Convergent plate boundaries.
true
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
Himalayas
Continental Collision Boundary
The Appalachian mountain.
true
Convergent boundary, which in this case would lead to mountain building (as in the Himalayas)
Plate tectonics, (inter-continental plate collision).
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
convergent plate boundary
Mountain-building is a result of continental collision, so destructive plate boundaries. One plate is destroyed by subduction below the other, which undergoes compression, buckling and uplift as the collision continues. This is happening at present in Asia, raising the Himalayan Mountains.
they are both formed by converging plates at a BOUNDARY THAT PUSH UP THE EARTH
The Andes Mountains. These are generally on the west side of the South American continent.
The Appalachian mountain.
Himalayas
There are actually two mountain ranges that act as a boundary, the Ural Mountains and the Caucuses.
The Cascade Range is located at a convergent boundary, where the Juan de Fuca Plate is subducting beneath the North American Plate. This subduction causes volcanic activity and mountain building in the region.