Duluth is a major port city in the U. S. state of Minnesota and the county seat of Saint Louis County. Duluth is the 4th largest city in Minnesota, it is the 2nd largest city on Lake Superior. The largest is Thunder Bay, Canada, it has the largest metropolitan area on the lake, with a population of 279,771 in 2010, the second-largest in the state. Situated on the north shore of Lake Superior at the westernmost point of the Great Lakes, Duluth is accessible to oceangoing vessels from the Atlantic Ocean 2,300 miles away via the Great Lakes Waterway and the Saint Lawrence Seaway. Duluth forms a metropolitan area with Wisconsin; the cities share the Duluth–Superior harbor and together are the Great Lakes' largest port, transporting coal, iron ore, grain. A tourist destination for the Midwest, Duluth features the United States' only all-freshwater aquarium, the Great Lakes Aquarium; the city is the starting point for vehicle trips along Minnesota's North Shore. The city is named for Daniel Greysolon, Sieur du Lhut, the first known European explorer of the area.
The Anishinaabe known as the Ojibwe or Chippewa, have inhabited the Lake Superior region for more than 500 years. They were preceded by the Dakota, Menominee and Gros Ventre peoples, whom they pushed out of the area. Established as traders, after the arrival of Europeans, the Anishinaabe found a niche as the middlemen between the French fur traders and other Native peoples, they soon became the dominant Indian nation in the region, forcing out the Dakota Sioux and Fox and winning a victory against the Iroquois west of Sault Ste. Marie in 1662. By the mid-18th century, the Ojibwe occupied all of Lake Superior's shores. For both the Ojibwe and the Dakota, interaction with Europeans during the contact period revolved around the fur trade and related activities; the Ojibwe are known for their crafting of birch bark canoes, use of copper arrow points, cultivation of wild rice. In 1745, they adopted guns from the British for use against the Dakota nation of the Sioux, whom they pushed to the south; the Ojibwe Nation was the first to set the agenda with European-Canadian leaders for signing more detailed treaties before many European settlers were allowed too far west.
The settlement in Ojibwe is Onigamiinsing, a reference to the small and easy portage across Minnesota Point between Lake Superior and western Saint Louis Bay, which forms Duluth's harbor. According to Ojibwe oral history, Spirit Island, near the Spirit Valley neighborhood, was the "Sixth Stopping Place", where the northern and southern branches of the Ojibwe Nation came together and proceeded to their "Seventh Stopping Place" near the present city of La Pointe, Wisconsin; the "Stopping Places" were the places the Native Americans occupied during their westward migration as the Europeans overran their territory. Several factors brought fur traders to the Great Lakes in the early 17th century; the fashion for beaver hats in Europe generated demand for pelts. French trade for beaver in the lower Saint Lawrence River had led to the depletion of the animals in that region by the late 1630s, so the French searched farther west for new resources and new routes, making alliances with the Native Americans along the way to trap and deliver their furs.
Étienne Brûlé is credited with the European discovery of Lake Superior before 1620. Pierre-Esprit Radisson and Médard des Groseilliers explored the Duluth area, Fond du Lac in 1654 and again in 1660; the French soon established fur posts near Duluth and in the far north where Grand Portage became a major trading center. The French explorer Daniel Greysolon, Sieur du Lhut, whose name is sometimes anglicized as "DuLuth", explored the Saint Louis River in 1679. After 1792 and the independence of the United States, the North West Company established several posts on Minnesota rivers and lakes, in areas to the west and northwest, for trading with the Ojibwe, the Dakota, other native tribes; the first post was where Superior, Wisconsin developed. Known as Fort Saint Louis, the post became the headquarters for North West's new Fond du Lac Department, it had stockaded walls, two houses of 40 feet each, a shed of 60 feet, a large warehouse, a canoe yard. Over time, Indian peoples and European Americans settled nearby, a town developed at this point.
