The Philippine plate collided with the Eurasian plate this is called a convergent boundary where the two plates collided and the plate melts and then shoots back up through the volcano causing an eruption
The plates involved in the Montserrat eruption are the North American Plate and the Caribbean Plate. Montserrat is located along the boundary where these two plates meet. The eruption was caused by the subduction of the North American Plate beneath the Caribbean Plate, leading to volcanic activity on the island.
The eruption of Mount Tarawera in 1886 was associated with a type of plate movement known as rifting. This event was caused by the North Island of New Zealand moving over the boundary between the Australian Plate and the Pacific Plate.
The eruption of Mount Merapi in 2010 was primarily caused by the subduction of the Indo-Australian Plate beneath the Eurasian Plate. This tectonic interaction generates significant volcanic activity in the region, as the subducted plate melts and contributes to magma formation. The resulting pressure and accumulation of magma ultimately led to the explosive eruption of Merapi.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
The eruption of Mount Vesuvius in 79 AD was caused by the subduction of the African Plate beneath the Eurasian Plate. This collision led to the formation of magma chambers beneath the Earth's surface, eventually resulting in the catastrophic eruption that buried the cities of Pompeii and Herculaneum.
The Philippine plate collided with the Eurasian plate this is called a convergent boundary where the two plates collided and the plate melts and then shoots back up through the volcano causing an eruption
The plates involved in the Montserrat eruption are the North American Plate and the Caribbean Plate. Montserrat is located along the boundary where these two plates meet. The eruption was caused by the subduction of the North American Plate beneath the Caribbean Plate, leading to volcanic activity on the island.
The eruption of Mount Tarawera in 1886 was associated with a type of plate movement known as rifting. This event was caused by the North Island of New Zealand moving over the boundary between the Australian Plate and the Pacific Plate.
it is a hot spot for the boundary because it represents the volcanic eruption
Destructive(collisional) plate margin/boundary
a desert plate and a dinner plate
transform boundary
Eyjafjallajökull volcano is located on a divergent plate boundary, specifically where the Mid-Atlantic Ridge intersects with a volcanic hot spot. This results in the formation of magma that rises to the surface, leading to volcanic activity. The eruption in 2010, which disrupted air travel in Europe, was caused by the interaction of the Eurasian and North American plates along this boundary.
It is geographically on the European plate.
Krakatau is located on a destructive plate boundary, where the Indo-Australian Plate is subducting beneath the Eurasian Plate. The subduction of the Indo-Australian Plate beneath the Eurasian Plate has led to volcanic activity in the region, including the eruption of Krakatau.
A convergent plate boundary is caused by a downward convection current in the mantle. At these boundaries, tectonic plates move towards each other, resulting in subduction zones or collision zones, where one plate is forced beneath the other.