The Watchtower
Elevation2791 m
Prominence651 m
RangeMaligne Range
Canadian Rockies
Parent peakMount Kerkeslin (2984  m)[1]
ListingMountains of Alberta
CountryCanada
ProvinceAlberta
Coordinates52°49′24″N 117°50′30″W
TopoNTS [2]
RockSedimentary rock
AgeCambrian
First ascent1951 R.K. Irvin, J. Mowat, R. Strong[3]
Easiest routeClimbing

The Watchtower is a 2,791-metre (9,157-foot) mountain summit located in the Maligne River valley of Jasper National Park, in the Canadian Rockies of Alberta, Canada. It is situated in the Maligne Range[4] and is visible from the Maligne Lake Road where it towers over Medicine Lake. Its nearest higher peak is Sirdar Mountain, 11.64 km (7.23 mi) to the north.[4]

History

The mountain was named in 1916 by Morrison P. Bridgland (1878-1948), a Dominion Land Surveyor who named many peaks in Jasper Park and the Canadian Rockies.[5][3] The mountain's name was officially adopted in 1947 when approved by the Geographical Names Board of Canada.[2]

The first ascent of The Watchtower was made in 1951 by R.K. Irvin, J. Mowat, and R. Strong.[1]

Geology

The Watchtower is composed of sedimentary rock laid down during the Cambrian period and pushed east and over the top of younger rock during the Laramide orogeny.[6]

Climate

Based on the Köppen climate classification, The Watchtower is located in a subarctic climate zone with long, cold, snowy winters, and mild summers.[7] Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from the mountain drains into Excelsior Creek and Watchtower Creek, both tributaries of the Maligne River which in turn empties into the Athabasca River.

See also

References

  1. ^ 444. Retrieved 2019-04-04.
  2. ^ IAOZD. Retrieved 2019-04-04.
  3. ^ 1497. Retrieved 2021-03-01.
  4. ^ 4536. Retrieved 2021-03-22.
  5. ^
  6. ^ Gadd, Ben (2008), "Geology of the Rocky Mountains and Columbias"
  7. ^ 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