In 1808, the American Fur Company was organized by German-born John Jacob Astor. The company began trading at the Head of the Lakes in 1809. In 1817, it erected a new headquarters at present-day Fond du Lac on the Saint Louis River. There, portages connected Lake Superior with Lake Vermillion to the north, with the Mississippi River to the south. After creating a powerful monopoly, Astor got out of the business about 1830, as the trade was declining, but active trade was carried on until the failure of the fur trade in the 1840s. European fashions had changed and many American areas were getting over-trapped, with game declining. Two Treaties of Fond du Lac were signed by natives with the United States in the present neighborhood of Fond du Lac in 1826 and 1847, by which the Ojibwe ceded land to the American government; as part of the Treaty of Washington with the Lake Superior Band of Chippewa, the United States set aside the Fond du Lac Indian Reservation upstream from Duluth near Cloquet, Minnesota.
The Ojibwe population was moved there. As European Americans continued to settle and encroach on Ojibwe lands, the U. S. gove
A spruce is a tree of the genus Picea, a genus of about 35 species of coniferous evergreen trees in the family Pinaceae, found in the northern temperate and boreal regions of the Earth. Spruces are large trees, from about 20–60 m tall when mature, have whorled branches and conical form, they can be distinguished from other members of the pine family by their needles, which are four-sided and attached singly to small persistent peg-like structures on the branches, by their cones, which hang downwards after they are pollinated. The needles are shed. In other similar genera, the branches are smooth. Spruce are used as food plants by the larvae of some Lepidoptera species, such as the eastern spruce budworm, they are used by the larvae of gall adelgids. In the mountains of western Sweden, scientists have found a Norway spruce, nicknamed Old Tjikko, which by reproducing through layering, has reached an age of 9,550 years and is claimed to be the world's oldest known living tree; the word spruce comes from a Middle English adjective spruse which meant from Prussia.
The adjective comes from an unknown alteration of an Old French form of Prussia - Pruce, which itself comes from New Latin, which adapted it from Old Prussian. Spruce and Sprws seem to have been generic terms for commodities brought to England by Hanseatic merchants, the tree thus was believed to be particular to Prussia, which for a time was figurative in England as a land of luxuries. DNA analyses have shown that traditional classifications based on the morphology of needle and cone are artificial. A recent study found that P. breweriana had a basal position, followed by P. sitchensis, the other species were further divided into three clades, suggesting that Picea originated in North America. Spruce has been found in the fossil record from the early Cretaceous, 136 million years ago. Thirty-five named species of spruce exist in the world; the Plant List has 59 accepted spruce names. Basal species: Picea breweriana – Brewer's spruce, Klamath Mountains, North America. Beyond that, determination can become more difficult.
Intensive sampling in the Smithers/Hazelton/Houston area of British Columbia showed Douglas, according to Coates et al. that cone scale morphology was the feature most useful in differentiating species of spruce. Daubenmire, after range-wide sampling, had recognized the importance of the 2 latter characters. Taylor had noted that the most obvious morphological difference
The fur trade is a worldwide industry dealing in the acquisition and sale of animal fur. Since the establishment of a world fur market in the early modern period, furs of boreal and cold temperate mammalian animals have been the most valued; the trade stimulated the exploration and colonization of Siberia, northern North America, the South Shetland and South Sandwich Islands. Today the importance of the fur trade has diminished. Animal rights organizations oppose the fur trade, citing that animals are brutally killed and sometimes skinned alive. Fur has been replaced in some clothing by synthetic imitations, for example, as in ruffs on hoods of parkas. Before the European colonization of the Americas, Russia was a major supplier of fur pelts to Western Europe and parts of Asia, its trade developed in the Early Middle Ages, first through exchanges at posts around the Baltic and Black seas. The main trading market destination was the German city of Leipzig. Kievan Russia, the first Russian State, was the first supplier of the Russian Fur Trade.
