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Hazardous Earth

Sea-floor spreading, palaeomagnetism and the age of the ocean floor

  • 2 things to know
  • Component 03

Overview

Recall questions on sea-floor spreading and Harry Hess, palaeomagnetism and the Curie point, geomagnetic reversals and symmetrical magnetic stripes explained by Vine and Matthews, the age of oceanic crust and why it is young, sediment thickness and heat flow across ocean basins, and confirmation by ocean drilling.

What you need to know

Answer each one before you reveal it.

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Numbers

Who put forward the idea of sea-floor spreading, and when?

Key term

Explain how cooling basalt records the Earth's magnetic field.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define sea-floor spreading.

    Model answer

    The process by which new oceanic crust forms at a mid-ocean ridge and moves outwards symmetrically on either side as the plates separate.

  2. 2

    Who put forward the idea of sea-floor spreading, and when?

    Model answer

    Harry Hess proposed it in 1962.

  3. 3

    What is palaeomagnetism?

    Model answer

    The record of the Earth's past magnetic field preserved in rocks by iron-rich minerals that aligned with the field as the rock cooled and solidified.

  4. 4

    Explain how cooling basalt records the Earth's magnetic field.

    Model answer

    As lava cools below the Curie point of about 580 °C, the magnetite crystals within it lock into alignment with the magnetic field of the time and hold that direction permanently.

  5. 5

    What is a geomagnetic reversal?

    Model answer

    An episode in which the Earth's magnetic field flips, so that magnetic north becomes magnetic south.

  6. 6

    Describe the pattern of magnetic stripes on the ocean floor.

    Model answer

    Bands of alternating normal and reversed polarity run parallel to the mid-ocean ridge and are mirrored in width and order on both sides of it.

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