Edexcel GCSE Geography A 1GA0
Changing Cities
Coastal Landscapes and ProcessesLandscape option
Ecosystems, Biodiversity and Management
Energy Resource ManagementResource option
Geographical Investigations – Fieldwork
Geographical Investigations − UK Challenges
Geographical Skills
Glaciated Upland Landscapes and ProcessesLandscape option
Global Development
Mathematics and Statistics Skills
Resource Management
River Landscapes and ProcessesLandscape option
The Changing Landscapes of the UK
Water Resource ManagementResource option
Weather Hazards and Climate Change
The Changing Landscapes of the UK
How the UK’s upland and lowland landscapes were formed
- 3 things to know
- Paper 1
Overview
What ice did to the mountains, corries, U-shaped valleys and till, freeze-thaw and chemical weathering, climate differences between west and east, rivers and slope processes since, and how farming, forestry and building altered the land.
What you need to know
Answer each one before you reveal it.
How does building a town or city alter the surface of the land?
What shape is a valley left behind by a glacier, and how does it differ from one cut by a river?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What did moving ice do to the mountains of Britain during the last glacial period?
Model answer
It scoured out deep, steep-sided valleys with flat floors, and gouged hollows and knife-edged ridges into the high ground.
- 2
Describe a corrie and say how ice made it.
Model answer
It is an armchair-shaped hollow high on a mountainside, deepened as ice rotated within it, plucking rock from the back wall and grinding the floor.
- 3
What shape is a valley left behind by a glacier, and how does it differ from one cut by a river?
Model answer
A glacier leaves a broad U-shape with steep sides and a wide flat floor, while a river cuts a narrow V-shape.
- 4
What material did the ice sheets dump across lowland Britain?
Model answer
Till, an unsorted mix of clay, sand and boulders dropped straight from the ice, together with sands and gravels sorted by meltwater streams.
- 5
Explain freeze–thaw weathering and say where in Britain it is most active.
Model answer
Water seeps into a crack, freezes and expands, prising the crack wider until fragments snap off, and it works hardest on exposed mountain summits where temperatures cross 0°C often.
- 6
How does rainwater chemically attack limestone and chalk?
Model answer
Rain is slightly acidic, so it dissolves the calcium carbonate, opening up joints into caves, gorges and underground passages.
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