To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Iskut volcanic field

From Wikipedia, the free encyclopedia

Iskut volcanic field
Iskut volcanic field is located in British Columbia
Iskut volcanic field
Iskut volcanic field
Location of the Iskut volcanic field
Highest point
PeakCinder Mountain
Elevation1,914 m (6,280 ft)
Coordinates56°33′53″N 130°37′35″W / 56.56472°N 130.62639°W / 56.56472; -130.62639
Geography
CountriesCanada and United States
Provinces/StatesBritish Columbia and Alaska
DistrictCassiar Land District
Parent rangeBoundary Ranges
Topo mapNTS 104B7 Unuk River
NTS 104B10 Snippaker Creek
NTS 104B14 Hoodoo Mountain
Geology
Age of rockPleistocene-to-Holocene
Mountain typeVolcanic field
Volcanic regionNorthern Cordilleran Province
Last eruption1904 (uncertain)[1]

The Iskut volcanic field is a group of volcanoes and lava flows on and adjacent to the AlaskaBritish Columbia border in the Boundary Ranges of the Coast Mountains. All the volcanoes in this volcanic field are situated in British Columbia along the Iskut and Unuk rivers and their tributaries, with lava flows having reached Alaska. The oldest volcanoes in the Iskut volcanic field are Little Bear Mountain and Hoodoo Mountain, which are 146,000 and 85,000 years old, respectively. Younger volcanic centres include Second Canyon, King Creek, Tom MacKay Creek, Snippaker Creek, Iskut Canyon, Cone Glacier, Cinder Mountain and Lava Fork, all of which formed in the last 70,000 years. All of the volcanoes are mafic in composition except for Hoodoo Mountain which consists of peralkaline rocks.[2] The latest volcanic eruption took place from the Lava Fork volcano in 1800, although an uncertain 1904 eruption is also attributed to this volcano.[1]

The name Iskut-Unuk River Cones is a nearly synonymous term for this volcanic field but it omits Hoodoo Mountain and Little Bear Mountain, the oldest volcanoes comprising the Iskut volcanic field.[2][3] The name for this area in the Tlingit language is Séxkhulé, referring to the time of Aan Galakhú (the World Flood) when people took refuge here from the rising flood waters.

YouTube Encyclopedic

  • 1/3
    Views:
    19 072
    12 056
    44 129
  • The Most Active Volcano in Canada; Iskut Unuk River Cones
  • The Active Volcano in Canada; Atlin Volcanic Field
  • The Active Volcano in Canada; Wells Gray Clearwater Volcanic Field

Transcription

See also

References

  1. ^ a b "Iskut-Unuk River Cones: Eruptive History". Global Volcanism Program. Smithsonian Institution. Archived from the original on 2021-04-03. Retrieved 2021-10-06.
  2. ^ a b Smellie, John L.; Edwards, Benjamin R. (2016). Glaciovolcanism on Earth and Mars: Products, Processes and Palaeoenvironmental Significance. Cambridge, England: Cambridge University Press. pp. 45, 46. doi:10.1017/CBO9781139764384. ISBN 1-107-03739-5.
  3. ^ Wood, Charles A.; Kienle, Jürgen (1990). Volcanoes of North America: United States and Canada. Cambridge, England: Cambridge University Press. pp. 128, 129. ISBN 0-521-43811-X.

External links


This page was last edited on 29 February 2024, at 18:18
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.