1.
James Bay (singer)
–
James Michael Bay is an English singer-songwriter and guitarist. In 2014, he released his single Hold Back the River, which has certified platinum, before releasing his debut studio album Chaos. The album went to one in the UK and number 15 in the US. In February 2015, Bay received the Brit Awards Critics Choice award, at the 2016 Brit Awards he received the award for Best British Male Solo Artist. Bay also received three nominations at the 2016 Grammy Awards, for Best New Artist, Best Rock Album, Bay was brought up in Hitchin, Hertfordshire and attended Hitchin Boys School. Aged 11, Bay was inspired to play guitar after hearing Eric Claptons Layla. Im trying to make songs that people feel something, and if Im lucky. Bay caught the attention of a Republic Records A&R after a fan uploaded a video to YouTube of him performing at an open mic in London and his first EP, The Dark of the Morning, was released in 2013. Within a year he was selling out his first UK headline tour, Bay released his debut extended play, The Dark of the Morning, on 18 July 2013. His second EP, Let It Go, was released on 12 May 2014, the Let It Go EP debuted in the top 10 iTunes album chart and the lead single, titled Let It Go, peaked at number 10 in the UK charts. Bay has performed live on the Burberry runway and has recorded a Burberry Acoustic session. Bay toured with Hozier in 2014, Bay recorded his entire debut studio album Chaos and the Calm at Blackbird Studios in Nashville, with producer Jacquire King. It debuted at one in the UK charts and has been certified platinum. His single, Hold Back The River peaked at number 2 in the UK charts and has certified platinum. Bay performed on the Pyramid Stage at Glastonbury Festival in June 2015, at the 2016 Brit Awards in London on 24 February, Bay received the award for Best British Male Solo Artist, and also performed Love Yourself with Justin Bieber at the ceremony. Bay endorses and plays Tone King amplifiers, a boutique brand of Premier Builders Guild. Chaos and the Calm Tour Boardmasters - Cornwall Toured with Kodaline UK and Ireland Toured with Hozier North America Taylor Swift –1989 World Tour
James Bay (singer)
–
Bay performing live in
Anaheim, California in 2013
James Bay (singer)
–
Bay performing at the
Glastonbury Festival on 26 June 2015
2.
Hudson Bay
–
Hudson Bay is a large body of saltwater in northeastern Canada with a surface area of 1,230,000 square kilometres. Hudson Bays southern arm is called James Bay, the Eastern Cree name for Hudson and James Bay is Wînipekw or Wînipâkw, meaning muddy or brackish water. Lake Winnipeg is similarly named by the local Cree, as is the location for the city of Winnipeg, Hudson Bay encompasses 1,230,000 square kilometres, making it the second-largest bay in the world. The bay is shallow and is considered an epicontinental sea. It is about 1,370 km long and 1,050 km wide, on the east it is connected with the Atlantic Ocean by Hudson Strait, on the north, with the Arctic Ocean by Foxe Basin, and Fury and Hecla Strait. Geographic coordinates, 78° to 95° W, 51° to 70° N. Hudson Bay is part of the North Atlantic Ocean, sometimes the Hudson Bay and Hudson Strait basins are considered part of the Arctic Ocean even though their waters flow predominantly to the Atlantic. Some sources describe Hudson Bay as a sea of the Atlantic Ocean. English explorers and colonists named Hudson Bay after Sir Henry Hudson who explored the bay beginning August 2,1610 on his ship Discovery. On his fourth voyage to North America, Hudson worked his way around Greenlands west coast and into the bay, Discovery became trapped in the ice over the winter, and the crew survived onshore at the southern tip of James Bay. When the ice cleared in the spring, Hudson wanted to explore the rest of the area and they left Hudson and others adrift in a small boat. No one knows the fate of Hudson or the crew members stranded with him, in 1668, Nonsuch reached the bay and traded for beaver pelts, leading to the creation of the Hudsons Bay Company which still bears the historic name. The HBC negotiated a trading monopoly from the British crown for the Hudson Bay watershed, called Ruperts Land, france contested this grant by sending several military expeditions to the region, but abandoned its claim in the Treaty of Utrecht. See Anglo-French conflicts on Hudson Bay, during this period, the Hudsons Bay Company built several forts and trading posts along the coast at the mouth of the major rivers. The strategic locations were bases for inland exploration, more importantly, they were trading posts with the indigenous peoples who came to them with furs from their trapping season. The HBC shipped the furs to Europe and continued to use these posts until the beginning of the 20th century, the port of Churchill is still an important shipping link for trade with Europe and Russia. HBCs trade monopoly was abolished in 1870, and it ceded Ruperts Land to Canada, starting in 1913, the Bay was extensively charted by the Canadian Governments CSS Acadia to develop it for navigation. This mapping progress led to the establishment of Churchill, Manitoba as a port for wheat exports in 1929. Due to a change in naming conventions, Hudsons Bay is now called Hudson Bay, as a result, the names of the body of water and the company are often mistaken for one another
Hudson Bay
–
Ice begins to form in early November at Hudson Bay.
Hudson Bay
–
Hudson Bay, Canada
Hudson Bay
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In late spring (May), large chunks of ice float near the eastern shore of the bay, while to the west, the center of the bay remains frozen. Between 1971 and 2007, the length of the ice-free season in the southwestern part of the Hudson Bay—historically the last area to thaw—increased by about seven days.
3.
Ontario
–
Ontario, one of the 13 provinces and territories of Canada, is located in east-central Canada. It is Canadas most populous province by a margin, accounting for nearly 40 percent of all Canadians. Ontario is fourth-largest in total area when the territories of the Northwest Territories and it is home to the nations capital city, Ottawa, and the nations most populous city, Toronto. There is only about 1 km of land made up of portages including Height of Land Portage on the Minnesota border. Ontario is sometimes divided into two regions, Northern Ontario and Southern Ontario. The great majority of Ontarios population and arable land is located in the south, in contrast, the larger, northern part of Ontario is sparsely populated with cold winters and is heavily forested. The province is named after Lake Ontario, a thought to be derived from Ontarí, io, a Huron word meaning great lake, or possibly skanadario. Ontario has about 250,000 freshwater lakes, the province consists of three main geographical regions, The thinly populated Canadian Shield in the northwestern and central portions, which comprises over half the land area of Ontario. Although this area mostly does not support agriculture, it is rich in minerals and in part covered by the Central and Midwestern Canadian Shield forests, studded with lakes, Northern Ontario is subdivided into two sub-regions, Northwestern Ontario and Northeastern Ontario. The virtually unpopulated Hudson Bay Lowlands in the north and northeast, mainly swampy. Southern Ontario which is further sub-divided into four regions, Central Ontario, Eastern Ontario, Golden Horseshoe, the highest point is Ishpatina Ridge at 693 metres above sea level located in Temagami, Northeastern Ontario. In the south, elevations of over 500 m are surpassed near Collingwood, above the Blue Mountains in the Dundalk Highlands, the Carolinian forest zone covers most of the southwestern region of the province. A well-known geographic feature is Niagara Falls, part of the Niagara Escarpment, the Saint Lawrence Seaway allows navigation to and from the Atlantic Ocean as far inland as Thunder Bay in Northwestern Ontario. Northern Ontario occupies roughly 87 percent of the area of the province. Point Pelee is a peninsula of Lake Erie in southwestern Ontario that is the southernmost extent of Canadas mainland, Pelee Island and Middle Island in Lake Erie extend slightly farther. All are south of 42°N – slightly farther south than the border of California. The climate of Ontario varies by season and location, the effects of these major air masses on temperature and precipitation depend mainly on latitude, proximity to major bodies of water and to a small extent, terrain relief. In general, most of Ontarios climate is classified as humid continental, Ontario has three main climatic regions
Ontario
–
Algonquin Provincial Park, Cache Lake
Ontario
–
Flag
Ontario
–
Summer at
Sandbanks Provincial Park on Lake Ontario.
Ontario
–
The
Niagara Escarpment on the
Bruce Peninsula.
4.
Quebec
–
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
Quebec
–
The arrival of
Samuel de Champlain, the father of
New France, on the site of
Quebec City.
Quebec
–
Flag
Quebec
–
Michel's falls on
Ashuapmushuan River in
Saint-Félicien,
Saguenay–Lac-Saint-Jean.
Quebec
–
View of
Jacques-Cartier River from Andante mountain.
5.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
Geographic coordinate system
–
Longitude lines are perpendicular and latitude lines are parallel to the equator.
6.
Drainage basin
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A drainage basin or catchment area is any area of land where precipitation collects and drains off into a common outlet, such as into a river, bay, or other body of water. Drainage basins connect into other drainage basins at elevations in a hierarchical pattern, with smaller sub-drainage basins. Other terms used to describe drainage basins are catchment, catchment basin, drainage area, river basin and water basin. In closed drainage basins the water converges to a point inside the basin, known as a sink, which may be a permanent lake. The drainage basin acts as a funnel by collecting all the water within the covered by the basin. Each drainage basin is separated topographically from adjacent basins by a perimeter, drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are defined to allow multiple inlets, outlets, or sinks, in a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins. Drainage basins of the oceans and seas of the world. Grey areas are endorheic basins that do not drain to the oceans, the following is a list of the major ocean basins, About 48. 7% of the worlds land drains to the Atlantic Ocean. The two major mediterranean seas of the world also flow to the Atlantic, The Caribbean Sea and Gulf of Mexico basin includes most of the U. S. The Mediterranean Sea basin includes much of North Africa, east-central Africa, Southern, Central, and Eastern Europe, Turkey, and the areas of Israel, Lebanon. Just over 13% of the land in the world drains to the Pacific Ocean, the Indian Oceans drainage basin also comprises about 13% of Earths land. It drains the eastern coast of Africa, the coasts of the Red Sea and the Persian Gulf, the Indian subcontinent, Burma, antarctica comprises approximately eight percent of the Earths land. The five largest river basins, from largest to smallest, are the basins of the Amazon, the Río de la Plata, the Congo, the Nile, and the Mississippi. The three rivers that drain the most water, from most to least, are the Amazon, Ganga, endorheic drainage basins are inland basins that do not drain to an ocean. Around 18% of all land drains to endorheic lakes or seas or sinks, the largest of these consists of much of the interior of Asia, which drains into the Caspian Sea, the Aral Sea, and numerous smaller lakes. Some of these, such as the Great Basin, are not single drainage basins but collections of separate, in endorheic bodies of standing water where evaporation is the primary means of water loss, the water is typically more saline than the oceans. An extreme example of this is the Dead Sea, drainage basins have been historically important for determining territorial boundaries, particularly in regions where trade by water has been important
Drainage basin
–
Animation of
Latoriţa River drainage basin,
Romania
Drainage basin
–
Example of a drainage basin. The dashed line is the main water divide of the hydrographic basin.
Drainage basin
–
Endorheic basin in
Central Asia
Drainage basin
–
The
Mississippi River drains the largest area of any
U.S. river, much of it
agricultural regions. Agricultural runoff and other water pollution that flows to the outlet is the cause of the
hypoxic, or dead zone in the
Gulf of Mexico.
7.
French language
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French is a Romance language of the Indo-European family. It descended from the Vulgar Latin of the Roman Empire, as did all Romance languages, French has evolved from Gallo-Romance, the spoken Latin in Gaul, and more specifically in Northern Gaul. Its closest relatives are the other langues doïl—languages historically spoken in northern France and in southern Belgium, French was also influenced by native Celtic languages of Northern Roman Gaul like Gallia Belgica and by the Frankish language of the post-Roman Frankish invaders. Today, owing to Frances past overseas expansion, there are numerous French-based creole languages, a French-speaking person or nation may be referred to as Francophone in both English and French. French is a language in 29 countries, most of which are members of la francophonie. As of 2015, 40% of the population is in Europe, 35% in sub-Saharan Africa, 15% in North Africa and the Middle East, 8% in the Americas. French is the fourth-most widely spoken mother tongue in the European Union, 1/5 of Europeans who do not have French as a mother tongue speak French as a second language. As a result of French and Belgian colonialism from the 17th and 18th century onward, French was introduced to new territories in the Americas, Africa, most second-language speakers reside in Francophone Africa, in particular Gabon, Algeria, Mauritius, Senegal and Ivory Coast. In 2015, French was estimated to have 77 to 110 million native speakers, approximately 274 million people are able to speak the language. The Organisation internationale de la Francophonie estimates 700 million by 2050, in 2011, Bloomberg Businessweek ranked French the third most useful language for business, after English and Standard Mandarin Chinese. Under the Constitution of France, French has been the language of the Republic since 1992. France mandates the use of French in official government publications, public education except in specific cases, French is one of the four official languages of Switzerland and is spoken in the western part of Switzerland called Romandie, of which Geneva is the largest city. French is the language of about 23% of the Swiss population. French is also a language of Luxembourg, Monaco, and Aosta Valley, while French dialects remain spoken by minorities on the Channel Islands. A plurality of the worlds French-speaking population lives in Africa and this number does not include the people living in non-Francophone African countries who have learned French as a foreign language. Due to the rise of French in Africa, the total French-speaking population worldwide is expected to reach 700 million people in 2050, French is the fastest growing language on the continent. French is mostly a language in Africa, but it has become a first language in some urban areas, such as the region of Abidjan, Ivory Coast and in Libreville. There is not a single African French, but multiple forms that diverged through contact with various indigenous African languages, sub-Saharan Africa is the region where the French language is most likely to expand, because of the expansion of education and rapid population growth
French language
–
The
"arrêt" signs (French for "stop") are used in
Canada while the international stop, which is also a valid French word, is used in France as well as other French-speaking countries and regions.
French language
–
Regions where French is the main language
French language
–
Town sign in
Standard Arabic and French at the entrance of
Rechmaya in
Lebanon.
