Coastal Processes Flashcards

1
Q

Marine processes

A

ARE caused by sea

Erosion, transportation and deposition

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2
Q

Sub-aerial processes

A

Aren’t directly caused by the sea
(Land based)

(Weathering, runoff and mass movement)

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3
Q

Positive Feedback in Weathering

A

Rate of debris removal exceeds the rate of weathering/mass movements

POSITIVE FEEDBACK as the rate of weathering/mass movement could increase

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4
Q

Negative Feedback in Weathering

A

Debris removal is slow and ineffective, leads to a build up of debris that reduces the exposure of the cliff face

NEGATIVE FEEDBACK as the weathering/mass movement rate will decrease further

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5
Q

Mass Movement

A

The downhill movement of weathered material under the force of gravity

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6
Q

When is a mass movement most likely to occur?

A

When cliffs are undercut by wave action - this causes an unsupported overhang, which is likely to collapse

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7
Q

Types of mass movement?

A
  1. Landslides (straight line)
  2. Slumps (with rotation)
  3. Rockfalls (breaks up and falls)
  4. Mudflows (downslope)
  5. Soil Creep
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8
Q

Landslides

A

Rate: usually rapid
Wet/Dry: both
Movement: slide

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9
Q

Slumps

A

Rate: usually rapid
Wet/Dry: both
Movement: slide

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10
Q

Rockfalls

A

Rate: rapid
Wet/Dry: dry
Movement: fall

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11
Q

Mudflows

A

Rate: often quite rapid
Wet/Dry: wet
Movement: flow

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12
Q

Soil creep

A

Rate: imperceptible
Wet/Dry: wet
Movement: creep

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13
Q

Unconsolidated rocks are prone to collapse as there’s little ________ between the _________ to hold them together

A

Friction

Particles

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14
Q

________ ______ can saturate unconsolidated rock, further reducing ________ and making it more likely to ___________

A

Heavy rain
Friction
Collapse

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15
Q

________ (the flow of water over the land) can ________ fine particles and transport they downslope

A

Runoff

Erode

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16
Q

Sub-aerial weathering is the ________ break down of _____ by agents such as…

A

Gradual
Rock

Ice
Salt
Plant roots
Acids

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17
Q

Weathering…

A

Weakens cliffs and makes them more vulnerable to erosion

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18
Q

Biological Weathering

A

The breakdown of rocks by organic activity is biological weathering

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19
Q

Biological weathering (3)

A

– Plant roots grow into cracks (cracks grow) as roots widen

– Water running through decaying vegetation becomes acidic

– Birds and animals dig burrows into cliffs (puffins and rabbits)

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20
Q

Chemical weathering

A

Involves a chemical reaction where salts may be dissolved or a claylike deposit may result (easily eroded)

21
Q

Chemical weathering (3)

A

– Carbonation (rainwater absorbs C02 = weak carbonic acid) reacts with CaCO to form calcium bicarbonate - easily eroded

– Oxidation (rock minerals - e.g. iron —> rust)

– Solution (Dissolving of rock minerals)

22
Q

Physical weathering

A

Involves the break up of rocks without any chemical changes taking place

23
Q

Physical weathering (3)

A

– Freeze thaw weathering (water increases in volume by 10%)

– Salt weathering (salty water enters cracks in rock at high tide, water evaporates forming salt crystals which exert pressure on rock as they form)

– Wetting and drying (rocks containing clay expand when wet and this pressure exerted breaks fragments off the rock)

24
Q

Processes of erosion (6)

A
Abrasion
Hydraulic action
Cavitation 
Wave quarrying 
Solution 
Attrition
25
Hydraulic action
Air in cracks in cliffs is compressed when waves crash in. The pressure exerted breaks up the rock.
26
Wave quarrying
The energy of a wave as it breaks can detach break off bits of rock.
27
Abrasion
Material being thrown against the rock by the waves, smoothening surfaces and breaking bits off
28
Attrition
Bits of rock in the water smash against each other and break into smaller pieces
29
Solution
Soluble rocks get gradually dissolved by the seawater
30
Cavitation
As waves recede, the compressed air expands violently, exerting pressure on the rock causing bits to break off.
31
Some of the many factors that affect the rate of coastal erosion include...
``` Defences Type of rock Type of coastline Wind direction Vegetation Fetch ```
32
Terminal scour
Higher than average rates of erosion at the end of a sea wall/sea management
33
Transportation processes (4)
Solution Suspension Saltation Traction
34
Solution
Soluble materials dissolve in the water and are carried along E.g. limestone is dissolved into water that’s slightly acidic
35
Suspension
Very fine material like silt and clay is carried in the water. Most eroded material is transported in this way
36
Saltation
Larger particles, pebbles/gravel, are bounced along the sea bed by the force of the water
37
Traction
Very large particles, (boulders) are pushed along the sea bed by the force of the water
38
2 key features which determine transportation process?
Energy & Size
39
Longshore Drift
The process of sediment being transported along the coastline by the swash (same angle as prevailing wind) and the backwash (90 degrees to sea.)
40
Swash
Carries sediment UP the beach, parallel to the prevailing wind.
41
Backwash
Carries sediment back DOWN the beach, at right angles to the shoreline.
42
Deposition is when...
Material being transported is dropped on the coast
43
Marine deposition
Sediment carried by the seawater is deposited
44
Aeolian deposition
Sediment carried by the wind is deposited
45
High energy coasts
Small particles easily transported whilst larger and heavier material is deposited forming shingle beaches
46
Low energy
Even the smallest material is deposited forming mudflats and saltmarshes
47
Deposition occurs when the s___________ l_____ exceeds the ability of the water/load to carry it. This is due to either:
Sediment load - Sediment load increases (e.g.landslide) - Wind/water flow slows down (so it has less energy)
48
Wind and water slow down due to...
- Friction increasing (water - shallower or wind - land) - Flow becomes turbulent - obstacle? Flow becomes tougher and overall speed decreases - Wind drops, wave height, speed and energy will decrease as well