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Lithosphere
Coastal deposition features
Sand bar
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Created by
Evie Yates
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Bars
form when there is a
change
in
direction
on a
coastline
which allows a
sheltered
area for
deposition.
Bars form when a
spit
grows across the
entrance
to a
bay
due to
long shore drift
(explain) (and
more
constructive waves than destructive waves).
A spit
growing
across a
bay
connects two
headlands
and
enclsoes
a sheltered
lagoon
behind it.
The
lagoon
forms as there is no
strong
flow of
river
water to the
sea.
Through time a
lagoon
(
stagnant
water) is filled in by
deposition.
Sand bar example:
Chesil beach