the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.
The Himalaya mountains were formed in a collision of the Indian Plate pushing into the Eurasian Plate, in a convergent boundary known as a continental collision.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as the Himalayas.
A Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
Continental mountain ranges are associated with the convergent boundaries of tectonic plates. When two plates collide, they can cause the Earth's crust to uplift, creating mountain ranges. Examples include the Rocky Mountains in North America and the Himalayas in Asia.
In a oceanic-continentalconvergent boundaryyou normally get subduction , when one plate slides under another. In this case the plate subducting, or going under is the oceanic plate ( it is more dense ), so the mountains would be just of the continental plate. In aoceanic-oceanic convergent boundary the mountains would just be oceanic ( basalt).
continental continental convergent boundary
Continental Collision Boundary
The Himalaya mountains were formed in a collision of the Indian Plate pushing into the Eurasian Plate, in a convergent boundary known as a continental collision.
Mountain formation is a feature associated with a continental plate boundary, where the collision of two continental plates results in the uplift of the Earth's crust, creating mountain ranges such as the Himalayas.
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Yes, the Zagros Mountains were formed due to the collision between the Arabian Plate and the Eurasian Plate along a convergent boundary. This ongoing tectonic activity continues to uplift and shape the Zagros Mountains.
The Himalayas are found at a convergent plate boundary also known as a subduction zone where one plate slips under the other driving the land mass up.
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 Collision plate boundary, where two continental plates that are the same in density and thickness, push against each other forming fold mountains and crumble zones. This causes Earthquakes from the pressure and stress but not volcanoes.
Continental mountain ranges are associated with the convergent boundaries of tectonic plates. When two plates collide, they can cause the Earth's crust to uplift, creating mountain ranges. Examples include the Rocky Mountains in North America and the Himalayas in Asia.
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.