This depends on what material (oceanic crust or continental crust) the leading edges are made of.
When Continental crust hits Continental crust (eg India ploughing into Asia) the crust thickens by thrusting and folding and a mountain belt forms (the Himalayas). There is little or no volcanic activity associated with this sort of collision.
When Oceanic crust meets Continental crust (eg the Pacific plate and the west coast of South America), the oceanic crust sinks below the continental crust forming an oceanic trench on the oceanic side (a subduction zone) and a mountain belt on the continental side (by folding and uplift). This sort of collision produces a large amount of volcanic activity.
When Oceanic Crust meets Oceanic Crust, the actively spreading side sinks below the stationary side to form a back arc basin associated with island arcs and subduction zones (eg the Caribbean or the east of Papua New Guinea). This sort of collision also involves a large amount of volcanic activity.
Convergent boundary
A convergent plate movement occurs when two tectonic plates collide with each other. This typically happens at subduction zones, where one plate is forced beneath the other due to differences in density. This can create mountains, earthquakes, and volcanic activity.
Density plays a key role in convergent boundaries. When two plates collide at a convergent plate boundary, it is the denser plate that will subduct.
"Collide divide slide" is a phrase used to describe the three main types of plate boundaries: convergent (collide), divergent (divide), and transform (slide). Convergent boundaries are where plates come together, divergent boundaries are where plates move apart, and transform boundaries are where plates slide past each other.
A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.
When plates collide it is called a convergent boundary.newtest3
The answer is the Convergent Boundary.
when two plates collide together
Convergent Boundary
A region where plates collide is known as a convergent boundary. Here, one plate is forced beneath the other in a process called subduction, leading to intense geological activity such as earthquakes, volcanic eruptions, and the creation of mountain ranges.
A convergent boundary is where two plates collide. This can lead to the formation of mountains, earthquakes, and volcanic activity.
convergent boundary
Convergent boundary
Convergent boundary
Convergent boundary
They create a convergent boundary and can often create mountains, over a period of years.
Yes. Tambora is located where the Indian-Australian plate and the Eurasian plate collide. When two plates collide, it forms a convergent boundary.