1.
Anticosti Island
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Anticosti Island is an island in the province of Quebec, Canada at the outlet of the Saint Lawrence River into the Gulf of Saint Lawrence, between 49° and 50° N. and between 61°40 and 64°30 W. At 7,892.52 km2 in size, it is the 90th largest island in the world, Anticosti Island is separated on the north from the Côte-Nord region of Quebec by the Jacques Cartier Strait, and on the south from the Gaspé Peninsula by the Honguedo Strait. The entire island constitutes one municipality known as LÎle-dAnticosti, due to more than 400 shipwrecks off its coasts, Anticosti Island is sometimes called the Cemetery of the Gulf. Anticosti Island is part of the eastern Saint Lawrence lowlands and it is 217 km long and has a maximum breadth of 48 km —1½ times as large as the province of Prince Edward Island. Its coastline is 520 km long, and is rocky and dangerous, offering shelter for ships except in Gamache, Ellis. There are large shoals to the south, the largest lake on the island is Lake Wickenden, which feeds the Jupiter River. There are numerous rivers on Anticosti, many of which flow through deep gorges and this plateau is a unidirectional structure slightly tilted to the south, and is characterized by rolling cuestas. The rocks exposed on the form a continuous sedimentary stratum more than 2,000 m thick. These are the most complete strata in eastern North America of the Ordovician and Silurian periods, the climate of Anticosti Island is maritime sub-boreal, tempered by the maritime influence of the Gulf of St. Lawrence which reduces the temperature differences. The average annual temperature is 1.9 °C, the month of July is the warmest with an average temperature of 14.79 °C. Conversely, February is the coldest month, on average −11.2 °C, snow precipitation is abundant, usually accumulating over 300 centimetres in the western and central parts. For thousands of years, Anticosti Island was the territory of the peoples who lived on the mainland. The Innu called it Notiskuan, translated as where bears are hunted, the French explorer Jacques Cartier sailed along its shore in the summer of 1534. He provided its first written description and named it Isle de lAssomption and this name had fallen into disuse by 1656. About 1586, the historian André Thevet wrote that the savages named Naticousti, while Samuel de Champlain spelled it Antiscoti, from that time on, France had officially incorporated the island into its colonial empire. Its first settlers arrived in 1680 when King Louis XIV gave Louis Jolliet the Seigneury of the Mingan Archipelago and Anticosti Island as compensation for exploring the Mississippi and Hudson Bay. Louis Jolliet erected a fort on Anticosti and in the spring of 1681 settled there with his wife, four children and six servants. His fort was captured and occupied during the winter of 1690 by some of the Massachusetts troops of William Phips during their retreat after an attempt to capture Quebec City
2.
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
3.
Country
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A country is a region that is identified as a distinct national entity in political geography. Sometimes the word countries is used to both to sovereign states and to other political entities, while other times it refers only to states. The word country comes from Old French contrée, itself derived from Vulgar Latin contrata and it most likely entered the English language after the Franco-Norman invasion during the 11th century. Areas much smaller than a state may be called by names such as the West Country in England, the Black Country, Constable Country. In many European countries the words are used for sub-divisions of the territory, as in the German Bundesländer. The modern Italian contrada is a word with its meaning varying locally, the term country is frequently used to refer to sovereign states. There is no agreement on the number of countries in the world. There are 206 sovereign states, of which 193 states are members of the United Nations, all are defined as states by declarative theory of statehood and constitutive theory of statehood. The latest proclaimed state is South Sudan in 2011, the Kingdom of Denmark, a sovereign state, comprises Metropolitan Denmark and two nominally separate countries—the Faroe Islands, and Greenland—which are almost fully internally self-governing. The Kingdom of the Netherlands, a state, comprises four separate countries, Netherlands, Aruba, Curaçao. The degree of autonomy of non-sovereign countries varies widely, some are possessions of sovereign states, as several states have overseas territories, with citizenry at times identical and at times distinct from their own
4.
Canada
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Canada is a country in the northern half of North America. Canadas border with the United States is the worlds longest binational land border, the majority of the country has a cold or severely cold winter climate, but southerly areas are warm in summer. Canada is sparsely populated, the majority of its territory being dominated by forest and tundra. It is highly urbanized with 82 per cent of the 35.15 million people concentrated in large and medium-sized cities, One third of the population lives in the three largest cities, Toronto, Montreal and Vancouver. Its capital is Ottawa, and other urban areas include Calgary, Edmonton, Quebec City, Winnipeg. Various aboriginal peoples had inhabited what is now Canada for thousands of years prior to European colonization. Pursuant to the British North America Act, on July 1,1867, the colonies of Canada, New Brunswick and this began an accretion of provinces and territories to the mostly self-governing Dominion to the present ten provinces and three territories forming modern Canada. With the Constitution Act 1982, Canada took over authority, removing the last remaining ties of legal dependence on the Parliament of the United Kingdom. Canada is a parliamentary democracy and a constitutional monarchy, with Queen Elizabeth II being the head of state. The country is officially bilingual at the federal level and it is one of the worlds most ethnically diverse and multicultural nations, the product of large-scale immigration from many other countries. Its advanced economy is the eleventh largest in the world, relying chiefly upon its abundant natural resources, Canadas long and complex relationship with the United States has had a significant impact on its economy and culture. Canada is a country and has the tenth highest nominal per capita income globally as well as the ninth highest ranking in the Human Development Index. It ranks among the highest in international measurements of government transparency, civil liberties, quality of life, economic freedom, Canada is an influential nation in the world, primarily due to its inclusive values, years of prosperity and stability, stable economy, and efficient military. While a variety of theories have been postulated for the origins of Canada. In 1535, indigenous inhabitants of the present-day Quebec City region used the word to direct French explorer Jacques Cartier to the village of Stadacona, from the 16th to the early 18th century Canada referred to the part of New France that lay along the St. Lawrence River. In 1791, the area became two British colonies called Upper Canada and Lower Canada collectively named The Canadas, until their union as the British Province of Canada in 1841. Upon Confederation in 1867, Canada was adopted as the name for the new country at the London Conference. The transition away from the use of Dominion was formally reflected in 1982 with the passage of the Canada Act, later that year, the name of national holiday was changed from Dominion Day to Canada Day
5.
Provinces and territories of Canada
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Canadas geography is divided into administrative divisions known as provinces and territories that are responsible for delivery of sub-national governance. Over its history, Canadas international borders have changed several times, the ten provinces are Alberta, British Columbia, Manitoba, New Brunswick, Newfoundland and Labrador, Nova Scotia, Ontario, Prince Edward Island, Quebec, and Saskatchewan. Several of the provinces were former British colonies, Quebec was originally a French colony, the three territories are Northwest Territories, Nunavut, and Yukon, which govern the rest of the area of the former British North America. Together, the provinces and territories make up the worlds second-largest country by area, the powers flowing from the Constitution Act are divided between the federal government and the provincial governments to exercise exclusively. In modern Canadian constitutional theory, the provinces are considered to be co-sovereign divisions, the territories are not sovereign, but simply part of the federal realm, and have a commissioner who represents the federal government. Notes, There are three territories in Canada, unlike the provinces, the territories of Canada have no inherent sovereignty and have only those powers delegated to them by the federal government. They include all of mainland Canada north of latitude 60° north and west of Hudson Bay, the following table lists the territories in order of precedence. Prior to Confederation, Ontario and Quebec were united as the Province of Canada, over the following years, Manitoba, British Columbia, and Prince Edward Island were added as provinces. The Hudsons Bay Company controlled large swathes of western Canada referred to as Ruperts Land and the North-Western Territory until 1870, subsequently, the area was re-organized into the province of Manitoba and the Northwest Territories. The remaining Arctic islands were transferred by Britain to Canada in 1880,1898 saw the Yukon Territory, later renamed simply as Yukon, carved from the parts of the Northwest Territories surrounding the Klondike gold fields. On September 1,1905, a portion of the Northwest Territories south of the 60th parallel north became the provinces of Alberta and Saskatchewan. In 1912, the boundaries of Quebec, Ontario and Manitoba were expanded northward, Manitobas to the 60° parallel, Ontarios to Hudson Bay, in 1907, Newfoundland acquired dominion status. In the middle of the Great Depression in Canada with Newfoundland facing a period of economic crisis. In 2001, it was officially renamed Newfoundland and Labrador, in 1903, the Alaska Panhandle Dispute fixed British Columbias northwestern boundary. This was one of two provinces in Canadian history to have its size reduced. In 1999, Nunavut was created from the portion of the Northwest Territories. Yukon lies in the portion of The North, while Nunavut is in the east. All three territories combined are the most sparsely populated region in Canada, covering 3,921,739 km2 in land area and they are often referred to as a single region, The North, for organisational and economic purposes
6.
