Paper 1 Section C Coastal erosion, deposition and management Flashcards
What is coastal erosion?
Erosion means wearing away the land. Coastal erosion means the sea causes this
- Corrasion - waves fling material at the cliff and pieces fall off
- Abrasion - pebbles wear away the rock they come into contact with - sandpaper effect
- Hydraulic action - waves get into cracks in the rock, create pressure and as the wave falls back the pressure is released taking small bits of rock with it (makes the crack bigger)
- Attrition - material in the sea bashes against eac other making pebbles smaller and more rounded
- Solution (or Corrosion) - acid/salt in the water wears away the rock eg limestone
How is material transported?
- Traction - rolling heavy material
- Saltation - water bounces the material along the bed
- Suspension - light materila floating in the water
- Solution - material dissolved in the water
Whay is material deposited?
Deposition happens when the material is too heavy for the water to carry; when the water slows down
What is longshore drift? Can you draw THE diagram accurately?
Longshore drift is the movement of material along the coastline. It depends on the direction of the prevailing wind.
Material is carried up the beach (swash) at the angle of the prevailing wind but returns to the sea (backwash) at right angles. Material therefore moves in a zig-zag pattern.
Name at least 6 features of coastal erosion you might sea at the coastline
What causes different coastal features?
- Headlands and bays
- Caves, arches, stacks and stumps
- Cliffs and wavecut platforms
Coastal features depend on the rock type - resistant or weaker rocks.
How are headlands and bays formed?
More resistant rock is separated by weaker rock.
The waves erode the weaker rock by hydraulic action and abrasion further inland than the more resistant rock
Deposition of the material forms the beach
(Aerial diagram)
Bays are sheltered areas - popular with tourists
The headlands may have caves, arches etc
How are caves, arches, stacks and stumps formed?
Learn the diagram!
Cracks (lines of weakness - joints and bedding planes) in the rock on a headland are widened by hydraulic action and abrasion
A crack forms a cave which is further eroded by HA into the headland
Another cave may also have formed on the other side of the headland. When these are back to back the wall between the 2 will collapse causing a sea arch.
Further abrasion and HA as well as weathering (eg freeze- thaw, rain) on top of the arch make the roof collapse to form a stack
HA and abrasion cause the stack to become smaller. The stump may be covered at high tide.
How are wavecut platforms formed?
Lines of weakness are widened by waves at high tide. HA causes a wavecut notch to be formed which erodes deeper into the cliff.
As nothing is then supporting the rock above the cliff will collaspe.
The sea will remove some of the material but the solid rock base remains which shows the extent of the erosion of the cliff.
The wavecut platform will be covered at high tide. Often a lighthouse marks where rocks are just below the surface of the sea.
What features are formed by coastal deposition?
Beaches
Sand dunes and
spits are caused by deposition
How are beaches formed?
Beaches are built up from deposits of sand
Created by constructive waves
Pebble beaches form where the waves are strong and wash away the sand. Pebble beaches are also called shingle beaches and are steeper than sandy ones.
What shape are the pebbles?
How are sand dunes formed?
See diagram
Small hills (embryo dunes) of sand are formed round obstacles eg rocks.
These remain in place and vegetation (eg marram grass) grows making them more stable
Decomposing vegetation makes the sand more fertile
Ponds may develop in the shallow hollows (slacks) between the dunes
Explain the formation of a coastal spit (or bar)
- LOngshore drift moves sand along the beach in the directionof the prevailing wind
- The coastline suddenly changes direction but LD continues (out into the sea)
- Material is deposited in the sea to create a bank of sand
- Occasionally the wind direction changes and a hook is formed at the end of the spit as the change of direction causes the sand to move in a different direction (a recurved end)
- When the prevailing wind returns the spit will continue to ‘grow’. Sand dunes oftern form and the spit is used for tourism. Lifeboat stations are often at the end of the spit. Hurst Castle spit had a wartime look out post which was converted to a prison. Groynes are often used to reduce LD along the spit
- A saltmarsh is created behind the spit where the water is shallow and sheltered. If there is a river mud deposits (mudflats) will build up
- A ‘bar’ is a spit which joins land to land (eg across a bay)
Name real examples of coastal features
The Dorset coastline on the south coast of the UK has:
Old Harry Rocks (Stacks and stumps)
Durdle Dor is a sea arch at Lyme Regis in Dorset
Swanage Bay is between Ballard Point (Headland) and Peveril point (headland)
There is a spit at Poole Harbour but we have used Hurst Castle Spit
OS MAPWORK
Practice labelling and identifying features using 4 and 6 fig grid references. Page 65 of your revision guide
What is hard engineering?
Name 4 examples and how they work
Hard engineering is the use of solid materials to manage coastal erosion
- A curved sea wall - built of concrete and curved to reflect the enegry of the waves back to sea as they hit the wall. They also act as a barrier against flooding.
- Revetments - can be sloping or stepped (Blackpool). These break the force of the waves and allow the water to return to the sea without eroding the land.
- Rip rap/rock armour is large boulders placed at the base of the coastline/cliff. They have gaps between them and allow the waves to break on to them, absorbing the energy, and return through the gaps back to the sea.
- Gabion crates are rock filled ‘baskets’. these are piled on top of each other and work like rip rap. They also protect the cliff behind (usually soft rock). Vegetation can grow on them and make them look more natural.
- Grounes are used to protect the beach from longshore drift and hold sand in place. They also allow waves to break on to them, absorbing the energy. Buils at right angles to the coastline.