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Geography Coast
Landforms of erosion
Cliffs
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Created by
Isabelle Clough
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Cards (6)
What is our hard rock cliff example and what rock type is it
Beachy Head
near
South Coast
Chalk cliffs
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What are the inputs of sediment and energy for Beachy Head
Wind and Waves:
direction of fe
tch=
southwest and it travels across En
glish Channel a
nd is approximately 150-200km
pr
evailing wind c
omes from So
uth west
Tides:
The ti
dal range i
s between 4-5 m
the speed of tidal currents can reach up to 2-3 kn
ots
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What are the controls on the coastline for Beachy Head
Well jointed rock (pressure release may have opened up the bedding planes and joints)
Material deprived from ro
ck fall w
ill be eroded by attrition and eventually removed by lo
ngshore drift
90
m h
igh hard, ch
alk c
liffs with vertical upper profile
chalk has crumbly appearance as a result of weathering (carbonation and physical weathering e.g freeze thaw)
Evidence of huge rock fall- hu
ndreds of thousands o
f tonnes of chalk vertically joins the cliff to the lighthouse
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What is our soft rock cliff example and what rock type is it
Holderness Coast
boulder clay
cliffs
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What are the inputs of sediment and energy for Holderness coast
Wind and Waves:
fe
tch c
an be up to 500-600 km
Prevailing wind direction is generally from the north-east across No
rth Sea
Tides:
The ti
dal range t
ypically ranges between 4-6m
tidal currents considered to be moderate to strong reaching speeds of up to 1.5 to 2 m pe
r second
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What are the controls on the coastline for Holderness Coast
Boulder clay is weak un
consolidated r
ock that cannot maintain a steep profile
There is a jumble of mud and small rocks= could be evidence of an ea
rthflow o
r mudflow
the beach sediment is rounded in by ma
rine processes o
f er
osion (
abrasion & attrition)
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