Fascinating Fact:
Biological weathering is caused by living organisms, such as plant roots forcing their way into cracks or animals burrowing.
In GCSE Geography, weathering explains how rocks are broken down in their original place without being moved. You study how physical, chemical, and biological processes gradually weaken rock, create loose material, and prepare landscapes for erosion. Understanding weathering helps you explain features such as scree slopes, rock pavements, and the early stages of soil development in different environments.
Key Terms
- Weathering: The breakdown of rock in its original place by physical, chemical, or biological processes.
- Mechanical weathering: Weathering that breaks rock into smaller pieces without changing its chemical composition, for example freeze-thaw action.
- Chemical weathering: Weathering that changes the minerals in rock, for example when acidic rainwater dissolves limestone.
Frequently Asked Questions (Click to see answers)
What is weathering in GCSE Geography?
In GCSE Geography, weathering is the process that breaks down rock where it is, using physical, chemical, or biological actions, without moving the material to a new place.
What are the three main types of weathering?
The three main types of weathering are mechanical (physical) weathering, chemical weathering, and biological weathering, each working in different ways to weaken and break rock apart.
How is weathering different from erosion?
Weathering breaks rock down in its original place, while erosion transports weathered material away using agents such as rivers, wind, ice, or the sea to new locations.
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