There is no such thing as a subduction boundary, there are divergent, convergent, and transform boundaries. When there is a continental-oceanic convergent boundary (when a continental plate and an oceanic plate smash together) the oceanic plate, because it is more dense sinks into deeper layers of the earth. The area where the two plates meet makes a trench which is a subduction zone. The oceanic plate will melt into the earth and because of the excess lava it rises out onto the continent and makes a volcanic mountain and the lava erupts.
Where crust is destroyed
Where oceanic crust meets continental crust and earthquakes can occur.
Yes, subduction zones are significant sites for earthquakes. They occur when one tectonic plate is forced beneath another, creating intense pressure and friction along the boundary. This buildup of stress can eventually be released in the form of earthquakes, which can be quite powerful and damaging. Many of the world's largest earthquakes occur in subduction zone regions.
Divergent boundaries are found primarily along mid-ocean ridges, where tectonic plates are moving away from each other. Additionally, divergent boundaries can also occur on continents, leading to the formation of rift valleys.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
they occur i think in the plate boundarys.
No, hotspot volcanoes do not occur along subduction zones. They occur when plates pass over mantle hot spots.
Where crust is destroyed
The deepest earthquakes occur at subduction zones where one tectonic plate is forced beneath another into the Earth's mantle. These earthquakes can occur as deep as 700 km below the surface.
For sure.
A compressional bounday is plate boundarys that are being compressed
Convergent Boundaries!
convergent boundaries collide but divergent boundaries move away from each other.
Cool
convergent
subduction boundary eruption
divergent boundarys