subduction zone

crustal generation and destructionThree-dimensional diagram showing crustal generation and destruction according to the theory of plate tectonics; included are the three kinds of plate boundaries—divergent, convergent (or collision), and strike-slip (or transform).
The Earth's crust is a jigsaw puzzle of huge rigid plates in constant relative motion. The plates are bounded by three types of features: ridge axes, where new seafloor is created in mid-ocean; transform faults, where plates slide past one another; and subduction zones, where plates overlap, with one plate sliding under the other.
The Earth's crust is a jigsaw puzzle of huge rigid plates in constant relative motion. The plates are bounded by three types of features: ridge axes, where new seafloor is created in mid-ocean; transform faults, where plates slide past one another; and subduction zones, where plates overlap, with one plate sliding under the other.

subduction zone, oceanic trench area marginal to a continent in which, according to the theory of plate tectonics, older and denser seafloor underthrusts the continental mass, dragging downward into the Earth’s upper mantle the accumulated trench sediments. The subduction zone, accordingly, is the antithesis of the mid-oceanic ridge. New seafloor is generated from the upper mantle at the mid-oceanic ridges, spreads laterally outward, and is eventually subducted, or consumed, at the margins of ocean basins. Subduction may also occur between two regions of oceanic crust, with older, denser sections underthrusting younger, less-dense ones.

This article was most recently revised and updated by John P. Rafferty.
Citation Information
Article Title: subduction zone
Website Name: Encyclopaedia Britannica
Publisher: Encyclopaedia Britannica, Inc.
Date Published: 08 January 2018
URL: https://www.britannica.comhttps://www.britannica.com/science/subduction-zone
Access Date: November 12, 2024