Garibaldi Volcanic Belt facts for kids
The Garibaldi Volcanic Belt is the northern part of the Cascade Volcanic Belt. It is in British Columbia and the northwestern United States. Its volcanos are the most explosive in Canada.
The volcanoes are also the closest to British Columbia's densely populated southwest corner. These volcanoes are the result of subduction of the Juan de Fuca tectonic plate: the plates meet just seaward of the west coast of Vancouver Island. The volcanoes of the Garibaldi Volcanic Belt are stratovolcanoes typical of subduction zones, and include Mount Garibaldi, Mount Cayley and Mount Meager. Meager's eruption 2,350 years ago is the youngest explosive eruption in Canada. It was similar to that of Mount St. Helens in 1980 and the ongoing eruption of Montserrat in the Caribbean.
Images for kids
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North face of Mount Garibaldi. The Table is the flat-topped steep-sided edifice in the foreground rising above Garibaldi Lake.
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South face of Pyroclastic Peak, the second highest peak of the Mount Cayley massif.
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A volcanic hot spring near Meager Creek related to volcanism at the Mount Meager massif. This hot spring lies in one of the few hot spring clusters near Meager.
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The Table, a flow-dominated tuya rising above the southwestern side of Garibaldi Lake.
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Keyhole Falls, the largest waterfall along the Lillooet River. The solid-looking rock cliffs formed when a lava flow front repeatedly collapsed and collected downslope from the vent associated with the eruption of Plinth Peak 2,350 years ago.