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
7.
Peninsula
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A peninsula is a piece of land surrounded by water on the majority of its border, while being connected to a mainland from which it extends out. Examples include the upper and lower peninsulas of the state of Michigan, the surrounding water is usually understood to be continuous, though not necessarily named as a single body of water. Peninsulas are not always named as such, one can also be a headland, cape, island promontory, bill, point, a point is generally considered a tapering piece of land projecting into a body of water that is less prominent than a cape. A river which courses through a very tight meander is also said to form a peninsula within the loop of water. In English, the plural of peninsula is peninsulas or, less commonly, peninsulas can be found on coastlines and in smaller bodies of water throughout the world, ranging in scale from square meters to millions of square kilometers. Theres the Scandinavian Peninsula in Northern Europe, and in Southern Europe theres the Iberian Peninsula, the Italian Peninsula, south America has the Brunswick Peninsula, and Antarctica has the Antarctic Peninsula. In Africa, theres the Horn of Africa, and in Australia, asia has the 3 largest peninsulas in the world, the Arabian Peninsula, the Indian Peninsula, and the Indochinese Peninsula
8.
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
9.
Matapedia Valley
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The Matapedia Valley was formed by the Chic-Choc Mountains of eastern Québec. Its name is derived from the river traverses the valley. It is situated in the southwest of the Gaspé Peninsula and stretches 375 km, the land is primarily made up of forest and agriculture, and is home to more than 20,000 inhabitants in some thirty municipalities. Most of them are concentrated along the avenue of communication. The city of Amqui is the seat of the RCM and is home to 6,261 people, the Mikmaq people first developed the valley around 500 BCE. French-Canadian settlement began in 1833 when Pierre Brochu moved to Lake Matapedia along Kempt Road, settlers began flocking to the land in the late nineteenth century with the development of land clearing, agriculture, and the logging industry. Silas Tertius Rand, a noted linguist and source from the nineteenth century. It has also been spelled many different ways over time such as Matapediach, Madapeguia, Matapeguia, Matapediac, Matakpediack, Madapeguia, Metapedia, at the western extremity of the valley is the village of Sainte-Angèle-de-Mérici, Quebec. From north to south, it runs a length of 375 km until it reaches the Restigouche River to the east, the village of Matapédia, Quebec lies on the valleys eastern tip. The valley is situated south of the Saint Lawrence River in the regions of Bas-Saint-Laurent. This makes it the region in the Gaspé Peninsula that does not border the sea. The Matapedia Valley is dug into the Chic-Choc mountain range, which is situated at the extremity of the Appalachians. It has two bodies of water, Lake Matapedia, which extends from Sayabec to Amqui, and Lac-au-Saumon. The valley reaches from the St. Lawrence River to Chaleur Bay, the northwest region of the valley is rather flat and surrounded by small mounts that do not exceed 400 metres. More towards the center of the valley, near St. Cleophas and St. Irène, the southeastern area of the valley is more rugged and steep, with summits reaching about 600 metres. At the other extreme, Lake Matapedia rests at an altitude of 158 metres, the Matapedia Valley includes 20,000 hectares of land dedicated to agriculture and 500,000 hectares of forest divided equally between the public and private sectors. The main agricultural municipalities of the valley are Amqui, Causapscal, Saint-Damase, Val-Brillant, the floor of the valley belongs to the Appalachian rock formation. It is composed primarily of Gaspé feldspar sandstone, Gaspé limestone, and a mixture of sandstone, mudstone, the territory of the Matapedia Valley is drained through the Matapedia River, which has a watershed area of 3,824 square kilometres
10.
Gulf of Saint Lawrence
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The Gulf of Saint Lawrence is the outlet of the North American Great Lakes via the Saint Lawrence River into the Atlantic Ocean. The gulf is a sea, covering an area of about 236,000 square kilometres and containing about 35,000 cubic kilometres of water. As for significant islands the Gulf of Saint Lawrence contains Anticosti Island, PEI, Îles-de-la-Madeleine, Cape Breton Island, Saint Pierre Island, and Miquelon-Langlade. Half of the ten provinces of Canada adjoin the Gulf, New Brunswick, Nova Scotia, Prince Edward Island, Newfoundland and Labrador, and Quebec. Branches of the Gulf include the Chaleur Bay, Fortune Bay, Miramichi Bay, St. Georges Bay, Bay St. George, Bay of Islands, the Cabot Strait between Newfoundland and Saint-Pierre and Cape Breton Island,104 km wide and 480 m deep at its deepest. The Strait of Canso between Cape Breton Island and the Nova Scotia peninsula,1.0 km wide and 60 m deep at its deepest. Due to the construction of the Canso Causeway across the strait in 1955, the limits of the Gulf of Saint Lawrence vary between sources. The International Hydrographic Organization defines the limits of the Gulf of Saint Lawrence as follows, Fisheries, St. Paul Island, Nova Scotia, off the northeastern tip of Cape Breton Island, is referred to as the Graveyard of the Gulf because of its many shipwrecks. Access to this island is controlled by the Canadian Coast Guard, the five provinces bordering the Gulf of Saint Lawrence also have several provincial parks apiece, some of which preserve coastal features. The Laurentian Channel is about 290 m deep and about 1,250 km long from the Continental Shelf to the mouth of the Saint Lawrence River. Deep waters with temperatures between 2 and 6.5 °C enter the Gulf at the slope and are slowly advected up the channel by estuariane circulation. Over the 20th century, the waters of the end of the channel have become hypoxic. The gulf has provided an important marine fishery for various First Nations that have lived on its shores for millennia. The first documented voyage by a European in its waters was by the French explorer Jacques Cartier in the year 1534. Cartier named the shores of the Saint Lawrence River The Country of Canadas, after a word meaning village or settlement. At just about the period, Basques came to frequent the area for whale-hunting and trade with the First Nations people of the modern Canadian Atlantic. They left vestiges of their presence in locations of the area—docks, furnaces, graveyards
11.
New Brunswick
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New Brunswick is one of Canadas three Maritime provinces and is the only constitutionally bilingual province. In the Canada 2016 Census, Statistics Canada estimated the population to have been 747,101, down very slightly from 751,171 in 2011. The majority of the population is English-speaking of Anglo and Celtic heritage and it was created as a result of the partitioning of the British colony of Nova Scotia in 1784 and was originally named New Ireland with the capital to be in Saint John. The name was replaced with New Brunswick by King George II. The provincial flag features a ship superimposed on a background with a yellow lion passant guardant on red pennon above it. The province is named for the city of Braunschweig, known in English and Low German as Brunswick, located in modern-day Lower Saxony in northern Germany. The then-colony was named in 1784 to honour the reigning British monarch, George III, the original First Nations inhabitants of New Brunswick were members of three distinct tribes. The largest tribe was the Mikmaq, and they occupied the eastern and they were responsible for the Augustine Mound, a burial ground built about 800 BCE near Metepnákiaq. The western portion of the province was the home of the Wolastoqiyik people. The smaller Passamaquoddy tribe occupied lands in the southwest of the province. The next French contact was in 1604, when a party led by Pierre du Gua de Monts and Samuel de Champlain set up camp for the winter on St. Croix Island, the colony relocated the following year across the Bay of Fundy to Port Royal, Nova Scotia. The whole maritime region was at that time claimed by France and was designated as the colony of Acadia, one of the provisions of the Treaty of Utrecht of 1713 was the surrender of Acadia to Queen Anne. The bulk of the Acadian population thus found themselves residing in the new British colony of Nova Scotia, the remainder of Acadia was only lightly populated and poorly defended. The Maliseet from their headquarters at Meductic on the Saint John River, participated in guerilla raids and battles against New England during Father Rales War. About 1750, to protect his interests in New France, Louis XV caused three forts to be built along the Isthmus of Chignecto and this caused what is known to historians as Father Le Loutres War. During the French and Indian War, the British completed their displacement of the Acadians over all of present-day New Brunswick, Fort Beauséjour, Fort Menagoueche and Fort Gaspareaux were captured by a British force commanded by Lt. Col. Robert Monckton in 1755. Inside Fort Beauséjour, the British forces found not only French regular troops, Governor Charles Lawrence of Nova Scotia used the discovery of Acadian civilians helping in the defence of the fort to order the expulsion of the Acadian population from Nova Scotia. The Acadians of the recently captured Beaubassin and Petitcodiac regions were included in the expulsion order, other actions in the war included British expeditions up the Saint John River in the St. John River Campaign
12.
