Convergent plate boundaries are also know as destructive plate boundaries because of subduction. They are actively deforming regions where two or more tectonic plates or fragments of the lithosphere move toward one another and collide and form either a subduction zone or a continental collision. They form volcanoes like Mt. St. Helens, chains of volcanoes like the Pacific Ring of Fire, mountain ranges like the Cascade Mountains, and island arc with a deep oceanic trench in front like the Marina trench near the Marina Islands.
The Himalayan Mountains, Southern Alps in New Zealand, Aleutian Islands, Andes Mountains, Pontic mountains in Turkey, etc. have been formed by convergent plate boundaries.
Convergent boundaries create uplift and reverse faults in the earth's crust.
these create rift valleys
It Creates A Mountian
mountains
Volcanoes are usually found near convergent an divergent plate boundaries, which are themselves major faults and usually create minor faults. Minor faults can also provide a pathway for magma to reach the surface.
A divergent boundary between two oceanic crusts can cause mid-ocean ridges such as the Mid-Atlantic Ridge. A divergent boundary between two continental crusts can cause rift valleys like the East African Rift Valley. Many volcanoes can be formed from the outflow of magma onto Earth's surface, and even volcanic islands such as Iceland can be formed.
plates moving together
Mountain ranges are created at convergent plate boundaries. That is where two plates, either ocean and continental or continental and continental come together.
Mountain ranges, such as the Himalayas, were formed when 2 plates collided. When 2 tectonic plates crash together, the force pushes the plate boundaries upward and create mountains. So, mountains are formed by convergent plate boundaries. By, Heather (11) ADDED: Correct, though the collision is more a steady push than a "crash". The Himalayas are still forming, with the up-lift slightly faster than the erosion, as India is still colliding with the Asian continental plate.
No. They occur at convergent boundaries.
Convergent boundaries are where two tectonic plates hit each other. This can cause earthquakes, but can also create mountains.
it is found in the Nepal where the Himalayas lye under that is the convergent boundary
No. They create faults like San Andreas in California. Volcanoes form at convergent boundaries.
Some similarities between convergent and divergent boundaries are that both create faults that are capable of producing earthquakes; both are tectonic plates; and both are part of the lithosphere.
Convergent boundaries are responsible for creating mountain ranges. When two tectonic plates collide, the land is forced upwards, creating intense pressure that results in the formation of mountain ranges. Examples of mountain ranges formed by convergent boundaries include the Himalayas and the Andes.
Any type of plate boundary can cause an earthquake. That said, areas along convergent, divergent, and transform tectonic plate boundaries are the most likely places for earthquakes to occur.
A mountain is an example of a possible result of converging plate boundaries. An actual example of a converging plate boundary would be the Indian-Eurasian Plate Boundarywhich is creating the Himalayan Mountain Range. Other convergent plates can create trenches such as the Mariana Trench, which is the lowest place on the surface of the Earth.
Volcanoes are usually found near convergent an divergent plate boundaries, which are themselves major faults and usually create minor faults. Minor faults can also provide a pathway for magma to reach the surface.
when the two plate boundaries breaks free, the force causes the water to overflow and create a tsunami. One or both of the plate have to be an oceanic plate. :D
Landforms that could be created at convergent boundaries would include: volcanoes, mountains, trenches, volcanic islands, and even deserts could result from the effects of converging boundaries.the landforms are mountains
The Himalayas, Andes, and Alps are examples of mountain ranges formed by continental-continental convergent boundaries. These boundaries occur when two continental plates collide, resulting in intense folding, faulting, and uplift of the Earth's crust to create mountain ranges.