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
Hazardous Earth
Fault scarps, rift valleys and the landscapes faulting creates
- 2 things to know
- Component 03
Overview
Recall questions on faults, normal, reverse and strike-slip movement, fault scarps and escarpments, grabens and horsts, how rift valleys form, the East African Rift system and the Ruwenzori block mountains, offset streams and ridges along strike-slip faults, and coastal uplift in earthquakes.
What you need to know
Answer each one before you reveal it.
Describe the movement on a normal fault and the stress that causes it.
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is a fault?
Model answer
A fracture in the crust along which the rock on either side has been displaced.
- 2
Describe the movement on a normal fault and the stress that causes it.
Model answer
Tension pulls the crust apart and one block slides down the inclined fault plane relative to the other.
- 3
Describe the movement on a reverse fault and the stress that causes it.
Model answer
Compression pushes the crust together and one block is driven up over the other along the fault plane.
- 4
What is a strike-slip fault?
Model answer
A fault on which the two blocks slide past one another horizontally, with little or no vertical movement.
- 5
Define a fault scarp.
Model answer
The steep step in the ground surface produced where vertical movement on a fault has raised one side above the other.
- 6
How does a fault scarp grow into a prominent escarpment?
Model answer
Each earthquake adds a small vertical displacement, and over thousands of events those offsets accumulate into a cliff or steep slope hundreds of metres high.
Other ways to work this
The same content, four other ways.
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