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Anyox, British Columbia. Anyox was a small company-owned mining town in British Columbia, Canada. [1] Today it is a ghost town, abandoned and largely destroyed.It is located on the shores of Granby Bay in coastal Observatory Inlet, about 60 kilometres (37 miles) southeast of (but without a land link to) Stewart, British Columbia, and about 20 kilometres (12 miles), across wilderness east of ...
Mountain ranges in the province of British Columbia, in Western Canada For individual mountains and peaks, see Category: Mountains of British Columbia . By province
officially Kemess South is only producer; Kemess West and Rat 1 are Showings, Kemess North is a developed prospect [39] [40] Kitsault Mine: Mo, Ag, Pb, Zn, Cu, W: Kitsault/Alice Arm (near Anyox) Alice Arm, Observatory Inlet: Amax 1967–1972/1982 [41] Lenora Mine
Eagle Mountain, also known as Eagle Ridge, [1] is the mountainous ridge with many indistinct summits between Buntzen Lake and Coquitlam Lake near Coquitlam, British Columbia. Its proximity to Coquitlam, and the houses being built on its southern slopes (known as Westwood Plateau ), make it a very popular weekend destination for hiking ...
Sandon is in the foothills of the Selkirk Mountains in the West Kootenay region of southeastern British Columbia. The near ghost town lies off BC Highway 31A, [1] and is at the confluence of Sandon Creek [2] into Carpenter Creek. [3] By road, the place is about 14 kilometres (9 mi) east of New Denver and 43 kilometres (27 mi) west of Kaslo.
The North Coast of British Columbia typically has winters that are remarkably similar to the southern Coast, but with much cooler summers between 13 and 20 °C (55 and 68 °F). It is also very wet, with 1,500 to 4,500 mm (59 to 177 in) of precipitation a year falling on around 230 days.
The Coast Mountains (French: La chaîne Côtière) are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia south to the Fraser River. [1]
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.