When an ocean plate dives under a continent
Age 14 · Geography
Open to everyone until Thursday, October 29
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Where two plates collide, the heavier oceanic plate sinks beneath the lighter continental plate, a process called subduction. This carves a deep trench in the seabed, and rock that melts above the sinking plate rises as magma to build a chain of volcanoes.
In the picture
- Oceanic plate: thin, dense crust that sinks beneath the continent
- Ocean trench: the deep trough where the oceanic plate dives down
- Magma: molten rock rising from above the sinking plate
- Volcanic chain: a row of volcanoes inland on the continental plate
Examples
- The Andes in South America, where the Nazca plate sinks under South America beside the Peru–Chile Trench.
- The Cascade volcanoes in the north-western United States, such as Mount St. Helens, fed by the Juan de Fuca plate sinking under North America.
Key takeaways
- Oceanic crust is denser than continental crust, so the oceanic plate is the one that sinks.
- Subduction zones produce deep trenches, volcanoes and powerful earthquakes.
Quiz: When an ocean plate dives under a continent (Age 14)
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When an oceanic plate and a continental plate collide, which one sinks, and why?
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What forms in the seabed at the place where the oceanic plate dives down?
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Where does the magma that builds the chain of volcanoes come from?
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