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The Cape Fear River
Estuary, as seen from space |
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San Francisco Bay, as seen from space.
Photo courtesy of the U.S. Geological
Survey |
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Albemarle-Pamlico Sound, as seen from space.
Photo courtesy of the U.S. Geological
Survey |
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A glacier and fjord in Chile, as seen from space.
Photo courtesy of
the National Aeronautics and Space
Administration (NASA), Johnson Space Center, Earth
Sciences and Image Analysis |
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No two estuaries are the same! One way that they are
grouped is by their
geology.
There are coastal plain estuaries,
tectonic
estuaries,
bar-built estuaries, and
fjords.
Coastal plain
estuaries formed during the end of the last
ice age.
At this time,
sea
level rose because of melting ice and warming ocean waters. The rising
water flooded coastal river
valleys,
forming estuaries. The Cape Fear River estuary is a
coastal plain estuary.
Tectonic estuaries form when the Earth’s
crust
folds or breaks to make
faults. Part of the land sinks and forms a hollow basin.
When the basin is filled in by the sea, an estuary is formed. San
Francisco Bay is a tectonic estuary.
Bar-built estuaries are found where
sand bars form
on a coastline. The
water behind the sand bars are partly cut off from the sea.
The Albemarle-Pamlico Sound behind the Outer Banks is a bar-built estuary.
Fjords are deeply cut valleys that are formed by the movement of
glaciers. When
glaciers moved north at the end of
the last ice age, the sea filled in the valleys and formed
estuaries. There are many fjord in the
Click on any of the maps on this page to enlarge
them for a closer look. Click on the bird at left to continue...
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