convergent
Haiti is located on the boundary between the Caribbean Plate and the North American Plate. The Caribbean Plate is an oceanic plate, while the North American Plate is a continental plate. This tectonic boundary is part of the complex system of plate movements in the region.
Chances Peak, which is part of the Soufrière Hills volcano, is located on the Caribbean plate boundary in the Caribbean region. The volcano is situated at the convergent boundary where the Caribbean plate is being subducted beneath the North American plate.
The Aleutian Islands are located on the boundary between the Pacific Plate and the North American Plate, with the Pacific Plate subducting beneath the North American Plate. This tectonic boundary is part of the larger Ring of Fire region characterized by tectonic activity including earthquakes and volcanic eruptions.
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.
Mount Bachelor is located near the western edge of the North American Plate in the Cascade Range. This region is primarily influenced by the Cascadia Subduction Zone, where the Juan de Fuca Plate is being subducted beneath the North American Plate. This makes Mount Bachelor part of a convergent plate boundary.
There is a clearly defined boundary. Part of that boundary is called the San Andreas Fault.
Japan is at the meeting place of four tectonic plates: The Pacific Plate, The Eurasian Plates, The Philippine Plate, and the Okhotsk Plate (sometimes considered part of the North American Plate).
Mount Pelee is located on the Caribbean Plate boundary, specifically along the boundary between the Caribbean Plate and the North American Plate. This area is part of the Lesser Antilles subduction zone where the denser North American Plate is being subducted beneath the Caribbean Plate.
Dukono is a volcano located in Indonesia that is part of the Pacific Ring of Fire, a region known for frequent seismic and volcanic activity due to the movement of tectonic plates. The volcano sits on the boundary between the Eurasian Plate and the Pacific Plate, where the Pacific Plate is subducting beneath the Eurasian Plate, leading to the volcanic activity in the region.
Canada is on the North American plate, the eastern part of this plate extends to the mid-Atlantic ridge, however this is far from Canada. The western coast of Canada is a subduction zone for the most part with a small amount of the Queen Charolette fault towards the north. The subduction zone is called the Cascadia subduction zone.
actually it is not a plate boundary it is a fault a strike slip fault -les bois student014
Mount Ruapehu is located on a convergent boundary between the Australian Plate and the Pacific Plate. This tectonic setting is characterized by the subduction of the Pacific Plate beneath the Australian Plate, which contributes to volcanic activity in the region. Ruapehu is an active stratovolcano and is part of the Taupo Volcanic Zone in New Zealand, showcasing the geological processes associated with such boundaries.