Thunder Bay is a city in, the seat of, Thunder Bay District, Canada. It is the most populous municipality in Northwestern Ontario with a population of 107,909 as of the Canada 2016 Census, the second most populous in Northern Ontario after Greater Sudbury. Located on Lake Superior, the census metropolitan area of Thunder Bay has a population of 121,621, consists of the city of Thunder Bay, the municipalities of Oliver Paipoonge and Neebing, the townships of Shuniah, Conmee, O'Connor, Gillies, the Fort William First Nation. European settlement in the region began in the late 17th century with a French fur trading outpost on the banks of the Kaministiquia River, it grew into an important transportation hub with its port forming an important link in the shipping of grain and other products from western Canada, through the Great Lakes and the Saint Lawrence Seaway, to the east coast. Forestry and manufacturing played important roles in the city's economy, they have declined in recent years, but have been replaced by a "knowledge economy" based on medical research and education.
Thunder Bay is the site of the Thunder Bay Regional Health Research Institute. The city takes its name from the immense Thunder Bay at the head of Lake Superior, known on 18th-century French maps as Baie du Tonnerre; the city is referred to as the "Lakehead", or "Canadian Lakehead", because of its location at the end of Great Lakes navigation on the Canadian side of the border. European settlement at Thunder Bay began with two French fur trading posts which were subsequently abandoned. In 1803, the Montreal-based North West Company established Fort William as its mid-continent entrepôt; the fort thrived until 1821 when the North West Company merged with the Hudson's Bay Company, Fort William was no longer needed. By the 1850s, the Province of Canada began to take an interest in its western extremity. Discovery of copper in the Keweenaw Peninsula of Michigan had prompted a national demand for mining locations on the Canadian shores of Lake Superior. In 1849, French-speaking Jesuits established the Mission de l'Immaculée-Conception on the Kaministiquia to evangelize the Ojibwe.
The Province of Canada negotiated the Robinson Treaty in 1850 with the Ojibwa of Lake Superior. As a result, an Indian reserve was set aside for them south of the Kaministiquia River. In 1859–60, the Department of Crown Lands surveyed two townships and the Town Plot of Fort William for European-Canadian settlement. Another settlement developed a few miles to the north of Fort William after construction by the federal Department of Public Works of a road connecting Lake Superior with the Red River Colony; the work was directed by Simon James Dawson. This public works depot or construction headquarters acquired its first name in May 1870 when Colonel Garnet Wolseley named it Prince Arthur's Landing, it was renamed Port Arthur by the Canadian Pacific Railway in May 1883. The arrival of the CPR in 1875 sparked a long rivalry between the towns, which did not end until their amalgamation in 1970; until the 1880s, Port Arthur was a much larger and dynamic community. The CPR, in collaboration with the Hudson's Bay Company, preferred east Fort William, located on the lower Kaministiquia River where the fur trade posts were.
Provoked by a prolonged tax dispute with Port Arthur and its seizure of a locomotive in 1889, the CPR relocated all its employees and facilities to Fort William. The collapse of silver mining after 1890 undermined the economy of Port Arthur, it had an economic depression. In the era of Sir Wilfried Laurier, Thunder Bay began a period of extraordinary growth, based on improved access to markets via the transcontinental railway and development of the western wheat boom; the CPR double-tracked its Winnipeg–Thunder Bay line. The Canadian Northern Railway established facilities at Port Arthur; the Grand Trunk Pacific Railway began construction of its facilities at the Fort William Mission in 1905, the federal government began construction of the National Transcontinental Railway. Grain elevator construction boomed as the volume of grain shipped to Europe increased. Both cities incurred debt to grant bonuses to manufacturing industries. By 1914, the twin cities had modern infrastructures Both Fort William and Port Arthur were proponents of municipal ownership.
As early as 1892, Port Arthur built Canada's first municipally-owned electric street railway. Both cities spurned Bell Telephone Company of Canada to establish their own municipally-owned telephone systems in 1902; the boom came to an end in 1913–1914, aggravated by the outbreak of the First World War. A war-time economy emerged with the making of munitions and shipbuilding. Men from the cities joined the 52nd, 94th, 141st Battalions of the Canadian Expeditionary Force. Railway employment was hurt when the federal government took over the National Transcontinental Railway and Lake Superior Division from the Grand Trunk in 1915, the Canadian Northern Railway in 1918; these were amalgamated with other government-owned railways in 1923 to form the Canadian National Railways. The CNR closed many of the Canadian Northern Railway facilities in Port Arthur, it opened the Neebing yards in Neebing Township in 1922. By 1929, the population of the two cities had recovered to pre-war levels; the forest products industry has played an important role in the Thunder Bay economy from the 1870s.
