Victoria british columbia dating
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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.The Columbia Mountains consist of three parallel north–south ranges (Purcell, Selkirk and Monashee) with sharp peaks of 2,000–3,000 m separated by long, narrow valleys occupied by Kootenay Lake and the Columbia River.
Regions British Columbia has two main regions, often called "the Coast" and "the Interior." These two regions both have numerous contrasts and variations within them.The so-called "Lower Mainland," dominated by metropolitan Vancouver, contains over 60 per cent of the province's population and is its commercial, cultural and industrial centre.A slightly broader region, sometimes called the “Georgia Strait” region, includes Victoria and the southeast coast of Vancouver Island; this area holds approximately 20 per cent of the population.The vast interior is dominated by parallel mountain ranges and its population spreads north–south along valleys, notably the Okanagan and the Kootenay.Population centres are dispersed, as at Kamloops and Prince George in the interior, Prince Rupert and Kitimat on the northern coast, and Dawson Creek and Fort St. Each of these towns are centres of separate sub-regions and depend more on world markets than local markets.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 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.
In the southern Rockies the sharp, jagged sedimentary rock peaks from the Palaeozoic era (542 to 251 million years ago) differ from the older more rounded, lower peaks of Proterozoic era (2.5 billion to 542 million years ago) to the north.
The Rocky Mountains terminate south of the The western boundary of the Rocky Mountains is the narrow Rocky Mountain Trench — the longest valley in North America, extending for 1,400 km from Montana to the Yukon and along the length of BC.
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.