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
Hazardous Earth
Continental collision and conservative boundaries
- 2 things to know
- Component 03
Overview
Recall questions on continental collision, the Himalayas and the Tethys Sea with a worked convergence calculation, why collision zones lack volcanoes but have destructive earthquakes, thick Himalayan crust, conservative boundaries such as the San Andreas and North Anatolian faults, stick-slip movement, shallow earthquakes, seismic gaps, and offset landscapes.
What you need to know
Answer each one before you reveal it.
India is converging with Asia at about 5 cm per year. Calculate how much convergence that gives in one million years.
Questions from this subtopic
Each one with the model answer underneath.
- 1
What happens when two continental plates converge?
Model answer
Neither is dense enough to subduct, so the crust between them is crumpled, faulted and thickened into fold mountains.
- 2
Which mountain range is forming at the collision of the Indian and Eurasian plates?
Model answer
The Himalayas.
- 3
What was the Tethys Sea, and what became of it?
Model answer
An ocean that lay between India and Asia; its floor was subducted as India moved north, and its sediments were folded up into the Himalayas when the two continents met.
- 4
India is converging with Asia at about 5 cm per year. Calculate how much convergence that gives in one million years.
Model answer
5 cm × 1,000,000 years = 5,000,000 cm, which is 50 km.
- 5
Why are there almost no volcanoes along a continental collision boundary?
Model answer
With no oceanic slab descending to release water into the mantle, very little magma is generated, so there is nothing to feed volcanoes.
- 6
Why can collision boundaries still produce very destructive earthquakes?
Model answer
The compressed crust fractures along thrust faults at shallow depth, so even a moderate magnitude releases its energy close to the surface beneath densely populated valleys.
Other ways to work this
The same content, four other ways.
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