Divergent
Mountains are onvergent.
Mount Everest is not created by either convergent or divergent plate movements. It is actually formed as a result of the Indian Plate converging with the Eurasian Plate, causing the crust to crumple and uplift, forming the Himalayan mountain range.
The Earth's tallest mountain ranges are formed at convergent plate boundaries.
At divergent boundaries, mid-ocean ridges are formed as tectonic plates pull apart. At converging boundaries, various geologic features are formed such as trenches, mountains, and volcanic arcs, depending on the type of plates involved (oceanic vs. continental).
Continental Collision Boundary
Convergent boundry
Mountains are onvergent.
No, the Alps are not a divergent boundary. The Alps are a mountain range formed from the collision of the African and Eurasian tectonic plates, a result of convergent boundary activity.
A mountain is typically formed at convergent boundaries, where two tectonic plates collide. This collision causes intense pressure that forces the Earth's crust to uplift and form mountain ranges.
Yes volcanos are formed on convergent and divergent plate boundries but NOT on transform boundries
Trenches are formed by divergent plates, Whereas Ridges are formed by plate in collision.
it was a convergent of divergent because it is a stratovolcano
Convergent and divergent boundaries are terms used in plate tectonics to describe the juncture at two plates and how they move in relation to each other. Divergent plates move apart and convergent move towards each other.
Convergent and divergent boundaries are terms used in plate tectonics to describe the juncture at two plates and how they move in relation to each other. Divergent plates move apart and convergent move towards each other.
Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
Mount Everest is not created by either convergent or divergent plate movements. It is actually formed as a result of the Indian Plate converging with the Eurasian Plate, causing the crust to crumple and uplift, forming the Himalayan mountain range.
Mountain ranges are normally formed at convergent plate boundaries.