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Chapter 11: The Coast: Beaches and Shoreline Processes

Chapter 11: The Coast: Beaches and Shoreline Processes. Coastal region. Shore between low tide and highest elevation affected by storm waves Coast from shore to farthest inland ocean features. Fig. 11-1. Beach. Actively changing Shore: backshore, foreshore, nearshore, offshore

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Chapter 11: The Coast: Beaches and Shoreline Processes

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  1. Chapter 11: The Coast: Beaches and Shoreline Processes

  2. Coastal region • Shore between low tide and highest elevation affected by storm waves • Coast from shore to farthest inland ocean features Fig. 11-1

  3. Beach • Actively changing • Shore: backshore, foreshore, nearshore, offshore • Berm, beach face, longshore bar, longshore trough Fig. 11-1

  4. Beach composition and shape • Locally available material • Coarser sediment • Beach steeper • Finer sediment • Beach more gentle

  5. Sand movement • Swash and backwash • Sediments moved up and down beach face • Smaller, low energy waves sand moved up beach face • Summertime beach • Larger, high energy waves sand moved off shore • Wintertime beach

  6. Sand movement • Longshore current • Longshore drift or transport • Parallel to shore • Increasing strength • More wave energy • Higher wave frequency • Steeper beach • Greater angle

  7. Longshore current main way sediments moved along coasts • Southward along both U.S. coasts most of the time

  8. Erosional-type shore • Headlands eroded • Sea arches • Sea stacks • Wave-cut cliffs • Sea caves • Tectonically active coasts • Example Pacific coast U.S.

  9. Depositional-type shores • Sediments re-distributed by ocean processes • Typical in tectonically passive areas

  10. Depositional features • Spit • Tombolo • Bay barrier or baymouth bar Fig. 11-7

  11. Barrier islands • Ocean beach • Dune • Barrier flat • High salt marsh • Low salt marsh • Lagoon • Rising sea level pushes barrier island landward Fig. 11-10

  12. Deltas FIG. 11.11b • Rivers deposit sediment at coast • If more fluvial influence than ocean influence • Bird’s foot delta • If more ocean influence than river influence • Arcuate delta

  13. Shepard classification of coasts • Primary • Geologically youthful • Controlled by non-marine processes • Examples • “Drowned” river or glacial valleys • Volcanic coasts • Coasts shaped by recent tectonic movements

  14. Secondary coasts • Geologically mature • Controlled by marine processes • Tectonically passive • Examples • Straightened coasts • Coral reefs • Marsh grass Fig. 11-13f

  15. Emergent coasts • Uplift or sea level drops • Once marine is now land • Marine terraces • Stranded beach deposits

  16. Submergent coasts • Subsidence or sea level rises • Once land (or shallower) is now underwater (or deeper) • Drowned beach deposits • Drowned river/glacial valleys • Submerged dunes

  17. Tectonic and isostatic changes • Tectonic uplift and subsidence • Larger scale: major parts of continents • Smaller scale: local deformation • Isostatic adjustments to loading • Sediments or ice • Regional and local effects • Affect sea level

  18. Eustatic changes in sea level • Global • Changes in spreading rates of ocean floor • Changes in ice volumes • Changes in ocean temperature • Global warming • Sea level rises • Ice melts, ocean warmer Fig. 11-15

  19. Atlantic coast of U.S. • Mainly submergent • Barrier islands • Glaciers shaped some shorelines • Eroding coasts • Subsidence in most areas

  20. Gulf coast of U.S. • Mainly submergent • Barrier islands • Mississippi delta • High rates of erosion • Tectonic subsidence

  21. Pacific coast of U.S. • Mainly emergent • Less erosion • Mainly rocky shoreline • Dams on rivers beach starvation • Tectonically active

  22. U.S. coastal erosion, deposition Fig. 11-17

  23. Hard stabilization • Groin and groin field • Perpendicular to shore • Traps sand between groins • Interrupts longshore current • Jetty similar • Built to protect harbor entrance • Sand on upcurrent side

  24. Breakwater • Parallel to shore • Offshore • Deposition behind breakwater

  25. Seawall • Built on beach • Parallel to beach • Erosion enhanced seaward of wall • Seawall destroyed • Beach narrowed Fig. 11-25

  26. Alternatives to hard stabilization • Limit construction near shore • Relocate businesses/homes destroyed by wave erosion

  27. End of Chapter 11: The Coast: Beaches and Shoreline Processes

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