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The Finlay tephras are two tephra deposits in northern British Columbia, Canada. They take their name from the Finlay River and were deposited just before
Finlay_tephras
Massif in British Columbia, Canada
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
Heart_Peaks
magmatic cycle may have deposited the Finlay tephras. These are two 5-to-10-millimetre-thick (0.20-to-0.39-inch) tephra layers of phonolitic to trachytic
Volcanism of the Mount Edziza volcanic complex
Volcanism_of_the_Mount_Edziza_volcanic_complex
Volcanic complex in British Columbia, Canada
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
Level_Mountain
Stratovolcano in British Columbia, Canada
source of the Finlay tephras. These are two 5 to 10 mm (0.20 to 0.39 in) thick phonolitic to trachytic tephra layers in the Dease Lake and Finlay River areas
Hoodoo_Mountain
Geological member in British Columbia, Canada
form of rare microphenocrysts. It is compositionally distinct from the Finlay tephras which may have originated from Level Mountain, Hoodoo Mountain, Heart
Sheep_Track_Member
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