Chaleur Bay
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Chaleur Bay - also known informally in English as Bay of Chaleur due to the influence of its French translation - is an arm of the Gulf of Saint Lawrence located between Quebec and New Brunswick. The name of the bay is attributed to explorer Jacques Cartier and it translates into English as bay of warmth or bay of torrid weather. Chaleur Bay opens to the east with its southern shore formed by the shore of New Brunswick. The northern shore is formed by the shore of the Gaspé Peninsula. The bay measures approximately 50 km in width at its widest point between Bathurst and New Carlisle, the western end of the bay transitions into the estuary of the Restigouche River at Dalhousie, New Brunswick. The mouth of the bay is delineated by a running from Haut-fond Leander near Grande-Rivière, Quebec in the north. Canadian Hydrographic Service chart number 4486 is the navigational data repository for the area. The shores of Chaleur Bay include numerous beaches, particularly on the southern shore, many rivers also form barachois or barrier beaches. This sand bar is not only because it has fresh water on one side and salt water on the next. Tourism in the region has been driven in the months by users of the bays beaches. The warm ocean currents that enter the bay from the larger Gulf of St. Lawrence result in some of the warmest saltwater on the Atlantic coast north of the state of Virginia. The estuaries of rivers emptying into the bay create a prominent smell of salt water. Patapédia River Chaleur Bay has several islands, although not entirely located within the bay, the northern shores of Miscou Island and Lameque Island form part of the southern shore of the bay. Heron Island lies near Dalhousie, New Brunswick and is located south of Carleton-sur-Mer, the bays shape and the steep cliffs along its northern shore sometimes create particularly windy conditions especially off Nepisiguit Bay. Under the right direction and speed, sea conditions on large areas of the bay can become quite treacherous. Tidal currents are weak, except at the mouths of some rivers. Its configuration tends to channel the wind for two reasons, the cliffs on its North side, and its V shape. This means that in the middle of this section, off Nepisiguit Bay, there is a zone that is particularly windy, tidal currents in this section rarely reach one knot, except at the mouths of some rivers and some channels
13.
Restigouche River
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The Restigouche River is a river that flows across the northwestern part of the province of New Brunswick and the southeastern part of Quebec. The river flows in a direction from its source in the Appalachian Mountains of northwestern New Brunswick to Chaleur Bay. Its meander length is approximately 200 kilometres and this estuary has been designated an Important Bird Area by the Canadian Wildlife Service. The Royal Canadian Navy has named two warships after this river, HMCS Restigouche and HMCS Restigouche, the source of Restigouche River is located at the confluence of the Little Main Restigouche River and Kedgwick River. The name Restigouche may have derived from the Migmaq name Listuguj for the First Nations band that lives in the area around the Restigouche River. Home to the Migmaq Nation for centuries, the Restigouche watershed is a land of many mountains, the Battle of Restigouche was a naval action between British and French forces which was fought on the river in 1760 during the latter stages of the war. Many Scottish families found work in the infancy of the industry and were at the forefront of industrialization of the forests throughout the 19th. The Restigouche River and its tributaries became a highway for log drives, bringing timber to the dozens of sawmills at Campbellton, further industrialization saw pulp and paper mills established in those communities by the 1930s to take advantage of the Restigouche watersheds timber resources. The river is world-renowned for its Atlantic salmon fishing, fly fishing/angling has become a significant source of revenue for many outfitters in the region and a 55-kilometre of the Restigouche has been designated part of the Canadian Heritage Rivers System. According to Restigouche Lodge between 15,000 and 25,000 salmon enter the Restigouche each year, which attracts anglers from all over the world. While many Atlantic salmon are reluctant to strike, the Restigouche variety are aggressive, the Restigouche River is known for its exclusivity, clear water and large Atlantic salmon. Fish over 40 pounds pounds are landed somewhere on the Restigouche every year, early spring through the end of June is the best time for catching these salmon. For more than 100 years, the worlds wealthiest people have come to enjoy the tranquil beauty. Many private fishing lodges have been established on the Restigouche which are owned and operated by major corporations, such leases are time-limited and, for the best fishing pools, can reportedly run into the millions of dollars for fishing rights lasting for only a few years. This is largely due to the proximity of the river to Boston, New York and Philadelphia. The designation of a 55-kilometre stretch of the Upper Restigouche as a Heritage River in 1998 was not the first attempt to preserve this area. Early issues with over-fishing by new arrivals to the area led to the implementation, in 1824 and this culminated in the implementation of the Fisheries Act in 1858 and opened the door for private hunting and fishing clubs by granting them fishing leases …. The efforts of conservationists continue today with groups such as the Canadian Parks and this group claims that only 1 percent of the Restigouche watershed is protected from development
14.
Mi'kmaq language
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The Mikmaq language is an Eastern Algonquian language spoken by nearly 11,000 Mikmaq in Canada and the United States out of a total ethnic Mikmaq population of roughly 20,000. The word Mikmaq is a word meaning my friends, the adjectival form is Míkmaw. The languages native name is Lnuismk, Míkmawísimk or Míkmwei, the phonemic inventory of Mikmaq is shown below. The consonants of Mikmaq can be divided into two groups, the obstruents /p, t, k, kʷ, t͡ʃ, s, x, xʷ/, the vowels of Mikmaq are also counted as sonorants. The obstruents have a variety of pronunciations. When they are located word-initially or next to another obstruent, they are voiceless, however, when they are located between sonorants, they are voiced, and appear as. When the stops and affricate are located word-finally, they may be aspirated, an example of each kind of pronunciation is given below. Mikmaq distinguishes between long and short vowels and consonants, symbolized in Listuguj by doubling the consonant. Beyond expanding in length, long consonants add a schwa when they precede other consonants, Listuguj orthography occasionally begins words with consonant clusters, such as with gtan or mgumi. However, such clusters are pronounced over separate syllables, with a preceding the cluster, for instance, gtan is pronounced /ək. ta. On the other hand, word-final clusters, such as in asigetg are pronounced over a single syllable, compare the pronunciation of asigetg, /a. si. getk/, with mestg, /mes. tək/. Mikmaq uses free word order, based on rather than a traditionally fixed order of subjects, objects. While it is difficult to classify Mikmaq under traditional word-order categories such as SVO or SOV. However, these elements of verbs are paired with markers that can appear throughout the word, depending again on emphasis. In short, while a few aspects of Mikmaq can be predicted, its syntax in general is largely free. Mikmaq is written using a number of Latin alphabets based on ones devised by missionaries in the 19th century, previously, the language was written in Mikmaq hieroglyphic writing, a script of partially native origin. The Francis-Smith orthography used here was developed in 1974, and adopted as the orthography of the Míkmaq Nation in 1980. It is the most widely used orthography, used by Nova Scotian Mikmaq and it is quite similar to the Lexicon orthography, differing from it only in its use of the straight apostrophe ⟨⟩ or acute accent ⟨´⟩ instead of the colon ⟨, ⟩ to mark vowel length
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Belgium
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Belgium, officially the Kingdom of Belgium, is a sovereign state in Western Europe bordered by France, the Netherlands, Germany, Luxembourg, and the North Sea. It is a small, densely populated country which covers an area of 30,528 square kilometres and has a population of about 11 million people. Additionally, there is a group of German-speakers who live in the East Cantons located around the High Fens area. Historically, Belgium, the Netherlands and Luxembourg were known as the Low Countries, the region was called Belgica in Latin, after the Roman province of Gallia Belgica. From the end of the Middle Ages until the 17th century, today, Belgium is a federal constitutional monarchy with a parliamentary system of governance. It is divided into three regions and three communities, that exist next to each other and its two largest regions are the Dutch-speaking region of Flanders in the north and the French-speaking southern region of Wallonia. The Brussels-Capital Region is a bilingual enclave within the Flemish Region. A German-speaking Community exists in eastern Wallonia, Belgiums linguistic diversity and related political conflicts are reflected in its political history and complex system of governance, made up of six different governments. Upon its independence, declared in 1830, Belgium participated in the Industrial Revolution and, during the course of the 20th century, possessed a number of colonies in Africa. This continuing antagonism has led to several far-reaching reforms, resulting in a transition from a unitary to a federal arrangement during the period from 1970 to 1993. Belgium is also a member of the Eurozone, NATO, OECD and WTO. Its capital, Brussels, hosts several of the EUs official seats as well as the headquarters of major international organizations such as NATO. Belgium is also a part of the Schengen Area, Belgium is a developed country, with an advanced high-income economy and is categorized as very high in the Human Development Index. A gradual immigration by Germanic Frankish tribes during the 5th century brought the area under the rule of the Merovingian kings, a gradual shift of power during the 8th century led the kingdom of the Franks to evolve into the Carolingian Empire. Many of these fiefdoms were united in the Burgundian Netherlands of the 14th and 15th centuries, the Eighty Years War divided the Low Countries into the northern United Provinces and the Southern Netherlands. The latter were ruled successively by the Spanish and the Austrian Habsburgs and this was the theatre of most Franco-Spanish and Franco-Austrian wars during the 17th and 18th centuries. The reunification of the Low Countries as the United Kingdom of the Netherlands occurred at the dissolution of the First French Empire in 1815, although the franchise was initially restricted, universal suffrage for men was introduced after the general strike of 1893 and for women in 1949. The main political parties of the 19th century were the Catholic Party, French was originally the single official language adopted by the nobility and the bourgeoisie
