Landforms Of Depostition Flashcards
Spit
Longshore drift moves material along the coastline. A spit forms when the material is deposited.
Bar
A ridge of sand or shingle which forms across the mouth of a river or entrance to a bay or harbour. Longshore drift transports sediment and deposits it.
Tombolo
Change in the shape of the headland results in the formation of a spit.
The spit grows out from the mainland and joins to an island creating a tombolo.
Storm beach
At the back of the beach, very powerful waves during storm conditions may deposit larger material forming a storm beach.
Cuspate foreland
Formed when longshore drift comes from both ways.
Breakpoint bar
Ridges of sediment with crests generally running parallel to the coast which form where steep destructive waves break.
Berm
Smaller ridges that develop at the position of the average high tide marks resulting from deposition.
Ridges and runnels
Occur in sand. They form parallel to the shore in the foreshore zone. Ridges are raised above the shore, either side of a runnel. They form as a simple drainage route for water.
Cusps
Beach cusps are made up of various grades of sediment in an arc pattern. The horns are made up of coarser materials and the embayment contains all the finer grade sediment.
Barrier islands
Narrow nearshore or offshore deposits of sand or sediments that are parallel to the coastline. The islands are separated from the mainland by a shallow lagoon. They are often found in chains and are separated by narrow tidal inlets. Glaciers melted after the last ice age, the sea levels rose and the contained sediment from the ice was released. Rising water pushed the sediment towards the land and was deposited in shallow areas just off the coast. Waves then continued to bring in sediment and build up the islands.
What 5 things do you need to form a sand dune?
- large supply of dry sand
- large tidal range (sand has longed to dry/ wet sand cannot be picked up)
- gently sloping beach
- onshore winds that are 15kph + (sand picked up and blown by wind- saltation)
- object/obstacle (forms a windbreak, slowing down sand)
How is a sand dune formed?
Sand piles up by and object and turns into an ever increasing wind break.
Sand piles into a dune at the back of the beach.
Sand is pushed over the dune crest, falling down the steeper windward slope.
The dune moves steadily inland.
Pioneer plants colonise the dunes.
Roots eventually hold sand in place.
New sand dunes build up behind the first dune.
3 features of new/embryo dunes
- continually moving sand (covers up pioneers, no anchor points for roots, very abrasive to plant tissue)
- very little freshwater (rainwater rapidly percolates through coarse sand, no organic matter to retain water, salt from sea spray makes it hard for plants to absorb water)
- very few nutrients (there is no dead organic matter being recycled in the sand)
Name 2 pioneer species for sand dunes
Sand couch grass
Lyme grass
How are pioneer species adapted to live on sand dunes? 3 adaptions
- tolerant of salt (live closer to sea)
- waxy leaf coating (retains water)
- rolled leaves (reduces transpiration)