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Madagascar's rainforests at risk

22nd April 2018

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Tropical rainforests have been at risk from deforestation for decades. Whether the cause is from logging, excavation of minerals or palm oil; the result is the same. Madagascar is facing a new demand from its forests - vanilla and it's a matter of life and death.

The global price of vanilla has risen more than tenfold in the last ten years as a result of the demand for vanilla flavouring from wealthy nations and the decline in the amount of vanilla as a result of crop damage from cyclones.  This has led to an increase in farmers choosing this crop to cultivate over other tropical crops.  In Madagascar, the rise of gangs has led to issues for the farmers as they steal the vanilla crop.  The gangs have become so confident over their ability to control the trade, that they even tell the farmers when they will be arriving.  This has led to vigilante groups targeting the gangs and killing them.  Check out the report here for more on this issue... https://www.theguardian.com/en...  

  • Tropical rainforest
  • Deforestation

Joanne Parkinson

An experienced, outstanding Geography teacher, GCSE examiner and Head of Humanities in a 11-18 school. I'm passionate about all geographical events and am a keen blogger.

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  • Case study - Food Shortage - Madagascar
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  • 3. Economic Development
  • 3.2 Food Production
  • 4. Food Shortage in Madagascar

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gcse geography madagascar case study

Case Study: Thanet Earth

Thanet earth.

Thanet Earth is the largest complex of greenhouses in England. Thanet Earth is in Kent and it uses hydroponics (growing plants in a water solvent) instead of growing plants in soil.

Illustrative background for Advantages of Thanet Earth

Advantages of Thanet Earth

  • Thanet Earth produces tomatoes every week of the year. This would not be possible outdoors in the UK.
  • Thanet Earth produces 225 million tomatoes each year (12% of the UK's total production).
  • Thanet Earth produces 13 million cucumbers each year (8% of the UK's total production).
  • The Thanet Earth complex is environmentally-friendly and any excess power generated is put into the UK's National Grid.
  • Over 250 people are employed at Thanet Earth.
  • More of the UK's vegetables are grown in the UK, rather than imported, so the UK has better food security.
  • Thanet Earth uses lower amounts of fertilisers and pesticides because of its greenhouses.

Illustrative background for Disadvantages of Thanet Earth

Disadvantages of Thanet Earth

  • The greenhouses were developed on top of existing farmland, so the development has reduced the amount of greenbelt land and likely destroyed some wildlife's habitats.
  • Heating, lighting, and running the greenhouses consume a lot of energy (although excesses are put back into the National Grid).
  • The high levels of lighting needed to grow plants creates light pollution.

