Coastal Sedimentary Environments

  • Richard A. DavisJr.

Table of contents

  1. Front Matter
    Pages i-ix
  2. Richard A. Davis
    Pages 1-3
  3. L. D. Wright
    Pages 5-68
  4. Robert B. Biggs
    Pages 69-99
  5. Robert W. Frey, Paul B. Basan
    Pages 101-169
  6. Victor Goldsmith
    Pages 171-235
  7. Richard A. Davis Jr.
    Pages 237-285
  8. Jon C. Boothroyd
    Pages 287-360
  9. John C. Kraft
    Pages 361-383
  10. William T. Fox
    Pages 385-413
  11. Back Matter
    Pages 415-422

About this book


Richard A. Davis The zone where land and sea meet is composed of a variety of complex environ­ ments. The coastal areas of the world contain a large percentage of its population and are therefore of extreme economic importance. Industrial, residential, and recreational developments, as well as large urban complexes, occupy much of the coastal margin of most highly developed countries. Undoubtedly future expan­ sion in many undeveloped maritime countries will also be concentrated on coastal areas. Accompanying our occupation of coasts in this age of technology is a dependence on coastal environments for transportation, food, water, defense, and recreation. In order to utilize the coastal zone to its capacity, and yet not plunder its resources, we must have extensive knowledge of the complex environ­ ments contained along the coasts. The many environments within the coastal zone include bays, estuaries, deltas, marshes, dunes, and beaches. A tremendously broad range of conditions is represented by these environments. Salinity may range from essentially fresh water in estuaries, such as along the east coast of the United States, to extreme hypersaline lagoons, such as Laguna Madre in Texas. Coastal environments may be in excess of a hundred meters deep (fjords) or may extend several meters above sea level in the form of dunes. Some coastal environments are well protected and are not subjected to high physical energy except for occasional storms, whereas beaches and tidal inlets are continuously modified by waves and currents.


Coast Küste Sediment Sedimentation chemistry environment geochemistry sea level

Editors and affiliations

  • Richard A. DavisJr.
    • 1
  1. 1.Department of GeologyUniversity of South FloridaTampaUSA

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