Nanisivik Mine
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Nanisivik Mine
Nanisivik Mine was a zinc-lead mine in the company town of Nanisivik, Nunavut, north of the Arctic Circle on Baffin Island. It was Canada's first mine in the Arctic. The mine first opened on 15 October 1976 and permanently closed in September 2002 due to low metal prices and declining resources. Mine reclamation began in April 2003. It was one of the most northerly mines in the world. The mine was served by a port and dock located about north. It was used for shipping concentrate from the site, and receiving supplies. It is currently used by the Canadian Coast Guard for training and is intended to become Nanisivik Naval Facility. The mine also had its own airport ( Nanisivik Airport) located about southwest and was the main airport for Arctic Bay, until they expanded the Arctic Bay Airport. The airport is about directly southeast of Arctic Bay but the road between them is .
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Nanisivik
Nanisivik ( iu, ᓇᓂᓯᕕᒃ, lit=the place where people find things; ) is a now-abandoned company town which was built in 1975 to support the lead-zinc mining and mineral processing operations for the Nanisivik Mine, in production between 1976 and 2002. The townsite is located just inland from Strathcona Sound, about east of the community of Arctic Bay in the Canadian territory of Nunavut. There is a port and dock about north of the abandoned mine site, which was used for shipping concentrate from the site, and receiving supplies (). It is used by the Canadian Coast Guard for training. Nanisivik Airport, located south, was used as the main airport for Arctic Bay until 2010, when the lengthened Arctic Bay Airport took over. The airport is about directly southeast of Arctic Bay but the road between them is . Demographics In the 2021 Canadian census conducted by Statistics Canada, Nanisivik had a population of 0, no change from its 2016 population of 0. With a land ...
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Nanisivik Naval Facility
The Nanisivik Naval Facility (french: links=no, installation navale de Nanisivik) is a Canadian Forces naval facility on Baffin Island, Nunavut. The station is built at the former lead-zinc mine site near the former company town of Nanisivik. The facility was undergoing final testing in mid-2019. Full operational capability had been expected to be achieved by mid-2020 with the first refuelling of a Royal Canadian Navy ship. However, in July 2020 it was confirmed that work on the facility would not be completed until 2022. On 30 March 2022, it was reported that the completion of the facility would be further delayed to 2023. Then in November 2022, the Auditor General of Canada reported that the facility would only actually start to be used by the Navy beginning in 2025. Description The naval station was originally planned to be home port of the Arctic offshore patrol ships that were proposed under the Harper government plan. These ships have ice-breaking capability and help the ...
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Zinc Mines In Canada
Zinc is a chemical element with the symbol Zn and atomic number 30. Zinc is a slightly brittle metal at room temperature and has a shiny-greyish appearance when oxidation is removed. It is the first element in group 12 (IIB) of the periodic table. In some respects, zinc is chemically similar to magnesium: both elements exhibit only one normal oxidation state (+2), and the Zn2+ and Mg2+ ions are of similar size.The elements are from different metal groups. See periodic table. Zinc is the 24th most abundant element in Earth's crust and has five stable isotopes. The most common zinc ore is sphalerite (zinc blende), a zinc sulfide mineral. The largest workable lodes are in Australia, Asia, and the United States. Zinc is refined by froth flotation of the ore, roasting, and final extraction using electricity (electrowinning). Zinc is an essential trace element for humans, animals, plants and for microorganisms and is necessary for prenatal and postnatal development. It is the secon ...
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Lead Mines In Canada
Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is a shiny gray with a hint of blue. It tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes are endpoints of major nuclear decay chains of heavier elements. Lead is toxic, even in small amounts, especially to children. Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of ...
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Mines In Nunavut
Mine, mines, miners or mining may refer to: Extraction or digging *Miner, a person engaged in mining or digging *Mining, extraction of mineral resources from the ground through a mine Grammar *Mine, a first-person English possessive pronoun Military * Anti-tank mine, a land mine made for use against armored vehicles * Antipersonnel mine, a land mine targeting people walking around, either with explosives or poison gas * Bangalore mine, colloquial name for the Bangalore torpedo, a man-portable explosive device for clearing a path through wire obstacles and land mines * Cluster bomb, an aerial bomb which releases many small submunitions, which often act as mines * Land mine, explosive mines placed under or on the ground * Mining (military), digging under a fortified military position to penetrate its defenses * Naval mine, or sea mine, a mine at sea, either floating or on the sea bed, often dropped via parachute from aircraft, or otherwise lain by surface ships or submarines * Pa ...
