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Hazardous Earth

Subduction at oceanic-continental and oceanic-oceanic boundaries

  • 2 things to know
  • Component 03

Overview

Recall questions on subduction, ocean trenches and the Challenger Deep, Benioff zones, how magma forms above a subducting slab and why it is silica-rich, accretionary prisms, the Andes, island arcs such as the Marianas and Aleutians, back-arc basins, great and deep-focus earthquakes, and violent eruptions.

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Answer each one before you reveal it.

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Key term

What is subduction?

Key term

At an oceanic-continental boundary, which plate is subducted, and why?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is subduction?

    Model answer

    The sinking of a dense oceanic plate beneath a less dense plate at a convergent boundary, carrying it back into the mantle.

  2. 2

    At an oceanic-continental boundary, which plate is subducted, and why?

    Model answer

    The oceanic plate, because it is denser than continental crust and so sinks beneath it.

  3. 3

    What is an ocean trench, and how does it form?

    Model answer

    A long, narrow, very deep depression in the ocean floor, formed where the subducting plate bends sharply downwards and drags the sea floor down with it.

  4. 4

    Name the deepest point on the ocean floor and the trench in which it lies.

    Model answer

    The Challenger Deep, in the Mariana Trench, at almost 11,000 m below sea level.

  5. 5

    What is a Benioff zone?

    Model answer

    The inclined plane of earthquake foci that marks the descending slab, becoming progressively deeper with distance from the trench.

  6. 6

    Explain why magma is generated above a subducting slab.

    Model answer

    Water driven out of the hydrated minerals in the sinking slab rises into the overlying mantle wedge and lowers its melting point, so it melts without being heated any further.

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