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Coastal Systems · England · AQA · Edexcel · OCR

The Holderness Coast

2m

per year.

Europe's fastest eroding coastline — 61km from Flamborough Head to Spurn Point, losing approximately 2 million tonnes of material annually.

Eroding chalk cliffs at the Holderness Coast, North Sea waves crashing at the base

Since Roman times, approximately 5km of land has vanished — including 23 towns and villages. The underlying soft boulder clay, deposited during the last glaciation, erodes far faster than the chalk bedrock it covers.

This is not a distant hazard. Homes are falling into the sea. A road serving Mappleton village was 34 metres from the cliff edge before emergency defences were installed in 1991.

2meroded every year

Destructive waves from the North-East carry a fetch of 500–800km across the North Sea, arriving with immense energy. The underlying Cretaceous chalk is largely buried beneath soft glacial boulder clay deposited 18,000 years ago — and it is this till that crumbles fastest. Sub-aerial erosion compounds the problem: rainwater infiltrates the clay, adding weight and triggering mass movement. The sea floor remains deep here, meaning waves lose little energy before impact.

Climate change link: Global temperatures have risen ~0.8°C over the past 150 years, with sea levels rising approximately 17cm. Accelerated sea level rise will intensify erosion rates, making current management strategies increasingly inadequate — a key evaluation point in exam answers.

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Aerial view of coastline showing tsunami damage and destruction, flattened coastal buildings and debris
Tectonic HazardsAQA · Edexcel · OCR · IB

Indian Ocean · 26 Dec 2004

The Boxing Day Tsunami

227,000lives lost across 14 countries

A 9.1-magnitude earthquake ruptured 1,200km of the Sunda Trench. The Indian Plate subducting beneath the Sunda/Burman plates caused a 3-metre vertical seafloor displacement across a 400×100km area, generating waves up to 30 metres. The earthquake was so powerful it shortened Earth's day by 2.68 microseconds.

Dense urban settlement in Mumbai showing colourful buildings, narrow lanes and rooftop water tanks in Dharavi
Urban GeographyAQA · Edexcel · IB

Mumbai, India · Est. 1884

Dharavi's Informal Economy

$1bn+generated annually by a 2.39km² settlement

Founded in 1884 during British colonial rule, Dharavi grew through expulsion of factories from Mumbai's peninsular city centre and sustained rural-urban migration. Its population of approximately 1,000,000 occupies 2.39km², creating one of the world's highest population densities at 418,410 per km².

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AQA A-Level Geography

12 case studies
Coastal Systems & Landscapes
Tectonic Hazards
Urban Issues & Challenges
Global Systems & Governance

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Updated for 2026

Climate data, erosion rates, and economic figures refreshed for current exam cycles.

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What People Say

From the Revision Desk

I used the Holderness case study the night before my Paper 1. The layer tabs made it so easy to revise physical processes separately from human impact — that's exactly how the exam questions split it.

Young South Asian woman with dark hair smiling, student profile photo

Priya Mehta

A-Level Geography, St Paul's Girls' School, London · Predicted A*

I projected the Dharavi section in a Year 13 lesson on urban inequality. Students were immediately engaged — the $1 billion economy figure alone sparked a 20-minute discussion I hadn't planned for.

Black male teacher with glasses and a warm smile, professional photo

Mr. James Okafor

Head of Geography, Northampton Academy

I'd read about the Boxing Day Tsunami in three different textbooks and none of them mentioned the Earth's day shortening. That detail went straight into my personal statement.

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Tom Whitfield

UCAS applicant · Geography, Durham University · Offer received

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