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