The features that are found on a coastline, and the processes which form them, is one of the topics looked at in GCSE Geography. This quiz looks specifically at those features which are caused by coastal deposition.
Is there anything more enjoyable than a day at the beach? Golden sand for lying on, the sea for swimming and surfing, rocky headlands that can be walked along, bays that are sheltered from the worst of the wind and waves, and tall, towering cliffs with rocky shingle beaches below and caves carved into their faces.
All these are beautiful features of a coastline, but have you ever thought about what caused them - specifically, how stuff is deposited on the coastal margins? Next time you’re walking on the shore you’ll be able to understand why the waves make two different noises as they wash up the beach and then wash down again, and what a reef actually is. Deposition can create marshes and coastal barriers as well as sand and shingle beaches.
[readmore]Coastal deposition is exactly what it sounds like - the laying down (or deposition) of material at the coastline by the sea. That material can come from rivers eroding material off the land and sometimes material lost in one country can wash up in another. Various management techniques exist to help encourage deposition at the coast, normally to help protect property and infrastructure, but further erosion elsewhere along the coast can be caused by this forced deposition. Deposition may also be a problem. The silting up of shipping channels will require the local authorities to dredge them using specially designed ships and machinery. Sand dunes, sand banks and other features may become colonised by plants that can stabilise their structures and lead eventually to the creation of new land.
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You can find more about this topic by visiting BBC Bitesize - Coastal environments
When waves enter a cove or bay they are more likely to slow in the shelter and drop their load rather than the other way round
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Swash is the period after the wave has broken and it washes up the beach. Swash normally acts at an angle to the beach rather than straight up and down. Swash and backwash are the noises you hear as the water runs up and down the beach
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On Holderness coast most of the eroded material is carred out to sea, but some is moved south via longshore drift to form Spurn Head
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Both coastal and river transport methods are the same - Solution, Suspension, Saltation and Traction
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When swash is stronger than backwash material is carried up the beach but not carried back down, leading to deposition
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Constructive waves occur when the swash is stronger than the backwash. A steep beach will have a strong backwash as water runs faster down steeper slopes. Steep cliffs are normally exposed with little material to protect them
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After an arch collapses a stack is left behind. The formal definition of a reef is a ridge of rock, shingle or sand at or just below the surface of the water
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These long low waves are created in calm weather and will deposit material on the coast
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A tip to remember is that material is deposited when energy levels drop, in this case because the coast in effect vanishes at the wide mouth of the Humber
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One of the key examples of a tombolo is Chesil Beach, connecting the Isle of Portland to the Dorset coastline
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