Dorset Coastline Case Study Flashcards

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1
Q

Name a high energy coastline

A

Dorset coastline

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2
Q

Prevailing wind direction

A

South west

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3
Q

Secondary wind direction

A

S/south-east

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4
Q

Domination /longest fetch length

A

7000km

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5
Q

Tidal range

A

2-3m

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6
Q

Average wave height

A

0.5-1m

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7
Q

Imputs of fluvial sediment

A

Osmington river

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8
Q

Sediment input from cliff/shoreline erosion

A

200 000 m3

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9
Q

Nature of longshore drift

A

From west to east but limited volumes of sediment moved

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10
Q

Geology of coastline and length of geology

A

50m wide Portland limestone
70m wide Wealden Clay
Narrow section of greensand and sandstone

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11
Q

Formation of Lulworth cove

A

1) A stream breaches the bastion (sea level) of the resistant limestone
2) Erosion continues to evolve the cove behind the narrow portland limestone entrance - the sea begins to erode the less reisistant wealden clay
3) The bay widens as the sea erodes the wealden rocks on either side
4) The seaward side the clays and sands are eroded away
5) The clay and sands are continually eroded and become wider and deeper, whilst the entrace is still a narrow gap in the portland limestone - wave action and weathering
6) The back of a cove is a 250m wide band of chalk - more resistant than clay and sandstone - shape
7) Chalk is slowly eroded and the wide section of clay and sands are have eroded - result of wave diffraction - narrow entrance ensures the waves enter into an arch shape

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12
Q

What type of coastline type does lulworth cove form on?

A

Concordant coastline

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13
Q

Describe the formation of Swanage Bay and Old Harry’s Rocks

A

Secondary wind direction more influcential than prevailing wind
Tidal range over a large fetch
Swanage Bay is a clay and portland limestone geology - less resistant clay eroded hence a bay formation and limestone more resistant hence headlands
Old Harry’s rocks chalk geology - more resistant - landforms
Discordant coastline

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14
Q

Describe the formation of Man O’ War Cove

A

Portland limestone more resistant - reinforced by the purbeck beds behind
This blocks the formation and erosion of the chalk and wealden clay behind
The cove behind is easily eroded - less resistant rock
High energy coastline with a strong preveailing wind
Concordant coastline

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