1.
Quebec
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Quebec is the second-most populous province of Canada and the only one to have a predominantly French-speaking population, with French as the sole provincial official language. Quebec is Canadas largest province by area and its second-largest administrative division and it also shares maritime borders with Nunavut, Prince Edward Island, and Nova Scotia. Quebec is Canadas second-most populous province, after Ontario, most inhabitants live in urban areas near the Saint Lawrence River between Montreal and Quebec City, the capital. Approximately half of Quebec residents live in the Greater Montreal Area, the Nord-du-Québec region, occupying the northern half of the province, is sparsely populated and inhabited primarily by Aboriginal peoples. Even in central Quebec at comparatively southerly latitudes winters are severe in inland areas, Quebec independence debates have played a large role in the politics of the province. Parti Québécois governments held referendums on sovereignty in 1980 and 1995, in 2006, the House of Commons of Canada passed a symbolic motion recognizing the Québécois as a nation within a united Canada. These many industries have all contributed to helping Quebec become an economically influential province within Canada, early variations in the spelling of the name included Québecq and Kébec. French explorer Samuel de Champlain chose the name Québec in 1608 for the colonial outpost he would use as the seat for the French colony of New France. The province is sometimes referred to as La belle province, the Province of Quebec was founded in the Royal Proclamation of 1763 after the Treaty of Paris formally transferred the French colony of Canada to Britain after the Seven Years War. The proclamation restricted the province to an area along the banks of the Saint Lawrence River, the Treaty of Versailles ceded territories south of the Great Lakes to the United States. After the Constitutional Act of 1791, the territory was divided between Lower Canada and Upper Canada, with each being granted an elected legislative assembly, in 1840, these become Canada East and Canada West after the British Parliament unified Upper and Lower Canada into the Province of Canada. This territory was redivided into the Provinces of Quebec and Ontario at Confederation in 1867, each became one of the first four provinces. In 1898, the Canadian Parliament passed the first Quebec Boundary Extension Act that expanded the provincial boundaries northward to include the lands of the aboriginal peoples. This was followed by the addition of the District of Ungava through the Quebec Boundaries Extension Act of 1912 that added the northernmost lands of the Inuit to create the modern Province of Quebec. In 1927, the border between Quebec and Newfoundland and Labrador was established by the British Judicial Committee of the Privy Council. Located in the part of Canada, and part of Central Canada. Its topography is very different from one region to another due to the composition of the ground, the climate. The Saint Lawrence Lowland and the Canadian Shield are the two main regions, and are radically different
2.
Capitale-Nationale
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Capitale-Nationale is one of 17 administrative regions of Quebec, Canada. Quebec City, Quebecs centre of government, is located in this region and it has a land area of 18,796.86 km2. It reported a resident population of 700,616 as of the Canada 2011 Census. Prior to January 2000, it was known as the Québec administrative region, regional County Municipalities Independent Parish Notre-Dame-des-Anges Native Peoples Reserve Wendake Francophone, Commission scolaire de Charlevoix
3.
Saint Lawrence River
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The Saint Lawrence River is a large river in the middle latitudes of North America. The Saint Lawrence River flows in a roughly north-easterly direction, connecting the Great Lakes with the Atlantic Ocean and forming the primary drainage outflow of the Great Lakes Basin. It traverses the Canadian provinces of Quebec and Ontario, and is part of the boundary between Ontario, Canada, and the U. S. state of New York. This river also provides the basis of the commercial Saint Lawrence Seaway, the estuary begins at the eastern tip of Île dOrléans, just downstream from Quebec City. The river becomes tidal around Quebec City, the St. Lawrence River runs 3,058 kilometres from the farthest headwater to the mouth and 1,197 km from the outflow of Lake Ontario. The farthest headwater is the North River in the Mesabi Range at Hibbing, the average discharge below the Saguenay River is 16,800 cubic metres per second. At Quebec City, it is 12,101 m3/s, the average discharge at the rivers source, the outflow of Lake Ontario, is 7,410 m3/s. The St. Lawrence River includes Lake Saint-Louis south of Montreal, Lake Saint Francis at Salaberry-de-Valleyfield, pierre Archipelago and the smaller Mingan Archipelago. Other islands include Île dOrléans near Quebec City and Anticosti Island north of the Gaspé and it is the second longest river in Canada. Lake Champlain and the Ottawa, Richelieu, Saguenay, and Saint-François rivers drain into the St. Lawrence. The St. Lawrence River is in an active zone where fault reactivation is believed to occur along late Proterozoic to early Paleozoic normal faults related to the opening of Iapetus Ocean. The faults in the area are related and are called the Saint Lawrence rift system. According to the United States Geological Survey, the St. Lawrence Valley is a province of the larger Appalachian division, containing the Champlain. However, in Canada, where most of the valley is, it is considered part of a distinct Saint Lawrence Lowlands physiographic division. Lawrence River itself was Jacques Cartier, at that time, the land along the river was inhabited by the St. Lawrence Iroquoians, at the time of Cartiers second voyage in 1535. Because Cartier arrived in the estuary on St. Lawrences feast day, the St. Lawrence River is partly within the U. S. and as such is that countrys sixth oldest surviving European place-name. The earliest regular Europeans in the area were the Basques, who came to the St Lawrence Gulf, the Basque whalers and fishermen traded with indigenous Americans and set up settlements, leaving vestiges all over the coast of eastern Canada and deep into the Saint Lawrence River. Basque commercial and fishing activity reached its peak before the Armada Invencibles disaster, initially, the whaling galleons from Labourd were not affected by the Spanish defeat
4.
Donnacona, Quebec
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Donnacona is an industrial town located about 40 kilometres west of Quebec City in Portneuf County, Quebec, Canada. Some people believe the city was named after Donnacona, a 16th-century St. Lawrence Iroquois chief who was taken to France, the chieftain lived further down-river in Stadacona. It was actually named after the first paper mill erected at the mouth of the Jacques-Cartier River and it was located where the Jacques-Cartier River meets the St. Lawrence River. The local paper mill played a key role in creating and quickly developing the settlement to the point of making Donnacona the most populous urban town in Portneuf County. Economic difficulties affected the lumber and pulp and paper industry and the factory was sold a number of times. In 2007, Bowater had a debt of $7 billion and merged with Abitibi-Consolidated, the merger was to sell off Abitibis assets and close its mills for liquidity to settle Bowaters debt. It had employed 240 people manufacturing of 230,000 tonnes per annum of commercial grade paper, the demolition was scheduled to take 12 to 14 months. For three years, the town tried to find an entrepreneur to restart the industry. Prior to the chartering of Donnacona as a town in 1915, the Federal Correctional Service Canada maximum security Donnacona Institution is located along Route 138. Autoroute 40 passes through the town and its sister city is Jarnac, France
5.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
6.
Quebec City
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Quebec City, French, Ville de Québec, officially Québec) is the capital city of the Canadian province of Quebec. Founded in 1608 by Samuel de Champlain, Quebec City is one of the oldest cities in North America. The citys landmarks include the Château Frontenac, a hotel which dominates the skyline, and La Citadelle, the National Assembly of Quebec, the Musée national des beaux-arts du Québec, and the Musée de la civilisation are found within or near Vieux-Québec. Thus, Québec is officially spelled with an accented é in both Canadian English and French, although the accent is not used in common English usage. Quebec City is one of the oldest European settlements in North America, while many of the major cities in Latin America date from the sixteenth century, among cities in Canada and the U. S. few were created earlier than Quebec City. Also, Quebecs Old Town is the only North American fortified city north of Mexico whose walls still exist, French explorer Jacques Cartier built a fort at the site in 1535, where he stayed for the winter before going back to France in spring 1536. He came back in 1541 with the goal of building a permanent settlement, Quebec was founded by Samuel de Champlain, a French explorer and diplomat on 3 July 1608, and at the site of a long abandoned St. Lawrence Iroquoian settlement called Stadacona. Champlain, also called The Father of New France, served as its administrator for the rest of his life, the name Canada refers to this settlement. Although called the cradle of the Francophone population in North America, the place seemed favourable to the establishment of a permanent colony. In 1629 there was the surrender of Quebec, without battle, however, Samuel de Champlain argued that the English seizing of the lands was illegal as the war had already ended, he worked to have the lands returned to France. As part of the negotiations of their exit from the Anglo-French War. These terms were signed into law with the Treaty of Saint-Germain-en-Laye, the lands in Quebec and Acadia were returned to the French Company of One Hundred Associates. In 1665, there were 550 people in 70 houses living in the city, one-quarter of the people were members of religious orders, secular priests, Jesuits, Ursulines nuns and the order running the local hospital, Hotel-Dieu. Quebec City was the headquarters of many raids against New England during the four French, in the last war, the French and Indian War, Quebec City was captured by the British in 1759 and held until the end of the war in 1763. France ceded New France, including the city, to Britain in 1763, at the end of French rule in 1763, forests, villages, fields and pastures surrounded the town of 8,000 inhabitants. The town distinguished itself by its architecture, fortifications, affluent homes of masonry and shacks in the suburbs of Saint-Jean. Despite its urbanity and its status as capital, Quebec City remained a small city with close ties to its rural surroundings. Nearby inhabitants traded their farm surpluses and firewood for imported goods from France at the two city markets, during the American Revolution revolutionary troops from the southern colonies assaulted the British garrison in an attempt to liberate Quebec City, in a conflict now known as the Battle of Quebec
7.
Laurentian mountains
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The Gatineau, LAssomption, Lièvre, Montmorency, Nord and St. Maurice rivers rise in lakes in this mountain range. Across the U. S. border to the south, the Adirondack Mountains in New York State, although Laurentides is one of Quebecs official regions, the mountain range of the same name runs through four other regions, Capitale-Nationale, Outaouais, Lanaudière, and Mauricie. Extending into central Ontario, the foothills of the Laurentian range are known as the Opeongo Hills, the Laurentian Mountain range is one of the oldest mountain ranges in the world. It contains rocks deposited before the Cambrian Period 540 million years ago, the Laurentians are the central part of the Grenville orogeny dating back to around a billion years
8.
Canadian Shield
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Composed of igneous rock resulting from its long volcanic history, the area is covered by a thin layer of soil. Human population is sparse, and industrial development is minimal, while mining is prevalent, the Canadian Shield is a physiographic division, consisting of five smaller, physiographic provinces, the Laurentian Upland, Kazan Region, Davis, Hudson and James. The shield extends into the United States as the Adirondack Mountains, the Canadian Shield is U-shaped and is a subsection of the Laurentia craton signifying the area of greatest glacial impact creating the thin soils. The Canadian Shield is more than 3.96 billion years old, the Canadian Shield once had jagged peaks, higher than any of todays mountains, but millions of years of erosion have changed these mountains to rolling hills. The Canadian Shield was the first part of North America to be elevated above sea level and has remained almost wholly untouched by successive encroachments of the sea upon the continent. It is the Earths greatest area of exposed Archean rock, the metamorphic base rocks are mostly from the Precambrian Supereon, and have been repeatedly uplifted and eroded. Today it consists largely of an area of low relief 300 to 610 m above sea level with a few monadnocks, during the Pleistocene Epoch, continental ice sheets depressed the land surface, scooped out thousands of lake basins, and carried away much of the regions soil. When the Greenland section is included, the Shield is approximately circular, bounded on the northeast by the northeast edge of Greenland and it covers much of Greenland, Labrador, most of Quebec north of the St. In total, the area of the Shield covers approximately 8,000,000 km2. The underlying rock structure also includes Hudson Bay, the Canadian Shield is among the oldest on earth, with regions dating from 2.5 to 4.2 billion years. The multitude of rivers and lakes in the region is caused by the watersheds of the area being so young. It has some of the oldest volcanoes on the planet and it has over 150 volcanic belts whose bedrock ranges from 600 to 1200 million years old. Each belt probably grew by the coalescence of accumulations erupted from numerous vents, many of Canadas major ore deposits are associated with Precambrian volcanoes. The Sturgeon Lake Caldera in Kenora District, Ontario, is one of the worlds best preserved mineralized Neoarchean caldera complexes, the Canadian Shield also contains the Mackenzie dike swarm, which is the largest dike swarm known on Earth. 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 Earths surface, the high pressures and temperatures at those depths provided ideal conditions for mineralization. Although these mountains are now eroded, many large mountains still exist in Canadas far north called the Arctic Cordillera. This is a vast deeply dissected mountain range, stretching from northernmost Ellesmere Island to the northernmost tip of Labrador, the ranges highest peak is Nunavuts Barbeau Peak at 2,616 metres above sea level
9.
