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Top Attractions in Northwest Territories

Diavik Diamond Mine

The Diavik Diamond Mine is a diamond mine in the North Slave Region of the Northwest Territories, Canada, about 300 kilometres north of Yellowknife. It has become an important part of the regional economy, employing 700, grossing C$100 million in sales, and producing approximately 7.5 million carats of diamonds annually. The area was surveyed in 1992 and construction began in 2001, with production commencing in January 2003. It is connected by an ice road and Diavik Airport with a 5,235 ft gravel runway regularly accommodating Boeing 737 jet aircraft. Diavik Diamond Mine is an industrial complex and town in one, set in a remote, sub-Arctic landscape. In the 2013 satellite image below, you can see the two main open pits, waste rock piles, and an airstrip capable of landing aircraft as large as 737s and C-130s. The complex also houses processing plants, fuel tanks, water and sewage processing facilities, administrative buildings, and accommodations for workers and other residents. The mine is owned by a joint venture between the Dominion Diamond Corporation and Diavik Diamond Mines Inc., a subsidiary of Rio Tinto Group. The lifespan of the mine is expected to be 16 to 22 years. The mine consists of three kimberlite pipes associated with the Lac de Gras kimberlite field and is located on an island 20 km2 in Lac de Gras and is informally called East Island. It is about 220 km south of the Arctic Circle. In 2006 the ice road from Yellowknife to the Diavik mine, and neighbouring mines, froze late and thawed early. The Diavik mine was unable to truck in all the supplies needed for the rest of 2006 before the road closed and arrangements had to be made to bring the remainder of the supplies in by air. On July 5, 2007 a consortium of seven mining companies, including Rio Tinto, announced they are sponsoring environmental impact studies to construct a deep-water port in Bathurst Inlet. Their plans include building a 211 km road connecting the port to their mines. The port would serve vessels of up to 25,000 tonnes. In March 2010, underground mining began at the mine. The transition from open pit to underground mining is expected to be completed by 2012.

Tungsten

The townsite of Tungsten (sometimes shown as Cantung on some maps) is located at Cantung Mine in the Northwest Territories. It is accessible from Watson Lake, Yukon. Tungsten was built in 1961 and the tungsten mine went into operation in 1962 as a large open pit mine in the Mackenzie Mountains. It originally consisted of several small bungalow houses. Total population of Tungsten during the 1960s was approximately 120 persons, including about 27 families. In 1968 families were housed in 28 units (single and duplex housing). Because of extremely good wages and benefits, turnover rates for the entire operation were quite low. Families benefited from the K-8 Grade school, and later a K-9 system. During the summer months, because of the open pit operation, manpower and townsite population grew to 160. In the mid-1970s, the townsite expanded to include a trailer court, three condominiums, bunkhouse trailers, and in 1982, a modern recreation complex. An 80-man bunkhouse was added in 1983. The town and mine were serviced by an all-weather road to Watson Lake and a 3700’ × 100’ (1 128 × 30.5 m) airstrip. In 1979 the estimated population had reached 506, 200 of whom were employees. By the fall of 1982, there were 450 residents and about 100 children were enrolled at Tungsten School. The community also had a public telephone exchange operated by Northwestel: area code 403, prefix 777. By 1986, it was estimated that only 280 people were living at Tungsten. The Cantung Mine closed in May 1986, and the townsite was closed. A year or two later, the telephone exchange, with only a handful of active lines on obsolescent electromechanical equipment, was shut down. Although the mine reopened in 2002, the nature of the mine had changed so that there was no longer an operating townsite with families. The mine closed again in 2003. Following an investment by the Kaska Dena Council in the Yukon in December 2004 the mine was reopened in 2005. The original bungalow houses remain to this day, along with the school, and stand as a monument to a time when town life was busy with local residents. The community has the distinction of being the only place in the Northwest Territories that is on Pacific Time rather than Mountain Time.

Dismal Lakes

Dismal Lakes are a series of three interconnected lakes in the Canadian Northwest Territories located roughly midway between the Coronation Gulf and Great Bear Lake, east of the Dease River. The Teshierpi River discharges into the narrows between the second and third Dismal Lakes, and the third lake discharges into the Kendall River. The lakes were named by explorer Thomas Simpson. Two miles west of the western lake is Sandy Creek, which flows south into the Dease River. The west end of western lake is surrounded by bare hills covered in sharp broken rock, and it is from this barren area that the lakes get their name. Three small brooks enter the lake at this end, one from the south, and two from the west. Approximately six miles from the western end of the lake it narrows to half a mile, and on the other side of these narrows the lake is surrounded by rounded slopes covered with grass and heaths. There is a shallow sandbar extending across the eastern end of the lake. The narrows between the first and second lakes are a favored crossing-place for the caribou. The narrow river is confined between steep gravel hills and has a fairly strong current. The center lake is hemmed in by mountains. On the north side the Coppermine Mountains rise in terraces to nearly one thousand feet. There are some small spruce in a cove on the north shore. On the south side of the lake is Teshierpi Mountain, the southern-most spur of the Coppermine Mountains, rising approximately 800 feet. At the east end of the lake is a shallow sandbar which extends across the width of the lake, followed by a series of small willow covered islands. The narrows between the second and third lakes is a short river with a sandy channel. The Teshierpi River joins this channel from the south. The eastern lake is the smallest of the three, approximately three miles long and a mile wide. It is surrounded by gently rising grassy shores and, at a distance, mountains. There is a shallow sandbar extending across the eastern end of the lake. The third lake discharges into the Kendall River, which flows southwest into the Coppermine River. The extreme end of the third lake is sparsely wooded with small spruce, which extend down the Kendall. The Dismal Lakes are one of the historical homes of Nagyuktogmiut, a Copper Inuit subgroup.

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