French language
–
An obsolete 100
Lebanese pound note with the French language inscriptions "Banque du Liban" and "Cent livres".
8.
Cree language
–
Despite numerous speakers within this wide-ranging area, the only region where Cree has any official status is in the Northwest Territories, alongside eight other aboriginal languages. Endonyms are Nēhiyawēwin ᓀᐦᐃᔭᐍᐏᐣ, Nīhithawīwin, Nehirâmowin, Nehlueun, Ilnu-Aimûn, Innu-Aimûn, Iyiniu-Ayamiwin, Iyiyiu-Ayamiwin, Ililîmowin, Inilîmowin, the Cree dialect continuum can be divided by many criteria. Dialects spoken in northern Ontario and the southern James Bay, Lanaudière, in several dialects, including northern Plains Cree and Woods Cree, the long vowels /eː/ and /iː/ have merged into a single vowel, /iː/. In the Quebec communities of Chisasibi, Whapmagoostui, and Kawawachikamach, see the table above for examples in the *kīla column. Very often the Cree dialect continuum is divided into two languages, Cree and Montagnais, Cree includes all dialects which have not undergone the *k > /tʃ/ sound change while Montagnais encompasses the territory where this sound change has occurred. These labels are useful from a linguistic perspective but are confusing as East Cree then qualifies as Montagnais. For practical purposes, Cree usually covers the dialects which use syllabics as their orthography, the term Naskapi typically refers to Kawawachikamach and Natuashish. The Cree dialects can be classified into nine groups. From west to east, This table is made to all possible consonant phonemes that may be included in a Cree language. Like many Native American languages, Cree features a complex polysynthetic morphology, a common grammatical feature in Cree dialects, in terms of sentence structure, is non-regulated word order. Word order is not governed by a set of rules or structure, instead. Subject, Verb, and Object in a sentence can vary in order, for example, SVO, VOS, OVS, obviation is also a key aspect of the Cree language. In a sense, the obviative can be defined as any third-person ranked lower on a hierarchy of discourse salience than some other discourse-participant. “Obviative animate nouns, are marked by ending –a, and are used to refer to persons who are more peripheral in the discourse than the proximate third person”. For example, Sam wâpam-ew Susan-a Sam see-3SG Susan-3OBV Sam sees Susan The suffix -a marks Susan as the obviative, or fourth person, another distinct feature of the Cree language is what could be understood as gender, similar to the French language’s genders of male and female nouns. Cree defines nouns as being animate or inanimate, there is no distinct rule governing the classification of animacy or inanimacy, rather, it is learned through immersive language acquisition. A Cree word can be long, and express something that takes a series of words in English. For example, the Plains Cree word for school is kiskinohamātowikamikw, both writing systems represent the language phonetically
Cree language
–
Trilingual plaque in English, French and Cree
Cree language
–
A rough map of Cree dialect areas
Cree language
–
A Quebec stop sign in Cree/English/French
9.
Arctic Ocean
–
The Arctic Ocean is the smallest and shallowest of the worlds five major oceans. Alternatively, the Arctic Ocean can be seen as the northernmost part of the all-encompassing World Ocean, located mostly in the Arctic north polar region in the middle of the Northern Hemisphere, the Arctic Ocean is almost completely surrounded by Eurasia and North America. It is partly covered by sea ice throughout the year and almost completely in winter, the summer shrinking of the ice has been quoted at 50%. The US National Snow and Ice Data Center uses satellite data to provide a record of Arctic sea ice cover. The Arctic may become ice free for the first time in human history within a few years or by 2040, for much of European history, the north polar regions remained largely unexplored and their geography conjectural. He was probably describing loose sea ice known today as growlers or bergy bits, his Thule was probably Norway, early cartographers were unsure whether to draw the region around the North Pole as land or water. The makers of navigational charts, more conservative than some of the more fanciful cartographers, tended to leave the region blank and this lack of knowledge of what lay north of the shifting barrier of ice gave rise to a number of conjectures. In England and other European nations, the myth of an Open Polar Sea was persistent, john Barrow, longtime Second Secretary of the British Admiralty, promoted exploration of the region from 1818 to 1845 in search of this. In the United States in the 1850s and 1860s, the explorers Elisha Kane, even quite late in the century, the eminent authority Matthew Fontaine Maury included a description of the Open Polar Sea in his textbook The Physical Geography of the Sea. Nevertheless, as all the explorers who travelled closer and closer to the reported, the polar ice cap is quite thick. Fridtjof Nansen was the first to make a crossing of the Arctic Ocean. The first surface crossing of the ocean was led by Wally Herbert in 1969, in a dog sled expedition from Alaska to Svalbard, with air support. The first nautical transit of the pole was made in 1958 by the submarine USS Nautilus. Since 1937, Soviet and Russian manned drifting ice stations have extensively monitored the Arctic Ocean, scientific settlements were established on the drift ice and carried thousands of kilometres by ice floes. In World War II, the European region of the Arctic Ocean was heavily contested, the Arctic Ocean occupies a roughly circular basin and covers an area of about 14,056,000 km2, almost the size of Antarctica. The coastline is 45,390 km long and it is surrounded by the land masses of Eurasia, North America, Greenland, and by several islands. It is connected to the Pacific Ocean by the Bering Strait and to the Atlantic Ocean through the Greenland Sea, countries bordering the Arctic Ocean are, Russia, Norway, Iceland, Greenland, Canada and the United States. There are several ports and harbours around the Arctic Ocean In Alaska, in Canada, ships may anchor at Churchill in Manitoba, Nanisivik in Nunavut, Tuktoyaktuk or Inuvik in the Northwest territories
Arctic Ocean
–
A
bathymetric /
topographic of the Arctic Ocean and the surrounding lands.
Arctic Ocean
–
Emanuel Bowen 's 1780s map of the Arctic features a "Northern Ocean".
Arctic Ocean
–
Sea cover in the Arctic Ocean, showing the median, 2005 and 2007 coverage
Arctic Ocean
–
Three
polar bears approach
USS Honolulu near the
North Pole.
10.
Akimiski Island
–
Akimiski Island is the largest island in James Bay, Canada, which is part of the Qikiqtaaluk Region of the territory of Nunavut. It has an area of 3,001 km2, making it the 163rd largest island in the world, Akimiski Island is only 19 km from the province of Ontario. From the western side of the island, one can see the Ontario coastline, the islands name is Cree land across the water. The island has no human inhabitants, however, it is part of the Attawapiskat First Nations traditional territory and is frequently used for traditional purposes. The surface of Akimiski is flat and slopes gradually to the north, most of the vegetation that covers the island consists of lichen, moss, sedges, and dwarf black spruce. The island is a wetland that includes mudflats, tidal marshes. Freshwater streams that flow into southwestern James Bay carry sediments and abundant nutrients that help to sustain the productive waterfowl habitat around Akimiski Island, the Akimiski Island Group includes Akimiski, Gasket, and Gullery Islands, Albert Shoal, and Akimiski Strait Isles. Mean annual temperature,2.5 °C Average rainfall,450 mm Average snowfall,250 mm Akimiski Island is a Canadian Important Bird Area and its eastern portion is also a federal Migratory Bird Sanctuary, and much of the coastline is a Key Migratory Bird Terrestrial Habitat site. The coastal waters and wetlands of Akimiski Island are important feeding grounds for many varieties of migratory birds, during fall migration, there is an abundance of birds when adults and young are present. In the springtime, the birds tend to reside in the areas of James Bay until the northern section thaws. Among mammalians, ringed seals, polar bears, and beluga whales can be found in the area, NASA Photo, STS085-713-070 Akimiski Island, Northwest Territory, Canada August 1997 Akimiski Island, a 2000-square-mile uninhabited island, is the largest island in James Bay
Akimiski Island
–
Landsat image of Akimiski Island
Akimiski Island
–
Closeup of Akimiski Island
Akimiski Island
–
Photo of western coast, viewed from north towards south, in mid-July
11.
Nunavut
–
Nunavut is the newest, largest, and northernmost territory of Canada. The creation of Nunavut resulted in the first major change to Canadas political map since the incorporation of the province of Newfoundland, Nunavut comprises a major portion of Northern Canada, and most of the Canadian Arctic Archipelago. Its vast territory makes it the fifth-largest country subdivision in the world, the capital Iqaluit, on Baffin Island in the east, was chosen by the 1995 capital plebiscite. Other major communities include the regional centres of Rankin Inlet and Cambridge Bay and it is Canadas only geo-political region that is not connected to the rest of North America by highway. Nunavut is the largest in area and the second least populous of Canadas provinces and territories. One of the worlds most remote, sparsely settled regions, it has a population of 35,944, mostly Inuit, spread over an area of just over 1,750,000 km2, Nunavut is also home to the worlds northernmost permanently inhabited place, Alert. A weather station farther down Ellesmere Island, Eureka, has the lowest average temperature of any Canadian weather station. Nunavut means our land in Inuktitut, Nunavut covers 1,877,787 km2 of land and 160,935 km2 of water in Northern Canada. This makes it the fifth largest subnational entity in the world, if Nunavut were a country, it would rank 15th in area. It also shares borders with Greenland and the provinces of Quebec, Ontario. Nunavuts highest point is Barbeau Peak on Ellesmere Island, the population density is 0.019 persons/km2, one of the lowest in the world. By comparison, Greenland has approximately the area and nearly twice the population. Nunavut experiences a climate in most regions, owing to its high latitude. In more southerly continental areas very cold climates can be found. The region now known as Nunavut has supported an indigenous population for approximately 4,000 years. Most historians identify the coast of Baffin Island with the Helluland described in Norse sagas, the materials were collected in five seasons of excavation at Cape Tanfield. Scholars determined that these provide evidence of European traders and possibly settlers on Baffin Island and they seem to indicate prolonged contact, possibly up to 1450. So you have to consider the possibility that as remote as it may seem, the ore turned out to be worthless, but Frobisher made the first recorded European contact with the Inuit
Nunavut
–
Niungvaliruluit (”pointer like a window“)
inuksuk, Foxe peninsula,
Baffin Island
Nunavut
–
Flag
Nunavut
–
Inuit women at Ashe Inlet, 1884.
Nunavut
–
Inuit village near
Frobisher Bay, 1865
12.
Hydroelectricity
–
Hydroelectricity is electricity produced from hydropower. In 2015 hydropower generated 16. 6% of the total electricity and 70% of all renewable electricity. Hydropower is produced in 150 countries, with the Asia-Pacific region generating 33 percent of global hydropower in 2013, China is the largest hydroelectricity producer, with 920 TWh of production in 2013, representing 16.9 percent of domestic electricity use. The cost of hydroelectricity is relatively low, making it a source of renewable electricity. The hydro station consumes no water, unlike coal or gas plants, the average cost of electricity from a hydro station larger than 10 megawatts is 3 to 5 U. S. cents per kilowatt-hour. With a dam and reservoir it is also a source of electricity since the amount produced by the station can be changed up or down very quickly to adapt to changing energy demands. Once a hydroelectric complex is constructed, the project produces no direct waste, Hydropower has been used since ancient times to grind flour and perform other tasks. In the mid-1770s, French engineer Bernard Forest de Bélidor published Architecture Hydraulique which described vertical-, by the late 19th century, the electrical generator was developed and could now be coupled with hydraulics. The growing demand for the Industrial Revolution would drive development as well, in 1878 the worlds first hydroelectric power scheme was developed at Cragside in Northumberland, England by William George Armstrong. It was used to power an arc lamp in his art gallery. The old Schoelkopf Power Station No.1 near Niagara Falls in the U. S. side began to produce electricity in 1881. The first Edison hydroelectric power station, the Vulcan Street Plant, began operating September 30,1882, in Appleton, Wisconsin, by 1886 there were 45 hydroelectric power stations in the U. S. and Canada. By 1889 there were 200 in the U. S. alone, at the beginning of the 20th century, many small hydroelectric power stations were being constructed by commercial companies in mountains near metropolitan areas. Grenoble, France held the International Exhibition of Hydropower and Tourism with over one million visitors, by 1920 as 40% of the power produced in the United States was hydroelectric, the Federal Power Act was enacted into law. The Act created the Federal Power Commission to regulate hydroelectric power stations on federal land, as the power stations became larger, their associated dams developed additional purposes to include flood control, irrigation and navigation. Federal funding became necessary for development and federally owned corporations, such as the Tennessee Valley Authority. Hydroelectric power stations continued to become larger throughout the 20th century, Hydropower was referred to as white coal for its power and plenty. Hoover Dams initial 1,345 MW power station was the worlds largest hydroelectric station in 1936
Hydroelectricity
–
The
Three Gorges Dam in Central China is the
world's largest power producing facilitiy of any kind.
Hydroelectricity
–
Museum Hydroelectric power plant ″Under the Town″ in
Serbia, built in 1900.
Hydroelectricity
–
Turbine row at Los Nihuiles Power Station in
Mendoza, Argentina
13.
