Coastal processes and landforms Flashcards

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1
Q

Onshore coast

A

60km inland

370km out to sea

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2
Q

Constructive waves

A
longer wavelength
strong swash
weak backwash
shallow gradient waves
beach builds up
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3
Q

Destructive waves

A
short wavelength
weak swash
strong backwash
steep gradient waves
erodes beach
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4
Q

attrition

A

sea carries rocks which knock against each other

the force breaks and chips the rocks so they become smaller and more rounded

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5
Q

abrasion

A

waves pick up stones and hurl them at cliffs

this wears down the rock surface

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6
Q

solution

A

sea water dissolves certain rocks

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7
Q

hydraulic action

A

the force of the waves hitting against the cliff forces pockets of air into the cracks and crevices, weakening the rock

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8
Q

biological weathering

A

animals burrowing or roots growing inside the bedrock of the cliff face, expand and weaken the rock until it breaks off

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9
Q

physical weathering

A

freeze-thaw
- water fills a crack in a rock, freezes and expands 9%. This repeats, the crack widening until scree breaks off

haloclasty
- salt crystals build up in cracks, expanding and weakening the rock until the scree breaks off

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10
Q

Chemical weathering

A

carbonation
- atmospheric CO2 reacts with water to make carbonic acid CO2 + H2O -> H2CO3
This acid rain reacts with calcium carbonate in certain rock(e.g. limestone), dissolving it
H2CO3 + CaCO3 -> Ca(H2CO3)2

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11
Q

rock fall

A

fragments of rock break away from cliff face due to weathering

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12
Q

landslide

A

erosion forms a wave-cut notch at the base of the cliff

the weight of the cliff can’t support itself and collapses

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13
Q

mud slide

A

saturated soil and weak rock flows down a slope

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14
Q

slumping

A

rain infiltrates cliffs made up off soil and boulder clay
the pore pressure is increased
the weight of the saturated cliff causes a rotational movement along a curved slip plane

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15
Q

Longshore drift

A
  1. prevailing winds blow in from an oblique angle
  2. this causes the swash of waves to move diagonally up the beach, moving sediment as well
  3. backwash moves material down the gradient of the beach at a right angle due to gravity
  4. process repeats, moving sediment up the coast
  5. until sediment is deposited at the river mouth
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16
Q

Headlands

A
  1. At discordant coastlines, differential erosion occurs, so less resistant(sand and clay) rock retreats quicker
  2. harder rock(chalk) is left protruding as a headland
  3. waves refract around the headland, concentrating their orthogonal energy on the sides
  4. This further erodes the headland
17
Q

Caves

A

Erosion on the sides of the headland widen the crack due to the concentrated orthogonal energy after the waves have refracted round

18
Q

Arch

A

erosion continues, cave becomes larger and breaks through headland

19
Q

Stack

A

Base of arch widens until the roof becomes too heavy to support itself and collapses into the sea, leaving a pillar of rock

20
Q

Stump

A

stack is undercut at the base, weakening the structure until it eventually collapses

21
Q

Rjas

A

drowned river valley

22
Q

Fjords

A

drowned glacial valleys

23
Q

Spit

A

deposited material at river mouth created by longshore drift

eg. spurn head

24
Q

Wave-cut platform

A

Sea erodes at the base of the cliff at high tide to create a wave-cut notch
as notch increases in size, the cliff becomes unstable and collapses, leading to the retreat of the cliff face
backwash carries away the eroded deposit, leaving a wave-cut platform

25
Q

bar

A

spit formed across a bay

e.g. Slapton

26
Q

tombolo

A

spit joins the land to and island

e.g. chesil beach

27
Q

Cuspate foreland

A

deposition in an area where two opposing longshore drifts meet(triangle)

28
Q

4 Hard engineering examples

A

recurved steel wall(reflects energy)
gabion - steel wire mesh cage filled with small rocks
riprap - large boulders(rock armour)
groyne - traps sediment carried by LSD

29
Q

4 Hard engineering disadvantages

A

expensive to build and maintain
can’t keep up with pace of rising sea levels
visual pollution
terminal groyne syndrome
- starves beach further down the coast, increasing rate of erosion elsewhere

30
Q

6 Soft engineering examples

A

beach nourishment
cliff regrading and drainage- reduce mass movement
dune regeneration- marram grass planted to trap sand
salt marsh conservation
reprofiling-sediment moved from lower to upper beach
fencing, hedging and replanting vegetation

31
Q

Reasons for managed retreat

A
political policy of austerity
- limited funding for engineering
eustatic yearly sea rise of 3mm
- pressure of engineering
isostatic readjustment
- sea taking over combats southeast sinking
creates new salt marshes(carbon sinks)
32
Q

Mass movement

A

bulk movements of soil and rock debris down slopes in response to the pull of gravity

4 types:
rock fall
slumping
landslide
mudslide