Well, darling, a constructive plate boundary is where two tectonic plates are moving away from each other. It's like a little separation party happening beneath the Earth's surface. This movement can result in the formation of new crust as magma rises up to fill the gap, creating some fresh real estate for those plates to chill on.
The Divergent Boundaries.
Mount Pinatubo is on a destructive plate boundary; it is above a subduction zone
A tsunami usually occurs on a destructive plate boundary.
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.
It is a transform boundary.
No, Iceland is on a constructive plate boundary.
mt Popocatépetl is a divergent plate boundary also known as a constructive boundary or an extensional boundary
A constructive plate boundary, as it pushes land upwards (which formed the mountains)
The Divergent Boundaries.
Mount Pinatubo is on a destructive plate boundary; it is above a subduction zone
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
A tsunami usually occurs on a destructive plate boundary.
Its to do with the viscosity of the lava, the thicker (more viscous) the lava the slower and less far it will travel making a shield volcano. This happens on a constructive plate boundary. on a destructive plate boundary the lava is less viscous and runs further making a conical shaped volcano
they are mainly conservative plate boundaries but can be all but constructive plate boundarys by callum 11
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.
destructive i do believe
a constructive plate boundary is where two plates move apart from eachother forming a gap which allows magma to rise and that leads to a earthquake.