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Mount Price (British Columbia)

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38: 601: 442: 1058: 138: 1066: 959: 887: 713: 145: 1239: 816: 1225: 1085:, this wilderness park covers an area of 194,650 hectares (481,000 acres). Lying within its boundaries are a number of other volcanoes, such as Mount Garibaldi and The Black Tusk. Located 70 kilometres (43 miles) north of Vancouver in the glaciated Coast Mountains, Garibaldi Provincial Park contains diverse vegetation, iridescent waters and a rich geological history. The park also has abundant wildlife, such as squirrels, chipmunks, 763:, inclosing the volcano on its west and southwest sides. It is now almost completely filled up by Mount Price, but some small areas of its floor are exposed on the north side. The basin likely formed as a result of glacial action as its north side appears to have been almost certainly glaciated. It might otherwise have been attributed to 1205:, known as the Mount Price Trail or the Mount Price Route, commences past the ranger station. This poorly marked path ascends to the shore of Garibaldi Lake and then returns inland where it traverses south along the lava flow forming The Barrier. The terrain of this part of the route is relatively rough, involving substantial 1157:
who was a member of the Garibaldi Park Board at the time of the park's formation in 1927. Price was born at Vancouver in 1887 and was a member of a mountaineering party that had climbed Mount Garibaldi by a new route in 1908. Clinker Peak and Clinker Ridge were both officially named on September 12,
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million years ago and continued intermittently until sometime in the last 15,000 years. Although the mountain is not known to have been volcanically active for thousands of years, it could erupt again, which would potentially endanger the nearby populace. If this were to happen, relief efforts could
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has been established to monitor earthquakes throughout Canada, but it is too far away to provide an accurate indication of activity under the mountain. It may sense an increase in seismic activity if Mount Price becomes highly restless, but this may only provide a warning for a large eruption; the
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Daisy Lake Road, 30 kilometres (19 miles) north of Squamish, provides access to Garibaldi Provincial Park from Highway 99. At the end of this 2.5-kilometre-long (1.6-mile) road is the Rubble Creek parking lot from which the 9-kilometre-long (5.6-mile) Garibaldi Lake Trail extends to the Garibaldi
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lava. As a result, andesite lava flows typically move slower than basaltic lava flows and are less likely to travel as far from their source. Dacite and rhyolite lavas are normally too viscous to flow away from a volcanic vent, resulting in the formation of lava domes. An exception is the
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Tobratov, Sergei A.; Zheleznova, Olga S. (2020). "Experience of Large-Scale Analysis of the Spatial Patterns of Plain Forest Ecosystem Productivity and Biogeochemical Processes". In Frank-Kamenetskaya, Olga V.; Vlasov, Dmitry Yu.; Panova, Elena G.; Lessovaia, Sofia N. (eds.).
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Mount Price is one of the four highest threat volcanoes in Canada situated within close proximity to major populations with critical civil and economic infrastructure, the other three being Mount Meager, Mount Garibaldi and Mount Cayley. Although
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Wilson, A. M.; Russell, J. K. (2019). "Quaternary glaciovolcanism in the Canadian Cascade volcanic arc – Paleoenvironmental implications". In Poland, Michael P.; Garcia, Michael O.; Camp, Victor E.; Grunder, Anita (eds.).
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After the Cordilleran Ice Sheet retreated from higher elevations less than 15,000 years ago, andesite eruptions of the third eruptive phase occurred from a satellite vent at Price Bay. These eruptions resulted in the creation of a small
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about 300,000 years ago, volcanism of the second phase shifted westward and constructed the nearly symmetrical stratovolcano of Mount Price. Episodic eruptions during this phase of activity produced andesite and dacite lavas, as well as
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and interior continental climates dominates the Eastern Pacific Ranges Ecosection. It is characterized by little precipitation and mild temperatures due to Pacific air often passing over this area. During winter, cold
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The Clinker Peak lava flows were one of the first described occurrences of lava having been impounded by glacial ice. They were the subject of significant study by William Henry Mathews, a pioneer in the study of
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Russel, J. K.; Hickson, C. J.; Andrews, Graham (2007). "Canadian Cascade volcanism: Subglacial to explosive eruptions along the Sea to Sky Corridor, British Columbia". In Stelling, Pete; Tucker, David S. (eds.).
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and volcano-ice interactions in North America. In 1952, Mathews cited substantial evidence supporting the conclusion that the Clinker Peak lava flows ponded against glacial ice. This included the existence of
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Mount Price has had at least three names throughout its history. It was originally named Red Mountain for its red appearance, but the date when this name was adopted has not been cited. Another peak west of
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nearby and the relocation of residents to new recreational subdivisions away from the hazard zone. The area below and adjacent to The Barrier has since been referred to as the Barrier Civil Defence Zone by
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occur along the western margin of the Pacific Ranges Ecoregion. The Pacific Ranges Ecoregion is part of the Coast and Mountains Ecoprovince which forms part of the Humid Maritime and Highlands Ecodivision.
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currently converge at a rate of 3 to 4 centimetres (1.2 to 1.6 inches) per year, only about half the rate of convergence from seven million years ago. This slowed convergence likely accounts for reduced
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against the Cordilleran Ice Sheet when it still filled valleys at lower elevations. Age estimates for this final volcanic phase have varied from 15,000 years ago to as recently as 8,000 years ago.
