Geography - Coasts Flashcards
What are the differences between constructive and destructive waves?
Constructive:
- strong swash
- long wavelength, short fetch
- builds the beach
Destructive:
- strong backwash
- short wavelength, long fetch
- erodes the beach, making it steeper
Explain the different types of coastal erosion.
- Attrition - rocks smash against each other and become smaller, rounder and smoother.
- Abrasion - rocks are smashed against the cliff wearing it away.
- Solution - rocks are dissolved
- Hydraulic action - the power of the wave forces air and water into cracks making them bigger.
What is the difference between discordant and concordant coastlines?
Concordant - when the geology (rocks) are arranged parallel to the coastline.
Discordant - when the geology (rocks) are at 90 degrees to the coastline.
What 3 factors affect the power of a wave?
- Fetch (the distance which the wind has blown over the sea)
- Power of the wind
- Length of time the wind has been blowing for
Describe the formation of a wave cut platform/notch.
- The sea attacks/erodes the base of the cliff (hydaulic action and abrasion)
- A wave cut notch is formed
- As the notch increases in size, the cliff becomes unstable so collapses, meaning that the cliff face retreats
- A wave cut platform is left behind where the cliff previously was
- This process repeats and the cliff continues to retreat
How are headlands and bays formed?
- On a discordant coastline, the cliff is made up of different types of rock/geology.
- The soft rock is less resistant so is eroded by the waves, creating bays. Bays are sheltered so material is often deposited by constructive waves, forming beaches.
- The hard rock is more resistant so is eroded much less and therefore remains, forming headlands.
Outline the steps of how a stump is created.
- Waves attack/erode a cliff/headland, creating a crack in the rock
- Hydraulic action widens the crack, forming a cave
- Abrasion fully breaks through the cave, creating an arch
- The arch continues to erode and is unsupported so collapses, leaving a stack
- Waves weaken the bottom of the stack; it falls over, forming a stump
Describe the process of longshore drift.
A wave approaches the beach in the direction of the prevailing wind, meaning that the wave’s swash carries material towards the beach at an angle. The backwash goes straight back to the sea (at a 90 degree angle to the beach) due to gravity. This causes material to be transported along the coastline.
Describe the process of longshore drift.
A wave approaches the beach in the direction of the prevailing wind, meaning that the wave’s swash carries material towards the beach at an angle. The backwash goes straight back to the sea (at a 90 degree angle to the beach) due to gravity. This causes material to be transported along the coastline.
Describe the formation of a spit.
Longshore drift carries material along the coastline, where the coastline changes direction deposition of material takes place forming a piece of land jutting out into the sea. When the wind changes direction, a hook can be made at the end of the spit. Behind a spit, the water is very sheltered as the waves cannot get past the spit so silts are often deposited, forming a salt marsh.
What are the impacts of longshore drift on the coastline?
- Can destroy a beach by removing all the material from it
- Can change the shape of a beach
- Can create landforms such as spits
- Can make estuaries used as harbours too shallow because of deposited material
Explain the factors affecting rate of landform change on two contrasting coastlines.
Holderness:
- Boulder clay is less resistant.
- Rock groyne stopped longshore drift and narrowed the beach.
- Sea wall and granite rip-rap at Withernsea to slow down erosion.
- The removal of sediment offshore has made the coastline more vulnerable
- Frequently subjected to powerful destructive waves from the North Sea.
Jurassic coastline:
- Discordant coastline created Swanage Bay and Headlands of Durlston and Ballard Point which have Old Harry’s stack.
- Concordant coastline has hard limestone parallel to coastline and in one place has punched through the outer layer and created Lulworth Cove from the less resistant clays and sands.
- Weight of buildings on cliff top e.g. The Grand Hotel in Swanage increase landslides.
- The construction of 19 timber groynes, restoration of the sea wall, beach replenishment with 160,000 tonnes, cliff regrading - reduced rate.
What is cost/benefit analysis?
Weighing up the costs of protection against the benefits of protection.
What are the two types of mass movement?
Rotational slumping - caused by water entering dry cracks in the cliff and saturates the soil so it becomes too heavy for the cliff and it slides down, quick movement of a lot of material
Soil creep - slow downhill movement of soil
What is weathering and what are the 3 types?
Weathering - the breakdown of rock in-situ
Physical Weathering - water gets into cracks, freezes and expands over night widening cracks (freeze-thaw weathering) or rock heated during day, expands and at night cools and contracts - layers peel off (onion skin weathering)
Biological - roots get into cracks and as plant grows, roots expand widening the cracks.
Chemical - acidic rain reacts with alkaline rock e.g. limestone and breaks it down