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

1
Q

Climate changes that occurred during a previous time period and the resultant sea level RISE

A

Warming climate (interglacial period) =

ice melts -> and water is released into the sea -> causing eustatic rise (globally)

land ice melts -> meaning the weight on land is reduced -> causing the land to rise (isostatic rebound) -> causing isostatic rise + fall on opposite side of land mass (relative change locally)

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2
Q

the influence of rising sea levels due to a warming climate and the geomorphic processes shaping
landforms in submergent landscapes
- rias

A

a drowned river valley
-> as a result of a rise in sea level

gentle sloping sides

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3
Q

the influence of rising sea levels due to a warming climate and the geomorphic processes shaping
landforms in submergent landscapes
- fjords

A

a drowned glacial valley
-> as a result of a rise in sea level

steep sides

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4
Q

the influence of rising sea levels due to a warming climate and the geomorphic processes shaping
landforms in submergent landscapes
- shingle beaches

A

depositional landform made up of larger sediment between 1-2cm to 5-7cm

when sea level drops -> new land is exposed -> in low energy environments -> sediment is deposited and accumulates

when sea levels rise -> waves push sediment onto shore -> creating shingle beaches

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5
Q

the modification of these landforms by processes associated with present climate and sea level changes

A
  • erosion- current sea levels are causing wave action to erode sides of valley of fjord and land where ria is- where this erosion occurs will depend on where present-day sea level reaches
  • weathering- current day weathering processes can lead to mass movement = can lead to a reduction in steepness of valley sides of fjords
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6
Q

the modification of these landforms by processes associated with future climate and sea level changes

A
  • sea levels predicted to rise by 0.6m within next 100 years -> marine erosion of rias and fjords likely to increase due to larger waves and more storms
  • shingle beaches- more sediment may be transported and removed -> shrinking these beaches over time (e.g. Chesil beach has been modified by LSD as sea levels have rose)
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