2.2.2

Periglacial Landforms

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Ice Wedges and Patterned Ground

Periglacial environments, such as northern Canada and northern Russia, have a range of characteristic landforms, including ice wedges and patterned ground.

Ice wedges

Ice wedges

  • Ice-wedge polygons are generally 20–30 m across.
  • They are formed in areas of continuous permafrost by ground freezing in the winter and thawing in the summer.
  • When temperatures fall in winter, water in fissures in the active layer freezes and so expands, pushing the ground apart.
  • The wedge shape is maintained as water further down from the surface, over 3m down, remains frozen.
  • The annual repetition of this process causes the gradual formation of marked ice-wedges which develop in polygonal patterns.
Patterned ground

Patterned ground

  • Stone polygons are smaller than ice-wedge polygons, less than 10 m across and are the result of frost heave.
  • During the winter, soils freeze downwards from the surface, reaching and ‘grabbing’ individual stones, which are pulled upwards by the expansion vertically of the frozen soil above them.
  • The empty space left beneath is filled with loose unfrozen soil, so the stone is prevented from moving back when the soil below freezes.
Patterned ground cont.

Patterned ground cont.

  • Stones are also pushed towards the surface because of the pressure of small ice lenses growing beneath them.
  • Stones warm up more quickly so, in the summer, the ice in the soil beneath the stone melts, allowing wet sediment to slump to fill the space beneath it.
  • This prevents it from sinking back into its original position.
  • As the stones collect on the surface of the ground, the larger stones are pushed towards the edge of the pile by ground expansion. Gravity and smaller stones, sands and silt are left in the middle, resulting in a polygonal shape.

Pingos

Pingos are domed mounds of layered sediments with a core of ice and are usually up to 100 m in diameter. They can be as wide as 2 km.

Open pingos

Open pingos

  • Pingos can be open or closed.
  • Open pingos can be seen in the Canadian Arctic and Siberia and are more likely to be found in clusters.
  • Open pingos are formed in areas of discontinuous permafrost when groundwater from small areas of talik moves upwards because of an increase in hydraulic pressure as the active layer re-freezes in winter.
  • As the water freezes near the surface, it causes the ground surface to dome upwards, forming the characteristic shape of a pingo.
Closed pingos

Closed pingos

  • Closed pingos are less common and are found in Alaska and Greenland.
  • Closed pingos are formed in areas of continuous permafrost when water pushed down from frozen lake sediments accumulates at depth, freezes and then expands again, causing the ground surface to dome.
  • Some pingos have a small depression at their top, resulting from localised melting there.
Jump to other topics
1

Tectonic Processes & Hazards

1.1

Tectonic Processes & Hazards

1.1.1Tectonic Plates1.1.2Distribution of Tectonic Hazards1.1.3Theoretical Frameworks1.1.4Earthquakes1.1.5Earthquake Hazards1.1.6Volcanoes1.1.7Tsunamis1.1.8End of Topic Test - Tectonic Processes1.1.9Exam-Style Question - Earthquakes
1.2

Natural Disasters

1.2.1Introduction to Natural Disasters1.2.2Impacts of Hazards1.2.3Comparing Hazards1.2.4Development & Governance
1.3

Natural Disaster Case Studies

1.3.1Tohoku Earthquake & Tsunami1.3.2Gorkha Earthquake1.3.3Mount Merapi Eruption
1.4

Trends & Patterns

1.4.1Disaster Trends1.4.2Prediction
1.5

Disaster Modification

1.5.1Hazard Management1.5.2Modifications1.5.3End of Topic Test - Natural Disasters1.5.4Exam-Style Question - Disaster Modification
2

Option 2A: Glaciated Landscapes & Change

2.1

Glaciated Landscapes Over Time

2.1.1Timeline of Glacial Change2.1.2Natural Causes2.1.3Ice Distributions
2.2

Periglacial Landscapes

2.2.1Periglacial Processes2.2.2Periglacial Landforms
2.3

Glacial Processes

2.3.1Mass Balance2.3.2Glacial Movement
2.4

Glacial Landforms

2.4.1Landscapes2.4.2Erosional Landforms2.4.3Erosional Landforms 22.4.4Erosional Landforms 32.4.5Depositional Landforms2.4.6Fluvioglaciation
2.5

The Future of Glaciated Landscapes

2.5.1The Value of Glaciated Landscapes2.5.2The Value of Glaciated Landscapes 22.5.3Threats to Glaciated Landscapes2.5.4Managing the Threats to Glaciated Landscapes
3

