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Subduction is the movement of one tectonic plate under another. The property of the plates that determines which plate is subducted at convergent boundaries is density.
Subduction
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In geology a trench is formed where one tectonic plate is subducted or forced under another plate.
Crust is subducted and destroyed at convergent plate boundaries, where one tectonic plate is forced beneath another. This process typically occurs at oceanic-continental or oceanic-oceanic boundaries, leading to the formation of deep ocean trenches and volcanic arcs. As the subducted plate descends into the mantle, it melts and contributes to geological phenomena such as earthquakes and volcanic activity.
When the Earth's crust is subducted, it sinks into the mantle at convergent plate boundaries, where one tectonic plate moves beneath another. This subduction process leads to increased temperature and pressure, causing the crust to partially melt and contribute to magma formation. The materials from the subducted crust can also lead to volcanic activity and the creation of mountain ranges over geological time. Eventually, some of the subducted material may be recycled back to the surface through volcanic eruptions or tectonic uplift.
The crust is subducted and destroyed at convergent plate boundaries, where an oceanic plate collides with a continental plate or another oceanic plate. In these zones, the denser oceanic plate is forced beneath the lighter continental crust into the mantle, leading to volcanic activity and the formation of deep ocean trenches. As the subducted material melts and is recycled, it contributes to geological processes such as magma formation and the creation of mountain ranges.
When a piece of crust is subducted, it is forced underneath another plate at a convergent boundary. This process can result in the crust melting and forming magma, leading to volcanic activity. Subduction zones are known for creating deep oceanic trenches and chains of volcanic islands.
Magma plumes can form at hotspots in the Earth's mantle, where unusually hot and buoyant rock rises towards the surface, leading to volcanic activity. They can also form at subduction zones where a tectonic plate is being subducted beneath another, causing melting of the mantle wedge above the subducted plate.
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The composition and density of the subducted plate, as well as the angle of subduction and presence of any obstacles in the subduction zone, can influence the descent angle of a subducted plate. Water content in the subducted plate can also affect its descent angle due to changes in the plate's buoyancy. The surrounding mantle flow and temperature conditions can further influence the descent angle of the subducted plate.
A subduction zone is where one plate is being subducted ( pulled down) under another plate, No it is not a plate boundary but it is were it happens. hope this helps