1 The Challenge of Natural Hazards

1.1 Natural Hazards

1.1.1 Types of Natural Hazards

1.1.2 Hazard Risk

1.1.3 Consequences of Natural Hazards

1.1.4 End of Topic Test - Natural Hazards

1.1.5 Exam-Style Questions - Natural Hazards

1.2 Tectonic Hazards

1.2.1 Tectonic Plates

1.2.2 Tectonic Plates & Convection Currents

1.2.3 Plate Margins

1.2.4 Volcanoes

1.2.5 Effects of Volcanoes

1.2.6 Responses to Volcanic Eruptions

1.2.7 Earthquakes

1.2.8 Earthquakes 2

1.2.9 Responses to Earthquakes

1.2.10 Case Studies: The L'Aquila & Kashmir Earthquakes

1.2.11 Earthquake Case Study: Chile 2010

1.2.12 Earthquake Case Study: Nepal 2015

1.2.13 Living with Tectonic Hazards 1

1.2.14 Living with Tectonic Hazards 2

1.2.15 End of Topic Test - Tectonic Hazards

1.2.16 Exam-Style Questions - Tectonic Hazards

1.2.17 Tectonic Hazards - Statistical Skills

1.3 Weather Hazards

1.3.1 Global Atmospheric Circulation

1.3.2 Surface Winds

1.3.3 UK Weather Hazards

1.3.4 Tropical Storms

1.3.5 Features of Tropical Storms

1.3.6 Impact of Tropical Storms 1

1.3.7 Impact of Tropical Storms 2

1.3.8 Tropical Storms Case Study: Katrina

1.3.9 Tropical Storms Case Study: Haiyan

1.3.10 UK Weather Hazards Case Study: Somerset 2014

1.3.11 End of Topic Test - Weather Hazards

1.3.12 Exam-Style Questions - Weather Hazards

1.3.13 Weather Hazards - Statistical Skills

1.4 Climate Change

1.4.1 Evidence for Climate Change

1.4.2 Causes of Climate Change

1.4.3 Effects of Climate Change

1.4.4 Managing Climate Change

1.4.5 End of Topic Test - Climate Change

1.4.6 Exam-Style Questions - Climate Change

1.4.7 Climate Change - Statistical Skills

2 The Living World

2.1 Ecosystems

2.1.1 Ecosystems

2.1.2 Ecosystem Cascades & Global Ecosystems

2.1.3 Ecosystem Case Study: Freshwater Ponds

2.2 Tropical Rainforests

2.2.1 Tropical Rainforests - Intro & Interdependence

2.2.2 Adaptations

2.2.3 Biodiversity of Tropical Rainforests

2.2.4 Deforestation

2.2.5 Case Study: Deforestation in the Amazon Rainforest

2.2.6 Sustainable Management of Rainforests

2.2.7 Case Study: Malaysian Rainforest

2.2.8 End of Topic Test - Tropical Rainforests

2.2.9 Exam-Style Questions - Tropical Rainforests

2.2.10 Deforestation - Statistical Skills

2.3 Hot Deserts

2.3.1 Overview of Hot Deserts

2.3.2 Biodiversity & Adaptation to Hot Deserts

2.3.3 Case Study: Sahara Desert

2.3.4 Desertification

2.3.5 Case Study: Thar Desert

2.3.6 End of Topic Test - Hot Deserts

2.3.7 Exam-Style Questions - Hot Deserts

2.4 Tundra & Polar Environments

2.4.1 Overview of Cold Environments

2.4.2 Adaptations in Cold Environments

2.4.3 Biodiversity in Cold Environments

2.4.4 Case Study: Alaska

2.4.5 Sustainable Management

2.4.6 Case Study: Svalbard

2.4.7 End of Topic Test - Tundra & Polar Environments

2.4.8 Exam-Style Questions - Cold Environments

3 Physical Landscapes in the UK

3.1 The UK Physical Landscape

3.1.1 The UK Physical Landscape

3.2 Coastal Landscapes in the UK

3.2.1 Types of Wave

3.2.2 Weathering & Mass Movement

3.2.3 Processes of Erosion & Wave-Cut Platforms

3.2.4 Headlands, Bays, Caves, Arches & Stacks

3.2.5 Transportation

3.2.6 Deposition

3.2.7 Spits, Bars & Sand Dunes

3.2.8 Case Study: Landforms on the Dorset Coast

3.2.9 Types of Coastal Management 1

3.2.10 Types of Coastal Management 2

3.2.11 Coastal Management Case Study - Holderness

3.2.12 Coastal Management Case Study: Swanage

3.2.13 Coastal Management Case Study - Lyme Regis

3.2.14 End of Topic Test - Coastal Landscapes in the UK

3.2.15 Exam-Style Questions - Coasts

3.3 River Landscapes in the UK

3.3.1 The River Valley

3.3.2 River Valley Case Study - River Tees

3.3.3 Erosion

3.3.4 Transportation & Deposition

3.3.5 Waterfalls, Gorges & Interlocking Spurs

3.3.6 Meanders & Oxbow Lakes

3.3.7 Floodplains & Levees

3.3.8 Estuaries

3.3.9 Case Study: The River Clyde

3.3.10 River Management

3.3.11 Hard & Soft Flood Defences

3.3.12 River Management Case Study - Boscastle

3.3.13 River Management Case Study - Banbury

3.3.14 End of Topic Test - River Landscapes in the UK

3.3.15 Exam-Style Questions - Rivers

3.4 Glacial Landscapes in the UK

3.4.1 Erosion

3.4.2 Landforms Caused by Erosion

3.4.3 Landforms Caused by Transportation & Deposition

3.4.4 Snowdonia

3.4.5 Land Use in Glaciated Areas

3.4.6 Tourism in Glacial Landscapes

3.4.7 Case Study - Lake District

3.4.8 End of Topic Test - Glacial Landscapes in the UK

