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79-525: Bowdoin College’s historic relationship with the Arctic dates back to 1860, when a group of Bowdoin students accompanied professor Paul Chadbourne on a research trip to Labrador and West Greenland . Peary and MacMillan made many trips to the Arctic, together and separately. Bowdoin students also accompanied MacMillan on several expeditions in the early-to-mid-20th century. To this day, professors and students of

158-564: A land claim for portions of Labradorian land in 1977. In 1988, the Labrador Inuit Association, the government of the province of Newfoundland, and the government of Canada began negotiations based on the land claim. An agreement-in-principle was achieved in 2001, and on May 26, 2004, the agreement was ratified by over 75% of eligible voters subject to the land claim. On January 22, 2005, the Inuit of Nunatsiavut signed

237-576: A 1999 resolution of the Assembly of First Nations claimed Labrador as a homeland for the Innu and demanded recognition in any further constitutional negotiations regarding the region. Labrador's Innu became status Indians under the Indian Act in 2002. Natuashish became a federal Indian reserve in 2003. Sheshatshiu became a federal reserve in 2006. The Labrador Inuit Association had filed

316-539: A concentration in Arctic Studies. These departments, together with the Peary–MacMillan Arctic Museum, provide students with opportunities to explore cultural, social, and environmental issues involving Arctic lands and peoples. The Director of the Peary–MacMillan Arctic Museum & Arctic Studies Center is Susan A. Kaplan, Professor of Anthropology. The Peary–MacMillan Arctic Museum is located in

395-651: A deep, common, joined bedrock region in eastern and central Canada , the shield stretches north from the Great Lakes to the Arctic Ocean , covering over half of Canada and most of Greenland ; it also extends south into the northern reaches of the continental United States . The Canadian Shield is a physiographic division comprising four smaller physiographic provinces: the Laurentian Upland , Kazan Region , Davis and James. The shield extends into

474-405: A myriad population of other birds, including ravens and crows , predatory birds and many songbirds . The Canadian Shield is one of the world's richest areas in terms of mineral ores . It is filled with substantial deposits of nickel , gold , silver , and copper . There are many mining towns extracting these minerals. The largest, and one of the best known, is Sudbury , Ontario. Sudbury

553-528: A natural harbour on the northeast coast of the Strait of Belle Isle. They gave this "new land" its Latin name Terranova . A whaling station was set up around the bay, which they called Butus and is now named Red Bay after the red terracotta roof tiles they brought with them. A whaling ship, the San Juan , sank there in 1565 and was raised in 1978. The Moravian Brethren of Herrnhut , Saxony , first came to

632-787: A project with Memorial University of Newfoundland to better understand their past through the Community-University Research Association (CURA). Following research by CURA, the "Labrador Metis" were understood to be a continuation of the Inuit of southern Labrador. In 2010, the Labrador Metis Association changed its name to reflect their newly discovered heritage, and became the NunatuKavut Community Council . The Southern Inuit of NunatuKavut , who are also seeking self-government, have their land claim before

711-590: A riding that included part of the Island of Newfoundland. Labrador is divided into four provincial electoral districts in the Newfoundland and Labrador House of Assembly . In 1809, Labrador was transferred from Lower Canada to the Newfoundland Colony, but the inland boundary of Labrador had never been precisely stated. Newfoundland argued it extended to the height of land, while Canada, stressing

790-552: A short border with Nunavut on Killiniq Island. Labrador also has a maritime border with Greenland. Northern Labrador's climate is classified as polar , while Southern Labrador's climate is classified as subarctic . Labrador can be divided into four geographical regions: the North Coast, Central Labrador, Western Labrador, and the South Coast. Each of those regions is described below. From Cape Chidley to Hamilton Inlet ,

869-526: A single railway that would carry cars, buses and trucks, was technologically the best option for such a link. However, the study also concluded that a fixed link was not economically viable. Conceivably, if built with federal aid, the 1949 terms of union would be amended to remove ferry service from Nova Scotia to Port aux Basques across the Cabot Strait . Although a highway link has, as of December 2009, been completed across Labrador, this route

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948-821: A small land border with the territory of Nunavut on Killiniq Island . The indigenous peoples of Labrador include the Northern Inuit of Nunatsiavut , the Southern Métis of NunatuKavut , and the Innu of Nitassinan . Labrador is named after João Fernandes Lavrador , a Portuguese explorer who sailed along the coasts of the Labrador Peninsula in 1498–99. Labrador's name in the Inuttitut / Inuktitut language (spoken in Nunatsiavut )

