They are formed by the continental contienal plates
A convergent boundary is formed when one tectonic plate descends beneath another. This process is known as subduction and typically leads to the formation of deep ocean trenches and volcanic arcs.
The plate boundary that causes mountains to form is called a convergent boundary.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
The South American Plate and the Nazca Plate are separated by a convergent boundary, specifically a subduction zone. This is where the Nazca Plate is forced under the South American Plate, creating the Andes mountain range and causing volcanic activity.
The North America and Caribbean plates meet at a transform plate boundary. This type of boundary is characterized by plates sliding past each other horizontally, causing earthquakes along the boundary.
The Alps are primarily located along a convergent boundary where the Eurasian Plate collides with the African Plate. This boundary is marked by intense tectonic activity resulting in the uplifting of the mountain range.
Covergent
Subduction boundaries
A plateau can form on a convergent plate boundary where two plates collide, causing uplift and compression of the crust. It can also form on a divergent plate boundary where two plates move apart, leading to the stretching and thinning of the crust, creating a high, flat landform.
one talc
When it reforms how it answers the lines once before.
A convergent boundary is formed when one tectonic plate descends beneath another. This process is known as subduction and typically leads to the formation of deep ocean trenches and volcanic arcs.
Divergent Plate Boundary. (Seafloor Spreading).
Japan is at the meeting place of four tectonic plates: The Pacific Plate, The Eurasian Plates, The Philippine Plate, and the Okhotsk Plate (sometimes considered part of the North American Plate).
a plate -.-
The plate boundary that causes mountains to form is called a convergent boundary.
When two edges of tectonic plates collide (convergent boundary) they can cause a crumpling effect and an upthrust to form mountains. The Himalayas, for instance, were formed when the Indian Plate crashed into the Asian Plate. Convergent boundary also applies to the situation where one plate moves under the other (subduction) this kind of plate boundary can also form mountain chains. An example of this is the Andes mountains.