Aboriginal peoples in Canada
–
Aboriginal peoples in Canada, are the indigenous peoples within the boundaries of present-day Canada. They comprise the First Nations, Inuit and Métis, although Indian is a term still commonly used in legal documents, the descriptors Indian and Eskimo have somewhat fallen into disuse in Canada and are pejorative. Old Crow Flats and Bluefish Caves are some of the earliest known sites of habitation in Canada. The Paleo-Indian Clovis, Plano and Pre-Dorset cultures pre-date current indigenous peoples of the Americas, projectile point tools, spears, pottery, bangles, chisels and scrapers mark archaeological sites, thus distinguishing cultural periods, traditions and lithic reduction styles. The characteristics of Canadian Aboriginal culture included permanent settlements, agriculture, civic and ceremonial architecture, complex societal hierarchies, the Métis culture of mixed blood originated in the mid-17th century when First Nation and Inuit people married Europeans. The Inuit had more limited interaction with European settlers during early period. Various laws, treaties, and legislation have been enacted between European immigrants and First Nations across Canada, Aboriginal Right to Self-Government provides opportunity to manage historical, cultural, political, health care and economic control aspects within first peoples communities. National Aboriginal Day recognizes the cultures and contributions of Aboriginal peoples to the history of Canada, First Nations, Inuit and Métis peoples of all backgrounds have become prominent figures and have served as role models in the Aboriginal community and help to shape the Canadian cultural identity. The terms First Peoples and First Nations are both used to refer to peoples of Canada. The terms First Peoples or Aboriginal peoples in Canada are normally broader terms than First Nations, as they include Inuit, Métis, First Nations has come into general use for the indigenous peoples of North America in Canada, and their descendants, who are neither Inuit nor Métis. On reserves, First Nations is being supplanted by members of various nations referring to themselves by their group or ethnical identity, in conversation this would be I am Haida, or we are Kwantlens, in recognition of their First Nations ethnicities. In this Act, Aboriginal peoples of Canada includes the Indian, Inuit, Indian remains in place as the legal term used in the Canadian Constitution. Its usage outside such situations can be considered offensive, Aboriginal peoples is more commonly used to describe all indigenous peoples of Canada. It also refers to self-identification of Aboriginal people who live within Canada claiming rights of sovereignty or Aboriginal title to lands, the term Eskimo has pejorative connotations in Canada and Greenland. Indigenous peoples in those areas have replaced the term Eskimo with Inuit, the Yupik of Alaska and Siberia do not consider themselves Inuit, and ethnographers agree they are a distinct people. They prefer the terminology Yupik, Yupiit, or Eskimo, the Yupik languages are linguistically distinct from the Inuit languages. Linguistic groups of Arctic people have no universal replacement term for Eskimo, inclusive of all Inuit and Yupik people across the area inhabited by the Inuit. Besides these ethnic descriptors, Aboriginal peoples are divided into legal categories based on their relationship with the Crown
Aboriginal peoples in Canada
–
Aboriginal peoples in Canada
Aboriginal peoples in Canada
–
An aboriginal community in
Northern Ontario
Aboriginal peoples in Canada
–
A
Clovis point created using
bi-facial percussion flaking. (that is, each face is flaked on both edges alternatively with a percussor) – Image courtesy of the Virginia Dept. of Historic Resources.
Aboriginal peoples in Canada
–
Thule site (
Copper Inuit) near the waters of Cambridge Bay (
Victoria Island)
14.
Kashechewan First Nation
–
The Kashechewan First Nation is a Cree First Nation band government located near James Bay in Northern Ontario, Canada. The community is located on the shore of the Albany River. Kashechewan First Nation is one of two communities that were established from Old Fort Albany in the 1950s, the other community is Fort Albany First Nation, which is now located on the southern bank of the Albany River. The community is connected to towns along the shore of James Bay by the seasonal ice road/winter road, linking it to the towns of Attawapiskat, Fort Albany. Kashechewan is policed by the Nishnawbe-Aski Police Service, an Aboriginal-based service, a fire at the detachment on January 9,2006, severely injured an officer and killed two inmates as they could not be rescued. When the community of Kashechewan came into being, the new residents chose the name Keeshechewan, however, when the sign for the new post office arrived, it had the misspelling Kashechewan, and this became the official name of the community. This official name has no meaning in the Cree language. Kashechewan First Nation is a community of the Mushkegowuk Council. The community and Mushkegowuk Council are represented by the Nishnawbe Aski Nation, NAN is a political territorial organization that represents the 49 First Nations that are part of the Treaty No.9 area in Northern Ontario. At the provincial level, the community, tribal council and political territorial organization participate in a coordinating body. The Assembly of First Nations represents the community along with other First Nations organizations and councils, as of 2015, the elected leaders of the First Nation include Chief Leo Friday Sr and Deputy Chief Hosea Wesley. The communitys leadership consists of a chief, a deputy chief and 12 Councillors plus one elder, a mens representative, local elections are held every three years, last in August 2015. St. Andrew’s Elementary School and Francine J. Wesley Secondary School are the schools located within Kashechewan. These services provide the education for the students of the community. The schools also have a system, which has 14 members as of January 2016. Kashechewan Health Services provides services that promote physical and mental health for community members and they provide health education regarding diabetes, cancer, and other serious aliments They also offer programs that help with addiction, pregnancy, parenting, drug awareness, and crisis intervention. Northern Store is the retail store offering food and other consumer goods in town. The store is the largest building in town, Northern Store also has a location in Fort Albany to the south, without it foods need to be flown in by air
Kashechewan First Nation
–
Map showing the location of Kashechewan, Ontario.
15.
Last glacial period
–
The last glacial period, popularly known as the Ice Age, was the most recent glacial period, which occurred from c. 110,000 – c. 11,700 years ago. This most recent glacial period is part of a pattern of glacial and interglacial periods known as the Quaternary glaciation. From this point of view, scientists consider this ice age to be merely the latest glaciation event in a larger ice age. During this last glacial period, there were changes between glacier advance and retreat. The Last Glacial Maximum, the extent of glaciation within the last glacial period, was approximately 22,000 years ago. Approximately 13,000 years ago, the Late Glacial Maximum began, around 11,700 years ago marked the beginning of the Holocene geological epoch, which includes the Holocene glacial retreat. From the point of view of archaeology, it falls in the Paleolithic and Mesolithic periods. When the glaciation event started, Homo sapiens were confined to Africa and used tools comparable to those used by Neanderthals in western and central Eurasia, near the end of the event, Homo sapiens spread into Eurasia and Australia. The retreat of the glaciers allowed groups of Asians to migrate to the Americas, glacials, on the other hand, refer to colder phases within an ice age that separate interglacials. Thus, the end of the last glacial period is not the end of the last ice age, the end of the last glacial period was about 11,700 years ago, while the end of the last ice age has not yet come. Over the past few years the glacial-interglacial cycle has been paced by periodic variations in the Earths orbit via Milankovitch cycles which are thus the cause of ice ages. The glaciations that occurred during this period covered many areas, mainly in the Northern Hemisphere. The geochronological Late Pleistocene comprises the late glacial and the immediately preceding penultimate interglacial preiond, the last glaciation centered on the huge ice sheets of North America and Eurasia. Considerable areas in the Alps, the Himalaya and the Andes were ice-covered, Canada was nearly completely covered by ice, as well as the northern part of the United States, both blanketed by the huge Laurentide ice sheet. Alaska remained mostly ice free due to climate conditions. Local glaciations existed in the Rocky Mountains and the Cordilleran ice sheet and as ice fields, the maximum extent of western Siberian glaciation was reached by approximately 16, 000–15,000 BCE and thus later than in Europe. Northeastern Siberia was not covered by an ice sheet. Instead, large, but restricted, icefield complexes covered mountain ranges within northeast Siberia, according to the sediment composition retrieved from deep-sea cores there must even have been times of seasonally open waters
Last glacial period
–
An artist's impression of the last glacial period at glacial maximum.
Last glacial period
–
Chronology of climatic events of importance for the Last Glacial Period (about the last 120 000 years)
Last glacial period
–
Map showing the extent of the
Patagonian Ice Sheet in the
Strait of Magellan area during the last glacial period. Selected modern settlements are shown with yellow dots.
16.
Cree
–
The Cree are one of the largest groups of First Nations in North America, with over 200,000 members living in Canada. The major proportion of Cree in Canada live north and west of Lake Superior, in Ontario, Manitoba, Saskatchewan, Alberta, in the United States, this Algonquian-speaking people historically lived from Lake Superior westward. Today, they live mostly in Montana, where they share a reservation with the Ojibwe, the documented westward migration over time has been strongly associated with their roles as traders and hunters in the North American fur trade. The Cree are generally divided into eight groups based on dialect and these divisions do not necessarily represent ethnic sub-divisions within the larger ethnic group, Naskapi and Montagnais are inhabitants of an area they refer to as Nitassinan. Their territories comprise most of the political jurisdictions of eastern Quebec. Their cultures are differentiated, as the Naskapi are still caribou hunters and more nomadic than the Montagnais, the total population of the two groups in 2003 was about 18,000 people, of which 15,000 lived in Quebec. Their dialects and languages are the most distinct from the Cree spoken by the groups west of Lake Superior, Attikamekw are inhabitants of the area they refer to as Nitaskinan, in the upper St. Maurice River valley of Quebec. James Bay Cree – Grand Council of the Crees, approximately 18,000 Cree of Eeyou Istchee and Nunavik regions of Northern Quebec. Moose Cree – Moose Factory in the Cochrane District, Ontario, Swampy Cree – this group lives in northern Manitoba along the Hudson Bay coast and adjacent inland areas to the south and west, and in Ontario along the coast of Hudson Bay and James Bay. Some also in eastern Saskatchewan around Cumberland House, Woods Cree group in northern Alberta and Saskatchewan. Plains Cree 34,000 people in Manitoba, Saskatchewan, Alberta, due to the many dialects of the Cree language, there is no modern collective autonym. The Plains Cree and Attikamekw refer to using modern forms of the historical nêhiraw, namely nêhiyaw and nêhirawisiw. Moose Cree, East Cree, Naskapi, and Montagnais all refer to using modern dialectal forms of the historical iriniw. Moose Cree use the form ililiw, coastal East Cree and Naskapi use iyiyiw, inland East Cree use iyiniw, the Cree use Cree, cri, Naskapi, or montagnais to refer to their people only when speaking the languages of the European colonists, French or English. Bands would usually have strong ties to their neighbours through intermarriage and would assemble together at different parts of the year to hunt and socialize together. Besides these regional gatherings, there was no formal structure. Each band remained independent of each other, however, Cree-speaking bands tended to work together and with their neighbours against outside enemies. When a band went to war, they would nominate a temporary military commander and this office was different from that of the peace chief, a leader who had a role more like that of diplomat
Cree
–
Nēhiyaw camp near
Vermilion, Alberta, in 1871
Cree
–
Cree Indian, taken by G. E. Fleming, 1903
Cree
–
Nehiyaw girl (1928).
Cree
–
"Group of Crees"
17.
Henry Hudson
–
Henry Hudson, born circa 1565-1570, dead 1611, was an English sea explorer and navigator in the early 17th century. Hudson made two attempts on behalf of English merchants to find a prospective Northwest Passage to Cathay via a route above the Arctic Circle. Hudson explored the region around modern New York metropolitan area while looking for a route to Asia while in the employment of the Dutch East India Company. He explored the Hudson River, and laid thereby the foundation for Dutch colonization of the region, Hudson discovered the Hudson Strait and the immense Hudson Bay on his final expedition. While searching for the Northwest Passage, Hudson and his son would lose their lives. In 1611, after wintering on the shore of James Bay, Hudson wanted to press on to the west, the mutineers cast Hudson, his son and seven others adrift, the Hudsons, and those cast off at their side, were never seen again. His name also lives on with the Hudsons Bay Company that explored and worked in the vast Hudson Bay watershed and this large company, and one of the longest lasting, was very successful with fur trading all across North America. Canada acquired a portion of land from the purchase of Hudsons Bay Company lands. Details of Hudsons birth and early life are mostly unknown, some sources have identified Hudson as having been born in about 1565, but others date his birth to around 1570. Other historians assert even less certainty, Mancall, for instance, states that was born in the 1560s. Hudson is thought to have spent many years at sea, beginning as a cabin boy, in 1607, the Muscovy Company of England hired Hudson to find a northerly route to the Pacific coast of Asia. The English were battling the Dutch for northwest routes and it was thought at the time that, because the sun shone for three months in the northern latitudes in the summer, the ice would melt and a ship could make it across the top of the world. Hudson sailed on 1 May with a crew of ten men and they reached the east coast of Greenland on 14 June, coasting it northward until the 22nd. Here they named a headland Youngs Cape, a high mount, like a round castle near it Mount of Gods Mercy. After turning east, they sighted Newland on the 27th, near the mouth of the great bay Hudson later simply named the Great Indraught. On 13 July Hudson and his crew thought they had sailed as far north as 80°23 N, the following day they entered what Hudson later in the voyage named Whales Bay, naming its northwestern point Collins Cape after his boatswain, William Collins. They sailed north the following two days, on the 16th they reached as far north as Hakluyts Headland at 79°49 N, thinking they saw the land continue to 82° N when really it trended to the east. Encountering ice packed along the north coast, they were forced to turn back south, Hudson wanted to make his return by the north of Greenland to Davis his Streights, and so for Kingdom of England, but ice conditions would have made this impossible
Henry Hudson
–
This speculative portrait from Cyclopedia of Universal History is one of several used to represent Henry Hudson.
Henry Hudson
–
Replica of
Henry Hudson's ship Halve Maen, donated in 1909 by the Dutch to the United States on the occasion of the 300-year anniversary of the discovery of what is now New York.
Henry Hudson
–
A map of Hudson's fourth voyage
Henry Hudson
–
John Collier 's painting of Henry Hudson with his son and some crew members after a mutiny on his icebound ship. The boat was set adrift and never heard from again.
18.
