Flamborough Head Flashcards

1
Q

How long is the coastline

A

60 km

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2
Q

What is the geology of north York moors

A

400m above sea level, made of sandstone, shales + limestone (formed during Jurassic period)

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3
Q

What is the geology of flamborough head

A

Made of chalk and topped with till

Differences in rock resistance responsible for varied coastal scenery

High cliffs, bays and headlands

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4
Q

Dominant wave direction

A

North and north-east

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5
Q

What is the fetch

A

1500 km

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6
Q

Where is the wave energy highest and why

A

The north facing nearest Saltburn as there is the most amount of exposed surface area

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7
Q

Why do rate of erosion vary

A

Due to the difference in wave energy inputs but also due to a variation in resistance of different geology is

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8
Q

What is the shale and clay erosion rates

A

0.8 mm per year

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9
Q

What is the wave height

A

Often exceed 4 m

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10
Q

What process operate from north to south

A

Long shore drift

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11
Q

Sediment from the river Esk

A

Supplies limited amount of sediment due to the construction of weirs and reinforce banks

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12
Q

Where is erosion and deposition occurring

A

Create a erosion occurs between Sunderland and Teeside, more deposition also occurs south of Scarborough

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13
Q

What direction is the nearshore sediment moving in

A

South

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14
Q

Where is the input Occuring

A

Robin Hood‘s Bay

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15
Q

What are the cliffs like along the coastline

A

The sediment is horizontally bedding as a result the profiles tend to have a vertical face

most of the cliffs of a layer of the week glacial till upon them which causes a low angle

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16
Q

What are the cliffs like at Flamborough

A

Cliffs made a chalk which is very strong due to tightly bonded mineral particles

The vertical cliffs are typically at 20 - 30 m high

with the overlying till lowered by mass movement processes to an angle of about 40°

17
Q

What are the cliffs like between Saltburn and Robin Hoods Bay

A

The cliffs are much higher but often with a stepped profile this reflects the more varied geology

steeper slope segments are formed in the more resistant sandstone and limestone

with gentle slopes corresponding to the weaker Clays and shales again lowered by mass movement

18
Q

Details of platforms at Robin Hood’s Bay

A

The platform slopes at a typical angle of 1° although ramped sections are steep as 15° the platform has a maximum width of about 500 m but extends much further into the offshore zone

19
Q

Headlands and bays at Robin Hood’s Bay

A

Robin Hoods Bay has been eroded into relatively weak shales with more resistant bands of sandstone Either forming the headlands of ravansgar to the south and ness point to the north

20
Q

What features are found in Sandwich Bay Flamborough head

A

Large joints or faults,

they are then exploited by the erosive action of the waves enlarging them to form caves and arches

a master joint in the chalk has been enlarged

21
Q

How many geos are there along the coastline

A

Over 50 geos have formed along this coastline

most of them aligned to the north east, facing the dominant wave direction

22
Q

Blowholes along the coastline?

A

They have developed were vertical master joints in the chalk have been enlarged subsequently chalk and border clay have collapsed into the underlying sea caves leaving a funnel like depression on the clifftop

23
Q

Where are beaches found along the coastline?

A

They are found in the sheltered low energy environment such as Scarborough and Filey Bay

24
Q

Why does sediment accumulate slowly

A

Deposits of sand and shingle accumulate slowly owing to low input of sediment from rivers and the slow rate of erosion of the resistant rocks

25
Q

Why are there no spits along the coastline despite there being LSD

A

Because high energy waves remove sediment before it can accumulate
although LSD is considerable the coastline has no spits due partly to the high tidal range of around 4 m and the lack of estuarine in environment that would provide sediment sinks