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Census
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A census is the procedure of systematically acquiring and recording information about the members of a given population. It is a regularly occurring and official count of a particular population, the term is used mostly in connection with national population and housing censuses, other common censuses include agriculture, business, and traffic censuses. United Nations recommendations also cover census topics to be collected, official definitions, classifications, the word is of Latin origin, during the Roman Republic, the census was a list that kept track of all adult males fit for military service. Current administrative data systems allow for other approaches to enumeration with the level of detail but raise concerns about privacy. A census can be contrasted with sampling in which information is obtained only from a subset of a population, typically main population estimates are updated by such intercensal estimates. Modern census data are used for research, business marketing, and planning. Census counts are necessary to adjust samples to be representative of a population by weighting them as is common in opinion polling, similarly, stratification requires knowledge of the relative sizes of different population strata which can be derived from census enumerations. In some countries, the census provides the official used to apportion the number of elected representatives to regions. In many cases, a carefully chosen random sample can provide accurate information than attempts to get a population census. A census is often construed as the opposite of a sample as its intent is to count everyone in a rather than a fraction. However, population censuses rely on a frame to count the population. This is the way to be sure that everyone has been included as otherwise those not responding would not be followed up on. The fundamental premise of a census is that the population is not known, the use of a sampling frame is counterintuitive as it suggests that the population size is already known. However, a census is also used to collect data on the individuals in the nation. This process of sampling marks the difference between historical census, which was a house to house process or the product of a decree. The sampling frame used by census is almost always an address register, thus it is not known if there is anyone resident or how many people there are in each household. Depending on the mode of enumeration, a form is sent to the householder, as a preliminary to the dispatch of forms, census workers will check any address problems on the ground. While it may seem straightforward to use the postal service file for this purpose, a particular problem is what are termed communal establishments which category includes student residences, religious orders, homes for the elderly, people in prisons etc
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Channel Islands
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The Channel Islands are an archipelago in the English Channel, off the French coast of Normandy. They are considered the remnants of the Duchy of Normandy, and although they are not part of the United Kingdom, it is responsible for the defence, the Crown dependencies are not members of the Commonwealth of Nations nor of the European Union. They have a population of about 168,000. The total area of the islands is 198 km2, the two bailiwicks have been administered separately since the late 13th century, each has its own independent laws, elections, and representative bodies. Any institution common to both is the rather than the rule. The Bailiwick of Guernsey is divided into three jurisdictions – Guernsey, Alderney and Sark – each with its own legislature, the term Channel Islands began to be used around 1830, possibly first by the Royal Navy as a collective name for the islands. The permanently inhabited islands of the Channel Islands are, Jersey Guernsey Alderney Sark Herm Jethou Brecqhou There are also several uninhabited islets and they are an incorporated part of the commune of Granville. While they are popular with visitors from France, Channel Islanders rarely visit them as there are no transport links from the other islands. Chausey is referred to as an Île normande, Îles Normandes and Archipel Normand have also, historically, been used in Channel Island French to refer to the islands as a whole. The lowest point is the Atlantic Ocean, the earliest evidence of human occupation of the Channel Islands has been dated to 250,000 years ago when they were attached to the landmass of continental Europe. The islands became detached by rising sea levels in the Neolithic period, hoards of Armorican coins have been excavated, providing evidence of trade and contact in the Iron Age period. Evidence for Roman settlement is sparse, although evidently the islands were visited by Roman officials, the Roman name for the Channel Islands was I. Lenuri and is included in the Peutinger Table The traditional Latin names used for the islands derive from the Antonine Itinerary, gallo-Roman culture was adopted to an unknown extent in the islands. In the sixth century, Christian missionaries visited the islands, samson of Dol, Helier, Marculf and Magloire are among saints associated with the islands. In the sixth century, they were included in the diocese of Coutances where they remained until reformation. The islands were inhabited by Britons, who also inhabited Wales, south west England, from the beginning of the ninth century, Norse raiders appeared on the coasts. Norse settlement succeeded initial attacks, and it is from this period that many names of Norse origin appear. In 933, the islands were granted to William I Longsword by Raoul King of Western Francia, in 1066, William II of Normandy invaded and conquered England, becoming William I of England, also known as William the Conqueror
18.
Cliffed coast
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A cliffed coast, also called an abrasion coast, is a form of coast where the action of marine waves has formed steep cliffs that may or may not be precipitous. It contrasts with a flat or alluvial coast, the slope is constantly being eroded. The waves attacking the cliff-foot form a notch by constant abrasion action producing an overhang. This overhang grows in size as the cliff is undercut, until it collapses under its own weight, the loose debris that has broken off is gradually carried away from the area in front of the cliff by the action of the sea. As the coastal cliffs collapse, the shoreline recedes inland, the speed at which this happens depends, in particular, on the strength of the surf, the height of the cliff, the frequency of storm surges and the hardness of the bedrock. Thus, the Mecklenburg coast in Germany recedes by about 25 centimetres per year, whereas the chalk cliffs of southern England retreat by just ½ a centimetre each year. A cliffed coast is made of a loose material, such as at the Red Cliff on the German island of Sylt. There are, however, differences between the former and the latter regarding some peculiarities of the coast line and it represents the foot of the cliff preserved at and below the level of water table. On a cliffed coast made up of material which is only fairly or even hardly resistant to erosion no wave-cut platform, if waves carve notches at a narrow point on both sides of a promontory on the rocky cliffed coast, a natural arch may be formed. When the arch collapses as the coastline recedes further a stack is left behind on the wave-cut platform, the best-known example in Germany is the Lange Anna on Heligoland. Furthermore, on a rocky cliffed coast wave action is not the driving force for coastline retreat. General weathering of the bedrock is almost equally important, living cliffs are those on a coast that is still active, i. e. that is being eroded and is receding. A dead cliff, by contrast, is reached by very high marine waves and is therefore subjected to very little change. A clear indication of a lack of activity at a cliff is a covering of vegetation that appears on the cliff as wave action against it subsides. Well-known coasts with living cliffs in Germany are the Red Cliff in Kampen on the island of Sylt or the cliffs on the Jasmund Peninsula. The Königsstuhl on the island of Rügen is an example of a dead cliff. Others may be found in the regions of the present-day Wadden Sea coast of the North Sea a few kilometres inland and these show the former coastline from which the sea retreated as the level of water in the North Sea fell. Steep sea cliffs can also be caused by catastrophic debris avalanches and these have been common on the submerged flanks of ocean island volcanos such as the Hawaiian Islands and the Cape Verde Islands
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Natural arch
