Ray Mountain is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Ray Mountain last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field. Lava from a conical vent on the southwest side of Ray Mountain flowed down Falls Creek for 6 or more miles almost to the outlet of Clearwater Lake.

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  • 2050
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  • 2050
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  • Ray Mountain is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Ray Mountain last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field. Lava from a conical vent on the southwest side of Ray Mountain flowed down Falls Creek for 6 or more miles almost to the outlet of Clearwater Lake.
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  • Ray Mountain
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  • 52.38333333 -120.20000000
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  • Ray Mountain is a subglacial mound in Wells Gray Provincial Park, British Columbia, Canada. Ray Mountain last erupted during the Pleistocene. It is part of the Wells Gray-Clearwater volcanic field. Lava from a conical vent on the southwest side of Ray Mountain flowed down Falls Creek for 6 or more miles almost to the outlet of Clearwater Lake.
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  • Ray Mountain
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  • 52.383335 (xsd:float)
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  • -120.199997 (xsd:float)
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  • Ray Mountain
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