marine erosion Flashcards
erosion is divided into two parts..
marine processes (base of cliff) sub-arial processes (cliff face)
marine erosion types
hydraulic action (storm or high energy waves hitting a sea wall or cliff foot)
cavitation (water trapped in cracks of the rock, compressed by the pounding of waves and when pressure is relased bubbles form and escape with an explosive nature)
abrasion (sediment hitting the base of the cliff from waves)
attrition (rock falls and slumps mean material is in the warer, moved by waves and hits against eachother)
solution (chemicals in the sea water dissolving rocks especailly limestone or chalk)
sub-arial processes
freeze thaw wathering salt weathering expholiation biological carbonation oxidation
freeze thaw
water seeps into cracks on the cliff face, freezes overnight and the water exampands by 10x, this widnes and weakens thwe crack.
repeated freezing and thawinf can make the rock crumble and split
slat weathering
Salt. weathering is a process of rock disintegration by salts that have accumulated at. and near the rock surface. It is the dominant weathering process in deserts. especially in coastal and playa areas where saline groundwater may be close to.
crystalisation- salt enters cracks and overtime the salt applies pressure onto the rock
exfoliation
extreme tempreture variations between day anmd night= expansion and contraction of the surface layers of rock on the cliff face
the stresses caused by these changes weaken the rock and surface layers peel off, increased availability of water at the coastline can speed up this process
biological
caused by roots of vegetation and nesting birds, cliffs often contrain halophytic (saly-loving) plants that grow in these cracks, widening them leading to biological weathering
seabirds sit of ledges of cliffs, their guano is extremely corrosive and can lead to the chemical weathering of some types of rocks
sub arial processes- mass movements
another sub-arial process is mass movement, the movements of material downslope under the influence of gravity they can be rapid events such as rock falls or landslides or slower ones sychas soil creep
rotational slumps
a common mass movement at coasts are rotational slumps,
what does mass movement occour near a coastline?
weathering weakens the rockd
rainwater lubricates the cracks
water adds weight to rocks
marine processes undermine the rock making it unstable
sources of coastal sediment
rivers bringing sediment from the land to the coast
erosion of cliffs
the sea- tides and waves bring material to the caostline.
factors affecting the rate of marine erosion
waves tides currents winds sediment supply rock reistance geology fetch length
waves
wave steepness- steep destrutive waves have more erosive power thsn construtuve waves
wave breaking point- waves breaking at a cliff base= prime marine erosion, waves breaking off shore loose energy
tides
spring tides= larger area zone for wave attack, neap tides= smaller zone
currents
longshore and rip currents carry larger quantities of material