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geography
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maddie levy
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Cards (52)
waves forming
wind
blows over the
sea
friction
on water surface causes ripples
distance wind blows across sea
fetch
bigger the fetch
bigger
the wave
constructive waves
storms
far
away
low
waves
more
swash
than
backwash
destructive waves
local
storms
waves
close
together
more
backwash
than
swash
weathering
the
weakening
or decay of rock due to action of
weather
,
plants
or
animals
mechanical- disintegration of rock
freeze-thaw
water
collects in cracks of rock
water
freezes
and
expands
temp
rise
and water seeps deeper
repetition
= rock fragments fall and collect as
scree
chemical - chemical changes
carbonation
rainfall absorbs
CO2
from air - acidic
contact with
alkaline
rocks
reaction
where rocks slowly dissolve
biological - flora and fauna
plant roots grow in
cracks
and animals
burrow
mass movement
sliding
of weathered material under the influence of
gravity
rockfall
rock breaks away due to
freeze thaw
landslide
blocks of
rock
slide downhill
mudflow
saturated
soil
flows downhill
rotational slip
slump of
saturated
soil along
curved
surface
erosion
wearing away the
landscape
solution
dissolving of
soluble
chemicals
corrasion
rock fragments picked up by
sea
thrown at cliffs
abrasion
sandpaper
- pebbles grinding over rocky platform
attrition
rock
knock
against each other
hydraulic power
waves
hit cliff
transportation
moving of the
rocks
solution
dissolved
chemicals
suspension
particles
carried
within water
traction
rolling
saltation
bouncing
why is sediment deposited
water
slows
down and waves lose their
energy
longshore drift
movement of
sediment
depending on the direction the waves approach the coast as a result of
prevailing
wind
waves approaching head on the beach
sediment moves
up
and
down
waves approaching at an angle
sediment moves in a
zig-zag
pattern
factors affecting coastal landforms
rock
type
geological
structure
headlands and bays
tougher
,
resistant
rock is eroded slowly forming
headlands
weaker
rock
erodes faster forming bays
bays are sheltered, deposition occurs -> beach
caves , arch , stack
abrasion
and
hydraulic
power widen fault ->
cave
erosion
leads to arch
arch enlarged and roof attacked by weathering
leaves isolated
stack
stack erodes and leaves a
stump
wave-cut platforms - erosion
waves
break against a cliff
erosion
causes a
wave-cut
notch
undercuts cliff
repetition
->
wave-cut
platform
beaches - deposition
deposits
of
sand
and
shingle
by
constructive waves
development of sand dunes - deposition
dunes form around
obstacles
stabilised
by vegetation (marram grass)
decomposing
vegetation fertilises sand
ponds
can form depressions
spits and bars - deposition
longshore
drift
transports sand across the coast
change in
shape
of coastline
spit grows from
land
out to sea
spit exposed to changes in
wind
+
wave direction
causing it to
curve
saltmarsh
forms in sheltered water
sand dunes
sand blown inwards and
builds
up
swanage
- south coast of england
coastlines - swanage ?
discordant
and
concordant
famous erosion landform?
old
harry stack
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