depositional landforms Flashcards
what is a beach?
the area of deposited material between the low water line to the limit of storm waves.
how are sandy beaches formed?
- usually formed in a sheltered bay
- low wave energy (most energy focused on surrounding headlands), constructive waves transport material to the shore
- gentle profile (tend to be quite flat)
how are pebbly beaches formed?
- more exposed beaches tend to be steeper and more pebbly.
- higher energy waves remove the sand, leaving the larger shingle behind, due to destructive waves having a large backwash.
what are sand dunes?
small ridges or hills of sand found at the top of a beach (away from the reach of the waves).
what conditions do sand dunes need to form?
- large supply of sand
- large, flat beach
- an onshore wind
- an obstacle for the dune to form against e.g. driftwood
how do sand dunes form?
- wind transports sand across a beach through saltation.
- deposition occurs around obstacles such as rocks or seaweed.
- over time, the sand builds up, creating small embryo dunes.
- these dunes are stabilised by vegetation such as marram grass. the long roots bind the sand together.
- the dunes develop even more, and over time, the rotting vegetation adds organic matter to the sand, and so more vegetation is able to grow.
what is a spit?
a long, narrow finger of sand or shingle jutting out into the sea from the land.
how do spits form?
- prevailing wind blows at an angle to the coastline.
- longshore drift occurs, due to the swash and backwash of the waves, and material is transported.
- when the coastline changes direction (e.g. turns a corner), deposition continues out into the sea, forming a spit.
- the spit continues to grow overtime, until a cross wind creates a recurved end.
- the area behind the spit is now sheltered, so deposition occurs, and a salt marsh may form.
why is the sediment at the end of the spit lighter and smaller than at the beginning of the spit?
- longshore drift can carry light material much further.
- the sediment has been transported further, so it may have been eroded more through attrition.
what are bars?
when a spit has grown across a bay, trapping a lagoon behind it.
how are bars formed?
- a spite grows across a bay
- it joins two headlands and becomes a bar
what prevents bars from forming?
if there’s a river with a strong current that travels through the bay and into the water behind the spit, it can prevent a bar from forming.