Case Study Overstrand Landforms Flashcards

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1
Q

Location?

A

North-east coastline in East Anglia, e.g. Overstrand

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2
Q

Waves?

A

Powerful and more destructive as they are built up over a large fetch: strong swash and weak backwash

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3
Q

Fetch?

A

3000km

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4
Q

Prevailing wind direction?

A

From the NE: waves hit cliff almost straight on- swash align beach and so erode rapidly

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5
Q

What is cliff made of?

A

Very weak: chalk bedrock is covered by a thick (2-5m) layer of glacial till which is unconsolidated so eroded easily

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6
Q

How do waves erode cliff and what do they create

A

Waves erode cliff by process of hydraulic action/pressure, abrasion and solution, creating a wave cut notch at the base of the cliff

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7
Q

What happens to cliff after being eroded?

A

Cliff collapse as unsupported cliff material slumps under its own weight - most common during heavy rains when cliff materials because saturated and very heavy.

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8
Q

What about other types of cliffs are there, what causes them?

A

Some are not very high or vertical because the unconsolidated glacial till collapses easily so they are instead gentle sloping and ave. 30m high - the underlying chalk is exposed in places

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9
Q

Erosional landform: Cliff retreat?

A

The cliffs retreat rapidly ave. 1m per year - a single powerful storm can erode hundreds of tonnes of material.

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10
Q

Erosional Landform: Wave cut notch visibility?

A

Wave-cut notch is only visible in some places because the unconsolidated glacial till collapses frequently, obscuring the notch.

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11
Q

Erosional Landform: wave cut platform (beach) description?

A

There is a gentle sloping wave cut platform in front of cliffs: left by rapid retreat of cliffs which is covered at high tide but exposed at low tide.

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12
Q

Erosion Landforms: wave cut platform (beach) coverage?

A

It is covered with a sandy beach: composed of slumped cliff material in process of being removed by longshore drift from the SE to the NW

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13
Q

Depositional landforms: Spit (Blakeney Point) waves?

A

Waves approach coastline at an angle: approach north-facing coastline from NE, which is the prevailing wind direction (drift align beach)

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14
Q

Depositional Landforms: spit (Blakeney point) longshore drift?

A

Long shore drift moves material EAST to WEST: waves move up beach at angle but returns at right angles due to gravity - material is moved along beach from east to west in process

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15
Q

Depositional Landform: spit (Blakeney Point) coastline?

A

Coastline changes direction as the coast bends SW as material being transported by longshore drift is deposited in the sheltered water where the coast changes direction.

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16
Q

Depositional Landforms: spit (Blakeney Point) finger of land, length & shingle?

A

Longshore drift from east to west provides more and more material deposited leading to finger of land being developed - Blakeney point is apx. 15KM long and shingle bank up to 10CM high

17
Q

Depositional Landforms: spit (Blakeney point) curved ends?

A

Occasional storm winds from north and north west, forces the end of the spit to curve around - Blakeney point has at least 3 prominent curved ends

18
Q

Depositional Landforms: salt marsh (Blakeney Marsh) wave energy?

A

Sheltered water behind the spit so wave energy is LOW

19
Q

Depositional Landforms: salt marsh (Blakeney marsh) sediment?

A

This occurs in rivers such as the Stiffkey Freshes Creek as they empty into this area on the way to the sea - silt and other fine sediment that they are transporting is deposited in sheltered water

20
Q

Depositional Landforms: salt marsh (Blakeney marsh) developing of salt marsh?

A

Over time silt builds up and plants able to colonise it e.g. spartina. The plants trap further sediment around their roots and stems and permanent marsh becomes established with +++ range of plants e.g. sea lavender, sea campion, samphire

21
Q

Importance of Blakeney Marsh?

A

It has become an important international breeding are for sea bird colonies e.g. arctic terms, oyster catchers