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The region is a basin or watershed, because it is surrounded by higher mountains.Many of the rocks are lavas of Cretaceous and Tertiary (65.5 million to 2.6 million years ago) geological ages with apparently little mineralization except around the plateau edges.The rocks are mostly granitic intrusions of Cretaceous and Tertiary ages and there are some recent volcanoes.The lower Coast Mountains (1,500–2,000 m) near the Skeena River increase in altitude to the north.The western section of the province’s mountain ranges consists of the Coast Mountains along the coast and the offshore Insular Mountains.The northern end of the Cascade Mountains of Washington State terminates at the Fraser River, and then the high, snow and ice-covered peaks of the Coast Mountains extend northward along the Alaskan Panhandle into the Yukon.The Peace River Lowland of the northeast is actually an extension of the Interior Plains and more closely resembles neighbouring Landforms, Geology and Drainage The Cordilleran mountain system of western North America covers most of British Columbia, except for the Peace River area in the northeast.The Rocky Mountains rise abruptly about 1,000–1,500 m above the foothills of Alberta, and some of their snow- and ice-covered peaks tower more than 3,000 m above sea level; the highest peak in the Canadian Rockies, Mount Robson, west of Jasper, AB, is 3,954 m.

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The highest peak on Vancouver Island is the Golden Hinde, at 2,200 m.British Columbia is Canada's most westerly province, and is a mountainous area whose population is mainly clustered in its southwestern corner.BC is Canada’s third-largest province after Québec and Ontario, making up 10 per cent of Canada’s land surface.British Columbia is a land of diversity and contrast within small areas.Coastal landscapes, characterized by high, snow-covered mountains rising above narrow fjords and inlets, contrast with the broad forested upland of the central interior and the plains of the northeast.Much of the development of resource-based economic activity in the province has been concerned with linking these separate regions together into a broader provincial economy.The northern half of the province is virtually uninhabited north of Prince Rupert and is cut off from the Pacific Ocean by the Alaska Panhandle.The highest peak in BC, Fairweather Mountain (4,663 m), straddles the Alaska border in the St Elias Mountains just northwest of the Coast Mountains.Only three major rivers have cut through the barrier of the Coast Mountains: the Fraser, Skeena and Stikine.Out of the trench flow the headwaters of the Kootenay, Columbia, Fraser, Parsnip, Finlay, Kechika and Liard rivers, each separated from the others by low drainage divides.Two other mountain systems lie west of the Rocky Mountain Trench: the Columbia Mountains to the south; and the Cassiar-Omineca Mountains to the north.


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