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Covergent
Subduction boundaries
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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.
They are formed by the continental contienal plates
Divergent Plate Boundary. (Seafloor Spreading).
Japan is at the meeting place of four tectonic plates: The Pacific Plate, The Eurasian Plates, The Philippine Plate, and the Okhotsk Plate (sometimes considered part of the North American Plate).
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The plate boundary that causes mountains to form is called a convergent boundary.
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.
The kind of plate boundary that moves apart is a Divergent Plate Boundary
The 'South Island'. A collision boundary.