The Holderness Coast Case Study Flashcards
Which 4 factors suggest why coastal erosion such an issue on the Holderness coast
- geology
- fetch
- LSD
- subaerial processes
Influences on coastal erosion - geology
what are cliffs composed of
- shallow & sloping cliffs ranging between 5 & 20 metres high
- mainly consists of boulder clay made of glacial till
- which is structurally weak
- & provides little resistance to erosion
what is glacial till
- a mixture of fine clay, boulder clay & sands deposited by glaciers during the Devensian period
Influences on coastal erosion - geology
erosional features on cliffs
- the chalkband that surrounds the boulder clay creates a headland
- erosion along fault lines & bedding planes has created cliffs arches & stacks here
Influences on coastal erosion - fetch
The North sea
- The holderness is exposed to waves & winds from the North-East
- meaning it has a large fetch of 500-800 km, across the North Sea
Influences on coastal erosion - fetch
The Atlantic Ocean
- currents circulate around the Atlantic Ocean
- which has a fetch of 5000km or more,
- so currents add energy to destructive waves
Influences on coastal erosion - fetch
Sea level
-low pressure air systems –> raises sea level
Influences on coastal erosion - fetch
small seas
small almost enclosed seas generate huge waves during storms
Influences on coastal erosion - fetch
friction
- sea floor is deep so there is less friction
- meaning wave height and speed is not lowered
Influences on coastal erosion - LSD
transportation of material
- the boulder clay erodes to produce mainly clay particles
- which are transported out to sea in suspension,
- rather than accumulating onshore as beach sand
Influences on coastal erosion - LSD
narrow beaches
- beaches are narrow
- which is the result of an imbalance between the input of sand & removal of sand
- so these narrow beaches offer little friction to absorb wave energy
Influences on coastal erosion - LSD
tidal flows
- tides flow southwards,
- transporting sand by LSD
- leaving the cliffs at Holderness poorly protected against wave attack
Influences on coastal erosion - subaerial processes
chemical weathering
- chemical weathering is relatively ineffective at the Holderness coast
- except on chalk cliffs
Influences on coastal erosion - subaerial processes
mechanical weathering
- mechanical weathering involves freeze-thaw & the alternate wetting / drying of the boulder clay,
- making it crumbly in the dry period
Influences on coastal erosion - subaerial processes
mass movement
- slumping results from the alternate wetting & drying of the clays
- causing expansion & shrinkage
- leading to cracks during long dry periods
- subsequent rain enters & percolates into these cracks
- which weakens the cliffs
- causing slides down & is then removed by the sea
Where is the Holderness coast located
East coast of England, in Yorkshire