Captain (nautical)
–
A sea captain is a high-grade licensed mariner in ultimate command of the merchant vessel. A ships captain commands and manages all ships personnel, and is typically in charge of the accounting, payrolls. The captain is responsible for responding to and reporting in case of accidents and incidents, the captain ensures that the ship complies with local and international laws and complies also with company policies. One of a particularly important duties is to ensure compliance with the vessels security plan. The security plan also covers such as refugees and asylum seekers, smuggling. On ships without a purser, the captain is in charge of the ships accounting and this includes ensuring an adequate amount of cash on board, coordinating the ships payroll, and managing the ships slop chest. On international voyages, the captain is responsible for satisfying requirements of the local immigration, customs requirements can include the master providing a cargo declaration, a ships stores declaration, a declaration of crewmembers personal effects, crew lists and passenger lists. The master acts as a liaison to local investigators and is responsible for providing complete and accurate logbooks, reports, statements, specific examples of the ship causing external damage include collisions with other ships or with fixed objects, grounding the vessel, and dragging anchor. Some common causes of damage include heavy weather, water damage, pilferage. There is a belief that ship captains have historically been. In most countries of ships registry, ship captains are not, the United States Navy defined a captain’s powers in its 1913 Code of Regulations, specifically stating, The commanding officer shall not perform a marriage ceremony on board his ship or aircraft. New Jerseys 1919 Bolmer v. Edsall said a shipboard marriage ceremony is governed by the laws of the nation where ownership of the vessel lies. In the United Kingdom, the captain of a merchant ship has never permitted to perform marriages. In other countries of ships registry, the situation varies. Most do not permit performance of a marriage by the master of a ship at sea, japan allows ship captains to perform a marriage ceremony at sea, but only for Japanese citizens. Malta and Bermuda permit captains of ships registered in their jurisdictions to perform marriages at sea, princess Cruises, whose ships are registered in Bermuda, has used this as a selling point for their cruises since 1998. In 2011, Cunard announced its intention to move the registration of “Queen Mary 2″, “Queen Victoria” and “Queen Elizabeth” from Southampton, in the United Kingdom, to Bermuda. Some captains obtain other credentials, which allow them to perform marriages in jurisdictions where they would otherwise not be permitted to do so
Captain (nautical)
–
The master works with the
harbour pilot, the
chief mate and an
able seaman during inner navigation aboard the vessel
Kristina Regina.
Captain (nautical)
–
A ship's captain must have a number of qualifications, including a license.
19.
History of Canada
–
The history of Canada covers the period from the arrival of Paleo-Indians thousands of years ago to the present day. Some of these civilizations had long faded by the time of the first European arrivals and have discovered through archaeological investigations. Starting in the late 15th century, French and British expeditions explored, colonized, the colony of New France was established in 1534 and was ceded to the United Kingdom in 1763 after the French defeat in the Seven Years War. The now British Province of Quebec was divided into Upper and Lower Canada in 1791, in 1867, the Province of Canada was joined with two other British colonies of New Brunswick and Nova Scotia through Confederation, forming a self-governing entity named Canada. The new dominion expanded by incorporating parts of British North America, finishing with Newfoundland. Although responsible government had existed in Canada since 1848, Britain continued to set its foreign, with the passing of the Statute of Westminster in 1931, Canada became co-equal with the United Kingdom. After the Constitution was repatriated in 1982, the vestiges of legal dependence on the British parliament were removed. Canada currently consists of ten provinces and three territories and is a democracy and a constitutional monarchy with Queen Elizabeth II as its head of state. Since the conclusion of the Second World War, Canadians have supported multilateralism abroad, archeological and Aboriginal genetic evidence indicate that North and South America were the last continents into which humans migrated. During the Wisconsin glaciation,50, 000–17,000 years ago, falling sea levels allowed people to move across the Bering land bridge, from Siberia into northwest North America. At that point, they were blocked by the Laurentide ice sheet covered most of Canada, confining them to Alaska. The exact dates and routes of the peopling of the Americas are the subject of an ongoing debate, by 16,000 years ago the glacial melt allowed people to move by land south and east out of Beringia, and into Canada. The Queen Charlotte Islands, Old Crow Flats, and Bluefish Caves contain some of the earliest Paleo-Indian archaeological sites in Canada, ice Age hunter-gatherers of this period left lithic flake fluted stone tools and the remains of large butchered mammals. The North American climate stabilized around 8000 BCE, climatic conditions were similar to modern patterns, however, the receding glacial ice sheets still covered large portions of the land, creating lakes of meltwater. Most population groups during the Archaic periods were still highly mobile hunter-gatherers, however, individual groups started to focus on resources available to them locally, thus with the passage of time, there is a pattern of increasing regional generalization. The Woodland cultural period dates from about 2000 BCE to 1000 CE and includes the Ontario, Quebec, the introduction of pottery distinguishes the Woodland culture from the previous Archaic-stage inhabitants. The Laurentian-related people of Ontario manufactured the oldest pottery excavated to date in Canada, the Hopewell tradition is an Aboriginal culture that flourished along American rivers from 300 BCE to 500 CE. At its greatest extent, the Hopewell Exchange System connected cultures and societies to the peoples on the Canadian shores of Lake Ontario, Canadian expression of the Hopewellian peoples encompasses the Point Peninsula, Saugeen, and Laurel complexes
History of Canada
–
The
Great Lakes are estimated to have been formed at the end of the
last glacial period (about 10,000 years ago), when the
Laurentide ice sheet receded.
History of Canada
–
PP
History of Canada
–
L'Anse aux Meadows on the island of Newfoundland, site of a
Norsemen colony.
History of Canada
–
Replica of Port Royal habitation, located at the
Port-Royal National Historic Site of Canada, Nova Scotia.
20.
Canada under British Imperial control (1764-1867)
–
Canada first came under British rule with the Treaty of Paris which ceded New France, of which Canada was a part, to the British Empire. Gradually, other territories, colonies, and provinces that were part of British North America would be added to Canada. The Royal Proclamation of 1763 enlarged the colony of Canada under the name of the Province of Quebec, with the Act of Union 1840 Upper and Lower Canada were joined to become the United Province of Canada. A number of other British colonies, such as Newfoundland and British Columbia, in North America, the Seven Years War officially ended with the signing of the Treaty of Paris on February 10,1763. As part of the treaty, France ceded all North American lands to Britain, except Louisiana, the Quebec Act became one of the Intolerable Acts that infuriated the thirteen British colonies in what would become the United States of America. In Acadia, the British had expelled French-speaking populations in 1755 from Acadia to Louisiana, creating the Cajun population, in the former French territory of Acadia, the British were confronted by a relatively large and well-established Catholic Mikmaq and Wabanaki Confederacy. The British Conquest of Acadia happened in 1710, much earlier than in what would become the rest of modern-day Canada, the Mikmaq never ceded land to either France or England. The first immigration of Protestants happened in the province with the founding of Halifax, the establishment of Halifax sparked Father Le Loutres War, which, in turn, led to the British expelling the Acadians from the region during the French and Indian War. As they later captured Cape Breton Island and Prince Edward Island, the few Acadians who managed to return to the area have created the contemporary Acadian society. Once the land was emptied, other settlements were formed by New England Planters, in 1775, American revolutionaries attempted to push their insurrection into Quebec. The habitants were divided, in areas, there was significant support. The Patriots laid siege to Fort Saint-Jean, capturing it and Montreal in November 1775 and they then marched on Quebec City, where an attempt to take the city on December 31,1775, failed. Following an ineffectual siege, the arrival of British troops in May 1776 sent the Patriots into retreat back toward Montreal, an attempt against British troops at Trois-Rivières failed, and the Patriots were driven from the province in June. Leaving with the army were about 250 Québécois in two regiments, James Livingstons 1st Canadian Regiment, and Moses Hazens 2nd Canadian Regiment. Quebeckers living in the forts of the Great Lakes region also massively sided with the Patriots and were instrumental in the taking of the fort by the Patriots. The only major event of their resistance was the Battle of Fort Cumberland, when Eddy and a force of Massachusetts Patriots, Acadians. The siege was broken and Eddys forces were scattered when British reinforcements arrived, Eddy and Allan continued to make trouble on the frontier between what are now Maine and New Brunswick from a base in Machias for several years. The Maritime provinces were affected by privateering, and raids on settlements by privateers in violation of their letters of marque
Canada under British Imperial control (1764-1867)
–
Loyalist Laura Secord warns British of an impending American attack at
Beaver Dams.
Canada under British Imperial control (1764-1867)
–
Map showing British territorial gains following the Treaty of Paris in pink, and Spanish territorial gains after the
Treaty of Fontainebleau in yellow.
Canada under British Imperial control (1764-1867)
–
Timber booms on the
Ottawa River, Canada, 1872.
Canada under British Imperial control (1764-1867)
–
The Papineau Rebellion of 1837.
21.
Pierre-Esprit Radisson
–
Pierre-Esprit Radisson was a French fur trader and explorer. He is often linked to his brother-in-law Médard des Groseilliers, the decision of Radisson and Groseilliers to enter the English service led to the formation of the Hudsons Bay Company. His career was notable for its repeated transitions between serving Britain and France. An affidavit from 1697 and a petition from 1698 contain statements from Radisson himself indicating that he was 61 and 62 years old respectively, which would place his year of birth at 1636. However, a 1681 census of New France indicated that he was, at the time,41 years old, in Radissons own writings, he claims that his family, the Hayet-Radissons, originally stemmed from the town of St. Malo. However, records seem to suggest that his family more likely came from either Paris or Avignon, baptismal Records from Carpentras, a city near Avignon, concerning Radissons father provide evidence in support of the latter option. As Radisson himself describes in his writings, he immigrated from France to Canada on the 24th of May, information regarding Radissons arrival in New France is scarce, but it is theorized that he arrived with, or as a result of, his half-sister Marguerite Hayet. It is also unknown whether or not he arrived alongside other members of his family, namely his two sisters Élisabeth and Françoise. According to Radissons account, in the year he had been hunting fowl with several other men near his home in Trois-Rivières when he was captured by the Iroquois. Initially a petty squabble had separated him from his friends and by the time he had found them and this assimilation was the custom for the Mohawk, who often replaced people lost to disease and warfare and adopted young captives from other tribes and European nations. After approximately six weeks of gradual integration, Radissons assimilation and partial adoption of Iroquois nationality was largely solidified, however, shortly thereafter, while out hunting with three Iroquois, Radisson reluctantly agreed to attempt escape after meeting an Algonquin man who offered to help him return to Trois-Rivières. Eventually he was released, and, overwhelmed with relief, described the experience as a moment in all my paines and griefs ceased. Bids me be merry, makes me sing, to wich I consented with all my heart, afterwards, following the healing of his torture wounds and a subsequent 5 months war-party expedition, Radisson departed for a trading trip, alongside other Mohawk warriors, at Fort Orange. Upon arriving at Fort Orange, then controlled by the Dutch, he was recognized as a Frenchman and offered freedom by the local governor, who was willing to pay his ransom. Radisson initially refused but, after returning to the Iroquois village, later regretted the decision, returning to Fort Orange once more, he met a Jesuit Priest, Joseph Antoine Poncet, who made him a great offer. Radisson never elaborates on what that offer other than the fact that it required him to return to Holland in early 1654. He returned to Trois-Rivières later that year and, over the three years, embarked on several missionary expeditions. The expedition ended in 1658 after rising tensions with local Iroquois caused the French to flee rather abruptly, Radisson returned to Quebec soon thereafter
Pierre-Esprit Radisson
–
Pierre-Esprit Radisson
Pierre-Esprit Radisson
–
Arrival of Radisson in an Indian camp in 1660.
22.
Prince Rupert of the Rhine
–
Rupert was a younger son of the German prince Frederick V, Elector Palatine and his wife Elizabeth, the eldest daughter of James I of England. Thus Rupert was the nephew of King Charles I of England, who made him Duke of Cumberland and Earl of Holderness, and his sister Electress Sophia was the mother of George I of Great Britain. Prince Rupert had a varied career and he was a soldier from a young age, fighting against Spain in the Netherlands during the Eighty Years War, and against the Holy Roman Emperor in Germany during the Thirty Years War. Aged 23, he was appointed commander of the Royalist cavalry during the English Civil War, becoming the archetypal Cavalier of the war and he surrendered after the fall of Bristol and was banished from England. He served under Louis XIV of France against Spain, and then as a Royalist privateer in the Caribbean, Rupert died in England in 1682, aged 62. Rupert is considered to have been a quick-thinking and energetic cavalry general, in the Interregnum, Rupert continued the conflict against Parliament by sea from the Mediterranean to the Caribbean, showing considerable persistence in the face of adversity. As the head of the Royal Navy in his years, he showed greater maturity and made impressive and long-lasting contributions to the Royal Navys doctrine. As a colonial governor, Rupert shaped the geography of modern Canada—Ruperts Land was named in his honour. He also played a role in the early African slave trade, Ruperts varied and numerous scientific and administrative interests combined with his considerable artistic skills made him one of the more colourful individuals of the Restoration period. Rupert was born in Prague in 1619, at the start of the Thirty Years War, to Frederick V, Elector Palatine, and Elizabeth Stuart and he was given his name in honour of King Rupert of Germany, a famous Wittelsbach ancestor. Ruperts father was a member of the Holy Roman Empire. This support was not forthcoming, resulting in a defeat at the hands of his Catholic enemies at the Battle of White Mountain in 1620. Ruperts parents were mockingly termed the Winter King and Queen as a consequence of their reigns in Bohemia having lasted only a single season. Rupert was almost left behind in the rush to escape Ferdinands advance on Prague, until Kryštof z Donína. Rupert accompanied his parents to The Hague, where he spent his years at the Hof te Wassenaer. Ruperts mother paid her children little attention even by the standards of the day, apparently preferring her pet monkeys, the result was a strict school routine including logic, mathematics, writing, drawing, singing and playing instruments. As a child, Rupert was at times badly behaved, fiery, mischievous, nonetheless, Rupert proved to be an able student. By the age of three he could speak some English, Czech and French, and mastered German while still young and he excelled in art, being taught by Gerard van Honthorst, and found the maths and sciences easy
Prince Rupert of the Rhine
–
Prince Rupert portrayed in Roman garb
Prince Rupert of the Rhine
–
Charles I Louis, Elector Palatine (left), and Rupert (right), in a 1637 portrait by
Anthony van Dyck
Prince Rupert of the Rhine
–
Rupert as a young man visiting his uncle,
King Charles I 's court in England, by Anthony van Dyck
Prince Rupert of the Rhine
–
Charles I holding a
council of war at
Edgecote on the day before the
Battle of Edgehill; Rupert, who would command the King's
cavalry during the battle, is seated at the table
23.
