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inspector calls
Geography
UK physical landscapes
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megan mansfield
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Cards (18)
chemical
weathering
caused by a chemical reaction when
rainwater
hits rock and
decomposes
it or eats it away
mechanical weathering
when rocks are
disintegrated
freeze-thaw weathering
when water enters a crack and freezes,
expanding
the crack
( ice is
9
% bigger than water )
slumping
common with cliffs made from
clay
heavy rainfall
causes the clay to become saturised, making it too
heavy
for it to support itself
this means the clay
falls
and
oozes
down toward the sea
creates a
slip plane
rock-falls
falling rocks which come from
freeze-thaw
weathering process
at the bottom of the cliff face, they form a
scree-slope
hydraulic action
water
crashes against cliffs
air and
water
is trapped and compressed into
cracks
when sea moves away, air expands and weakens the rock
cracks enlarge and rocks break away
abrasion
caused by falling rock fragments battering the
land
, and
breaking
off other pieces of rock
attrition
when rock fragments collide into eachother, getting
smaller
and
smoother
solution
chemical action of sea and rock, dissolved rock in water (
limestone
)
longshore drift occurs when waves break at an
oblique
angle to the shore
traction
larger
pebbles
are
rolled
along the sea bed
suspension
fine sediment is carried in the water,
suspended.
makes the water look
murky
saltation
small
pebbles
are moved when another
pebbles
hits against another. causes a chain reaction
a
concordant coastline
is when rocks are parrelel to the coastline
a
discordant
coastline is where rocks are
perpendicular
to the coastline
wave
cut platform
waves erode rocks through hydraulic action, abrasion and corrosion
a notch is slowly formed at the high water mark
the rock above the notch slowly becomes unstable, and it collapses
a wave cut platform is formed as this process continues, as the base of the cliffs are left as the cliff receeds
swash aligned beaches
are where
waves
are directly parralel to the shore
drift aligned beaches
form when waves approach the beach at an angle