1027-610: A solid Eurasian continent running from Scandinavia around the North Pole, including Asia's arctic coast, to Newfoundland-Labrador and Greenland. On the extreme northeast promontory of North America, Maggiolo place-names include Terra de los Ingres (Land of the English), and Terra de Lavorador de rey de portugall (Land of Lavrador of the King of Portugal). Further south are the phrases Terra de corte real e de rey de portugall (Land of

1106-614: A transmission line to the neighbouring province of Quebec. Construction of a large hydroelectric dam project at Muskrat Falls began in 2012 by Nalcor Energy and the Province of Newfoundland. Muskrat Falls is 45 km (30 miles) west of Happy Valley-Goose Bay on the Grand River (Newfoundland name: Churchill River). A transmission line began construction in October 2014 and was completed in 2016 that delivers power down to

1185-736: Is Nunatsuak ( ᓄᓇᑦᓱᐊᒃ ), meaning "the big land" (a common English nickname for Labrador ). Labrador has a roughly triangular shape that encompasses the easternmost section of the Canadian Shield , a sweeping geographical region of thin soil and abundant mineral resources. Its western border with Quebec is the drainage divide of the Labrador Peninsula. Lands that drain into the Atlantic Ocean are part of Labrador, while lands that drain into Hudson Bay are part of Quebec. Labrador's extreme northern tip, at 60°22′N, shares

1264-531: Is NunatuKavut) and the multitude of icebergs that pass by the coast via the Labrador Current . Red Bay is known as one of the best examples of a preserved 16th-century Basque whaling station. It is also the location of four 16th-century Spanish galleons. The lighthouse at Point Amour is the second-largest lighthouse in Canada. MV Kamutik , a passenger ferry between the mainland and St. Barbe on

1343-535: Is a geologic shield , a large area of exposed Precambrian igneous and high-grade metamorphic rocks . It forms the North American Craton (or Laurentia) , the ancient geologic core of the North American continent. Glaciation has left the area with only a thin layer of soil , through which exposures of igneous bedrock resulting from its long volcanic history are frequently visible. As

1422-595: Is a collage of Archean plates and accreted juvenile arc terranes and sedimentary basins of the Proterozoic Eon that were progressively amalgamated during the interval 2.45–1.24 Ga, with the most substantial growth period occurring during the Trans-Hudson orogeny , between c. 1.90–1.80 Ga. The Canadian Shield was the first part of North America to be permanently elevated above sea level and has remained almost wholly untouched by successive encroachments of

1501-647: Is an exception to the normal process of forming minerals in the shield since the Sudbury Basin is an ancient meteorite impact crater . Ejecta from the meteorite impact was found in the Rove Formation in May 2007. The nearby but less-known Temagami Magnetic Anomaly has striking similarities to the Sudbury Basin. This suggests it could be a second metal-rich impact crater. In northeastern Quebec,

1580-601: Is home to a number of flora and fauna species. Most of the Upper Canadian and Lower Hudsonian mammalian species are found in Labrador. Notably the Polar bear ( Ursus maritimus ) reaches the southeast of Labrador on its seasonal movements. Early settlement in Labrador was tied to the sea as demonstrated by the Innu (formerly called Montagnais) and Inuit, although these peoples also made significant forays throughout

1659-587: Is one of the world's best preserved mineralized Neoarchean caldera complexes, which is 2.7 Ga. The Canadian Shield also contains the Mackenzie dike swarm , which is the largest dike swarm known on Earth. The North American craton is the bedrock forming the heart of the North American continent, and the Canadian Shield is the largest exposed part of the craton's bedrock. The Canadian Shield

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1738-673: Is part of an ancient continent called Arctica , which was formed about 2.5 Ga during the Neoarchean era. Mountains have deep roots and float on the denser mantle much like an iceberg at sea . As mountains erode, their roots rise and are eroded in turn. The rocks that now form the surface of the shield were once far below the Earth's surface. The high pressures and temperatures at those depths provided ideal conditions for mineralization. Although these mountains are now heavily eroded, many large mountains still exist in Canada's far north called

