Edexcel A-Level Geography 9GE0
Tectonic Processes and Hazards
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Glaciated Landscapes and Change
Evidence for Pleistocene ice extent
- 2 things to know
- Paper 1
Overview
Recall questions on erratics, striations, moraines, drumlins and till as records of how far the ice reached.
What you need to know
Answer each one before you reveal it.
What do till deposits reveal about Pleistocene glaciation?
Questions from this subtopic
Each one with the model answer underneath.
- 1
How do erratics show how far the ice reached during the Pleistocene?
Model answer
They are large boulders transported by ice and deposited far from their source rock, indicating the former presence and movement direction of ice sheets.
- 2
What do striations on bedrock reveal about past glaciation?
Model answer
They are scratches carved into rock by debris embedded in moving ice, indicating the direction of former ice flow beyond present ice margins.
- 3
How do U-shaped valleys serve as evidence for Pleistocene glaciation?
Model answer
Their distinctive cross-profile with steep sides and flat floors indicates erosion by valley glaciers that once occupied areas now ice-free.
- 4
What do moraines indicate about former ice extent?
Model answer
They are ridges of glacial debris deposited at ice margins, marking the former positions and maximum extent of glaciers and ice sheets.
- 5
How do drumlins provide evidence for past ice sheet coverage?
Model answer
These streamlined hills of glacial sediment indicate the direction of ice flow and the presence of former ice sheets in areas now ice-free.
- 6
What do till deposits reveal about Pleistocene glaciation?
Model answer
Unsorted sediments deposited directly by ice indicate former glacial coverage in areas far beyond present ice margins.
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