I'm pretty sure this is the answer. High mountain ranges form
a piece of lithosphere that becomes part of a larger landmass when tectonic plats collide at a convergent boundary
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
In plate tectonics, a convergent boundary also known as a destructive plate boundary (because of subduction), is an actively deforming region where two (or more) tectonic plates or fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.
In plate tectonics, a convergent boundary also known as a destructive plate boundary (because of subduction), is an actively deforming region where two (or more) tectonic plates or fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.
An area where two tectonic plates collide is called a boundary. There are three kinds of boundaries. They are convergent, divergent, and transform boundaries.
In plate tectonics, a convergent boundary also known as a destructive plate boundary (because of subduction), is an actively deforming region where two (or more) tectonic plates or fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.
A convergent boundary is where plates move together.
The boundary between plates is called a plate boundary, which is where tectonic plates meet. These boundaries can be divergent, convergent, or transform faults, and are characterized by various geological activities such as earthquakes, volcanic eruptions, and mountain building. Plate boundaries are dynamic regions where the Earth's lithosphere is constantly changing.
convergent boundary
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 antonym for divergent boundary is convergent boundary. In a divergent boundary, tectonic plates move away from each other, while in a convergent boundary, they move towards each other. This can result in subduction zones, mountain formation, or continental collision.
A convergent plate boundary is a place where tectonic plates are moving together. The plates are sliding across the the plastic asthenosphere.