A Mountain belt.
Oceanic crust is denser and thinner than continental crust, which is thicker and less dense. When they converge at tectonic plate boundaries, the denser oceanic crust is forced beneath the continental crust in a process known as subduction. This occurs because the buoyancy of the continental crust prevents it from sinking, while the oceanic crust is subjected to greater gravitational forces. As a result, this subduction leads to geological phenomena such as earthquakes and the formation of volcanic arcs.
At a convergent boundary, two tectonic plates collide, typically involving either oceanic crust, continental crust, or a combination of both. Oceanic crust is usually subducted beneath continental crust due to its higher density, leading to the formation of trenches and volcanic arcs. In cases where two continental plates converge, they can create mountain ranges through a process called orogeny, as neither plate is easily subducted.
When two continental plates converge, a major landform created is a mountain range. The intense pressure and collision between the plates causes the Earth's crust to uplift, forming large mountain ranges such as the Himalayas or the Alps.
This process is called continental collision, and it typically results in the formation of mountain ranges. When two continental plates converge, neither plate is subducted due to their buoyancy, leading to the uplift of the crust. This phenomenon is exemplified by the collision between the Indian and Eurasian plates, which created the Himalayas.
As oceanic crust is thinner, it sinks under the continental crust and forms a subduction zone. This can also form a line of volcanoes.a deep sea trench and an island arc form.
Deep sea trenches, Mountain ranges, Volcanoes, and Earthquakes.
Trench
Oceanic crust is denser and thinner than continental crust, so when the two converge at a subduction zone, the oceanic crust is forced to sink beneath the less dense continental crust. This process of subduction is driven by the difference in density between the two types of crust, as well as the movement of tectonic plates.
A Mountain belt.
When oceanic crust collides with continental crust, the denser oceanic crust is forced beneath the continental crust in a process called subduction. This happens because oceanic crust is heavier, colder, and more dense than continental crust, making it susceptible to being subducted under the lighter continental crust. This collision can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches.
a valley or a canyon
Oceanic crust is denser and thinner than continental crust, which is thicker and less dense. When they converge at tectonic plate boundaries, the denser oceanic crust is forced beneath the continental crust in a process known as subduction. This occurs because the buoyancy of the continental crust prevents it from sinking, while the oceanic crust is subjected to greater gravitational forces. As a result, this subduction leads to geological phenomena such as earthquakes and the formation of volcanic arcs.
The contiental cdrust is forced under the continental crust in a process called subduction.
continental-continental collision I think. When I got down to the last one, that was the only answer left.
It creates a mountain
The contiental cdrust is forced under the continental crust in a process called subduction.