Coast case studies Flashcards

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1
Q

What are a few facts about old man hoy?

A
  • Vegetation helps it to stabilise
  • Horizontal bedding planes
  • Slight seaward dip
  • Base stack is igneous basalt
  • Blocks at the bottom from former arch
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2
Q

What are a few facts about Flamborough head?

A
  • Base of cliff is where undercutting occurs forming wave cut notch- undercutting until cliff collapses
  • Surface of wave-cut platform uneven due to differential erosion
  • Limestone cliffs
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3
Q

What are a few facts about a spit?

A
  • Spurn point a sand and shingle spit 5.5km long and 50 miles wide
  • Spit forms sweeping curve which continues the line of the coast because of different prevailing wind
  • The energy in the waves transporting materials reduces where north sea meets Humber estuary causing deposition
  • LSD moves east to south, so prevailing wind is from south east
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4
Q

What are a few facts about a tombolo?

A
  • Tombolo which connects two land masses is 500m long and is subject to waves form different directions
  • In winter sand is lost from the centre and builds up at the ends and is summer opposite occurs
  • During low tides it can be 70m wide and during high spring tide it can be submerged
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5
Q

What are a few facts about a barrier beach?

A
  • 18-mile-wide shingle barrier beach stretching from west Bay to Portland
  • In some places 15ft high and 200m wide
  • Behind is a shallow tidal lagoon and barrier beach protects it (Submergent)
  • Longshore drift going from east to west, so prevailing wind is from southeast
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6
Q

What are a few facts about a cuspate foreland?

A
  • Formed as prevailing wind brings sediment through LSD together in opposite directions
  • Headland cuspate foreland off the coast of Kent and mostly made up of shingle
  • Some cuspate forelands may be stabilised by vegetation, while others migrate down the shoreline
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7
Q

What are a few facts about a hooked spit?

A
  • Formed be LSD from the west
  • The salt marsh has formed behind Hurst castle spit, which has formed because of LSD from the West
  • Key haven salt marsh are under threat from the construction of groynes down current (to the west) which were designed to trap sediment.
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8
Q

What are a few facts about UK sediment cell 2?

A
  • Starts at Flamborough head and finishes at the wash
  • Transfers- Longshore drift south to southeast towards the wash, Offshore currents into the North Sea.
  • Inputs- Holderness coast cliffs, Flamborough head and the Humber estuary.
  • Sinks- Spurn head spit, beaches to the south of Grimsby
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9
Q

California Coastal flooding case study

A
  • California coast stretches 1,264 miles, so hard to manage
  • More than half of California people reside in coastal regions
  • California has two natural bays SF bay and SD bay
    Subsidence:
  • 80% of water extraction is from farmers – increases subsidence as water is removed from the ground – CA sinking by 1 foot per year
    El Nino:
  • Happens in tropical Pacific Ocean- fluctuation in earth’s climate system weather trade winds mean more warm sea in eastern pacific- more low-pressure systems- which leads to lots of erosion and flooding
    Waves:
  • Hurricane Marie 2014- Storm surge can add 50-100% of existing water
  • Areas like laguna beach lots of beach replenishment but exposed to lots of waves on the coast-High risk to coastal flooding
  • Santa Monica prioritised for coastal management- large amount of beach replenishment – Better protection and more successful
  • Santa Barbara- high risk of flooding and coastal recession
  • San Francisco bay natural wetlands- Salt marsh removed for development- low lying estuarine region
  • Land subsidence on estuary led to higher flood risk
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10
Q

Bangladesh coastal flooding case study

A

Mangrove swamps protect Bangladesh from storm surge because they absorb wave energy

  • Bangladesh is vulnerable because only above sea level by 5-8m near Dhaka- Vulnerable to storm surge
  • Waves funnelled into one area most wave energy hitting one area- Bay of Bengal- more vulnerable to storm surge
  • Mangrove swamps removed for development less wave energy dissipated- more vulnerable
  • Sundarbans only protected mangrove forest while others damaged/removed
  • Mangrove forests income generation and food security
  • Increasing industrial development- gradually deteriorating mangrove ecosystem
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11
Q

Maldives coastal flooding case study

A

Economic impacts:
- Loss of tourism (about 33%of GDP)
- Makana national airport may be shut down due to flooding cutting of international tourism- 1 million travelled in 2015
- Coastal flooding may also damage fish processing plants- reducing Maldives fish exports (10% of GDP)
Social impacts:
- Houses could be damaged or destroyed and severe flooding can make entire communities homeless
- Supplies of freshwater are already low on many of the islands and at a risk of being polluted by sea water- many have tp rely on rainwater and desalinisation plant (economic)
Environmental impacts:
- Coastal flooding wears away beach at very rapid rate- Destroying habitats
- Soil on most islands shallow and can be easily washed away- most plants unable to grow

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12
Q

Dawlish storm surge case study

A
  • 1.2 billion pounds lost
    After winter 2013:
  • 25000 tonnes of collapsed cliff removed at Teignmouth
  • Hundreds of tonnes of debris removed
  • Line was shut for 2 months
  • £35m reduction in holiday spending
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13
Q

Holderness coast- skip sea- East riding of Yorkshire case study

A
  • No national scheme to compensate people losing their homes
  • Local council have to cover the demolition of the houses- limited money given to those moving
  • Offering up to £1000 in relocation expenses and up to £200 in hardship expenses
  • Council expects 100 homes to be lost in next few decades
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14
Q

Kiribati-nation under threat due to climate change- case study

A
  • Risk of being inhabitable due to sea level rise
  • Seawalls have been broken
  • United states responsible for ¼ of CO2 emissions
  • 40% of people live near the coast
  • People of Kiribati trapped 6ft above sea level- salt water can poison ground and sources
  • People leaving
  • Purchasing land in Fiji for civilisation
  • People of Kiribati being rejected as climate refugees
  • 145 million people live only 3ft above sea level or less
  • Also affects developing countries through flooding- lots of floods in New Orleans and San Francisco
  • Trump withdrew from Paris climate agreement
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15
Q

Australia- consequences of coastal recession case study

A

Causes of risk:
- 3mm of sea level rise per year
- Overall, 1.2m of sea level rise
- Many mega cities on low-lying areas
- Sea level stable until 19th century- Industrial revolution
- 13cm of flooding could have big risk
Social impacts:
- 250,000 houses at risk
- May lose 7-5 hospitals
- Increase in unemployment- fisheries- 30 billion GDP and tourism
Economic impacts:
- Loss of potential 120 ports and 5 power stations
- 0.5m sea level rise = 2.8 billion in damage
- $3.9 million a year spent on beach nourishment
Environmental impacts:
- Affects natural ecosystems – Freshwater habitats
- Ground water affected by salt intrusion

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16
Q

Philippines- consequences of coastal recession case study

A

Causes of risk:
- 5.8mm of sea level rise per year
- Pacific Ocean currents and trade winds move water towards islands
Social impacts:
- Up to 2.3 million people could be affected
- 90% of wealth owned by 15% of population
- High levels of inequality and poverty
Economic impacts:
- Loss of 6.5 billion per year due to sea level rise
- Economically vulnerable due to high poverty
- Property loss of 12.5 million
- High unemployment and near alternative jobs harder to find
Environmental impacts:
- Natural ecosystems- mangroves, corals and seashells already damaged- pollution and siltation
- Less natural barriers