OCR GCSE Geography A J383
Ecosystems of the Planet
Environmental Threats to Our Planet
Fieldwork Skills
Geographical Skills
Landscapes of the UK
People of the Planet
People of the UK
UK Environmental Challenges
Landscapes of the UK
Geomorphic processes: weathering, mass movement, erosion, transport and deposition
- 3 things to know
- Component 01
Overview
Weathering against erosion, freeze-thaw, chemical and biological weathering, mass movement, sliding and slumping, abrasion, hydraulic action, attrition and solution, traction, saltation and suspension, and why deposition takes place.
What you need to know
Answer each one before you reveal it.
How do abrasion, hydraulic action and attrition each erode rock in a river or at the coast?
How does freeze-thaw, the main type of mechanical weathering, break up rock?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is the difference between weathering and erosion?
Model answer
Weathering breaks rock down where it stands without moving it, while erosion wears rock away and carries the loosened material off.
- 2
How does freeze-thaw, the main type of mechanical weathering, break up rock?
Model answer
Water collects in a crack and expands as it freezes below 0 °C, widening the crack, and repeated freezing and thawing eventually splits the rock apart.
- 3
What happens during chemical weathering?
Model answer
Slightly acidic rainwater reacts with minerals in the rock and dissolves them, as when carbonation slowly eats away limestone.
- 4
Give two ways living things cause biological weathering.
Model answer
Plant roots grow into cracks and prise the rock apart, and burrowing animals loosen and break up material.
- 5
What is mass movement?
Model answer
The downhill movement of rock, soil and mud under gravity, often triggered when heavy rain makes the material heavier and more slippery.
- 6
What happens when material slides down a slope?
Model answer
A mass of material moves rapidly straight downslope along a flat surface of weakness, keeping much of its original shape.
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