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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. When two plates move towards one another, they form either a subduction zone or a continental collision. This depends on the nature of the plates involved. In a subduction zone, the subducting plate, which is normally a plate with oceanic crust, moves beneath the other plate, which can be made of either oceanic or continental crust. During collisions between two continental plates, large mountain ranges, such as the Himalayas are formed.

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South American plate and the pacific plate.

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Q: What are 2 plates that meet at a convergent boundary?
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Related questions

What are the sub-types of convergent plates boundrys?

1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.


Where do convergent boundary form?

convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.


The boundary formed between 2 plates that are colliding?

A convergent boundary is formed when two tectonic plates collide. This collision can result in one plate being forced beneath the other in a process called subduction, where the denser plate sinks into the mantle. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.


What are the three types of convergent plate boundries?

The three types of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental boundaries. Oceanic-continental boundaries occur when an oceanic plate subducts beneath a continental plate. Oceanic-oceanic boundaries happen when one oceanic plate subducts beneath another oceanic plate. Continental-continental boundaries involve the collision of two continental plates.


What are plates that push together called?

when two plates push together, it could either cause mountains or a subduction zone. When they cause mountains it's when two


Where convergent plate boundary form?

convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.


What type of fault is convergent boundary?

A convergent boundary is a reverse fault. It's a reverse fault because it it pushing together, while a divergent boundary is a normal fault because 2 plates are pushing away from each other.


What are the types of convergent boundary?

There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.


What type of fault is a convergent boundary?

A convergent boundary is a type of fault where two tectonic plates collide, causing compression forces that lead to the plates being pushed together. This can lead to the formation of mountain ranges, deep ocean trenches, and powerful earthquakes.


Which boundary is a convergent boundary?

A convergent boundary is a tectonic boundary where two lithospheric plates are moving towards each other. When they collide, one plate is typically forced beneath the other in a process known as subduction. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.


What are 2 different convergent boundaries?

Oceanic-continental convergent boundary: Where oceanic plates subduct beneath continental plates, creating deep ocean trenches and volcanic arcs on the overriding plate. Continental-continental convergent boundary: Where two continental plates collide, causing intense folding and faulting to create mountain ranges. An example is the collision of the Indian Plate with the Eurasian Plate, forming the Himalayas.


What is rebound tendency?

Rebound tendency is when 2 plates from a convergent boundary slide past one another to form a trench