Geological Structure

Concordant vs Discordant Coastlines

The shape of a coastline is continually changing due to the surrounding geology which contributes to its morphology. Coasts are either concordant or discordant.

Concordant coastlines

Concordant coastlines have alternating bands of hard and soft rock parallel to the coast.

Discordant coastlines

Discordant coastlines have alternating bands of hard and soft rock at 90^o to the coast.
- Erosional landforms are more common on discordant coastlines because erosion happens at different rates along their length.

Example of a discordant coast

In Dorset, the coastline consists of Portland limestone and Greensands.
- The Greensands is less resistant to erosional processes, and so retreats at a faster rate than the Portland limestone.
  - This has resulted in the creation of a bay and headlands.

Coastal Morphology

The shape of a coastline is continually changing because of the surrounding geology, which contributes to its morphology.

Pacific coasts

Concordant coastlines, also referred to as Pacific coasts, lead to the formation of Dalmatian coasts.
Dalmatian coasts are made up of offshore islands and coastal inlets running parallel to the coastline.
- E.g. Lulworth Cove, located on the south-west Dorset coastline. Here, the more-resistant rock (e.g. limestone) acts as a barrier to protect the less-resistant rock.

Atlantic coasts

Headlands and bays often form on discordant coastlines (also referred to as Atlantic coasts).
- As the faster eroding, less-resistant rock retreats (e.g. the clays at Swanage Bay), this leaves behind the more-resistant rock as headlands.

Bays and headlands

On discordant coastlines, the retreating, less resistant rock and the exposed resistant rocks cause a change in the shape of the coastline. This leads to wave refraction.
This change in the way in which waves approach the coastline can cause an increase in the rate of erosion on the headlands.
This leads to the formation of headland features like caves, arches, stacks and stumps.

Geological Structure

The shape of a coastline is continually changing because of the surrounding geology, which contributes to its morphology.

Joints and faults

The geological structure of rocks (the formation of joints, the angle of the dip, faulting and folding) is caused by the deformation and stress placed on them from tectonic processes.
Rocks with the presence of more joints and faults, like sedimentary rocks, are more susceptible to the processes of erosion and weathering. This is because these processes exert forces on the weaknesses found in the layers of the rocks.

Illustrative background for Dip ?? "content

Dip

The angle the rock layer forms with the horizontal bedding plane is referred to as the dip. Rocks can dip either towards land or towards the sea.
Bedding planes that dip towards the sea create a gentler cliff profile. But these cliffs are vulnerable to mass movement processes, like rockfalls.
Bedding planes that dip towards land tend to create a steeper cliff profile. But these cliffs are more vulnerable to erosion processes, like hydraulic action and abrasion.