1817-556: Is somewhat longer than a proposed Quebec North Shore highway that presently does not exist. Part of the "highway", Route 389 , starting approximately 212 kilometres (132 mi) from Baie-Comeau to 482 kilometres (300 mi), is of an inferior alignment, and from there to 570 kilometres (350 mi), the provincial border, is an accident-prone section notorious for its poor surface and sharp curves. Quebec in April 2009 announced major upgrades to Route 389 to be carried out. Route 389 and

1896-498: Is the administrative centre. Central Labrador extends from the shores of Lake Melville into the interior. It contains the Churchill River , the largest river in Labrador and one of the largest in Canada. The hydroelectric dam at Churchill Falls is the second-largest underground power station in the world. Most of the supply is bought by Hydro-Québec under a long-term contract. The Lower Churchill Project will develop

1975-500: Is the most isolated region of Labrador, with snowmobiles , boats, and planes being the only modern modes of transportation. The largest community in this region is Nain . Nunatsiavut is an Inuit self-government region in Labrador created on June 23, 2005. The settlement area comprises the majority of Labrador's North Coast, while the land-use area also includes land farther to the interior and in Central Labrador. Nain

2054-682: Is the territory of the NunatuKavummiut or Central-Southern Labrador Inuit (formerly known as the Labrador Métis ). It includes portions of Central and Western Labrador, but more NunatuKavummiut reside in its South Coast portion: it is peppered with tiny Inuit fishing communities, of which Cartwright is the largest. From Cape Charles to the Quebec/Labrador coastal border, the Straits is known for its Labrador sea grass (as

2133-500: Is typically cool and cloudy. Winters are long, cold, and extremely snowy, due to the Icelandic Low . Springtime most years does not arrive until late April, with the last snow fall usually falling during early June. Labrador is a very cloudy place, with sunshine levels staying relatively low during spring and summer due to the amount of rain and clouds, before sharply dropping off during September as winter draws nearer. Labrador

2212-723: The 52nd parallel north . One of Newfoundland's conditions for joining Confederation in 1949 was that this boundary be entrenched in the Canadian constitution. While this border has not been formally accepted by the Quebec government, the Henri Dorion Commission ( Commission d'étude sur l'intégrité du territoire du Québec ) concluded in the early 1970s that Quebec no longer has a legal claim to Labrador. In 2001, Parti Québécois cabinet ministers Jacques Brassard and Joseph Facal reasserted that Quebec has never recognized

2291-472: The Arctic Cordillera . This is a vast, deeply dissected mountain range, stretching from northernmost Ellesmere Island to the northernmost tip of Labrador. The range's highest peak is Nunavut's Barbeau Peak at 2,616 metres (8,583 ft) above sea level. Precambrian rock is the major component of the bedrock. The current surface expression of the shield is one of very thin soil lying on top of

2370-606: The Canadian War Museum . The Canadian government built a major air force base at Goose Bay , at the head of Lake Melville during the Second World War, a site selected because of its topography, access to the sea, defensible location, and minimal fog. During the Second World War and the Cold War, the base was also home to American, British, and later German, Dutch, and Italian detachments. Today, Serco,

2449-646: The Greenland section is included, the Canadian Shield is approximately circular, bounded on the northeast by the northeast edge of Greenland, with Hudson Bay in the middle. It covers much of Greenland, all of Labrador and the Great Northern Peninsula of Newfoundland , most of Quebec north of the St. Lawrence River , much of Ontario including northern sections of the Ontario Peninsula ,

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2528-604: The Newfoundland Railway and later Canadian National Railway / CN Marine / Marine Atlantic became a critical lifeline for communities on the coast, which for the majority of that century did not have any road connection with the rest of North America. Labrador was part of New France until the French and Indian War . By the Treaty of Paris (1763) , which ended the war, New France (including Labrador, though excluding

2607-611: The North Warning System ; however, the military settlements during the early part of the Cold War surrounding these stations have largely continued as local Innu and Inuit populations have clustered near their port and airfield facilities. During the first half of the 20th century, some of the largest iron ore deposits in the world were discovered in the western part of Labrador and adjacent areas of Quebec. Deposits at Mont Wright , Schefferville , Labrador City, and Wabush drove industrial development and human settlement in

2686-620: The Smallwood Reservoir has flooded much of the old hunting land—submerging several grave sites and trapping cabins in the process. Western Labrador is also home to the Iron Ore Company of Canada , which operates a large iron ore mine in Labrador City . Together with the small community of Wabush , the two towns are known as "Labrador West". From Hamilton Inlet to Cape St. Charles / St. Lewis , NunatuKavut