St. Lawrence Lowlands
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The Great Lakes-St. Lawrence Lowland is a bowl-shaped area located near to the Great Lakes. The Great Lakes basin area became a lake after the ice sheet melted. However, due to the presence of a deep faultline, all of water was eventually siphoned into the ocean. Thus, the primary defining historic feature of the lowlands the presence of deep soils within the watershed, the lowlands are split into these sub-regions by intrusions from adjacent physiographic regions. The next notable pinching occurs at Quebec City, where again the Shield meets the shore, anticosti and Newfoundland, both being islands, are separated by stretches of open salt water. There are animals such as warblers, wolves, snowshoe hares, blue birds, white-tailed deer, red-winged black birds, coyotes, frogs, eagles, and beavers. Even though the St. Lawrence Lowlands is the smallest landform region in Canada, it has a dense population, the Lowlands are abundant with agriculture, commerce, recreation locations, and transportation hubs. The St. Lawrence Lowlands is the most heavily industrialized landform in Canada and it is 70% of Canadas manufacturing systems and also 70% farm land. The soil is good for agricultural uses. It has the most fertile top soil in Canada
10.
Pont-Rouge
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Pont-Rouge is a city along the Jacques-Cartier River in southern Quebec, Canada. In the Canada 2011 Census the population was 8,723 inhabitants, the first efforts to colonise the area came around 1769. On April 15,1867, the archbishop of Quebec, Charles-François Baillargeon, founded the parish of Sainte-Jeanne-de-Neuville from portions of Cap-Santé, Saint-Basile, and Neuville. After the separation of the parish in two in 1911, the new City of Pont-Rouge was established when these two merged on January 3,1996. Transportation had considerable influence on the development of the parish, mainly the two bridges and the construction of the Canadian Pacific Railway bridge in 1874, the Royal Bridge, was reconstructed several times because of the weakness of the centre of the bridge. This bridge served its purpose for the transportation of heavy loads, the bridge was a toll bridge, and the money served the construction of a second bridge le pont Rouge, which was free. It united the western part to the part of Dupont Street, named in honour of Father Charles-François Dupont. A newer bridge has now replaced this bridge as of 2009. 7% French as first language,98. 2% English and French as first language, 0% Other as first language,1. 1%
11.
Laurentides Wildlife Reserve
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Réserve faunique des Laurentides is a wildlife reserve in Quebec, Canada, located between Quebec City and the Saguenay–Lac-Saint-Jean region. The territory of the reserve has over 2000 lakes and many summits of over 1000 meters, the reserve is known by outdoor enthusiasts for hunting and fishing. The reserve, often called the park by locals, is split in half by route 175, linking the cities of Quebec, route 169 leads to Hebertville, the main entrance to the Lac St-Jean area. Parc des Laurentides was created in 1895 as a forest reserve, réserve faunique des Laurentides - official site
12.
Jacques-Cartier National Park
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Jacques-Cartier National Park is a provincial park located 50 kilometres north of Quebec City. The park aims to protect wildlife in the Laurentian massif and it lies within the Eastern forest-boreal transition ecoregion. The Montagnais and the Huron peoples used to inhabit lands that make up Jacques-Cartier National Park. During the 17th century, Hurons worked as guides for Jesuits who wanted to travel between Quebec City and Lac Saint-Jean without using the St. Lawrence River, starting in the mid-19th century, the area was a major producer of lumber. Due to pressure from the American conservationist movement, the Laurentian Wildlife Reserve, the end of World War II, as well as improved road networks, brought in an considerable increase in the number of visitors to the area. In 1972, Hydro-Québec proposed building a dam on the Jacques-Cartier river, due to public pressure, the project was abandoned in 1975. That same year saw the end of the lumber industry in the region. In 1981, Jacques-Cartier National Park was created from the southernmost lands of the Laurentian Wildlife Reserve, Jacques-Cartier National Park is located in the Laurentian Mountains along the Jacques-Cartier River valley, to the west of Quebec Route 175. Jacques-Cartier is a 30 minutes drive from Québec City, grands-Jardins National Park is located to the northeast of the park, while the Laurentian Wildlife Reserve is located to the north. The park is located near the Canadian Forces military base CFB Valcartier. The park contains several glacial landforms such as drumlins and moraine, the most prominent glacial landform in Jacques-Cartier National Park is the Jacques-Cartier Valley. The U-shaped valley is 550 metres deep and was formed during the last glacial period, the plateau consists mainly of coniferous trees such as the black spruce, while the valley consists mainly of deciduous trees such as sugar maple and yellow birch. The invasive Japanese knotweed has also appeared in the parks boundaries, the wildlife is typical of a boreal forest. Animals that can be found in the park include moose, caribou, white-tailed deer, gray wolf, red fox, the Canada lynx, the bear, river otter, porcupine. Atlantic salmon, brook trout and the Arctic char can be found in the lakes, the park is also visited by more than 100 species of birds. Jacques-Cartier National Park had 145,600 visitors in 2005, with a third of visitors coming from outside the region. Activities at the park include 100 kilometres of hiking trails,30 kilometres of biking trails, accommodations at the park include 9 cabins,5 yurts and 114 campsites. In 2009, the park underwent a $2.3 million renovation to modernize and build new infrastructure such as roads and cottages
13.
Glaciated valley
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A valley is a low area between hills, often with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide, the terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of two main types or a mixture of them, with respect to the cross section of the slopes or hillsides. A valley in its broadest geographic sense is known as a dale. A valley through which a river runs may also be referred to as a vale, a small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath, a mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow, a deep, narrow valley is known as a cwm. Similar geological structures, such as canyons, ravines, gorges, gullies, chines, a valley formed by erosion is called an erosional valley, a valley formed by geologic events such as drop faults or the rise of highlands is called a structural valley. A valley formed by flowing water, or river valley, is usually V-shaped, the exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls, shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment, in prehistory, the rivers were used as a source of fresh water and food, as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, most of the first civilizations developed from these river valley communities. In geography, a vale is a river valley, usually with a particularly wide flood plain or flat valley bottom. In Southern England, vales commonly occur between the escarpment slopes of pairs of chalk formations, where the dome has been eroded, exposing less resistant underlying rock. Rift valleys, such as the Albertine Rift, are formed by the expansion of the Earths crust due to tectonic activity beneath the Earths surface, there are various forms of valley associated with glaciation that may be referred to as glacial valleys. A valley carved by glaciers is normally U-shaped, the valley becomes visible upon the recession of the glacier that forms it. When the ice recedes or thaws, the remains, often littered with small boulders that were transported within the ice. Floor gradient does not affect the shape, it is the glaciers size that does
14.
Glaciation
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A glacial period is an interval of time within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the hand, are periods of warmer climate between glacial periods. The last glacial period ended about 15,000 years ago, the Holocene epoch is the current interglacial. A time when there are no glaciers on Earth is considered a greenhouse climate state, within the Quaternary glaciation, there have been a number of glacials and interglacials. The last glacial period was the most recent glacial period within the current ice age, occurring in the Pleistocene epoch, the glacial advance reached its maximum extent about 18,000 BP. In Europe, the ice sheet reached northern Germany, since orbital variations are predictable, computer models that relate orbital variations to climate can predict future climate possibilities. Work by Berger and Loutre suggests that the current warm climate may last another 50,000 years
15.
Hurons
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By the 15th century, the pre-contact Wyandots settled in the large area from the north shores of most of present-day Lake Ontario, northwards up to Georgian Bay. They were located in the part of what is now the Canadian province of Ontario around Georgian Bay. Drastically reduced in number by epidemic diseases after 1634, they were dispersed by war in 1649 from the Iroquois, today the Wyandot have a First Nations reserve in Quebec, Canada. They also have three major settlements in the United States, two of which have independently governed, federally recognized tribes, due to differing development of the groups, they speak distinct forms of Wendat and Wyandot languages. Early theories placed Huron origin in the St. Lawrence Valley, with some arguing for a presence near Montreal, in 1975 and 1978, archeologists excavated a large 15th-century Huron village, now called the Draper Site, in Pickering, Ontario near Lake Ontario. In 2003 a larger village was discovered five kilometres away in Whitchurch-Stouffville, the sites each were surrounded by a palisade, as was typical of Iroquoian cultures. The Mantle Site had more than 70 multi-family longhouses, subsequently they moved from there to their historic territory on Georgian Bay, where they were encountered by Champlain in 1615. In the early 17th century, this Iroquoian people called themselves the Wendat, the Wendat historic territory was bordered on three sides, by the waters of Georgian Bay and Lake Simcoe. Early French explorers referred to these natives as the Huron, either from the French huron, according to tradition, French sailors thought that the bristly hairstyle of Wendat warriors resembled that of a boar. However, these negative etymological meanings conflict with the bon Iroquois attitude held by the French fur traders and explorers, an alternate etymology is from the Algonquin words ronon, or Irri-ronon. It was pronounced Hirri-ronon by the French, eventually shortened to Hirr-on, other etymological possibilities come from the Algonquin words ka-ron or tu-ron. The Wendat were not a tribe, but a confederacy of four or more tribes with mutually intelligible languages, according to tradition, this Wendat Confederacy was initiated by the Attignawantans and the Attigneenongnahacs, who made their alliance in the 15th century. They were joined by the Arendarhonons about 1590, and the Tahontaenrats around 1610, a fifth group, the Ataronchronons, may not have attained full membership in the confederacy, and may have been a division of the Attignawantan. The largest Wendat settlement, and capital of the confederacy, was located at Ossossane, near modern-day Elmvale and they called their traditional territory Wendake. Closely related to the people of the Huron Confederacy were the Tionontate and they lived further south and were divided into two groups, the Deer and the Wolves. Considering that they formed the nucleus of the later known as the Wyandot. Tuberculosis was endemic among the Huron, aggravated by the close, despite this, the Huron on the whole were healthy, the Jesuits wrote that the Huron effectively employed natural remedies and were more healthy than we. The earliest written accounts of the Huron were made by the French, news of the Europeans reached the Huron, particularly when Samuel de Champlain explored the Saint Lawrence River in the early 17th century
16.