Logs and lumber were shipped to the United States. In 1917, the first pulp and paper mill was established in Port Arthur, it was followed by a mill at Fort William, in 1920. There were four mil
Humid continental climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by large seasonal temperature differences, with warm to hot summers and cold winters. Precipitation is distributed throughout the year; the definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below −3 °C and there must be at least four months whose mean temperatures are at or above 10 °C. In addition, the location in question must not be arid; the Dfb and Dsb subtypes are known as hemiboreal. Humid continental climates are found between latitudes 40° N and 60° N, within the central and northeastern portions of North America and Asia, they are much less found in the Southern Hemisphere due to the larger ocean area at that latitude and the consequent greater maritime moderation. In the Northern Hemisphere some of the humid continental climates in Scandinavia, Nova Scotia, Newfoundland are maritime-influenced, with cool summers and winters being just below the freezing mark.
More extreme humid continental climates found in northeast China, southern Siberia, the Canadian Prairies, the Great Lakes region of the American Midwest and Central Canada combine hotter summer maxima and colder winters than the marine-based variety. Using the Köppen climate classification, a climate is classified as humid continental when the temperature of the coldest month is below −3 °C and there must be at least four months whose mean temperatures are at or above 10 °C; these temperatures were not arbitrary. In Europe, the −3 °C average temperature isotherm was near the southern extent of winter snowpack; the 10 °C average temperature was found to be the minimum temperature necessary for tree growth. Wide temperature ranges are common within this climate zone. Second letter in the classification symbol defines seasonal rainfall as follows: s: A dry summer—the driest summer month has less than 40 millimetres of rainfall and has less than 1⁄3 the precipitation of the wettest winter month, w: A dry winter—the driest winter month has less than one‑tenth of the precipitation found in the wettest summer month, f: Without dry season—does not meet either of the alternative specifications.while the third letter denotes the extent of summer heat: a: Hot summer, warmest month averages at least 22 °C, b: Warm summer, warmest month averages below 22 °C and at least four months averages above 10 °C.
Within North America, moisture within this climate regime is supplied by the Gulf of Mexico and adjacent western subtropical Atlantic. Precipitation is well distributed year-round in many areas with this climate, while others may see a marked reduction in wintry precipitation, which increases the chances of a wintertime drought. Snowfall occurs in all areas with a humid continental climate and in many such places is more common than rain during the height of winter. In places with sufficient wintertime precipitation, the snow cover is deep. Most summer rainfall occurs during thunderstorms, in North America and Asia an tropical system. Though humidity levels are high in locations with humid continental climates, the "humid" designation means that the climate is not dry enough to be classified as semi-arid or arid. By definition, forests thrive within this climate. Biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous, temperate evergreen forests, coniferous forests.
Within wetter areas, spruce, pine and oak can be found. Fall foliage is noted during the autumn. A hot summer version of a continental climate features an average temperature of at least 22 °C in its warmest month. Since these regimes are limited to the Northern Hemisphere, the warmest month is July or August. For example, Chicago has average July afternoon temperatures near 29 °C, while average January afternoon temperature are near −1 °C. Frost free periods last 4–6 months within this climate regime. Within North America, this climate includes small areas of central and southeast Canada, portions of the central and eastern United States from the 100th meridian eastward to the Atlantic. Precipitation is less seasonally uniform in the west; the western states of the central United States have thermal regimes which fit the Dfa climate type, but are quite dry, are grouped with the steppe climates. In the Eastern Hemisphere, this climate regime is found within interior Eurasia, east-central Asia, parts of India.
