MarketGeography of Newfoundland and Labrador
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Geography of Newfoundland and Labrador

Newfoundland and Labrador is the easternmost province in Canada. The Strait of Belle Isle separates the province into two geographical regions, Labrador and the island of Newfoundland. The province also includes over seven thousand small islands.

Physical geography
Newfoundland is roughly triangular, with each side being approximately , and having an area of . Newfoundland extends between latitudes 46°36'N and 51°38'N. It lies at similar latitudes to Great Britain, and the Kamchatka Peninsula in Russia. Labrador is an irregular shape: the western part of its border with Quebec is the drainage divide for the Labrador Peninsula. Lands drained by rivers that flow into the Atlantic Ocean are part of Labrador, the rest belongs to Quebec. Labrador's extreme northern tip, at 60°22'N, shares a short border with Nunavut on Killiniq Island. Labrador's area (including associated small islands) is . The island of Newfoundland is separated from Labrador by the Strait of Belle Isle, which is long and from wide. In addition to the island of Newfoundland, the province is made up of 12 larger islands with a total area of and 7,170 smaller islands with a total area of . == Geology ==
Geology
A large part of the island of Newfoundland is an extension of the Appalachian system. The plateau in the Avalon Peninsula averages above sea level. Glaciers which helped shape these tolts left other evidence around Newfoundland. Large blocks of stone called glacial erratics have been left scattered across much of the landscape. The long narrow lakes of the west coast, notably those in Gros Morne National Park resulted from glacial erosion. The lack of good soil on most parts of the island is a result of the scouring effect of glaciers during the most recent ice age. Newfoundland's nickname, "The Rock", is partially a result of the ice ages. is a fjord within Gros Morne National Park which resulted from glacial erosion. One of the most noteworthy aspects of Newfoundland geology is a result of the constant movement of tectonic plates. Approximately 500 million years ago, the action of these plates forced sections of the oceanic crust that had been underlying the Iapetus Ocean up and over the eastern margin of the North American plate. Sections of oceanic crust which overlie continental crust are known as ophiolites. Gros Morne National Park was designated a UNESCO World Heritage Site because it is one of the best places in the world to see the effects of plate tectonics Another notable geology site is at Mistaken Point, where rocks containing probably the oldest metazoan fossils in North America and the most ancient deep-water marine fossils in the world are found preserved in layers of volcanic ash. Labrador is the easternmost part of the Canadian Shield and is composed of ancient Precambrian igneous and metamorphic rocks. The interior averages about above sea level and is cut by large, east-flowing rivers, such as the Churchill River and its tributaries. == Biosphere ==
Biosphere
The biosphere is subdivided into geographical regions called biomes. Newfoundland and Labrador are divided into two biomes: tundra and taiga. Northern Labrador is part of the tundra, while southern Labrador is part of the taiga. Newfoundland is not typical of either biome, as it lacks much of the plant and animal life that are characteristic to these biomes. During the last ice age the island of Newfoundland was completely covered by glaciers and swept clean of life. Large herds of woodland caribou can be found in the barren interior regions of the island. Two animals formerly resident in Newfoundland have been declared extinct: the great auk, a flightless seabird, and the Newfoundland wolf, a subspecies of the gray wolf. The Labrador duck, believed to have nested in Labrador, was one of the first North American bird species to be recorded as becoming extinct. Many herbaceous plants and insects occur on the island. Brayas are small perennial herbs of the family Brassicaceae. They are only found on a narrow strip of land extending approximately on the extreme western portion of the Great Northern Peninsula, a limestones barrens habitat. The braya population is low due to habitat loss from gravel quarrying. Researchers have only found three populations of Long's braya, and 14 or 15 populations of Fernald's brayas. Researchers have focused on how various types of disturbances affect the long-term viability of these populations. The Province of Newfoundland and Labrador, with many partners, is studying the rare plant flora of the island of Newfoundland and in 2002 announced a recovery plan