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Geography - PHYSICAL
geography - coasts
booklet 5 - processes
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Isabel M
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Cards (16)
subaerial processes
-
weathering
-
mass movement
-
run off
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weathering
the weakening and breakdown of
rocks
in
situ
(in place)
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mass movement
downward movement of material due to
gravity
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run off
overland flow
where material is washed down a
slope
, potentially forming an input to the
sediment cell
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mechanical weathering
-
freeze thaw
- wetting and drying
- pressure release
- salt crystallisation
-
exfoliation
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biological weathering
plants
and
animals
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chemical weathering
-
oxidation
-
hydrolysis
- hydration
-
carbonation
- solution
-
acid rain
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where / when might rate of chemical weathering be fastest?
depends on
rock type
-
limestone
breaks down with
acid rain
and calcium carbonate on the coast
- exposure to salt spray
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where / when might rate of mechanical weathering be fastest?
-
onion skin weathering
in hot climates
-
freeze thaw weathering
- temps above and below freezing,
hard rock
with lots of cracks / fault lines
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what is mass movement dependent on?
- the
cohesion
of sediment
- the
height
and angle of slope
-
grain size
within the sediment
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types of mass movement
-
soil creep
-
mud flows
- rockfall
-
rotational slumping
-
landslide
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soil creep
- slow form of
movement
of individual soil
particles
downhill
- involves particles rising towards ground surface due to
wetting
/
freezing
then returning to surface as soil dries /
thaws
- action implied by formation of shallow
terracettes
(build up of soil on upslopes)
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mud flows
- earth and mud flowing downhill usually over
unconsolidated
/ weak rock, often after
heavy rainfall
- water gets trapped, increasing pressure, forces
rock particles
apart
- often sudden and fast flowing
--- represent significant
natural hazards
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rockfalls - AKA blockfalls
- sudden collapse/ breaking away of individual rock fragments
- commonlyh associated with steep or vertical cliffs in quite resistant rock
- triggered by
mechanical weathering
or
earthquake
- rocks fall down slope to form a
scree
at foot of slope
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rotational slumping
- found in
unconsolidated
sands + clays
- slide surface is curved
- when permeable rock overlies impermeable rock, causing build up of
pore water pressure
- multiple landslips result in
terraced
appearance on cliff face
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landslide
- frequently triggered by
earthquakes
/ very heavy
rainfall
- when
slip
becomes lubricated +
frictions
reduced
- tend to be
rapid
+ pose considerable threat to people and property
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