White River Ash
The White River Ash is a 1,200-year-old ash deposit. It was formed by two large (VEI 6) explosive eruptions from the stratovolcano of Mount Churchill that occurred around 850 AD and blanketed 340,000 km2 (130,000 sq mi) of Yukon and Northwest Territories, Canada and the U.S. state of Alaska with ash.[1]
See also[]
References[]
- ^ 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.
Transatlantic distribution of the Alaskan White River Ash
 | This Alaska location article is a stub. You can help Wikipedia by . |
 | This article about a Yukon location is a stub. You can help Wikipedia by . |
 | This Canadian Northwest Territories location article is a stub. You can help Wikipedia by . |
Categories:
- Volcanism of Alaska
- Volcanism of Yukon
- Volcanism of the Northwest Territories
- Holocene volcanism
- VEI-6 eruptions
- Volcanic eruptions in the United States
- Alaska geography stubs
- Yukon geography stubs
- Northwest Territories geography stubs