AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Glacial Systems and Landscapes
Moraines, Till and Fluvioglacial Landforms
- 3 things to know
- Component 1
Overview
Recall questions on lateral, medial, terminal, recessional and ground moraines, till plains and till, and on meltwater channels, kames, kame terraces, eskers and outwash plains, and how fluvioglacial deposits differ from till.
What you need to know
Answer each one before you reveal it.
Name three types of meltwater channel based on their position relative to the ice.
Where does the meltwater that forms an esker flow?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Where does a lateral moraine form?
Model answer
At the margins (sides) of a valley glacier, from debris falling from valley walls and material pushed aside by the ice.
- 2
How does a medial moraine originate?
Model answer
When two glaciers merge, their adjacent lateral moraines combine to form a single ridge of debris running down the centre of the enlarged glacier.
- 3
What does a terminal moraine indicate about former ice extent?
Model answer
It marks the maximum advance of the glacier, where debris accumulated at the ice front.
- 4
Distinguish a recessional moraine from a terminal moraine.
Model answer
A recessional moraine forms during pauses in glacial retreat, whereas a terminal moraine marks the furthest advance of the ice.
- 5
Where is ground moraine deposited?
Model answer
Beneath the glacier, spread across the valley floor as the ice melts.
- 6
Define a till plain.
Model answer
An extensive flat area of ground moraine deposited as a sheet of unsorted glacial sediment beneath or at the margin of an ice sheet.
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