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| {{Short description|Cinder cone in Canada}} | |||
| '''Prindle Volcano''' is an isolated ] located in eastern ], ], in the headwaters of the East Fork of the ]. The cone is fresh-looking and has a base approximately 900 meters wide. It is the northwesternmost expression of the ]. It is a basaltic cinder cone, with lava flows extending approximately 11 km, which erupted in the Pliocene approximately 176,000 years ago.<ref>Blondes et al 2007</ref> Rocks forming the Prindle Volcano occur within, and penetrated through, the ] which is a large region of mostly Paleozoic-Mesozoic metamorphosed and deformed sedimentary, volcanic, and intrusive rocks that are intruded by younger Cretaceous and Tertiary granitic rocks.<ref>http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Prindle%20Volcano</ref> Xenoliths contained in the volcano's ejecta provide a sample of lower crust material<ref>http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V6J-4PFDDY3-2&_user=10&_coverDate=03%2F31%2F2008&_rdoc=1&_fmt=high&_orig=search&_sort=d&_docanchor=&view=c&_searchStrId=1205837951&_rerunOrigin=google&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=8ff649358baf16465a9989e9feaa4ae3</ref> | |||
| '''Prindle Volcano''' is an isolated basaltic ] located in eastern ], ], in the headwaters of the East Fork of the ], approximately 80 kilometers northeast of ].<ref name=":0" /> The cone is fresh-looking and has a base approximately {{convert|900|m|yd|abbr=off}} wide. It is the northwesternmost expression of the ]. The cinder cone, and an approximately {{convert|11|km|mi||adj=on|abbr=off}} long lava flow which breached the margin of the cone, erupted in the ] approximately 176,000 years ago.<ref></ref> The lava flow extends to the southeast, then turns southwest and continues in a river valley.<ref name=":0">{{Cite book |last=Wood |first=Charles A. |url=https://books.google.com/books?id=eyDRib-FJh4C&dq=Prindle+Volcano&pg=PA109 |title=Volcanoes of North America: United States and Canada |date=1992-11-27 |publisher=Cambridge University Press |isbn=978-0-521-43811-7 |language=en}}</ref> | |||
| Rocks forming the Prindle Volcano occur within, and penetrated through, the ] which is a large region of mostly ]-] ] and deformed ], ], and ] rocks that are intruded by younger ] and ] ] rocks.<ref>{{cite web|url=http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Prindle%20Volcano |title=Prindle Volcano - Introduction |publisher=Avo.alaska.edu |date=2013-09-24 |access-date=2013-10-16}}</ref> ]s in the volcano's ejecta provide a sample of lower crust material.<ref>{{cite web|url=http://www.avo.alaska.edu/pdfs/P0550B_p115to119.pdf |title=Granulite and Peridotite Inclusions from Prindle Volcano, Yukon–Tanana Upland, Alaska |publisher=Avo.alaska.edu |access-date=2013-10-16}}</ref><ref>{{cite journal|title=Granulite facies xenoliths from Prindle volcano, Alaska: Implications for the northern Cordilleran crustal lithosphere |date=2008-03-31 |doi=10.1016/j.lithos.2007.07.016|volume=101|journal=]|pages=344–358|last1=Ghent |first1=Edward D. |last2=Edwards |first2=Benjamin R. |last3=Russell |first3=J.K. |last4=Mortensen |first4=James |issue=3–4 }}</ref> | |||
| ⚫ | ==References== | ||
| ⚫ | *{{gnis|1408309}} | ||
| ==See also== | ==See also== | ||
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| *] | *] | ||
| ⚫ | ==References== | ||
| ⚫ | {{Northern Cordilleran volcanoes}} | ||
| {{Reflist}} | |||
| ==External links== | |||
| ⚫ | *{{gnis|1408309}} | ||
| *{{cite gvp|name=Prindle|vn=315800|access-date=2021-06-28}} | |||
| ⚫ | {{Northern Cordilleran volcanoes}} | ||
| {{coord|63|42|54|N|141|37|44|W|display=title}} | {{coord|63|42|54|N|141|37|44|W|display=title}} | ||
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Latest revision as of 03:42, 31 December 2024
Cinder cone in CanadaPrindle Volcano is an isolated basaltic cinder cone located in eastern Alaska, United States, in the headwaters of the East Fork of the Fortymile River, approximately 80 kilometers northeast of Tok, Alaska. The cone is fresh-looking and has a base approximately 900 metres (980 yards) wide. It is the northwesternmost expression of the Northern Cordilleran Volcanic Province. The cinder cone, and an approximately 11-kilometre (6.8-mile) long lava flow which breached the margin of the cone, erupted in the Pleistocene approximately 176,000 years ago. The lava flow extends to the southeast, then turns southwest and continues in a river valley.
Rocks forming the Prindle Volcano occur within, and penetrated through, the Yukon–Tanana upland which is a large region of mostly Paleozoic-Mesozoic metamorphosed and deformed sedimentary, volcanic, and intrusive rocks that are intruded by younger Cretaceous and Cenozoic granitic rocks. Xenoliths in the volcano's ejecta provide a sample of lower crust material.
See also
References
- ^ Wood, Charles A. (1992-11-27). Volcanoes of North America: United States and Canada. Cambridge University Press. ISBN 978-0-521-43811-7.
- "Dating young basalt eruptions by (U-Th)/He on xenolithic zircons" Geology, v. 35 no. 1 p. 17-20, 2006 doi: 10.1130/G22956A.1
- "Prindle Volcano - Introduction". Avo.alaska.edu. 2013-09-24. Retrieved 2013-10-16.
- "Granulite and Peridotite Inclusions from Prindle Volcano, Yukon–Tanana Upland, Alaska" (PDF). Avo.alaska.edu. Retrieved 2013-10-16.
- Ghent, Edward D.; Edwards, Benjamin R.; Russell, J.K.; Mortensen, James (2008-03-31). "Granulite facies xenoliths from Prindle volcano, Alaska: Implications for the northern Cordilleran crustal lithosphere". Lithos. 101 (3–4): 344–358. doi:10.1016/j.lithos.2007.07.016.
External links
- U.S. Geological Survey Geographic Names Information System: Prindle Volcano
- "Prindle". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-28.
63°42′54″N 141°37′44″W / 63.71500°N 141.62889°W / 63.71500; -141.62889
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