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Depositional Landforms - Coggle Diagram
Depositional Landforms
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Bars
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In the UK some offshore bars have been driven onshore by rising sea levels following ice melt at the end of the last glacial period some 8000 years ago
ridges of sand across the bay, connecting the land on both sides
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Tombolos
A tombolo is formed when a spit connects the mainland coast to an island. A spit is a feature that is formed through deposition of material at coastlines. The process of longshore drift occurs and this moves material along the coastline.
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