Innu people
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Their population in 2003 included about 18,000 people, of which around 14,000 lived in Quebec, under 3000 in Labrador, and the rest outside their traditional territory. Their ancestors were known to have lived on these lands as hunter-gatherers for several thousand years and their subsistence activities were historically centred on hunting and trapping caribou, moose, deer and small game. Some coastal clans also practised agriculture, fished, and managed maple sugarbush and their language, Innu or Ilnu, is spoken throughout Nitassinan, with certain dialect differences. It is part of Cree language group, and unrelated with neighboring Inuit languages, the Innu were allied with neighbouring Atikamekw, Maliseet and Algonquin against their traditional enemies, the Mikmaq and Iroquois. During the Beaver Wars the Iroquois repeatedly invaded their territories, and enslaved women and warriors, since these raids were made by the Iroquois with unprecedented brutality, the Innu themselves adopted the torment, torture, and cruelty of their enemies. The Naskapi, on the hand, were usually in conflicts with the southward advancing Inuit in the east. The Innu recognize several distinctions based on different regional affiliations and various dialects of the Innu language, the word Naskapi was first recorded by French colonists in the 17th century and was subsequently applied to Innu groups beyond the reach of missionary influence. It particularly applied to living in the lands which bordered Ungava Bay. It is here that the term came to be used for the Naskapi First Nation, the Naskapi are traditionally nomadic peoples, in contrast with the more sedentary Montagnais, who establish settled territories. Mushuau Innuat, while related to the Naskapi, split off from the tribe in the 1900s and they were subject to a government relocation program at Davis Inlet. Some of the families of the Naskapi Nation of Kawawachikamach have close relatives in the Cree village of Whapmagoostui, on the eastern shore of Hudson Bay. Since 1990, the Montagnais people have chosen to be officially referred to as the Innu. On July 29,1609, at Ticonderoga or Crown Point, New York, Champlain, a battle began the next day. Two hundred Iroquois advanced on Champlains position as a native guide pointed out the three Iroquois chiefs to the French, Champlain fired his arquebus and killed two of them with one shot. One of his men killed the third and this was to set the tone for French-Iroquois relations for the next 100 years. As the forest and mining began at the turn of the 20th century. In 1999 Survival International published a study of the Innu communities of Labrador and it assessed the impact of the Canadian governments relocating the people far from their ancestral lands and preventing their practising their ancient way of life. Survival International considered these policies to be in violation of international law, by 2000, the Innu island community of Davis Inlet asked the Canadian government to assist with a local addiction crisis
17.
First Nation
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The First Nations are the predominant Aboriginal peoples of Canada south of the Arctic. Those in the Arctic area are distinct and known as Inuit, the Métis, another distinct ethnicity, developed after European contact and relations primarily between First Nations people and Europeans. There are currently 634 recognized First Nations governments or bands spread across Canada, roughly half of which are in the provinces of Ontario and British Columbia. Under the Employment Equity Act, First Nations are a group, along with women, visible minorities. First Nations are not defined as a minority under the Act or by the criteria of Statistics Canada. Within Canada, First Nations has come into general use—replacing the deprecated term Indians—for the indigenous peoples of the Americas, individuals using the term outside Canada include supporters of the Cascadian independence movement, as well as U. S. tribes within the Pacific Northwest. The singular, commonly used on culturally politicized reserves, is the term First Nations person, North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700, 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, explorers, and missionaries give important evidence of early contact culture, in addition, archeological and anthropological research, as well as linguistics, have helped scholars piece together understanding of ancient cultures and historic peoples. Combined with later development, this relatively non-combative history has allowed First Nations peoples to have an influence on the national culture. Collectively, First Nations, Inuit, and Métis peoples constitute Aboriginal peoples in Canada, Indigenous peoples of the Americas, First Nations came into common usage in the 1980s to replace the term Indian band in referring to groups of Indians with common government and language. Elder Sol Sanderson says that he coined the term in the early 1980s, others say that the term came 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 Aboriginal peoples in Canada have also adopted the term First Nation to replace the word band in the formal name of their community. While the word Indian is still a term, its use is erratic. Some First Nations people consider the term offensive, while others prefer it to Aboriginal person/persons/people, the term 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 United States government and it refers more specifically to the Aboriginal peoples residing within the boundaries of the United States. The parallel term Native Canadian is not commonly used, but Natives and autochthones are, under the Royal Proclamation of 1763, also 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, unlike alternative terms, bands and nations may have slightly different meanings
18.
Samuel de Champlain
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Samuel de Champlain, The Father of New France, was a French navigator, cartographer, draftsman, soldier, explorer, geographer, ethnologist, diplomat, and chronicler. He founded New France and Quebec City on July 3,1608 and he is important to Canadian history because he made the first accurate map of the coast and he helped establish the settlements. Born into a family of mariners, Champlain, while still a man, began exploring North America in 1603 under the guidance of François Gravé Du Pont. Then, in 1608, he established the French settlement that is now Quebec City, Champlain was the first European to explore and describe the Great Lakes, and published maps of his journeys and accounts of what he learned from the natives and the French living among the Natives. He formed relationships with local Montagnais and Innu and later with others farther west, with Algonquin and with Huron Wendat, in 1620, Louis XIII of France ordered Champlain to cease exploration, return to Quebec, and devote himself to the administration of the country. In every way but formal title, Samuel de Champlain served as Governor of New France and he established trading companies that sent goods, primarily fur, to France, and oversaw the growth of New France in the St. Lawrence River valley until his death in 1635. The most notable of these is Lake Champlain, which straddles the border between northern New York and Vermont, extending slightly across the border into Canada. Champlain was born to Antoine Champlain and Marguerite Le Roy, in either Hiers-Brouage, or the city of La Rochelle. He was born on or before August 13,1574 according to a recent baptism record found by Jean-Marie Germe, although Léopold Delayant wrote as early as 1867 that Rainguets estimate was wrong, the books of Rainguet and Laverdière have had a significant influence. The 1567 date was carved on numerous monuments dedicated to Champlain and is regarded as accurate. In the first half of the 20th century, some authors disagreed, in 1978 Jean Liebel published groundbreaking research about these estimates of Champlains birth year and concluded, Samuel Champlain was born about 1580 in Brouage, France. Liebel asserts that some authors, including the Catholic priests Rainguet and Laverdière, Champlain claimed to be from Brouage in the title of his 1603 book, and to be Saintongeois in the title of his second book. The exact location of his birth is also not known with certainty. Born into a family of mariners, Samuel Champlain learned to navigate, draw, make nautical charts and his education did not include Ancient Greek or Latin, so he did not read or learn from any ancient literature. During this time he claimed to go on a secret voyage for the king. By 1597 he was a capitaine dune compagnie serving in a garrison near Quimper, in 1598, his uncle-in-law, a navigator whose ship Saint-Julien was chartered to transport Spanish troops to Cádiz pursuant to the Treaty of Vervins, gave Champlain the opportunity to accompany him. After a difficult passage, he spent some time in Cadiz before his uncle, whose ship was chartered to accompany a large Spanish fleet to the West Indies. His uncle, who gave command of the ship to Jeronimo de Valaebrera and this journey lasted two years, and gave Champlain the opportunity to see or hear about Spanish holdings from the Caribbean to Mexico City
19.
Jacques Cartier
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Jacques Cartier was a French explorer of Breton origin who claimed what is now Canada for France. Jacques Cartier was born in 1491 in Saint-Malo, the port on the north-west coast of Brittany, Cartier, who was a respectable mariner, improved his social status in 1520 by marrying Mary Catherine des Granches, member of a leading family. His good name in Saint-Malo is recognized by its frequent appearance in baptismal registers as godfather or witness, the king had previously invited the Florentine explorer Giovanni da Verrazzano to explore the eastern coast of North America on behalf of France in 1524. Le Veneur cited voyages to Newfoundland and Brazil as proof of Cartiers ability to lead ships to the discovery of new lands in the New World. On April 20,1534, Cartier set sail under a commission from the king, hoping to discover a western passage to the markets of Asia. In the words of the commission, he was to certain islands and lands where it is said that a great quantity of gold. It took him twenty days to sail across the ocean, starting on May 10 of that year, he explored parts of Newfoundland, areas that now comprise the Canadian Atlantic provinces and the Gulf of St. Lawrence. During one stop at Îles aux Oiseaux, his crew slaughtered around 1000 birds, Cartiers first two encounters with aboriginal peoples in Canada on the north side of Chaleur Bay, most likely the Mikmaq, were brief, some trading occurred. His third encounter took place on the shores of Gaspé Bay with a party of St. Lawrence Iroquoians, the 10-meter cross bearing the words Long Live the King of France took possession of the territory in the name of the king. The change in mood was an indication that the Iroquoians understood Cartiers actions. Here he kidnapped the two sons of their captain, Cartier wrote that they later told him this region where they were captured was called by them Honguedo. The natives captain at last agreed that they could be taken, Cartier returned to France in September 1534, sure that he had reached an Asian land. Jacques Cartier set sail for a voyage on May 19 of the following year with three ships,110 men, and his two Iroquoian captives. Reaching the St. Lawrence, he sailed up-river for the first time, and reached the Iroquoian capital of Stadacona, Cartier left his main ships in a harbour close to Stadacona, and used his smallest ship to continue on to Hochelaga, arriving on October 2,1535. Hochelaga was far more impressive than the small and squalid village of Stadacona, the site of their arrival has been confidently identified as the beginning of the Sainte-Marie Sault – where the bridge named after him now stands. The expedition could proceed no further, as the river was blocked by rapids, after spending two days among the people of Hochelaga, Cartier returned to Stadacona on October 11. It is not known exactly when he decided to spend the winter of 1535–1536 in Stadacona, Cartier and his men prepared for the winter by strengthening their fort, stacking firewood, and salting down game and fish. From mid-November 1535 to mid-April 1536, the French fleet lay frozen solid at the mouth of the St. Charles River, under the Rock of Quebec, ice was over a fathom thick on the river, with snow four feet deep ashore
20.
Jesuit
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The Society of Jesus Latin, Societas Iesu, S. J. SJ or SI) is a religious congregation of the Catholic Church which originated in Spain. The society is engaged in evangelization and apostolic ministry in 112 nations on six continents, Jesuits work in education, intellectual research, and cultural pursuits. Jesuits also give retreats, minister in hospitals and parishes, and promote social justice, Ignatius of Loyola founded the society after being wounded in battle and experiencing a religious conversion. He composed the Spiritual Exercises to help others follow the teachings of Jesus Christ, ignatiuss plan of the orders organization was approved by Pope Paul III in 1540 by a bull containing the Formula of the Institute. Ignatius was a nobleman who had a background, and the members of the society were supposed to accept orders anywhere in the world. The Society participated in the Counter-Reformation and, later, in the implementation of the Second Vatican Council, the Society of Jesus is consecrated under the patronage of Madonna Della Strada, a title of the Blessed Virgin Mary, and it is led by a Superior General. The Society of Jesus on October 3,2016 announced that Superior General Adolfo Nicolás resignation was officially accepted, on October 14, the 36th General Congregation of the Society of Jesus elected Father Arturo Sosa as its thirty-first Superior General. The headquarters of the society, its General Curia, is in Rome, the historic curia of St. Ignatius is now part of the Collegio del Gesù attached to the Church of the Gesù, the Jesuit Mother Church. In 2013, Jorge Mario Bergoglio became the first Jesuit Pope, the Jesuits today form the largest single religious order of priests and brothers in the Catholic Church. As of 1 January 2015, Jesuits numbered 16,740,11,986 clerics regular,2,733 scholastics,1,268 brothers and 753 novices. In 2012, Mark Raper S. J. wrote, Our numbers have been in decline for the last 40 years—from over 30,000 in the 1960s to fewer than 18,000 today. The steep declines in Europe and North America and consistent decline in Latin America have not been offset by the significant increase in South Asia, the Society is divided into 83 Provinces with six Independent Regions and ten Dependent Regions. On 1 January 2007, members served in 112 nations on six continents with the largest number in India and their average age was 57.3 years,63.4 years for priests,29.9 years for scholastics, and 65.5 years for brothers. The current Superior General of the Jesuits is Arturo Sosa, the Society is characterized by its ministries in the fields of missionary work, human rights, social justice and, most notably, higher education. It operates colleges and universities in countries around the world and is particularly active in the Philippines. In the United States it maintains 28 colleges and universities and 58 high schools and he ensured that his formula was contained in two papal bulls signed by Pope Paul III in 1540 and by Pope Julius III in 1550. The formula expressed the nature, spirituality, community life and apostolate of the new religious order, the meeting is now commemorated in the Martyrium of Saint Denis, Montmartre
21.
