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Round Mountain is an eroded volcanic outcrop in the Garibaldi Volcanic Belt in British Columbia, Canada, located 8 km southwest of Eanastick Meadows, 9 km (6 mi) east of Brackendale and 10 km (6 mi) south of Mount Garibaldi. It is the highpoint of Paul Ridge and is located in the southwest corner of Garibaldi Provincial Park. Round Mountain formed as a result of subduction of the Juan de Fuca Plate beneath the North American Plate, known as the Cascadia subduction zone. Round Mountain last erupted during the Pleistocene.

Round Mountain
Highest point
Elevation	1,646 m (5,400 ft)
Prominence	225 m (738 ft)
Coordinates	49°45′53.5″N 123°01′27.1″W
Geography
Location	British Columbia, Canada
District	New Westminster Land District
Parent range	Garibaldi Ranges
Topo map	NTS 92G14 Cheakamus River
Geology
Age of rock	Pleistocene
Mountain type	Outcrop
Last eruption	Pleistocene
Climbing
Easiest route	gravel road

See also

• Cascade Volcanoes
• Garibaldi Volcanic Belt
• List of volcanoes in Canada
• Volcanism of Canada
• Volcanism of Western Canada

External links

• Catalogue of Canadian volcanoes
• Canadian Mountain Encyclopedia

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