geo.wikisort.org - Mountains

Search / Calendar

The Monarch is a 2,895-metre (9,498-foot) mountain summit located in the Ball Range of the Canadian Rockies in British Columbia, Canada. The Monarch is situated on the boundary between Kootenay National Park and Mount Assiniboine Provincial Park, four kilometres to the west side of the Continental Divide. Although not visible from roads, The Monarch is a prominent feature seen from the slopes above Sunshine Village ski resort. Its nearest higher peak is Mount Bourgeau, 10.35 km (6.43 mi) to the north-northeast.[1]

The Monarch
The Monarch
Highest point
Elevation2,895 m (9,498 ft)[1]
Prominence555 m (1,821 ft)[2]
Parent peakMount Brett (2984 m)[2]
ListingMountains of British Columbia
Coordinates51°03′05″N 115°50′54″W[3]
Geography
The Monarch
Location of The Monarch in British Columbia
The Monarch
The Monarch (Canada)
LocationBritish Columbia, Canada
DistrictKootenay Land District
Parent rangeBall Range,[1] Canadian Rockies
Topo mapNTS 82O4 Banff[3]
Geology
Age of rockCambrian
Type of rocksedimentary rock
Climbing
First ascent1913 Conrad Kain with Interprovincial Boundary Survey[2]
Easiest routeScrambling
The Monarch seen from Healy Pass
The Monarch seen from Healy Pass

History


The first ascent of the mountain was made in 1913 by Conrad Kain with Interprovincial Boundary Survey.[2] In a report by the Interprovincial Boundary Survey, the mountain is referred to as Monarch Mountain, a fine piece of mountain architecture dominating the Simpson Pass area.[4]

The mountain's name became official in 1924 when approved by the Geographical Names Board of Canada.[3]


Geology


The Monarch is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[5] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[6]


Climate


Based on the Köppen climate classification, the mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers.[7] Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from The Monarch drains into tributaries of the Simpson River, which is a tributary of the Vermilion River.


See also



References


  1. "The Monarch, British Columbia". Peakbagger.com. Retrieved 2019-11-10.
  2. "The Monarch". Bivouac.com. Retrieved 2018-12-05.
  3. "The Monarch". Geographical Names Data Base. Natural Resources Canada. Retrieved 2018-12-05.
  4. "The Monarch". PeakFinder.com. Retrieved 2019-11-10.
  5. 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.
  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.




Текст в блоке "Читать" взят с сайта "Википедия" и доступен по лицензии Creative Commons Attribution-ShareAlike; в отдельных случаях могут действовать дополнительные условия.

Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.

2019-2025
WikiSort.org - проект по пересортировке и дополнению контента Википедии