marine erosion Flashcards

1
Q

erosion is divided into two parts..

A
marine processes (base of cliff)
sub-arial processes (cliff face)
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2
Q

marine erosion types

A

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)

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3
Q

sub-arial processes

A
freeze thaw wathering 
salt weathering 
expholiation
biological
carbonation
oxidation
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4
Q

freeze thaw

A

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

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5
Q

slat weathering

A

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

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6
Q

exfoliation

A

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

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7
Q

biological

A

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

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8
Q

sub arial processes- mass movements

A

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

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9
Q

rotational slumps

A

a common mass movement at coasts are rotational slumps,

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10
Q

what does mass movement occour near a coastline?

A

weathering weakens the rockd
rainwater lubricates the cracks
water adds weight to rocks
marine processes undermine the rock making it unstable

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11
Q

sources of coastal sediment

A

rivers bringing sediment from the land to the coast

erosion of cliffs

the sea- tides and waves bring material to the caostline.

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12
Q

factors affecting the rate of marine erosion

A
waves
tides
currents
winds 
sediment supply 
rock reistance 
geology 
fetch length
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13
Q

waves

A

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

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14
Q

tides

A

spring tides= larger area zone for wave attack, neap tides= smaller zone

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15
Q

currents

A

longshore and rip currents carry larger quantities of material

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16
Q

winds

A

onshore winds erode fine beach sand to from dunes
offshore winds may erode dunes and nourish the beach
the longer the fetch, the greate wave-energy potential

17
Q

sediment supply

A

continual supply is necissary for abrasion and attrition, whereas oversupply can protect the coast

18
Q

rock reistance

A

e.g. granites are very resistant whereas unconsoludated volcantic ash or boulder clay have little reistance to wave attack

19
Q

rock geology/ structure

A

many joints or cracks in rocks make them suseptable to erosion
horizontal or verticle structures produe steep cliffs

20
Q

orinetation of the coast

A

headlands with verticle cliffs tend to concentrate wave energy by refraction

21
Q

topography

A

the seabed.
a steep seadbed generates higher and steeper waves than one with a gentle gradient
longhashore bars cause waves to break off shore and loose energy.