Missionary
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A missionary is a member of a religious group sent into an area to proselytize and/or perform ministries of service, such as education, literacy, social justice, health care, and economic development. The word mission originates from 1598 when the Jesuits sent members abroad, derived from the Latin missionem, meaning act of sending or mittere, meaning to send. The word was used in light of its usage, in the Latin translation of the Bible. The term is most commonly used for Christian missions, but can be used for any creed or ideology, a Christian missionary can be defined as one who is to witness across cultures. The Lausanne Congress of 1974, defined the term, related to Christian mission as, Missionaries can be found in many countries around the world. Jesus instructed the apostles to make disciples of all nations and this verse is referred to by Christian missionaries as the Great Commission and inspires missionary work. The New Testament-era missionary outreach of the Christian church from the time of St Paul expanded throughout the Roman Empire and beyond to Persia, in 596, Pope Gregory the Great sent the Gregorian Mission into England. In their turn, Christians from Ireland and from Britain became prominent in converting the inhabitants of central Europe, about the same time, missionaries such as Francis Xavier as well as other Jesuits, Augustinians, Franciscans, and Dominicans started moving into Asia and the Far East. The Portuguese sent missions into Africa and these are some of the most well-known missions in history. While some missions accompanied imperialism and oppression, others were relatively peaceful, contemporary Christian missionaries argue that working for justice forms a constitutive part of preaching the Gospel, and observe the principles of inculturation in their missionary work. Over time, the Vatican gradually established a church structure in the mission areas, often starting with special jurisdictions known as apostolic prefectures. The two 9th-century saints Cyril and Methodius had extensive success in central Europe. The Byzantines expanded their work in Ukraine after a mass baptism in Kiev in 988. The Serbian Orthodox Church had its origins in the conversion by Byzantine missionaries of the Serb tribes when they arrived in the Balkans in the 7th century, Orthodox missionaries also worked successfully among the Estonians from the 10th to the 12th centuries, founding the Estonian Orthodox Church. The Russian St. Nicholas of Japan took Eastern Orthodoxy to Japan in the 19th century, the Russian Orthodox Church also sent missionaries to Alaska beginning in the 18th century, including Saint Herman of Alaska, to minister to the Native Americans. Quaker publishers of truth visited Boston and other mid-17th century colonies, the Danish government began the first organized Protestant mission work through its College of Missions, established in 1714. This funded and directed Lutheran missionaries such as Bartholomaeus Ziegenbalg in Tranquebar, India and he also got to know a slave from the Danish colony in the West Indies. Within thirty years, Moravian missionaries had become active on every continent, and they are famous for their selfless work, living as slaves among the slaves and together with the Native Americans, the Delaware and Cherokee Indian tribes
22.
Lac Saint-Jean
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Lac Saint-Jean is a large, relatively shallow lake in south-central Quebec, Canada, in the Laurentian Highlands. It is situated 206 kilometres north of the Saint Lawrence River and it covers an area of 1,053 km2, and is 63.1 m at its deepest point. Its name in the Innu language is Piekuakami, the lake is fed by dozens of small rivers, including the Ashuapmushuan, the Mistassini, the Peribonka, the Des Aulnaies, the Métabetchouane, and the Ouiatchouane. The towns on its shores include Alma, Dolbeau-Mistassini, Roberval, Normandin, three Regional County Municipalities lie on its shores, Lac-Saint-Jean-Est, Le Domaine-du-Roy, and Maria-Chapdelaine. The lake was named Piekuakami by the Innu, the people who occupied the area at the time of European arrival. It was given its French name after Jean de Quen, a Jesuit missionary who in 1647 was the first European to reach its shores, industry on the lake was dominated by the fur trade until the 19th century. Colonization began in the Saguenay–Lac-Saint-Jean region in the early 19th century, industry was mainly forestry and agriculture. In the 20th century, pulp and paper mills and aluminum smelting rose to importance, encouraged by hydroelectric dams at Alma, Lac Saint-Jean also has an important summer resort and sport-fishing industry. The area is featured in the classic French-language novel Maria Chapdelaine by Louis Hémon published in 1914 and subsequently translated into twenty languages. In the 1940s, during World War II, Lac Saint-Jean, along various other regions within Canada, such as the Saguenay, Saint Helens Island and Hull. Lac Saint-Jeans was numbered and remained unnamed just like most of Canadas other war prisons, the prisoners of war were classified into categories including their nationality and civilian or military status. By 1942 this region had two camps with at least 50 POWs, prisoners worked the land, including lumbering and assisting in the production of pulp and paper. Birthplace of NHL Hall of Famer and Team Canada 1972 member Jean Ratelle, birthplace of McGill Professor Mario Chevrette, Ph. D of Molecular and Cell Biology. List of lakes of Quebec Saguenay Graben Lac-Saint-Jean travel guide from Wikivoyage
23.
Logging
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Logging is the cutting, skidding, on-site processing, and loading of trees or logs onto trucks or skeleton cars. In forestry, the logging is sometimes used in a narrow sense concerning the logistics of moving wood from the stump to somewhere outside the forest. However, in usage, the term may be used to indicate a range of forestry or silviculture activities. Illegal logging refers to what in forestry might be called timber theft by the timber mafia and it can also refer to the harvesting, transportation, purchase, or sale of timber in violation of laws. Clearcut logging is not necessarily considered a type of logging but a harvesting or silviculture method, in the forest products industry logging companies may be referred to as logging contractors, with the smaller, non-union crews referred to as gyppo loggers. Cutting trees with the highest value and leaving those with lower value and it is sometimes called selective logging, and confused with selection cutting, the practice of managing stands by harvesting a proportion of trees. Logging usually refers to above-ground forestry logging, submerged forests exist on land that has been flooded by damming to create reservoirs. Such trees are logged using underwater logging or by the lowering of the reservoirs in question, ootsa Lake and Williston Lake in British Columbia, Canada are notable examples where timber recovery has been needed to remove inundated forests. Clearcutting, or clearfelling, is a method of harvesting that removes all the standing trees in a selected area. Silviculture objectives for clearcutting, and a focus on forestry distinguish it from deforestation, other methods include shelterwood cutting, group selective, single selective, seed-tree cutting, patch cut, and retention cutting. The above operations can be carried out by different methods, of which the three are considered industrial methods, Trees are felled and then delimbed and topped at the stump. The log is then transported to the landing, where it is bucked and loaded on a truck and this leaves the slash in the cut area, where it must be further treated if wild land fires are of concern. This ability is due to the advancement in the style felling head that can be used, the trees are then delimbed, topped, and bucked at the landing. This method requires that slash be treated at the landing, in areas with access to cogeneration facilities, the slash can be chipped and used for the production of electricity or heat. Full-tree harvesting also refers to utilization of the tree including branches. Cut-to-length logging is the process of felling, delimbing, bucking, harvesters fell the tree, delimb, and buck it, and place the resulting logs in bunks to be brought to the landing by a skidder or forwarder. This method is available for trees up to 900 mm in diameter. Harvesters are employed effectively in level to steep terrain
24.
Log driving
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Log driving is a means of moving logs from a forest to sawmills and pulp mills downstream using the current of a river. It was the transportation method of the early logging industry in Europe. Later, bigger circular sawmills were developed in the reaches of a river. In the broader, slower stretches of a river, the logs might be bound together into timber rafts, in the smaller, wilder stretches of a river, rafts couldnt get through, so masses of individual logs were driven down the river like huge herds of cattle. The log drive was one step in a process of lumber-making in remote places. There the logs were decked onto rollways, in the spring when snow thawed and water levels rose, the logs were rolled into the river, and the drive commenced. To ensure that logs drifted freely along the river, men called log drivers or river pigs were needed to guide the logs, the drivers typically divided into two groups. The more experienced and nimble men comprised the jam crew or beat crew and they watched the spots where logs were likely to jam, and when a jam started, tried to get to it quickly and dislodge the key logs before many logs stacked up. If they didnt, the river would keep piling on more logs, millions of board feet of lumber could back up for miles upriver, requiring weeks to break up, with some lumber possibly lost if it was shoved far enough into the shallows. So when the jam crew saw a jam start, they rushed to it and tried to break it up, using peaveys and this job required some understanding of physics, strong muscles, and extreme agility. The jam crew was a dangerous occupation, with the drivers standing on the moving logs. Many drivers lost their lives by falling and being crushed by the logs, each crew was accompanied by an experienced boss often selected for his fighting skills to control the strong and reckless men of his team. The overall drive was controlled by the boss who moved from place to place to coordinate the various teams to keep logs moving past problem spots. Stalling a drive near a saloon often created a cascade of drunken personnel problems, a larger group of less experienced men brought up the rear, pushing along the straggler logs that were stuck on the banks and in trees. They spent more time wading in icy water than balancing on moving logs and they were called the rear crew. Other men worked with them from the bank, pushing logs away with pike poles, others worked with horses and oxen to pull in the logs that had strayed furthest out into the flats. Bateaux ferried log drivers using pike poles to dislodge stranded logs while maneuvering with the log drive, a wannigan was a kitchen built on a raft which followed the drivers down the river. The wannigan served four meals a day to fuel the men working in cold water and it also provided tents and blankets for the night if no better accommodations were available
25.
Battle of the Plains of Abraham
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The Battle of the Plains of Abraham, also known as the Battle of Quebec, was a pivotal battle in the Seven Years War. The culmination of a siege by the British, the battle lasted about 15 minutes. In the wake of the battle, the French evacuated the city, their military force in Canada. While the French forces continued to fight and prevailed in several battles after Quebec was captured and that tenacity carried over to other areas in North America, within four years, France ceded most of its possessions in eastern North America to Great Britain in the Treaty of Paris. The decisive success of the British forces and the subsequent capture of Quebec City formed part of what became known as the Annus Mirabilis in Great Britain. As the Seven Years War entered its later stages through 1758 and 1759, in 1758 after defeat in July at the Battle of Carillon, the British took Louisbourg in August, causing Atlantic Canada to fall into British hands, and opening the sea route to attack Quebec. Fort Frontenac fell to the British in the month, costing the French supplies for the Ohio Valley campaign. When some of the Indian supporters of the French made peace with the British, French leadership, specifically Governor de Vaudreuil and General Montcalm, were unsettled by the British successes. However, Quebec was still able to protect itself as the British prepared an attack for 1759. James Wolfe expected to lead 12,000 men, but was greeted by only approximately 7,000 regular troops,400 officers, Wolfes troops were supported by a fleet of 49 ships and 140 smaller craft led by Admiral Charles Saunders. In preparation for the approach to Quebec, James Cook surveyed a large portion of the river. Cooks ship was one of the first ships up the river, sounding the channel and guiding the fleet as it moved up, eventually landing Wolfe and his men on the Île dOrléans on 28 June. Despite an air of defeatism among the leadership, the professional French troops, prior to the arrival of the British, a small fleet of supply ships had arrived in Quebec with much needed supplies. Those supplies, along with 500 reinforcements, were likely behind the lengthened siege, in addition, a screen of trees along the Montmorency River made an approach on that route dangerous. On 31 July, the first serious attempt by Wolfes troops to land on the northern shore led to the Battle of Beauport, approximately 3,500 troops, supported by a heavy bombardment, attempted to land, but were caught under fire in the river shallows. Some French officers felt the Montmorency defeat would be the last British attack, Wolfe, I assure you, will make no progress… He contented himself with losing about five hundred of his best soldiers. He predicted another attack would come within days, others in the French camp felt the campaign was over. For the remainder of the summer, Wolfes focus changed, possibly due to frustration with Montcalms tactics and his troops, along with American Rangers, attacked and destroyed small French settlements along the St. Lawrence
26.
