There are two plate boundaries that cause volcanoes. They are the divergent and convergent plate boundaries.
lithospheric plate movement
Mount Colima is formed at a convergent plate boundary, where the Cocos Plate is subducting beneath the North American Plate. This subduction process generates volcanic activity, leading to the formation of the stratovolcano. The intense geological activity at this boundary is responsible for Mount Colima's eruptions and ongoing volcanic development.
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 Vesuvius is located on a convergent plate boundary where the African plate is subducting beneath the Eurasian plate. This type of boundary is associated with intense tectonic activity and is responsible for the volcanic eruptions in the region.
At Mount Pelee, the plate boundary interaction causes the subduction of the North American Plate beneath the Caribbean Plate. This subduction process generates intense heat and pressure, leading to the melting of rock beneath the surface. The molten rock then rises to the surface, resulting in volcanic eruptions at Mount Pelee.
Transform boundaries do not produce volcanic activity.
Convergent, divergent, and, although not a plate boundary, they also occur from hotspots.
The Philippines is located on the boundary of two tectonic plates: the Philippine Sea Plate to the east and the Eurasian Plate to the west. This boundary is characterized by frequent seismic and volcanic activity, making the Philippines prone to earthquakes and volcanic eruptions.
lithospheric plate movement
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 Vesuvius is located on a convergent plate boundary where the African plate is subducting beneath the Eurasian plate. This type of boundary is associated with intense tectonic activity and is responsible for the volcanic eruptions in the region.
This type of boundary is called a convergent boundary or subduction zone, where the oceanic plate is pushed beneath the continental plate. The descending oceanic plate melts due to the heat and pressure, leading to volcanic activity and the formation of volcanic arcs.
At Mount Pelee, the plate boundary interaction causes the subduction of the North American Plate beneath the Caribbean Plate. This subduction process generates intense heat and pressure, leading to the melting of rock beneath the surface. The molten rock then rises to the surface, resulting in volcanic eruptions at Mount Pelee.
Mount Vesuvius is located on a destructive plate boundary. It is situated on the boundary where the African Plate subducts beneath the Eurasian Plate. This subduction process is what causes volcanic activity in the area.
The area of volcanic activity far from a tectonic plate boundary is called a "hotspot." Hotspots are characterized by plumes of hot mantle material that can create volcanic islands and chains, such as the Hawaiian Islands. These volcanic activities occur independently of tectonic plate movements, often resulting in long-lived eruptions in a localized area.
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.
All the countries of the Pacific ring of fire are on a tectonic plate edge. Canada, USA, Mexico, Panama, Colombia, Peru, Ecuador, Chile, China, Philippines, Japan, South Korea, North Korea, Indonesia, Costa Rica, Nicaragua, Russia, Papua New Guinea etc