Stratovolcanoes are common at subduction zones, forming chains along plate tectonic boundaries where oceanic crust is drawn under continental crust. Examples are the Andes and the Aleutian Islands.
Usually convergent plate boundaries, although there are exceptions like the Hawaiian Islands which are over a hot spot in the mantle.
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
Continental mountains, ocean trenches, volcanic mountains, volcanic islands and arcs.
Convergent Boundary.
collision plate boundary because they make mountains
at an oceanic to continental convergent boundary trenches and volcanic mountains can form. at an oceanic to oceanic convergent boundary trenches and volcanic islands can form. at a continental to continental convergent boundary fold mountains can form
The landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
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.
Continental mountains, ocean trenches, volcanic mountains, volcanic islands and arcs.
Convergent Boundary.
Convergent Boundary.
Mountains form at convergent plate boundaries.
collision plate boundary because they make mountains
convergent plate boundaries
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)
Transform boundaries do not produce volcanic activity.
north american plate