Within Europe, the Dfa climate type is present near the Black Sea in southern Ukraine, the Southern Federal District of Russia, southern Moldova, parts of southern Romania, Bulgaria, but tends to be drier and can be semi-arid in these places. In East Asia, this climate exhibits a monsoonal tendency with much higher precipitation in summer than in winter, due the effects of the strong Siberian High much colder winter temperatures than similar latitudes around the world, however with lower snowfall, the exception being western Japan with its heavy snowfall. Tōhoku, between Tokyo and Hokkaidō and Wester
Relative humidity is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at a given temperature. Relative humidity depends on the pressure of the system of interest; the same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is that of dewpoint; the relative humidity of an air–water mixture is defined as the ratio of the partial pressure of water vapor in the mixture to the equilibrium vapor pressure of water over a flat surface of pure water at a given temperature: ϕ = p H 2 O p H 2 O ∗. Relative humidity is expressed as a percentage. At 100 % relative humidity, the air is at its dewpoint. Climate control refers to the control of temperature and relative humidity in buildings and other enclosed spaces for the purpose of providing for human comfort and safety, of meeting environmental requirements of machines, sensitive materials and technical processes. Along with air temperature, mean radiant temperature, air speed, metabolic rate, clothing level, relative humidity plays a role in human thermal comfort.
According to ASHRAE Standard 55-2017: Thermal Environmental Conditions for Human Occupancy, indoor thermal comfort can be achieved through the PMV method with relative humidities ranging from 0% to 100%, depending on the levels of the other factors contributing to thermal comfort. However, the recommended range of indoor relative humidity in air conditioned buildings is 30-60%. In general, higher temperatures will require lower relative humidities to achieve thermal comfort compared to lower temperatures, with all other factors held constant. For example, with clothing level = 1, Metabolic rate = 1.1, air speed 0.1 m/s, a change in air temperature and mean radiant temperature from 20 degrees C to 24 degrees C would lower the maximum acceptable relative humidity from 100% to 65% to maintain thermal comfort conditions. The CBE Thermal Comfort Tool can be used to demonstrate the effect of relative humidity for specific thermal comfort conditions and it can be used to demonstrate compliance with ASHRAE Standard 55-2017.
When using the adaptive model to predict thermal comfort indoors, relative humidity is not taken into account. Although relative humidity is an important factor for thermal comfort, humans are more sensitive to variations in temperature than they are to changes in relative humidity. Relative humidity has a small effect on thermal comfort outdoors when air temperatures are low, a more pronounced effect at moderate air temperatures, a much stronger influence at higher air temperatures. In cold climates, the outdoor temperature causes lower capacity for water vapor to flow about, thus although it may be snowing and the relative humidity outdoors is high, once that air comes into a building and heats up, its new relative humidity is low, making the air dry, which can cause discomfort. Dry cracked. Low humidity causes tissue lining nasal passages to dry and become more susceptible to penetration of Rhinovirus cold viruses. Low humidity is a common cause of nosebleeds; the use of a humidifier in homes bedrooms, can help with these symptoms.
Indoor relative humidities should be kept above 30% to reduce the likelihood of the occupant's nasal passages drying out. Humans can be comfortable within a wide range of humidities depending on the temperature—from 30% to 70%—but ideally between 50% and 60%. Low humidity can create discomfort, respiratory problems, aggravate allergies in some individuals. In the winter, it is advisable to maintain relative humidity above. Low relative humidities may cause eye irritation. For climate control in buildings using HVAC systems, the key is to maintain the relative humidity at a comfortable range—low enough to be comfortable but high enough to avoid problems associated with dry air; when the temperature is high and the relative humidity is low, evaporation of water is rapid. Wooden furniture can shrink; when the temperature is low and the relative humidity is high, evaporation of water is slow. When relative humidity approaches 100 percent, condensation can occur on surfaces, leading to problems with mold, corrosion and other moisture-related deterioration.
Condensation can pose a safety risk as it can promote the growth of mold and wood rot as well as freezing emergency exits shut. Certain production and technical processes and treatments in factories, laboratories and other facilities require specific relative humidity levels to be maintained using humidifiers and associated control systems; the basic principles for buildings, above apply to vehicles. In addition, there may be safety considerations. For instance, high humidity inside a vehicle can lead to problems of condensation, such
Pulp and paper industry
The pulp and paper industry comprises companies that use wood as raw material and produce pulp, paper and other cellulose-based products. The pulp is fed to a paper machine where it is formed as a paper web and the water is removed from it by pressing and drying. Pressing the sheet removes the water by force. Once the water is forced from the sheet, a special kind of felt, not to be confused with the traditional one, is used to collect the water. Whereas, when making paper by hand, a blotter sheet is used instead. Drying involves using heat to remove water from the paper sheets. In the earliest days of paper making, this was done by hanging the sheets like laundry. In more modern times, various forms of heated drying mechanisms are used. On the paper machine, the most common is the steam heated can dryer; the commercial planting of domesticated mulberry trees to make pulp for papermaking is attested as early as the 6th century. Due to advances in printing technology, the Chinese paper industry continued to grow under the Song dynasty to meet the rising demand for printed books.
