Paracutin is in the trans-Mexican volcanic belt formed by the riviera and cocos plates subducting under the north American plate
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.
A landform that can be formed at a convergent plate boundary is a mountain range. This occurs when two continental plates collide, pushing up rock layers and creating uplifted peaks. Examples include the Himalayas formed by the collision of the Indian Plate with the Eurasian Plate.
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.
Salar de Uyuni was formed from uplift and evaporation of a giant prehistoric lake, caused by the collision of the Nazca and South American Plates.
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 Paricutin is located on the North American Plate in the state of Michoacán, Mexico, at the boundary between the North American Plate and the Cocos Plate. It is considered a landmark example of an active cinder cone volcano.
The boundary that is formed is called a Tranform Boundary
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.
Divergent boundary is formed
Mount Tambora was formed by a convergent plate boundary. It is located on the Indonesian island of Sumbawa, where the Australian Plate converges with the Sunda Plate, causing subduction and volcanic activity in the region.
Convergent boundary
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.
It is not on a plate boundary but in the middle of a plate. Kilauea has formed over a hot spot.
convergent plate boundary
A constructive plate boundary, as it pushes land upwards (which formed the mountains)
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.