Russia exported raw furs, consisting in most cases of the pelts of martens, wolves, foxes and hares. Between the 16th and 18th centuries, Russians began to settle in Siberia, a region rich in many mammal fur species, such as Arctic fox, sable, sea otter and stoat. In a search for the prized sea otter pelts, first used in China, for the northern fur seal, the Russian Empire expanded into North America, notably Alaska. From the 17th through the second half of the 19th century, Russia was the world's largest supplier of fur; the fur trade played a vital role in the development of Siberia, the Russian Far East and the Russian colonization of the Americas. As recognition of the importance of the trade to the Siberian economy, the sable is a regional symbol of the Ural Sverdlovsk Oblast and the Siberian Novosibirsk and Irkutsk Oblasts of Russia; the European discovery of North America, with its vast forests and wildlife the beaver, led to the continent becoming a major supplier in the 17th century of fur pelts for the fur felt hat and fur trimming and garment trades of Europe.
Fur was relied on to make warm clothing, a critical consideration prior to the organization of coal distribution for heating. Portugal and Spain played major roles in fur trading after the 15th century with their business in fur hats. From as early as the 10th century and boyars of Novgorod had exploited the fur resources "beyond the portage", a watershed at the White Lake that represents the door to the entire northwestern part of Eurasia, they began by establishing trading posts along the Volga and Vychegda river networks and requiring the Komi people to give them furs as tribute. Novgorod, the chief fur-trade center prospered as the easternmost trading post of the Hanseatic League. Novgorodians expanded farther east and north, coming into contact with the Pechora people of the Pechora River valley and the Yugra people residing near the Urals. Both of these native tribes offered more resistance than the Komi, killing many Russian tribute-collectors throughout the tenth and eleventh centuries.
As Muscovy gained more power in the 15th century and proceeded in the "gathering of the Russian lands", the Muscovite state began to rival the Novgorodians in the North. During the 15th century Moscow began subjugating many native tribes. One strategy involved exploiting antagonisms between tribes, notably the Komi and Yugra, by recruiting men of one tribe to fight in an army against the other tribe. Campaigns against native tribes in Siberia remained insignificant until they began on a much larger scale in 1483 and 1499. Besides the Novgorodians and the indigenes, Muscovites had to contend with the various Muslim Tatar khanates to the east of Muscovy. In 1552 Ivan IV, the Tsar of All the Russias, took a significant step towards securing Russian hegemony in Siberia when he sent a large army to attack the Kazan Tartars and ended up obtaining the territory from the Volga to the Ural Mountains. At this point the phrase "ruler of Obdor and all Siberian lands" became part of the title of the Tsar in Moscow.
So, problems ensued after 1558 when Ivan IV sent Grigory Stroganov to colonize land on the Kama and to subjugate and enserf the Komi living there. The Stroganov family soon came into conflict with the Khan of Sibir. Ivan told the Stroganovs to hire Cossack mercenaries to protect the new settlement from the Tatars. From ca 1581 the band of Cossacks led by Yermak Timofeyevich fought many battles that culminated in a Tartar victory and the temporary end to Russian occupation in the area. In 1584 Ivan’s son Fyodor sent military governors and soldiers to reclaim Yermak conquests and to annex the land held by the Khanate of Sibir. Similar skirmishes with Tartars took place across Siberia. Russian conquerors treated the natives of Siberia as exploited enemies who were inferior to them; as they penetrated deeper into Siberia, traders built outposts or winter lodges called zimovya where they lived and collected fur tribute from native tribes. By 1620 Russia dominated the land from the Urals eastward to the Yenisey valley and to the Altai Mountains in the south, comprising about 1.25 million square miles of land.
Furs would become Russia's largest source of wealth during the seventeenth centuries. Keeping up with the advances of Western Europe required significant capital and Russia did not have sources of gold and silver, but it did have furs, which became known as "soft gold" and provided Russia with hard cur
In the fields of horticulture and botany, the term deciduous means "falling off at maturity" and "tending to fall off", in reference to trees and shrubs that seasonally shed leaves in the autumn. The term deciduous means "the dropping of a part, no longer needed" and the "falling away after its purpose is finished". In plants, it is the result of natural processes. "Deciduous" has a similar meaning when referring to animal parts, such as deciduous antlers in deer, deciduous teeth in some mammals. Wood from deciduous trees is used in a variety of ways in several industries including lumber for furniture and flooring, bowling pins and baseball bats and furniture, cabinets and paneling. In botany and horticulture, deciduous plants, including trees and herbaceous perennials, are those that lose all of their leaves for part of the year; this process is called abscission. In some cases leaf loss coincides with winter -- namely in polar climates. In other parts of the world, including tropical and arid regions, plants lose their leaves during the dry season or other seasons, depending on variations in rainfall.
