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1. Drowned River Valleys
   Drowned River
        Valleys
 -are most extensively
    developed along
     coastlines with
relatively low and wide
     coastal plains.

                          Chesapeake Bay which is
                          located on the mid-Atlantic
                          coast of the United States.
2. Fjord-type Estuaries

Fjord-type Estuary
    -are deep, U-
   shaped coastal
indentures gouged
out by glaciers and
  generally with a
shallow sill at their
mouths formed by
  terminal glacial
      deposits.         The famous fjords of Norway
3. Bar-built Estuaries
•shallow basins, often partly exposed at low tide
•enclosed by a chain of offshore bars or barrier
islands
•broken at intervals by inlets (thus insuring “a free
connection with the sea”
•Sometimes the sand bars are deposited
offshore, but in other instances the barriers may
represent former coastal dunes that have become
isolated by recent gradual rises in sea levels.
•In the former case the estuary develops from a
former marine area, while in the latter case it
develops on a flooded area of former coastal plain.
The “sounds” behind the “outer banks” of North Carolina
        (Cape Hatteras National Seashore Park)
4. Estuaries produced by
         Tectonic Processes
 Estuaries produced
by tectonic processes
      -are coastal
indentures formed by
geological faulting or
 by local subsidence,
  often with a large
inflow of fresh water.
                         San Francisco Bay

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Types of Estuaries - Drowned River Valleys, Fjords, Bar-Built & Tectonic

  • 1.
  • 2. 1. Drowned River Valleys Drowned River Valleys -are most extensively developed along coastlines with relatively low and wide coastal plains. Chesapeake Bay which is located on the mid-Atlantic coast of the United States.
  • 3. 2. Fjord-type Estuaries Fjord-type Estuary -are deep, U- shaped coastal indentures gouged out by glaciers and generally with a shallow sill at their mouths formed by terminal glacial deposits. The famous fjords of Norway
  • 4. 3. Bar-built Estuaries •shallow basins, often partly exposed at low tide •enclosed by a chain of offshore bars or barrier islands •broken at intervals by inlets (thus insuring “a free connection with the sea” •Sometimes the sand bars are deposited offshore, but in other instances the barriers may represent former coastal dunes that have become isolated by recent gradual rises in sea levels. •In the former case the estuary develops from a former marine area, while in the latter case it develops on a flooded area of former coastal plain.
  • 5. The “sounds” behind the “outer banks” of North Carolina (Cape Hatteras National Seashore Park)
  • 6. 4. Estuaries produced by Tectonic Processes Estuaries produced by tectonic processes -are coastal indentures formed by geological faulting or by local subsidence, often with a large inflow of fresh water. San Francisco Bay