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A natural arch, natural bridge or, less commonly, a rock arch is a natural rock formation where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on sides of the formation beneath the relatively harder stratum, or caprock. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, the choice between bridge and arch is somewhat arbitrary. The Natural Arch and Bridge Society identifies a bridge as a subtype of arch that is primarily water-formed, by contrast, the Dictionary of Geological Terms defines a natural bridge as a natural arch that spans a valley of erosion. The largest natural arch, by a significant margin, is the Xianren Bridge in China, on coasts two different types of arches can form depending on the geology. On discordant coastlines rock types run at 90° to the coast, wave refraction concentrates the wave energy on the headland, and an arch forms when caves break through the headland. Two examples of type of arch are London Arch—previously known as London Bridge—in Victoria, Australia. When these arches eventually collapse, they form stacks and stumps, on concordant coastlines rock types run parallel to the coastline, with weak rock such as shale protected by stronger rock such as limestone. The wave action along concordant coastlines breaks through the strong rock, good examples of this type of arch are the Durdle Door and Stair Hole near Lulworth Cove on Dorsets Jurassic Coast in south England. When Stair Hole eventually collapses it will form a cove, weather-eroded arches begin their formation as deep cracks which penetrate into a sandstone layer. Erosion occurring within the cracks wears away exposed rock layers and enlarges the surface cracks isolating narrow sandstone walls which are called fins, alternating frosts and thawing cause crumbling and flaking of the porous sandstone and eventually cut through some of the fins. The resulting holes become enlarged to arch proportions by rockfalls and weathering, the arches eventually collapse leaving only buttresses that in time will erode. Many weather-eroded arches are found in Arches National Park, Canyonlands National Park, some natural bridges may look like arches, but they form in the path of streams that wear away and penetrate the rock. Pothole arches form by chemical weathering as water collects in natural depressions, Natural Bridges National Monument in Utah protects the area surrounding three large natural bridges all of which were formed by streams running through canyons. The largest of which is named Sipapu Bridge with a span of 225 feet, Natural bridges can form from natural limestone caves, where paired sinkholes collapse and a ridge of stone is left standing in between, with the cave passageway connecting from sinkhole to sinkhole. Like all rock formations, natural bridges are subject to continued erosion, one example of this was the double-arched Victorian coastal rock formation, London Bridge, which lost an arch after storms increased erosion
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Appalachian Mountains
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The Appalachian Mountains, often called the Appalachians, are a system of mountains in eastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period and it once reached elevations similar to those of the Alps and the Rocky Mountains before naturally occurring erosion. The Appalachian chain is a barrier to east-west travel, as it forms a series of alternating ridgelines, definitions vary on the precise boundaries of the Appalachians. A common variant definition does not include the Adirondack Mountains, which belong to the Grenville Orogeny and have a different geological history from the rest of the Appalachians. The range covers parts of the islands of Saint Pierre and Miquelon, the system is divided into a series of ranges, with the individual mountains averaging around 3,000 ft. The highest of the group is Mount Mitchell in North Carolina at 6,684 feet, the term Appalachian refers to several different regions associated with the mountain range. Most broadly, it refers to the mountain range with its surrounding hills. The Ouachita Mountains in Arkansas and Oklahoma were originally part of the Appalachians as well, the name was soon altered by the Spanish to Apalachee and used as a name for the tribe and region spreading well inland to the north. Pánfilo de Narváezs expedition first entered Apalachee territory on June 15,1528, now spelled Appalachian, it is the fourth-oldest surviving European place-name in the US. After the de Soto expedition in 1540, Spanish cartographers began to apply the name of the tribe to the mountains themselves. The first cartographic appearance of Apalchen is on Diego Gutierrezs map of 1562, the name was not commonly used for the whole mountain range until the late 19th century. A competing and often more popular name was the Allegheny Mountains, Alleghenies, in the early 19th century, Washington Irving proposed renaming the United States either Appalachia or Alleghania. In U. S. dialects in the regions of the Appalachians. In northern parts of the range, it is pronounced /ˌæpəˈleɪtʃᵻnz/ or /ˌæpəˈleɪʃᵻnz/, the third syllable is like lay. There is often debate between the residents of the regions as to which pronunciation is the more correct one. Elsewhere, a commonly accepted pronunciation for the adjective Appalachian is /ˌæpəˈlætʃiən/, the whole system may be divided into three great sections, Northern, The northern section runs from the Canadian province of Newfoundland and Labrador to the Hudson River. The Monteregian Hills, which cross the Green Mountains in Quebec, are also unassociated with the Appalachians, Central, The central section goes from the Hudson Valley to the New River running through Virginia and West Virginia. Southern, The southern section runs from the New River onwards and it consists of the prolongation of the Blue Ridge, which is divided into the Western Blue Ridge Front and the Eastern Blue Ridge Front, the Ridge-and-Valley Appalachians, and the Cumberland Plateau
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Chic-Choc Mountains
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The Chic-Choc Mountains, also spelled Shick Shocks, is a mountain range in the central region of the Gaspé Peninsula in Quebec, Canada. It is a part of the Notre Dame Mountains, which is a continuation of the Appalachian Mountains, the name Chic-Chocs comes from the Mikmaq word sigsôg, meaning crags or rocky mountains. It has undergone many different spellings over time, including Chikchâks, Shick-shock, the Chic-Chocs run parallel to the St. Lawrence River and are located some 20 to 40 kilometers inland. They are a band of mountains approximately 95 kilometres long and 10 kilometres wide. The Chic-Chocs are heavily eroded, with rounded, flattened tops, over 25 mountains in the range have peaks higher than 1,000 metres, the highest is Mont Jacques-Cartier at 1,268 metres. Caribou can be found in the plateaus of this region, although visited by just a few tourists, Chic-Choc Mountains became much more popular in the late 1990s as backcountry skiing gained popularity in Eastern Canada. A network of trails, including the International Appalachian Trail, passes through these mountains, quebecs Parc national de la Gaspésie protects most of the mountain range. Brennan Landscape Paintings of the Chic-Choc Mountains
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Mount Albert (Quebec)
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Mont Albert is a mountain in the Chic-Choc range in the Gaspésie National Park in the Gaspé Peninsula of eastern Quebec, Canada. At 1,151 m, it is one of the highest mountains in southern Quebec, the summit of Mount Albert is a plateau 13 km across called La Table à Moïse, or Mosess Table. It includes two summits, Albert North and Albert South, each of the summits is situated at either side of the plateau
23.
Alpine tundra
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Alpine tundra is a type of natural region or biome that does not contain trees because it is at high altitude. The high altitude causes an adverse climate, which is too cold, Alpine tundra transitions to sub-alpine forests below the tree line, stunted forests occurring at the forest-tundra ecotone are known as Krummholz. With increasing elevation it ends at the line where snow. Alpine tundra occurs in mountains worldwide, the flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the tundra is caused by the lack of greenhouse effect at high altitude. Alpine tundra occurs at high altitude at any latitude. Portions of Montane grasslands and shrublands ecoregions worldwide include alpine tundra, Alpine tundra occupies high-mountain summits, slopes, and ridges above timberline. Aspect plays a role as well, the treeline often occurs at higher elevations on warmer equator-facing slopes, with limited access to infrastructure, only a handful of human communities exist in alpine zones. Many are small and have heavily specialized economies, often relying on such as agriculture, mining. An example of such a town is La Rinconada, Peru, a gold-mining town. A counterexample is El Alto, Bolivia, at 4,150 metres, which has a diverse service and manufacturing economy. Alpine climate is the weather for the alpine tundra. The climate becomes colder at high elevations—this characteristic is described by the rate of air, air tends to get colder as it rises. The dry adiabatic lapse rate is 10 °C per km of elevation or altitude, therefore, moving up 100 metres on a mountain is roughly equivalent to moving 80 kilometers towards the pole. This relationship is only approximate, however, since local factors such as proximity to oceans can drastically modify the climate, typical high-elevation growing seasons range from 45 to 90 days, with average summer temperatures near 10 °C. Growing season temperatures frequently fall below freezing, and frost occurs throughout the season in many areas. Precipitation occurs mainly as snow, but soil water availability is highly variable with season, location. For example, snowfields commonly accumulate on the lee sides of ridges while ridgelines may remain nearly snow free due to redistribution by wind, some alpine habitats may be up to 70% snow free in winter
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Tree line
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The tree line is the edge of the habitat at which trees are capable of growing. It is found at high elevations and in frigid environments, beyond the tree line, trees cannot tolerate the environmental conditions. The tree line should not be confused with a lower timberline or forest line, at the tree line, tree growth is often sparse and stunted, with the last trees forming densely matted bushes, known as krummholz. The tree line, like other natural lines, appears well-defined from a distance. Trees grow shorter towards the inhospitable climate until they stop growing. The climate above the line of mountains is called an alpine climate. In the northern hemisphere treelines on north-facing slopes are lower than on south-facing slopes because the increased shade on north-facing slopes means the snowpack takes longer to melt and this shortens the growing season for trees. In the southern hemisphere, the slopes have the shorter growing season. The alpine tree line boundary is seldom abrupt, it forms a transition zone between closed forest below and treeless alpine tundra above. Environmentally dwarfed shrubs commonly forms the upper limit, the decrease in air temperature due to increasing elevation causes the alpine climate. Skin effects and topography can create microclimates that alter the general cooling trend, however, the number of degree days calculated from leaf temperatures may be very similar in the two kinds of timberlines. A series of warm summers in the 1940s seems to have permitted the establishment of “significant numbers” of spruce seedlings above the treeline in the hills near Fairbanks. Survival depends on a sufficiency of new growth to support the tree, the windiness of high-elevation sites is also a potent determinant of the distribution of tree growth. However, snow accumulation in sheltered gullies in the Selkirk Mountains of southeastern British Columbia causes timberline to be 400 metres lower than on exposed intervening shoulders. In a desert, the line marks the driest places where trees can grow. These tend to be called the tree line and occur below about 5,000 ft elevation in the Desert Southwestern United States. In some mountainous areas, higher elevations above the line or on equator-facing and leeward slopes can result in low rainfall. This dries out the soil, resulting in an arid environment unsuitable for trees