Option 2B: Coastal Landscapes & Change

3.1

Coastal Landscapes

3.1.1The Wider Coastal Landscape3.1.2Geological Structure3.1.3Lithology & Vegetation
3.2

Coastal Erosion & Deposition

3.2.1Shaping Coastlines3.2.2Coastal Formations3.2.3Sediment Transportation3.2.4Subaerial Processes
3.3

Coastal Risks

3.3.1Sea Level Change3.3.2Coastal Retreat3.3.3Coastal Flooding
3.4

Managing Coastlines

3.4.1Consequences of Coastal Recession3.4.2Engineering Management Approaches3.4.3Governance Approaches
4

Globalisation

4.1

Globalisation

4.1.1Intro to Globalisation4.1.2Development of Globalisation4.1.3Economic Policy & Globalisation4.1.4Government Policy & Globalisation4.1.5International Organisations & Globalisation4.1.6Measuring Globalisation4.1.7TNCs & Globalisation4.1.8TNCs - Aramco & Anglo-Iranian Oil
4.2

Negatives of Globalisation

4.2.1'Switched Off' Places
4.3

Global Shift

4.3.1Global Shift for Developing Nations4.3.2Global Shift for Developing Nations 24.3.3Global Shift for Developed Nations4.3.4End of Topic Test - Globalisation
4.4

Migration

4.4.1Megacities4.4.2International Migration4.4.3Country Interdependence
4.5

Culture

4.5.1Global Culture4.5.2Cultural Erosion
4.6

Measuring Development

4.6.1Measuring Development
4.7

Responses to Globalisation

4.7.1Tensions Caused by Globalisation4.7.2Government Control of Globalisation4.7.3Ethical Responses to Globalisation4.7.4End of Topic Test - Migration, Culture, & Response
5

Option 4A: Regenerating Places

5.1

Types of Economies

5.1.1Economic Activity5.1.2Employment5.1.3Economic Activity - Health & Life5.1.4Economic Activity - Education & Inequality
5.2

Function of Places

5.2.1Characteristics of Places5.2.2Changes in Places5.2.3International Influences on Places5.2.4Historic Influences on Places5.2.5The Perception of Places5.2.6Lived Experience & Attachment
5.3

Regeneration

5.3.1Migration & Capital5.3.2Success & Regeneration5.3.3Tensions & Conflict in Communities5.3.4Regeneration in the UK5.3.5Local Government Policies5.3.6Regeneration Strategies5.3.7Measuring Regeneration Success
5.4

Regeneration Case Studies

5.4.1Stratford5.4.2Salford Quays5.4.3Croyde
6

Option 4B: Diverse Places

6.1

Population Structure

6.1.1The UK6.1.2Population Characteristics6.1.3Government & Change
6.2

Past & Present Connections

6.2.1International Influence on Places6.2.2Historic Influences on Places6.2.3The Perception of Places6.2.4Image & Identity
6.3

Urban & Rural Spaces

6.3.1Perceptions of Urban Places6.3.2Perceptions of Rural Places6.3.3Evaluating Living Space
6.4

Diversity

6.4.1UK Migrations6.4.2Challenges6.4.3Tensions & Conflict6.4.4Wider Outcomes of Tensions6.4.5Managing Tensions
6.5

Urban & Rural Case Studies

6.5.1Stakeholders
6.6

Case Study - Tower Hamlets

6.6.1Background6.6.2Characteristics6.6.3Issues
6.7

Case Study - Sturton-le-Steeple

6.7.1Background6.7.2Characteristics6.7.3Issues
7

The Water Cycle & Water Insecurity (A2 only)

7.1

Hydrological Processes Global to Local

7.1.1Global Hydrological Cycle7.1.2Drainage Basin Hydrological Cycle7.1.3Water Budgets7.1.4River Regimes7.1.5Storm Hydrographs
7.2

Influences on the Water Cycle

7.2.1Causes of Drought7.2.2Impacts of Drought7.2.3Causes of Flooding7.2.4Impacts of Flooding7.2.5Climate Change & The Water Cycle7.2.6Impacts of Climate Change7.2.7End of Topic Test - The Water Cycle
7.3

Water Insecurity

7.3.1Water Stress7.3.2Causes of Water Insecurity7.3.3Water Insecurity Risk7.3.4Conflict Over Water
7.4

Water Supply Management

7.4.1Hard Engineering Schemes7.4.2Sustainable Management7.4.3Water Treaties & Framework7.4.4End of Topic Test - Water Insecurity & Management
8

