Coasts Flashcards

1
Q

What are the 4 management options at a coastline and explain

A
  1. Hold the line - maintain current position - often hard engineeeing
  2. Advance the line - extend coastline - build up beach e.g nourishment
  3. Manages retreat - allowing retreat within management e.g creating salt marshes
  4. Do nothing
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2
Q

What are the 5 types of erosion?

A
  1. Hydraulic action - force of water against cliff
  2. Wave quarrying - breaking waves trap air against cliff - air trapped and compressed, pressure builds
  3. Attrition - rocks hitting against each other or abrasion wearing rocks down
  4. Solution - chemicals dissolve rocks - not common in sea bc water alkaline
  5. Cavitation - bubbles in sea may explode under pressure - can be against rock - pressure
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3
Q

Name 4 landforms

A
  1. Tombolo- forms similar to spit - ridge or sand/shingle which joins a mainland and an island
  2. Barrier beach - a ridge of sand or shingle which joins 2 headlands - parallel to coast - firms lagoon behind
  3. Bar - ridge of sand/shingle which forms across mouth of river, or bay or harbour - usually parallel to coast
  4. Offshore bar- partly submerged ridges of material
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4
Q

What are the two types of spits

A
  1. Simple spit - a bar of sand without barbs or hooks

2. Compound spits - spits with barbs or hooks on their landward side

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5
Q

Conditions for sand dune formation

A
  1. Large tidal range - exposure so sand dries out
  2. Large quantity of sediment available
  3. Dominant onshore winds - blows dry sand up the beach
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6
Q

Sand dune types

A
  1. Embryo dune - no more than 1m high, plants: Lyme grass
  2. Fore dune - drought resistant - up to 5m, plants: Lyme grass, marram grass
  3. Yellow dune - more shelter, more plants, humus later build, up to 10m
  4. Grey dune - sheltered from wind, soil forms, 100% vegetation
  5. Dune slack - before mature dune, plants adapt to damp and sheltered conditions
  6. Mature dunes - 100m from shoreline, support shrubs and mabs trees
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7
Q

Eustatic change

A

Global change in sea level due to rise or fall in sea level itself
- either thermal expansion or land ice melt

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8
Q

Isostatic change

A

Sea level change due to land rising or falling relative to the sea
- occurs over long period of time

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9
Q

Landforms of submergent coastlines

A
  1. Rias - river valley at the coast inundated by the sea (an unglaciated river valley)
  2. Fjords - formed when glacial troughs are flooded - long and steep-sided
  3. Dalmatian coasts - valleys flooded by rising sea levels - tops of valleys remain above surface of the water - looks like islands
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10
Q

Landforms of emergence

A
  1. Marine platforms - fall in sea level/land rising causes former shoreline to be exposed
  2. Raised beaches - land rises/ sea level falls - more coastline exposed
  3. Relict cliffs -
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11
Q

Hard engineering strategies

A
  1. Sea wall
  2. Groynes
  3. Gabions
  4. Revetments - sloping wooden concrete structures at foot of cliff
  5. Barrages - partly submerged structures containing sluice gates to control flow of the sea
  6. Offshore reefs - material e.g concrete boulders sunk offshore - dissipate wave energy
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12
Q

Slapton sands, what has been done/defences?

A
  • sea wall put in place at Torcross - rebuilt numerous times - last completed sea wall 1980
  • Storms in 2001 undermined section of the road - caused Slapton Line Partnership to form
  • 2002 new 2 way road built 21 metres back from previous road
  • 12,000 tons of shingle moved from strete gate to protect the line
  • jan 2014 £250,000 spent on moving 25,000 tons of shingle from one end of torcross to the other
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13
Q

Challenges of Slapton sands

A
  • 2001 storms undermined section of the road - took 12 months for new section to open (single trade in meantime)
  • Slapton Line Partnership have to balance economic and environmental issues
  • the £250,000 wasted on moving shingle in torcross bc it didn’t last
  • 2016 section of sea wall collapsed - A379 temporarily closed - 3500 people temporarily left without bus service - repairs took a year
  • problem of protecting the ley or retreating the road
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14
Q

Sustainability at Slapton Sands

A
  • Shingle movement proven not to be cost effective

- sea wall has had few problems - won’t last forever

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15
Q

Background odisha

A

In India

Very dynamic coastline - subject to change

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16
Q

Risks at odisha

A
  1. Erosion increasing at the coasts - risk to coastal communities
  2. Human intervention shifts problem further along the beach
  3. Majority of states population live on coastal plain - subject to natural hazards
  4. Ecosystem may be damaged with sea level rise
17
Q

Opportunities in Odisha

A
  1. Offshore benefits - oil, natural gas, seabed mining
  2. Potential for offshore wind, tidal, wave power
  3. Tourism important - beaches and wildlife major attractions
  4. Jobs in coastal fishing and aquaculture
18
Q

ICZM in odisha

A

Integrated Coastal Zone Management

  • developed ICZM in odisha - promote sustainable coast
  • co-ordinates sustainable management for coastlines
  • project is a venture income committees e.g Indian government, world bank
  • individual villages been consulted about some of the issues
  • issues included: biodiversity conservation, vulnerability to disaster
19
Q

Mangroves in odisha

A
  • amount of mangroves severely reduced bc of room for building and agriculture
  • mangroves slow waves down and provide protection for coastal communities
  • offshore ecosystems provide livelihood for fisherman and locals
  • super-cyclone Kalina in 1999 hit l, villages with 4 or more km of mangroves has no deaths and those with less than 3km had deaths
  • Wetlands International (an NGO), Indian gov and ICZM project are trying to reverse decades of mangrove destruction - its sustainable and appropriate coastal management scheme