3.4.9 Exam-Style Questions - Glacial Landscapes

4 Urban Issues & Challenges

4.1 Urban Issues & Challenges

4.1.1 Urbanisation

4.1.2 Urbanisation Case Study: Lagos

4.1.3 Urbanisation Case Study: Rio de Janeiro

4.1.4 UK Cities

4.1.5 Case Study: Urban Regen Projects - Manchester

4.1.6 Case Study: Urban Change in Liverpool

4.1.7 Case Study: Urban Change in Bristol

4.1.8 Sustainable Urban Life

4.1.9 End of Topic Test - Urban Issues & Challenges

4.1.10 Exam-Style Questions - Urban Issues & Challenges

4.1.11 Urban Issues -Statistical Skills

5 The Changing Economic World

5.1 The Changing Economic World

5.1.1 Measuring Development

5.1.2 Classifying Countries Based on Wealth

5.1.3 The Demographic Transition Model

5.1.4 Physical & Historical Causes of Uneven Development

5.1.5 Economic Causes of Uneven Development

5.1.6 How Can We Reduce the Global Development Gap?

5.1.7 Case Study: Tourism in Kenya

5.1.8 Case Study: Tourism in Jamaica

5.1.9 Case Study: Economic Development in India

5.1.10 Case Study: Aid & Development in India

5.1.11 Case Study: Economic Development in Nigeria

5.1.12 Case Study: Aid & Development in Nigeria

5.1.13 Economic Development in the UK

5.1.14 Economic Development UK: Industry & Rural

5.1.15 Economic Development UK: Transport & North-South

5.1.16 Economic Development UK: Regional & Global

5.1.17 End of Topic Test - The Changing Economic World

5.1.18 Exam-Style Questions - The Changing Economic World

5.1.19 Changing Economic World - Statistical Skills

6 The Challenge of Resource Management

6.1 Resource Management

6.1.1 Global Distribution of Resources

6.1.2 Food in the UK

6.1.3 Water in the UK 1

6.1.4 Water in the UK 2

6.1.5 Energy in the UK

6.1.6 Resource Management - Statistical Skills

6.2.1 Areas of Food Surplus & Food Deficit

6.2.2 Food Supply & Food Insecurity

6.2.3 Increasing Food Supply

6.2.4 Case Study: Thanet Earth

6.2.5 Creating a Sustainable Food Supply

6.2.6 Case Study: Agroforestry in Mali

6.2.7 End of Topic Test - Food

6.2.8 Exam-Style Questions - Food

6.2.9 Food - Statistical Skills

6.3.1 The Global Demand for Water

6.3.2 What Affects the Availability of Water?

6.3.3 Increasing Water Supplies

6.3.4 Case Study: Water Transfer in China

6.3.5 Sustainable Water Supply

6.3.6 Case Study: Kenya's Sand Dams

6.3.7 Case Study: Lesotho Highland Water Project

6.3.8 Case Study: Wakel River Basin Project

6.3.9 Exam-Style Questions - Water

6.3.10 Water - Statistical Skills

6.4.1 Global Demand for Energy

6.4.2 Factors Affecting Energy Supply

6.4.3 Increasing Energy Supply: Renewables

6.4.4 Increasing Energy Supply: Non-Renewables

6.4.5 Carbon Footprints & Energy Conservation

6.4.6 Case Study: Rice Husks in Bihar

6.4.7 Exam-Style Questions - Energy

6.4.8 Energy - Statistical Skills

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AQA GCSE Geography

gcse geography madagascar case study

Lake District Case Study: Glacial Formations

The Lake District National Park in Cumbria, North West England, is a scenic region known for its lakes, mountains and forests, along with features created by glaciers. It was named a UNESCO World Heritage Site in 2017 and holds keys to understanding England’s geological history.

In this case study, we’ll explore the glacial formations found in the Lake District, their impacts on the region, and management strategies implemented to address the challenges.

Glacial Formations in the Lake District

Helvellyn is one of England’s highest mountains, standing at an impressive 949 metres above sea level. It mainly consists of hard igneous rock and formed around 450 million years ago.

The surrounding landscape and many of Helvellyn’s features were shaped during the last ice age, roughly 20,000 years ago.

Breathtaking landscape from Helvellyn mountain summit, featuring a rugged rocky foreground, green rolling hills in the mid-distance, and a panoramic view of valleys, peaks, and a few fluffy clouds against a blue sky.

Below, we’ll outline some noteworthy glacier-formed landmarks in Helvellyn and the greater Lake District:

Glacial erosional formations

Glacier erosion creates distinct landforms, including a few remarkable examples found in the Lake District:

Deep hollows, known as corries , were carved into the mountainsides by glacier erosion. One notable example is Red Tarn, which is a corrie lake located on the Eastern side of Helvellyn.