The converse of deciduous is evergreen, where foliage is shed on a different schedule from deciduous trees, therefore appearing to remain green year round. Plants that are intermediate may be called semi-deciduous. Other plants are semi-evergreen and lose their leaves before the next growing season, retaining some during winter or dry periods; some trees, including a few species of oak, have desiccated leaves that remain on the tree through winter. Many deciduous plants flower during the period when they are leafless, as this increases the effectiveness of pollination; the absence of leaves improves wind transmission of pollen for wind-pollinated plants and increases the visibility of the flowers to insects in insect-pollinated plants. This strategy is not without risks, as the flowers can be damaged by frost or, in dry season regions, result in water stress on the plant. There is much less branch and trunk breakage from glaze ice storms when leafless, plants can reduce water loss due to the reduction in availability of liquid water during cold winter days.
Leaf drop or abscission involves complex physiological changes within plants. The process of photosynthesis degrades the supply of chlorophylls in foliage; when autumn arrives and the days are shorter or when plants are drought-stressed, deciduous trees decrease chlorophyll pigment production, allowing other pigments present in the leaf to become apparent, resulting in non-green colored foliage. The brightest leaf colors are produced when days grow short and nights are cool, but remain above freezing; these other pigments include carotenoids that are yellow and orange. Anthocyanin pigments produce red and purple colors, though they are not always present in the leaves. Rather, they are produced in the foliage in late summer, when sugars are trapped in the leaves after the process of abscission begins. Parts of the world that have showy displays of bright autumn colors are limited to locations where days become short and nights are cool. In other parts of the world, the leaves of deciduous trees fall off without turning the bright colors produced from the accumulation of anthocyanin pigments.
The beginnings of leaf drop starts when an abscission layer is formed between the leaf petiole and the stem. This layer is formed in the spring during active new growth of the leaf; the cells are sensitive to a plant hormone called auxin, produced by the leaf and other parts of the plant. When auxin coming from the leaf is produced at a rate consistent with that from the body of the plant, the cells of the abscission layer remain connected; the elongation of these cells break the connection between the different cell layers, allowing the leaf to break away from the plant. It forms a layer that seals the break, so the plant does not lose sap. A number of deciduous plants remove nitrogen and carbon from the foliage before they are shed and store them in the form of proteins in the vacuoles of parenchyma cells in the roots and the inner bark. In the spring, these proteins are used as a nitrogen source during the growth of new leaves or flowers. Plants with deciduous foliage have advantages and disadvantages compared to plants with evergreen foliage.
Since deciduous plants lose their leaves to conserve water or to better survive winter weather conditions, they must regrow new foliage during the next suitable growing season. Evergreens suffer greater water loss during the winter and they can experience greater predation pressure when small. Losing leaves in winter may reduce damage from insects. Removing leaves reduces cavitation which can damage xylem vessels in plants; this allows deciduous plants to have xylem vessels with larger diameters and therefore a greater rate of transpiration during the summer growth period
A glacier is a persistent body of dense ice, moving under its own weight. Glaciers deform and flow due to stresses induced by their weight, creating crevasses and other distinguishing features, they abrade rock and debris from their substrate to create landforms such as cirques and moraines. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets in the polar regions, but glaciers may be found in mountain ranges on every continent including Oceania's high-latitude oceanic island countries such as New Zealand and Papua New Guinea. Between 35°N and 35°S, glaciers occur only in the Himalayas, Rocky Mountains, a few high mountains in East Africa, New Guinea and on Zard Kuh in Iran. Glaciers cover about 10 percent of Earth's land surface. Continental glaciers cover nearly 13 million km2 or about 98 percent of Antarctica's 13.2 million km2, with an average thickness of 2,100 m.
