Mount Robertson is a

mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher t ...

in the

Canadian Rockies The Canadian Rockies () or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, w ...

, standing astride the British Columbia-Alberta boundary between Palliser Pass and North Kananaskis Pass. The British Columbia side of the pass is in

Mount Assiniboine Provincial Park Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. History The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wo ...

. The mountain is named for Sir William Robertson (1860–1933), 1st Baronet,

Chief of the Imperial General Staff Chief of the General Staff (CGS) has been the title of the professional head of the British Army since 1964. The CGS is a member of both the Chiefs of Staff Committee and the Army Board; he is also the Chair of the Executive Committee of the A ...

from 1916 to 1918 during the

First World War World War I or the First World War (28 July 1914 – 11 November 1918), also known as the Great War, was a World war, global conflict between two coalitions: the Allies of World War I, Allies (or Entente) and the Central Powers. Fighting to ...

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Geology

Mount Robertson is composed of

sedimentary rock Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or de ...

laid down during the

Precambrian The Precambrian ( ; or pre-Cambrian, sometimes abbreviated pC, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of t ...

Jurassic The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. ...

periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the

Laramide orogeny The Laramide orogeny was a time period of mountain building in western North America, which started in the Late Cretaceous, 80 to 70 million years ago, and ended 55 to 35 million years ago. The exact duration and ages of beginning and end of the o ...

. The Haig Glacier, largest singular glacier in

Kananaskis Country Kananaskis Country (abbreviated: K-Country) is a multi-use area west of Calgary, Alberta, Canada in the Rocky Mountain Foothills, foothills and front ranges of the Canadian Rockies. Its western edge borders Banff National Park and the Alberta-Br ...

, lies to the south of the peak.

Climate

Based on the

Köppen climate classification The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (te ...

, Mount Robertson is located in a

subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of ...

with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

References

;Notes {{DEFAULTSORT:Robertson Three-thousanders of British Columbia Three-thousanders of Alberta Spray Mountains Kootenay Land District

Geology

Climate

See also

References