interpretation of transgressive sequences along the entire Atlantic Coast.

Keywords

Marsh Surface Marine Transgression Plant Fragment Muddy Sand Holocene Transgression 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Kraft, John C. 1971a. Sedimentary fades patterns and geologic history of a Holocene marine transgression. Geol. Soc. Am. 82 ,2131–2158.CrossRefGoogle Scholar
  2. Kraft, John C. 1971b. A Guide to the Geology of Delaware’s Coastal En vironments. Coll. of Marine Studies, Univ. Delaware, Newark.Google Scholar

Copyright information

© Springer-Verlag New York Inc. 1975

Authors and Affiliations

  • John C. Kraft
  • Elizabeth A. Allen

There are no affiliations available

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