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
- 20 subtopics
- 45 things to know
- Component 1 Section A
- Component 1 Section A, one landscape of two
What Glaciated Landscapes covers
Glaciated Landscapes is examined in Component 1 Section A, if glaciated is the landscape you sit. It covers the glacier as a system: inputs, outputs, stores and transfers, the glacial budget, mass balance and feedback, the Quaternary Ice Age and the Little Ice Age, cold-based and warm-based glaciers, glacier ice movement and types of flow, types of ice mass and their distribution, freeze-thaw weathering and glacial erosion processes, factors affecting the rate of glacial erosion, cirques, arêtes and pyramidal peaks, glacial troughs, ribbon lakes, hanging valleys and truncated spurs, roches moutonnées, crag and tail and striations, glacial and fluvioglacial transport, till and types of moraine, drumlins and lowland glacial deposition, ice-contact fluvioglacial landforms, proglacial landforms: sandurs, varves and kettle holes, glacial landscape suites and change over time, periglacial ground ice and permafrost features, periglacial weathering, mass movement, water and wind and glacial landscapes and human activity.
Where it is assessed
Component 1 Section A
Changing Landscapes, one of two.
Check the Eduqas specification ↗The 20 subtopics
Each one has its own page.
- The glacier as a system: inputs, outputs, stores and transfersMain inputs of mass to a glacier, energy inputs to a glacial system and main outputs from a glacier.Open →
- The glacial budget, mass balance and feedbackGlacial budget, net mass balance and equilibrium line.Open →
- The Quaternary Ice Age and the Little Ice AgeGlacial period, loch Lomond Stadial and how eccentricity affects the glacial cycle.Open →
- Cold-based and warm-based glaciersCold-based glacier, warm-based glacier and pressure melting point.Open →
- Glacier ice movement and types of flowInternal deformation, intergranular slip and laminar flow within a glacier.Open →
- Types of ice mass and their distributionCirque glacier, valley glacier and highland icefield.Open →
- Freeze-thaw weathering and glacial erosion processesHow freeze-thaw weathering breaks up rock, glacial abrasion and rock flour.Open →
- Factors affecting the rate of glacial erosionHow ice thickness influences erosion and why altitude and aspect influence how much erosion occurs.Open →
- Cirques, arêtes and pyramidal peaksProcess of nivation, formation of a cirque from start to finish and typical dimensions of a cirque.Open →
- Glacial troughs, ribbon lakes, hanging valleys and truncated spursGlacial trough, truncated spur and hanging valley.Open →
- Roches moutonnées, crag and tail and striationsRoche moutonnée and crag and tail.Open →
- Glacial and fluvioglacial transportSupraglacial transport, englacial transport and subglacial transport.Open →
- Till and types of moraineLodgement till, ablation till and deformation till.Open →
- Drumlins and lowland glacial depositionShape of a drumlin in relation to ice flow, typical elongation ratio of a drumlin and drumlin swarm.Open →
- Ice-contact fluvioglacial landformsHow an esker forms, how a delta kame forms and how a kame terrace forms.Open →
- Proglacial landforms: sandurs, varves and kettle holesHow a sandur is built, world's largest sandur and give its size and why a varve has two contrasting layers.Open →
- Glacial landscape suites and change over timeSuite of landforms typical of a highland glaciated landscape, suite of landforms typical of a lowland glaciated landscape and knock and lochan topography.Open →
- Periglacial ground ice and permafrost featuresActive layer, periglacial environment and ice lens.Open →
- Periglacial weathering, mass movement, water and windNivation hollow, process of nivation in stages and scree slope and how one forms.Open →
- Glacial landscapes and human activityGlacial lake outburst flood, named GLOF and its consequences and GLOF outside the Himalayas.Open →
What you need to know
Answer each one before you reveal it.
Describe the formation of a cirque from start to finish.
Why is a glacier described as an open system?
Define the glacial budget.
When did the Quaternary Ice Age begin?
Define a cold-based glacier.
Define internal deformation.
