convergent plates
The San Gabriel Mountains were formed by the collision of the Pacific Plate and the North American Plate along a transform boundary. The northward movement of the Pacific Plate scraping against the North American Plate created pressure and uplift that contributed to the formation of the mountains.
Volcanic mountains are not formed by plate collision. These mountains are created when magma from within the Earth's mantle rises to the surface and solidifies.
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 Cascade Range mountains were created by a convergent boundary where the Juan de Fuca Plate is being subducted beneath the North American Plate. This collision led to magma being generated and rising to the surface, resulting in the volcanic peaks of the Cascade Range.
Aleutian type mountains are formed by the subduction of the Pacific Plate under the North American Plate along the Aleutian Trench. This subduction leads to the volcanic activity in the region, forming a chain of volcanic islands known as the Aleutian Islands. As the Pacific Plate sinks beneath the North American Plate, magma rises to the surface, creating the characteristic volcanic peaks of the Aleutian Mountains.
The San Gabriel Mountains were formed by the collision of the Pacific Plate and the North American Plate along a transform boundary. The northward movement of the Pacific Plate scraping against the North American Plate created pressure and uplift that contributed to the formation of the mountains.
weathering and erosion
Volcanic mountains are not formed by plate collision. These mountains are created when magma from within the Earth's mantle rises to the surface and solidifies.
volcanoes
Mountains form along convergent boundaries when 2 plates collide. These are also called colliding boundaries.
Mountains form at convergent plate boundaries.
Divergent plate movement.
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.
Convergent Boundaries.
each plate boundary has a different boundaries. if you want the movement for a specific plate boundary, write the name of the plate boundary. :]
No, the Andes are near a subduction zone type plate edge but the Appalachian Mountains are not near any plate edge of any kind.
The Antarctic Plate.