Geography- Unit 1.2.1/ How do coasts change overtime? Flashcards

1
Q

Constructive waves characteristics

A

-They have a stronger swash
-Long wavelength but low in height
-Break on the shore and deposit material
-Low frequency (less than 10 per minute)

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2
Q

Destructive waves characteristics

A

-They have a stronger backwash
-Created in stormy conditions
-Created by a long fetch and high wave energy.
-Short wavelength but are tall
- High frequency (10-14 per minute)

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3
Q

What is Mechanical weathering?

A

Any process that causes physical disintegration of material without changing the chemical composition. e.g temperature change from day to night causes ice in rocks to expand and contract, causing the rock to crack

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4
Q

What is chemical weathering?

A

Disintegration of material through chemical reactions. e.g carbonation when acid rain reacts with limestone and causes cracks to form.

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5
Q

What is biological weathering?

A

When living organisms cause the disintegration/ changing material. E.g Plants grow into cracks inside rocks and break them apart.

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6
Q

Labelling a wave

A

1) Crest- top of the wave
2) Trough- Bottom of a wave
3) Backwash- water rus back down the beach
4) Swash- Wave breaks and washes up the beach
5/6) Destructive or constructive

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7
Q

Why do waves form?

A

Waves begin in a circular motion, however friction causes the base movement of the wave to slow creating an elliptical movement. As the sea bed rises, more friction is applied, and the motion becomes so elliptical that the top of the wave breaks over.

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8
Q

What is longshore drift?

A

Prevailing wind pushes constructive waves towards the shore at an angle, causing the swash to occur at an angle. The backwash moves at a 90 degrees angle back. This causes the mass movement of sediment up and down the beach, each time moving further along the coastline.

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9
Q

How is a headland and bay formed?

A

The soft rock in a discordant coastline are eroded causing a bay, whilst the harder rock layers remain protruding out, as headlands. This is process is also called differential erosion.

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10
Q

What is a concordant coastline?

A

Concordant coasts have alternating layers of hard and soft rock that run parallel to the coast/ it faces one type of rock then the other type of rock is behind it.

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11
Q

What is a discordant coastline?

A

Discordant coastline is where the alternating layers of hard and soft rock run perpendicular to the coastline/ vertical.

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12
Q

Why are there more constructive waves near bays?

A

Leading to bays, the sea bed rises, causing increased friction meaning the waves become smaller and more constructive.

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13
Q

How are caves formed?

A

Hydraulic action causes large cracks, which ( by hydraulic action and abrasion) indents in the cliff and is thus a cave.

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14
Q

How are arches formed?

A

By hydraulic action and abrasion, the cave breaks through the headland, created an arch shape

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15
Q

How are stacks formed?

A

The rock forming the arch collapses, creating a stump situated next to another area of land.

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16
Q

Ho are stumps formed?

A

The stack is weathered down to create a smaller structure, the stump.

17
Q

What is a wave cut platform?

A

-Bottomof cliff is eroded at sea level
-Without support, the top collapeses creating a 90 degree cliff
- This continuous, retreating the land and creating a platform

18
Q

How is a wave cut platform formed and why are cliff faces always verticle?

A

Waves erode part of the cliff just above sea-level ( most powerful waves hit there) , creating an indent called a wave cut notch. This leaves an overhang which eventually collapses, creating a vertical cliff face. This process repeats, causing the cliff face to retreat and leaving a flat piece of land called the wave cut platform.

19
Q

What and how was lulworth cove formed?

A

Lulworth cove is a near circular bay and is a great example of a concordant coastline.
Waves slowly eroded a small path through resistant rock such as portland, once through, easily eroded the weaker rock on the next layer. This weaker rock was eroded in every direction, creating the circular bay.

20
Q

Why does the south of the uk experience many destructive waves?

A

Because the waves have a large fetch as they have travelled over the atlantic ocean

21
Q

Famous uk arch

A

Durdle door in dorset.

22
Q

What is a beach?

A

A buffer zone between the sea and land, made from eroded material. This occurs when waves become less energetic,

23
Q

What is a spit?

A

A long narrow piece of land made from sand or shingle, attached to the mainland at one end, whilst the other protrudes out into the sea.

24
Q

Where is a famous uk spit?

A

Spurn point in yorkshire.

25
Q

Where is a spit generally formed?

A

At an embayment or estuary (mouth of a large river)

26
Q

How is a spit formed?

A

Through longshore drift, and the deposition of finer material further from the mainland, creating the long narrow shape. These can curve causing a hook, as secondary winds and shallow water change the angle from which the swash travels.

27
Q

What is and how is a bar formed?

A

It is a sand or shingle beach, connecting two areas of land or headlands together, with a shallow lagoon (once a bay) behind. This is caused by the elongate growth of a spit.

28
Q

What is another name for a bar?

A

A barrier beach

29
Q

What is and how is a tombolos formed?

A

It is a sand or shingle bar attaching the coastline to an island. Due to the shallow waters surrounding an island, the waves lose energy and deposit more material, causing a connection between the island and mainland.

30
Q

How are salt marshes formed?

A

They form behind a spit or in a river estuary as it is sheltered and therefore more material is deposited. Here in mud flats, vegetation develops and colonises overtime.

31
Q

How do plants survive in salt marshes?

A

-Plants must be adapted to suit saline conditions e.g salt grass.
- Withstand being submerged in water
-Use roots as an anchor, these also reduce the tidal flor and traps more material, creating a better habitat.

32
Q

How are sand dunes formed?

A

Saltation, sand blows dry wind back off the coastline and they pile together.

33
Q

Unconsolidated rock

A

A form of weak rock that has not been compacted, cemented or transformed into actual rock.

34
Q

How many villages have been lost in holderness coast?

A

29

35
Q

How much of holderness coastline is eroded annually?

A

2m

36
Q

Why does holderness coast erode quickly?

A

Physical:
GEOLOGY- Because the bedrock is made from unconsolidated till deposited by glaciers over 18,000 years ago.
FETCH- Waves travelling there have a large fetch.
Human:
DREDGING- removing material from the coast to build houses
MANAGEMENT- Built groynes that causes sediment causes more erosion further along the coastline. terminal groyne syndrome.
GLOBAL WARMING- heat causes water to expands and glaciers melt causing sea level rise.

37
Q

Where is the holderness coast and what are some surrounding towns and rivers ?

A

Is on the North- east coast of England, surrounded by towns such as kingston upon hull, grimsby and bridlington.
- North of River Humber