Topic3(2)- Coastal Processes Flashcards

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1
Q

Six main ways waves erode coast

A

1) corrasion (abrasion)
2) hydraulic action
3) cavitation
4) wave quarrying
5) solution (corrosion)
6) Attrition

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2
Q

Abrasion (corrasion)

A

Bits of rock/sediment transported by waves smash and grind against rocks and cliffs, breaking bits off & smoothing surfaces

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3
Q

Hydraulic action

A

Air in cracks in cliffs is compressed when waves crash in. The pressure exerted by compressed air breaks off rock pieces

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4
Q

Cavitation

A

As waves recede, the compressed air expands violently, again exerting pressure on the rock causing pieces to break off

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5
Q

Wave quarrying

A

The energy of a wave as it breaks against a cliff is enough to detach bits of rock

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6
Q

Solution (corrosion)

A

Soluble rocks (limestone n chalk) get gradually dissolved by the seawater

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7
Q

Attrition

A

Bits of rock in water smash against each other and break into smaller bits

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8
Q

4 main processes of transportation

A
  1. Solution
  2. Suspension
  3. Saltation
  4. Traction
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9
Q

Solution (transportation)

A

Substances that can be dissolved are carried along in the water e.g limestone in slightly acidic water

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10
Q

Suspension

A

Very fine material, like silt and clay, is whipped up by turbulence (erratic swirling of water) and carried along in water

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11
Q

Saltation

A

Larger particles, such as pebbles, are too heavy to be carried via suspension. Instead the force of water causes them to bounce along sea bed

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12
Q

Traction

A

Very large particles, like boulders, are pushed along sea bed by force of water

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13
Q

Longshore drift

A

1) Swash carries sediment up the beach, parallel to prevailing wind. Backwash carries sediment down beach at right angles to shoreline
2) when theres an angle between the prevailing wind and the shoreline, a few rounds of swash and backwash move the sediment along coastline

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14
Q

Deposition and its 2 types

A

When material being transported is dropped on the coast

1) marine deposition - sediment carried by sea water deposited
2) Aeolian deposition- sediment carried by wind deposited

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15
Q

When do Marine and Aeolian deposition happen? And why?

A

-When the sediment load exceeds the ability of water or wind to carry it
-this can happen due to an increase in sediment load or wind or water flow slows down (less energy)
-

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16
Q

2 reasons wind and water slow down:

A

1) friction increases (shallow water or wind reaches land, friction slows them down)
2) Flow becomes turbulent (encountering of an obstacle- flow becomes rough and speed decreases)

17
Q

What happens to waves if wind slows down

A

Wave height, speed and energy decrease

18
Q

Sub-aerial weathering

A

Gradual break down of rock by agents such as ice, salt, plant roots and acids. Weathering weakens cliffs, making them more vulnerable to erosion

19
Q

4 types of Sub-aerial weathering

A

1) salt weathering
2) freeze-thaw weathering
3) chemical weathering
4) wetting and drying

20
Q

Salt weathering

A
  • caused by saline (salty) water
  • saline water enters cracks in rocks at high tide
  • as tide goes out, rocks dry and water evaporates, forming salt crystals
  • the salt crystals expand as they form, exerting pressure on the rock, causing pieces to fall off
21
Q

Freeze-thaw weathering

A
  • occurs in areas where temperatures fluctuate above and below freezing
  • water enters joints and crevices in rocks
  • if temp. drops below 0 celcius, water freezes and expands in cracks
  • over time, repeated freeze-thaw weakens the rocks and causes pieces to fall off
22
Q

Chemical weathering

A
  • the breakdown of rock by changing its chemical composition
  • e.g. Carbon dioxide in atmosphere dissolves in rainwater, forming a weak carbonic acid. This acid reacts with rock which contains calcium carbonate
23
Q

Wetting and drying

A
  • some rocks contain clay

- when clay gets wet, it expands and the pressure causes fragments of rock to break off

24
Q

Mass movement

A

The shifting of material downhill due to gravity
In coastal areas its most likely to occur when cliffs are undercut by wave action (unsupported overhang causing it to collapse)

25
Q

4 types of mass movement

A

1) Slides
2) Slumps
3) Rockfalls
4) Mudflows

26
Q

Slides

A

Material shifts in a straight line

27
Q

Slumps

A

Material shifts with a rotation

28
Q

Rockfalls

A

Material breaks up and falls

29
Q

Mudflows

A

Material flows downslope

30
Q

Factors affecting mass movement

A
  • unconsolidated rocks are prone to collapse as theres little friction between particles to hold them together
  • heavy rain, can saturate unconsolidated rock , further reducing friction making it more likely to collapse
  • Runoff can erode fine particles and transport them downslope