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Serpentine subgroup
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The serpentine subgroup are greenish, brownish, or spotted minerals commonly found in serpentinite rocks. They are used as a source of magnesium and asbestos, the name is thought to come from the greenish color being that of a serpent. In mineralogy and gemology, serpentine may refer to any of 20 varieties belonging to the serpentine group, owing to admixture, these varieties are not always easy to individualize, and distinctions are not usually made. There are three important mineral polymorphs of serpentine, antigorite, chrysotile and lizardite, the serpentine group of minerals are polymorphous, meaning that they have the same chemical formulae, but the atoms are arranged into different structures, or crystal lattices. Chrysotile, which has a habit, is one polymorph of serpentine and is an important component of asbestos. Other polymorphs in the group may have a platy habit. Antigorite and lizardite are the polymorphs with platy habit, many types of serpentine have been used for jewellery and hardstone carving, sometimes under the name false jade or Teton jade. Their olive green colour and smooth or scaly appearance is the basis of the name from the Latin serpentinus, meaning serpent rock and they have their origins in metamorphic alterations of peridotite and pyroxene. Serpentines may also pseudomorphously replace other magnesium silicates, alterations may be incomplete, causing physical properties of serpentines to vary widely. Where they form a significant part of the surface, the soil is unusually high in clay. Antigorite is the polymorph of serpentine that most commonly forms during metamorphism of wet ultramafic rocks and is stable at the highest temperatures—to over 600 °C at depths of 60 km or so. In contrast, lizardite and chrysotile typically form near the Earths surface and break down at low temperatures. It has been suggested that chrysotile is never stable relative to either of the other two serpentine polymorphs, samples of the oceanic crust and uppermost mantle from ocean basins document that ultramafic rocks there commonly contain abundant serpentine. Antigorite contains water in its structure, about 13 percent by weight, the flora is generally very distinctive, with specialised, slow-growing species. Areas of serpentine-derived soil will show as strips of shrubland and open, scattered small trees within otherwise forested areas, most serpentines are opaque to translucent, light, soft, infusible and susceptible to acids. All are microcrystalline and massive in habit, never being found as single crystals, lustre may be vitreous, greasy or silky. Colours range from white to grey, yellow to green, and brown to black, many are intergrown with other minerals, such as calcite and dolomite. Occurrence is worldwide, New Caledonia, Canada, US, Afghanistan, Britain, Greece, China, Ural Mountains, France, Korea, Austria, India, Myanmar, New Zealand, Norway and Italy are notable localities
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Flora
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Flora is the plant life occurring in a particular region or time, generally the naturally occurring or indigenous—native plant life. The corresponding term for animal life is fauna, Flora, fauna and other forms of life such as fungi are collectively referred to as biota. Sometimes bacteria and fungi are also referred to as flora, as in the gut flora or skin flora. The word flora comes from the Latin name of Flora, the goddess of plants, flowers, the distinction between vegetation and flora was first made by Jules Thurmann. Prior to this, the two terms were used indiscriminately, plants are grouped into floras based on region, period, special environment, or climate. Regions can be geographically distinct habitats like mountain vs. flatland, floras can mean plant life of a historic era as in fossil flora. Lastly, floras may be subdivided by special environments, Native flora, the native and indigenous flora of an area. The plants that are grown by humans. Traditionally this classification was applied to plants regarded as undesirable, many native plants previously considered weeds have been shown to be beneficial or even necessary to various ecosystems. The flora of an area or time period can be documented in a publication also known as a flora. Floras may require specialist botanical knowledge to use with any effectiveness, traditionally they are books, but some are now published on CD-ROM or websites. It is said that the Flora Sinensis by the Polish Jesuit Michał Boym was the first book that used the name Flora in this meaning, however, despite its title it covered not only plants, but also some animals of the region. A published flora often contains diagnostic keys, often these are dichotomous keys, which require the user to repeatedly examine a plant, and decide which one of two alternatives given best applies to the plant
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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
28.
Murdochville, Quebec
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Murdochville is a town located in Quebec, Canada, one of only a few inland communities on the Gaspé Peninsula. Murdochville is located along Quebec Route 198 in the township of Holland,40 kilometres south of LAnse-Pleureuse and 93 kilometres west of Gaspé. It is 535 metres above sea level and surrounded by high mountains, in 1921, copper ore was discovered in the area by the Miller brothers, Alfred, Sydney, Frederick, Angus and Theophilus. However, it was not until 1950 that Noranda Mines actually began mining, the mining town was set up and named after James Y. Murdoch, owner of the mine and first president of Noranda, in 1953, the town was incorporated. The mining operation in the town was large, starting with mining the raw ore. In the 1970s, the operation in Murdochville was large enough to support a population of 5,000 inhabitants. A number of large battles in Murdochville also helped lay the groundwork for ideas that still exist today. Workers in Murdochville fought for their rights in 1957, which led to the adoption of new laws protecting the rights of unionized workers in Quebec. In 1987, the mine was destroyed by an underground fire. The mine closed in 1999, leaving the town to fight for survival, after several close calls, the small town has decided to fight back, in an effort to reverse the economic uncertainty that has befallen the town. This has included the creation of large wind turbine projects, along with the diversification of the local economy. Murdochville lies between the subarctic and the cold humid continental climates. Summers are relatively cool and short, whereas winters are long, the brief summers are, however, mild enough to keep September right on the edge of the 10 °C isotherm for humid continental. The high amount of precipitation and snowfall would also be very unusual for subarctic climates, list of cities in Quebec Town of Murdochville Tourist Information about Murdochville CBC Radio Story, No Company Town, The Story of Murdochville
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Wind turbine
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A wind turbine is a device that converts the winds kinetic energy into electrical power. Wind turbines are manufactured in a range of vertical and horizontal axis types. The smallest turbines are used for such as battery charging for auxiliary power for boats or caravans or to power traffic warning signs. Slightly larger turbines can be used for making contributions to a power supply while selling unused power back to the utility supplier via the electrical grid. Wind turbines were used in Persia about 500–900 A. D, the windwheel of Hero of Alexandria marks one of the first known instances of wind powering a machine in history. However, the first known practical wind turbines were built in Sistan and these Panemone were vertical axle wind turbines, which had long vertical drive shafts with rectangular blades. Made of six to twelve sails covered in reed matting or cloth material, these turbines were used to grind grain or draw up water. Wind turbines first appeared in Europe during the Middle Ages, the first historical records of their use in England date to the 11th or 12th centuries and there are reports of German crusaders taking their windmill-making skills to Syria around 1190. By the 14th century, Dutch wind turbines were in use to areas of the Rhine delta. Advanced wind mills were described by Croatian inventor Fausto Veranzio, in his book Machinae Novae he described vertical axis wind turbines with curved or V-shaped blades. The first electricity-generating wind turbine was a battery charging machine installed in July 1887 by Scottish academic James Blyth to light his home in Marykirk. Some months later American inventor Charles F, although Blyths turbine was considered uneconomical in the United Kingdom electricity generation by wind turbines was more cost effective in countries with widely scattered populations. In Denmark by 1900, there were about 2500 windmills for mechanical loads such as pumps and mills, the largest machines were on 24-meter towers with four-bladed 23-meter diameter rotors. By 1908 there were 72 wind-driven electric generators operating in the United States from 5 kW to 25 kW, around the time of World War I, American windmill makers were producing 100,000 farm windmills each year, mostly for water-pumping. By the 1930s, wind generators for electricity were common on farms, in this period, high-tensile steel was cheap, and the generators were placed atop prefabricated open steel lattice towers. A forerunner of modern wind generators was in service at Yalta. This was a 100 kW generator on a 30-meter tower, connected to the local 6.3 kV distribution system and it was reported to have an annual capacity factor of 32 percent, not much different from current wind machines. In the autumn of 1941, the first megawatt-class wind turbine was synchronized to a utility grid in Vermont, the Smith-Putnam wind turbine only ran for 1,100 hours before suffering a critical failure
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Acadia
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Acadia was a colony of New France in northeastern North America that included parts of eastern Quebec, the Maritime provinces, and modern-day Maine to the Kennebec River. During much of the 17th and early 18th centuries, Norridgewock on the Kennebec River, the actual specification by the French government for the territory refers to lands bordering the Atlantic coast, roughly between the 40th and 46th parallels. Later, the territory was divided into the British colonies which became Canadian provinces, the population of Acadia included members of the Wabanaki Confederacy and descendants of emigrants from France. The two communities intermarried, which resulted in a significant portion of the population of Acadia being Métis, the first capital of Acadia, established in 1605, was Port-Royal. Over seventy-four years there were six colonial wars, in which English, during these wars, along with some French troops from Quebec, some Acadians, the Wabanaki Confederacy, and French priests continuously raided New England settlements along the border in Maine. While Acadia was officially conquered in 1710 during Queen Annes War, present-day New Brunswick, present-day Prince Edward Island and Cape Breton as agreed under Article XIII of the Treaty of Utrecht remained under French control. By militarily defeating the Wabanaki Confederacy and the French priests, present-day Maine fell during Father Rales War, during King Georges War, France and New France made significant attempts to regain mainland Nova Scotia. After Father Le Loutres War, present-day New Brunswick fell to the British, finally, during the French and Indian War, both Île Royale and Île Saint-Jean fell to the British in 1758. Today, the term Acadia is used to refer to regions of North America that are associated with the lands, descendants. It can also be used to refer to the Acadian diaspora in southern Louisiana, in the abstract, Acadia refers to the existence of a French culture in any of these regions. People living in Acadia, and sometimes former residents and their descendants, are called Acadians, Arcadia derives from the Arcadia district in Greece which since Classical antiquity had the extended meanings of refuge or idyllic place. In 1603 a colony south of the St. Lawrence between the 40th and 46th parallels was agreed by Henry IV, who recognised the territory as La Cadie, also in the 17th century Champlain fixed its present orthography with the r omitted. William Francis Ganong, a cartographer, has shown its gradual progress northeastwards, in a succession of maps, another interesting note is the similarity in the pronunciation of Acadie and the Míkmawísimk suffix -akadie, which means a place of abundance. The modern usage is seen in place names such as Shunacadie or Shubenacadie. It is thought that intercultural conversation between early French traders and Mikmaq hunters may have resulted in the name lArcadie being changed to lAcadie, the history of Acadia was significantly influenced by the warfare that took place on its soil during the 17th and 18th century. Prior to that period, the Mi’kmaq lived in Acadia for centuries. The French arrived in 1604, and Catholic Mi’kmaq and Acadians were the predominant populations in the colony for the next 150 years. Early European colonists, who would become known as Acadians, were French subjects primarily from the Pleumartin to Poitiers in the Vienne département of west-central France
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Overfishing
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Overfishing is a form of overexploitation where fish stocks are reduced to below acceptable levels. Overfishing can occur in bodies of any sizes, such as ponds, rivers, lakes or oceans. Sustained overfishing can lead to critical depensation, where the population is no longer able to sustain itself. Some forms of overfishing, for example the overfishing of sharks, has led to the upset of entire marine ecosystems, the ability of a fishery to recover from overfishing depends on whether the ecosystems conditions are suitable for the recovery. For example, once trout have been overfished, carp might take over in a way makes it impossible for the trout to re-establish a breeding population. Overfishing occurs when fish are caught than the population can replace through natural reproduction. Gathering as many fish as possible may seem like a profitable practice, the results not only affect the balance of life in the oceans, but also the social and economic well-being of the coastal communities who depend on fish for their way of life. Overfishing has significantly affected many fisheries around the world, as much as 85% of the worlds fisheries may be over-exploited, depleted, fully exploited or in recovery from exploitation. Significant overfishing has been observed in pre-industrial times, in particular, the overfishing of the western Atlantic Ocean from the earliest days of European colonisation of the Americas has been well documented. Following World War Two, industrial fishing rapidly expanded with rapid increases in worldwide fishing catches, however, many fisheries have either collapsed or degraded to a point where increased catches are no longer possible. Daniel Pauly, a fisheries scientist known for pioneering work on the impacts on global fisheries, has commented. We are gradually winning this war to exterminate them, and to see this destruction happen, for nothing really – for no reason – that is a bit frustrating. Examples of overfishing exist in such as the North Sea, the Grand Banks of Newfoundland. In these locations, overfishing has not only proved disastrous to fish stocks, the Peruvian coastal anchovy fisheries crashed in the 1970s after overfishing and an El Niño season largely depleted anchovies from its waters. Anchovies were a natural resource in Peru, indeed,1971 alone yielded 10.2 million metric tons of anchovies. However, the five years saw the Peruvian fleets catch amount to only about 4 million tons. This was a loss to Perus economy. The collapse of the cod fishery off Newfoundland, and the 1992 decision by Canada to impose a moratorium on the Grand Banks, is a dramatic example of the consequences of overfishing
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Overexploitation
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Overexploitation, also called overharvesting, refers to harvesting a renewable resource to the point of diminishing returns. Sustained overexploitation can lead to the destruction of the resource, the term applies to natural resources such as, wild medicinal plants, grazing pastures, game animals, fish stocks, forests, and water aquifers. In ecology, overexploitation describes one of the five main activities threatening global biodiversity, ecologists use the term to describe populations that are harvested at a rate that is unsustainable, given their natural rates of mortality and capacities for reproduction. This can result in extinction at the level and even extinction of whole species. The term is used and defined somewhat differently in fisheries, hydrology. Overexploitation can lead to destruction, including extinctions. However it is possible for overexploitation to be sustainable, as discussed below in the section on fisheries. Overexploitation is not an activity limited to humans, introduced predators and herbivores, for example, can overexploit native flora and fauna. Concern about overexploitation is relatively recent, though overexploitation itself is not a new phenomenon and it has been observed for millennia. For example, ceremonial cloaks worn by the Hawaiian kings were made from the mamo bird, the dodo, a flightless bird from Mauritius, is another well-known example of overexploitation. As with many species, it was naive about certain predators, allowing humans to approach. From the earliest of times, hunting has been an important human activity as a means of survival, there is a whole history of overexploitation in the form of overhunting. The overkill hypothesis explains why the megafaunal extinctions occurred within a short period of time. This can be traced with human migration, the most convincing evidence of this theory is that 80% of the North American large mammal species disappeared within 1000 years of the arrival of humans on the western hemisphere continents. A second wave of extinctions occurred later with European settlement, overexploitation doesnt necessarily lead to the destruction of the resource, nor is it necessarily unsustainable. However, depleting the numbers or amount of the resource can change its quality, for example, footstool palm is a wild palm tree found in Southeast Asia. Its leaves are used for thatching and food wrapping, and overharvesting has resulted in its leaf size becoming smaller, the tragedy of the commons refers to a dilemma described in an article by that name written by Garrett Hardin and first published in the journal Science in 1968. Central to Hardins essay is an example which is a parable for understanding how overexploitation can occur
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Tourism