Greenland and Patagonia have huge expanses of continental glaciers. Glacial ice is the largest reservoir of fresh water on Earth. Many glaciers from temperate and seasonal polar climates store water as ice during the colder seasons and release it in the form of meltwater as warmer summer temperatures cause the glacier to melt, creating a water source, important for plants and human uses when other sources may be scant. Within high-altitude and Antarctic environments, the seasonal temperature difference is not sufficient to release meltwater. Since glacial mass is affected by long-term climatic changes, e.g. precipitation, mean temperature, cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change and are a major source of variations in sea level. A large piece of compressed ice, or a glacier, appears blue, as large quantities of water appear blue; this is. The other reason for the blue color of glaciers is the lack of air bubbles. Air bubbles, which give a white color to ice, are squeezed out by pressure increasing the density of the created ice.
The word glacier is a loanword from French and goes back, via Franco-Provençal, to the Vulgar Latin glaciārium, derived from the Late Latin glacia, Latin glaciēs, meaning "ice". The processes and features caused by or related to glaciers are referred to as glacial; the process of glacier establishment and flow is called glaciation. The corresponding area of study is called glaciology. Glaciers are important components of the global cryosphere. Glaciers are categorized by their morphology, thermal characteristics, behavior. Cirque glaciers form on the slopes of mountains. A glacier that fills a valley is called a valley glacier, or alternatively an alpine glacier or mountain glacier. A large body of glacial ice astride a mountain, mountain range, or volcano is termed an ice cap or ice field. Ice caps have an area less than 50,000 km2 by definition. Glacial bodies larger than 50,000 km2 are called continental glaciers. Several kilometers deep, they obscure the underlying topography. Only nunataks protrude from their surfaces.
The only extant ice sheets are the two that cover most of Greenland. They contain vast quantities of fresh water, enough that if both melted, global sea levels would rise by over 70 m. Portions of an ice sheet or cap that extend into water are called ice shelves. Narrow, fast-moving sections of an ice sheet are called ice streams. In Antarctica, many ice streams drain into large ice shelves; some drain directly into the sea with an ice tongue, like Mertz Glacier. Tidewater glaciers are glaciers that terminate in the sea, including most glaciers flowing from Greenland, Antarctica and Ellesmere Islands in Canada, Southeast Alaska, the Northern and Southern Patagonian Ice Fields; as the ice reaches the sea, pieces break off, or calve. Most tidewater glaciers calve above sea level, which results in a tremendous impact as the iceberg strikes the water. Tidewater glaciers undergo centuries-long cycles of advance and retreat that are much less affected by the climate change than those of other glaciers.
Thermally, a temperate glacier is at melting point throughout the year, from its surface to its base. The ice of a polar glacier is always below the freezing point from the surface to its base, although the surface snowpack may experience seasonal melting. A sub-polar glacier includes both temperate and polar ice, depending on depth beneath the surface and position along the length of the glacier. In a similar way, the thermal regime of a glacier is described by its basal temperature. A cold-based glacier is below freezing at the ice-ground interface, is thus frozen to the underlying substrate. A warm-based glacier is above or at freezing at the interface, is able to slide at this contact; this contrast is thought to a large extent to govern the ability of a glacier to erode its bed, as sliding ice promotes plucking at rock from the surface below. Glaciers which are cold-based and warm-based are known as polythermal. Glaciers form where the accumulation of ice exceeds ablation. A glacier originates from a landform called'cirque' – a armchair-shaped geological feature (such as a depressio
Populus tremuloides is a deciduous tree native to cooler areas of North America, one of several species referred to by the common name aspen. It is called quaking aspen, trembling aspen, American aspen, mountain or golden aspen, trembling poplar, white poplar, popple, as well as others; the trees have tall trunks, up to 25 meters tall, with smooth pale bark, scarred with black. The glossy green leaves, dull beneath, become golden to yellow red, in autumn; the species propagates through its roots to form large clonal groves originating from a shared root system. These roots are not rhizomes, as new growth develops from adventitious buds on the parent root system. Populus tremuloides is the most distributed tree in North America, being found from Canada to central Mexico, it is the defining species of the aspen parkland biome in the Prairie Provinces of Canada and extreme northwest Minnesota. The Quaking Aspen is the state tree of Utah; the quaking or trembling of the leaves, referred to in the common names is due to the flexible flattened petioles.