1Tectonic Processes & Hazards

1.1Tectonic Processes & Hazards

1.1.1Tectonic Plates

1.1.2Distribution of Tectonic Hazards

1.1.3Theoretical Frameworks

1.1.4Earthquakes

1.1.5Earthquake Hazards

1.1.6Volcanoes

1.1.7Tsunamis

1.1.8End of Topic Test - Tectonic Processes

1.1.9Exam-Style Question - Earthquakes

1.2Natural Disasters

1.2.1Introduction to Natural Disasters

1.2.2Impacts of Hazards

1.2.3Comparing Hazards

1.2.4Development & Governance

1.3Natural Disaster Case Studies

1.3.1Tohoku Earthquake & Tsunami

1.3.2Gorkha Earthquake

1.3.3Mount Merapi Eruption

1.4Trends & Patterns

1.4.1Disaster Trends

1.4.2Prediction

1.5Disaster Modification

1.5.1Hazard Management

1.5.2Modifications

1.5.3End of Topic Test - Natural Disasters

1.5.4Exam-Style Question - Disaster Modification

2Option 2A: Glaciated Landscapes & Change

2.1Glaciated Landscapes Over Time

2.1.1Timeline of Glacial Change

2.1.2Natural Causes

2.1.3Ice Distributions

2.2Periglacial Landscapes

2.2.1Periglacial Processes

2.2.2Periglacial Landforms

2.3Glacial Processes

2.3.1Mass Balance

2.3.2Glacial Movement

2.4Glacial Landforms

2.4.1Landscapes

2.4.2Erosional Landforms

2.4.3Erosional Landforms 2

2.4.4Erosional Landforms 3

2.4.5Depositional Landforms

2.4.6Fluvioglaciation

2.5The Future of Glaciated Landscapes

2.5.1The Value of Glaciated Landscapes

2.5.2The Value of Glaciated Landscapes 2

2.5.3Threats to Glaciated Landscapes

2.5.4Managing the Threats to Glaciated Landscapes

3Option 2B: Coastal Landscapes & Change

3.1Coastal Landscapes

3.1.1The Wider Coastal Landscape

3.1.2Geological Structure

3.1.3Lithology & Vegetation

3.2Coastal Erosion & Deposition

3.2.1Shaping Coastlines

3.2.2Coastal Formations

3.2.3Sediment Transportation

3.2.4Subaerial Processes

3.3Coastal Risks

3.3.1Sea Level Change

3.3.2Coastal Retreat

3.3.3Coastal Flooding

3.4Managing Coastlines

3.4.1Consequences of Coastal Recession

3.4.2Engineering Management Approaches

3.4.3Governance Approaches

4Globalisation

4.1Globalisation

4.1.1Intro to Globalisation

4.1.2Development of Globalisation

4.1.3Economic Policy & Globalisation

4.1.4Government Policy & Globalisation

4.1.5International Organisations & Globalisation

4.1.6Measuring Globalisation

4.1.7TNCs & Globalisation

4.1.8TNCs - Aramco & Anglo-Iranian Oil

4.2Negatives of Globalisation

4.2.1'Switched Off' Places

4.3Global Shift

4.3.1Global Shift for Developing Nations

4.3.2Global Shift for Developing Nations 2

4.3.3Global Shift for Developed Nations

4.3.4End of Topic Test - Globalisation

4.4Migration

4.4.1Megacities

4.4.2International Migration

4.4.3Country Interdependence

4.5Culture

4.5.1Global Culture

4.5.2Cultural Erosion

4.6Measuring Development

4.6.1Measuring Development

4.7Responses to Globalisation

4.7.1Tensions Caused by Globalisation

4.7.2Government Control of Globalisation

4.7.3Ethical Responses to Globalisation

4.7.4End of Topic Test - Migration, Culture, & Response

5Option 4A: Regenerating Places

6Option 4B: Diverse Places

6.1Population Structure

6.1.1The UK

6.1.2Population Characteristics

6.1.3Government & Change

6.2Past & Present Connections

6.2.1International Influence on Places

6.2.2Historic Influences on Places

6.2.3The Perception of Places

6.2.4Image & Identity

6.3Urban & Rural Spaces

6.3.1Perceptions of Urban Places

6.3.2Perceptions of Rural Places

6.3.3Evaluating Living Space

6.4Diversity

6.4.1UK Migrations

6.4.2Challenges

6.4.3Tensions & Conflict

6.4.4Wider Outcomes of Tensions

6.4.5Managing Tensions

6.5Urban & Rural Case Studies

6.5.1Stakeholders

6.6Case Study - Tower Hamlets

6.6.1Background

6.6.2Characteristics

6.6.3Issues

6.7Case Study - Sturton-le-Steeple

6.7.1Background

6.7.2Characteristics

6.7.3Issues

7The Water Cycle & Water Insecurity (A2 only)

