hydraulic action is the force of water pushing against the rock and air gets trapped in cracks causing it to break
abrasion is when rocks are launched against cliff face during high energy conditions, weakening structure
solution/corrosion: the dissolving of soluble rocks by seawater
attrition is when particles roll over each other due to friction and strong wave action
solution is when dissolved material is carried in water
suspension is when fine sediment is carried in water, making the water look murky
saltation is when small pebbles bounce along the seabed
traction is when larger, heavier material are dragged along seabed
sliding refers to the downhill movement of large material on steep hillsides and cliff faces after heavy rainfall has weakened the slope
rotational slumping often occurs after long periods of rainfall which seeps through the soil. where the permeable rock meets an impermeable rock, the saturated rock slumps and slips along a curved surface.
rockfalls happen suddenly when pieces of rock fall from a cliff that has been weathered or undercut by wave action
chemical weathering (solution) is the breakdown of rocks by chemical reactions in the atmosphere. Water reacts with CaCO3 in rocks which dissolves and is washed away, weakening the rocks
mechanical weathering (freeze thaw)
water gets trapped in crack in rock
when temperature is really cold, water freezes and expands, putting pressure on rock
process repeats and further weakens the rock
biological weathering (root action) is the breakdown of rocks by living organisms, such as bacteria and fungi
plant roots can enter a small crack in a rock
as the root grows larger the crack in the rock gets larger
weakens the structure of the rock until it eventually breaks away
coastal erosion is the wearing away of land at the coastline
wave refraction is the bending of waves around headlands and spits
Longshore drift is the process where the waves transport material (sand) along the beach in the direction of the prevailing wind
swash moves material up the beach at an angle, as the waves approach in a similar direction to the wind
backwash moves back down the beach at 90° due to gravity in the direction of the prevailing wind
movement continues at 90 degree angle
influence of geology on the coast
headlands are more resistant to erosion since they're made out of hardrock- juts out
bays are less resistant and erode quicker because they're made out of softrock
causes differential erosion
influence of vegetation on the coast
brings stability to low energy coasts
allows flocculation- binding of sediment in big clusters when it's too heavy to carry by wind/water
plants protect sediments from current speeds and erosion
influence of people on the coast
housing for commuters
agriculture destroys habitats for space to grow crops
coral mining ruins coral reefs
dynamite fishing causes coastal erosion and beach degradation
influence of sea level changes on the coast
can destroy agriculture and coasts
global warming -> thermal expansion and ice sheets melting -> sea levels rise (eustatic change)
more frequent storms -> wave energy moves inwards onshore -> erosion of cliffs
constructive waves have
a strong swash but weak backwash
long wavelength, low in height and frequency
sandy beaches (depositional)
destructive waves have
weak swash but strong backwash
short wavelength but high in height and frequency
shingle beaches (erosional)
conflicts on coast
human needs (development) vs well being of coastal ecosystems (conservation)
development (farmers and fishermen): provides more jobs to boost economy, more houses to support population and more ports for trade to increase GDP
conservation (environmentalists): protects wildlife by acting as a coastal barrier and brings more tourism
what causes coastal flooding
high tides: periodic- happen nearly everyday, worse when combined with storm surges, threatens infrastructure and agriculture
sea level rise: increased global warming = thermal expansion
storm surges: rising sea levels = frequent flooding = severe storms, scale and height are intense making it a huge threat
tsunamis: infrequent but predicted by seismometers
The Holderness coastline is located on the east coast of England and is the fastest eroding coastline in Europe (1.8m each year)
Reasons for rapid erosion at Holderness
Rock types - cliffs are made from less-resistantboulder clay which slumps when wet
Narrow beaches- give less protection to the coast as they don't reduce the power of the waves.
Hard engineering- groynes stop LSD and build up the beaches which narrows unprotected beaches as new sand does not replace sand eroded by waves.
Powerful waves - travel long distances over the North Sea (so have a long fetch) which means they will increase in energy.
Management strategies
Bridlington is protected by a 4.7 km long sea wall.
Hornsea is protected by a sea wall, groynes and rock armour.
Coastal management at Withernsea has tried to make the beach wider by using groynes, and a sea wall to protect the coast.
Mappleton is protected by rock groynes.
Spurn Head is protected with groynes and rock armour.
conflicts
There has been an increase in erosion at Mappleton because the groynes used leads to farms being destroyed by erosion
Some people disagree with where the sea defences have been located, especially if land in their community is not protected.
Some sea defences negatively impact tourism and reduce the amount of money coming in to the area.
erosional processes are hydraulic action, abrasion, attrition and solution
mass movement is when rocks loosen and fall down a slope due to gravity (rotational slumping, sliding and rockfall)
weathering is the breakdown of rocks by natural processes, such as water, and wind (biological, chemical and mechanical)
what are the 4 ways sediment can be transported along a beach