Coasts case studies Flashcards

1
Q

Holderness background

A
  • Yorkshire
  • losing 2m of coast per year
  • lost 4km since Roman times
  • 29 villages lost to the sea
  • 80000m2 of farmland lost per year
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2
Q

Why is there so much erosion at Holderness?

A
  • Geology: weak boulder clay
  • waves: powerful and destructive (5000km atlantic fetch)
  • narrow beaches
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3
Q

What’s happening at Mappleton?

A
  • population 250
  • road 34m from the sea, cheaper to defend than move
  • community built their own revetment and groynes
  • terminal scour
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4
Q

What’s happening at Kilnsea?

A
  • most southerly village on Holderness
  • lost 300m of land in 150 years
  • population 90
  • vulnerable to floods
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5
Q

Why is the coast of west africa eroding so quickly?

A
  • 1-2m retreat per year
  • rising sea levels
  • lack of defences
  • dams trap sediment which can’t be deposited at coast
  • destruction of mangroves
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6
Q

What is the Deltawerken (Netherlands)?

A
  • hard engineering megaproject
  • dams and gates constructed to control flow of water between the eastern islands
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7
Q

What is happening at Kiribati?

A
  • roads eroded
  • food insecurity
  • homes submerged/destroyed
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8
Q

Where is eustacy affecting?

A
  • Kiribati
  • Flooding rias eg Kingsbridge
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9
Q

where is isostacy affecting?

A

ice melting in scotland
- scotland rising by 1.5mm p/year
- south uk sinking by 1mm p/year eg essex

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10
Q

what is happening in the isle of arran, scotland?

A

relict cliffs eg kings cave
isle of arran - raised beach 5m above sea level
due to isostatic uplift

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11
Q

why is bangladesh vulnerable to floods?

A

monsoons, himalayan snowmelt
- 2004 floods covered half of country, killed 600

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12
Q

Ria

A

Kingsbridge, south devon

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13
Q

fjord

A

Sognefjord, norway
- 205km long
- 1.3km deep
- 4.5km wide

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14
Q

Fjard

A

Kanholmsfjarden, Sweden

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15
Q

Dalmatian coast

A

croatia
- 1240 islands parallel to coast

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16
Q

maldives

A

The Maldives have an average height of 1.5 m above sea level, but its population of 400,000 is too large to be easily accommodated elsewhere. It’s highest point is 2.3 m above sea level, and a 50 cm rise would flood 77% of it.

17
Q

hallsands

A

sediment cell disruption
shingle dredged offshore to provide material for construction of dockyard in plymouth, so shingle from the beach slipped into holes left. As sea levels fell, deep fast-flowing channels which stopped material being deposited at Hallsands developed