Holderness Flashcards

1
Q

What are two key features of the Holderness coast?

A

Spurn Head in the South and Flamborough Head in the North

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2
Q

3 reasons for erosion here

A

Geology, fetch and LSD/Beach material

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3
Q

What is the geology like and what is the positive and negative impacts of it?

A

Chalk & Boulder clay
Good fertile soils for farming
BUT little resistance so rapid erosion when wet producing shallow sloping cliffs

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4
Q

Why is the fetch expected the be quite small?

A

Winds comes from NE

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5
Q

Why is the fetch actually quite big?

A

Swell circulates from Atlantic - powerful desctructive
Low pressure weather systems
Small enclosed seas - energy can’t be dissipated
Deep sea floor - doesn’t help weaken waves through friction

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6
Q

How are Holderness cliffs so unprotected?

A

Boulder clay eroding to form unconsolidated clay particles , easily transported southwards by LSD form Spurn Head spit and cliffs left with nothing.

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7
Q

2 types of cliff erosion occurring?

A

Cliff foot erosion and sub aerial processes

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8
Q

What processes are involved in cliff foot erosion?

A

Abrasion, corrosion, hydraulic action and corrosion

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9
Q

What processes are involved in sub aerial processes?

A

Freeze thaw, biological weathering, chemical weathering - dissolves chalk at Flamborough Head

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10
Q

What is the process of mass movement of the Holderness cliffs?

A

Slumping: alternate wetting and drying, expanding and shrinking, cracks, percolation, lubrication, gravity, sliding

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11
Q

What could increase the level of risk in Holderness?

A

Eustatic sea level rise and Isostatic change meaning towns further inland could be at risk - Mappleton.

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