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Val D'Or Star
Val may refer to: Val-a Film * ''Val'' (film), an American documentary about Val Kilmer, directed by Leo Scott and Ting Poo Military equipment * Aichi D3A, a Japanese World War II dive bomber codenamed "Val" by the Allies * AS Val, a Soviet assault rifle Music *''Val'', album by Val Doonican *VAL (band), Belarusian pop duo People * Val (given name), a unisex given name * Rafael Merry del Val (1865–1930), Spanish Catholic cardinal * Val (sculptor) (1967–2016), French sculptor * Val (footballer, born 1983), Lucivaldo Lázaro de Abreu, Brazilian football midfielder * Val (footballer, born 1997), Valdemir de Oliveira Soares, Brazilian football defensive midfielder Places * Val (Rychnov nad Kněžnou District), a village and municipality in the Czech Republic * Val (Tábor District), a village and municipality in the Czech Republic * Vál, a village in Hungary * Val, Iran, a village in Kurdistan Province, Iran * Val, Italy, a ''frazione'' in Cortina d'Ampezzo, Veneto, ...
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El Mochito Mine
El Mochito mine is an underground zinc and silver mine in Honduras that is owned by Ascendant Resources. The mine is located near the municipality of Las Vegas in northwest section Honduras. At approximately northeast of the mine, the closest major city is San Pedro Sula, which also acts as the commercial centre of the country. History The deposit was discovered in 1938. The Rosario Mining Company purchased the property in 1943 and began production in 1948. American Pacific Mining Corporation purchased the property in September 1987, and in March 1990, Breakwater Resources acquired American Pacific and the mine. In August 2011, Nyrstar successfully completed its acquisition of Breakwater Resources. On December 20, 2016 the mine was acquired by the Canadian firm Morumbi Resources, which renamed itself to Ascendant Resources effective December 21, 2016. See also *El Toqui mine *Nanisivik Mine Nanisivik Mine was a zinc-lead mine in the company town of Nanisivik, Nunavut, north ...
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El Toqui Mine
El Toqui mine is a zinc-gold mine in Chile. Besides silver and lead are also mined in El Toqui. The mine is owned by Breakwater Resources through its wholly owned subsidiary company Sociedad Contractual Minera el Toqui. The mine was purchased from Barrick Gold Corporation in 1997. The mine is powered by a 4 Mw diesel power plant and a 2 Mw hydroelectric power plant. See also *Mining in Chile *El Mochito mine *Nanisivik Mine Nanisivik Mine was a zinc-lead mine in the company town of Nanisivik, Nunavut, north of the Arctic Circle on Baffin Island. It was Canada's first mine in the Arctic. The mine first opened on 15 October 1976 and permanently closed in September ... References Zinc mines in Chile Gold mines in Chile Lead mines in Chile Silver mines in Chile Mines in Aysén Region Underground mines in Chile {{Mining-stub ...
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Polaris Mine
Polaris zinc mine was a former underground mine on Little Cornwallis Island in the Canadian territory of Nunavut (Northwest Territories prior to Nunavut's official separation). The Polaris zinc mine was located north of the Arctic Circle, and north of the community of Resolute. The Polaris mine closed in July 2002 following more than twenty years of zinc production. History In 1964 Vancouver-based Cominco optioned all the mineral claims in Canada's Arctic that were controlled by Bankaro Mines. Mineral and economic assessments resulted in a 23 million ton reserve at a zinc grade of 14.1 per cent. Approval of the project was obtained in 1979, then Prime Minister Joe Clark waived environmental assessment hearings and pledged to ship half of the concentrate from the mine in the federally owned icebreaker MV Arctic. The entire mineral processing plant, power plant and workshop were built upon a barge and travelled from Quebec to the mine site. In 1981 the mine commenced producti ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Polar Climate
The polar climate regions are characterized by a lack of warm summers but with varying winters. Every month in a polar climate has an average temperature of less than . Regions with polar climate cover more than 20% of the Earth's area. Most of these regions are far from the equator and near the poles, and in this case, winter days are extremely short and summer days are extremely long (could last for the entirety of each season or longer). A polar climate consists of cool summers and very cold winters, which results in treeless tundra, glaciers, or a permanent or semi-permanent layer of ice. It is identified with the letter E in the Köppen climate classification. Subtypes There are two types of polar climate: ET, or tundra climate; and EF, or ice cap climate. A tundra climate is characterized by having at least one month whose average temperature is above , while an ice cap climate has no months averaging above . In a tundra climate, even coniferous trees cannot grow, but o ...
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Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ...
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