Subduction | Definition, Process & Effects
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Subduction | Definition, Process & Effects
Where does subduction occur? In this lesson, learn what a subduction zone is, learn how the subduction process works, and understand why plates subduct.
146K viewsMar 27, 2016
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Subduction Zone | Definition, Characteristics & Examples
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Subduction Zone | Definition, Characteristics & Examples
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The subduction of dense oceanic crust into the mantle plays an essential role in driving plate tectonics. However, the details of how new subduction zones form are poorly understood. In this model a section of buoyant oceanic crust arrives at a subduction trench and blocks it, causing the already-subducted slab to break off, and halting subduction. Then subduction starts in the opposite direction. The model shows not just a reversal, but how a new subduction can start, which is a matter of much
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The subduction of dense oceanic crust into the mantle plays an essential role in driving plate tectonics. However, the details of how new subduction zones form are poorly understood. In this model a section of buoyant oceanic crust arrives at a subduction trench and blocks it, causing the already-subducted slab to break off, and halting subduction. Then subduction starts in the opposite direction. The model shows not just a reversal, but how a new subduction can start, which is a matter of much
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Subduction zone earthquakes are the largest and most destructive on earth. In 2004 a 9.1 megaquake hit Sumatra off the coast of Indonesia, unleashing a massive tsunami and killing 227,898 people. And in 2011, the Tohoku earthquake struck Japan, killing around 20,000 and triggering the infamous Fukushima nuclear disaster. In the Pacific northwest lurks the Cascadia Subduction Zone, which has been dormant for centuries and is overdue for its next “big one.” In this episode we’re going to tell you
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Study.com
The subduction of dense oceanic crust into the mantle plays an essential role in driving plate tectonics. However, the details of how new subduction zones form are poorly understood. In this model a section of buoyant oceanic crust arrives at a subduction trench and blocks it, causing the already-subducted slab to break off, and halting subduction. Then subduction starts in the opposite direction. The model shows not just a reversal, but how a new subduction can start, which is a matter of much
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The subduction of dense oceanic crust into the mantle plays an ess…
843 viewsJan 6, 2022
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