Tectonic plate boundary
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's volcanoes.
Cinder Cones Mainly Form At Hot Spots off the coast of Africa, Eurasian Plate boundary, etc.
Yellowstone is not on a plate boundary, but is a 'hotspot' where magma seeps from the mantle to the surface, or near the surface. The case is the same for Hawaii.
Volcanoes are common on this type of plate boundary
High mountain ranges without volcanoes are built at convergent continental plate boundaries. These vary greatly from divergent boundaries which cause volcanoes to form.
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's volcanoes.
Convergent
Cinder Cones Mainly Form At Hot Spots off the coast of Africa, Eurasian Plate boundary, etc.
It isn't on a plate boundary. It's on a hotspot.
Yellowstone is not on a plate boundary, but is a 'hotspot' where magma seeps from the mantle to the surface, or near the surface. The case is the same for Hawaii.
Volcanoes are common on this type of plate boundary
hot spots
High mountain ranges without volcanoes are built at convergent continental plate boundaries. These vary greatly from divergent boundaries which cause volcanoes to form.
convergence plate boundary, where tectonic plates move towards each other and collide, leading to subduction zones which are highly constructive regions of volcanoes. Volcanoes also form at divergent plate boundaries. A good example being the numerous Icelandic volcanoes which have formed over he Mid Atlantic Ridge.
The type of boundary associated with Icelandic volcanoes is the constructive plate boundary, where two plates slowly move apart and magma seeps up through the gap.
Volcanoes on continents can develop at path convergent and divergent boundaries. They can occur where an oceanic plate subducts under a continental plate, producing a volcanic arc such as in the Cascade Range. Volcanoes can also occur in areas of rifting, such as Africa's Great Rift Valley, a developing divergent boundary. Where two oceanic plates converge volcanoes can develop underwater and eventually form volcanic islands. Volcanoes can also develop away from a plate boundary over a hot spot.
Volcanoes form igneous rock.