Edexcel A-Level Geography 9GE0
Tectonic Processes and Hazards
Glaciated Landscapes and ChangeLandscape
Coastal Landscapes and ChangeLandscape
Globalisation
Regenerating PlacesPlaces
Diverse PlacesPlaces
The Water Cycle and Water Insecurity
The Carbon Cycle and Energy Security
Superpowers
Health, Human Rights and InterventionConnections
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Glaciated Landscapes and Change
Erratics and reconstructing former ice movement
- 3 things to know
- Paper 1
Overview
Recall questions on using erratics, crag and tail, drumlin orientation and till fabric to work out where the ice came from.
What you need to know
Answer each one before you reveal it.
In a crag and tail landform, which feature is located on the up-glacier side?
How can erratics be used to reconstruct former glacial conditions?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is an erratic?
Model answer
A rock transported by glacial ice and deposited in a location where it differs from the local bedrock, providing evidence of ice movement direction and provenance.
- 2
Why must an erratic be a distinctive rock type to be useful evidence of ice movement?
Model answer
Only a distinctive rock can be matched to one known outcrop, which is what allows the direction and distance of ice transport to be traced.
- 3
How can erratics be used to reconstruct former glacial activity?
Model answer
Erratics indicate provenance (source area) and transport direction because their rock type can be traced back to their origin, showing where ice came from and the path it travelled.
- 4
What information about former ice sheets can be determined from the positions of moraines?
Model answer
Moraine positions show the extent of former ice coverage, with terminal moraines marking maximum advance and recessional moraines indicating stages of retreat.
- 5
How does crag and tail orientation help reconstruct past glacial conditions?
Model answer
Crag and tail orientation shows ice flow direction, with the resistant crag on the upstream side and the tail of deposited material extending downstream in the direction of ice movement.
- 6
What does the alignment of drumlin long axes reveal about former glaciation?
Model answer
Drumlin long axes align parallel to the direction of ice movement, with the steeper stoss end facing upstream and the gentler lee slope pointing downstream.
Other ways to work this
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