Charles I of England
–
Charles I was monarch of the three kingdoms of England, Scotland, and Ireland from 27 March 1625 until his execution in 1649. Charles was the son of King James VI of Scotland, but after his father inherited the English throne in 1603, he moved to England. He became heir apparent to the English, Irish, and Scottish thrones on the death of his brother, Henry Frederick, Prince of Wales. Two years later, he married the Bourbon princess Henrietta Maria of France instead, after his succession, Charles quarrelled with the Parliament of England, which sought to curb his royal prerogative. Charles believed in the right of kings and thought he could govern according to his own conscience. Many of his subjects opposed his policies, in particular the levying of taxes without parliamentary consent and he supported high church ecclesiastics, such as Richard Montagu and William Laud, and failed to aid Protestant forces successfully during the Thirty Years War. From 1642, Charles fought the armies of the English and Scottish parliaments in the English Civil War, after his defeat in 1645, he surrendered to a Scottish force that eventually handed him over to the English Parliament. Charles refused to accept his captors demands for a constitutional monarchy, re-imprisoned on the Isle of Wight, Charles forged an alliance with Scotland, but by the end of 1648 Oliver Cromwells New Model Army had consolidated its control over England. Charles was tried, convicted, and executed for treason in January 1649. The monarchy was abolished and a called the Commonwealth of England was declared. The monarchy was restored to Charless son, Charles II, in 1660, the second son of King James VI of Scotland and Anne of Denmark, Charles was born in Dunfermline Palace, Fife, on 19 November 1600. James VI was the first cousin twice removed of Queen Elizabeth I of England, in mid-July 1604, Charles left Dunfermline for England where he was to spend most of the rest of his life. His speech development was slow, and he retained a stammer, or hesitant speech. In January 1605, Charles was created Duke of York, as is customary in the case of the English sovereigns second son, Thomas Murray, a Presbyterian Scot, was appointed as a tutor. Charles learnt the usual subjects of classics, languages, mathematics, in 1611, he was made a Knight of the Garter. Eventually, Charles apparently conquered his physical infirmity, which might have been caused by rickets and he became an adept horseman and marksman, and took up fencing. Even so, his public profile remained low in contrast to that of his stronger and taller elder brother, Henry Frederick, Prince of Wales. However, in early November 1612, Henry died at the age of 18 of what is suspected to have been typhoid, Charles, who turned 12 two weeks later, became heir apparent
Charles I of England
–
Portrait from the studio of
Anthony van Dyck, 1636
Charles I of England
–
Engraving by
Simon de Passe of Charles and his parents, King James and Queen Anne, c. 1612
Charles I of England
–
Portrait by
Robert Peake, c. 1610
Charles I of England
–
Portrait of Charles as Prince of Wales after
Daniel Mytens, c. 1623
24.
Charles II of England
–
Charles II was king of England, Scotland and Ireland. He was king of Scotland from 1649 until his deposition in 1651, Charles IIs father, Charles I, was executed at Whitehall on 30 January 1649, at the climax of the English Civil War. Cromwell defeated Charles II at the Battle of Worcester on 3 September 1651, Cromwell became virtual dictator of England, Scotland and Ireland, and Charles spent the next nine years in exile in France, the Dutch Republic and the Spanish Netherlands. A political crisis followed the death of Cromwell in 1658 resulted in the restoration of the monarchy. On 29 May 1660, his 30th birthday, he was received in London to public acclaim, after 1660, all legal documents were dated as if he had succeeded his father as king in 1649. Charless English parliament enacted laws known as the Clarendon Code, designed to shore up the position of the re-established Church of England, Charles acquiesced to the Clarendon Code even though he favoured a policy of religious tolerance. The major foreign policy issue of his reign was the Second Anglo-Dutch War. In 1670, he entered into the treaty of Dover. Louis agreed to aid him in the Third Anglo-Dutch War and pay him a pension, Charles attempted to introduce religious freedom for Catholics and Protestant dissenters with his 1672 Royal Declaration of Indulgence, but the English Parliament forced him to withdraw it. In 1679, Titus Oatess revelations of a supposed Popish Plot sparked the Exclusion Crisis when it was revealed that Charless brother, the crisis saw the birth of the pro-exclusion Whig and anti-exclusion Tory parties. Charles sided with the Tories, and, following the discovery of the Rye House Plot to murder Charles and James in 1683, Charles dissolved the English Parliament in 1681, and ruled alone until his death on 6 February 1685. He was received into the Roman Catholic Church on his deathbed, Charless wife, Catherine of Braganza, bore no live children, but Charles acknowledged at least twelve illegitimate children by various mistresses. He was succeeded by his brother James, Charles II was born in St Jamess Palace on 29 May 1630. His parents were Charles I and Henrietta Maria, Charles was their second son and child. Their first son was born about a year before Charles but died within a day, England, Scotland and Ireland were respectively predominantly Anglican, Presbyterian and Roman Catholic. At birth, Charles automatically became Duke of Cornwall and Duke of Rothesay, at or around his eighth birthday, he was designated Prince of Wales, though he was never formally invested. During the 1640s, when Charles was still young, his father fought Parliamentary, by spring 1646, his father was losing the war, and Charles left England due to fears for his safety. Charles I surrendered into captivity in May 1646, at The Hague, Charles had a brief affair with Lucy Walter, who later falsely claimed that they had secretly married
Charles II of England
–
Charles II in the robes of the
Order of the Garter, by
John Michael Wright or studio, c. 1660–1665
Charles II of England
–
Charles II as an infant in 1630, painting attributed to
Justus van Egmont
Charles II of England
–
Portrait by
William Dobson, c. 1642 or 1643
Charles II of England
–
"The Scots Holding Their Young King's Nose To the Grindstone", from a satirical English pamphlet
25.
Northern Canada
–
Northern Canada, colloquially the North, is the vast northernmost region of Canada variously defined by geography and politics. Politically, the term refers to three territories of Canada, Yukon, Northwest Territories, and Nunavut, similarly, the Far North may refer to the Canadian Arctic, the portion of Canada north of the Arctic Circle and lies east of Alaska and west of Greenland. This area covers about 39 percent of Canadas total land area, for some purposes, Northern Canada may also include Northern Quebec and Northern Labrador. These reckonings somewhat depend on the concept of nordicity, a measure of so-called northernness that other Arctic territories share. Canada is the northernmost country in the Americas and roughly 80% of its 35 million inhabitants are concentrated along its border with the United States. Combined with the fact that all of the country experiences severely cold winters along with short and relatively cool summers. Due to the concentration of its population along the border. Southern Canada is therefore considered to be a region only when it is contrasted against or viewed from the North, as a social rather than political region, the Canadian north is often subdivided into two distinct regions based on climate, the near north and the far north. The different climates of these two regions result in different vegetation, and therefore very different economies, settlement patterns. The near north or subarctic is mostly synonymous with the Canadian boreal forest and this area has traditionally been home to the Indigenous peoples of the Subarctic, that is the First Nations, who were hunters of moose, freshwater fishers and trappers. This region was involved in the North American fur trade during its peak importance. The area was part of Ruperts Land or the North-Western Territory under the nominal control of the Hudsons Bay Company from 1670–1869. The HBCs claim was purchased by the Canadian government in 1869 and this opened the region to non-Native settlement, as well as to forestry, mining, and oil and gas drilling. Today several million people live in the north, around 15% of the Canadian total. The far north is synonymous with the north of the tree line. This area is home to the various sub-groups of the Inuit and these are people who have traditionally relied mostly on hunting marine mammals and caribou, mainly barren-ground caribou, as well as fish and migratory birds. This area was somewhat involved in the fur trade, but was influenced by the whaling industry. Very few non-Aboriginal people have settled in areas, and the residents of the far north represent less than 1% of Canadas total population
Northern Canada
–
A
boreal forest landscape in
Northern Quebec.
Northern Canada
–
Northern Canada, defined politically to comprise (from west to east)
Yukon,
Northwest Territories, and
Nunavut.
Northern Canada
–
A typical
tundra landscape in
Nunavut.
Northern Canada
–
The western Canadian Arctic early June 2010.
26.
Ketch
–
A ketch is a sailing craft with two masts. The distinguishing characteristic of a ketch is that the forward of the two masts is larger than the after mast, historically the ketch was a square-rigged vessel, most commonly used as a freighter or fishing boat in northern Europe, particularly in the Baltic and North seas. In modern usage, the ketch is a rigged vessel used as a yacht or pleasure craft. To assist going to windward, a ketch may carry one or more jibs or foresails, if a ketch has no jibs, it is called a cat ketch or a periauger. On older, larger ketches the main mast may in addition one or more square rigged topsails. The large fore-and-aft sail on the mainmast is the mainsail, while the sail on the mizzen mast is the mizzen and these sails may be any type of fore-and-aft sail, in any combination. Most modern ketches are Bermuda rigged, but other possible rigs on a ketch include gunter rigs, the Scots Zulu, for example, had a dipping lug main with a standing lug mizzen. In northern Europe and among long distance cruisers, the ketch is often preferred to a sloop, since the additional sail allows a balance. An advantage of the ketch is when sudden increases in wind strength require a rapid reefing, the ketch rig also allows sailing only on the mizzen and jib, without introducing excessive lee helm, and in an emergency can be quite well steered without use of the rudder. When running before the wind or reaching across the wind, a ketch may set extra sails such as a spinnaker on the main mast, and a spinnaker or mizzen staysail on the mizzen mast. Another advantage of a ketch is at anchor, where the sail may be used to hold the boat steady in the wind. The square-rigged ketch was largely supplanted by the brig, which differs from the ketch by having a forward mast smaller than the after mast, and by the hoy, other similar craft include the snow and the pink. But the balance of sail area can be an overriding characteristic, if 20% or more of the sail area is in the mizzen sail the rig would be termed a ketch. This is particularly true on center cockpit yachts, compared to a ketch, a similar size yawls mizzen sail is much smaller than the main, because of the limitations of the mizzen sheet. So on a ketch, the purpose of the mizzen sail is to both propel and balance the vessel, while on a yawl, the smaller mizzen mainly serves the purpose of trim or balance. Yawls tend to have mainsails almost as large as those of comparable sloops, a ketch may be distinguished from a cutter or a sloop by virtue of having two masts rather than one, though a ketch with two foresails is sometimes called a cutter-rigged ketch. Both the ketch and the yawl differ from the two-masted schooner, if a vessel has two masts of approximately the same height, the rig with the larger sail forward is called a ketch, while the rig with the larger sail aft is a schooner. The American two-masted schooner is rare in Europe, where the rig is preferred
Ketch
–
2013 Ahmanson Cup Regatta yacht Zapata II Classic Calkins Ketch sailing, hard on the wind with the mizzen furled on the rear boom
Ketch
–
Square-rigged ketch
Ketch
–
A double-gaff ketch with a Bermuda-rigged main topsail and a lug-rigged mizzen topsail
27.
List of Hudson Bay rivers
–
This list of Hudson Bay rivers includes the principal rivers draining into the Hudson, James and Ungava bays of the Arctic Ocean. The total surface area of the Hudson Bay watershed is about 3,861,400 square kilometres, the drainage basin includes parts of five Canadian provinces, territories and four American states. The two principal waterways are the La Grande Rivière, in Québec, and the Nelson River in Manitoba, the rivers are presented by coastline, clockwise, starting with the George River in northeastern Quebec, just south of Cape Chidley and the entrance to the Atlantic Ocean. Characteristics and Trends of River Discharge into Hudson, James and Ungava Bays, 1964-2000, Journal of Climate,18, pages 2540-2557
List of Hudson Bay rivers
–
BC
28.
Religious Society of Friends
–
Quakers are members of a historically Christian group of religious movements generally known as the Religious Society of Friends. They include those with evangelical, holiness, liberal, and traditional Quaker understandings of Christianity, to differing extents, the different movements that make up the Religious Society of Friends/Friends Church avoid creeds and hierarchical structures. In 2007, there were about 359,000 adult Quakers, in 2012, there were 377,055 adult Quakers. Some meetings of both types have Recorded Ministers in their meetings—Friends recognised for their gift of vocal ministry, the first Quakers lived in mid-17th century England. The movement arose from the Legatine-Arians and other dissenting Protestant groups, some of these early Quaker ministers were women. They emphasized a personal and direct experience of Christ, acquired through both direct religious experience and the reading and studying of the Bible. Quakers focused their private life on developing behaviour and speech reflecting emotional purity, in the past, Quakers were known for their use of thee as an ordinary pronoun, refusal to participate in war, plain dress, refusal to swear oaths, opposition to slavery, and teetotalism. & J. Clark and the big three British confectionery makers Cadbury, Rowntree and Frys, and philanthropic efforts, including abolition of slavery, prison reform, during and after the English Civil War many dissenting Christian groups emerged, including the Seekers and others. A young man named George Fox was dissatisfied with the teachings of the Church of England and he had a vision on Pendle Hill in Lancashire, England, in which he believed that the Lord let me see in what places he had a great people to be gathered. Following this he travelled around England, the Netherlands, and Barbados preaching and teaching with the aim of converting new adherents to his faith, the central theme of his Gospel message was that Christ has come to teach his people himself. His followers considered themselves to be the restoration of the true Christian church, in 1650, Fox was brought before the magistrates Gervase Bennet and Nathaniel Barton, on a charge of religious blasphemy. According to George Foxs autobiography, Bennet was the first that called us Quakers and it is thought that George Fox was referring to Isaiah 66,2 or Ezra 9,4. Thus, the name Quaker began as a way of ridiculing George Foxs admonition, Quakerism gained a considerable following in England and Wales, and the numbers increased to a peak of 60,000 in England and Wales by 1680. This was relaxed after the Declaration of Indulgence and stopped under the Act of Toleration 1689, with the restructuring of the family and household came new roles for women, Fox and Fell viewed the Quaker mother as essential to developing holy conversation in her children and husband. Quaker women were responsible for the spirituality of the larger community, coming together in meetings that regulated marriage. The persecution of Quakers in North America began in 1656 when English Quaker missionaries Mary Fisher and they were considered heretics because of their insistence on individual obedience to the Inner Light. They were imprisoned and banished by the Massachusetts Bay Colony and their books were burned, and most of their property was confiscated. They were imprisoned in terrible conditions, then deported, in 1660, English Quaker Mary Dyer was hanged on Boston Common for repeatedly defying a Puritan law banning Quakers from the colony
Religious Society of Friends
–
Heritage-listed Quaker meeting house,
Sydney,
Australia
Religious Society of Friends
–
Symbol used by Friends' service organizations since the late 19th century
Religious Society of Friends
–
James Nayler, a prominent Quaker leader, being pilloried and whipped
Religious Society of Friends
–
William Penn, the founder of Pennsylvania, as a young man
29.