The specific epithet, evokes this trembling behavior and can be translated as "like tremula", the European trembling aspen. Quaking aspen is a tall, fast growing tree 20–25 m at maturity, with a trunk 20 to 80 cm in diameter; the bark is smooth, colored greenish-white to gray, is marked by thick black horizontal scars and prominent black knots. Parallel vertical scars are tell-tale signs of elk, which strip off aspen bark with their front teeth; the leaves on mature trees are nearly round, 4–8 centimeters in diameter with small rounded teeth, a 3–7-centimeter long, flattened petiole. Young trees and root sprouts have much larger nearly triangular leaves; some species of Populus have petioles flattened along their length, while the aspens and some other poplars have them flattened from side to side along the entire length of the petiole. Aspens are dioecious, with separate male and female clones; the flowers are catkins. Quaking aspen occurs across Canada in all provinces and territories, with the possible exception of Nunavut.
In the United States, it can be found as far north as the northern foothills of the Brooks Range in Alaska, where road margins and gravel pads provide islands of well-drained habitat in a region where soils are waterlogged due to underlying permafrost. It occurs at low elevations as far south as central Indiana. In the western United States, this tree survives at elevations lower than 1,500 feet due to hot summers experienced below that elevation, is found at 5,000–12,000 feet, it grows at high altitudes as far south as Mexico. Quaking aspen grows in a wide variety of climatic conditions. January and July average temperatures range from −30 °C and 16 °C in the Alaska Interior to −3 °C and 23 °C in Fort Wayne, Indiana. Average annual precipitation ranges from 1,020 mm in Gander and Labrador to as little as 180 mm in the Alaska Interior; the southern limit of the species' range follows the 24 °C mean July isotherm. Shrub-like dwarf clones exist in marginal environments too cold and dry to be hospitable to full-size trees, for example at the species' upper elevation limits in the White Mountains.
Quaking aspen propagates itself through root sprouts, extensive clonal colonies are common. Each colony is its own clone, all trees in the clone have identical characteristics and share a single root structure. A clone may turn color earlier or in the fall than its neighbouring aspen clones. Fall colors are bright tones of yellow; as all trees in a given clonal colony are considered part of the same organism, one clonal colony, named Pando, is considered the heaviest and oldest living organism at six million kilograms and 80,000 years old. Aspens do produce seeds, but grow from them. Pollination is inhibited by the fact that aspens are either male or female, large stands are all clones of the same sex. If pollinated, the small seeds are only viable a short time as they lack a stored food source or a protective coating. Beginning in 1996, individual North American scientists noticed an increase in dead or dying aspen trees; as this accelerated in 2004, word spread and a debate over causes began.
No insect, disease, or environmental condition is yet identified as a joint cause. Trees adjacent to one another are stricken or not. In other instances, entire groves have died. Many areas of the Western US have experienced increased diebacks which are attributed to ungulate grazing and wildfire suppression. At high altitudes where grasses can be rare, ungulates can browse young aspen sprouts and prevent those young trees from reaching maturity; as a result, some aspen groves close to cattle or other grazing animals, such as deer or elk, have few young trees and can be invaded by conifers, which are not browsed. Another possible deterrent to aspen regeneration is widespread wildfire suppression. Aspens are vigorous resprouters and though
In Canada, the First Nations are the predominant indigenous peoples in Canada south of the Arctic Circle. Those in the Arctic area are distinct and known as Inuit; the Métis, another distinct ethnicity, developed after European contact and relations between First Nations people and Europeans. There are 634 recognized First Nations governments or bands spread across Canada half of which are in the provinces of Ontario and British Columbia. Under the Employment Equity Act, First Nations are a "designated group", along with women, visible minorities, people with physical or mental disabilities. First Nations are not defined as a visible minority under the Act or by the criteria of Statistics Canada. North American indigenous; some of their oral traditions describe historical events, such as the Cascadia earthquake of 1700 and the 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of Discovery, beginning in the late 15th century.
