Vermilion River, 70 km (from its headstream to its confluence with the Kootenay R), rises in the Continental Ranges on the BC-Alberta border at the N end of KOOTENAY NATIONAL PARK. Fed by Tokumm Cr, it drains in a southerly direction, eventually emptying into the Kootenay R. It takes its name from mineral springs, located 9 km SW of VERMILION PASS, where Indians obtained iron oxide for decorative purposes and body paint. For most of its length, the river is paralleled by the 105 km Banff-Windermere Hwy. Like many mountain rivers, the Vermilion features instances of potholing and abrasion.
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- MLA 8TH EDITION
- Evans, David. "Vermilion River". The Canadian Encyclopedia, 23 January 2014, Historica Canada. www.thecanadianencyclopedia.ca/en/article/vermilion-river. Accessed 27 May 2023.
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- APA 6TH EDITION
- Evans, D. (2014). Vermilion River. In The Canadian Encyclopedia. Retrieved from https://www.thecanadianencyclopedia.ca/en/article/vermilion-river
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- CHICAGO 17TH EDITION
- Evans, David. "Vermilion River." The Canadian Encyclopedia. Historica Canada. Article published February 07, 2006; Last Edited January 23, 2014.
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- TURABIAN 8TH EDITION
- The Canadian Encyclopedia, s.v. "Vermilion River," by David Evans, Accessed May 27, 2023, https://www.thecanadianencyclopedia.ca/en/article/vermilion-river
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CloseVermilion River
Article by | David Evans |
Published Online | February 7, 2006 |
Last Edited | January 23, 2014 |
Vermilion River, 70 km (from its headstream to its confluence with the Kootenay R), rises in the Continental Ranges on the BC-Alberta border at the N end of KOOTENAY NATIONAL PARK. Fed by Tokumm Cr, it drains in a southerly direction, eventually emptying into the Kootenay R.
Vermilion River, 70 km (from its headstream to its confluence with the Kootenay R), rises in the Continental Ranges on the BC-Alberta border at the N end of KOOTENAY NATIONAL PARK. Fed by Tokumm Cr, it drains in a southerly direction, eventually emptying into the Kootenay R.