Results 1 to 10 of about 36 (30)

Chronology and Eruption Dynamics of the Historic∼1700 CE Eruption of Tseax Volcano, British Columbia, Canada [PDF]

Frontiers in Earth Science, 2022
Despite having relatively short timespans of eruptions, monogenetic volcanoes can pose significant risks to the nearby population. Here, we describe the ∼1700 CE eruption of Tseax volcano, British Columbia, which killed up to 2,000 people of the Nisga’a ...
Yannick Le Moigne, Glyn Williams-Jones, Nathalie Vigouroux, Nathalie Vigouroux, James K. Russell   +4 more
doaj   +7 more sources

Inflated pyroclasts in proximal fallout deposits reveal abrupt transitions in eruption behaviour. [PDF]

Nat Commun, 2022
During explosive eruption of low viscosity magmas, pyroclasts are cooled predominantly by forced convection. Depending on the cooling efficiency relative to other timescales, a spectrum of deposits can be formed.
Jones TJ, Le Moigne Y, Russell JK, Williams-Jones G, Giordano D, Dingwell DB.   +5 more
europepmc   +2 more sources

Physical volcanology of Tseax Volcano, British Columbia, Canada [PDF]

Journal of Maps, 2020
Tseax volcano erupted ∼ 250 years ago in NW British Columbia, Canada producing tephra deposits and lava flows. Field mapping has defined the stratigraphy of Tseax and the lava flow morphologies.
Yannick Le Moigne, Glyn Williams-Jones, Kelly Russell, Steve Quane   +3 more
doaj   +2 more sources

Determining the Volcanic Eruption Style of Tephra Deposits From Infrared Spectroscopy

Earth and Space Science, Volume 8, Issue 2, February 2021., 2021
Abstract Orbital imagery and spectroscopy at Mars have identified a variety of deposits potentially consistent with volcanic tephra formed during explosive volcanic eruptions, and some of these deposits may have formed due to water‐ or ice‐magma interactions during phreatomagmatic eruptions.
M. J. B. Henderson, B. H. N. Horgan, M. C. Rowe, K. T. Wall, N. A. Scudder   +4 more
wiley   +1 more source

Table1_Chronology and Eruption Dynamics of the Historic∼1700 CE Eruption of Tseax Volcano, British Columbia, Canada.docx

, 2022
Despite having relatively short timespans of eruptions, monogenetic volcanoes can pose significant risks to the nearby population. Here, we describe the ∼1700 CE eruption of Tseax volcano, British Columbia, which killed up to 2,000 people of the Nisga’a ...
Glyn Williams-Jones (1263795), James K. Russell (6810014), Nathalie Vigouroux (1263798), Yannick Le Moigne (8828729)   +3 more
core   +1 more source

The Cascadia megathrust earthquake of 1700 may have rejuvenated an isolated basalt volcano in western Canada: Age and petrographic evidence

, 2009
The basaltic Tseax flow is the product of one of only two eruptions in western Canada during the last thousand years. Reinterpretations of 14C and paleomagnetic data indicate that Tseax volcano last erupted between 1668 and 1714 CE.
Higgins, Michael D.
core   +1 more source

Enquête sur l'éruption volcanique la plus meurtrière du Canada et atténuation des risques futurs

, 2020
Monogenetic volcanoes are the most common volcanic landforms on Earth and usually form isolated small-volume volcanic centres with a wide range of eruptive styles and products.
Le Moigne, Yannick
core  

Vigouroux-Caillibot, Nathalie

currentPhD (SFU) MSc (Oregon University) BSc (McGill University) Douglas College Faculty Member since September 2013. Nathalie is a geologist who specializes in volcanology, geochemistry, and geothermal geology.

core  

Digital elevation model of the Tseax Volcano and lava flow, British Columbia

, 2014
S Tavakoli, R B Cocking, M Ulmi, C J Hickson   +3 more
openaire   +1 more source

Rethinking natural hazards research and engagement to include co-creation with Indigenous communities. [PDF]

NPJ Nat Hazards
Jones TJ, Nyce H, Le Moigne Y, Williams-Jones G, Nyce D.   +4 more
europepmc   +1 more source