First Nations
–
The First Nations are the predominant Aboriginal peoples of Canada south of the Arctic. Those in the Arctic area are distinct and known as Inuit, the Métis, another distinct ethnicity, developed after European contact and relations primarily between First Nations people and Europeans. There are currently 634 recognized First Nations governments or bands spread across Canada, roughly half of which are in the provinces of Ontario and British Columbia. Under the Employment Equity Act, First Nations are a group, along with women, visible minorities. First Nations are not defined as a minority under the Act or by the criteria of Statistics Canada. Within Canada, First Nations has come into general use—replacing the deprecated term Indians—for the indigenous peoples of the Americas, individuals using the term outside Canada include supporters of the Cascadian independence movement, as well as U. S. tribes within the Pacific Northwest. The singular, commonly used on culturally politicized reserves, is the term First Nations person, North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700, written records began with the arrival of European explorers and colonists during the Age of Discovery, beginning in the late 15th century. European accounts by trappers, traders, explorers, and missionaries give important evidence of early contact culture, in addition, archeological and anthropological research, as well as linguistics, have helped scholars piece together understanding of ancient cultures and historic peoples. Combined with later development, this relatively non-combative history has allowed First Nations peoples to have an influence on the national culture. Collectively, First Nations, Inuit, and Métis peoples constitute Aboriginal peoples in Canada, Indigenous peoples of the Americas, First Nations came into common usage in the 1980s to replace the term Indian band in referring to groups of Indians with common government and language. Elder Sol Sanderson says that he coined the term in the early 1980s, others say that the term came into common usage in the 1970s to avoid using the word Indian, which some Canadians considered offensive. No legal definition of the term exists, some Aboriginal peoples in Canada have also adopted the term First Nation to replace the word band in the formal name of their community. While the word Indian is still a term, its use is erratic. Some First Nations people consider the term offensive, while others prefer it to Aboriginal person/persons/people, the term is a misnomer given to indigenous peoples of North America by European explorers who erroneously thought they had landed on the Indian subcontinent. The use of the term Native Americans, which the United States government and it refers more specifically to the Aboriginal peoples residing within the boundaries of the United States. The parallel term Native Canadian is not commonly used, but Natives and autochthones are, under the Royal Proclamation of 1763, also known as the Indian Magna Carta, the Crown referred to indigenous peoples in British territory as tribes or nations. The term First Nations is capitalized, unlike alternative terms, bands and nations may have slightly different meanings
First Nations
First Nations
–
Squamish woman
First Nations
First Nations
–
Aboriginal peoples
in Canada
30.
Manitoba
–
Manitoba is a province at the longitudinal centre of Canada. It is one of the three provinces and Canadas fifth-most populous province with its estimated 1.3 million people. Manitoba covers 649,950 square kilometres with a varied landscape. Aboriginal peoples have inhabited what is now Manitoba for thousands of years, in the late 17th century, fur traders arrived in the area when it was part of Ruperts Land and owned by the Hudsons Bay Company. In 1869, negotiations for the creation of the province of Manitoba led to an uprising of the Métis people against the Government of Canada. The rebellions resolution led to the Parliament of Canada passing the Manitoba Act in 1870 that created the province, Manitobas capital and largest city, Winnipeg, is Canadas eighth-largest census metropolitan area. Winnipeg is the seat of government, home to the Legislative Assembly of Manitoba, four of the provinces five universities and all four of its professional sports teams are in Winnipeg. The name Manitoba is believed to be derived from the Cree, the name derives from Cree manitou-wapow or Ojibwa manidoobaa, both meaning straits of Manitou, the Great Spirit, a place referring to what are now called The Narrows in the centre of Lake Manitoba. It may also be from the Assiniboine for Lake of the Prairie, the lake was known to French explorers as Lac des Prairies. Thomas Spence chose the name to refer to a new republic he proposed for the south of the lake. Métis leader Louis Riel also chose the name, and it was accepted in Ottawa under the Manitoba Act of 1870 and it adjoins Hudson Bay to the northeast, and is the only prairie province to have a saltwater coastline. The Port of Churchill is Canadas only Arctic deep-water port and the shortest shipping route between North America and Asia, Lake Winnipeg is the tenth-largest freshwater lake in the world. Hudson Bay is the worlds second-largest bay, Manitoba is at the heart of the giant Hudson Bay watershed, once known as Ruperts Land. It was a area of the Hudsons Bay Company, with many rivers. The province has a saltwater coastline bordering Hudson Bay and more than 110,000 lakes, Manitobas major lakes are Lake Manitoba, Lake Winnipegosis, and Lake Winnipeg, the tenth-largest freshwater lake in the world. Some traditional Native lands and boreal forest on Lake Winnipegs east side are a proposed UNESCO World Heritage Site. Manitoba is at the centre of the Hudson Bay drainage basin, with a volume of the water draining into Lake Winnipeg. This basins rivers reach far west to the mountains, far south into the United States, major watercourses include the Red, Assiniboine, Nelson, Winnipeg, Hayes, Whiteshell and Churchill rivers
Manitoba
Manitoba
–
Deep Lake at Riding Mountain National Park.
Manitoba
–
Polar bears are common in northern Manitoba
31.
Winnipeg
–
Winnipeg is the capital and largest city of the province of Manitoba in Canada. It is located near the centre of North America and is 110 kilometres from the U. S. border. It is also the place of the confluence of the Red, the city is named after the nearby Lake Winnipeg, the name comes from the Western Cree words for muddy water. The region was a centre for aboriginal peoples long before the arrival of Europeans. French traders built the first fort on the site in 1738, a settlement was later founded by the Selkirk settlers of the Red River Colony in 1812, the nucleus of which was incorporated as the City of Winnipeg in 1873. As of 2011, Winnipeg is the seventh most populated municipality in Canada, being located very far inland, the local climate is extremely seasonal even by Canadian standards with average January lows of around −21 °C and average July highs of 26 °C. Known as the Gateway to the West, Winnipeg is a railway, Winnipeg was the first Canadian host of the Pan American Games. It is home to professional sports franchises, including the Winnipeg Blue Bombers, the Winnipeg Jets, Manitoba Moose. Winnipeg lies at the confluence of the Assiniboine and the Red River of the North and this point was at the crossroads of canoe routes travelled by First Nations before European contact. Winnipeg is named after nearby Lake Winnipeg, the name is a transcription of the Western Cree words for muddy or brackish water. Estimates of the date of first settlement in this area are varied, in 1805, Canadian colonists observed First Nations peoples engaged in farming activity along the Red River. The practice quickly expanded, driven by the demand by traders for provisions, the rivers provided an extensive transportation network linking northern First Peoples with those to the south along the Missouri and Mississippi rivers. The Ojibwe made some of the first maps on birch bark, sieur de La Vérendrye built the first fur trading post on the site in 1738, called Fort Rouge. French trading continued at this site for decades before the arrival of the British Hudsons Bay Company after France ceded the territory following its defeat in the Seven Years War. Many French and later British men who were trappers married First Nations women, their mixed-race children hunted, traded and they gradually developed as an ethnicity known as the Métis because of sharing a traditional culture. Lord Selkirk was involved with the first permanent settlement, the purchase of land from the Hudsons Bay Company, the North West Company built Fort Gibraltar in 1809, and the Hudsons Bay Company built Fort Douglas in 1812, both in the area of present-day Winnipeg. The two companies competed fiercely over trade, the Métis and Lord Selkirks settlers fought at the Battle of Seven Oaks in 1816. In 1821, the Hudsons Bay and North West Companies merged, Fort Gibraltar was renamed Fort Garry in 1822 and became the leading post in the region for the Hudsons Bay Company
Winnipeg
–
Clockwise from top:
Downtown featuring the
Canadian Museum for Human Rights,
Investors Group Field,
Saint Boniface and the
Esplanade Riel bridge, Wesley Hall at the
University of Winnipeg,
Manitoba Legislative Building.
Winnipeg
–
Winnipeg's old City Hall in 1887
Winnipeg
–
The Winnipeg General Strike, 21 June 1919
Winnipeg
–
River walkway near
The Forks, with
St. Boniface Cathedral in the background
32.
Rocky Mountains
–
The Rocky Mountains, commonly known as the Rockies, are a major mountain range in western North America. The Rocky Mountains stretch more than 3,000 miles from the northernmost part of British Columbia, in western Canada, to New Mexico, in the Southwestern United States. Within the North American Cordillera, the Rockies are somewhat distinct from the Pacific Coast Ranges, the Rocky Mountains were initially formed from 80 million to 55 million years ago during the Laramide orogeny, in which a number of plates began to slide underneath the North American plate. The angle of subduction was shallow, resulting in a belt of mountains running down western North America. Since then, further tectonic activity and erosion by glaciers have sculpted the Rockies into dramatic peaks, at the end of the last ice age, humans started to inhabit the mountain range. The first mention of their present name by a European was in the journal of Jacques Legardeur de Saint-Pierre in 1752, the Rocky Mountains are commonly defined as stretching from the Liard River in British Columbia south to the Rio Grande in New Mexico. The United States definition of the Rockies includes the Cabinet and Salish Mountains of Idaho and their counterparts north of the Kootenai River, the Columbia Mountains, are considered a separate system in Canada, lying to the west of the huge Rocky Mountain Trench. This runs the length of British Columbia from its beginnings in the middle Flathead River valley in western Montana to the bank of the Liard River. The Rockies vary in width from 70 to 300 miles, also west of the Rocky Mountain Trench, farther north and facing the Muskwa Range across the trench, are the Stikine Ranges and Omineca Mountains of the Interior Mountains system of British Columbia. A small area east of Prince George, British Columbia on the side of the Trench. In Canada geographers define three main groups of ranges, the Continental Ranges, Hart Ranges and Muskwa Ranges, the Muskwa and Hart Ranges together comprise what is known as the Northern Rockies. The western edge of the Rockies includes ranges such as the Wasatch near Salt Lake City, the Great Basin and Columbia River Plateau separate these sub-ranges from distinct ranges further to the west, most prominent among which are the Sierra Nevada, Cascade Range and Coast Mountains. The Rocky Mountain System within the United States is a United States physiographic region, the Rocky Mountains are notable for containing the highest peaks in central North America. The ranges highest peak is Mount Elbert located in Colorado at 14,440 feet above sea level, Mount Robson in British Columbia, at 12,972 feet, is the highest peak in the Canadian Rockies. The Continental Divide of the Americas is located in the Rocky Mountains, triple Divide Peak in Glacier National Park is so named because water that falls on the mountain reaches not only the Atlantic and Pacific, but Hudson Bay as well. Farther north in Alberta, the Athabasca and other rivers feed the basin of the Mackenzie River, see Rivers of the Rocky Mountains for a list of rivers. Human population is not very dense in the Rocky Mountains, with an average of four people per square kilometer, however, the human population grew rapidly in the Rocky Mountain states between 1950 and 1990. The 40-year statewide increases in range from 35% in Montana to about 150% in Utah
Rocky Mountains
–
Moraine Lake, and the
Valley of the Ten Peaks,
Banff National Park,
Alberta,
Canada
Rocky Mountains
–
The Front Range of the Rocky Mountains near
Denver, Colorado
Rocky Mountains
–
The
Tetons are a rugged subrange in Wyoming
Rocky Mountains
–
Mount Robson in
British Columbia.
33.
Canadian Shield
–
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
Canadian Shield
Canadian Shield
–
Canadian Shield geography in the
Flin Flon,
Manitoba region. The lake in the background is Big Island Lake.
Canadian Shield
Canadian Shield
–
Typical Canadian Shield: spruce, lakes, bogs, and rock.
34.
