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Tectonic Hazards

Conservative margins and hot spots

  • 3 things to know
  • Component 3 Section A

Overview

San Andreas Fault, conservative margin outside the United States and elastic rebound theory.

What you need to know

Answer each one before you reveal it.

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Key term

What happens at a conservative plate margin?

Key term

Why are there no volcanoes at conservative margins?

Key term

Describe the San Andreas Fault.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What happens at a conservative plate margin?

    Model answer

    Two plates slide past one another, and no crust is created or destroyed. Friction locks the fault until the stored stress is released as an earthquake.

  2. 2

    Why are there no volcanoes at conservative margins?

    Model answer

    Neither plate descends into the mantle, so no additional melting takes place. Lack of a magma supply means earthquakes occur without eruptions.

  3. 3

    Describe the San Andreas Fault.

    Model answer

    The San Andreas Fault runs about 1,300 km through California, where the Pacific Plate slides north-west past the North American Plate. Relative movement averages around 5 cm yr⁻¹.

  4. 4

    Which earthquake destroyed San Francisco, and what was its magnitude?

    Model answer

    The San Francisco earthquake of 18 April 1906 is estimated at moment magnitude 7.9. Around 3,000 deaths are attributed to the shaking and the fires that followed.

  5. 5

    Name a conservative margin outside the United States.

    Model answer

    The North Anatolian Fault carries the Anatolian Plate westwards past the Eurasian Plate across northern Turkey. The fault extends for around 1,500 km.

  6. 6

    Describe the İzmit earthquake of 1999.

    Model answer

    The İzmit earthquake of 17 August 1999 on the North Anatolian Fault reached moment magnitude 7.6. Official figures compiled by 2000 recorded more than 17,000 deaths.

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