2765-759: The Torngat Mountains National Park in the northern area of the land claim. The agreement was ratified by the Labrador Inuit, the General Assembly of Newfoundland and Labrador , and the Parliament of Canada , where it received Royal Assent on June 23, 2005, whereafter elections would be held for the Nunatsiavut Assembly and self-government would begin. In the late 1970s, the Labrador Metis Association

2844-429: The 1927 border: Les ministres rappellent qu'aucun gouvernement québécois n'a reconnu formellement le tracé de la frontière entre le Québec et Terre-Neuve dans la péninsule du Labrador selon l'avis rendu par le comité judiciaire du Conseil privé de Londres en 1927. Pour le Québec, cette frontière n'a donc jamais été définitivement arrêtée. [The ministers reiterate that no Quebec government has ever formally recognised

2923-478: The 1960s, the Churchill River (Labrador name: Grand River) was diverted at Churchill Falls , resulting in the flooding of an enormous area – today named the Smallwood Reservoir after Joey Smallwood , the first premier of Newfoundland. The flooding of the reservoir destroyed large areas of habitat for the threatened Woodland Caribou. A hydroelectric generating station was built in Labrador as well as

3002-707: The Adirondack Mountains of New York , the northernmost part of Lower Michigan and all of Upper Michigan , northern Wisconsin , northeastern Minnesota , the central and northern portions of Manitoba , northern Saskatchewan , a small portion of northeastern Alberta , mainland Northwest Territories to the east of a line extended north from the Saskatchewan-Alberta border, most of Nunavut's mainland and, of its Arctic Archipelago , Baffin Island and significant bands through Somerset , Southampton , Devon and Ellesmere islands. In total,

3081-604: The Arctic, ranging from natural life, such as plants and animals, to cultural life of people native to the Arctic region. Artifacts in the Museum's collection include Peary and MacMillan's expedition equipment, anthropological objects, Inuit art , films, archival papers, publications, and natural history specimens. The Museum's exhibitions change regularly. To see current exhibits visit the museum's website . Bowdoin College's Departments of Sociology, Anthropology, and Geology offer

3160-526: The Government of Canada. The Government of Newfoundland and Labrador refuses to recognise or negotiate with the Inuit of NunatuKavut until their claim has been accepted by the Government of Canada. The Labrador region, with its 26,655 population, is lower than any of the Northern Canada territories, Yukon , Northwest Territories and Nunavut . Newfoundland Island contains the majority of

3239-466: The John and Lile Gibbons Center for Arctic Studies, which opened in 2023. 43°54′27″N 69°57′48″W  /  43.9075°N 69.96325°W  / 43.9075; -69.96325 Labrador Labrador ( / ˈ l æ b r ə d ɔːr / LAB -rə-dor ) is a geographic and cultural region within the Canadian province of Newfoundland and Labrador . It is the primarily continental portion of

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3318-547: The Labrador Coast in 1760 to minister to the migratory Inuit tribes there. They founded Nain, Okak, Hebron, Hopedale and Makkovik. Quite poor, both European and First Nations settlements along coastal Labrador came to benefit from cargo and relief vessels that were operated as part of the Grenfell Mission (see Wilfred Grenfell ). Throughout the 20th century, coastal freighters and ferries operated initially by

3397-744: The Labrador Inuit Lands Claims Agreement with the federal and provincial governments covering 72,520 km (28,000 sq mi) of land, including the entire northern salient of Labrador north of Nain as well as a portion of the Atlantic coast south of there. The agreement also includes 44,030 km (17,000 sq mi) of sea rights. Although the Inuit will not own the whole area, they were granted special rights related to traditional land use, and they will own 15,800 km (6,100 sq mi) designated Labrador Inuit Lands. The agreement also establishes

3476-535: The Royal Court and of the King of Portugal) and Terra de pescaria (Land for Fishing). In the 1532 Wolfenbüttel map, believed to be the work of Diogo Ribeiro , along the coast of Greenland, the following legend was added: As he who first sighted it was a farmer from the Azores Islands, this name remains attached to that country. This is believed to be João Fernandes. For the first seven decades or so of

