1.2.1 the coast and waves Flashcards
describe an overview of waves on the coast.
- the coast is a narrow contact zone between the land and the sea
- it is a changing landscape
- waves are the primary force causing erosion along the coastline
- a wave is formed by wind blowing across the sea.
- the distance of wind flow is called ‘fetch’
- the larger the wave the more energy it contains
name the features of a cliff.
- the cliff
- the wave cut platform
- the wave cut notch. this is at the foot of the cliff and there is more energy (and thus erosion) as there are more waves. eventually the cliff will crumble because of the weight.
how are these landforms created?
- the original position of the cliff is eaten away by the low and high water mark
- the cliff retreats, causing the wave-cut platform
- the cliff increases in height as a wave-cut notch is formed
describe the process of longshore drift.
position 1:
- prevailing (usual) wind direction is against the start of the beach, with the direction of the waves
- material is carried up the beach
position 2:
- backwash takes material straight down the beach under gravity.
- this repeats in a zig-zag process.
- material is carried along the beach by longshore drift.
what is the swash?
the water that rushes up a beach after the wave has broken is called the swash. it picks up material, travelling in the same direction as breaking waves.
where is the prevailing wind in britain?
the south-west. material is moved from west to wast along the south coast of england.
name a response to longshore drift and what it does.
groynes reduce the force of waves and cause material to pile up on their windward side.
what is a vulnerability of groynes?
they leave further down the coast with less sediment and material, therefore there is a smaller barrier between the land and waves.
what are spits created from?
deposition.
what is a spit?
an extended piece of beach material that projects out to sea and is joined to the mainland at one end.
why does longshore drift occur on spits?
because the prevailing wind blows at an angle to the coast.
how does a spit form?
- longshore drift moves material
- a spit forms where it is deposited
- the spit grows and develops a hook if wind direction changes
- waves cannot get past which creates a sheltered area silt is deposited
- they commonly form mud flats or salt marshes
why do spits form?
- when longshore drift moves a lot of material along a beach to reach it’s end
- where there is a sudden change in direction of the coastline
- is the sea is shallow and sheltered
- second wind direction
- a change in direction like the river mouth or estuary. it loses energy as the waves have nothing to push against
what processes occur with longshore drift?
- suspension, saltation and traction
why do spits have the characteristics they do?
- they usually have hooked ends as the wind may come from a second direction
- they don’t usually go across the estuary as the river flow is too powerful
- salt marshes often develop behind them