What is the Garibaldi Volcanic Belt?
Q: What is the Garibaldi Volcanic Belt?
A: The Garibaldi Volcanic Belt is the northern part of the Cascade Volcanic Belt located in British Columbia and the northwestern United States.
Q: Are the volcanoes in the Garibaldi Volcanic Belt explosive?
A: Yes, the volcanoes in the Garibaldi Volcanic Belt are the most explosive in Canada.
Q: Where is the location of Garibaldi Volcanic Belt relative to British Columbia?
A: Garibaldi Volcanic Belt is the closest to British Columbia's densely populated southwest corner.
Q: What is responsible for the formation of volcanoes in the Garibaldi Volcanic Belt?
A: The Garibaldi Volcanic Belt is a result of subduction of the Juan de Fuca tectonic plate, where the plates meet just seaward of the west coast of Vancouver Island.
Q: Which type of volcanoes are present in the Garibaldi Volcanic Belt?
A: The volcanoes in the Garibaldi Volcanic Belt are stratovolcanoes typical of subduction zones.
Q: What are some examples of volcanoes in the Garibaldi Volcanic Belt?
A: Some examples of volcanoes in the Garibaldi Volcanic Belt include Mount Garibaldi, Mount Cayley, and Mount Meager.
Q: What is significant about the eruption of Mount Meager?
A: The eruption of Mount Meager 2,350 years ago is the youngest explosive eruption in Canada, and it was similar to that of Mount St. Helens in 1980 and the ongoing eruption of Montserrat in the Caribbean.
