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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.

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Key term

What happens when two continental plates converge?

Numbers

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. 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. 2

    Which mountain range is forming at the collision of the Indian and Eurasian plates?

    Model answer

    The Himalayas.

  3. 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. 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. 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. 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.

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AThe lower quartile is the 2nd value, 11 cm.
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