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
- 17 subtopics
- 45 things to know
- Component 01
What Glaciated Landscapes covers
Glaciated Landscapes is examined in Component 01, Physical systems. It covers the glacier as a system of inputs, stores, flows and outputs; mass balance and the equilibrium line; how climate, latitude, altitude, geology, relief and aspect control glaciation; how snow becomes glacier ice in valley glaciers and ice sheets; warm-based and cold-based ice and how glaciers move; and weathering, nivation, glacial erosion and the entrainment, transport and deposition of sediment. It also covers the landforms of glaciated uplands and lowlands, from corries, arêtes, troughs and ribbon lakes to moraines, drumlins and till sheets, with Helvellyn and the Laurentide Ice Sheet as examples; kames, eskers and outwash plains left by deglaciation; permafrost, patterned ground and pingos; and how resource extraction, thermokarst, dams, reservoirs and tourism change periglacial and glaciated landscapes.
The 17 subtopics
Each one has its own page.
- The glacier system: inputs, stores, flows and outputsRecall questions on the glaciated landscape as an open system: its inputs of matter and energy, stores, flows and outputs, dynamic equilibrium, negative and positive feedback, albedo, and the glacial sediment budget with a worked storage calculation.Open →
- Glacier mass balance and the equilibrium lineRecall questions on glacier mass balance, accumulation, ablation and sublimation, the accumulation zone and equilibrium line, the seasonal balance of an Alpine glacier, water equivalent and net balance calculations, the accumulation area ratio, and why a snout advances or retreats only after a lag.Open →
- Climate, latitude and altitude as controls on glaciationRecall questions on how precipitation, maritime and continental climates, latitude and altitude control glaciation, the dry interior of Antarctica, the environmental lapse rate with a worked calculation, the snow line on Kilimanjaro and in Norway, and why glaciers reach sea level in Greenland.Open →
- Geology, relief and aspect in glaciated landscapesRecall questions on lithology and geological structure in glaciated landscapes, how jointing and weak or resistant rock bands shape erosion and troughs, the Skiddaw Slates and Borrowdale Volcanic rocks of the Lake District, and how relief and aspect decide where ice forms and why corries face north-east.Open →
- Firn, glacier ice, valley glaciers and ice sheetsRecall questions on how snow becomes firn and then glacier ice, the densities involved, why glacier ice looks blue, the role of meltwater, and valley glaciers, ice caps, piedmont glaciers and the Antarctic and Greenland ice sheets.Open →
- Warm-based and cold-based ice, and the mechanisms of glacier movementRecall questions on warm-based and cold-based glaciers and the pressure melting point, basal sliding, regelation, enhanced basal creep and internal deformation, the velocity profile of a valley glacier, extending and compressing flow, crevasses, glacier surges and the effect of summer meltwater.Open →
- Weathering, mass movement and nivation in cold environmentsRecall questions on frost shattering and freeze-thaw, blockfields, pressure release and chemical weathering in cold environments, scree slopes, rockfall after glacier retreat, solifluction and avalanches, and how nivation deepens a hollow into the first stage of a corrie.Open →
- Glacial erosion and the marks it leaves on rockRecall questions on abrasion and plucking, rock flour and striations, reading ice direction from roches moutonnées, crag and tail, whalebacks, knock and lochan topography, erosion by subglacial meltwater, and why thicker ice erodes faster.Open →
- Entrainment, transport and deposition of glacial sedimentRecall questions on how glaciers entrain debris, supraglacial, englacial and subglacial debris, passive transport, lodgement and ablation till, telling till from glacio-fluvial deposits, summer sediment output, and fieldwork using till fabric analysis, clast roundness and the Mann-Whitney U test.Open →
- Corries, arêtes and pyramidal peaksRecall questions on the shape and formation of corries, rotational slip, bergschrunds, rock lips and tarns such as Red Tarn on Helvellyn, arêtes such as Striding Edge, pyramidal peaks such as the Matterhorn, cols, and mapping corrie orientation with a chi-squared test.Open →
- Glacial troughs, hanging valleys and ribbon lakesRecall questions on the U-shaped cross profile of a glacial trough, truncated spurs, hanging valleys and waterfalls, misfit streams, ribbon lakes and rock basins such as Wastwater, trough ends, rock steps, and fjords such as the Sognefjord.Open →
- Moraines, erratics, drumlins and till sheetsRecall questions on lateral, medial, terminal, recessional, push and ground moraines, erratics such as the Norber erratics and the Ailsa Craig microgranite, the shape, size and formation of drumlins and basket of eggs topography, and till sheets.Open →
- Characteristic glaciated landscapes and how they change over timeRecall questions on the landform assemblages of glaciated uplands and ice-sheet lowlands, the Helvellyn area of the Lake District, the Laurentide Ice Sheet with the Canadian Shield, Long Island and the Finger Lakes, change over seconds, seasons and millennia, varves, and Britain's relict glaciated landscape.Open →
- Glacio-fluvial landforms of deglaciation: kames, eskers and outwash plainsRecall 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.Open →
- Permafrost, patterned ground and pingosRecall questions on periglacial environments, continuous, discontinuous and sporadic permafrost, the active layer, frost heave and patterned ground, ice wedges, open-system and closed-system pingos in the Mackenzie Delta, relict periglacial features in Britain, and the effects of present-day warming.Open →
- People in periglacial landscapes: resource extraction and thermokarstRecall questions on resource extraction in periglacial regions, Prudhoe Bay and the Trans-Alaska Pipeline, building on permafrost in Yakutsk, gravel pads and ice roads, how disturbance causes thermokarst, thaw lakes and drunken forests, the Batagaika crater, and the carbon released by thawing permafrost.Open →
- People in glaciated landscapes: dams, reservoirs and valley changeRecall questions on hydro-electric schemes in glacial troughs, the Grande Dixence dam in Switzerland, reservoir sedimentation, scour and bed armouring below dams, altered discharge regimes, and how ski pistes, snow-making, glacier retreat and tourist access around the Mer de Glace change mountain landscapes.Open →
What you need to know
Answer each one before you reveal it.
