Eduqas A-Level Geography A110QS
Coastal LandscapesLandscape
Glaciated LandscapesLandscape
Changing Places
Water and Carbon Cycles
Global Migration
Global Governance of the Oceans
Tectonic Hazards
EcosystemsContemporary theme
Economic Growth and Challenge: IndiaContemporary theme
Economic Growth and Challenge: ChinaContemporary theme
Development in an African ContextContemporary theme
Energy Challenges and DilemmasContemporary theme
Weather and ClimateContemporary theme
Geographical Skills
Glaciated Landscapes
Proglacial landforms: sandurs, varves and kettle holes
- 2 things to know
- Component 1 Section A
Overview
How a sandur is built, world's largest sandur and give its size and why a varve has two contrasting layers.
What you need to know
Answer each one before you reveal it.
Explain how a sandur is built.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define a sandur.
Model answer
A sandur, or outwash plain, is a broad, flat spread of sand and gravel beyond a glacier snout. Meltwater streams deposit the material as they leave the ice.
- 2
Explain how a sandur is built.
Model answer
Meltwater leaving the snout loses velocity as it spreads out across open ground. The coarsest gravel is dropped nearest the ice and progressively finer sand and silt further away.
- 3
Why is a sandur crossed by braided channels?
Model answer
Meltwater discharge varies enormously between seasons and the load is very large. Shallow channels choke with sediment and divide repeatedly around temporary bars.
- 4
Name the world's largest sandur and give its size.
Model answer
Skeiðarársandur in southern Iceland covers roughly 1,300 km². Meltwater from Vatnajökull built and maintains it.
- 5
What is a jökulhlaup?
Model answer
A jökulhlaup is a sudden, catastrophic outburst of meltwater from beneath or in front of a glacier. Volcanic activity under an ice cap is a common trigger in Iceland.
- 6
Describe the 1996 Icelandic jökulhlaup and its effects.
Model answer
An eruption beneath Vatnajökull melted ice into the Grímsvötn caldera, which burst out in November 1996. Peak discharge reached roughly 50,000 m³ s⁻¹ and the flood destroyed bridges on the ring road across Skeiðarársandur.
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