| The Tower | |
|---|---|
 West aspect, viewed from Tent Ridge | |
| Highest point | |
| Elevation | 3,117 m (10,226 ft) |
| Prominence | 618 m (2,028 ft) |
| Parent peak | Mount Bogart (3144 m) |
| Listing | Mountains of Alberta |
| Coordinates | 50°51′24″N 115°17′22″W / 50.85667°N 115.28944°W / 50.85667; -115.28944 |
| Geography | |
  The TowerLocation in Alberta
| |
| Country | Canada |
| Province | Alberta |
| Parent range | Kananaskis Range |
| Topo map | NTS 82J14 Spray Lakes Reservoir |
| Climbing | |
| First ascent | Unknown |
The Tower is the unofficial name for a large prominent peak that sits above Rummel Lake. It is located between Mount Engadine and Mount Galatea of the Kananaskis Range in Alberta, Canada.
Geology
The Tower 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.
Climate
Based on the Köppen climate classification, The Tower is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.
References
- "Topographic map of The Tower". opentopomap.org. Retrieved 2022-01-14.
- ^ "The Tower". Bivouac.com. Retrieved 2022-01-14.
- "The Tower". cdnrockiesdatabases.ca. Retrieved 2022-01-14.
- Belyea, Helen R. (1960). The Story of the Mountains in Banff National Park (PDF). parkscanadahistory.com (Report). Ottawa: Geological Survey of Canada. Archived (PDF) from the original on 2015-10-02. Retrieved 2019-09-13.
- Gadd, Ben (2008). Geology of the Rocky Mountains and Columbias.
- Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN 1027-5606.
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