Wells Gray-Clearwater

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  • Canada
  • Canada
  • Cinder cone(s)
  • 1550 CE
  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 52.33°N
  • 120.57°W

  • 2015 m
    6609 ft

  • 320150
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Wells Gray-Clearwater.



 Available Weekly Reports

There are no Weekly Reports available for Wells Gray-Clearwater.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1550 (?) Unknown Confirmed   Dendrochronology Kostal Cone
5650 BCE (?) Unknown Confirmed   Radiocarbon (uncorrected) Dragon Cone

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Campbell R B, 1961. Quesnel Lake, west half, British Columbia. Geol Surv Can Map, 3-1961.

Campbell R B, 1963. Quesnel Lake, east half, British Columbia. Geol Surv Can Map, 1-1963.

Campbell R B, 1967. Canoe River, west half, British Columbia. Geol Surv Can Map, 15-1967.

Campbell R B, Tipper H W, 1971. Geology of Bonaparte Lake map-area, British Columbia. Geol Surv Can Mem, 363: 1-100.

Davis N F G, 1930. Clearwater Lake area, British Columbia. Geol Surv Can Summary Rpt, Part A: 274-293.

Hickson C J, 1986. Quaternary volcanism in the Wells Grey-Clearwater area, east central British Columbia. Unpublished PhD thesis, Univ British Columbia, 357 p.

Hickson C J, Edwards B R, 2001. Volcanoes and Volcanic Hazards in Canada. In; Brooks G R (ed) {A Synthesis of Geological Hazards in Canada}, Geol Surv Can Bull, 548: 1-248.

Hickson C J, Soos A, Wright R, 1994. Catalogue of Canadian volcanoes. Geol Surv Canada Open-File Rpt.

Hickson C J, Souther J G, 1984. Late Cenozoic volcanic rocks of the Clearwater-Wells Gray area, British Columbia. Can J Earth Sci, 21: 267-277.

Holland S S, 1976. Landforms of British Columbia, a physiographic outline. Brit Columbia Dept Mines Petrol Resour Bull, 48: 1-138 (2nd printing).

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Metcalf P, 1987. Petrogenesis of Quaternary alkaline lavas in Wells Gray Provincial Park, B.C. and constraints on the petrology of the subcordilleran mantle. Unpublished PhD thesis, Univ Alberta, 395 p.

Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.

The Wells Gray-Clearwater volcanic field in the Quesnel Highland of east-central British Columbia contains basaltic cones and lava flows of early Pleistocene-to-Holocene age. Pleistocene deposits include plateau-capping lava flows, subglacial mounds and tuyas, and hyaloclastites. Buck Hill Cone was erupted during the latest Pleistocene during the waning stages of the Fraser glaciation. Holocene eruptions took place in the Spanish Creek, Ray Lake and Kostal Lake areas (Hickson and Souther, 1984), forming cinder cones and producing lava flows that traveled up to 14 km. A lava flow from Dragon cone is radiocarbon dated at about 7600 years ago, and flows from Flourmill, Kostal, and Spanish Lake Cones rest on glaciated bedrock without an intervening paleosol, suggesting an early Holocene age. The latest eruption took place from Kostal cone about 400 years ago (Hickson and Edwards, 2001).