3555-404: The Trans-Labrador Highway were added to Canada's National Highway System in September 2005. Labrador constitutes a federal electoral district electing one member to the House of Commons of Canada . Due to its size, distinct nature, and large Aboriginal population, Labrador has one seat despite having the smallest population of any electoral district in Canada. Formerly, Labrador was part of

3634-529: The United States as the Adirondack Mountains (connected by the Frontenac Axis ) and the Superior Upland . The Canadian Shield is a U-shaped subsection of the Laurentia craton signifying the area of greatest glacial impact (scraping down to bare rock) creating the thin soils. The age of the Canadian Shield is estimated to be 4.28 Ga . The Canadian Shield once had jagged peaks, higher than any of today's mountains, but millions of years of erosion have changed these mountains to rolling hills. The Canadian Shield

3713-417: The area during the second half of the 20th century. The present community of Labrador West is entirely a result of the iron ore mining activities in the region. The Iron Ore Company of Canada operates the Quebec North Shore and Labrador Railway to transport ore concentrate 578 km (359 mi) south to the port of Sept-Îles, Quebec , for shipment to steel mills in North America and elsewhere. During

3792-426: The bedrock, with many bare outcrops . This arrangement was caused by severe glaciation during the ice ages that covered the shield and scraped the rock clean. The lowlands of the Canadian Shield have a very dense soil that is not suitable for forestation; it also contains many marshes and bogs ( muskegs ). The rest of the region has coarse soil that does not retain moisture well and is frozen with permafrost throughout

3871-521: The case of polar bears ( Ursus maritimus ), the shield area contains many of their denning locations, such as the Wapusk National Park . The many lakes and rivers on the shield contain a plentiful quantity of different sports fish species, including walleye , northern pike , lake trout , yellow perch , whitefish , brook trout , arctic grayling , and many types of baitfish. The water surfaces are also home to many waterfowl , most notably Canada geese , loons and gulls . The vast forests contain

3950-403: The college continue to travel to the Arctic to pursue research. The Peary–MacMillan Arctic Museum was made possible by generous donations from the Class of 1925, George B. Knox (Class of 1929), and other alumni and friends. The Museum was dedicated in June 1967, with both MacMillan and Peary's daughter, Marie Ahnighito Peary , in attendance. Established in 1985, the Arctic Studies Center links

4029-408: The company contracted to operate CFB Goose Bay is one of the largest employers for the community of Happy Valley-Goose Bay . Additionally, both the Royal Canadian Air Force and United States Air Force built and operated a number of radar stations along coastal Labrador as part of the Pinetree Line , Mid-Canada Line and DEW Line systems. Today, the remaining stations are automated as part of

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4108-448: The drawing of the border between Quebec and Newfoundland in the Labrador peninsula according to the opinion rendered by the London Judicial Committee of the Privy Council in 1927. For Quebec, this border has thus never been definitively defined.] A Royal Commission in 2002 determined that there is some public pressure from Labradorians to break from Newfoundland and become a separate province or territory. After decades of negotiation with

4187-426: The early 2000s and is resulting in significant changes to the coastal ferry system in the Strait of Belle Isle and southeastern Labrador. These "highways" are so called only because of their importance to the region; they would be better described as roads, and were not completely paved until July 2022. A study on a fixed link to Newfoundland, in 2004, recommended that a tunnel under the Strait of Belle Isle , being

4266-489: The exposed area of the shield covers approximately 8,000,000 km (3,100,000 sq mi). The true extent of the shield is greater still and stretches from the Western Cordillera in the west to the Appalachians in the east and as far south as Texas , but these regions are overlaid with much younger rocks and sediment. The Canadian Shield is among the oldest geologic areas on Earth, with regions dating from 2.5 to 4.2 billion years. The multitude of rivers and lakes in

4345-405: The giant Manicouagan Reservoir is the site of an extensive hydroelectric project (Manic-cinq, or Manic-5). This is one of the largest-known meteorite impact craters on Earth , though not as large as the Sudbury crater. The Flin Flon greenstone belt in central Manitoba and east-central Saskatchewan "is one of the largest Paleoproterozoic volcanic-hosted massive sulfide ( VMS ) districts in

4424-420: The historical use of the term "Coasts of Labrador", argued the boundary was 1 statute mile (1.6 km) inland from the high-tide mark. As Canada and Newfoundland were separate Dominions , but both within the British Empire , the matter was referred to the Judicial Committee of the Privy Council (in London). Their decision set the Labrador boundary mostly along the coastal watershed, with part being defined by