for the braya species. Many plants and animals have been introduced to Newfoundland, either by chance or deliberately. Rats and mice were unintentionally introduced while mink escaped from fur farms. Newfoundland has no native amphibians, but frogs were introduced onto the island in the 1860s and toads almost a century later. The marine waters around the province are considered boreal, or sub-Arctic, in nature. Precipitation is low. Soil a meter below ground and deeper is permanently frozen (permafrost), which does not allow water to drain easily through the soil, so it collects in shallow pools. Trees and shrubs are stunted since their roots cannot grow into the permafrost. Low shrubs, lichens, mosses, and small herbaceous plants are found instead. The most common mammals on the tundra are the barren-ground caribou, Arctic wolf, Arctic fox, Arctic hare, lemmings, and voles. Occasional sightings of muskoxen have been made near Cape Chidley, Labrador's most northerly point. The polar bear is the dominant carnivore of the tundra, but is an occasional visitor to coastal Newfoundland, especially in the spring. Many birds migrate to Labrador in spring to lay their eggs and raise their young before returning south for the winter, including the common eider, harlequin duck, common redpoll and American pipit. The Labrador tundra is also permanent home to ptarmigan. Southern Labrador is mostly taiga. It is characterized by low winter temperatures, a longer growing season, and more precipitation than the tundra. Soils are typically lacking important nutrients such as nitrogen and phosphorus. The taiga is dominated by coniferous trees, notably balsam fir and black spruce, though the deciduous white birch, trembling aspen and mountain ash are also present. The most common animals are the moose, American black bear, Canada lynx, red fox, pine marten, short-tailed weasel, and American mink. Beavers, muskrats, and river otters thrive in the many rivers, streams, and wetlands. Willow ptarmigan, common raven, and blackpoll warbler inhabit the forests of southern Labrador while golden eagles, rough-legged hawks and peregrine falcons nest on steep cliffs. == Climate ==
Climate
The province has been divided into seven climate types, The data used in making the graphs is the average taken over thirty years. Error bars on the temperature graph indicate the range of daytime highs and night time lows. Snowfall is the total amount which fell during the month, not the amount accumulated on the ground. This distinction is particularly important for St. John's where a heavy snowfall can be followed by rain so that no snow remains on the ground. Surface water temperatures on the Atlantic side reaches a summer average of inshore and offshore to winter lows of inshore and offshore. Sea temperatures on the west coast are warmer than Atlantic side by 1 to 3 °C (approximately 2 to 5 °F). The sea keeps winter temperatures slightly higher and summer temperatures a little lower on the coast than at places inland. The maritime climate produces more variable weather, ample precipitation in a variety of forms, greater humidity, lower visibility, more clouds, less sunshine, and higher winds than a continental climate. The entire 84-man crew perished, making it the worst Canadian marine disaster in decades. Newfoundland and Labrador has the strongest winds of any of the provinces, with most places having average annual wind speeds over 20 kilometres per hour (12 mph). St. John's has one of the mildest winters in Canada (third mildest city next to Victoria and Vancouver), yet has the most freezing rain days of any major Canadian city. == Hydrography ==
Hydrography
Fresh water Shallow soil and bedrock deeply scored by glaciers are responsible for the numerous lakes and ponds, and short, swift flowing rivers scattered across Newfoundland and Labrador. The area of freshwater in Newfoundland and Labrador is , covering 7.7% of the total surface of area of the province and accounting for 3.5% of the freshwater area of Canada. Approximately 40,000 medium to large icebergs annually calve from Greenland glaciers, and depending on wind, and air and water temperature, between 400 and 800 of these go as far south as 48° north latitude (St. John's). and the hazard is aggravated by dense fog in this area. During the first half of each year the waters off Newfoundland may become covered with floes of sea ice or "pack ice". == Time zones ==
Time zones
Newfoundland is located in a unique time zone in North America. It is a half an hour ahead of Atlantic Time, one and a half hours ahead of Eastern Canada and 4 ½ hours ahead of the west coast of the country. Labrador operates on Atlantic Time, except for the coast between L'Anse au Clair and Norman's Bay, which is on Newfoundland time. == Natural resources ==
