An earthquake or if at sea a tsunami.
when two plates collide they form trenches.
collision
A convergent boundary
Examples of collision mountain ranges include the Himalayas (formed by the collision of the Indian Plate with the Eurasian Plate), the Alps (formed by the collision of the African Plate with the Eurasian Plate), and the Andes (formed by the collision of the South American Plate with the Nazca Plate).
A continent-continent collision can produce large mountain ranges, such as the Himalayas formed by the collision between the Indian Plate and the Eurasian Plate. This collision typically results in intense folding and faulting of the Earth's crust, leading to the uplift of rocks and the creation of deep mountain roots.
An example of a continental to continental crust collision is the collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayan mountain range. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
The Himalayas, located in South Asia, are formed by the collision of the Indian Plate with the Eurasian Plate. This collision has caused the land to uplift, creating some of the highest mountains in the world.
Its when the oceanic crust and the continental crsut colide together.
The collision of the Nazca Plate and the South American Plate.