The lithosphere is destroyed.
Oceanic lithosphere is subducted under continental lithosphere at convergent plate boundaries. This process occurs when the denser oceanic plate sinks beneath the less dense continental plate, creating deep ocean trenches and volcanic arcs. The subducted oceanic plate eventually melts and contributes to the formation of magma that leads to volcanic activity.
Oceanic lithosphere is destroyed when it is subducted at a convergent plate boundary and forced into the mantle where it melts. You shouldn't use the internet to look up answers on a test. You should use your notes and textbook! DW Thanks for the answer but um, What about people in online school, where the only "textbook" you get is an agenda? yeah the awnser for Gradpoint is Convergent Boundary
The process of thrusting oceanic lithosphere into the mantle along a convergent plate boundary is called subduction. This occurs when one tectonic plate is forced below another due to their collision, leading to the recycling of Earth's crust and the formation of volcanic arcs.
At transform plate boundaries, the lithosphere slides past each other horizontally. This movement can cause earthquakes as the tectonic plates experience frictional forces. The lithosphere is neither created nor destroyed at transform plate boundaries.
The process of one tectonic plate moving beneath another is called subduction. This usually occurs at convergent plate boundaries where one plate is forced beneath the other due to differences in density. Subduction zones can lead to the formation of deep ocean trenches and volcanic arcs.
subduction
Lithosphere is neither destroyed nor created.
convergent boundary ^.<
Oceanic lithosphere is subducted under continental lithosphere at convergent plate boundaries. This process occurs when the denser oceanic plate sinks beneath the less dense continental plate, creating deep ocean trenches and volcanic arcs. The subducted oceanic plate eventually melts and contributes to the formation of magma that leads to volcanic activity.
The Andes Mountains are an example of mountain building activity at a convergent plate boundary, where the South American plate is colliding with the Nazca plate. This collision has led to the uplift and formation of the Andes mountain range.
Oceanic lithosphere plunges beneath an overriding continental plate at a convergent boundary, specifically at a subduction zone. The denser oceanic plate is forced beneath the less dense continental plate due to tectonic forces, leading to the formation of deep oceanic trenches and volcanic arcs on the overriding plate.
The oceanic lithosphere is subducted at convergent plate boundaries, where an oceanic plate meets a continental plate or another oceanic plate. This process typically occurs in areas known as subduction zones, characterized by deep ocean trenches. As the denser oceanic lithosphere sinks into the mantle, it leads to geological phenomena such as volcanic activity and the formation of mountain ranges.
These form when continent lithosphere on one plate collides with another.
These form when continent lithosphere on one plate collides with another.
These form when continent lithosphere on one plate collides with another.
Oceanic lithosphere is destroyed when it is subducted at a convergent plate boundary and forced into the mantle where it melts. You shouldn't use the internet to look up answers on a test. You should use your notes and textbook! DW Thanks for the answer but um, What about people in online school, where the only "textbook" you get is an agenda? yeah the awnser for Gradpoint is Convergent Boundary
At a convergent boundary, typically an oceanic lithosphere collides with either another oceanic lithosphere or continental lithosphere. When an oceanic plate meets a continental plate, the denser oceanic plate subducts beneath the continental plate, leading to the formation of deep ocean trenches and volcanic arcs. If two oceanic plates collide, one may subduct beneath the other, resulting in the creation of island arcs.