Mount Kelud is located on a destructive plate boundary, specifically the subduction zone where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This type of boundary is characterized by intense geological activity such as volcanic eruptions and earthquakes.
Mount Kelud is a stratovolcano, which is a type of volcano characterized by its steep slopes and explosive eruptions.
Mount Kelud is a stratovolcano, which is a type of volcano characterized by steep sides and a cone shape. It is located in Indonesia and is known for its explosive eruptions.
yes
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's volcanoes.
Mount Tambora is associated with a convergent plate boundary.
Mount Kelud is a stratovolcano, which is a type of volcano characterized by its steep slopes and explosive eruptions.
None. Mount Tabora is not creating a boundary. It was created by a convergent plate boundary.
Mount Kelud is a stratovolcano, which is a type of volcano characterized by steep sides and a cone shape. It is located in Indonesia and is known for its explosive eruptions.
mount etna is on asubduction plate boundary under the african and eurasian plate
yes
Divergent plate boundary.
Mount Nyamuragira is on a convergent boundry
subduction
Mount Adatara is associated with a convergent plate boundary, as are all of Japan's 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 Tambora is associated with a convergent plate boundary.
Mount Merapi is near a convergent plate boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate.