G131 HOME
INFORMATION
SCHEDULE
RESOURCES
EXERCISES
NOTES
Links to summaries of key issues for each topic
PREAMBLE
Introduction
History

PART I
Water Planet
Plate Tectonics
Sea Floor
Review 1
Physical Prop.
Chemistry
Ocean Stuct.

PART II
Atmosphere
Currents
Review 2
Waves
Tides

PART III
Coasts/Beaches
Environ. for Life
Production
Plankton
Nekton
Benthos
Review 3



VISUALS

Links to images employed in lectures on a topic-by-topic basis

TEXT
Link to chapter outlines at online learning center at McGraw Hill.
NOTES
Links to summaries of key issues for each topic

 
Coasts, Beaches and Estuaries

Notes on Topic:

  • The notes represent summaries of key issues for each topic
  • They emphasize the terminology used to describe the various phenomena.

  • 1. Coastal Zones:
    Learning Objectives: 
    • Comprehension of the features associated with coastlines
    • Understanding of the factors that govern coastal characteristics
    Forms and Types of Coasts: 
    • Forms of coastline: 
      • cliffs, dunes, beaches, bays, coves, river mouths and the ocean.
      • shore: region extending out to limit of wave action
      • beach: accumulation of sediment affected by coastal processes.
    • Types of coasts:
      • landforms and processes: geomorphology
      • modified by sea level changes
      • affected by rivers, currents, storms, ice, corals
      • coastal characteristics are governed by either land or ocean processes: 
        • land - primary coasts:
          • erosion by water, wind, ice, sea level
          • sediments from rivers, wind, glaciers
          • volcanic activity, e.g. lava flow
          • earth movements, e.g. earthquakes; 
        • ocean - secondary coasts: 
          • erosion due to waves, currents, seawater
          • deposition of sediments by waves, tides, currents
          • alteration by marine plants and animals

    Primary Coasts:
    • U-shaped valleys carved by glaciers: fjords. 
      • often with a shallow sill at entrance
      • moraine formed from debris deposited by glacier when it retreated
    • V-shaped valleys formed from river valleys drowned by sea-level rise
    • Deltas: 
      • sediment deposits from suspended load at river mouths
      • alluvial plains formed by sediment deposits. 
    • Dune coasts: 
      • wind modified formed by migration of sand
    • Lava coasts, cratered coasts: 
      • shaped by volcanic deposits and processes
    • Tectonic Coasts: 
      • fault-dominated systems
    Secondary Coasts:
    • Produced by marine processes of deposition and erosion
    • Cliffs, or pinnacles, sea stacks 
    • Eroded materials may form bars, barrier islands, sand spits, hooks
    • Reef coasts: biological influence
    • Mangroves and salt marshes: 
      • plants retain sediments
      • periodically flooded by tides.
    2. Beaches:
    Learning Objectives: 
    • Appreciation of beach characteristics and approaches to their description
    • Understanding of the dynamic forces that shape and change beaches over time
    Characteristics:
    • Shoreline divided into zones: 
      • offshore, inshore (where breakers occur)
      • foreshore (low to high tide)
      • backshore (affected by storms)
      • typical features: 
      • sand bars, longshore bars and troughs, (parallel to coastline)
      • summer and winter berms (high tide crest)
        • changed by storms and storm surges
          • requires strength to erode & deposit
      • wave-cut scarps, terraces, longshore bars and troughs.
    • Beaches are described by:
      • shape and structure: 
        • whether wide or narrow, steep or flat, long or discontinuous,
        • spits and tombolos
      • composition (sand, coral, shells, lava) 
      • size (mud, sand, pebbles) 
        • depend on processes and forces acting on beach 
        • lag deposits, armored beach.
      • color: 
        • white, black, green, pink sands.
    Beach Dynamics:
    • A dynamic equilibrium between depositional and erosion processes
      • differs from summer to winter. 
    • Motion of water: 
      • onshore current creates surf zone 
      • longshore current parallel to shore moves sediment
      • longshore transport within drift zone
      • up-rush of waves: swash, may form cusps. 
    • Accreting regions where deposition occurs
      • rip current carry sediment away as part of coastal circulation. 
    • Sediment budgets of beaches can be described as littoral cells
      • sand accumulates or is lost by offshore transport, or wind.


     
       
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    Indiana University
    Department of Geological Sciences, 
    1001 E. Tenth Street, Bloomington, IN 47405-1403
    Phone: (812) 855-5582  Last updated: 7 December 2000
    Comments: simon@indiana.edu
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