European accounts by trappers, traders and missionaries give important evidence of early contact culture. In addition and anthropological research, as well as linguistics, have helped scholars piece together an understanding of ancient cultures and historic peoples. Although not without conflict, Euro-Canadians' early interactions with First Nations, Métis, Inuit populations were less combative compared to the violent battles between colonists and native peoples in the United States. Collectively, First Nations, Métis peoples constitute Indigenous peoples in Canada, Indigenous peoples of the Americas, or first peoples. First Nation as a term became used beginning in 1980s to replace the term Indian band in referring to groups of Indians with common government and language; the term had come into common usage in the 1970s to avoid using the word Indian, which some Canadians considered offensive. No legal definition of the term exists; some indigenous peoples in Canada have adopted the term First Nation to replace the word band in the formal name of their community.
A band is a "body of Indians for whose use and benefit in common lands... have been set apart... moneys are held... or declared... to be a band for the purposes of" the Indian Act by the Canadian Crown. The term Indian is a misnomer given to indigenous peoples of North America by European explorers who erroneously thought they had landed on the Indian subcontinent; the use of the term Native Americans, which the US government and others have adopted, is not common in Canada. It refers more to the Indigenous peoples residing within the boundaries of the United States; the parallel term Native Canadian is not used, but Native and autochtone are. Under the Royal Proclamation of 1763 known as the "Indian Magna Carta," the Crown referred to indigenous peoples in British territory as tribes or nations; the term First Nations is capitalized. Bands and nations may have different meanings. Within Canada, First Nations has come into general use for indigenous peoples other than Inuit and Métis. Individuals using the term outside Canada include U.
S. tribes within the Pacific Northwest, as well as supporters of the Cascadian independence movement. The singular used on culturally politicized reserves, is the term First Nations person. A more recent trend is for members of various nations to refer to themselves by their tribal or national identity only, e.g. "I'm Haida". For pre-history, see: Paleo-Indians and Archaic periods First Nations by linguistic-cultural area: List of First Nations peoplesFirst Nations peoples had settled and established trade routes across what is now Canada by 1,000 BC to 500 BC. Communities developed, each with its own culture and character. In the northwest were the Athapaskan-speaking peoples, Slavey, Tłı̨chǫ, Tutchone-speaking peoples, Tlingit. Along the Pacific coast were the Haida, Kwakiutl, Nuu-chah-nulth, Nisga'a and Gitxsan. In the plains were the Blackfoot, Kainai and Northern Peigan. In the northern woodlands were the Chipewyan. Around the Great Lakes were the Anishinaabe, Algonquin and Wyandot. Along the Atlantic coast were the Beothuk, Innu and Micmac.
The Blackfoot Confederacies reside in the Great Plains of Montana and Canadian provinces of Alberta, British Columbia and Saskatchewan. The name "Blackfoot" came from the colour of the peoples' leather footwear, known as moccasins, they had painted the bottoms of their moccasins black. One account claimed that the Blackfoot Confederacies walked through the ashes of prairie fires, which in turn coloured the bottoms of their moccasins black, they had migrated onto the Great Plains from the Plateau area. The Blackfoot may have lived in their homeland since the end of the Pleistocene 11,000 years ago.. For thousands of years, they managed the prairie to support bison herds and cultivated berries and edible roots, they allowed only legitimate traders into their territory, making treaties only when the bison herds were exterminated in the 1870s. The Squamish history is a series of past events, both passed on through oral tradition and recent history, of the Squamish indigenous peoples of the Pacific Northwest Coast.
Prior to colonization, they recorded their history through oral tradition as a way to transmit stories and knowledge across generations. This was common among all the peoples; the writing system esta