There is a compressional stress on the rocks which causes the crust to shorten. Reverse faults (the hanging wall moves up) occur at convergent plate boundaries. In continental-continental convergent boundaries, where two continents collide, the crust becomes deformed and thickened forming mountain chains. This is known as orogenesis or mountain building. This occurrence explains the creation of the Himalayas where India and Asia collided.
Strictly speaking, it is the tectonic plates that collide, not just the continents.
The shortening of the land may be accommodated by land folding. For example, the Indian Plate is colliding with the Asian Plate, causing land shortening and mountain folding and building. (Have a glance at the path of the rivers rising in the Himalayas.).
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
Either plates gets subducted which is usually the older plate.
The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.
When tectonic plates collide with oceanic plates, the denser oceanic plate is usually forced beneath the less dense continental plate in a process called subduction. This can lead to the formation of volcanic arcs and deep ocean trenches. The collision can also cause earthquakes and crustal deformation.
They create a convergent boundary and can often create mountains, over a period of years.
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
when continents collide you bum your pet hamster
a subduction zone forms
a subduction zone forms
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
Either plates gets subducted which is usually the older plate.
At an ocean ocean convergent boundary, there will be a formation of volcanoes.
Either plates gets subducted which is usually the older plate.
When two continental plates come together, they can form convergent boundaries where one plate is forced beneath the other in a process known as subduction. This can lead to the formation of mountain ranges, earthquakes, and volcanic activity as the plates interact and collide.
It is folded and uplifted, or subducted into the mantle, depending on the type of convergent boundary.