Subduction - Wikipedia, the free encyclopedia
In geology, subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate, sinking into the Earth's mantle, as the plates converg...
en.wikipedia.org/wiki/Subduction
Cascadia subduction zone - Wikipedia, the free encyclopedia
The Cascadia subduction zone (also referred to as the Cascadia fault ) is a subduction zone, a type of convergent plate boundary that stretches from northern Vancouver Island to northern Californi...
en.wikipedia.org/wiki/Cascadia_subduction_zone
When this happens, subduction terminates along the collision zone, the trench disappears, and the continents collide, resulting in the birth of a new mountain range. ... Volcanic Island Arcs form at subduction zones...
www.platetectonics.com/book/page_12.asp
Subduction Zone Studies ... In places these are separated by non-rigid (deforming) zones. Elsewhere plate boundaries of three types exist: divergent or spreading (e.g., mid-oceanic ridges), convergent (e.g., subduction zones), and strike-slip (e.g., the San Andreas fault zone in California or oceanic transform faults).
www.ruf.rice.edu/~leeman/billarcmaps.html
The subduction of the Juan de Fuca plate beneath North America changes markedly along the length of the subduction zone, notably in the angle of subduction, distribution of earthquakes, volcanism, geologic and seismic structure of the upper plate, and regional horizontal stress.
earthquake.usgs.gov/research/structure/crust/cascadia.p... earthquake.usgs.gov/research/structure/crust/cascadia.php
USGS Earthquake Hazards Program, responsible for monitoring, reporting, and researching earthquakes and earthquake hazards ... The subduction zone is the place where two lithospheric plates come together, one riding over the other. Most volcanoes on land occur parallel to and inland from the boundary between the two plates.
earthquake.usgs.gov/learning/glossary.php?term=subducti... earthquake.usgs.gov/learning/glossary.php?term=subduction%20zone
This process is called subduction. The slab that is forced back into the Earth usually undergoes melting when the edges get to a depth which is hot enough. (A temperature hot enough to melt lithosphere is about a thousand degrees!). This process is called "subduction".
www.windows.ucar.edu/tour/link=/earth/interior/subducti... www.windows.ucar.edu/tour/link=/earth/interior/subduction.html
The melted crust also releases gases of the atmosphere which had become trapped in the ground. Thus subduction of the crust helps to recycle the atmosphere!
www.windows.ucar.edu/tour/link=/earth/interior/subducti... www.windows.ucar.edu/tour/link=/earth/interior/subduction.html&edu=elem
In the immense furnace of a subduction zone, the denser plate plunges beneath its neighbor, and portions of it may be melted by the intense heat generated within the mantle, turning the solid rock of the crust into molten magma.
sio.ucsd.edu/volcano/about/subduction.html sio.ucsd.edu/volcano/about/subduction.html
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