Mount Santiago is a stratovolcano, characterized by its steep profile and periodic explosive eruptions. These volcanoes are formed from alternating layers of lava flow, ash, and other volcanic debris. Stratovolcanoes are typically associated with subduction zones, where an oceanic plate is forced beneath a continental plate, leading to the formation of magma. Mount Santiago, located in the Philippines, exhibits these typical features of stratovolcanoes.
Mt. Pelee is a Cinder Cone Volcano.
Composite Volcano (stratovolcano).
Mt hekla is a statovolcano
Mount Trident is a cinder cone type of volcano.
it is an active complex volcano
shield volcano
stratovolcano
mt. vesuvious is known as a cinder volcano
Composite, or Stratovolcano
cinder cone
It's a stratovolcano.
An extinct volcano