Demand for paper was stimulated by the Song government, which needed a large supply of paper for printing paper money and exchange certificates. The first mechanised paper machine was installed at Frogmore Paper Mill, Hertfordshire in 1803, followed by another in 1804; the site operates as a museum. The pulp and paper industry has been criticized by environmental groups like the Natural Resources Defense Council for unsustainable deforestation and clearcutting of old-growth forest; the industry trend is to expand globally to countries like Russia and Indonesia with low wages and low environmental oversight. According to Greenpeace, farmers in Central America illegally rip up vast tracts of native forest for cattle and soybean production without any consequences, companies who buy timber from private land owners contribute to massive deforestation of the Amazon Rainforest. On the other hand, the situation is quite different where forest growth has been on the increase for a number of years, it is estimated for instance that since 1990 forests have grown in Europe by a size equivalent to that of Switzerland, supported through the practice of sustainable forest management by the industry.
In Sweden, for every tree, felled, two are planted. The industry is dominated by northern European and East Asian countries. Australasia and Brazil have significant pulp and paper enterprises; the industry has a significant presence in a number of European countries including Germany, Italy, the Netherlands and Poland. The United States had been the world's leading producer of paper until it was overtaken by China in 2009. According to statistic data by RISI, main producing countries of paper and paperboard, not including pulp, in the world are as follows: The world's main paper and paperboard company groups are as follows.: In 2008, the top 10 forest and packaging products companies were, according to a report by PricewaterhouseCoopers: Leading manufacturers of capital equipment with over $1 billion in annual revenue for the pulp and paper industry include: Valmet Bellmer Andritz Metso Voith Kadant American Forest & Paper Association List of paper mills Converters Paper pollution Pulp and Paper Pulp and paper industry in Canada Pulp and paper industry in Europe Confederation of European Paper Industries Pulp and paper industry in Japan Pulp and paper industry in the United States Roll hardness tester Wood industry Forestry industry Environmental impact of paper Confederation of European Paper Industries American Forest & Paper Association Forest Products Association of Canada
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, sleet, snow and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and "precipitates", thus and mist are not precipitation but suspensions, because the water vapor does not condense sufficiently to precipitate. Two processes acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called "showers."Moisture, lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain occurs. A stationary front is present near the area of freezing rain and serves as the foci for forcing and rising air.
Provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. The cloud droplets will grow large enough to form raindrops and descend toward the Earth where they will freeze on contact with exposed objects. Where warm water bodies are present, for example due to water evaporation from lakes, lake-effect snowfall becomes a concern downwind of the warm lakes within the cold cyclonic flow around the backside of extratropical cyclones. Lake-effect snowfall can be locally heavy. Thundersnow is possible within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation. On the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. Most precipitation is caused by convection; the movement of the monsoon trough, or intertropical convergence zone, brings rainy seasons to savannah climes.
Precipitation is a major component of the water cycle, is responsible for depositing the fresh water on the planet. 505,000 cubic kilometres of water falls as precipitation each year. Given the Earth's surface area, that means the globally averaged annual precipitation is 990 millimetres, but over land it is only 715 millimetres. Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on other celestial bodies, e.g. when it gets cold, Mars has precipitation which most takes the form of frost, rather than rain or snow. Precipitation is a major component of the water cycle, is responsible for depositing most of the fresh water on the planet. 505,000 km3 of water falls as precipitation each year, 398,000 km3 of it over the oceans. Given the Earth's surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective and orographic rainfall.
Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation. Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice. Mixtures of different types of precipitation, including types in different categories, can fall simultaneously. Liquid forms of precipitation include drizzle. Rain or drizzle that freezes on contact within a subfreezing air mass is called "freezing rain" or "freezing drizzle". Frozen forms of precipitation include snow, ice needles, ice pellets and graupel; the dew point is the temperature to which a parcel must be cooled in order to become saturated, condenses to water. Water vapor begins to condense on condensation nuclei such as dust and salt in order to form clouds. An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus.
Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. It can form due to the lifting of advection fog during breezy conditions. There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, evaporative cooling. Adiabatic cooling occurs when air expands; the air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain. Conductive cooling occurs when the air comes into contact with a colder surface by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation; the main ways water vapor is added to the air are: wind convergence into areas of upward motion, precipitation or virga falling from above, daytime heating evaporating water from the surface of oceans, water bodies or wet lan
House of Commons of Canada
The House of Commons of Canada is a component of the Parliament of Canada, along with the Sovereign and the Senate. The House of Commons meets in a temporary Commons chamber in the West Block of the parliament buildings on Parliament Hill in Ottawa, while the Centre Block, which houses the traditional Commons chamber, undergoes a ten-year renovation; the House of Commons is a democratically elected body whose members are known as Members of Parliament. There were 308 members in the last parliament, but that number has risen to 338 following the election on Monday October 19, 2015. Members are elected by simple plurality in each of the country's electoral districts, which are colloquially known as ridings. MPs may hold office until Parliament is dissolved and serve for constitutionally limited terms of up to five years after an election. However, terms have ended before their expiry and the sitting government has dissolved parliament within four years of an election according to a long-standing convention.
In any case, an Act of Parliament now limits each term to four years. Seats in the House of Commons are distributed in proportion to the population of each province and territory. However, some ridings are more populous than others, the Canadian constitution contains some special provisions regarding provincial representation; as a result, there is some regional malapportionment relative to population. The House of Commons was established in 1867, when the British North America Act—now called the Constitution Act, 1867—created the Dominion of Canada, was modelled on the British House of Commons; the lower of the two houses making up the parliament, the House of Commons in practice holds far more power than the upper house, the Senate. Although the approval of both Houses is necessary for legislation, the Senate rarely rejects bills passed by the commons. Moreover, the Cabinet is responsible to the House of Commons; the prime minister stays in office only as long as they retain the support, or "confidence", of the lower house.
The term derives from the Anglo-Norman word communes, referring to the geographic and collective "communities" of their parliamentary representatives and not the third estate, the commonality. This distinction is made clear in the official French name of the body, Chambre des communes. Canada and the United Kingdom remain the only countries to use the name "House of Commons" for a lower house of parliament; the House of Commons came into existence in 1867, when the British Parliament passed the British North America Act, uniting the Province of Canada, Nova Scotia and New Brunswick into a single federation called the Dominion of Canada. The new Parliament of Canada consisted of the Senate and the House of Commons; the Parliament of Canada was based on the Westminster model. Unlike the UK Parliament, the powers of the Parliament of Canada were limited in that other powers were assigned to the provincial legislatures; the Parliament of Canada remained subordinate to the British Parliament, the supreme legislative authority for the entire British Empire.
Greater autonomy was granted by the Statute of Westminster 1931, after which new acts of the British Parliament did not apply to Canada, with some exceptions. These exceptions were removed by the Canada Act 1982. From 1867, the Commons met in the chamber used by the Legislative Assembly of Canada until the building was destroyed by fire in 1916, it relocated to the amphitheatre of the Victoria Memorial Museum—what is today the Canadian Museum of Nature, where it met until 1922. Until the end of 2018, the Commons sat in Centre Block chamber. Starting with the final sitting before the 2019 federal election, the Commons sits in a temporary chamber in the West Block until at least 2028, while renovations are undertaken in the Centre Block of Parliament; the House of Commons comprises 338 members. The constitution specifies a basic minimum of 295 electoral districts, but additional seats are allocated according to various clauses. Seats are distributed among the provinces in proportion to population, as determined by each decennial census, subject to the following exceptions made by the constitution.
