3.b. Submergent coastal landscapes form as sea level rises Flashcards

1
Q

What are submergent coastal landforms

A

-landfroms that form as sea level rises

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2
Q

How does climate change lead to sea level rise

A

rise in global temperature, melting of ice stores on the land, increase in the volume of water in the oceans, sea level rise. A 1degrees rise in global temperature could lead to a rise of 2m at sea level

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3
Q

How does sea level rise influence geomorphic processes and landforms

A
  • the main influence of a rise of sea level is the submergence of river valleys, forming rias, and glacial valleys forming fjords
  • shingle beaches appear when former coastal sediment is pushed onshore by wave action
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4
Q

Description of rias

A
  • submerged river valleys, formed as sea levels rise
  • the lowest part of a rivers course and the floodplains are submerged
  • the higher valley sides, middle and upper course remain exposed
  • the centre is deeper and the exposed valley sides slope
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5
Q

Example of rias

A
  • examples found in Devon and cornwall
  • names include Fowey and Kingsbridge
  • alluvial deposits were laid down during glacial periods
  • thresholds can form at the mouth of each river
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6
Q

Modification of rias and fjords

A
  • modified by the wave processes acting on their sides at the present day sea level
  • the valley sides may be affected by the operation of sub-aerial processes-lead to a reduction in the steepness of the valley sides of fjords
  • sea levels predicted to rise by 0.6m in the next 100 years
  • marine erosion will increase
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7
Q

Description of fjords

A
  • submerged glacial valleys
  • steep, cliff like valley sides
  • u shaped cross section
  • the threshold at the end is shallower due to limited erosion
  • further deepened during the Flandrain Transgression
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8
Q

Example of fjords

A
  • can be found in Scotland, Norway and Nea Zealand

- scottish fjords less well developed as ice was never thick

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9
Q

Description of shingle beaches

A
  • when sea level falls and the land based ice increases, large areas of ‘new’ land emerge
  • rivers, meltwater and constructive waves accumulate sediment on the surfaces
  • as eustatic level rise occurs, wave processes puch sediments onshore
  • contribute to the formation of tombolos and bars
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10
Q

Example of shingle beaches

A
  • Chesil beach is a tombolo formed during Flandrian transgression
  • sediment was carried into the English Channel by meltwater during Würm glacial period
  • as sea levels rose, sediment was carried north east due to a south westerly wind
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11
Q

Modification of shingle beaches

A
  • the tombolo at Chesil beach has been affected by longshore drift
  • shingle may move northest and a beach will cause storms
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