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andesite lava flows. They are both at least 300 metres (980 feet) thick and 6 kilometres (3.7 miles) long, extending to the northwest and southwest. Their unusually large thickness is due to them
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are posted at the zone to make visitors aware of the potential danger and to minimize the chance of fatalities in the event of a slide. For safety reasons, BC Parks recommends visitors not to
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over boulders of the lava flow. Eventually the trail reaches open terrain north of Mount Price and approaches the base of the volcano. Climbing Mount Price or Clinker Peak involves
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on Mount Price's northern flank with an elevation of 1,788 metres (5,866 feet). Possibly contemporaneous volcanism occurred at Clinker Peak with the eruption of two hornblende-
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Wilson, Alexander M.; Kelman, Melanie C. (2021). Assessing the relative threats from Canadian volcanoes (Report). Geological Survey of Canada, Open File 8790.
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Mount Price attains an elevation of 2,049 metres (6,722 feet) and is one of several Garibaldi Belt volcanoes that have been volcanically active throughout the
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was created to outline the notification procedure of some of the main agencies that would respond to an erupting volcano in Canada, an eruption close to the
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million years; the oldest volcanic rocks are found at Mount Price and The Black Tusk. Several volcanic rocks with differing compositions are present in the
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system might detect activity only once the volcano has started erupting. If Mount Price were to erupt, mechanisms exist to orchestrate relief efforts. The
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in the past. The most recent major landslide in 1855–1856 resulted from failure along vertical rock fractures. It travelled 6 kilometres (3.7 miles) down
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are known in the Garibaldi area, there is evidence of anomalously high heat flow in Table Meadows just south of Mount Price and elsewhere.
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to declare the area immediately below it unsafe for human habitation in 1980. This led to the evacuation of the small resort village of
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between 15,000 and 8,000 years ago that ponded against glacial ice. These lava flows are structurally unstable, having produced large
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flows. The fragments are characterized by several sharp, jagged spines and are normally less than 150 millimetres (5.9 inches) wide.
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and flickers. Garibaldi Provincial Park is named after Mount Garibaldi, which is in turn named after the Italian patriot and soldier
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Anderson, Sean; Bryant, Leslie; Harris, Brian; Hoare, Jay; Hughes, Colin; Manyk, Mike; Mussio, Russell; Soroka, Stepan (2019).
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Because andesite is the main type of lava erupted from Mount Price, lava flows are a low to moderate hazard. Andesite is
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10 cubic feet) of rock. The southwest lava flow is in the upper reaches of the Culliton Creek valley and forms
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adopt the name Mount Price for this mountain after Thomas E. Price, a former mountaineer and engineer of the
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At least three phases of eruptive activity have been identified at Mount Price. The first eruptive phase 1.2
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on the southeastern flank of Mount Garibaldi, a length that is normally attained by basaltic lava flows.
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forests dominate nearly all the valleys and lower slopes of this ecosection, the upper slopes containing
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and the lack of an oceanic trench. The best evidence for ongoing subduction is the existence of active
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Floods, Faults, and Fire: Geological Field Trips in Washington State and Southwest British Columbia
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lies just above the subalpine forests, which is normally overlain by barren rock. Wildlife such as
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Evans, S.G.; Savigny, K.W. (1994). "Landslides in the Vancouver-Fraser Valley-Whistler region".
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in its vicinity. It lies within an ecological region that surrounds much of the Pacific Ranges.
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indicative of rapid quenching in meltwater or in water-soaked pyroclastic rocks under the ice.
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maps 92G and 92J in 1930 after a committee of the Garibaldi Park Board was set up to deal with
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are situated within the Eastern Pacific Ranges Ecosection, all of which are connected to the
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have not been identified at Mount Price, Peléan eruptions can also produce large amounts of
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Backpacking in Southwestern British Columbia: The Essential Guide to Overnight Hiking Trips
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Burwash, Edward M. (1914). "Pleistocene Vulcanism of the Coast Range of British Columbia".
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in Canada, Mount Price has a nearly symmetrical structure. Its western slope is flanked by
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Like other volcanoes in the Garibaldi Volcanic Belt, Mount Price formed as a result of
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Geology and Geological Hazards of the Vancouver Region, Southwestern British Columbia
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A prominent feature of the Clinker Peak lava flows are the levees that demarcate the
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on the south side of the valley of Garibaldi Lake. This basin consists of a wall of
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Geology and Geothermal Potantial of the AWA Claim Group, Squamish, British Columbia
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Mount Price is one of the three principal volcanoes in the southern segment of the
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Topographic map of the Garibaldi Lake area depicting Mount Price and adjacent peaks
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Several rivers flow through the Eastern Pacific Ranges Ecosection, including the
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Like other volcanoes in the Garibaldi Lake volcanic field, Mount Price is not
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who are prepared to notify people threatened by volcanic eruptions in Canada.
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Processes and Phenomena on the Boundary Between Biogenic and Abiogenic Nature
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Engineering Geology and Geomorphology of Glaciated and Periglaciated Terrains
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Quaternary Magmatism in the Cascades – Geologic Perspectives
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rivers on its western side and the Lillooet River in the middle. Coastal
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was identified as Red Mountain on a 1923 sketch by Canadian mountaineer
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Field Volcanology: A Tribute to the Distinguished Career of Don Swanson
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that could significantly affect the nearby communities of Whistler and
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to the Cheakamus River valley, depositing 30,000,000 cubic metres (1.1
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Mount Price is associated with a small group of volcanoes called the
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Mount Garibaldi with Mount Price and Clinker Peak in the left-centre
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stage, which spans the time between 774,000 and 129,000 years ago.