Define a cirque glacier.
Why does the basal thermal regime control the rate of erosion?
Define a glacial trough.
Define a roche moutonnée.
Define supraglacial transport.
Define till.
Define a drumlin.
Define an esker.
Define a sandur.
Describe the suite of landforms typical of a highland glaciated landscape.
Define permafrost.
Why is frost weathering so effective in a periglacial climate?
Define a glacial lake outburst flood.
Name the main inputs of mass to a glacier.
What is meant by net mass balance?
Define a glacial period.
Define a warm-based glacier.
What is intergranular slip?
Describe a valley glacier.
Explain how freeze-thaw weathering breaks up rock.
How does ice velocity affect erosion?
Define a cirque.
Explain how a glacial trough is formed.
Which side of a roche moutonnée is the stoss side?
Define englacial transport.
What is lodgement till?
Describe the shape of a drumlin in relation to ice flow.
Explain how an esker forms.
Explain how a sandur is built.
Describe the suite of landforms typical of a lowland glaciated landscape.
Distinguish continuous, discontinuous and sporadic permafrost.
Define a nivation hollow.
Why has the risk of GLOFs risen in the Himalayas?
What are the energy inputs to a glacial system?
Where on a glacier is the accumulation zone?
Define an interglacial.
What is the pressure melting point?
Explain laminar flow within a glacier.
Take Glaciated Landscapes further
The same content, four other ways.
Commonly confused
Pairs that lose marks when they are blurred together.
Abrasion vs Plucking
Abrasion: scouring the bedrock with debris held in the ice. Plucking: tearing whole jointed blocks away after refreezing.
Questions from this topic
Each one with the model answer underneath.
- 1
Why is a glacier described as an open system?
Model answer
A glacier exchanges both energy and matter with its surroundings. Snow and rock debris enter it and meltwater and sediment leave it.
- 2
Name the main inputs of mass to a glacier.
Model answer
Direct snowfall is the largest input to most glaciers. Avalanches from valley sides, wind-blown snow and rockfall debris add further material.
- 3
What are the energy inputs to a glacial system?
Model answer
Solar radiation, geothermal heat from the bedrock and the potential energy of ice held at altitude are the energy inputs. Friction at the bed converts some of that potential energy into heat.
- 4
List the main outputs from a glacier.
Model answer
Meltwater, calved icebergs, water vapour lost by sublimation and deposited sediment are the outputs. All are grouped together as ablation.
- 5
Define ablation.
Model answer
Ablation is the total loss of mass from a glacier by any process. The processes involved are melting, sublimation, calving and wind erosion of snow.
- 6
Define accumulation.
Model answer
Accumulation is the total gain of mass by a glacier. Snowfall, avalanche and wind-blown snow are the main contributors.
What is inside Levo
Six ways to work the same material.
Glaciated Landscapes revision questions
- What does Glaciated Landscapes cover in Eduqas A-Level Geography?
- 20 subtopics: the glacier as a system: inputs, outputs, stores and transfers, the glacial budget, mass balance and feedback, the quaternary ice age and the little ice age, cold-based and warm-based glaciers, glacier ice movement and types of flow, types of ice mass and their distribution, freeze-thaw weathering and glacial erosion processes, factors affecting the rate of glacial erosion, cirques, arêtes and pyramidal peaks, glacial troughs, ribbon lakes, hanging valleys and truncated spurs, roches moutonnées, crag and tail and striations, glacial and fluvioglacial transport, till and types of moraine, drumlins and lowland glacial deposition, ice-contact fluvioglacial landforms, proglacial landforms: sandurs, varves and kettle holes, glacial landscape suites and change over time, periglacial ground ice and permafrost features, periglacial weathering, mass movement, water and wind and glacial landscapes and human activity. Each one has its own page with questions and model answers.
- How is Glaciated Landscapes organised?
- By the Eduqas A110QS specification, subtopic by subtopic, so it matches the order you are taught it in.
Every question in Glaciated Landscapes, on a schedule.
Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.
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