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Tourism is travel for pleasure or business, also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. Tourism may be international, or within the travellers country, Tourism can be domestic or international, and international tourism has both incoming and outgoing implications on a countrys balance of payments. Today, tourism is a source of income for many countries. International tourism receipts grew to US$1.03 trillion in 2011, the ITB Berlin is the worlds leading tourism trade fair. The word tourist was used by 1772 and tourism by 1811. It is formed from the tour, which is derived from Old English turian, from Old French torner, from Latin tornare, to turn on a lathe. Tourism is an important, even vital, source of income for many regions and it also creates opportunities for employment in the service sector of the economy associated with tourism. This is in addition to goods bought by tourists, including souvenirs, in 1936, the League of Nations defined a foreign tourist as someone traveling abroad for at least twenty-four hours. Its successor, the United Nations, amended this definition in 1945 and it includes movements for all purposes. In 1981, the International Association of Scientific Experts in Tourism defined tourism in terms of particular activities chosen and undertaken outside the home, in this context, travel has a similar definition to tourism, but implies a more purposeful journey. The terms tourism and tourist are sometimes used pejoratively, to imply a shallow interest in the cultures or locations visited, by contrast, traveler is often used as a sign of distinction. The sociology of tourism has studied the values underpinning these distinctions. International tourist arrivals reached 1.035 billion in 2012, up from over 996 million in 2011, the World Tourism Organization reports the following ten destinations as the most visited in terms of the number of international travellers in 2016. International tourism receipts grew to US$1.2 trillion in 2014, based upon air traffic, the MasterCard Global Destination Cities Index reports the following cities as the top ten most popular destinations of international tourism worldwide. MasterCard reports the following cities as the top ten biggest earners on international tourism worldwide in 2015, as early as Shulgi, however, kings praised themselves for protecting roads and building waystations for travelers. During the Roman Republic, spas and coastal resorts such as Baiae were popular among the rich, pausanias wrote his Description of Greece in the 2nd century AD. In ancient China, nobles sometimes made a point of visiting Mount Tai and, on occasion, the Islamic hajj is still central to its faith and Chaucers Canterbury Tales and Wu Chengens Journey to the West remain classics of English and Chinese literature. The 10th- to 13th-century Song dynasty also saw secular travel writers such as Su Shi, under the Ming, Xu Xiake continued the practice
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Tertiary sector of the economy
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The tertiary sector or service sector is the third of the three economic sectors of the three-sector theory. The others are the secondary sector, and the primary sector, the basic characteristic of this sector is the production of services instead of end products. Services include attention, advice, access, experience, and discussion, the production of information has long been regarded as a service, but some economists now attribute it to a fourth sector, the quaternary sector. The tertiary sector of industry involves the provision of services to businesses as well as final consumers. The goods may be transformed in the process of providing the service, however, the focus is on people interacting with people and serving the customer rather than transforming physical goods. It is sometimes hard to define whether a company is part of the secondary or tertiary sector. These governmental classification systems have a hierarchy that reflects whether the economic goods are tangible or intangible. Unlike governmental classification systems, the first level of market-based classification systems divides the economy into functionally related markets or industries, the second or third level of these hierarchies then reflects whether goods or services are produced. For the last 100 years, there has been a shift from the primary and secondary sectors to the tertiary sector in industrialised countries. The tertiary sector is now the largest sector of the economy in the Western world and these are not necessarily busboys and live-in maids. Many of them are in the professional category and they are earning as much as manufacturing workers, and often more. The first economy to follow path in the modern world was the United Kingdom. The speed at which other economies have made the transition to service-based economies has increased over time, historically, manufacturing tended to be more open to international trade and competition than services. Service providers face obstacles selling services that goods-sellers rarely face, services are intangible, making it difficult for potential customers to understand what they will receive and what value it will hold for them. Indeed, some, such as consultants and providers of investment services, since the quality of most services depends largely on the quality of the individuals providing the services, people costs are usually a high fraction of service costs. Whereas a manufacturer may use technology, simplification, and other techniques to lower the cost of goods sold, for example, how does one choose one investment adviser over another, since they are often seen to provide identical services. Charging a premium for services is usually an option only for the most established firms, who charge extra based upon brand recognition
35.
Forillon National Park
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Forillon National Park, one of 42 national parks and park reserves across Canada, is located at the outer tip of the Gaspé Peninsula of Quebec and covers 244 km2. Created in 1970, Forillon was the first national park in Quebec, the park includes forests, sea coast, salt marshes, sand dunes, cliffs, and the Eastern End of the Appalachians. The word forillon is thought to have referred to an island or sea stack which used to be a landmark in the area but has since collapsed into the ocean. The area was a summer hunting and fishing ground for the Micmac. This area was used for its rich supply of wood. People living in LAnse-au-Griffon were once involved in the industry here. The creation of the park in 1970 was preceded by the removal of 225 families through expropriation, when preparing to create the new park, the Government of Canada requested that the Quebec government expropriate the homes of these families. The Quebec government sub-contracted the appropriation and negotiations to a private firm and this firm allegedly used various bullying tactics to scare the residents into agreeing to settlements of reduced value. This stratagem ensured a profit margin for the contractor. On 14 February 2011, the House of Commons adopted a motion which issued an apology to the people whose properties were expropriated to create Forillon Park. This expropriation is the subject of a song titled Forillon by the group Le Vent du Nord on their album Têtu, raptors that inhabit this park are great horned owls, northern harriers, peregrine falcons, kestrels, bald eagles, rough-legged hawks, and ospreys. Activities at interpretation sites bring visitors to more about human. The Grande-Grave National Heritage Site attests to the way of life of fishing families, the Hyman Store features collections of articles that were sold at the time, and the store owners tell tales of thriving fisheries industry. Close by, the pedestrian walk Une Tournée dans les Parages brings visitors around houses, fields, Forillon encloses the site of Fort Péninsule, near the Penouille beach. Visitors today can enter a tunnel to see cannon in place since that time. National Parks of Canada List of National Parks of Canada List of Quebec national parks Forillon National Park Watch the NFB documentary A Day in Forillon
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International Appalachian Trail
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Further sections have been designated within Great Britain and Ireland, and there are proposals to extend it further within Europe and North Africa. Following route selection, construction of the trail took place through the late 1990s, the first person to thruhike the IAT, as it then existed, was John Brinda from Washington State, in 1997. He did this as part of his thruhike of the Eastern Continental Trail starting in Key West and he was the first person to thruhike the entire Eastern Continental Trail. The Newfoundland and Labrador extension to the IAT was proposed in 2003 and is still under construction, when completed, it will add an additional 1,200 km of trail. The official opening of the first trail section of the IAT Newfoundland was September 23,2006, from Cap Gaspé, the IAT skips to Prince Edward Island, Nova Scotia, and over the Gulf of St. From there the IAT skips over the Strait of Belle Isle to the terminus of the Appalachian Mountain chain at Belle Isle. With the break-up of Pangaea, sections of the range remained with the continents as they drifted to their present locations. Inspired by this evidence, efforts are being made to extend the IAT into Western Europe, in April 2010 Greenland became the seventh chapter of the International Appalachian Trail. The route is on the Nuussuaq Peninsula near Uummannaq Fjord, Greenland was followed by Scotland in June, when the West Highland Way became the first IAT trail in Europe. In October 2010 the IAT expanded further into Europe when nine new chapters joined the IAT at a meeting in Aviemore, the meeting was attended by the IAT President and representatives from Coast Alive, the British Geological Survey, Visit Scotland, and Fáilte Ireland. The new chapters include Norway, Sweden, Denmark, the Netherlands, England, Ireland, Wales, the Faroe Islands, spain also joined the IAT in 2010. After 2,169 Miles, Whats Another 690, new York Times. com - Personal journals of hikers on the IAT
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Quebec Route 132
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Route 132 is the longest highway in Quebec. This highway is known as the Navigators Route and it passes through the Montérégie, Centre-du-Québec, Chaudière-Appalaches, Bas-Saint-Laurent and Gaspésie regions of the province. Unlike the more direct Autoroute 20, which it shadows from Longueuil to Luceville, until the connection between Rivière-du-Loup and Le Bic is completed, this highway provides a link between the two sections of Autoroute 20. At Rivière-du-Loup, the Trans-Canada Highway continues south on Autoroute 85 to Edmundston and this eastern section of the highway, from Rivière-du-Loup towards Gaspé, was the former Route 6, until the early 1970s realignment of route numbers into a grid. At Sainte-Flavie, the splits and one branch turns south following the valley of the Matapédia River to reach the New Brunswick border near Campbellton. The other branch continues east to follow the coast of the Gaspé peninsula, the total length of this loop is over 930 km. Highway 132 joins Autoroute 15 in Candiac at its Exit 42 and overlaps it until Exit 53, in Brossard, there, Highway 132 begins its overlap with Autoroute 20 until Boucherville, where Autoroute 20 splits off onto Autoroute Jean-Lesage. From that point, Highway 132 continues to the east of Boucherville as a four-lane expressway formerly known as Autoroute 430, list of Quebec provincial highways Heritage Highway Route 132, a 2010 crime film set on Route 132 Provincial Route Map
Canada
Quebec
Quebec Route 132 circles the peninsula, with one branch following the coast and the other cutting across it at Sainte-Flavie.
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