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stages, which together cover a timespan ranging from 2.58 to 0.774
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Lake campground and ranger station. A 5-kilometre-long (3.1-mile)
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become more serious as the Lower Mainland grows in population.
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1972, to retain Mount Price's earlier name, Clinker Mountain.
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15-kilometre-long (9.3-mile) Ring Creek dacite lava flow from
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between the Juan de Fuca and North American plates. These two
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is the current geologic epoch, which began 11,700 years ago.
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would also be at risk. Mount Price is also close to a major
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Dictionary Geotechnical Engineering / Wörterbuch GeoTechnik
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False colour image of Mount Price and associated lava flows
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Eyton, Taryn (2021). "Garibaldi Lake and Taylor Meadows".
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Concerns about The Barrier's instability due to volcanic,
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characterized by high, steep and rugged mountains made of
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and snow plodding; both peaks do not require scrambling.
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Pushing the Limits: The Story of Canadian Mountaineering
2148:"Garibaldi volcanic belt: Garibaldi Lake volcanic field" 1802:. International Commission on Stratigraphy. March 2020. 894:
on the right and the forested Price Bay dome on the left
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on its western flank, which was the source of two thick
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than basaltic lava but is less viscous than dacite or
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The Pacific Ranges Ecoregion is subdivided into seven
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An Introduction to the Ecoregions of British Columbia
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105 Hikes In and Around Southwestern British Columbia
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Volcanoes of North America: United States and Canada
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is downwind from Mount Price. An eruption producing
2109:West, Terry R.; Shakoor, Abdul (2018). "Minerals". 1073:Mount Price and its eruptive products lie within a 804:activity. Later, the volcano was overridden by the 2474: 2070: 1122:identified Mount Price as Clinker Mountain in the 1069:Garibaldi Lake with Mount Price behind on the left 572:are locally present. The communities of Whistler, 1590:Hui, Stephen (2018). "Hikes North of Vancouver". 1061:Mount Price with Garibaldi Lake in the foreground 616:. Mount Price is also part of the Garibaldi Lake 4290: 1302:is the current geologic period, which began 2.58 1997: 1388:is a dark green, black or brown mineral of the 822:is part of a thick lava flow that erupted from 787:on the floor of the cirque-like basin after an 1890: 4007: 2953: 2690: 2349:"Lava flows destroy everything in their path" 2254: 2187: 1423:"Garibaldi Lake: Synonyms & Subfeatures" 1038:Interagency Volcanic Event Notification Plan 379:Interagency Volcanic Event Notification Plan 2530:(8). American Journal of Science: 553–565. 2108: 1998:Martin, C. J.; Griffiths, James S. (2017). 4014: 4000: 2960: 2946: 1827: 1543: 1044:or any eruption that would affect Canada. 612:, the other two being Mount Garibaldi and 2569:. Butterworth & Company. p. 17. 2264: 1893:Volcano-Ice Interaction on Earth and Mars 1797:"International Chronostratigraphic Chart" 1544:Wood, Charles A.; Kienle, Jürgen (1990). 