Edexcel A-Level Geography 9GE0
Tectonic Processes and Hazards
Glaciated Landscapes and ChangeLandscape
Coastal Landscapes and ChangeLandscape
Globalisation
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The Water Cycle and Water Insecurity
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Coastal Landscapes and Change
Spits, bars, tombolos and other depositional landforms
- 3 things to know
- Paper 1
Overview
Recall questions on recurved and double spits, offshore and barrier bars, tombolos and cuspate forelands.
What you need to know
Answer each one before you reveal it.
Define a barrier beach and describe its relationship to the land behind it.
How do double spits form?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is a recurved spit and what causes its distinctive shape?
Model answer
A recurved spit is an elongated depositional feature where the distal end curves landward due to wave refraction or secondary wave direction.
- 2
How do double spits form?
Model answer
Double spits form where spits grow from opposite sides of an estuary or bay entrance, extending towards each other.
- 3
What is an offshore bar?
Model answer
An offshore bar is a submerged or partially exposed ridge of sediment running parallel to the coast.
- 4
Define a barrier beach and describe its relationship to the land behind it.
Model answer
A barrier beach is an elongated depositional feature parallel to the coast that encloses a lagoon or marsh behind it.
- 5
How do barrier bars differ from offshore bars?
Model answer
Barrier bars are ridges of sediment exposed above sea level that stretch across a bay and trap a lagoon behind them, whereas offshore bars are submerged ridges of sediment parallel to the shoreline.
- 6
What is a tombolo?
Model answer
A tombolo is a depositional feature that connects an island to the mainland via a sand or shingle bar.
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