Calderas
No. Oceanic plates are denser than conitnental plates.
Tectonic
Everytime a volcano erupts, the magma gets higher and higher everytime it hardens. This causes an island arc
The oceanic plate subducts under the continental because it is denser. The Andes are being formed in this way and the Himalayas started that way also.
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
No. Oceanic plates are denser than conitnental plates.
the lithosphere is thinner under the oceanic crust
Tectonic
Oceanic. Most of the Pacific plate is under the Pacific Ocean.
destuctive plate margin
When oceanic lithosphere and continental lithosphere collide, the continental lithosphere may be obducted over the oceanic lithosphere or the oceanic lithosphere may be subducted under the continental lithosphere. The latter is thought to be more common. This subduction and obduction generally results in tectonic activity such as volcanoes and earthquakes.
That's a hotly debated question among scientists. We do know that trenches form where oceanic lithosphere subducts under continental lithosphere. as to what drives the plates together, it is probably continents being moved by the currents of the partially liquified asthenosphere below it. Many scientists think that it is the weight of the oceanic lithosphere being pulled by gravity and pushed from the higher mid-ocean ridges. To me that seems a bit like a chihuahua pulling a house.
It subducts under the continental plate because the oceanic plate is denser.
Thickness - continental = much thickerDensity - oceanic crust is denser than continental, which is why the oceanic crust subducts under the continental at destructive plates boundaries.
Everytime a volcano erupts, the magma gets higher and higher everytime it hardens. This causes an island arc
oceanic lithosphere sinks at subduction zones but not at mid ocean ridges because at subduction zones the oceanic lithosphere is subducted, or sinks, under another plate. Oceanic Lithosphere sinks at subduction zones which are usually at convergent boundaries, but at mid-ocean ridges the plates are actually separating not coming together
the oceanic plate subducts under the continental plate and then melts in the mantle and often will create volcanos along the conitinental plate.\