974:content, indicating that it has a higher 457:. A transitional climate between coastal 16:Stratovolcano in British Columbia, Canada 4023:Volcanoes of the Garibaldi Volcanic Belt 2597: 1714: 1621: 1064: 1056: 994:or heavy rainfall activity prompted the 957: 885: 814: 711: 599: 474:, which lies near the headwaters of the 440: 3803:List of communities in British Columbia 2516: 1968: 1927: 1891:Smellie, J. L.; Chapman, M. G. (2002). 4291: 2031: 2029: 2027: 2025: 2023: 1539: 1537: 1535: 1533: 1531: 1529: 1527: 1525: 1523: 1521: 3995: 2941: 2763: 2761: 2739: 2735: 2733: 2696:. GSA Special Papers. Vol. 538. 2512: 2510: 2472: 2436: 2434: 2183: 2181: 2179: 2177: 2142: 2140: 2138: 2136: 2134: 2132: 2130: 2035: 1809:from the original on October 27, 2021 1754: 1752: 1750: 1519: 1517: 1515: 1513: 1511: 1509: 1507: 1505: 1503: 1501: 1417: 1415: 1413: 1411: 1409: 1407: 1253:List of mountains of British Columbia 1161: 1033:Canadian National Seismograph Network 1031:to ascertain its activity level. The 748:has given the mountain a red colour. 372:. Mount Price began its formation 1.2 2564: 1791: 1789: 1787: 1785: 1710: 1708: 1706: 1704: 1665: 1663: 1661: 1659: 1617: 1615: 1613: 1611: 1585: 1583: 1581: 1579: 1577: 1468: 1466: 1464: 1462: 1460: 1458: 1456: 1454: 915:and most of the Lower Mainland. The 736:stratovolcano containing a breached 4299:Two-thousanders of British Columbia 2770:Vancouver, Coast & Mountains BC 2601:Topographical Map of Garibaldi Park 2567:Fundamentals of Engineering Geology 2381:. February 26, 2009. Archived from 2020: 1828:Woodsworth, Glenn J. (April 2003). 1589: 1149:. The committee requested that the 1133:The name Mount Price appeared on a 881: 826:between 15,000 and 8,000 years ago. 770: 144: 13: 2967: 2786: 2758: 2730: 2507: 2431: 2359:from the original on July 5, 2021. 2329:from the original on July 18, 2021 2174: 2127: 1770:from the original on July 16, 2021 1747: 1552:. pp. 113–114, 143–144, 148. 1498: 1404: 1118:. In 1952, Canadian volcanologist 854:. The northwest lava flow forms a 732:, a 1,983-metre-high (6,506-foot) 377:be organized by teams such as the 349:as recently as the 1850s. A large 14: 4345: 3841:Stein Valley Nlaka'pamux Heritage 2825: 2608:from the original on June 3, 2019 1782: 1701: 1675:. GSA Field Guides. Vol. 9. 1656: 1608: 1574: 1451: 939:and endanger water supplies from 520:forests and, to a lesser extent, 2772:. Mussio Ventures. p. 135. 2481:. Rocky Mountain Books. p.  2050:Geological Association of Canada 1237: 1223: 1195: 1047: 501:rivers on its eastern side, the 389:Mount Price is located south of 364:. This forms part of the larger 353:surrounds Mount Price and other 143: 136: 36: 2915:Catalogue of Canadian volcanoes 2862:Catalogue of Canadian volcanoes 2684: 2652: 2620: 2591: 2558: 2466: 2397: 2363: 2353:United States Geological Survey 2341: 2323:United States Geological Survey 2307: 2291:. April 2, 2009. Archived from 2273: 2248: 2218: 2158:. April 1, 2009. Archived from 2152:Catalogue of Canadian volcanoes 2102: 2064: 1991: 1962: 1921: 1884: 1868:. April 2, 2009. Archived from 1862:Catalogue of Canadian volcanoes 1850: 1821: 1633:United States Geological Survey 1379: 1362: 1333: 1309: 1292: 1279: 935:, threaten communities such as 254:Less than 1.2 million years old 4049:Salal Glacier volcanic complex 3946:Say Nuth Khaw Yum (Indian Arm) 2801:University of British Columbia 2415:. June 4, 2008. Archived from 2230:Government of British Columbia 2113:. Waveland Press. p. 25. 2111:Geology Applied to Engineering 1837:Government of British Columbia 1726:Government of British Columbia 1141:in 1928. It later appeared on 1114:on September 2, 1930, for its 1: 4314:Volcanoes of British Columbia 4309:Garibaldi Lake volcanic field 3846:Spruce Lake (South Chilcotin) 2698:Geological Society of America 1677:Geological Society of America 1398: 1372:is a synonymous term for the 1052: 1018: 626:Garibaldi Lake volcanic field 399:New Westminster Land District 362:Garibaldi Lake volcanic field 335:New Westminster Land District 193:New Westminster Land District 4334:Pleistocene British Columbia 2891:Geographical Names Data Base 2838:Geographical Names Data Base 2226:"Where do landslides occur?" 2086:10.1007/978-3-030-21614-6_18 2004:Geological Society of London 1897:Geological Society of London 1839:. p. 10. Archived from 1715:Demarchi, Dennis A. (2011). 