4503-404: The installation of the equipment was the only-known armed German military operation on the North American mainland during the war. The station broadcast weather observations to the German navy for only a few days, but was not discovered until 1977 when a historian, working with the Canadian Coast Guard , identified its location and mounted an expedition to recover it. The station is now exhibited in

4582-439: The interior. It is believed that the Norsemen were the first Europeans to sight Labrador around 1000 AD. The area was known as Markland in Greenlandic Norse and its inhabitants were known as the Skrælings . In 1499 and 1500, the Portuguese explorers João Fernandes Lavrador and Pero de Barcelos reached what was probably now Labrador, which is believed to be the origin of its name. Maggiolo's World Map , 1511, shows

4661-471: The island of Newfoundland , is based in Blanc Sablon, Quebec , near the Labrador border. L'Anse-au-Loup is the largest town on the Labrador Straits. L'Anse-au-Clair is a small town on the Labrador side of the border. Most of Labrador (from Cartwright north and west) uses Atlantic Time (UTC−4 in winter, UTC−3 in summer). The south eastern tip nearest Newfoundland uses Newfoundland Time (UTC−3:30 in winter, UTC−2:30 in summer) to stay co-ordinated with

4740-452: The islands of Saint Pierre and Miquelon southwest of Newfoundland) was transferred to the British, who administered the northern portion of it as the Province of Quebec until splitting it in two in 1791, with Labrador located in Lower Canada . However, in 1809, the British Imperial government detached Labrador from Lower Canada for transfer to the separate, self-governing Newfoundland Colony . As part of Newfoundland since 1809, Labrador

4819-447: The long, thin, northern tip of Labrador holds the Torngat Mountains , named after an Inuit spirit believed to inhabit them. The mountains stretch along the coast from Port Manvers to Cape Chidley , the northernmost point of Labrador. The Torngat Mountain range is also home to Mount Caubvick , the highest point in the province. This area is predominantly Inuit, with the exception of a small Innu community, Natuashish . The North Coast

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4898-401: The more populous part of the province. Most of Labrador has a subarctic climate ( Dfc ), but northern Labrador has a tundra climate (ET) and Happy Valley - Goose Bay has a humid continental (Dfb) microclimate. Summers are typically cool to mild across Labrador and very rainy, and usually last from late June to the end of August. Autumn is generally short, lasting only a couple of weeks and

4977-413: The most northerly parts of Manitoba and Saskatchewan. Hydrologic drainage is generally poor, the soil compacting effects of glaciation being one of the many causes. Tundra typically prevails in the northern regions. Many mammals such as beaver , caribou , white-tailed deer , moose , wolves , wolverines , weasels , mink , otters , grizzly bear , polar bears and black bears are present. In

5056-469: The plateau during the Cenozoic Era. During the Pleistocene Epoch, continental ice sheets depressed the land surface (creating Hudson Bay ) but also tilted up its northeastern "rim" (the Torngat ), scooped out thousands of lake basins, and carried away much of the region's soil. The northeastern portion, however, became tilted up so that, in northern Labrador and Baffin Island , the land rises to more than 1,500 metres (5,000 feet) above sea level. When

5135-410: The population of the province of Newfoundland and Labrador . The municipalities of Labrador are mainly under 1,000 in population. Census Division 10 (excludes Nunatsiavut-Nain) Census Division 11 (Nunatsiavut-Nain) Canadian Shield The Canadian Shield ( French : Bouclier canadien [buklje kanadjɛ̃] ), also called the Laurentian Shield or the Laurentian Plateau ,

5214-429: The province and constitutes 71% of the province's area but is home to only 6% of its population. It is separated from the island of Newfoundland by the Strait of Belle Isle . It is the largest and northernmost geographical region in the four Atlantic provinces . Labrador occupies most of the eastern part of the Labrador Peninsula . It is bordered to the west and south by the province of Quebec . Labrador also shares

5293-448: The provincial and federal governments, the Nunatsiavut region of northern and northeastern Labrador was created in 2005 as an autonomous region with its own elected Assembly and executive drawn from members of the region's Assembly. Some of the Innu nation would have the entirety of Labrador become a homeland for them, much as Nunavut and Nunatsiavut is for the Inuit , as a good portion of Nitassinan falls within Labrador's borders;