Firstly, the "senatorial clause" guarantees that each province will have at least as many MPs as Senators. Secondly, the "grandfather clause" guarantees each province has at least as many Members of Parliament now as it had in 1985; as a result of these clauses, smaller provinces and provinces that have experienced a relative decline in population have become over-represented in the House. Ontario, British Columbia, Alberta are under-represented in proportion to their populations, while the other seven provinces are over-represented. Boundary commissions, appointed by the federal government for each province, have the task of drawing the boundaries of the electoral districts in each province. Territorial representation is independent of population; the calculation for the provinces is done with a base of 279 seats. The total population of the provinces is divided by 279 to equal the electoral quotient; the population of the province is divided by the electoral q
European Canadians known as White Canadians and Euro-Canadians, are Canadians with ancestry from Europe. They form the largest panethnic group within Canada; the French were the first Europeans to establish a continuous presence in. Hélène Desportes is considered the first white child born in New France, she was born circa 1620, to Françoise Langlois. In the 2016 census, the largest European ancestry groups were British Isles origins, Scottish, German, Italian. However, the country's largest self-reported ethnic origin is "Canadian". Since 1996, "Canadian" as an ethnic group has been added to census questionnaires for possible ancestry, which caused English Canadians, British Canadians and French Canadians to become underrepresented; the grouping is similar to that of "American" in neighbouring United States and is most espoused by European Canadians whose ancestors have been some of the earliest European settlers of what is now Canada, to the point where they no longer feel a connection to their countries of origin.
In the 2011 National Household Survey Profile, 10,563,805 people chose "Canadian" as their ethnic group, making it the single largest group in the country. The table shows the European-Canadian population showing a gradual increase from the 1871 Census, their proportion of the total Canadian population has been decreasing since the mid-twentieth century to the most recent census in 2011. Canada enumerated its population by ethnic origins. European Canadians are still the largest ethnic group in Canada. Elements of Aboriginal, French and more recent immigrant customs and religions have combined to form the culture of Canada and thus a Canadian identity. Canada has been influenced by its linguistic and economic neighbour, the United States; the top ten cities as per population of European Canadians are as follows: Toronto 1,282,750 Montreal 1,082,615 Calgary 744,625 Ottawa 652,650 Edmonton 524,265 Quebec City 475,720 Hamilton 415,740 Winnipeg 412,645 Halifax 336,375 Mississauga 302,375The top ten such Census Metropolitan Areas are as follows: Montreal 3,070,210 Toronto 2,804,630 Vancouver 1,179,100 Ottawa - Gatineau 981,630 Calgary 869,555 Edmonton 857,085 Quebec City 729,310 Hamilton 590,310 Winnipeg 473,360 Kitchener - Cambridge - Waterloo 407,460 The culture of the Canadians of European descent, European-Canadian culture, is the main culture of Canada.
From their earliest presence in North America, European Canadians have contributed literature, architecture and theater, religion and philosophy, agricultural skills, medicine and technology, fashion and clothing styles, language, economics, legal system, political system, social and technological innovation to Canadian culture. European-Canadian culture derived its earliest influences from English, Scottish and Irish settlers and is quantitatively the largest proportion of Canadian culture; the overall Canadian culture reflects European-Canadian culture known as White Canadian culture. The culture has been developing since long. Much of Canadian culture shows influences from English culture. Colonial ties to Great Britain spread the English language, legal system and other cultural attributes. Canadian flag - In 1964, Prime Minister Lester B. Pearson formed a committee to resolve the issue, sparking a serious debate about a flag change to replace the Union Flag. Out of three choices, the maple leaf design by George Stanley, based on the flag of the Royal Military College of Canada, was selected.
The flag made its first official appearance on February 15, 1965. Another area of cultural influence are Canadian Patriotic songs: Canadian National Anthem - Two Canadians of French descent Adolphe-Basile Routhier wrote the lyrics and Calixa Lavallée composed the music in 1880; the English lyrics, the official and most popular version were written in 1908 by Scottish-Canadian Robert Stanley Weir. The Maple Leaf Forever - is an older but unofficial national anthem written by Scotsman Alexander Muir in 1867, it was in consideration for official national anthem, however, no French version was written, so, it was never popular with Francophones. Ice Hockey - British soldiers and immigrants to Canada and the United States brought their stick-and-ball games with them and played them on the ice and snow of winter. Ice hockey was first played in Canada during the early nineteenth century, based on similar sports such as field hockey that were played in Europe; the sport was played with a stick and ball, but in 1860 a group of English veterans from the Royal Canadian Rifle Regiment played a game in Kingston, utilising a puck for what is believed to be the first time.
This match, played on the frozen harbour by the city, is sometimes considered to be the birth of modern ice hockey. Most of the heritage that all twenty-three Canadian Prime Ministers come from: is British ancestry. Canadian Prime Ministers' ancestry can be traced to ancestors from multiple nations in Europe. European diaspora Métis people Ethnic origins of people in Canada European Americans Demographics of Canada