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Finlay tephras information


Finlay tephras
VolcanoUnknown volcano(es) in the Northern Cordilleran Volcanic Province
Date10,220-10,560 years ago
TypeTephra deposits
LocationBritish Columbia, Canada

The Finlay tephras are two tephra deposits in northern British Columbia, Canada. They take their name from the Finley River and were deposited just before 10,220–10,560 years ago. The source for the two tephra deposits is unknown but were likely erupted during two closely spaced periods of volcanism at one or two volcanoes associated with the Northern Cordilleran Volcanic Province.[1] Volcanoes suggested to have erupted the tephras include Hoodoo Mountain, Heart Peaks, the Mount Edziza volcanic complex and Level Mountain.[1]

  1. ^ a b "Holocene tephras in lake cores from northern British Columbia, Canada" (PDF). Archived from the original (PDF) on 2011-07-18. Retrieved 2010-07-12.

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Finlay tephras

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The Finlay tephras are two tephra deposits in northern British Columbia, Canada. They take their name from the Finley River and were deposited just before...

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Heart Peaks

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have a similar chemistry to the glass composition of the Finlay tephras. However, no tephras or pyroclastic rocks have been found at Hoodoo Mountain that...

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Sheep Track Member

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form of rare microphenocrysts. It is compositionally distinct from the Finlay tephras which may have originated from Level Mountain, Hoodoo Mountain, Heart...

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Hoodoo Mountain

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the Finlay tephras. These are two 5-to-10-millimetre-thick (0.20-to-0.39-inch) phonolitic to trachytic tephra layers in the Dease Lake and Finlay River...

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Level Mountain

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the mountain. Two tephra deposits, collectively known as the Finlay tephras, occur in organic-rich mud in the Dease Lake and Finlay River areas. They...

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Bowie Seamount

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24 km (15 mi) wide. Its flat-topped summit is made of weakly consolidated tephra and consists of two terraces. The lowest terrace is about 230 m (750 ft)...

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