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Summary 3.3 Sediment Sources, Cells and Budgets AQA Physical Geography £5.09
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Summary 3.3 Sediment Sources, Cells and Budgets AQA Physical Geography

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Key notes on Unit 3.3 Sediment Sources, Cells and Budgets in AQA Physical Geography A level. Includes key definitions, diagrams etc and provided a final A* grade.

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  • Unit 3.3
  • May 2, 2023
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  • 2022/2023
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3.3 - Sediment sources, cells and budgets

SOURCES OF SEDIMENT - the crustal sediments that form depositional features such
as beaches and mudflats originate from the following sources:

Sediment sources:
1. Rivers: sediment will be deposited in river mouths and estuaries where it will be
reworked by waves, tides and currents, accounts for 90% of coastal sediment.

2. Cliff erosion: extremely important in areas of soft or unconsolidated rock (contributes
only 5% or less to coastal systems)

3. Longshore drift: sediment is transported from one stretch of coastline (as an input) to
another stretch of coastline (as an output).

4. Wind: in glacial or hot arid environments, wind-blown sand can be deposited in coastal
regions.

5. Glaciers: ice shelves break into the sea, depositing sediment trapped within the ice

6. Offshore: rising sea levels have meant that sediment from continental shelf areas have
been swept to the shoreline.

7. Biological origin: for example, shells and corals (very small % of sediment budget)


SEDIMENT CELLS
Sediment cell: a stretch of coastline, usually bordered by two prominent headlands, where
the movement of sediment cell is more or less contained.




Figure 3 – The sediment cell system

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