AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Hot Desert Systems and Landscapes
Wadis, Bahadas and Pediments
- 3 things to know
- Component 1
Overview
Recall questions on wadis and the rainfall and rapid runoff that cut them, on bahadas formed as alluvial fans merge at a mountain front, and on pediments, slope retreat and the transport of debris across them.
What you need to know
Answer each one before you reveal it.
What happens when sediment-laden water exits a confined channel onto a bahada?
What transports debris across the pediment surface?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is a wadi?
Model answer
A steep-sided, flat-floored ephemeral river channel that carries water only during and immediately after rainfall events.
- 2
What happens to a wadi channel between rainfall events?
Model answer
The channel dries out.
- 3
What type of rainfall event initiates wadi formation?
Model answer
An intense rainfall event.
- 4
Why does rapid surface runoff occur in desert environments during rainfall?
Model answer
Because surfaces are impermeable or sparsely vegetated.
- 5
What type of erosion cuts the channel of a wadi?
Model answer
High-energy erosion from flash floods.
- 6
Define a bahada (bajada).
Model answer
A gently sloping plain of coalesced alluvial fans formed where multiple wadis deposit sediment at the base of mountain fronts.
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