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
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
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
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
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
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
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
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
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
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
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