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It is a convergent/destructive plate boundary.
Convergent means where plates are moving together. Divergent means where plates are moving apart.
The mantle is below the plates.
No, Nyiragongo is not located on a convergent plate boundary. It is situated within the East African Rift system, which is associated with a divergent plate boundary where the African Plate is splitting into two tectonic plates.
a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.Read more: What_is_the_difference_between_a_constructive_plate_boundary_and_a_destructive_plate_boundary
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
The Andes are a result of the convergent boundary between the Nazca and South American Plate.
a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.Read more: What_is_the_difference_between_a_constructive_plate_boundary_and_a_destructive_plate_boundary
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
The boundary between two plates moving together is called a convergent boundary. At convergent boundaries, one plate is usually subducted beneath the other, leading to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
The plate boundary for Unzen volcano is the subduction zone where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. This subduction zone is part of the larger convergent boundary between the Philippine Sea Plate and the Eurasian Plate.
Mountain-building is a result of continental collision, so destructive plate boundaries. One plate is destroyed by subduction below the other, which undergoes compression, buckling and uplift as the collision continues. This is happening at present in Asia, raising the Himalayan Mountains.