1176:boulders in the lava flows, 962:Mount Price and Clinker Peak 779:million years ago deposited 751:Mount Price stands within a 707: 384: 157:Location in British Columbia 65:2,049 m (6,722 ft) 7: 4278:Watts Point volcanic centre 2523:American Journal of Science 1940:University of Chicago Press 1760:"Garibaldi Provincial Park" 1268:Volcanism of Western Canada 1258:List of volcanoes in Canada 1216: 1143:National Topographic System 1124:American Journal of Science 1042:Canada–United States border 1029:Geological Survey of Canada 921:Greater Vancouver watershed 429:. Several coastal islands, 119: 10: 4350: 2794:"Hut Management Plan 2019" 1975:Springer Berlin Heidelberg 1550:Cambridge University Press 1151:Geographic Board of Canada 791:glacial event. During the 595: 592:by a network of highways. 4329:Stratovolcanoes of Canada 4029: 3811: 3795: 3709: 3663: 3181: 2975: 2036:Green, Nathan L. (1990). 1969:Bucksch, Herbert (2013). 1858:"Garibaldi volcanic belt" 1263:List of Cascade volcanoes 1139:Garibaldi Provincial Park 1096: 755:-like basin cut into the 298: 286: 270: 258: 248: 243: 224: 210: 205:Garibaldi Provincial Park 198: 188: 176: 166: 130: 125: 113: 108: 69: 59: 54: 35: 28: 23: 4100:Franklin Glacier Complex 2919:Natural Resources Canada 2896:Natural Resources Canada 2866:Natural Resources Canada 2843:Natural Resources Canada 2598:Campbell, A. J. (1928). 2413:Natural Resources Canada 2379:Natural Resources Canada 2289:Natural Resources Canada 2257:Natural Resources Canada 2194:Natural Resources Canada 2156:Natural Resources Canada 1866:Natural Resources Canada 1428:Global Volcanism Program 1273: 1155:Canadian Pacific Railway 669:Cascadia subduction zone 1685:10.1130/2007.fld009(01) 1433:Smithsonian Institution 1083:Class A provincial park 1081:. Founded in 1927 as a 931:could destroy parts of 659:zone volcanism. As the 610:Garibaldi Volcanic Belt 393:on the western side of 366:Garibaldi Volcanic Belt 293:Garibaldi Volcanic Belt 4199:Monmouth Creek complex 3891:Princess Louisa Marine 2803:. 2019. Archived from 2371:"Monitoring volcanoes" 1931:The Journal of Geology 1622:Hildreth, Wes (2007). 1070: 1062: 1027:closely enough by the 963: 895: 827: 724:. In contrast to most 717: 605: 446: 304:15,000–8,000 years ago 93:49.91750°N 123.03556°W 2706:10.1130/2018.2538(06) 2665:BC Geographical Names 2633:BC Geographical Names 2544:10.2475/AJS.250.8.553 2447:BC Geographical Names 2196:. pp. 268, 270. 1479:BC Geographical Names 1120:William Henry Mathews 1068: 1060: 996:provincial government 961: 889: 818: 806:Cordilleran Ice Sheet 715: 603: 466:air invades from the 444: 4324:Quaternary volcanoes 4319:Subduction volcanoes 4242:Silverthrone Caldera 4131:Little Ring Mountain 2565:Bell, F. G. (1983). 2473:Scott, Chic (2000). 2419:on February 14, 2009 1318:is a green to black 1169:subglacial eruptions 702:Cascade Volcanic Arc 665:North American Plate 409:rocks. Much of this 370:Canadian Cascade Arc 98:49.91750; -123.03556 4255:Machmell River Cone 4136:Mount Meager massif 2744:. Greystone Books. 2536:1952AmJS..250..553M 2409:Volcanoes of Canada 2375:Volcanoes of Canada 2295:on February 2, 2009 2285:Volcanoes of Canada 1846:on January 9, 2022. 1594:. Greystone Books. 943:. Fisheries on the 845:ponding and cooling 812:of the Quaternary. 765:explosive volcanism 486:, which lie in the 89: /  42:Mount Price behind 4273:Tricouni Southwest 4248:Mount Silverthrone 4149:Capricorn Mountain 2315:Neal, Christina A. 2281:"Volcanic hazards" 2236:on August 18, 2010 1652:on March 26, 2009. 