Mount Lyell is a mountain on the Alberta–British Columbia border in western Canada. Comprising five distinct summits, Mount Lyell reaches a height of 3,498 m (11,476 ft).[1] The mountain was named by James Hector in 1858 in recognition of Scottish geologist Sir Charles Lyell.[4]
| Mount Lyell | |
|---|---|
 Mt. Lyell & its 5 subpeaks, plus the Lyell Icefield, taken from Mt. Forbes (Columbia Icefield peaks on the horizon - click image for more details) | |
| Highest point | |
| Elevation | 3,498 m (11,476 ft)[1][2] |
| Prominence | 1,078 m (3,537 ft)[3] |
| Parent peak | Mount Forbes |
| Listing | |
| Coordinates | 51°57′24″N 117°06′12″W / 51.95667°N 117.10333°W[4] |
| Geography | |
  Mount Lyell  Mount Lyell  Mount Lyell | |
 | |
| Interactive map of Mount Lyell | |
| Country | Canada |
| Provinces | Alberta and British Columbia |
| Parent range | Lyell Group, Central Icefields Canadian Rockies |
| Topo map | NTS 82N14 Rostrum Peak |
| Climbing | |
| First ascent | 1902, James Outram, guided by Christian Kaufmann[5] |
Geography
editMount Lyell is located on the Great Divide, which forms the BC-Alberta boundary in this area, in Banff National Park. Collectively, the five peaks, and the Mt. Lyell massif itself, are commonly referred to as 'the Lyells'.[3] The mountain is the highest in the Lyell Group, a subrange of the Central Icefields in the Canadian Rockies.[6]
In 1972, five distinct peaks on Mt. Lyell (formerly referred to as only Lyell 1 through 5 or L1 through L5), were named after Swiss mountain guides who settled in Golden, British Columbia in 1912. Running south to north along the interprovincial boundary, these peaks are: Christian Peak (L5), Walter Peak (L4), and Ernest Peak (L3), named after Christian Hässler, Walter Feuz and Ernest Feuz. Located entirely in Alberta are Edward Peak (L2) and Rudolph Peak (L1), named after Edward Feuz Jr. and Rudolph Aemmer.[4]
Mount Lyell marks the limit between the South Saskatchewan and Columbia watersheds.
Geology
editMount Lyell is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[7] The Lyell Formation is named after Mount Lyell.[8] Geology for all five subpeaks is identical due to their proximity to the central peak (maximum distance: 1.6 km or 1 mile).
Climate
editBased on the Köppen climate classification, Mount Lyell is located in a subarctic climate with cold, snowy winters, and mild summers.[9] Temperatures can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F).
Gallery
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Mount Lyell 1, 2 & 3 from the Columbia Icefield
See also
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References
edit- ^ a b Jones, David J. (2018). The Climbers Guide to the Rocky Mountains of Canada, Vol. Three: Rockies West. Golden, B.C.: Thin Gruel Press. pp. 208–209. ISBN 978-1-7753241-0-2.
- ^ "Topographic map of Mount Lyell". opentopomap.org. Retrieved 2022-07-04.
- ^ a b "Mount Lyell". Bivouac.com. Retrieved 2009-01-02.
- ^ a b c "Mount Lyell". BC Geographical Names. Retrieved 2009-02-28.
- ^ "Mount Lyell". cdnrockiesdatabases.ca. Retrieved 2019-08-19.
- ^ "Mount Lyell, Alberta/British Columbia". Peakbagger.com. Retrieved 2014-02-02.
- ^ Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
- ^ Gadd, Ben (1986). Handbook of the Canadian Rockies. Jasper: Corax Press. pp. 106–108.
- ^ Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606.