Explain why a very cold polar desert may hold only small glaciers.
Why do vehicle tracks across tundra persist for decades?
Why does thawing permafrost matter far beyond the local landscape?
Describe the seasonal pattern of mass balance for an Alpine glacier through one year.
Define lithology as a control on glaciated landscapes
What is firn?
Name two sources of heat that can bring the base of a thick glacier to its pressure melting point.
What is frost shattering?
Name three conditions needed for effective abrasion.
How does a glacier pick up debris from its bed?
Give the Welsh and French terms for a corrie.
Why does a glacier produce a U-shaped valley where a river produces a V-shaped one?
How can a series of recessional moraines be used to reconstruct a glacier's history?
Which landforms would you expect to find together in an upland shaped by valley glaciers?
Describe the climate change that ended the last glacial period in Britain.
Define permafrost.
Name the tallest gravity dam in the world and the country in which it stands.
Name the three main inputs of matter into a glaciated landscape system.
Why is mass balance measured in metres of water equivalent rather than metres of snow?
How does the annual precipitation total affect the size of a glacier?
What is meant by geological structure in a glaciated landscape?
Outline the stages by which fresh snow becomes glacier ice.
Why is a cold-based glacier associated with very little erosion?
What conditions make freeze-thaw weathering most effective?
What is plucking?
What is till?
Name a corrie tarn on Helvellyn in the Lake District.
How is a hanging valley formed?
Name a British site where erratics rest on limestone pedestals.
Which landforms characterise a lowland shaped by an ice sheet?
How did post-glacial warming change the dominant geomorphic process in a deglaciating landscape?
Distinguish continuous permafrost from discontinuous permafrost.
How is water gathered for the Grande Dixence scheme?
Which two sources supply the energy that drives a glaciated landscape system?
Explain why there is a lag between a negative mass balance and a visible retreat of the snout.
Roughly how much precipitation falls each year in the interior of Antarctica?
Explain how well-jointed rock increases the rate of glacial erosion.
Why does dense glacier ice appear blue?
Compare typical rates of movement of warm-based and cold-based glaciers.
What is pressure release weathering?
Why is plucking most effective on well-jointed rock?
State two ways of telling till from glacio-fluvial deposits in the field.
What is the typical ratio of a corrie's length to its height?
What is commonly found where a hanging valley meets a main trough?
Take Glaciated Landscapes further
The same content, four other ways.
Commonly confused
Pairs that lose marks when they are blurred together.
Accumulation vs Ablation
Accumulation: mass is added to a glacier, chiefly as snowfall but also by avalanche and by hoar frost. Ablation: mass is lost from a glacier by surface thaw, sublimation, evaporation and the calving of icebergs.
Till vs Glacio-fluvial deposits
Till: material dumped directly by the ice, so it is unsorted, unstratified and angular. Glacio-fluvial deposits: material laid down by meltwater, so it is sorted by size, arranged in layers and rounded by transport.
Lateral moraine vs Kame terrace
Lateral moraine: a ridge of unsorted angular debris built along the side of a valley from rock that fell onto the edge of the ice. Kame terrace: a bench of sorted sand and gravel along a valley side, left by a stream that ran between the ice and the valley wall.
Questions from this topic
Each one with the model answer underneath.
- 1
What does it mean to describe a glaciated landscape as an open system?
Model answer
Both energy and matter can cross its boundaries, so the landscape exchanges material and energy with the environment around it.
- 2
Name the three main inputs of matter into a glaciated landscape system.
Model answer
Snow and ice, rock debris from weathering and mass movement, and liquid water from rainfall and melt.
- 3
Which two sources supply the energy that drives a glaciated landscape system?
Model answer
Solar radiation, which drives melting and evaporation, and gravitational potential energy, which drives the movement of ice, water and debris downslope.
- 4
State two outputs from a glaciated landscape system.
Model answer
Meltwater and water vapour leaving the system, and sediment carried out beyond the ice margin by meltwater streams or icebergs.
- 5
What is a store in a glaciated landscape system?
Model answer
A place where matter or energy is held for a period of time, such as the glacier ice itself, a snowfield, a moraine or a proglacial lake.
- 6
Explain the difference between a store and a flow in a glacial system.
Model answer
A store holds material in one place, while a flow is the transfer of material or energy from one store to another.
What is inside Levo
Six ways to work the same material.
Glaciated Landscapes revision questions
- What does Glaciated Landscapes cover in OCR A-Level Geography?
- 17 subtopics: the glacier system: inputs, stores, flows and outputs, glacier mass balance and the equilibrium line, climate, latitude and altitude as controls on glaciation, geology, relief and aspect in glaciated landscapes, firn, glacier ice, valley glaciers and ice sheets, warm-based and cold-based ice, and the mechanisms of glacier movement, weathering, mass movement and nivation in cold environments, glacial erosion and the marks it leaves on rock, entrainment, transport and deposition of glacial sediment, corries, arêtes and pyramidal peaks, glacial troughs, hanging valleys and ribbon lakes, moraines, erratics, drumlins and till sheets, characteristic glaciated landscapes and how they change over time, glacio-fluvial landforms of deglaciation: kames, eskers and outwash plains, permafrost, patterned ground and pingos, people in periglacial landscapes: resource extraction and thermokarst and people in glaciated landscapes: dams, reservoirs and valley change. Each one has its own page with questions and model answers.
- How is Glaciated Landscapes organised?
- By the OCR H481 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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