1370:Middle Pleistocene 1359:million years ago. 1322:mineral common in 1306:million years ago. 1174:glacially striated 1162:Geological studies 1091:Giuseppe Garibaldi 1071: 1063: 964: 896: 828: 793:Middle Pleistocene 783:andesite lava and 718: 677:continental margin 663:thrusts under the 661:Juan de Fuca Plate 606: 447: 55:Highest point 4286: 4285: 4142:Bridge River Vent 3989: 3988: 3916:Blackcomb Glacier 3836:Mount Elphinstone 3374:Frederick William 2810:on August 4, 2021 2042:Geoscience Canada 1343:is an unofficial 1341:Early Pleistocene 1328:metamorphic rocks 1104:Overlord Mountain 1077:called Garibaldi 1075:conservation area 949:air traffic route 901:Plinian eruptions 890:Mount Price with 798:pyroclastic flows 789:Early Pleistocene 785:pyroclastic rocks 744:of Mount Price's 638:basaltic andesite 530:Alpine vegetation 308: 307: 4341: 4304:Garibaldi Ranges 4257: 4250: 4226: 4207: 4193: 4186: 4179: 4172: 4165: 4158: 4151: 4144: 4120: 4113: 4079: 4072: 4070:Pyroclastic Peak 4016: 4009: 4002: 3993: 3992: 3976:Homathko Estuary 3906:Brandywine Falls 2962: 2955: 2948: 2939: 2938: 2934: 2932: 2930: 2925:on June 29, 2009 2921:. Archived from 2906: 2904: 2902: 2881: 2879: 2877: 2872:on June 28, 2009 2868:. Archived from 2853: 2851: 2849: 2820: 2819: 2817: 2815: 2809: 2798: 2790: 2784: 2783: 2765: 2756: 2755: 2737: 2728: 2727: 2688: 2682: 2681: 2679: 2677: 2672:on July 22, 2021 2668:. Archived from 2656: 2650: 2649: 2647: 2645: 2640:on July 22, 2021 2636:. Archived from 2624: 2618: 2617: 2615: 2613: 2595: 2589: 2588: 2562: 2556: 2555: 2514: 2505: 2504: 2480: 2470: 2464: 2463: 2461: 2459: 2454:on July 22, 2021 2450:. Archived from 2438: 2429: 2428: 2426: 2424: 2401: 2395: 2394: 2392: 2390: 2367: 2361: 2360: 2345: 2339: 2338: 2336: 2334: 2311: 2305: 2304: 2302: 2300: 2277: 2271: 2270: 2268: 2252: 2246: 2245: 2243: 2241: 2232:. Archived from 2222: 2216: 2215: 2185: 2172: 2171: 2169: 2167: 2144: 2125: 2124: 2106: 2100: 2099: 2068: 2062: 2061: 2033: 2018: 2017: 1995: 1989: 1988: 1966: 1960: 1959: 1925: 1919: 1918: 1888: 1882: 1881: 1879: 1877: 1872:on June 15, 2008 1854: 1848: 1847: 1845: 1834: 1825: 1819: 1818: 1816: 1814: 1808: 1801: 1793: 1780: 1779: 1777: 1775: 1756: 1745: 1744: 1742: 1740: 1734: 1723: 1712: 1699: 1698: 1667: 1654: 1653: 1651: 1645:. Archived from 1630: 1619: 1606: 1605: 1587: 1572: 1571: 1541: 1496: 1495: 1493: 1491: 1486:on July 22, 2021 1482:. Archived from 1470: 1449: 1448: 1446: 1444: 1439:on July 22, 2021 1435:. Archived from 1419: 1393: 1383: 1377: 1366: 1360: 1358: 1337: 1331: 1313: 1307: 1305: 1296: 1290: 1283: 1247: 1245:Mountains portal 1242: 1241: 1240: 1233: 1231:Volcanoes portal 1228: 1227: 953:volcanic hazards 882:Volcanic hazards 873: 778: 771:Volcanic history 628:. This includes 623: 522:Engelmann spruce 518:mountain hemlock 468:Central Interior 427:Washington state 419:British Columbia 417:in southwestern 413:encompasses the 375: 327:British Columbia 325:in southwestern 319:Garibaldi Ranges 219:Garibaldi Ranges 214: 183:British Columbia 147: 146: 140: 104: 103: 101: 100: 99: 94: 90: 87: 86: 85: 82: 40: 31:Clinker Mountain 21: 20: 4349: 4348: 4344: 4343: 4342: 4340: 4339: 4338: 4289: 4288: 4287: 4282: 4253: 4246: 4222: 4203: 4189: 4182: 4177:Perkin's Pillar 4175: 4168: 4161: 4156:Devastator Peak 4154: 4147: 4140: 4116: 4109: 4105:Mount Garibaldi 4075: 4068: 4025: 4020: 3990: 3985: 3871:Birkenhead Lake 3807: 3791: 3777:Powder Mountain 3705: 3659: 3177: 2971: 2966: 2928: 2926: 2909: 2900: 2898: 2884: 2875: 2873: 2856: 2847: 2845: 2831: 2828: 2823: 2813: 2811: 2807: 2796: 2792: 2791: 2787: 2780: 2766: 2759: 2752: 2738: 2731: 2716: 2700:. p. 141. 2689: 2685: 2675: 2673: 2660:"Clinker Ridge" 2658: 2657: 2653: 2643: 2641: 2626: 2625: 2621: 2611: 2609: 2596: 2592: 2577: 2563: 2559: 2515: 2508: 2493: 2471: 2467: 2457: 2455: 2440: 2439: 2432: 2422: 2420: 2403: 2402: 2398: 2388: 2386: 2385:on June 8, 2008 2369: 2368: 2364: 2347: 2346: 2342: 2332: 2330: 2312: 2308: 2298: 2296: 2279: 2278: 2274: 2253: 2249: 2239: 2237: 2224: 2223: 2219: 2204: 2186: 2175: 2165: 2163: 2162:on May 13, 2008 2146: 2145: 2128: 2121: 2107: 2103: 2096: 2080:. p. 324. 2078:Springer Nature 2069: 2065: 2034: 2021: 2014: 1996: 1992: 1985: 1977:. p. 308. 1973:. Vol. 1. 1967: 1963: 1926: 1922: 1907: 1899:. p. 202. 