Coast Mountains | |
Range | |
![]() The Coast Mountains, including Mount Waddington (far background, centre) viewed from a distance
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Countries | Canada, United States |
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Province/States | British Columbia, Alaska, Yukon |
Part of | Pacific Cordillera |
Highest point | Mount Waddington |
- elevation | 4,019 m (13,186 ft) |
- coordinates | |
The Coast Mountains are a mountain range of the Pacific Cordillera, running along the north western shore of the North American continent, extending south from the Alaska Panhandle and covering most of coastal British Columbia. They are part of a larger grouping, the Pacific Coast Ranges, which includes the Alaska Range, the Chugach Mountains, the Saint Elias Mountains, the Cascade Range, the Sierra Nevada and the Sierra Madre Occidental in Mexico.
The Coast Mountains are approximately 1600 km long and average 200 km in width. Its southern and southeastern boundaries are described by the Fraser River and the Interior Plateau. North of the Nechako Diversion, the Coast Mountains are flanked on the inland side by the Hazelton Mountains, the Skeena Mountains, the Stikine Plateau and the Tahltan and Tagish Highlands. Its far northwestern edge is delimited by the Kelsall River at the north end of the Alaska Panhandle, beyond which are the Saint Elias Mountains.
Covered in dense temperate rainforest on its western exposures, the range rises to heavily glaciated peaks, including the largest temperate-latitude icefields in the world. It then tapers to the dry interior plateau on its eastern flanks, or to the subarctic boreal forest of the Skeena Mountains and Stikine Plateau.
Mount Waddington, at 4,019 metres (13,186 ft), is the highest peak in the Coast Mountains and also the highest peak entirely within British Columbia.
Although the Coast Mountains are commonly considered to be the westernmost range of the Pacific Cordillera, the Insular Mountains are the true westernmost range,[1] which includes Vancouver Island and the Queen Charlotte Islands.
The largest icefield in the Coast Mountains is the Ha-Iltzuk Icefield.
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The Coast Mountains has its origins with a formerly active volcanic arc, called the Coast Range Arc, which began forming about 100 million years ago. Over millions of years, the volcanoes of the Coast Range Arc had their summits worn down and isostatic rebound has caused their solidified magma chambers to rise, forming the Coast Mountains.
During the early to middle Miocene, the Coast Mountains were favored thermally-driven uplift arising from the Miocene passage of the Anahim hotspot beneath the range, and response to convergence in late Miocene-Pliocene time.
Mountain/Peak | Height (metres) | Prominence (metres) | Location |
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Mount Waddington | 4019 | 3289 | |
Monarch Mountain | 3555 | 2930 | |
Razorback Mountain | 3183 | 2253 | |
Skihist Mountain | 2968 | 2463 | |
Mount Ratz | 3090 | 2430 | |
Mount Queen Bess | 3298 | 2355 | |
Wedge Mountain | 2892 | 2249 | |
Otter Mountain | 2692 | 2242 | |
Mount Silverthrone | 2860 | 974 | |
Kwatna Peak | 2290 | 2225 | |
Scud Peak | 2987 | 2172 |
The Coast Mountains are subdivided into numerous mountain ranges:
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