Coasts Flashcards

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1
Q

Anticlines and Synclines

A

Geological folds caused by compression. Anticlines form crests and synclines form troughs.

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2
Q

Beach morphology

A

Beach profile and type of sediment

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3
Q

Concordant coast

A

Where bands of more resistant and less resistant rock run parallel to the coast

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4
Q

Emergent coast

A

Coastline that has been exposed by receding sea levels or isostatic uplift/rebound

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5
Q

Eustatic change

A

when the sea level itself rises or falls which has an effect globally

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6
Q

Isostatic change

A

when the land rises or falls and has an effect in that local area

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7
Q

Rotational slump

A

Where the slope fails and slides down due to undercutting or weathering of unconsolidated material

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8
Q

Thermal expansion

A

The main cause of sea level rise; the volume of ocean water increases as temperatures rise

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9
Q

Flocculation

A

Small particles like clay join together and get larger until they are deposited.

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10
Q

Sub-aerial processes

A

Land based processes which alter the shape of the coastline. Includes mass movement and weathering.

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11
Q

Mechanical weathering

A

Frost cracking where water gets into cracks and expands or salt cracking.

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12
Q

Biological weathering

A

Where roots or plants get into cracks and expand

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13
Q

Chemical weathering

A

Acidic rainwater and sea spray react with calcium carbonate in some rocks.

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14
Q

Mass movement

A

Slumping or Block/rock fall

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15
Q

Slumping

A

On unconsolidated cliffs which are eroded at the base rainwater enters the cliff and makes sediment more heavy, material slides down a slip plane. Rotational scars are left at the top of the cliff.

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16
Q

Rock fall

A

erosion at the base of resistant cliffs which creates an overhang, well jointed rocks are vulnerable to freeze-thaw, rocks fall.

17
Q

Discordant coast

A

More resistant and less resistant rock at right angles to the coast

18
Q

Joints and bedding planes

A

Joints are vertical cracks bedding planes are horizontal cracks.

19
Q

Strata

A

Layers of rock

20
Q

Concordant coast example

A

Isle of Purbeck, Dorset

21
Q

Wave cut platform example

A

Southerndown coast, Wales. Horizontally bedded layers of limestone left a 400m platform

22
Q

Tombolo

A

A beach that joins an island to the mainland. A spit grows to join them.

23
Q

Salt marsh example

A

Scolt Head island, Norfolk.

24
Q

Flamborough Head sediment cell

A

Sources: Soft boulder clay deposited by glaciers
Transfers: Longshore drift and backwash
Sinks: Spurn point (spit)
Rock groynes are disrupting sediment

25
Q

Emergent landforms

A

Raised beach due to isostatic uplift
Fossil cliff due to isostatic uplift

26
Q

Submergent landforms

A

Fjord - a flooded glaciated valley
Dalmatian coast - Several linked parallel valleys which are flooded - example Croatia

27
Q

Kiribati

A

lowest lying region in the world, sea level rising 1.2 cm per year
impacts: sanitation issues, drought and flooding.

28
Q

Bangladesh

A

46% of the population lives less than 10m above sea level
lies on the floodplain of 3 rivers.
NGO friendship encouraging people to plant mangroves.

29
Q

The Holderness Coast

A

Retreating a 2m per year. Mad eof boulder clay. 200 homes will disappear due to coastal erosion by 2100.

30
Q

Impact of coastal management on the Holderness coast

A

The seawall at Hornsea protects that part of the coast, but starves the beach at Mappleton and it’s cliffs are exposed to wave attack. BY THE 1990s nearly 4m of cliff were being eroded at mappleton every year.

31
Q

Impact of wave along the Holderness coast

A

Factors such as currents and low pressure weather systems cause high energy waves. The waves are not slowed down by friction with the sea floor as it is relatively deep.

32
Q

Withernsea and Mappleton management

A

Withernsea - beach nourishment
Mappleton - Cliff regrading reduces angle of the cliff to stabilise it. two rock groynes starving south

33
Q

Medmerry, sussex

A

Shingle sea wall but it was not effective //
A saltwater marsh and nature reserve created. // lost agriculture

34
Q

Abbots Hall Farm

A

In Essex . Managed realignmentby breaching the sea wall in five places allowing new salt marsh to form inland. because land value was low. Key players - RSPB and fishermen. oyster and some bird habitats disrupted.

35
Q

stair hole near lulworth

A

Purbeck Limestone is intensely folded, known as the Lulworth Crumple. The folding created heavy jointing making the Purbeck Limestone erode much more rapidly

36
Q

easington gas terminal

A

2.25% of all UK gas comes through this station.
1 km long revetment was built