Fascinating Fact:
Beaches are formed by deposited material, with sandy beaches usually found in sheltered areas and shingle beaches on more exposed coasts.
In GCSE Geography, coastal deposition is studied alongside erosion to explain how coastlines develop over time. Pupils learn how constructive waves, longshore drift, and changes in wave energy lead to the build-up of sediment. This helps to explain the formation of beaches, spits, and bars, as well as why different stretches of coastline can look and behave very differently.
Key Terms
- Coastal deposition: The process where waves lose energy and drop sand, shingle, or mud, building up new features along the coastline.
- Longshore drift: The movement of beach material along the coast, caused by waves approaching at an angle and returning straight down the beach under gravity.
- Spit: A narrow stretch of sand or shingle that extends from the land out to sea, formed when deposited material builds up beyond a headland or river mouth.
Frequently Asked Questions (Click to see answers)
What is coastal deposition in GCSE Geography?
In GCSE Geography, coastal deposition is when waves drop the material they are carrying because they no longer have enough energy to transport it. This builds up features such as spits, bars, and wide beaches.
What conditions encourage deposition along a coastline?
Deposition is encouraged by gentle, constructive waves, sheltered bays, low wind speeds, and a good supply of sediment from rivers or eroding cliffs. Under these conditions, more material is deposited than removed.
How does longshore drift help form new coastal landforms?
Longshore drift moves material step by step along the shore. Where the coastline changes direction, or at a river mouth, this transported sediment can build out into the sea, forming landforms such as spits and bars.
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