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.
Wiki User
∙ 10y agoWiki User
∙ 13y agoSouth American plate and the pacific plate.
Wiki User
∙ 12y agoIt is called a divergent plate boundary.
Examples of a divergent boundary would be a mid-ocean ridge. Two plates are pulling apart from each other. If you have heard before, the magma from the asthenosphere find a way to get out through the crack of the diverging plates and makes new land. Another type of devergent boundary would be a fissure. It is a long linear crack made by the plates moving apart. I think maybe another one would probably be a volcano, but I am not sure.
A boundary between 2 air masses of different density moisture or temperature is a front.
It can hold 2 metal plates together.
At plate boundaries you're more likely to get earthquakes and volcanoes due to the plates moving. If they rub against each other, they can lock together and build up energy that'd be released as an Earthquake. If one plate moves under another, it'll turn in to magma because the heat of the mantle would melt it, and it'd eventually be released from a volcano. You don't get these problems in the middle of the plate because there aren't plates moving there.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.
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.
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.
when two plates push together, it could either cause mountains or a subduction zone. When they cause mountains it's when two
convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.
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.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic 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.
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.
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.
Rebound tendency is when 2 plates from a convergent boundary slide past one another to form a trench