Natural resources
All currency is in Canadian dollars. Exploitation of natural resources is a major part of the economic geography of Newfoundland and Labrador. In 2005 the gross domestic product (GDP) of Newfoundland and Labrador was approximately fourteen billion dollars. Service industries accounted for over $8 billion and resource-based activities such as mining, oil production, fishery and forest-based industries (sawmills and paper mills) accounted for the remainder. Minerals and petroleum Mines in Labrador, the iron ore mine at Wabush/Labrador City, and the new nickel mine in Voisey's Bay produced a total of $2.5 billion worth of ore in 2006. A new mine at Duck Pond (30 kilometres (18 mi) south of the now-closed mine at Buchans), started producing copper, zinc, silver and gold in 2007 and prospecting for new ore bodies continues. Mining accounted for 3.5% of the provincial GDP in 2006. Quarries producing dimension stone such as slate and granite, account for less than $10 million worth of material per year. Oil production from offshore oil platforms on Hibernia, White Rose and Terra Nova oil fields on the Grand Banks was which contributed 15% of the provinces GDP in 2006. Total production from the Hibernia field from 1997 to 2006 was with an estimated value of $36 billion. Remaining reserves are estimated at almost as of December 31, 2006. Exploration for new reserves is ongoing. The value of newsprint exports varies greatly from year to year, depending on the global market price. Lumber is produced by numerous mills in Newfoundland. Agriculture Agriculture in Newfoundland in limited to areas south of St. John's, near Deer Lake and in the Codroy Valley. Elsewhere the soil is mostly unsuitable for farming. Potatoes, rutabagas, known locally as "turnips", carrots and cabbage are grown for local consumption. Wild blueberries, partridge berries and bakeapples are harvested commercially and used in jams and wine making. == Human geography ==
Human geography
Newfoundland and Labrador had a population of 505,469 (2005 estimate) and a population density of 1.27 per km2 (3.1 per sq mi). The provincial capital is St. John's, which had a population of 181,113 in 2005). St John's is located at the extreme eastern edge of the island on the Avalon Peninsula. The other cities are Mount Pearl and Corner Brook. Human inhabitation in Newfoundland and Labrador can be traced back over 9,000 years to the people of the Maritime Archaic Tradition. They were gradually displaced by people of the Dorset Culture and finally by the Innu and Inuit in Labrador and the Beothuks on the island. The oldest known European contact was made over a thousand years ago when the Vikings briefly settled in L'Anse aux Meadows. Five hundred years later, European explorers (John Cabot, Gaspar Corte-Real, Jacques Cartier and others), fishermen from England, Portugal, France and Spain and Basque whalers (the remains of several whaling stations have been found at Red Bay, Newfoundland and Labrador) began exploration and exploitation of the area. Early European (primarily from England, Ireland and France) settlement in Newfoundland was confined to the coast. The rich cod fishery on the Grand Banks and along the shore of the island was the primary reason for these settlements. The rugged shoreline provided many small, but isolated, harbors (outports) from which to conduct the fishery. The Avalon Peninsula was, and is, the most populous part of the island, and as such had the best developed system of early roads and trails. Transportation between communities on other parts of the coast, especially the south coast between Fortune Bay and Port aux Basques, was exclusively by boat. Almost all communities are now accessible by roads which are part of the provincial road system. The now-defunct Newfoundland Railway, built in the latter part of the 19th century, and the development of the lead, zinc and copper mine at Buchans and the paper mill in Grand Falls in the early 20th century marked the beginning of the settlement of the interior of the island. Despite these developments the majority of the population is still found along the coast. Settlement of Labrador followed a similar pattern, with the interior being settled only in the latter part of the 20th century with the development of the iron ore mines at Wabush, hydroelectric generation at Churchill Falls and the military base at Goose Bay. Aboriginal peoples include the Innu, Inuit and Métis of Labrador and the Mi'kmaq in Newfoundland. One aboriginal group, the Beothuks, became extinct in the early 19th century. == See also ==
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