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Physical Landscapes in the UK
Coasts
Coastal Processes
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Cards (16)
Hydraulic Action
High pressure
water
causes
cracks
to force apart and widen
Abrasion
Rocks
eroding
by
rubbing
on the
river bed
Attrition
Rocks
eroding
by
hitting
each other
Constructive waves
Strong
swash
, weak
backwash
Builds
up
beaches
Small wave height,
long
wavelength
Destructive waves
Weak swash
,
strong backwash
Destroys beaches
Large wave height
,
short wavelength
Mechanical
weathering
is the breakup of rock without changing its chemical composition
Chemical weathering
is the breakdown of rock by changing its chemical composition
Slightly
acidic
rain can chemically
weather
rocks causing them to
dissolve
Mass movement
is the
downhill movement
of
cliff material
under the influence of
gravity
Types of mass movement are
Sliding
Slumping
Rock falls
Slumping
occurs when the base of a cliff is
eroded
and then the
saturated weight
causes it to
collapse
Landslides occur when the
base
of a cliff is
eroded
leaving a
wave cut notch
and then the cliff
collapses
under it
weight
Rockfall
occurs when rock fragments break away from the cliff face often due to
freeze-thaw
weathering
Longshore drift
is the movement of material along the shore by
wave action
Longshore drift
Swash moves at an angle due to the
prevailing
wind
Backwash is
perpendicular
to the beach due to
gravity
Process
repeats
and
sediment
is transported across the beach
Deposition
is when
material
that is being
transported
is
dropped
by
constructive waves
because
waves
have
less energy