Coasts Flashcards
(38 cards)
Soil creep
surface runoff slowly moving soil downhill
slumping
Area of saturated land slips downhill
Physical (freeze-thaw)
Rocks break due to changes in temperature
Biological
plants and animals break up the rocks
Chemical
acid in rainwater dissolves the rock
Corrosion (solution)
Material dissolved by the river
Abrasion (corrasion)
Load wears away river channel
Hydraulic action
force of current dislodges loose material
Attrition
Load collides
Traction
Rolling of large load
Saltation
Bouncing of smaller load
suspension
Fine material held within the water
solution
rocks dissolved within the water
Headlands and bays
Headlands and bays are usually found together on the same stretch of coastline.
Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run
perpendicular to the coast.
Bays form where weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger
(more resistant) rocks (such as chalk, limestone, granite) forming a headland.
Cliffs, wave cut notch and wave cut platforms
In areas of more resistant cliff material erosion is greatest when waves break at the foot of a cliff. This causes erosion at the base of the cliff.
- Erosional processes such as hydraulic action and abrasion cut into the base of the cliff forming a wave-
cut notch. As the notch increases in size the weight of the cliff above become too much and the cliff collapses. - The material from the cliff is broken up through attrition and is smoothed out through abrasion, this
leaves a flat terrace at the base of the cliff known as a wave cut platform.
Caves, arches, stacks and stumps
Even hard rock, that forms headlands, contains weaknesses. Hydraulic action forms cracks in the rock
until an opening is formed.
* As the waves continue to attack the rock it is hollowed out to form a cave.
* Further erosion means that the cave is widened and deepened until it becomes an arch.
* Widening of the arch through undercutting means that material becomes unsupported and collapses
into the sea forming a stack.
* Further undercutting causes the stack to collapse leaving only a stump.
Longshore drift
Material is moved in a zigzag manner along the
coastline by a process called Longshore drift.
Waves are pushed towards the shore by prevailing
wind.
The swash carries material up the beach at an angle.
The backwash carries material back to sea at right
angles to the coastline.
If the waves are constructive more material is
deposited than is removed as the swash is stronger
than the backwash.
4 processes of transportation
Traction, saltation, suspension and solution
2 processes of movement
soil creep and slumping
3 processes of weathering
Physical, biological and Chemical
4 processes of erosion
Corrosion, abrasion, hydraulic action and attrition
How are beaches formed
Beaches are made up from eroded material that has been transported and then deposited by the sea.
* Deposition occurs when waves have limited energy, so beaches often form in sheltered areas like bays.
* Constructive waves build up beaches as they have a strong swash and a weak backwash.
* Sandy beaches are usually found in bays where the water is shallow, and the waves have less energy.
* Pebble beaches often form where cliffs are being eroded, and where there are higher energy waves.
* Beaches profile has lots of ridges called berms. They show the lines of high tides and storm tides.
* The size of the material is larger at the top of the beach, due to the high-energy storm waves carrying
large sediment.
* The smallest material is found nearest the water as the waves break here and break down the rock
through attrition.
* A sandy beach typically has a gentle sloping profile, whereas a shingle beach can be much steeper.
* On sandy beaches, the backwash of the waves removes material forming a gently sloping beach. On
shingle beaches the swash is dissipated because the large particle size allows percolation, so the
backwash is not very powerful, and the beach remains steep.
What is a spit?
A spit is a long beach made up of sand and
shingle that extends out to sea. It is found:
* In areas of shallow water.
* On a bend in the coastline.
* Eroded material is carried along the
coast by longshore drift. This action continues
until secondary winds and waves force the spit
to start to curve.
How are spits formed
Sediment is carried by longshore drift
When there is a change in the shape of the coastline deposition occurs. A long thin ridge of material is deposited, this is the spit
A hooked end can form if there is a change in wind direction
Waves cannot get behind the spit meaning that the land behind will erode less and is very sheltered.
Slits are deposited here to form salt marshes or mud flats