Yellow birch
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Betula alleghaniensis, is a large and important lumber species of birch native to North-eastern North America. The name yellow birch reflects the color of the trees bark, the name Betula lutea was used expansively for this tree but has now been replaced. Betula alleghaniensis is the tree of Quebec, where it is commonly called merisier. It is a medium-sized, typically single stemmed, deciduous tree reaching 60–80 feet tall with a trunk typically 2–3 ft in diameter, yellow birch is a relatively long lived birch which typically grows 150 years and may even grow up to 300 in old growth forests. Mature trees typically start producing seeds at about 40 years but may start as young as 20, the optimum age for seed production is about 70 years. Good seed crops are not produced every year, and tend to be produced in intervals of 1–4 years with the years between good years having little seed production. The seeds germinate best on mossy logs, decaying wood or cracks in boulders since they cannot penetrate the leaf litter layer, yellow birch saplings will not establish in full shade so they typically need disturbances in a forest in order to establish and grow. The bark on trees is a shiny yellow-bronze which flakes. The bark often has small black marks and dark horizontal lenticels, after the tree reaches a diameter greater than 1 ft the bark typically stops shredding and reveal a platy outer bark although the thinner branches will still have the shreddy bark. There is an uncommon, alternate form of the tree grows in the southern part of the range. F. fallax has darker gray-brown bark which shreds less than the typical form. The twigs, when scraped, have a scent of wintergreen oil. However, the potency of the odor is not considered a reliable identification method unless it is combined with other characteristics, the leaves are alternately placed on the stem, oval in shape with a pointed tip and often a slightly heart shaped base. They are 2–5 in long and typically half as wide with a serrated margin. They are dark green in color on the side and lighter on the bottom. The leaves arise in pairs or singularly from small spur shoots, in the fall the leaves turn a bright yellow color. The leaf has a short petiole. 25–.5 in long. The flowers are wind-pollinated catkins which open in later spring, both male and female flowers will occur on the same tree making the plant monoecious
27.
Sugar maple
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Sugar maple is best known for its bright fall foliage and for being the primary source of maple syrup. Acer saccharum is a tree normally reaching heights of 25–35 m. A 10-year-old tree is typically about 5 m tall, when healthy, the sugar maple can live for over 400 years. The leaves are deciduous, up to 20 cm long and equally wide, the basal lobes are relatively small, while the upper lobes are larger and deeply notched. In contrast with the angular notching of the maple, however. The fall color is often spectacular, ranging from yellow through orange to fluorescent red-orange. Sugar maples also have a tendency to color unevenly in fall, in some trees, all colors above can be seen at the same time. They also share a tendency with red maples for certain parts of a tree to change color weeks ahead of or behind the remainder of the tree. The leaf buds are pointy and brown-colored, the recent years growth twigs are green, and turn dark brown. The flowers are in panicles of five to 10 together, yellow-green and without petals, the sugar maple will generally begin flowering when it is between 10 and 15 years old. The fruit is a pair of samaras, the seeds are globose, 7–10 mm in diameter, the wing 2–3 cm long. The seeds fall from the tree in autumn, where they must be exposed to 90 days of temperatures below −18 °C to break their coating down. Germination of A. saccharum is slow, not taking place until the spring when the soil has warmed. It is closely related to the maple, which is sometimes included in this species. The western American bigtooth maple is also treated as a variety or subspecies of sugar maple by some botanists, the sugar maple is also often confused with the Norway maple, though they are not closely related within the genus. The sugar maple is most easily identified by clear sap in the petiole, brown, sharp-tipped buds. Also, the lobes of the sugar maple have a more triangular shape. The sugar maple is an important species to the ecology of many forests in the northern United States
28.
Boreal forest
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Taiga also known as boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces and larches. The taiga is the worlds largest biome apart from the oceans, in North America it covers most of inland Canada and Alaska as well as parts of the extreme northern continental United States, where it is known as the Northwoods or North woods. However, the tree species, the length of the growing season. Hoffman discusses the origin of this use in North America. Although at high elevations taiga grades into alpine tundra through Krummholz, it is not an alpine biome only like subalpine forest, Taiga is the worlds largest land biome, and makes up 29% of the worlds forest cover, the largest areas are located in Russia and Canada. The taiga is the terrestrial biome with the lowest annual average temperatures after the tundra, extreme winter minimums in the northern taiga are typically lower than those of the tundra. The lowest reliably recorded temperatures in the Northern Hemisphere were recorded in the taiga of northeastern Russia, the taiga or boreal forest has a subarctic climate with very large temperature range between seasons, but the long and cold winter is the dominant feature. This climate is classified as Dfc, Dwc, Dsc, Dfd and Dwd in the Köppen climate classification scheme, meaning that the summer lasts 1–3 months. In Siberian taiga the average temperature of the coldest month is between −6 °C and −50 °C, the mean annual temperature generally varies from -5 °C to 5 °C, but there are taiga areas in eastern Siberia and interior Alaska-Yukon where the mean annual reaches down to -10 °C. According to some sources, the boreal forest grades into a mixed forest when mean annual temperature reaches about 3 °C. The winters, with temperatures below freezing, last five to seven months. Temperatures vary from −54 °C to 30 °C throughout the whole year, the summers, while short, are generally warm and humid. In much of the taiga, -20 °C would be a winter day temperature and 18 °C an average summer day. In Canada, Scandinavia and Finland, the season is often estimated by using the period of the year when the 24-hour average temperature is +5 °C or more. For the Taiga Plains in Canada, growing season varies from 80 to 150 days, some sources claim 130 days growing season as typical for the taiga. Other sources mention that 50–100 frost-free days are characteristic, data for locations in southwest Yukon gives 80–120 frost-free days. The closed canopy boreal forest in Kenozersky National Park near Plesetsk, Arkhangelsk Province, Russia, the longest growing season is found in the smaller areas with oceanic influences, in coastal areas of Scandinavia and Finland, the growing season of the closed boreal forest can be 145–180 days. High latitudes mean that the sun not rise far above the horizon
29.
Black spruce
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Picea mariana is a North American species of spruce tree in the pine family. It is widespread across Canada, found in all 10 provinces and its range extends into northern parts of the United States, in Alaska, the Great Lakes region, and the upper Northeast. It is a frequent part of the known as taiga or boreal forest. Through much of its range it averages 5–15 m tall with a trunk 15–50 cm diameter at maturity, the bark is thin, scaly, and grayish brown. The leaves are needle-like, 6–15 mm long, stiff, four-sided, dark green on the upper sides. Natural hybridization occurs regularly with the closely related Picea rubens, numerous differences in details of its needle and pollen morphology also exist but require careful microscopic examination to detect. From true firs, such as Abies balsamea, it differs in having pendulous cones, persistent woody leaf-bases, older taxonomic synonyms include Abies mariana, Picea brevifolia, or Picea nigra. In swamp and muskeg it shows progressively slower growth rates from the edges toward the centre, the roots are shallow and wide spreading, resulting in susceptibility to windthrow. In the northern part of its range, ice pruned asymmetric black spruce are often seen with diminished foliage on the windward side, tilted trees colloquially called drunken trees are associated with thawing of permafrost. In the southern portion of its range it is primarily on wet organic soils. In the Great Lakes States it is most abundant in peat bogs and swamps, in these areas it is rare on uplands, except in isolated areas of northern Minnesota and the Upper Peninsula of Michigan. Most stands are even-aged due to frequent fire intervals in black spruce forests and it commonly grows in pure stands on organic soils and in mixed stands on mineral soils. It is tolerant of soils, and is commonly found on poorly drained acidic peatlands. The frequent fire return interval, a fire ecology, perpetuates numerous successional communities. Throughout boreal North America, Betula papyrifera and Populus tremuloides are successional hardwoods that frequently invade burns in black spruce, black spruce typically seeds in promptly after fire, and with the continued absence of fire, will eventually dominate the hardwoods. It is a pioneer that invades the sedge mat in filled-lake bogs, though often preceded slightly by Larix laricina, with which it may in time form a stable forest cover in swamps. The larvae of the spruce budworm moth cause defoliation which will lead to death if it occurs several years in a row, trees most at risk are those growing with balsam fir and white spruce. Numerous cultivars have been selected for use in parks and gardens, the cultivar P. mariana Nana is a dwarf form which has gained the Royal Horticultural Societys Award of Garden Merit
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American black bear
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The American black bear is a medium-sized bear native to North America. It is the continents smallest and most widely distributed bear species, Black bears are omnivores, with their diets varying greatly depending on season and location. They typically live in forested areas, but do leave forests in search of food. Sometimes they become attracted to human communities because of the availability of food. The American black bear is the worlds most common bear species, along with the brown bear, it is one of only two of the eight modern bear species not considered globally threatened with extinction by the IUCN. American black bears often mark trees using their teeth and claws as a form of communication with other bears, a behavior common to many species of bears. Despite living in North America, American black bears are not closely related to bears and polar bears. American and Asian black bears are considered sister taxa, and are closely related to each other than to other species of bear. Reportedly, the sun bear is also a recent split from this lineage. A small primitive bear called Ursus abstrusus is the oldest known North American fossil member of the genus Ursus and this suggests that U. abstrusus may be the direct ancestor of the American black bear, which evolved in North America. Although Wolverton and Lyman still consider U. vitabilis an apparent precursor to modern black bears, the ancestors of American black bears and Asiatic black bears diverged from sun bears 4.58 mya. The American black bear then split from the Asian black bear 4.08 mya, the earliest American black bear fossils, which were located in Port Kennedy, Pennsylvania, greatly resemble the Asiatic species, though later specimens grew to sizes comparable to grizzlies. From the Holocene to present, American black bears seem to have shrunk in size, the American black bear lived during the same period as short-faced bears and the Florida spectacled bear. These Tremarctine bears evolved from bears that had emigrated from Asia to North America 7–8 ma, however, both Arctodus and Tremarctos had survived several other ice ages. American black bears are reproductively compatible with several other bear species, according to Jack Hannas Monkeys on the Interstate, a bear captured in Sanford, Florida, was thought to have been the offspring of an escaped female Asian black bear and a male American black bear. In 1859, a bear and a Eurasian brown bear were bred together in the London Zoological Gardens. In the reports published since this date three species have produced young, a black bear shot in autumn 1986 in Michigan was thought by some to be a black bear/grizzly bear hybrid, due to its unusually large size and its proportionately larger braincase and skull. DNA testing was unable to determine whether it was a black bear or grizzly
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Bobcat