5372-446: The region is classical example of a deranged drainage system , caused by the watersheds of the area being disturbed by glaciation and the effect of post-glacial rebound . The shield was originally an area of very large, very tall mountains (about 12,000 m or 39,000 ft) with much volcanic activity, but the area was eroded to nearly its current topographic appearance of relatively low relief over 500 Ma. Erosion has exposed

5451-411: The remaining potential of the river and supply it to provincial consumers. Known as "the heart of the Big Land", the area's population comprises people from all groups and regions of Labrador. Central Labrador is also home to Happy Valley-Goose Bay . Once a refuelling point for plane convoys to Europe during World War II , CFB Goose Bay is now operated as a NATO tactical flight training site. It

5530-435: The resources of the museum and the library with teaching and research efforts, and hosts lectures, workshops, and educational outreach projects. "Through course offerings, field research programs, employment opportunities, and special events, the Arctic Studies Center promotes anthropological, archaeological, geological, and environmental investigations of the North." The Arctic Museum's exhibitions focus on different aspects of

5609-522: The roots of the mountains, which take the form of greenstone belts in which belts of volcanic rock that have been altered by metamorphism are surrounded by granitic rock. These belts range in age from 3.6 to 2.7 Ga. Much of the granitic rock belongs to the distinctive tonalite–trondhjemite–granodiorite family of rocks, which are characteristic of Archean continental crust . Many of Canada's major ore deposits are associated with greenstone belts. The Sturgeon Lake Caldera in Kenora District , Ontario,

5688-558: The sea upon the continent. It is the Earth's greatest area of exposed Archean rock. The metamorphic base rocks are mostly from the Precambrian (between 4.5 Ga and 540 Ma) and have been repeatedly uplifted and eroded. Today it consists largely of an area of low relief 300–610 m (980–2,000 ft) above sea level with a few monadnocks and low mountain ranges (including the Laurentian Mountains ) probably eroded from

5767-567: The sixteenth century, the name Labrador was sometimes also applied to what is now known as Greenland. Labrador ("lavrador" in Portuguese) means husbandman or farmer of a tract of land (from "labor" in Latin) – the land of the labourer. European settlement was largely concentrated in coastal communities, particularly those south of St. Lewis and Cape Charles, and are among Canada's oldest European settlements. In 1542, Basque mariners came ashore at

5846-525: The southern tip of Labrador and underwater across the Strait of Belle Isle to the Province of Newfoundland in 2018. From the 1970s to early 2000s, the Trans-Labrador Highway was built in stages to connect various inland communities with the North American highway network at Mont Wright, Quebec (which in turn is connected by a highway running north from Baie-Comeau , Quebec). A southern extension of this highway has opened in stages during

5925-481: The world, containing 27 copper - zinc -( gold ) deposits from which more than 183 million tonnes of sulfide have been mined." The portion in the Northwest Territories has recently been the site of several major diamond discoveries. The kimberlite pipes in which the diamonds are found are closely associated with cratons, which provide the deep lithospheric mantle required to stabilize diamond as

6004-523: The year. Forests are not as dense in the north. The shield is covered in parts by vast boreal forests in the south that support natural ecosystems as well as a major logging industry. The boreal forest area gives way to the Eastern Canadian Shield taiga that covers northern Quebec and most of Labrador. The Midwestern Canadian Shield forests that run westwards from Northwestern Ontario have boreal forests that give way to taiga in

6083-599: Was an alternate landing zone for the United States' Space Shuttle . Other major communities in the area are North West River and the large Innu reserve known as Sheshatshiu . The highlands above the Churchill Falls were once an ancient hunting ground for the Innu First Nations and settled trappers of Labrador. After the construction of the hydroelectric dam at Churchill Falls in 1970,

6162-418: Was created by the inhabitants of Labrador's southern coast to gain recognition as a distinct ethnocultural group, as at the time despite a pre-existing treaty protected under the constitution, the "Inuit-Metis" were considered to be merely the descendants of Inuit who had joined Western society. Little was known about the history of the "Inuit-Metis" of the time. In 2006, the Labrador Metis Association initiated

6241-596: Was still being disputed by Quebec until the British Privy Council resolved their border in 1927 . In 1949, Newfoundland entered into confederation , becoming part of Canada (see above articles for full information). Labrador played strategic roles during both World War II and the Cold War . In October 1943, a German U-boat crew installed an automated weather station on the northern tip of Labrador near Cape Chidley, code-named Weather Station Kurt ;

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