1889: 1885: 1875: 1873: 1856: 1855: 1851: 1843: 1832: 1826: 1822: 1812: 1810: 1806: 1799: 1795: 1794: 1783: 1773: 1771: 1758: 1757: 1748: 1738: 1736: 1735:on May 11, 2021 1732: 1721: 1713: 1702: 1695: 1668: 1657: 1649: 1643: 1628: 1620: 1609: 1602: 1588: 1575: 1560: 1542: 1499: 1489: 1487: 1472: 1471: 1452: 1442: 1440: 1421: 1420: 1405: 1401: 1396: 1384: 1380: 1367: 1363: 1356: 1347:that spans the 1338: 1334: 1314: 1310: 1303: 1297: 1293: 1284: 1280: 1276: 1243: 1238: 1236: 1229: 1222: 1219: 1198: 1180:relations with 1164: 1135:topographic map 1099: 1079:Provincial Park 1055: 1050: 1021: 884: 871: 810:glacial periods 776: 773: 738:volcanic crater 726:stratovolcanoes 710: 689:tectonic plates 621: 598: 511:western hemlock 505:, Squamish and 480:Mount Garibaldi 403:Coast Mountains 387: 373: 351:provincial park 238:Cheakamus River 212: 162: 161: 160: 159: 158: 155: 154: 153: 152: 148: 120:Thomas E. Price 97: 95: 91: 88: 83: 80: 78: 76: 75: 50: 30: 17: 12: 11: 5: 4347: 4337: 4336: 4331: 4326: 4321: 4316: 4311: 4306: 4301: 4284: 4283: 4281: 4280: 4275: 4270: 4265: 4260: 4259: 4258: 4251: 4239: 4237:Round Mountain 4234: 4229: 4228: 4227: 4215: 4210: 4209: 4208: 4196: 4195: 4194: 4187: 4180: 4173: 4166: 4159: 4152: 4145: 4133: 4128: 4123: 4122: 4121: 4114: 4102: 4097: 4092: 4087: 4082: 4081: 4080: 4077:Vulcan's Thumb 4073: 4061: 4056: 4051: 4046: 4041: 4036: 4034:The Black Tusk 4030: 4027: 4026: 4019: 4018: 4011: 4004: 3996: 3987: 3986: 3984: 3983: 3978: 3973: 3968: 3963: 3958: 3953: 3951:Pinecone-Burke 3948: 3943: 3938: 3933: 3928: 3926:Stawamus Chief 3923: 3918: 3913: 3908: 3903: 3898: 3893: 3888: 3883: 3878: 3873: 3868: 3863: 3858: 3853: 3851:Upper Lillooet 3848: 3843: 3838: 3833: 3828: 3823: 3817: 3815: 3809: 3808: 3806: 3805: 3799: 3797: 3793: 3792: 3790: 3789: 3784: 3779: 3774: 3769: 3764: 3759: 3754: 3749: 3744: 3739: 3737:Garibaldi Névé 3734: 3729: 3724: 3719: 3713: 3711: 3707: 3706: 3704: 3703: 3698: 3693: 3688: 3683: 3678: 3673: 3667: 3665: 3661: 3660: 3658: 3657: 3651: 3646: 3641: 3636: 3634:Vulcan's Thumb 3631: 3626: 3621: 3616: 3611: 3606: 3601: 3596: 3591: 3586: 3581: 3576: 3571: 3566: 3561: 3556: 3551: 3546: 3541: 3536: 3531: 3526: 3521: 3516: 3511: 3506: 3501: 3496: 3491: 3486: 3481: 3476: 3471: 3466: 3461: 3456: 3451: 3446: 3441: 3436: 3431: 3426: 3421: 3416: 3411: 3406: 3401: 3396: 3391: 3386: 3381: 3376: 3371: 3366: 3361: 3356: 3351: 3346: 3341: 3336: 3331: 3326: 3321: 3316: 3311: 3306: 3301: 3296: 3291: 3286: 3281: 3276: 3271: 3266: 3261: 3256: 3251: 3246: 3241: 3236: 3231: 3226: 3224:The Black Tusk 3221: 3216: 3211: 3206: 3201: 3196: 3191: 3185: 3183: 3179: 3178: 3176: 3175: 3170: 3165: 3160: 3155: 3150: 3145: 3140: 3135: 3130: 3125: 3120: 3115: 3110: 3105: 3100: 3095: 3090: 3085: 3080: 3075: 3070: 3065: 3060: 3055: 3050: 3045: 3040: 3035: 3030: 3025: 3020: 3015: 3010: 3005: 3000: 2995: 2990: 2985: 2979: 2977: 2973: 2972: 2969:Pacific Ranges 2965: 2964: 2957: 2950: 2942: 2936: 2935: 2911:"Clinker Peak" 2907: 2886:"Clinker Peak" 2882: 2854: 2827: 2826:External links 2824: 2822: 2821: 2785: 2779:978-1926806952 2778: 2757: 2751:978-1771646697 2750: 2729: 2715:978-0813795386 2714: 2683: 2651: 2628:"Clinker Peak" 2619: 2590: 2576:978-0408011693 2575: 2557: 2518:Mathews, W. H. 2506: 2492:978-0921102595 2491: 2465: 2442:"Fissile Peak" 2430: 2396: 2362: 2340: 2306: 2272: 2266:10.4095/328950 2259:. p. 50. 2247: 2217: 2203:978-0660157849 2202: 2173: 2126: 2120:978-1478635000 2119: 2101: 2095:978-3030216139 2094: 2063: 2019: 2013:978-1786203021 2012: 2006:. p. 33. 1990: 1984:978-3662033265 1983: 1961: 1948:10.1086/622148 1920: 1906:978-1862391215 1905: 1883: 1849: 1820: 1781: 1746: 1700: 1694:978-0813700090 1693: 1679:. p. 12. 1655: 1642:978-1411319455 1641: 1635:. p. 67. 1607: 1601:978-1771642873 1600: 1573: 1558: 1497: 1450: 1402: 1400: 1397: 1395: 1394: 1378: 1361: 1332: 1308: 1291: 1277: 1275: 1272: 1271: 1270: 1265: 1260: 1255: 1249: 1248: 1234: 1218: 1215: 1197: 1194: 1163: 1160: 1108:Neal M. Carter 1098: 1095: 1054: 1051: 1049: 1046: 1020: 1017: 917:catchment area 883: 880: 772: 769: 746:volcanic rocks 709: 706: 673:oceanic trench 648:. Although no 618:volcanic field 614:The Black Tusk 597: 594: 590:Lower Mainland 554:mountain goats 488:Squamish River 476:Lillooet River 415:Pacific Ranges 395:Garibaldi Lake 386: 383: 331:Garibaldi Lake 323:Pacific Ranges 306: 305: 302: 296: 295: 290: 284: 283: 274: 268: 267: 262: 256: 255: 252: 246: 245: 241: 240: 228: 222: 221: 216: 208: 207: 202: 200:Protected area 196: 195: 190: 186: 185: 180: 174: 173: 168: 164: 163: 156: 150: 149: 142: 141: 135: 134: 133: 132: 131: 128: 127: 123: 122: 117: 111: 110: 