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The bobcat is a North American cat that appeared during the Irvingtonian stage of around 1.8 million years ago. Containing 12 recognized subspecies, it ranges from southern Canada to central Mexico, the bobcat is an adaptable predator that inhabits wooded areas, as well as semidesert, urban edge, forest edge, and swampland environments. It remains in some of its range, but populations are vulnerable to local extinction by coyotes. With a gray to brown coat, whiskered face, and black-tufted ears and it is smaller on average than the Canada lynx, with which it shares parts of its range, but is about twice as large as the domestic cat. It has distinctive black bars on its forelegs and a black-tipped, stubby tail, though the bobcat prefers rabbits and hares, it hunts insects, chickens, geese and other birds, small rodents, and deer. Prey selection depends on location and habitat, season, and abundance, like most cats, the bobcat is territorial and largely solitary, although with some overlap in home ranges. It uses several methods to mark its boundaries, including claw marks. The bobcat breeds from winter into spring and has a period of about two months. Although bobcats have been hunted extensively by humans, both for sport and fur, their population has proven resilient though declining in some areas, the elusive predator features in Native American mythology and the folklore of European settlers. The Lynx genus is now accepted, and the bobcat is listed as Lynx rufus in modern taxonomic sources. Johnson et al. reported Lynx shared a clade with the puma, leopard cat, the first wave moved into the southern portion of North America, which was soon cut off from the north by glaciers. This population evolved into modern bobcats around 20,000 years ago, a second population arrived from Asia and settled in the north, developing into the modern Canada lynx. Hybridization between the bobcat and the Canada lynx may sometimes occur, the bobcat resembles other species of the Lynx genus, but is on average the smallest of the four. Its coat is variable, though generally tan to grayish-brown, with streaks on the body and dark bars on the forelegs. Its spotted patterning acts as camouflage, the ears are black-tipped and pointed, with short, black tufts. Generally, a color is seen on the lips, chin. Bobcats in the regions of the southwest have the lightest-colored coats, while those in the northern. Kittens are born well-furred and already have their spots, a few melanistic bobcats have been sighted and captured in Florida
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Common raccoon
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The raccoon, sometimes spelled racoon, also known as the common raccoon, North American raccoon, northern raccoon and colloquially as coon, is a medium-sized mammal native to North America. The raccoon is the largest of the family, having a body length of 40 to 70 cm. Its grayish coat mostly consists of dense underfur which insulates it against cold weather, two of the raccoons most distinctive features are its extremely dexterous front paws and its facial mask, which are themes in the mythology of several Native American ethnic groups. Raccoons are noted for their intelligence, with studies showing that they are able to remember the solution to tasks for up to three years, the diet of the omnivorous raccoon, which is usually nocturnal, consists of about 40% invertebrates, 33% plant foods, and 27% vertebrates. As a result of escapes and deliberate introductions in the century, raccoons are now also distributed across mainland Europe, Caucasia. Though previously thought to be solitary, there is now evidence that raccoons engage in social behavior. Home range sizes vary anywhere from 3 hectares for females in cities to 5,000 hectares for males in prairies, after a gestation period of about 65 days, two to five young, known as kits, are born in spring. The kits are subsequently raised by their mother until dispersal in late fall, although captive raccoons have been known to live over 20 years, their life expectancy in the wild is only 1.8 to 3.1 years. In many areas, hunting and vehicular injury are the two most common causes of death, the word raccoon was adopted into English from the native Powhatan term, as used in the Virginia Colony. It was recorded on Captain John Smiths list of Powhatan words as aroughcun and it has also been identified as a Proto-Algonquian root *ahrah-koon-em, meaning one who rubs, scrubs and scratches with its hands. Similarly, Spanish colonists adopted the Spanish word mapache from the Nahuatl mapachitli of the Aztecs, in French and European Portuguese, the washing behavior is combined with these languages term for rat, yielding, respectively, raton laveur and ratão-lavadeiro. The colloquial abbreviation coon is used in words like coonskin for fur clothing and in phrases like old coon as a self-designation of trappers. In the 1830s, the U. S. Whig Party used the raccoon as an emblem, causing them to be known as coons by their political opponents. Soon after that it became an ethnic slur, especially in use between 1880 and 1920, and the term is considered offensive. In 1780, Gottlieb Conrad Christian Storr placed the raccoon in its own genus Procyon and it is also possible that Storr had its nocturnal lifestyle in mind and chose the star Procyon as eponym for the species. Based on fossil evidence from France and Germany, the first known members of the family Procyonidae lived in Europe in the late Oligocene about 25 million years ago. Similar tooth and skull structures suggest procyonids and weasels share a common ancestor, after the then-existing species crossed the Bering Strait at least six million years later in the early Miocene, the center of its distribution was probably in Central America. Coatis and raccoons have been considered to share common descent from a species in the genus Paranasua present between 5.2 and 6.0 million years ago
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Gray wolf
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The gray wolf or grey wolf, also known as the timber wolf or western wolf, is a canine native to the wilderness and remote areas of Eurasia and North America. It is the largest extant member of its family, with males averaging 43–45 kg, like the red wolf, it is distinguished from other Canis species by its larger size and less pointed features, particularly on the ears and muzzle. Its winter fur is long and bushy, and predominantly a mottled gray in color, although pure white, red. As of 2005,37 subspecies of C. lupus are recognised by MSW3 and it is nonetheless closely related enough to smaller Canis species, such as the eastern wolf, coyote, and golden jackal to produce fertile hybrids. It is an animal, travelling in nuclear families consisting of a mated pair. The gray wolf is typically an apex predator throughout its range, with only humans and it feeds primarily on large ungulates, though it also eats smaller animals, livestock, carrion, and garbage. The gray wolf is one of the worlds best known and well researched animals, although the fear of wolves is pervasive in many human societies, the majority of recorded attacks on people have been attributed to animals suffering from rabies. The English wolf stems from the Old English wulf, which is thought to be derived from the Proto-Germanic *wulfaz. The Latin lupus is a Sabine loanword, both derive from the Proto-Indo-European root *wlqwos/*lukwos. The species Canis lupus was first recorded by Carl Linnaeus in his publication Systema Naturae in 1758, the thirty-seven subspecies of Canis lupus are listed under the designated common name of wolf in Mammal Species of the World third edition that was published in 2005. The nominate subspecies is the Eurasian wolf, also known as the common wolf, the subspecies includes the domestic dog, dingo, eastern wolf and red wolf, but lists C. l. italicus and C. l. communis as synonyms of C. l. lupus. However, the classification of several as either species or subspecies has recently been challenged, ecological factors including habitat type, climate, prey specialization and predatory competition will greatly influence the wolfs genetic population structure and cranio-dental plasticity. The domestic dog is the most widely abundant large carnivore and a descendant from one of those now-extinct wolf populations, in 2013, a genetic study found that the wolf population in Europe was divided along a north-south axis and formed five major clusters. Three clusters were identified occupying southern and central Europe in Italy, the Carpathians, another two clusters were identified occupying north-central Europe and the Ukrainian steppe. The Italian wolf consisted of a population with low genetic diversity. Wolves from Croatia, Bulgaria, and Greece formed the Dinaric-Balkans cluster, the wolves from the Carpathians were more similar to the wolves from the Pontic-Caspian Steppe than they were to wolves from north-central Europe. These clusters may have been the result of expansion from glacial refugia, an adaptation to environments, and landscape fragmentation. These six wolf ecotypes were named West Forest, Boreal Forest, Arctic, High Arctic, Baffin, the studies found that precipitation and mean diurnal temperature range were the most influential variables
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Northern river otter
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The North American river otter, also known as the northern river otter or the common otter, is a semiaquatic mammal endemic to the North American continent found in and along its waterways and coasts. An adult river otter can weigh between 5.0 and 14 kg, the river otter is protected and insulated by a thick, water-repellent coat of fur. The river otter, a member of the subfamily Lutrinae in the family, is equally versatile in the water. It establishes a close to the waters edge in river, lake, swamp, coastal shoreline, tidal flat. The den typically has many openings, one of which generally allows the otter to enter. Female otters give birth in these burrows, producing litters of one to six young. North American river otters, like most predators, prey upon the most readily accessible species, fish is a favored food among the otters, but they also consume various amphibians, freshwater clams, mussels, snails, small turtles and crayfish. Instances of river otters eating small mammals and occasionally birds have been reported as well, the range of the North American river otter has been significantly reduced by habitat loss, beginning with the European colonization of North America. In some regions, though, their population is controlled to allow the trapping and harvesting of otters for their pelts, River otters are very susceptible to the effects of environmental pollution, which is a likely factor in the continued decline of their numbers. A number of projects have been initiated to help stabilize the reduction in the overall population. The North American river otter was first described by German naturalist Johann Christian Daniel von Schreber in 1777. The mammal was identified as a species of otter and has a variety of names, including North American river otter, northern river otter, common otter and, simply. Other documented common names are American otter, Canada otter, Canadian otter, fish otter, land otter, nearctic river otter, the river otter was first classified in the genus Lutra, Lutra was the early European name. The species name was Lutra canadensis, the species epithet canadensis means of Canada. In a new classification, the species is called Lontra canadensis, molecular biological techniques have been used to determine when the river otter and the giant otter of South America diverged. These analyses suggest they diverged in the Miocene epoch 23.03 to 5.33 million years ago, which is much earlier than indicated in the fossil record. Fossils of a giant river otter dating back 3.5 Mya have been found in the US Midwest, the earliest known fossil of Lontra canadensis, found in the US Midwest, is from the Irvingtonian stage. The oldest fossil record of an Old World river otter comes from the late Pliocene epoch
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North American porcupine
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The North American porcupine, also known as the Canadian porcupine or common porcupine, is a large rodent in the New World porcupine family. The beaver is the rodent in North America that is larger than the North American porcupine. The word porcupine comes from the middle or old French word porcespin and its roots derive from the Latin words porcus or pig and spina meaning thorns. Other colloquial names for the animal include quill pig and it is also referred to as the Canadian porcupine or common porcupine. The porcupines scientific name, Erethizon dorsatum, can be translated as the animal with the irritating back. Several Native American names exist, such as the Lakota name pahin meaning quill, the North American porcupine migrated from South America, where all New World porcupines or hystricomorphs evolved. Erethizon appeared in North America shortly after the two joined together in the later Tertiary period. Other hystricomorphs also migrated, but Erethizon was the one to survive north of Mexico. No known fossils are attributed to prior to the late Tertiary period. Some fossils, such as species from the family Paramyidae, show resemblance to the porcupine, South American hystricomorphs first appeared in the Lower Oligocene period. They are thought to have migrated from Africa, ancestors of the Old World porcupines or Hystricidae or they originated based on a migration of the North American Paramyidae. The earliest appearance of E. dorsatum is from the Pleistocene era found along the Arroyo del Cedazo near Aguascalientes, seven subspecies of E. dorsatum are recognized. They are subdivided by different ranges across North America, by far the most common is E. d. dorsatum, which ranges from Nova Scotia to Alberta and from Virginia to the Yukon. E. d. picinum occupies a range in northeastern Quebec. E. d. couesi is the most southern ranging from northern Mexico to Colorado, E. d. bruneri can be found in the midwest from Arkansas to Montana. The last three are western species, from south to north they are E. d. epixanthum, E. d. nigrescens, and E. d. myops. Porcupines are usually brown or black in color, with white highlights. They have a body, a small face, short legs
