Which description best defines subduction?

Prepare for the Gemological Institute of America's Graduate Diamonds Exam. Enhance your expertise with comprehensive quizzes and insightful explanations. Be ready to excel!

Multiple Choice

Which description best defines subduction?

Explanation:
Subduction is the sinking of one tectonic plate into the mantle at a convergent boundary, driven by density differences—usually the oceanic plate sliding beneath a less dense continental or another oceanic plate. This descent creates a subduction zone, deep ocean trenches, volcanic activity, and earthquakes as the slab melts and interacts with mantle rocks. The description fits this idea because it specifies a collision between a continental plate and an oceanic plate, with the oceanic plate being forced down into the mantle. Why the other ideas don’t fit: flow of magma beneath plates describes general magma movement rather than the entire process of one plate descending; continents splitting apart refers to rifting and continental drift in a distinct boundary type; and the collision of two continental plates leads to mountain building without subduction of oceanic crust, since there isn’t a dense oceanic slab to sink.

Subduction is the sinking of one tectonic plate into the mantle at a convergent boundary, driven by density differences—usually the oceanic plate sliding beneath a less dense continental or another oceanic plate. This descent creates a subduction zone, deep ocean trenches, volcanic activity, and earthquakes as the slab melts and interacts with mantle rocks.

The description fits this idea because it specifies a collision between a continental plate and an oceanic plate, with the oceanic plate being forced down into the mantle.

Why the other ideas don’t fit: flow of magma beneath plates describes general magma movement rather than the entire process of one plate descending; continents splitting apart refers to rifting and continental drift in a distinct boundary type; and the collision of two continental plates leads to mountain building without subduction of oceanic crust, since there isn’t a dense oceanic slab to sink.

Subscribe

Get the latest from Passetra

You can unsubscribe at any time. Read our privacy policy