The Andes mountains were formed from the interaction of the South American Plate and the Nazca Plate, which is a convergent plate boundary. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift and formation of the Andes mountains.
The Andes mountain range is a result of convergent plate boundary formation, where the South American Plate is subducting beneath the Nazca Plate. This collision has led to the uplift and formation of the Andes mountains through various geological processes over millions of years.
The Andes Mountains in South America and the Cascades Range in North America were formed as a result of ocean-continental convergence. These mountains were created through the subduction of oceanic plates beneath continental plates, leading to the uplift of land and the formation of mountain ranges.
When an oceanic plate subducts beneath a continental plate (convergent boundary) it can create enormous mountains due to the intense compression and uplift of the continental crust. An example of this is the Andes Mountains in South America, formed by the subduction of the Nazca Plate beneath the South American Plate.
The Himalayan range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.The Andes are the result of plate tectonics processes, caused by the subduction of oceanic crust beneath the South American plate. The main cause of the rise of the Andes is the compression of the western rim of the South American Plate due to the subduction of the Nazca Plate and the Antarctic Plate.
The Jura Mountains and the Zagros Mountains are examples of the fold mountains. The fold mountain is formed as a result of the effects if the folding on layers within the upper part of the crust of the earth.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
A constructive plate boundary, as it pushes land upwards (which formed the mountains)
A convergent boundary between an oceanic plate and a continental plate.
The Andes Mountain Chain is formed as a result of a convergent plate boundary, the collision of the South American Plate with the Nazca Plate.
convergent boundary.
The Andes Mountains were formed through subduction of the oceanic plate underneath the South American plate.
the andes mountains were formed by a continental collision
The Andes Mountians.
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The Andes Mountains. These are generally on the west side of the South American continent.
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.