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Moose
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The moose or elk, Alces alces, is the largest extant species in the deer family. Moose are distinguished by the broad, flat antlers of the males, Moose typically inhabit boreal forests and temperate broadleaf and mixed forests of the Northern Hemisphere in temperate to subarctic climates. Hunting and other activities have caused a reduction in the size of the mooses range over time. Moose have been reintroduced to some of their former habitats, currently, most moose are found in Canada, Alaska, New England, Fennoscandia, Latvia, Estonia and Russia. Their diet consists of terrestrial and aquatic vegetation. The most common predators are the gray wolf along with bears. Unlike most other species, moose are solitary animals and do not form herds. Although generally slow-moving and sedentary, moose can become aggressive and move quickly if angered or startled and their mating season in the autumn features energetic fights between males competing for a female. Alces alces is called a moose in North American English, and that same word elk in North American English refers to a completely different species of deer, the Cervus canadensis, also called the wapiti. A mature male moose is called a bull, a female a cow. The word elk originated from Proto-Germanic languages, from which Old English evolved, the British English word elk has cognates in other Indo-European languages, for example elg in Danish/Norwegian, älg in Swedish, alnis in Latvian, Elch in German, and łoś in Polish. In the continental-European languages, these forms of the word elk almost always refer to the Alces alces, the word moose first entered English by 1606 and is borrowed from the Algonquian languages, and possibly involved forms from multiple languages mutually reinforcing one another. The term moose is a name of North American origin, the animal is known in British English as the elk. The moose became extinct in Britain during the Bronze Age, long before the Europeans discovery of America, the youngest bones were found in Scotland and are roughly 3900 years old. Dictionaries of the 18th century simply described elk as a deer that was as large as a horse, confusingly, the word elk is used in North America to refer to a different animal, Cervus canadensis, which is also called by the Algonkian indigenous name, wapiti. The British began colonizing America in the 17th century, and found two common species of deer for which they had no names, the wapiti appeared very similar to the red deer of Europe although it was much larger and was not red. The moose was a rather strange-looking deer to the colonists, the wapiti is very similar to the red deer of central and western Europe, although it is distinctly different behaviorally and genetically. Early European explorers in North America, particularly in Virginia where there were no moose, called the wapiti elk because of its size, the moose resembled the German elk, which was less familiar to the British colonists
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White-tailed deer
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The white-tailed deer, also known as the whitetail, is a medium-sized deer native to the United States, Canada, Mexico, Central America, and South America as far south as Peru and Bolivia. It has also introduced to New Zealand, Cuba, Jamaica, Hispaniola, Puerto Rico, Bahamas, Lesser Antilles, and some countries in Europe, such as Finland, the Czech Republic. In the Americas, it is the most widely distributed wild ungulate, in North America, the species is widely distributed east of the Rocky Mountains, but elsewhere, it is mostly replaced by the black-tailed or mule deer. Some taxonomists have attempted to separate white-tailed deer into a host of subspecies, genetic studies, however, suggest fewer subspecies within the animals range, as compared to the 30 to 40 subspecies that some scientists described in the last century. The Florida Key deer, O. virginianus clavium, and the Columbian white-tailed deer, in the United States, the Virginia white-tail, O. virginianus virginianus, is among the most widespread subspecies. The white-tailed deer species has tremendous genetic variation and is adaptable to several environments, several local deer populations, especially in the southern states, are descended from white-tailed deer transplanted from various localities east of the Continental Divide. Some of these populations may have been from as far north as the Great Lakes region to as far west as Texas, yet are also quite at home in the Appalachian. These deer over time have intermixed with the indigenous deer populations. Central and South America have a number of white-tailed deer subspecies that range from Guatemala as far south as Peru. This list of subspecies of deer is more exhaustive than the list of North American subspecies, however, the white-tailed deer populations in these areas are difficult to study, due to overhunting in many parts and a lack of protection. Some areas no longer carry deer, so it is difficult to assess the genetic difference of these animals, the deer can be recognized by the characteristic white underside to its tail. It raises its tail when it is alarmed to warn the predator that it has been detected, a population of white-tailed deer in New York is entirely white —not albino—in color. The former Seneca Army Depot in Romulus, New York, has the largest known concentration of white deer, strong conservation efforts have allowed white deer to thrive within the confines of the depot. White-tailed deers horizontally slit pupils allow for night vision and color vision during the day. The white-tailed deer is highly variable in size, generally following Bergmanns rule that the size is larger farther away from the Equator. North American male deer usually weigh 45 kilograms, but in rare cases, mature bucks over 180 kilograms have been recorded in the northernmost reaches of their native range, specifically, Minnesota and Ontario. In 1926, Carl J. Lenander, Jr. took a white-tailed buck near Tofte, MN, the female in North America usually weighs from 40 to 90 kg. White-tailed deer from the tropics and the Florida Keys are markedly smaller-bodied than temperate populations, averaging 35 to 50 kg, white-tailed deer from the Andes are larger than other tropical deer of this species and have thick, slightly woolly looking fur
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Caribou
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A caribou is any of several North American subspecies, ecotypes, populations, and herds of the species Rangifer tarandus, or reindeer. In North America caribou vary in size from the smallest, the Peary caribou, to the largest, barren-ground, porcupine caribou and Peary caribou live in the tundra, while the shy woodland caribou prefers the boreal forest. The migrations of caribou herds are among the longest of any terrestrial mammal. Barren-land caribou are found in Kitaa in Greenland, but the larger herds are in Alaska, the Northwest Territories. The George River caribou herd, in the Ungava Peninsula of Quebec, by 2012 the herd numbered 27,600 and declined to 14,200 animals in 2014. The metapopulation of the more-sedentary subspecies R. t. caribou, or woodland caribou and they are shy animals whose main food source is arboreal lichens of the mature forests and mainly live in marshes, bogs, lakes, and river regions. Since it takes hundreds of years for a biomass of tree lichen to be adequate to sustain boreal woodland caribou populations, deforestation has been a major factor in the decline of their numbers. The historic range of the woodland caribou covered over half of present-day Canada, stretching from Alaska to Newfoundland and Labrador and as far south as New England, Idaho. The smallest subspecies in North America, the Peary caribou is found in the High and Low Arctic, in the Northwest Territories, Caribou can reach a speed of 60–80 km/h. Young caribou can already outrun an Olympic sprinter when only a day old, the caribous favourite winter food is fruticose deer lichen. Seventy percent of the diet of woodland caribou consists of arboreal lichen which take hundreds of years to grow and are only found in mature forests. Although there are variations in colour and size, Canadian Geographic magazine states that in general. Barren-ground caribou have large distinguishing white patches of fur that extend beyond the neck onto the back, a white muzzle and their fur is sandy-beige in winter and light brown in summer. The woodland caribou have a more compact body and wider antlers. The coat is a dark brown in summer and dark grey in winter. Both the barren-ground and woodland caribou often have white socks above their hooves, on average the male weighs 90–110 kg and measures 0. 9–1.7 m in shoulder height. The woodland caribou are the largest, and the Peary caribou are the smallest, the largest Alaskan male Porcupine caribou can weigh as much as 310 kilograms. Female caribou can live up to 17 years, and male caribou live about 13 years, both sexes grow antlers, though in some woodland caribou populations, the females lack antlers completely
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Mammal
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Mammals are any vertebrates within the class Mammalia, a clade of endothermic amniotes distinguished from reptiles by the possession of a neocortex, hair, three middle ear bones and mammary glands. All female mammals nurse their young with milk, secreted from the mammary glands, Mammals include the largest animals on the planet, the great whales. The basic body type is a quadruped, but some mammals are adapted for life at sea, in the air, in trees. The largest group of mammals, the placentals, have a placenta, Mammals range in size from the 30–40 mm bumblebee bat to the 30-meter blue whale. With the exception of the five species of monotreme, all modern mammals give birth to live young, most mammals, including the six most species-rich orders, belong to the placental group. The largest orders are the rodents, bats and Soricomorpha, the next three biggest orders, depending on the biological classification scheme used, are the Primates, the Cetartiodactyla, and the Carnivora. Living mammals are divided into the Yinotheria and Theriiformes There are around 5450 species of mammal, in some classifications, extant mammals are divided into two subclasses, the Prototheria, that is, the order Monotremata, and the Theria, or the infraclasses Metatheria and Eutheria. The marsupials constitute the group of the Metatheria, and include all living metatherians as well as many extinct ones. Much of the changes reflect the advances of cladistic analysis and molecular genetics, findings from molecular genetics, for example, have prompted adopting new groups, such as the Afrotheria, and abandoning traditional groups, such as the Insectivora. The mammals represent the only living Synapsida, which together with the Sauropsida form the Amniota clade, the early synapsid mammalian ancestors were sphenacodont pelycosaurs, a group that produced the non-mammalian Dimetrodon. At the end of the Carboniferous period, this group diverged from the line that led to todays reptiles. Some mammals are intelligent, with some possessing large brains, self-awareness, Mammals can communicate and vocalize in several different ways, including the production of ultrasound, scent-marking, alarm signals, singing, and echolocation. Mammals can organize themselves into fission-fusion societies, harems, and hierarchies, most mammals are polygynous, but some can be monogamous or polyandrous. They provided, and continue to provide, power for transport and agriculture, as well as commodities such as meat, dairy products, wool. Mammals are hunted or raced for sport, and are used as model organisms in science, Mammals have been depicted in art since Palaeolithic times, and appear in literature, film, mythology, and religion. Defaunation of mammals is primarily driven by anthropogenic factors, such as poaching and habitat destruction, Mammal classification has been through several iterations since Carl Linnaeus initially defined the class. No classification system is accepted, McKenna & Bell and Wilson & Reader provide useful recent compendiums. Though field work gradually made Simpsons classification outdated, it remains the closest thing to a classification of mammals
40.
