OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Glaciated Landscapes
Glacio-fluvial landforms of deglaciation: kames, eskers and outwash plains
- 2 things to know
- Component 01
Overview
Recall questions on glacio-fluvial processes and deposits after the last glacial period, eskers, kames and kame terraces, outwash plains such as Skeiðarársandur in Iceland, jökulhlaups, kettle holes, and how these landforms are changing today.
What you need to know
Answer each one before you reveal it.
How did post-glacial warming change the dominant geomorphic process in a deglaciating landscape?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What does the term glacio-fluvial mean?
Model answer
It describes material deposited or landforms shaped by meltwater flowing from a glacier, rather than by the ice itself.
- 2
Describe the climate change that ended the last glacial period in Britain.
Model answer
Temperatures rose sharply from about 11,700 years ago, ending the last cold snap and causing the rapid melting of the remaining ice.
- 3
How did post-glacial warming change the dominant geomorphic process in a deglaciating landscape?
Model answer
Direct glacial erosion and deposition gave way to enormous volumes of meltwater, so sorting, fluvial transport and glacio-fluvial deposition took over.
- 4
How can glacio-fluvial deposits be recognised in the field?
Model answer
They are sorted by size into distinct layers and their stones have been rounded by water transport.
- 5
What is an esker?
Model answer
It is a long, winding ridge of sorted sand and gravel deposited by a stream flowing in a tunnel beneath or within the ice.
- 6
Why can an esker run uphill across the landscape?
Model answer
The meltwater in the tunnel was under hydrostatic pressure from the weight of ice above it, so it could be forced up gradients.
Other ways to work this
The same content, four other ways.
What is inside Levo
Six ways to work the same material.
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