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Kostal Cone

Kostal Cone, also called Kostal Volcano and Fire Mountain, is a young cinder cone in Wells Gray Provincial Park in east-central British Columbia, Canada. It rises from the northeast shore of Kostal Lake in the Cariboo Mountains. With an elevation of 1,440 m (4,724 ft), Kostal Cone is one of the lowest volcanoes in the Wells Gray-Clearwater volcanic field.

Kostal Cone
Kostal Cone
Highest point
Elevation1,440 m (4,720 ft)
Prominence190 m (620 ft)
CoordinatesCA-BC 52°10′N 119°57′W / 52.167°N 119.950°W / 52.167; -119.950
Geography
DistrictKamloops Division Yale Land District
Parent rangeCariboo Mountains
Topo mapNTS 83D4 Murtle Lake
Geology
Age of rockHolocene
Mountain typeCinder cone
Last eruption1550 (?)

There has been activity at this site as recently as 7,600 years ago, though more likely less than 1,000 years ago. Kostal Cone is too young for the commonly used potassium-argon dating technique (usable on specimens over 100,000 years old), and no charred organic material for radiocarbon dating has been found. However, the uneroded structure of the cone with the existence of trees on its flanks and summit have it an area for dendrochronology studies, which reveals the growth of tree-ring patterns. Tree-growth data has revealed an age of 400 years for Kostal Cone,[1] making it the youngest volcano in the Wells Gray-Clearwater volcanic field and one of the youngest volcanoes in Canada.

Kostal Cone is made of fragmented and solidified lava called cinder and its summit contains a bowl-shaped crater. Kostal's cinders were ejected by lava fountain eruptions and accumulated around the volcano's vent in the shape of a cone when they fell back around its surroundings. Lava flows from Kostal's 400 BP eruption are basaltic in composition and forms a lava bed. It is an example of volcanic activity that has occurred in the Wells Gray-Clearwater volcanic field since the last glacial period; others include the Dragon's Tongue lava flow from Dragon Cone just north of Kostal Cone and the Flourmill Volcanoes north of Mahood Lake.

See also edit

References edit

  1. ^ Wood, Charles A.; Kienle, Jürgen, eds. (1990). Volcanoes of North America. Cambridge University Press. p. 137. ISBN 0-521-43811-X.
  • . Catalogue of Canadian volcanoes. Archived from the original on 2011-06-04.
  • "Wells Gray Murtle Lake Marine Guide" (PDF). BC Parks.
  • "Kostal Cone". BC Geographical Names.


kostal, cone, also, called, kostal, volcano, fire, mountain, young, cinder, cone, wells, gray, provincial, park, east, central, british, columbia, canada, rises, from, northeast, shore, kostal, lake, cariboo, mountains, with, elevation, lowest, volcanoes, well. Kostal Cone also called Kostal Volcano and Fire Mountain is a young cinder cone in Wells Gray Provincial Park in east central British Columbia Canada It rises from the northeast shore of Kostal Lake in the Cariboo Mountains With an elevation of 1 440 m 4 724 ft Kostal Cone is one of the lowest volcanoes in the Wells Gray Clearwater volcanic field Kostal ConeKostal ConeHighest pointElevation1 440 m 4 720 ft Prominence190 m 620 ft CoordinatesCA BC 52 10 N 119 57 W 52 167 N 119 950 W 52 167 119 950GeographyKostal ConeBritish Columbia CanadaDistrictKamloops Division Yale Land DistrictParent rangeCariboo MountainsTopo mapNTS 83D4 Murtle LakeGeologyAge of rockHoloceneMountain typeCinder coneLast eruption1550 This article includes a list of general references but it lacks sufficient corresponding inline citations Please help to improve this article by introducing more precise citations July 2011 Learn how and when to remove this message There has been activity at this site as recently as 7 600 years ago though more likely less than 1 000 years ago Kostal Cone is too young for the commonly used potassium argon dating technique usable on specimens over 100 000 years old and no charred organic material for radiocarbon dating has been found However the uneroded structure of the cone with the existence of trees on its flanks and summit have it an area for dendrochronology studies which reveals the growth of tree ring patterns Tree growth data has revealed an age of 400 years for Kostal Cone 1 making it the youngest volcano in the Wells Gray Clearwater volcanic field and one of the youngest volcanoes in Canada Kostal Cone is made of fragmented and solidified lava called cinder and its summit contains a bowl shaped crater Kostal s cinders were ejected by lava fountain eruptions and accumulated around the volcano s vent in the shape of a cone when they fell back around its surroundings Lava flows from Kostal s 400 BP eruption are basaltic in composition and forms a lava bed It is an example of volcanic activity that has occurred in the Wells Gray Clearwater volcanic field since the last glacial period others include the Dragon s Tongue lava flow from Dragon Cone just north of Kostal Cone and the Flourmill Volcanoes north of Mahood Lake See also editVolcanism of Western Canada List of volcanoes in CanadaReferences edit Wood Charles A Kienle Jurgen eds 1990 Volcanoes of North America Cambridge University Press p 137 ISBN 0 521 43811 X Kostal Cone Catalogue of Canadian volcanoes Archived from the original on 2011 06 04 Wells Gray Murtle Lake Marine Guide PDF BC Parks Kostal Cone BC Geographical Names nbsp This article about a location in the Cariboo Regional District Canada is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Kostal Cone amp oldid 1176988086, wikipedia, wiki, book, books, library,

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