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The geology of British Columbia is a function of its location on the leading edge of the North American continent. The mountainous physiography and the diversity of the different types and ages of rock hint at the complex geology , which is still undergoing revision despite a century of exploration and mapping.
A few years later, George Dawson surveyed the geology of the area, and his 1878 report to the Geological Survey of Canada used the spelling Tatlayoco. [3] Maps of British Columbia published in the 1880s and 1890s continued to use minor variations of Tatlahco Lake, [4] while many geological publications used Dawson's spelling of Tatlayoco. [5] [6]
The Quilchena fossil locality is dated to 51.5 ± 0.4 Ma corresponding to the Early Eocene Climatic Optimum (EECO), and is reconstructed as the warmest and wettest of the Early Eocene upland sites from the Okanagan Highlands of British Columbia and northern Washington State. Mean annual temperature (MAT) is estimated from leaf margin analysis ...
Beattie Peaks Formation (British Columbia) Show map of British Columbia The Beattie Peaks Formation is a geologic formation of Early Cretaceous ( Valanginian ) age in the Western Canada Sedimentary Basin that consists primarily of marine mudstone .
The Spectrum Range was labelled as the Rainbow Mountains on a BC Lands map published in 1929 which was followed by the renaming of the mountain range to the Spectrum Mountains in 1945. [3] In 1954, the form of the name was changed to the Spectrum Range in accordance to the Geological Survey of Canada memoir 247 published in 1948.
The Britannia Range is a small mountain range of the Coast Mountains that runs along the eastern shore of Howe Sound just north of Vancouver, British Columbia, Canada.It is a subrange of the Pacific Ranges and often considered part of the North Shore Mountains.
Clearwater Lake, a lava dammed lake in the Wells Gray-Clearwater volcanic field. Based on radiocarbon and potassium-argon dating, volcanic activity in the Wells Gray-Clearwater volcanic field began in the early Pleistocene epoch, creating valley-filling and plateau-capping lava flows that have a total volume of approximately 25 km 3 (6 cu mi). [6]
British Columbia has a large number of Indian Reserves which are outside the municipal and regional district systems and are self-governing by numerous band governments, most of which belong to tribal councils, which is an association of bands with common interests and not governments as such. Many bands claim sovereignty, having signed no ...
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