The Carbon Cycle & Energy Security (A2 only)

8.1

The Carbon Cycle

8.1.1Carbon Stores8.1.2Carbon Stores 28.1.3Biological Carbon8.1.4Atmospheric Carbon8.1.5Burning Fossil Fuels
8.2

Energy Consumption

8.2.1Consumption8.2.2Access to Energy8.2.3Energy Players8.2.4Supply & Demand8.2.5Pathways8.2.6End of Topic Test - Carbon & Consumption
8.3

Alternative Energy

8.3.1Unconventional Fuels8.3.2Non-Fossil Fuels8.3.3Non-Fossil Fuels 2
8.4

Growing Demand for Resources

8.4.1Deforestation8.4.2Water8.4.3Climate Change
8.5

The Future

8.5.1Future Uncertainty8.5.2Adaptation Strategies8.5.3Mitigation Strategies
9

Superpowers (A2 only)

9.1

Superpowers

9.1.1Introduction to Superpowers9.1.2Superpowers - Economic Power & Size9.1.3Superpowers - Political & Military Power9.1.4Superpowers - Culture, Demography & Resources9.1.5Geo-Strategic Location
9.2

Hard & Soft Power

9.2.1Hard & Soft Power9.2.2Emerging Powers - China Rivalry9.2.3Emerging Powers - Chinese Sources of Power9.2.4Emerging Powers - Brazil9.2.5Emerging Powers - Russia9.2.6Emerging Powers - India9.2.7Theories of Development9.2.8Power Case Studies: Chinese One Belt One Road9.2.9Power Case Studies: Pakistan Nuclear Arms9.2.10Power Case Studies: OPEC
9.3

IGOs, TNCs & Alliances

9.3.1Superpowers & IGOs9.3.2Superpowers & TNCs9.3.3Superpowers & Global Action9.3.4Superpowers & Alliances9.3.5Superpowers & the Environment
9.4

Changing Global Influence

9.4.1Recent Tensions between Powers9.4.2China in Africa & Asia9.4.3Tensions in the Middle East9.4.4Economic Problems for Superpowers9.4.5Future Pattern of Power
10

Option 8A: Health & Human Rights (A2 only)

10.1

Human Development

10.1.1Measuring Development10.1.2Factors Improving Development10.1.3Variations in Health
10.2

Role of Governments & IGOs

10.2.1Targets & Attitudes10.2.2Financial IGOs10.2.3The United Nations (UN)10.2.4The UN's MDGs & SDGs
10.3

Human Rights

10.3.1Human Rights10.3.2Differences Between Countries10.3.3Transitions to Democracy10.3.4Differences Within Countries10.3.5The Demand for Equality
10.4

Interventions

10.4.1Geopolitical Interventions10.4.2International Intervention Players10.4.3Evaluating Geopolitical Intervention10.4.4Military Interventions10.4.5Evaluating Military Interventions
10.5

Development Aid

10.5.1Forms10.5.2Successes10.5.3Criticisms10.5.4Development Aid & the Environment10.5.5Evaluating Development Aid10.5.6Economic Inequalities
11

Option 8B: Migration & Identity (A2 only)

11.1

Globalisation & Migration

11.1.1Intro to Migration11.1.2Trends in Migration11.1.3Common Migration Patterns11.1.4Causes of Migration11.1.5Restrictions on Migration
11.2

Consequences of Migration

11.2.1Intro to Culture11.2.2Social & Demographic Tensions of Migration11.2.3Political & Economic Tensions of Migration
11.3

Nation States

11.3.1Intro to Nation States11.3.2Borders11.3.3Nationalism
11.4

Responses to Global Migration

11.4.1Responses to Global Migration11.4.2Global Organisations11.4.3IGOs and World Trade11.4.4Financial IGOs11.4.5Environmental IGOs
11.5

Sovereignty & Identity

11.5.1Sovereignty & Nationalism11.5.2Complex Identities11.5.3Challenges to National Identities11.5.4Tensions within Nations11.5.5Failed States

Practice questions on Periglacial Landforms

Can you answer these? Test yourself with free interactive practice on Seneca — used by over 10 million students.

  1. 1
    How wide are ice-wedge polygons usually?Multiple choice
  2. 2
    Patterned Ground FormationPut in order
  3. 3
    In what type of permafrost would you find an open pingo?Multiple choice
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Periglacial Processes

Mass Balance