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1 See also  





2 References  














White River Ash







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From Wikipedia, the free encyclopedia
 


The White River Ash is a 1,500-year-old tephra deposit found in the southern part of the Yukon Territory, Canada and eastern Alaska.[1] The deposit is bilobate,[2] formed by two large (VEI6) explosive eruptions from the stratovolcanoofMount Churchill that occurred around 850 AD and blanketed 340,000 km2 (130,000 sq mi).[3] While originally believed to only exist within North America, recent observations (2014) have found crypto-tephra from the eruption across northern Europe.

See also

[edit]

References

[edit]
  1. ^ Lerbekmo, J. F.; Campbell, F. A. (February 1969). "Distribution, composition, and source of the White River Ash, Yukon Territory". Canadian Journal of Earth Sciences. 6 (1): 109–116. doi:10.1139/e69-011. ISSN 0008-4077.
  • ^ Lerbekmo, J. F.; Campbell, F. A. (February 1969). "Distribution, composition, and source of the White River Ash, Yukon Territory". Canadian Journal of Earth Sciences. 6 (1): 109–116. doi:10.1139/e69-011. ISSN 0008-4077.
  • ^ West, K.D.; Donaldson, J.D. (2000). "Evidence for winter eruption of the White River Ash (eastern lobe), Yukon Territory". CGRG Bibliography of Canadian Geomorphology. The Canadian Geomorphology Research Group. Archived from the original on 2009-04-08. Retrieved 2007-07-09.

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  • Retrieved from "https://en.wikipedia.org/w/index.php?title=White_River_Ash&oldid=1218413992"

    Categories: 
    Volcanism of Alaska
    Volcanism of Yukon
    Volcanism of the Northwest Territories
    Holocene volcanism
    VEI-6 eruptions
    Volcanic eruptions in the United States
    Holocene Yukon
    Tephra deposits
    Alaska geography stubs
    Yukon geography stubs
    Northwest Territories geography stubs
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    Articles with short description
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