Red Tarn has typical features of a corrie, such as:

  • A steep back wall constructed by freeze-thaw weathering and plucking
  • Steep ridges and a lake

For a refresher on these terms, feel free to revisit our pages on glacial processes and landform formations .

The Lake District has several arêtes , which are narrow ridges that form between two glacial valleys due to erosion. Striding Edge and Swirral Edge, both located on Helvellyn, are examples of arêtes.

Aerial view of a clear Red Tarn lake surrounded by green terrain, with a steep rocky ridge to the right and distant valleys and water bodies in the background.

As you can see in the map below, Striding Edge and Swirral Edge are opposite each other, with Red Tarn between them.

gcse geography madagascar case study

Map from © OpenStreetMaps

U-shaped valleys

U-shaped valleys , also known as glacial troughs, are landforms sculpted by glaciers. Borrowdale is a valley with its iconic ribbon lakes, such as Derwentwater. It is a classic example of a glacial trough.

View of Borrowdale valley, with a calm lake, in the Lake District including reflections of mountains, with different sized pebbles in the foreground and a splash of yellow wildflowers.

Ribbon lakes

Ribbon lakes are long, narrow lakes occupying the deep, U-shaped valleys carved by glacial erosion. One of the largest and most beautiful lakes in the Lake District is Ullswater, which is an example of this type of formation.

Scenic view of the Lake District showcasing lush greenery, with Ullswater lake surrounded by rolling hills and mountains under a blue sky with scattered clouds.

Glacial depositional formations

Glacial depositional formations occur when a moving glacier leaves behind rocks or soil. This happened around 20,000 years ago in the last ice age, shaping several land features in the process.

If any terms confuse you, make sure to revisit our page on Glacial Deposition and Landforms Created .

  • In the Lake District, you can find moraines , which are piles of rocks and sediment left by glaciers, in areas like Bannerdale and Haweswater. Some of these moraines are now covered with plants.
  • Drumlins are another formation found at valley bottoms, characterised by their elongated, rounded hill shape created from boulder clay deposits. The Lowther Hills, located near Penrith, are notable drumlin formations in the Lake District.

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Internet Geography

The Holderness Coast

The Holderness Coast is Europe’s fastest eroding coastline.

The Holderness Coast Case Study

Looking for information on the landforms of erosion and deposition on the Holderness Coast? You can find it here .

What is the location of the Holderness Coast?

The Holderness Coast is located on the east coast of England. It extends 61km from Flamborough in the north to Spurn Point in the south.

Lost settlements on the Holderness Coast

Lost settlements on the Holderness Coast

The Holderness Coastline is one of Europe’s fastest eroding at an average annual rate of around 2 metres. This is around 2 million tonnes of material every year. Approximately 3 miles (5kms) of land has been lost since Roman times, including 23 towns/villages. These are shown on the map below.

What is the geology of the Holderness Coast?

Underlying the Holderness Coast is bedrock made up of Cretaceous Chalk. However, in most places, this is covered by glacial till deposited over 18,000 years ago. It is this soft boulder clay that is being rapidly eroded.

There are two main reasons why this area is eroding so rapidly. The first is the result of the strong prevailing winds creating destructive waves. The second is that the cliffs are made of soft boulder clay, which erodes rapidly when saturated.

Holderness Coast Case Study

The Holderness Coast is a great case study for examining coastal processes and their associated features. This is because the area contains ‘textbook’ examples of coastal erosion and deposition. The exposed chalk of Flamborough provides examples of erosion and features such as caves, arches and stacks. Coastal management at Hornsea and Withernsea are examples of hard engineering solutions to coastal erosion. Erosion at Skipsea illustrates the human impact of erosion in areas where coastlines are not being defended.  Mappleton is an excellent case study of an attempt at coastal management, which has a negative impact further along the coast.

Spurn Point provides evidence of longshore drift on the Holderness Coast. It is an excellent example of a spit, a depositional landform . Around 3% of the material eroded from the Holderness Coast is deposited here annually.

Find out more about the landforms of coastal erosion and deposition on the Holderness Coast .

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Use the images below to explore locations along the Holderness Coast.

Flamborough

Geos and mass movement at Flamborough

Spurn Point

Spurn Point

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