Named after Prime Minister Alexander Mackenzie, they are a northern continuation, 800 km long, of the eastern system of the Rocky Mountains, composed almost entirely of folded sedimentary strata. They consist of several ranges trending in a NW-SE orientation, straddling the greater part of the NWT-Yukon boundary. The main core, the Backbone Ranges, is a mass of peaks and ridges reaching a maximum height, in Mt Sir James MacBrien, of 2759 m, the highest peak in the NWT. The Mackenzie Mountains lie in the precipitation shadow of the Selwyn Mountains farther west and are relatively dry. The timberline is low, leaving their slopes bare and rock covered.
- MLA 8TH EDITION
- Finlayson, Douglas. "Mackenzie Mountains". The Canadian Encyclopedia, 23 May 2018, Historica Canada. https://www.thecanadianencyclopedia.ca/en/article/mackenzie-mountains. Accessed 15 October 2019.
- APA 6TH EDITION
- Finlayson, D., Mackenzie Mountains (2018). In The Canadian Encyclopedia. Retrieved from https://www.thecanadianencyclopedia.ca/en/article/mackenzie-mountains
- CHICAGO 17TH EDITION
- Finlayson, Douglas, "Mackenzie Mountains". In The Canadian Encyclopedia. Historica Canada. Article published February 07, 2006; Last Edited May 23, 2018. https://www.thecanadianencyclopedia.ca/en/article/mackenzie-mountains
- TURABIAN 8TH EDITION
- Finlayson, Douglas. The Canadian Encyclopedia, s.v. "Mackenzie Mountains", Last Edited May 23, 2018, https://www.thecanadianencyclopedia.ca/en/article/mackenzie-mountains
|Article by||Douglas Finlayson|
|Published Online||February 7, 2006|
|Last Edited||March 4, 2015|