OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Dryland Landscapes
Weathering and mass movement in dryland landscapes
- 2 things to know
- Component 01
Overview
Recall questions on salt weathering and sodium sulfate, tafoni, insolation weathering and the moisture debate, freeze-thaw, hydration and oxidation in deserts, desert varnish, and rockfalls, debris flows and dry ravel on desert slopes.
What you need to know
Answer each one before you reveal it.
Define weathering in a dryland landscape
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define the term weathering.
Model answer
Weathering is the breakdown of rock in place at or near the Earth's surface, without any transport of the material produced.
- 2
How does salt weathering break up desert rock?
Model answer
Salt-bearing water is drawn into pores and cracks and then evaporates, and the salt crystals that grow exert pressure against the pore walls, so repeated crystallisation prises grains and flakes apart.
- 3
Why is salt weathering especially effective in deserts?
Model answer
High evaporation constantly concentrates salts at and just below the surface, and there is too little rainfall to flush them away again.
- 4
Which salt is particularly destructive because it expands greatly when it takes up water?
Model answer
Sodium sulfate is particularly destructive, because it swells substantially as it hydrates to form mirabilite.
- 5
What is tafoni?
Model answer
Tafoni are cavernous hollows weathered into a rock face, usually excavated by salt crystallisation working behind a harder case-hardened outer skin.
- 6
Explain the process of insolation weathering.
Model answer
Intense daytime heating expands the outer layer of a rock while the interior stays cooler, and the repeated expansion and contraction sets up stresses that flake, granulate or shatter the surface.
Other ways to work this
The same content, four other ways.
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Six ways to work the same material.
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