Coastal processes and landforms Flashcards
Onshore coast
60km inland
370km out to sea
Constructive waves
longer wavelength strong swash weak backwash shallow gradient waves beach builds up
Destructive waves
short wavelength weak swash strong backwash steep gradient waves erodes beach
attrition
sea carries rocks which knock against each other
the force breaks and chips the rocks so they become smaller and more rounded
abrasion
waves pick up stones and hurl them at cliffs
this wears down the rock surface
solution
sea water dissolves certain rocks
hydraulic action
the force of the waves hitting against the cliff forces pockets of air into the cracks and crevices, weakening the rock
biological weathering
animals burrowing or roots growing inside the bedrock of the cliff face, expand and weaken the rock until it breaks off
physical weathering
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
Chemical weathering
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
rock fall
fragments of rock break away from cliff face due to weathering
landslide
erosion forms a wave-cut notch at the base of the cliff
the weight of the cliff can’t support itself and collapses
mud slide
saturated soil and weak rock flows down a slope
slumping
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
Longshore drift
- prevailing winds blow in from an oblique angle
- this causes the swash of waves to move diagonally up the beach, moving sediment as well
- backwash moves material down the gradient of the beach at a right angle due to gravity
- process repeats, moving sediment up the coast
- until sediment is deposited at the river mouth
Headlands
- At discordant coastlines, differential erosion occurs, so less resistant(sand and clay) rock retreats quicker
- harder rock(chalk) is left protruding as a headland
- waves refract around the headland, concentrating their orthogonal energy on the sides
- This further erodes the headland
Caves
Erosion on the sides of the headland widen the crack due to the concentrated orthogonal energy after the waves have refracted round
Arch
erosion continues, cave becomes larger and breaks through headland
Stack
Base of arch widens until the roof becomes too heavy to support itself and collapses into the sea, leaving a pillar of rock
Stump
stack is undercut at the base, weakening the structure until it eventually collapses
Rjas
drowned river valley
Fjords
drowned glacial valleys
Spit
deposited material at river mouth created by longshore drift
eg. spurn head
Wave-cut platform
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
bar
spit formed across a bay
e.g. Slapton
tombolo
spit joins the land to and island
e.g. chesil beach
Cuspate foreland
deposition in an area where two opposing longshore drifts meet(triangle)
4 Hard engineering examples
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
4 Hard engineering disadvantages
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
6 Soft engineering examples
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
Reasons for managed retreat
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)
Mass movement
bulk movements of soil and rock debris down slopes in response to the pull of gravity
4 types: rock fall slumping landslide mudslide