Taiga
–
Taiga also known as boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces and larches. The taiga is the worlds largest biome apart from the oceans, in North America it covers most of inland Canada and Alaska as well as parts of the extreme northern continental United States, where it is known as the Northwoods or North woods. However, the tree species, the length of the growing season. Hoffman discusses the origin of this use in North America. Although at high elevations taiga grades into alpine tundra through Krummholz, it is not an alpine biome only like subalpine forest, Taiga is the worlds largest land biome, and makes up 29% of the worlds forest cover, the largest areas are located in Russia and Canada. The taiga is the terrestrial biome with the lowest annual average temperatures after the tundra, extreme winter minimums in the northern taiga are typically lower than those of the tundra. The lowest reliably recorded temperatures in the Northern Hemisphere were recorded in the taiga of northeastern Russia, the taiga or boreal forest has a subarctic climate with very large temperature range between seasons, but the long and cold winter is the dominant feature. This climate is classified as Dfc, Dwc, Dsc, Dfd and Dwd in the Köppen climate classification scheme, meaning that the summer lasts 1–3 months. In Siberian taiga the average temperature of the coldest month is between −6 °C and −50 °C, the mean annual temperature generally varies from -5 °C to 5 °C, but there are taiga areas in eastern Siberia and interior Alaska-Yukon where the mean annual reaches down to -10 °C. According to some sources, the boreal forest grades into a mixed forest when mean annual temperature reaches about 3 °C. The winters, with temperatures below freezing, last five to seven months. Temperatures vary from −54 °C to 30 °C throughout the whole year, the summers, while short, are generally warm and humid. In much of the taiga, -20 °C would be a winter day temperature and 18 °C an average summer day. In Canada, Scandinavia and Finland, the season is often estimated by using the period of the year when the 24-hour average temperature is +5 °C or more. For the Taiga Plains in Canada, growing season varies from 80 to 150 days, some sources claim 130 days growing season as typical for the taiga. Other sources mention that 50–100 frost-free days are characteristic, data for locations in southwest Yukon gives 80–120 frost-free days. The closed canopy boreal forest in Kenozersky National Park near Plesetsk, Arkhangelsk Province, Russia, the longest growing season is found in the smaller areas with oceanic influences, in coastal areas of Scandinavia and Finland, the growing season of the closed boreal forest can be 145–180 days. High latitudes mean that the sun not rise far above the horizon
Taiga
–
Jack London Lake at Kolyma, Russia
Taiga
–
White spruce taiga, Denali Highway, Alaska Range, Alaska
Taiga
–
The taiga in the river valley near
Verkhoyansk,
Russia, at 67°N, must deal with the coldest winter temperatures in the northern hemisphere, but the extreme continentality of the climate gives an average daily high of 22 °C (72 °F) in July.
Taiga
–
Boreal forest near Shovel Point in
Tettegouche State Park, along the northern shore of Lake Superior in
Minnesota.
35.
Ecoregion
–
An ecoregion is an ecologically and geographically defined area that is smaller than a bioregion, which in turn is smaller than an ecozone. All three of these are less or greater than an ecosystem. Ecoregions cover relatively large areas of land or water, and contain characteristic, the biodiversity of flora, fauna and ecosystems that characterise an ecoregion tends to be distinct from that of other ecoregions. Three caveats are appropriate for all bio-geographic mapping approaches, firstly, no single bio-geographic framework is optimal for all taxa. Ecoregions reflect the best compromise for as many taxa as possible, secondly, ecoregion boundaries rarely form abrupt edges, rather, ecotones and mosaic habitats bound them. Thirdly, most ecoregions contain habitats that differ from their assigned biome, biogeographic provinces may originate due to various barriers. Some physical, some climatic and some ocean chemical related, the history of the term is somewhat vague as it was used in many contexts, forest classifications, biome classifications, biogeographic classifications, etc. The concept of ecoregion of Bailey gives more importance to ecological criteria, while the WWF concept gives more importance to biogeography, there is significant, but not absolute, spatial correlation among these characteristics, making the delineation of ecoregions an imperfect science. Such transition zones are called ecotones, Ecoregions can be categorized using an algorithmic approach or a holistic, “weight-of-evidence” approach where the importance of various factors may vary. An example of the approach is Robert Bailey’s work for the U. S. The intended purpose of ecoregion delineation may affect the method used, according to WWF, the boundaries of an ecoregion approximate the original extent of the natural communities prior to any major recent disruptions or changes. WWF has identified 867 terrestrial ecoregions, and approximately 450 freshwater ecoregions across the Earth, the use of the term ecoregion is an outgrowth of a surge of interest in ecosystems and their functioning. In particular, there is awareness of issues relating to spatial scale in the study and it is widely recognized that interlinked ecosystems combine to form a whole that is greater than the sum of its parts. The Global 200 is the list of ecoregions identified by WWF as priorities for conservation, Terrestrial ecoregions are land ecoregions, as distinct from freshwater and marine ecoregions. In this context, terrestrial is used to mean of land, WWF ecologists currently divide the land surface of the Earth into 8 major ecozones containing 867 smaller terrestrial ecoregions. The WWF effort is a synthesis of previous efforts to define. Many consider this classification to be decisive, and some propose these as stable borders for bioregional democracy initiatives. The eight terrestrial ecozones follow the major floral and faunal boundaries, identified by botanists and zoologists, ecozone boundaries generally follow continental boundaries, or major barriers to plant and animal distribution, like the Himalayas and the Sahara
Ecoregion
–
A map location of the
Amazon rainforest ecoregions. The yellow line encloses the ecoregions per the World Wide Fund for Nature.
Ecoregion
–
A map of North America's Bioregions
Ecoregion
–
The
Ötztal Alps, a
mountain range in the central
Alps of
Europe, are part of the
Central Eastern Alps, and can both be termed as ecoregions.
Ecoregion
–
A conifer forest in the
Swiss Alps (
National Park).
36.
Tundra
–
In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons. The term tundra comes through Russian тундра from the Kildin Sami word tūndâr uplands, there are three types of tundra, Arctic tundra, alpine tundra, and Antarctic tundra. In tundra, the vegetation is composed of shrubs, sedges and grasses, mosses. Scattered trees grow in tundra regions. The ecotone between the tundra and the forest is known as the line or timberline. Arctic tundra occurs in the far Northern Hemisphere, north of the taiga belt, the word tundra usually refers only to the areas where the subsoil is permafrost, or permanently frozen soil. Permafrost tundra includes vast areas of northern Russia and Canada, the polar tundra is home to several peoples who are mostly nomadic reindeer herders, such as the Nganasan and Nenets in the permafrost area. Arctic tundra contains areas of landscape and is frozen for much of the year. The soil there is frozen from 25–90 cm down, and it is impossible for trees to grow, instead, bare and sometimes rocky land can only support low growing plants such as moss, heath, and lichen. There are two seasons, winter and summer, in the polar tundra areas. During the winter it is cold and dark, with the average temperature around −28 °C. However, extreme temperatures on the tundra do not drop as low as those experienced in taiga areas further south. During the summer, temperatures rise somewhat, and the top layer of seasonally-frozen soil melts, the tundra is covered in marshes, lakes, bogs and streams during the warm months. Generally daytime temperatures during the rise to about 12 °C. Arctic tundras are sometimes the subject of conservation programs. In Canada and Russia, many of areas are protected through a national Biodiversity Action Plan. Tundra tends to be windy, with winds often blowing upwards of 50–100 km/h, however, in terms of precipitation, it is desert-like, with only about 15–25 cm falling per year. Although precipitation is light, evaporation is also relatively minimal, there is a natural pattern of accumulation of fuel and wildfire which varies depending on the nature of vegetation and terrain
Tundra
–
Tundra in Greenland
Tundra
–
Tundra in
Siberia
Tundra
–
Vuntut National Park in Canada
Tundra
–
A group of
muskoxen in Alaska
37.
Hudson Bay Lowlands
–
Hudson Bay Lowlands are a vast wetland located between the Canadian Shield and southern shores of Hudson Bay and James Bay. Most of the lies within the province of Ontario, with smaller portions reaching into Manitoba. This is the largest wetland in Canada, and one of the largest in the world, the region can be subdivided into three bands running roughly northwest to southeast, the Coastal Hudson Bay Lowland, Hudson Bay Lowland, and James Bay Lowland. The entire area was covered by ice during the last glaciation, plants from more temperate regions mix with arctic species. A majority of the wetland is peat bog, although saline marshes occur along the coast, the wetlands provide important habitat for migratory birds including shorebirds and waterfowl. Large mammals include polar bear and wolverine, the local Ojibwa and Cree most likely came into contact with the region but did not populate the region due to the harsh, undesirable conditions and poor drainage patterns of the area. When Europeans arrived in the area, The Hudsons Bay Company set up trading posts such as Rankin Inlet, however, these never grew into sizable towns, again because of the poor living conditions and climate. To this day, not all of the lowlands have been properly explored, there are a few small First Nations settlements on the southern shore of Hudson Bay Lowlands at places like Moose Factory, Moosonee, Attawapiskat, and Fort Severn. The region is named after the inland sea, Hudson Bay. The entire area drains into the bay through rivers such as the Churchill, Severn, the region is located in the extreme north of Ontario, extending into both Manitoba to the west and Quebec in the east, and covers around 25 percent of Ontarios total land area. The area was covered in ice during the last ice age, peatlands, both bogs and fens now cover much of the landscape, with other kinds of wetlands along rivers and the coast. The climate of the region depends largely on the surface of the bay. In the winter the bay freezes over again, bringing freezing temperatures, the vegetation is mostly conifer forest and peatland, with typical sub arctic and boreal plants. Hudson Bay in The Canadian Encyclopedia Hudson Bay Lowlands - Ottertooth Arctic Institute paper by Hugo Sjörs, Bogs, Hudson Bay Lowlands show recent effects of global warming. Max Paris Environment Unit, CBC News
Hudson Bay Lowlands
–
Snow geese migrate north each year to breed in the coastal marshes of the Hudson Bay Lowland.
Hudson Bay Lowlands
–
The Hudson Bay Lowlands approximately coincide with the Southern Hudson Bay Taiga Ecoregion of North America.
Hudson Bay Lowlands
–
Biogeography
38.
Muskeg
–
Muskeg is an acidic soil type common in Arctic and boreal areas, although it is found in other northern climates as well. Muskeg is approximately synonymous with bogland, but muskeg is the term in Western Canada and Alaska. The term became common in these areas because it is of Cree origin, large tracts of this soil existing in Siberia may be called muskeg or bogland interchangeably. Muskeg consists of plants in various states of decomposition, ranging from fairly intact sphagnum moss, to sedge peat. Pieces of wood can make up five to 15 percent of the peat soil, Muskeg tends to have a water table near the surface. The sphagnum moss forming it can hold 15 to 30 times its own weight in water, Muskeg patches are ideal habitats for beavers, pitcher plants, agaric mushrooms and a variety of other organisms. Muskeg forms because permafrost, clay or bedrock prevents water drainage, the water from rain and snow collects, forming permanently waterlogged vegetation and stagnant pools. It needs two conditions to develop, abundant rain and cool summers, a dead plant that falls on dry soil is normally attacked by bacteria and fungi and quickly rots. If the same plant lands in water or on saturated soil, less oxygen is available under water, so aerobic bacteria and fungi fail to colonize the submerged debris effectively. In addition, cool temperatures retard bacterial and fungal growth and this causes slow decomposition, and thus the plant debris gradually accumulates to form peat and eventually muskeg. Depending on the topography of the land, muskeg can reach depths greater than 30 metres. Although at first glance resembles a plain covered with short grasses. Small stands of stunted and often dead trees, which vaguely resemble Bonsai trees, grow where land protrudes above the water table and its grassland appearance invites the unwary to walk on it, but even the most solid muskeg is spongy and waterlogged. Traveling through muskeg is a strange and dangerous experience for the unaccustomed, Muskeg can grow atop bodies of water, especially small ponds and streams. Because of the water beneath, the muskeg surface sometimes ripples underfoot, thinner patches allow large animals to fall through, becoming trapped under the muskeg and drowning. Moose are at a disadvantage in muskeg due to their long legs, minimal hoof area. Hunters and hikers may occasionally encounter young moose in muskeg-covered ponds submerged up to their torsos or necks, Muskeg can be a significant impediment to transportation. During the 1870s, muskeg in Northern Ontario was reported to have swallowed a railroad engine whole when a track was laid on muskeg instead of clearing down to bedrock
Muskeg
–
Stunted
shore pine growing on muskeg in
Wrangell, Alaska.
Muskeg
–
Poplar growing on muskeg
Muskeg
–
Heavy equipment breaking through thawing muskeg in
Wabasca oil field in Alberta.
Muskeg
–
Tracked excavator placing corduroy on muskeg near
Rocky Mountain House,
Alberta
39.
Ringed seal
–
The ringed seal, also known as the jar seal and as netsik or nattiq by the Inuit, is an earless seal inhabiting the Arctic and sub-Arctic regions. The ringed seal is a small seal, rarely greater than 1.5 m in length, with a distinctive patterning of dark spots surrounded by light grey rings. Ringed seals are one of the prey of polar bears and have long been a component of the diet of indigenous people of the Arctic. The ringed seal is the smallest and most common seal in the Arctic, with a head, short cat-like snout. Its coat is dark with silver rings on the back and sides with a silver belly, depending on subspecies and condition, adult size can range from 100 to 175 cm and weigh from 32 to 140 kg. The seal averages about 5 ft long with a weight of about 50–70 kg and this species is usually considered the smallest species in the true seal family, although several related species, especially the Baikal seal, may approach similarly diminutive dimensions. Their small front flippers have claws more than 1 inch thick that are used to maintain breathing holes through 6.5 ft thick ice, the taxonomy of ringed seal has been much debated and revised in the literature. Due to its range, as many as ten subspecies have been described. The ringed seal is most closely related to the Caspian seal and Baikal seal, all of which share similar small sizes, features of skull morphology and affinity for ice. The closest phylogenetic relatives to the seal are the grey seal. Together with the northern latitude ice seals, these seals constitute the subfamily Phocinae. Ringed seals occur throughout the Arctic Ocean and they can be found in the Baltic Sea, the Bering Sea and the Hudson Bay. They prefer to rest on ice floe and will move north for denser ice. Two subspecies can be found in freshwater, Ringed seals have a circumpolar distribution from approximately 35°N to the North Pole, occurring in all seas of the Arctic Ocean. In the North Pacific, they are found in the southern Bering Sea and range as far south as the seas of Okhotsk, throughout their range, ringed seals have an affinity for ice-covered waters and are well adapted to occupying seasonal and permanent ice. They tend to prefer large floes and are found in the interior ice pack where the sea ice coverage is greater than 90%. They remain in contact with ice most of the year and pup on the ice in late winter-early spring, distribution in Alaska, Ringed seals are found throughout the Beaufort, Chukchi, and Bering Seas, as far south as Bristol Bay in years of extensive ice coverage. During late April through June, ringed seals are distributed throughout their range from the ice edge northward
Ringed seal
–
Ringed seal
Ringed seal
–
backflippers
Ringed seal
–
Pup of ringed seal.
