Mount Merapi is not a plate. However, it was formed by the convergence of a oceanic plate and a continental plate. The oceanic Indo-Australian plate subducted under the continetal Eurasian plate causing a line of volcanoes.
Mount Merapi is a convergent boundary type, specifically a subduction zone where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction has led to the explosive volcanic activity and frequent eruptions characteristic of Mount Merapi.
Mount Merapi sits on the destructive plate boundary between the Indo-Australian Plate and the Eurasian Plate in Indonesia. This boundary is characterized by subduction, where the Indo-Australian Plate is moving beneath the Eurasian Plate, leading to volcanic activity in the region.
Mount Usu is created by the movement of the Pacific Plate subducting beneath the North American Plate along a convergent plate boundary. The volcanic activity at Mount Usu is a result of the melting of subducted oceanic crust and the magma rising to the surface.
Mount Bromo is located in Indonesia on the island of Java, which sits on the Indo-Australian Plate. This plate is slowly moving northward and colliding with the Eurasian Plate, leading to volcanic activity in the region. The volcanic arc that includes Mount Bromo is due to subduction of the Indo-Australian Plate beneath the Eurasian Plate.
Mount Pavlof in Alaska is located along the boundary between the Pacific Plate and the North American Plate. The subduction of the Pacific Plate beneath the North American Plate in this region leads to volcanic activity, resulting in the formation of Mount Pavlof.
Mount. Merapi is on the Sunda Plate, which forms a convergent margin with the Indian-Australian Plate
Mount Merapi is near a convergent plate boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate.
Mount Merapi is a convergent boundary type, specifically a subduction zone where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction has led to the explosive volcanic activity and frequent eruptions characteristic of Mount Merapi.
The Indo-Australian plate and the Sunda plate were involved in the volcanic activity at Mount Merapi in Indonesia. The collision between these plates led to the subduction of the Indo-Australian plate beneath the Sunda plate, creating the conditions for volcanic eruptions.
yup, mount merapi is the youngest (about 40000yrs old)
The last major eruption of Mount Merapi in Indonesia began on May 11, 2018, with periodic eruptions continuing for several months.
yes, it is the most active volcano in Indonesia
Yogyakarta
Mount Merapi is the active volcano near Yogyakarta in Java, Indonesia.
Stratovolcano
look on line
Mount Merapi sits on the destructive plate boundary between the Indo-Australian Plate and the Eurasian Plate in Indonesia. This boundary is characterized by subduction, where the Indo-Australian Plate is moving beneath the Eurasian Plate, leading to volcanic activity in the region.