106: 105: 73: 67: 66: 63: 57: 56: 52: 51: 48:Panorama Ridge 44:Garibaldi Lake 41: 33: 32: 26: 25: 15: 9: 6: 4: 3: 2: 4346: 4335: 4332: 4330: 4327: 4325: 4322: 4320: 4317: 4315: 4312: 4310: 4307: 4305: 4302: 4300: 4297: 4296: 4294: 4279: 4276: 4274: 4271: 4269: 4266: 4264: 4261: 4256: 4252: 4249: 4245: 4244: 4243: 4240: 4238: 4235: 4233: 4232:Ring Mountain 4230: 4225: 4221: 4220: 4219: 4216: 4214: 4211: 4206: 4202: 4201: 4200: 4197: 4192: 4188: 4185: 4181: 4178: 4174: 4171: 4167: 4164: 4160: 4157: 4153: 4150: 4146: 4143: 4139: 4138: 4137: 4134: 4132: 4129: 4127: 4126:Glacier Pikes 4124: 4119: 4115: 4112: 4108: 4107: 4106: 4103: 4101: 4098: 4096: 4093: 4091: 4088: 4086: 4083: 4078: 4074: 4071: 4067: 4066: 4065: 4062: 4060: 4059:Cauldron Dome 4057: 4055: 4052: 4050: 4047: 4045: 4042: 4040: 4037: 4035: 4032: 4031: 4028: 4024: 4017: 4012: 4010: 4005: 4003: 3998: 3997: 3994: 3982: 3979: 3977: 3974: 3972: 3969: 3967: 3964: 3962: 3959: 3957: 3956:Shannon Falls 3954: 3952: 3949: 3947: 3944: 3942: 3939: 3937: 3936:Mount Seymour 3934: 3932: 3929: 3927: 3924: 3922: 3919: 3917: 3914: 3912: 3909: 3907: 3904: 3902: 3899: 3897: 3894: 3892: 3889: 3887: 3884: 3882: 3879: 3877: 3874: 3872: 3869: 3867: 3864: 3862: 3859: 3857: 3854: 3852: 3849: 3847: 3844: 3842: 3839: 3837: 3834: 3832: 3829: 3827: 3824: 3822: 3819: 3818: 3816: 3814: 3810: 3804: 3801: 3800: 3798: 3794: 3788: 3785: 3783: 3780: 3778: 3775: 3773: 3770: 3768: 3765: 3763: 3760: 3758: 3755: 3753: 3750: 3748: 3745: 3743: 3740: 3738: 3735: 3733: 3730: 3728: 3725: 3723: 3720: 3718: 3715: 3714: 3712: 3708: 3702: 3699: 3697: 3694: 3692: 3689: 3687: 3684: 3682: 3679: 3677: 3674: 3672: 3669: 3668: 3666: 3662: 3655: 3652: 3650: 3647: 3645: 3642: 3640: 3637: 3635: 3632: 3630: 3627: 3625: 3622: 3620: 3617: 3615: 3612: 3610: 3607: 3605: 3602: 3600: 3597: 3595: 3592: 3590: 3587: 3585: 3582: 3580: 3577: 3575: 3572: 3570: 3567: 3565: 3562: 3560: 3557: 3555: 3552: 3550: 3547: 3545: 3542: 3540: 3537: 3535: 3532: 3530: 3527: 3525: 3522: 3520: 3517: 3515: 3512: 3510: 3507: 3505: 3502: 3500: 3499:Petlushkwohap 3497: 3495: 3492: 3490: 3487: 3485: 3482: 3480: 3477: 3475: 3472: 3470: 3467: 3465: 3462: 3460: 3457: 3455: 3454:Middle Finger 3452: 3450: 3447: 3445: 3442: 3440: 3437: 3435: 3432: 3430: 3427: 3425: 3424:Little Finger 3422: 3420: 3417: 3415: 3412: 3410: 3407: 3405: 3402: 3400: 3397: 3395: 3392: 3390: 3387: 3385: 3382: 3380: 3377: 3375: 3372: 3370: 3367: 3365: 3362: 3360: 3357: 3355: 3352: 3350: 3347: 3345: 3342: 3340: 3337: 3335: 3332: 3330: 3327: 3325: 3322: 3320: 3317: 3315: 3312: 3310: 3307: 3305: 3304:Crevasse Crag 3302: 3300: 3297: 3295: 3292: 3290: 3287: 3285: 3282: 3280: 3277: 3275: 3274:Castle Towers 3272: 3270: 3267: 3265: 3262: 3260: 3257: 3255: 3252: 3250: 3247: 3245: 3242: 3240: 3237: 3235: 3232: 3230: 3227: 3225: 3222: 3220: 3217: 3215: 3212: 3210: 3207: 3205: 3202: 3200: 3197: 3195: 3192: 3190: 3187: 3186: 3184: 3180: 3174: 3171: 3169: 3166: 3164: 3161: 3159: 3156: 3154: 3151: 3149: 3146: 3144: 3141: 3139: 3136: 3134: 3131: 3129: 3126: 3124: 3121: 3119: 3116: 3114: 3111: 3109: 3106: 3104: 3101: 3099: 3096: 3094: 3091: 3089: 3086: 3084: 3081: 3079: 3076: 3074: 3071: 3069: 3066: 3064: 3061: 3059: 3056: 3054: 3051: 3049: 3046: 3044: 3041: 3039: 3036: 3034: 3031: 3029: 3026: 3024: 3021: 3019: 3016: 3014: 3011: 3009: 3006: 3004: 3001: 2999: 2996: 2994: 2991: 2989: 2986: 2984: 2981: 2980: 2978: 2974: 2970: 2963: 2958: 2956: 2951: 2949: 2944: 2943: 2940: 2924: 2920: 2916: 2912: 2908: 2897: 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Index

A lightly glaciated mountain rising above trees and a lake in the foreground.
Garibaldi Lake
Panorama Ridge
Elevation
Coordinates
49°55′03″N 123°02′08″W / 49.91750°N 123.03556°W / 49.91750; -123.03556
Etymology
Thomas E. Price
Mount Price is located in British Columbia
Canada
Province
British Columbia
New Westminster Land District
Protected area
Garibaldi Provincial Park
Parent range
Garibaldi Ranges
Topo map
NTS
92G14
Cheakamus River
Age of rock
Mountain type
Stratovolcano
Type of rock
Andesite
dacite
Volcanic belt
Garibaldi Volcanic Belt
Last eruption

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