Barred owl
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The barred owl is a large typical owl native to North America. Best known as the hoot owl for its call, it goes by many other names, including eight hooter, rain owl, wood owl. The adult is 40–63 cm long with a 96–125 cm wingspan, weight in this species is 500 to 1,050 g. It has a face with dark rings around the eyes. It is the typical owl of the eastern United States which has brown eyes. The upper parts are mottled gray-brown, the underparts are light with markings, the chest is barred horizontally while the belly is streaked vertically. The legs and feet are covered in feathers up to the talons, the head is round and lacks ear tufts. Outside of the closely related spotted owl, this streaky, dark-eyed, the spotted owl is similar in appearance, but is slightly smaller and has spots rather than streaks down the underside. The great horned owl is much larger, has ear tufts, during the past century, barred owls expanded their range from forests east of the Great Plains to forests throughout most of central and western North America. Evidently, barred owls originally traveled across the northern Great Plains via the forested riparian corridors of the Missouri, Yellowstone, from there, they accessed western forests in southwestern Montana, moved to northwestern Montana and then expanded their range in two general directions. They moved north and east to northern Alberta and Saskatchewan where they encountered other barred owls coming westward from Manitoba. They also moved north to northern British Columbia, southeastern Alaska and Northwest Territories, and west and south to Washington, Idaho, Oregon, and California. The historical lack of trees in the Great Plains evidently acted as a barrier to the range expansion, so it appears the range expansion was prohibited for millennia by actions of Native Americans and recently facilitated by actions of European settlers. Breeding habitats are dense woods across Canada, the United States, the species is particularly numerous in a variety of wooded habitats in the southeastern United States. Recent studies show suburban neighborhoods can be habitat for barred owls. Using transmitters, scientists found that some regional populations increased faster in the suburban settings than in old growth forest, a factor of this suburban success may be easily accessible rodent prey in such settings. However, for breeding and roosting needs, this species needs at least some large trees, the main danger to owls in suburban settings is from cars. The increased offspring offset the death rate due to impacts from cars and disease
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American kestrel
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The American kestrel is the smallest and most common falcon in North America. It has about a two to one range in size over subspecies and sex, varying in size from about the weight of a blue jay to a mourning dove. It also ranges to South America, and is an established species that has evolved seventeen subspecies adapted to different environments and habitats throughout the Americas. It exhibits sexual dimorphism in size and plumage, although both sexes have a back with noticeable barring. Its plumage is colorful and attractive, and juveniles are similar in plumage to adults, the American kestrel usually hunts in energy conserving fashion by perching and scanning the ground for prey to ambush, though it also hunts from the air. It sometimes hovers in the air with rapid wing beats while homing in on prey and its diet typically consists of grasshoppers and other insects, lizards, mice, and small birds. This broad diet has contributed to its success as a species. It nests in cavities in trees, cliffs, buildings, the female lays three to seven eggs, which both sexes help to incubate. Its breeding range extends from central and western Alaska across northern Canada to Nova Scotia, and south throughout North America, into central Mexico and it is a local breeder in Central America and is widely distributed throughout South America. Most birds breeding in Canada and the northern United States migrate south in the winter and it is an occasional vagrant to western Europe. Though the species has not been renamed as a result of genetic analyses. Instead, a process of convergent evolution to fit a small prey niche in the ecosystem as the true kestrels has left it with similar physical characteristics. The American kestrel is a bird used in falconry, especially by beginners. Under traditional classification, the American kestrel is the smallest raptor in America, the American kestrel is sexually dimorphic, although there is some overlap in plumage coloration between the sexes. The bird ranges from 22 to 31 cm in length with a wingspan of 51–61 cm, the female kestrel is larger than the male, though less so than larger falcons, being typically about 10% to 15% larger within a subspecies. The more northern subspecies tend to larger sizes, with a large northern female being about twice the size of a small southern male, the male typically weighs 80–143 g, and the female 86–165 g. In standard measurements, the bone is 16–21 cm long, the tail is 11–15 cm. Physically, American kestrels are leaner and less muscular than larger falcons, the pectoral flight muscles of the American kestrel make up only about 12% of its body weight, as compared to about 20% for the strongest flying falcons such as the peregrine
42.
Osprey
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The osprey —also called fish eagle, sea hawk, river hawk, and fish hawk—is a diurnal, fish-eating bird of prey with a cosmopolitan range. It is a raptor, reaching more than 60 cm in length and 180 cm across the wings. It is brown on the upperparts and predominantly greyish on the head, the osprey tolerates a wide variety of habitats, nesting in any location near a body of water providing an adequate food supply. It is found on all continents except Antarctica, although in South America it occurs only as a non-breeding migrant, as its other common names suggest, the ospreys diet consists almost exclusively of fish. It possesses specialised physical characteristics and exhibits unique behaviour to assist in hunting and catching prey, as a result of these unique characteristics, it has been given its own taxonomic genus, Pandion and family, Pandionidae. Four subspecies are recognized, one of which has recently been given full species status. Despite its propensity to nest near water, the osprey is not classed as a sea eagle, the osprey was one of the many species described by Carl Linnaeus in his 18th-century work, Systema Naturae, and named as Falco haliaeetus. The genus, Pandion, is the member of the family Pandionidae, and used to contain only one species. The genus Pandion was described by the French zoologist Marie Jules César Savigny in 1809, the osprey differs in several respects from other diurnal birds of prey. Its toes are of length, its tarsi are reticulate. The osprey and owls are the only raptors whose outer toe is reversible and this is particularly helpful when they grab slippery fish. The Sibley-Ahlquist taxonomy has placed it together with the diurnal raptors in a greatly enlarged Ciconiiformes. The osprey is unusual in that it is a living species that occurs nearly worldwide. Even the few subspecies are not unequivocally separable, there are four generally recognised subspecies, although differences are small, and ITIS lists only the first two. P. h. carolinensis –, North America and this form is larger, darker bodied and has a paler breast than nominate haliaetus. P. h. ridgwayi – Maynard,1887, Caribbean islands and this form has a very pale head and breast compared with nominate haliaetus, with only a weak eye mask. Its scientific name commemorates American ornithologist Robert Ridgway, P. h. cristatus –, coastline and some large rivers of Australia and Tasmania. The smallest and most distinctive subspecies, also non-migratory, recently, P. h. cristatus has been given full species status as eastern osprey
43.
Brook trout
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The brook trout is a species of freshwater fish in the salmon family Salmonidae. It is native to Eastern North America in the United States and Canada, in parts of its range, it is also known as the eastern brook trout, speckled trout, brook charr, squaretail, or mud trout, among others. A potamodromous population in Lake Superior is known as trout or, simply. The brook trout was first scientifically described as Salmo fontinalis by the naturalist Samuel Latham Mitchill in 1814, the specific epithet fontinalis comes from the Latin for of a spring or fountain, in reference to the clear, cold streams and ponds in its native habitat. The species was moved to the char genus Salvelinus. Though commonly called a trout, the trout is thus actually one of the chars, which in North America also include the lake trout, bull trout, Dolly Varden. There is little recognized systematic substructure in the trout. On the other hand, three forms are distinguished. The aurora trout, S. f. timagamiensis, is a native to two lakes in the Temagami District of Ontario, Canada. The silver trout, is an extinct species or subspecies last seen in Dublin Pond, New Hampshire. It is considered by fisheries biologist Robert J. Behnke as a specialized form of brook trout. Robert J. Behnke describes three forms of the brook trout. A large lake form evolved in the lakes in the northern reaches of its range and are generally piscivorous as adults. A sea-run form that migrates into saltwater for short periods of time to feed evolved along the Atlantic coastline, finally, a smaller generalist form that evolved in the small lakes, ponds, rivers, and streams throughout most of the original native range. This generalist form rarely attains sizes larger than 12 in or lives for more than three years, all three forms have the same general appearance. The brook trout produces hybrids both with its congeners Salvelinus namaycush and Salvelinus alpinus, and intergeneric hybrids with Salmo trutta, the splake is an intrageneric hybrid between the brook trout and lake trout. Although uncommon in nature, they are propagated in substantial numbers for stocking into brook trout or lake trout habitats. Although they are fertile, back-crossing in nature is behaviorally problematic, splake grow more quickly than brook trout and become piscivorous sooner and are more tolerant of competitors than brook trout
44.
Atlantic salmon
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The Atlantic salmon is a species of ray-finned fish in the family Salmonidae. It is found in the northern Atlantic Ocean, in rivers that flow into the north Atlantic and, due to human introduction, the Atlantic salmon was given its scientific binomial name by zoologist and taxonomist Carl Linnaeus in 1758. The name, Salmo salar, derives from the Latin salmo, meaning salmon, and salar, meaning leaper, according to M. Barton, lewis and Shorts Latin Dictionary translates salar as a kind of trout from its use in the Idylls of the poet Ausonius. Later, the differently coloured smolts were found to be the same species, other names used to reference Atlantic salmon are, bay salmon, black salmon, caplin-scull salmon, Sebago salmon, silver salmon, fiddler, or outside salmon. At different points in their maturation and life cycle, they are known as parr, smolt, grilse, grilt, kelt, slink, Atlantic salmon that do not journey to sea are known as landlocked salmon or ouananiche. The species is the longest and heaviest in genus Salmo, after two years at sea, the fish average 71 to 76 cm in length and 3.6 to 5.4 kg in weight. But specimens that spend four or more winters feeding at sea can be much larger. An Atlantic salmon netted in 1960 in Scotland, in the estuary of the river Hope, was weighed in at 49.44 kg, the colouration of young Atlantic salmon does not resemble the adult stage. While they live in water, they have blue and red spots. At maturity, they take on a silver-blue sheen, the easiest way of identifying them as an adult is by the black spots predominantly above the lateral line, though the caudal fin is usually unspotted. When they reproduce, males take on a green or red colouration. The salmon has a body, and well-developed teeth. All fins, save the adipose, are bordered with black, the distribution of Atlantic salmon depends on water temperature. Because of climate change, some of the southern populations, in Spain. Before human influence, the breeding grounds of Atlantic salmon were rivers in Europe. When North America was settled by Europeans, eggs were brought on trains to the west coast, other attempts to bring Atlantic salmon to new settlements were made, e. g. But since there are no suitable ocean currents on New Zealand, there is at least one landlocked population of Atlantic salmon on New Zealand, where the fish never go out to sea. Young salmon spend one to four years in their natal river, when they are large enough, they smoltify, changing camouflage from stream-adapted with large, gray spots to sea-adapted with shiny sides
45.
Alsek River
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The Alsek River is a wilderness river flowing from Yukon into Northern British Columbia and into Alaska. It enters the Gulf of Alaska at Dry Bay, most of the Alsek Rivers basin is within protected wilderness areas and National Parks. The Alsek and its tributary, the Tatshenshini River, are part of the Canadian Heritage Rivers System. The Alsek starts at the confluence of the Dezadeash River and Kaskawulsh River in Kluane National Park, after flowing south into the northwestern tip of British Columbia, it is joined by the Tatshenshini River in Tatshenshini-Alsek Park. It reaches the Pacific Ocean at Dry Bay, in the Gulf of Alaska, south of Yakutat, Alaska, although the river is navigable by kayak or rubber raft in its northern reaches, it rapidly becomes unnavigable—for any but the most experienced and skilled kayakers—at Turnback Canyon. On older maps, the Alsek river is labeled as the Kaskawulsh, some Yukon First Nation elders also refer to the river as the Kaskawulsh. The river flows next to the Lowell glacier which has sometimes blocked off the river and created a lake behind it. The last such blockage took place in 1850, its release created a massive flood, the river carries a lot of silt from the Alsek lake/glacier, which contributes to the rivers low temperature. The Alsek and nearby East Alsek rivers were at one time connected, the Alsek glacier contacts the Grand Plateau Glacier, which faces the shoreline. Also in the general area are the Doame foothills and Doame River. The first known kayak descent of Turnback Canyon was by Walt Blackadar and he wrote about his trip for Sports Illustrated. I want any other kayaker or would-be expert to read my words well, despite this sincere warning from a man who apparently felt lucky to be alive, groups of expert kayakers have successfully run Turnback Canyon since then. A prominent mountain which overlooks the Alsek was named Mount Blackadar in his honor, the portion of the river inside Kluane National Park has been designated a Canadian Heritage River. In 1958, a magnitude 7.7 earthquake centered near Lituya bay significantly changed the lay of the land, the earthquake caused the Doame River and East Alsek River to join together. The Alsek and East Alsek rivers are a part of the Yakutat area limited entry set gillnet fishery, both rivers produce king, silver, and sockeye commercially. Chum and pink salmon can also be caught, but are not generally sought after due to their lack of worth/quality. These two rivers can be characterized as low volume fisheries, while the Alsek river in particular produces particularly high quality due to its low temperature. The Alseks silt content also prevents the sun from damaging the fish, the area also supports subsistence and sport fishing
