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Hazardous Earth

Lava flows, pyroclastic flows and volcanic gases

  • 2 things to know
  • Component 03

Overview

Recall questions on the damage and reach of lava flows, pyroclastic flows, their speed, temperature, lethality and origins, Mount Pelée and Saint-Pierre in 1902, volcanic gases, carbon dioxide, sulphur dioxide and acid rain, cooling after Pinatubo, fluorine poisoning, volcanic smog, and the deadly gases of long effusive eruptions.

What you need to know

Answer each one before you reveal it.

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Key term

Why do lava flows rarely kill people?

Key term

Define a pyroclastic flow.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Why do lava flows rarely kill people?

    Model answer

    Most flows advance slowly enough for people to walk away from them, so the loss is of property and land rather than of life.

  2. 2

    What damage does a lava flow do?

    Model answer

    It buries and burns everything in its path, setting fire to buildings and vegetation and leaving a sterile rock surface that takes decades to become useful land again.

  3. 3

    What determines how far a lava flow travels?

    Model answer

    Its viscosity, its eruption temperature, the rate at which it is supplied from the vent, and the steepness and shape of the ground.

  4. 4

    Define a pyroclastic flow.

    Model answer

    A dense, ground-hugging avalanche of hot gas, ash and rock fragments that rushes down the flanks of a volcano.

  5. 5

    State the typical speed and temperature of a pyroclastic flow.

    Model answer

    They commonly move at more than 100 km per hour and reach several hundred degrees Celsius, sometimes over 700 °C.

  6. 6

    Why is a pyroclastic flow so much more lethal than a lava flow?

    Model answer

    It travels far faster than anyone can escape and kills instantly by heat and asphyxiation, so there is no time to evacuate once it has begun.

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