7.1Hydrological Processes Global to Local

7.1.1Global Hydrological Cycle

7.1.2Drainage Basin Hydrological Cycle

7.1.3Water Budgets

7.1.4River Regimes

7.1.5Storm Hydrographs

7.2Influences on the Water Cycle

7.2.1Causes of Drought

7.2.2Impacts of Drought

7.2.3Causes of Flooding

7.2.4Impacts of Flooding

7.2.5Climate Change & The Water Cycle

7.2.6Impacts of Climate Change

7.2.7End of Topic Test - The Water Cycle

7.3Water Insecurity

7.3.1Water Stress

7.3.2Causes of Water Insecurity

7.3.3Water Insecurity Risk

7.3.4Conflict Over Water

7.4Water Supply Management

7.4.1Hard Engineering Schemes

7.4.2Sustainable Management

7.4.3Water Treaties & Framework

7.4.4End of Topic Test - Water Insecurity & Management

8The Carbon Cycle & Energy Security (A2 only)

8.1The Carbon Cycle

8.1.1Carbon Stores

8.1.2Carbon Stores 2

8.1.3Biological Carbon

8.1.4Atmospheric Carbon

8.1.5Burning Fossil Fuels

8.2Energy Consumption

8.2.1Consumption

8.2.2Access to Energy

8.2.3Energy Players

8.2.4Supply & Demand

8.2.5Pathways

8.2.6End of Topic Test - Carbon & Consumption

8.3Alternative Energy

8.3.1Unconventional Fuels

8.3.2Non-Fossil Fuels

8.3.3Non-Fossil Fuels 2

8.4Growing Demand for Resources

8.4.1Deforestation

8.4.2Water

8.4.3Climate Change

8.5The Future

8.5.1Future Uncertainty

8.5.2Adaptation Strategies

8.5.3Mitigation Strategies

9Superpowers (A2 only)

9.1Superpowers

9.1.1Introduction to Superpowers

9.1.2Superpowers - Economic Power & Size

9.1.3Superpowers - Political & Military Power

9.1.4Superpowers - Culture, Demography & Resources

9.1.5Geo-Strategic Location

9.2Hard & Soft Power

9.2.1Hard & Soft Power

9.2.2Emerging Powers - China Rivalry

9.2.3Emerging Powers - Chinese Sources of Power

9.2.4Emerging Powers - Brazil

9.2.5Emerging Powers - Russia

9.2.6Emerging Powers - India

9.2.7Theories of Development

9.2.8Power Case Studies: Chinese One Belt One Road

9.2.9Power Case Studies: Pakistan Nuclear Arms

9.2.10Power Case Studies: OPEC

9.3IGOs, TNCs & Alliances

9.3.1Superpowers & IGOs

9.3.2Superpowers & TNCs

9.3.3Superpowers & Global Action

9.3.4Superpowers & Alliances

9.3.5Superpowers & the Environment

9.4Changing Global Influence

9.4.1Recent Tensions between Powers

9.4.2China in Africa & Asia

9.4.3Tensions in the Middle East

9.4.4Economic Problems for Superpowers

9.4.5Future Pattern of Power

10Option 8A: Health & Human Rights (A2 only)

11Option 8B: Migration & Identity (A2 only)

11.1Globalisation & Migration

11.1.1Intro to Migration

11.1.2Trends in Migration

11.1.3Common Migration Patterns

11.1.4Causes of Migration

11.1.5Restrictions on Migration

11.2Consequences of Migration

11.2.1Intro to Culture

11.2.2Social & Demographic Tensions of Migration

11.2.3Political & Economic Tensions of Migration

11.3Nation States

11.3.1Intro to Nation States

11.3.2Borders

11.3.3Nationalism

11.4Responses to Global Migration

11.4.1Responses to Global Migration

11.4.2Global Organisations

11.4.3IGOs and World Trade

11.4.4Financial IGOs

11.4.5Environmental IGOs

11.5Sovereignty & Identity

11.5.1Sovereignty & Nationalism

11.5.2Complex Identities

11.5.3Challenges to National Identities

11.5.4Tensions within Nations

11.5.5Failed States

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