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Physical geography
Coastal landscapes
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Cards (94)
Inputs to coastal systems
wind
Waves
Tides
Sea
currents
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Outputs from coastal systems
Sediments
washed out
to sea
Sediments
deposited
further along the coast
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Flows/transfers within coastal systems
1.
Erosion
2.
Weathering
3.
Transportation
4.
Deposition
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Stores/components of coastal systems
Beaches
Dunes
Spits
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Dynamic equilibrium
Inputs
and
outputs
are balanced in coastal systems
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Change in one input or output
Often causes
negative feedbacks
that restore the
balance
of the system
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Negative feedback
System causes other
changes
to have the
opposite
effect
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Positive feedback
Change in the system causes other
changes
to have a
similar
effect
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Wind
Created by air moving from
high
to
low
pressure
Stronger during storms due to high
pressure
gradient
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Strong winds
Generate powerful
waves
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Prevailing winds
Consistently blow from the
same
direction, causing
higher-energy
waves
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Waves
Created by
wind
blowing over
sea
surface
Wave
height
affected by wind
speed
and
fetch
Waves break as they approach
shore
, with
swash
and
backwash
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Constructive waves
Low
frequency,
low
height but
long
, powerful
swash
carries
material
up beach
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Destructive waves
Higher
frequency,
high
and
steep
, strong
backwash
removes
material
from beach
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Tides
Periodic
rise
and
fall
of ocean surface, caused by
gravitational
pull of
moon
and
sun
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Tides
Affect
position
where waves
break
on beach
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Currents
General flow of
water
in
one
direction, caused by
wind
or variation in
temperature
and
salinity
Move
material
along the coast
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High energy coasts
Receive
high
inputs of
energy
from
powerful waves
, have sandy coves and rocky landforms,
erosion
rate greater than
deposition
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Low energy coasts
Receive
low
inputs of
energy
from small, gentle waves, have
salt marshes
and
tidal mudflats
,
deposition
rate greater than
erosion
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Sediment sources
Rivers
Sea
level rise
flooding
river valleys
Cliff
erosion
Crushed
marine organism
shells
Offshore
deposits
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Sediment budget
Difference between
sediment entering
and
leaving
coastal system
Positive
budget = coastline
builds outwards
Negative
budget = coastline
retreats
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Sediment cells
Lengths of coastline that are
self-contained
for sediment movement,
processes
in one cell do not affect
another
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6 main ways waves erode the coastline
Corrosion
(abrasion)
Hydraulic
action
Cavitation
Wave
quarrying
Solution
Attrition
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Corrosion (abrasion)
Bits of
rock
and
sediment
being carried by
waves
, are
smashed
and
grinded
against the seabed and cliffs, therefore becoming
smoother
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Hydraulic action
Air cracks in
cliffs
are compressed when
waves
crash in. The
pressure
exerted by the
compressed
air breaks off
rock
pieces
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Cavitation
As waves
recede
, the
compressed
air expands violently, again exerting
pressure
on rocks and causing them to
break
off
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Wave quarrying
The
energy
of a wave as it breaks against a
cliff
is enough to
detach
bits of rock
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Solution
Soluble
rocks being
dissolved
in seawater
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Attrition
Rocks smash against
each other
and break into
smaller
bits
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Processes of sediment transportation
Solution
Suspension
Saltation
Traction
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Solution
Substances that can be
dissolved
are moved along with the
water
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Suspension
Very fine material, such as silt and clay particles are whipped up by
turbulence
and carried along the water. Most
eroded
material is transported this way
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Saltation
Larger particles, such as pebbles or gravel are too heavy to be carried by suspension. Instead, they
bounce
along the
seabed
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Traction
Large
boulders are rolled along the
seabed
by the force of
water
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Longshore drift
Process of
sediment
transported along the
shore
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Swash
Carries
sediment
up the beach
parallel
to prevailing wind
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Backwash
Carries
sediment
back
down
beach at a right angle to shoreline
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Types of deposition
Marine
deposition
Aeolian
deposition
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Marine deposition
Sediment
carried by
seawater
is deposited
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Aeolian deposition
Sediment
carried by
wind
is deposited
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