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
Rock type and structure in dryland landscapes
- 3 things to know
- Component 01
Overview
Recall questions on lithology and rock resistance in deserts, mesas and buttes in Monument Valley, permeability, joints and bedding planes, calcrete, gypcrete and silcrete duricrusts, sandstone as a dune source, dipping strata, and faulting in the Basin and Range Province.
What you need to know
Answer each one before you reveal it.
Why do horizontally bedded resistant strata produce mesas and buttes?
Name a desert landscape famous for mesas and buttes cut in horizontal sandstone.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define the term lithology.
Model answer
Lithology is the physical and chemical character of a rock, including its mineral composition, grain size, hardness and permeability.
- 2
How does rock resistance control the shape of a desert slope?
Model answer
Resistant beds stand out as vertical cliffs and caprocks while weaker beds are worn back into gentler debris-covered slopes, producing a stepped slope profile.
- 3
Why do horizontally bedded resistant strata produce mesas and buttes?
Model answer
A hard caprock protects the weaker rock beneath it, so the plateau can only retreat by undercutting and collapse at its edges, leaving flat-topped remnants that shrink into isolated buttes.
- 4
Name a desert landscape famous for mesas and buttes cut in horizontal sandstone.
Model answer
Monument Valley, on the Colorado Plateau of the south-western United States, is famous for its mesas and buttes.
- 5
How does permeability influence runoff in a desert?
Model answer
Permeable rocks such as jointed sandstone and limestone absorb what little rain falls so surface channels are rare, while impermeable shale and clay shed water and develop dense gully networks.
- 6
Why are joints and bedding planes so important in desert weathering?
Model answer
They are lines of weakness along which water, salts and roots can penetrate the rock, so weathering attacks inwards from them and progressively loosens individual blocks.
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