either subduction (e.g. pacific ring of fire) or mountain building (e.g. himalayas)
a subduction boundry, this is where one plate gets pushed under the other. in this case the pacific plate is being pushed under the eurasion!
the India Plate and the Eurasian Plate pushed into each other, until the Indian Plate was pushed UNDER the Eurasian Plate, causing the Eurasian Plate to be raised up 10m
The plates get pushed up, then the the plate that gets pushed, pushes land up then you have a volcano.
The India plate crashing into the Asia plate caused the formation of the Himalayas. It can also cause subduction, when one plate is pushed beneath the other plate and so pushed back into the molten mantle.
The techtonic plates are shifting. One plate is being overlaped by the other.
When one tectonic plate is pushed beneath another plate, it is called subduction. This process occurs at convergent plate boundaries where one plate is denser than the other, causing it to sink into the mantle. Subduction zones are associated with deep ocean trenches and can lead to volcanic activity and earthquakes.
Plate techtonics or shifting of the earth's crust.
Subduction, is when one plate is pushed down into the magma, by the other plate sliding over the top.
Juan de fuca plate are being pushed under the north american plate
A convergent plate boundary is where one of the plates is sinking beneath another, and the other one is being pushed on top of the subducting plate. This is called a subduction zone. This happens when denser, heavier oceanic crust meets less dense, thicker, continental crust.When two plates converge, and one is less dense, that plate goes under the more dense plate into the mantle, this is called subduction.subduction will happen and a volcano will be formed. when one plate slides beneath another one magma from earths mantle is being pushed up on earths surface.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.