Coastal deposition Flashcards

(23 cards)

1
Q

What are depositional landforms?

A

Coastal landforms created primarily due to processes of transportation and deposition

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What are example of depositional landforms?

A

Spit, beach, barrier beach, tombolo, sand dunes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What are depositional landscapes?

A

Low-energy coastlines where rates of transportation exceed rates of erosion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What is an example of a depositional landscape?

A

Estuarine coast

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

How many of the world’s coastlines are depositional in nature?

A

Almost 20%

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Where do depositional coastlines generally occur?

A

In low energy environments, where the effects of waves, storms and tides are much reduced

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What is a drift-aligned beach?

A
  1. Sediment is transferred along the coast by longshore drift
  2. These beaches tend to be longer and have graded material (i.e. sediment becomes finer further along the beach)
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What is an example of a drift-aligned beach?

A

Mappeton, Holderness coast

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is a swash-aligned beach?

A

Sediment moves up and down the beach with little lateral transfer

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Where to swash-aligned beaches occur?

A

In tight bays and so are protected from the effects of LSD

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What is an example of a swash-aligned beach?

A

Barafundle Bay, Pembrokshire Coast

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is an offshore bar?

A
  1. Destructive waves erode sand and coarse sediment from the beach
  2. The strong backwash pulls it offshore and then deposits it as a bar
  3. These cause waves to break further out to sea
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What is a cuspate foreland?

A
  1. Longshore drift occurs in opposite directions
  2. Sediment is deposited at the point where they meet
  3. Vegetation then grows and stabilises these landforms
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

What is an example of a cuspate foreland?

A

Dungeness, Kent

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What is a tombolo?

A
  1. Longshore drift creates a beach between an island and the mainland
  2. Sometimes they are covered at high tide
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What is an example of a tombolo?

A

St Ninians, Shetland

17
Q

What is a spit

A
  1. Longshore drift carries material along a beach
  2. A sudden change in coastal shape will initiate a deposition of material
  3. The presence of a river, or extension to water currents will prevent the spit from extending
  4. Can form recurved and double spits
18
Q

What is an example of a spit?

A

Hurst Spit, Hampshire

19
Q

What is a barrier beach?

A
  1. Longshore drift extends a spit between two headlands
  2. These barrier beaches trap water behind as a lagoon
  3. When it becomes separated from the mainland, it forms a barrier island
20
Q

What is an example of a barrier beach?

A

Slapton Sands, Devon

21
Q

What is gravity settling?

A

When the energy of transporting water becomes too low to move sediment; large sediment will be deposited first followed by smaller sediment

22
Q

What is flocculation?

A

Important for very small particles, such as clay, which are so small they remain suspended in water. Clay particles clump together due to electrical or chemical attraction and become large enough to sink

23
Q

What is a littoral cell system?

A

A simplified model that examines coastal processes and patterns in a given area. It operates at a variety of scales, from a single bay, to a regional scale