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
Deflation Hollows, Yardangs and Zeugen
- 3 things to know
- Component 1
Overview
Recall questions on how deflation strips fine sediment to form deflation hollows and desert pavements, on ventifacts, and on the differential erosion of softer and harder rock that shapes yardangs and undercuts zeugen beneath their cap rock.
What you need to know
Answer each one before you reveal it.
What is a desert pavement?
What role does harder rock play in yardang development?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What process removes loose, fine-grained sediment from the desert surface to form deflation hollows?
Model answer
Wind erosion removes fine particles from the surface.
- 2
Why does coarser material remain at the surface during deflation hollow formation?
Model answer
Coarser material is too heavy for the wind to transport.
- 3
How does a deflation hollow change over time as wind erosion continues?
Model answer
The depression deepens over time as more fine material is removed.
- 4
What is a desert pavement?
Model answer
A surface of closely packed stones left behind after wind removes finer material, creating a protective armour layer.
- 5
What are ventifacts?
Model answer
Rocks shaped and polished by wind-blown sand abrasion, often developing flat faces (facets) oriented toward prevailing winds.
- 6
In yardang formation, what happens to softer rock compared to harder rock?
Model answer
Softer rock is eroded more rapidly than harder rock.
Other ways to work this
The same content, four other ways.
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