Fascinating Fact:
Limestone pavements have flat, exposed blocks called clints, separated by deep cracks known as grikes, which provide sheltered habitats for plants.
In GCSE Geography, limestone and chalk features are studied as classic examples of how rock type controls landscape. Pupils explore pavements, gorges, caves, dry valleys, and chalk escarpments, and consider how people use and manage these fragile environments for farming, tourism, and conservation.
Key Terms
- Limestone pavement: A flat, exposed limestone surface divided into blocks (clints) and deep cracks (grikes) by weathering.
- Chalk escarpment: A steep chalk slope with a gentle dip slope on one side and a steep scarp face on the other.
- Karst landscape: A landscape formed on soluble rocks, such as limestone, with features like sinkholes, caves, and disappearing streams.
Frequently Asked Questions (Click to see answers)
What are limestone and chalk in GCSE Geography?
In GCSE Geography, limestone and chalk are sedimentary rocks made mainly of calcium carbonate. They form in shallow seas from shells and skeletons, and create distinctive upland and coastal scenery.
What landforms are created by limestone and chalk?
Limestone can form pavements, gorges, swallow holes, caves, and dry valleys. Chalk often forms escarpments, rolling downs, and white sea cliffs where it meets the coast.
Why are limestone and chalk areas important to people?
These areas provide tourist attractions, good grazing land, building stone, and underground water supplies, but they also need careful management to protect fragile habitats and landscapes.
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