Ringed seal
–
Preparation of the ringed seal
40.
Polar bear
–
The polar bear is a carnivorous bear whose native range lies largely within the Arctic Circle, encompassing the Arctic Ocean, its surrounding seas and surrounding land masses. It is a bear, approximately the same size as the omnivorous Kodiak bear. A boar weighs around 350–700 kg, while a sow is about half that size, although most polar bears are born on land, they spend most of their time on the sea ice. Their scientific name means maritime bear and derives from this fact, Polar bears hunt their preferred food of seals from the edge of sea ice, often living off fat reserves when no sea ice is present. Because of expected habitat loss caused by change, the polar bear is classified as a vulnerable species. For decades, large-scale hunting raised international concern for the future of the species, for thousands of years, the polar bear has been a key figure in the material, spiritual, and cultural life of circumpolar peoples, and polar bears remain important in their cultures. Constantine John Phipps was the first to describe the polar bear as a species in 1774. He chose the scientific name Ursus maritimus, the Latin for maritime bear, the Inuit refer to the animal as nanook. The Yupik also refer to the bear as nanuuk in Siberian Yupik, the bear is umka in the Chukchi language. In Russian, it is usually called бе́лый медве́дь, though a word still in use is ошку́й. In the Norwegian-administered Svalbard archipelago, the bear is referred to as Isbjørn. The polar bear was considered to be in its own genus. The bear family, Ursidae, is thought to have split off from other carnivorans about 38 million years ago, the Ursinae subfamily originated approximately 4.2 million years ago. The oldest known polar bear fossil is a 130,000 to 110, 000-year-old jaw bone, fossils show that between 10,000 and 20,000 years ago, the polar bears molar teeth changed significantly from those of the brown bear. Polar bears are thought to have diverged from a population of bears that became isolated during a period of glaciation in the Pleistocene or from the eastern part of Siberia. The evidence from DNA analysis is more complex, the mitochondrial DNA of the polar bear diverged from the brown bear, Ursus arctos, roughly 150,000 years ago. The mtDNA of extinct Irish brown bears is particularly close to polar bears, when the polar bear was originally documented, two subspecies were identified, Ursus maritimus maritimus by Constantine J. Phipps in 1774, and Ursus maritimus marinus by Peter Simon Pallas in 1776. This distinction has since been invalidated, one alleged fossil subspecies has been identified, Ursus maritimus tyrannus became extinct during the Pleistocene
Polar bear
–
Polar bear
Polar bear
–
Polar bears have evolved adaptations for Arctic life, for example, large furry feet and short, sharp, stocky claws give them good traction on ice.
Polar bear
–
Polar bears investigate the submarine
USS Honolulu 450 kilometres (280 mi) from the
North Pole.
Polar bear
–
Polar bear jumping on fast ice
41.
Beluga whale
–
The beluga whale or white whale is an Arctic and sub-Arctic cetacean. It is one of two members of the family Monodontidae, along with the narwhal, and the member of the genus Delphinapterus. This marine mammal is commonly referred to as the beluga, melonhead and it is adapted to life in the Arctic, so has anatomical and physiological characteristics that differentiate it from other cetaceans. Amongst these are its all-white colour and the absence of a dorsal fin and it possesses a distinctive protuberance at the front of its head which houses an echolocation organ called the melon, which in this species is large and deformable. The belugas body size is between that of a dolphins and a true whales, with growing up to 5.5 m long and weighing up to 1,600 kg. This whale has a stocky body, a large percentage of its weight is blubber, as is true of many cetaceans. Its sense of hearing is highly developed and its echolocation allows it to move about, belugas are gregarious and form groups of up to 10 animals on average, although during the summer, they can gather in the hundreds or even thousands in estuaries and shallow coastal areas. They are slow swimmers, but can dive to 700 m below the surface and they are opportunistic feeders and their diets vary according to their locations and the season. The majority of live in the Arctic Ocean and the seas and coasts around North America, Russia and Greenland. They are migratory and the majority of groups spend the winter around the Arctic ice cap, some populations are sedentary and do not migrate over great distances during the year. The native peoples of North America and Russia have hunted belugas for many centuries and they were also hunted commercially during the 19th century and part of the 20th century. Whale hunting has been under control since 1973. Currently, only certain Inuit and Alaska Native groups are allowed to carry out hunting of belugas. Other threats include natural predators, contamination of rivers, and infectious diseases, of seven Canadian beluga populations, the two inhabiting eastern Hudson Bay and Ungava Bay are listed as endangered. Belugas are one of the most commonly kept cetaceans in captivity and are housed in aquariums, dolphinariums, and wildlife parks in North America, Europe and they are popular with the public due to their colour and expression. The beluga was first described in 1776 by Peter Simon Pallas and it is a member of the Monodontidae family, which is in turn part of the parvorder Odontoceti. The Irrawaddy dolphin was once placed in the family, recent genetic evidence suggests these dolphins belong to the Delphinidae family. The narwhal is the other species within the Monodontidae besides the beluga
Beluga whale
–
Beluga
Beluga whale
–
Skull of a cross between a narwhal and a beluga whale, at the Zoological Museum, Copenhagen
Beluga whale
–
Skeleton of D. leucas
Beluga whale
–
Front view
42.
Harricana River
–
The Harricana River is a river in western Quebec and northeastern Ontario, Canada. It is 533 kilometres long, has an area of 29,300 square kilometres. While 80% of its area is in Quebec, the river flows for a short distance through Ontario before it ends in Hannah Bay off James Bay. Because of its nature, easy upstream access, and the possibility to paddle to and take out at Moosonee. The Harricana originates at Lake Blouin just north of Val-dOr, from here De Montigny and Lemoine Lakes add to it before it flows through a series of lakes such as Malartic, La Motte, and Figuery Lakes. After flowing through the town of Amos, one significant lake follows. North of Amos the river crosses lush boreal forests, where extensive logging takes place, toward its mouth at Hannah Bay, the forest gradually decreases and is replaced with many wetlands. Here the Harricana has considerable speed and a relief, flowing through undeveloped wilderness. As a tributary of the James bay, and thus of the Hudson Bay, but not until 1801, Alexander MacKenzie mapped the entire route of the river for the first time and identified it by name Harricanaw. In 1835, the map of Bradford called it Harricana, the Ruperts Land Act 1868 transferred the river and its basin to the Dominion of Canada and was officially annexed to the Province of Quebec in 1898. Thereafter colonization and settlement on the upper Harricana began in earnest, in 1906, Henry O Sullivan explored the shores of Harricana and in 1908, the first camps were established on its banks at the rapids. These were provisioning camps for the railroad construction. A few years later, in 1910, the first colonists arrive, the rivers name originates from the Algonquin word Nanikana, meaning the main way or Biscuit River, depending on the source. Biscuit refers to the flat stones, sand, limestone and clay concretions. Through history various spellings have been reported, anâkona, uhnahkoonah, the Algonquins also use the name Inikana, meaning river route. A segment of the river was called Wajaha Sibi, which means river to the bay, List of rivers of Ontario List of rivers of Quebec
Harricana River
–
The Harricana River in Amos
Harricana River
–
Log driving on the Harricana at Amos, circa 1916.
Harricana River
–
The Harricana River and its mouth at Hannah Bay is visible on the left.
43.
Migratory Birds Convention Act
–
A permit is required to engage in any of these activities. In 1909 the federal government established the Advisory Board on Wildlife Protection, hewitt and James Harkin as prominent members. This board would go on to sign the Migratory Bird Convention with the United States because of both countries had regarding the uncontrolled hunting of waterfowl and shorebirds. The original MBCA law was passed to satisfy the terms of agreement with the United States. The updated version includes stronger enforcement and greater penalties, to establish complete habitat protection, the more stringent requirements of the Canada Wildlife Act are necessary. List of Migratory Bird Sanctuaries of Canada Migratory Bird Treaty Act of 1918, the American law implementing the treaty Migratory Birds Convention Act,1994
Migratory Birds Convention Act
–
Mont Saint-Hilaire in southern Quebec was made a Migratory Bird Sanctuary in 1960
44.
Southern James Bay
–
Southern James Bay is a Canadian coastal wetland complex in northeastern Ontario bordering James Bay and Quebec. It was designated as a wetland of international importance via the Ramsar Convention on May 27,1987, the shallow waters of the James Bay region represent an important late autumn staging area for migratory, Arctic-breeding waterbirds. As many as 75,000 geese of various species may use the staging area in autumn. Substantial numbers of diving sea ducks occur offshore, the sites are located on Ontario Crown land, except for outlying islands that are part of the Nunavut, which are federal Crown land. They are demarcated to prevent hunting within their boundaries, a policy which is enforced, hunting is permitted in adjacent land. Gradually rising inland from sea level, it attains elevations of no more than 50 metres
Southern James Bay
–
Satellite view of the frozen Hannah Bay and Harricana River
45.
Ramsar Convention
–
The Ramsar Convention is an international treaty for the conservation and sustainable use of wetlands. It is also known as the Convention on Wetlands and it is named after the city of Ramsar in Iran, where the Convention was signed in 1971. The most recent COP12 was held in Punta del Este, Uruguay, cOP13 will take place in Dubai, United Arab Emirates, in 2018. The List of Wetlands of International Importance included 2,231 Ramsar Sites in March 2016 covering over 2.1 million square kilometres. The country with the highest number of Sites is the United Kingdom with 170, the Ramsar Sites Information Service is a searchable database which provides information on each Ramsar Site. As of 2016 there are 18 Transboundary Ramsar Sites, as of 2016 there are 15 Ramsar Regional Initiatives covering regions of the Mediterranean, Asia, Africa and South America. The Ramsar Convention works closely with six other known as International Organization Partners. The IOPs also participate regularly as observers in all meetings of the Conference of the Parties and as members of the Scientific. Conference of the Parties Conference of the Parties is the Conventions governing body consisting of all governments that have ratified the treaty and this ultimate authority reviews progress under the Convention, identifies new priorities, and sets work plans for members. The COP can also make amendments to the Convention, create expert advisory bodies, review progress reports by member nations, and collaborate with other international organizations and agreements. The Standing Committee The Standing Committee is the executive body which represents the COP between its triennial meetings, within the framework of the decisions made by the COP. The Contracting Parties that are members of the Standing Committee are elected by each meeting of the COP to serve for the three years until the next one, the Secretariat The Secretariat carries out the day-to-day coordination of the Convention’s activities. It is based at the headquarters of the International Union for the Conservation of Nature in Gland, Switzerland, the 2nd of February each year is World Wetlands Day, marking the date of the adoption of the Convention on Wetlands on 2 February 1971. Established to raise awareness about the value of wetlands for humanity, in 2015 World Wetlands Day was celebrated in 59 countries
Ramsar Convention
–
Wetland
Ramsar Convention
–
Ramsar logo
Ramsar Convention
–
General
Ramsar Convention
–
Marine
46.
Mudflat
–
Mudflats or mud flats, also known as tidal flats, are coastal wetlands that form when mud is deposited by tides or rivers. They are found in sheltered areas such as bays, bayous, lagoons, mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and marine animal detritus. Most of the sediment within a mudflat is within the intertidal zone, in the past tidal flats were considered unhealthy, economically unimportant areas and were often dredged and developed into agricultural land. Several especially shallow mudflat areas, such as the Wadden Sea, are now popular among those practising the sport of mudflat hiking. On the Baltic Sea coast of Germany in places, mudflats are exposed not by tidal action and these wind-affected mudflats are called windwatts in German. Tidal flats, along with salt marshes and mangrove forests, are important ecosystems. They are often of importance to migratory birds, as well as certain species of crabs, mollusks. In the United Kingdom mudflats have been classified as a Biodiversity Action Plan priority habitat, the maintenance of mudflats is important in preventing coastal erosion. However, mudflats worldwide are under threat from predicted sea level rises, land claims for development, dredging due to shipping purposes, in some parts of the world, such as East and South-East Asia, mudflats have been reclaimed for aquaculture, agriculture, and industrial development. For example, around the Yellow Sea region of East Asia, mudflat sediment deposits are focused into the intertidal zone which is composed of a barren zone, marsh and salt pan. Within these areas are various ratios of sand and mud that make up the sedimentary layers, the associated growth of coastal sediment deposits can be attributed to rates of subsidence along with rates of deposition and changes in sea level. Barren zones extend from the lowest portion of the zone to the marsh areas. Beginning in close proximity to the bars, sand dominated layers are prominent. Common bedding types include laminated sand, ripple bedding, and bay mud, bioturbation also has a strong presence in barren zones. Marshes contain an abundance of plants while the sediment layers consist of thin sand. Mudcracks are a common as well as wavy bedding planes, marshes are also the origins of coal/peat layers because of the abundant decaying plant life. Salt pans can be distinguished in that they contain thinly laminated layers of clayey silt, the main source of the silt comes from rivers. Dried up mud along with wind erosion forms silt dunes, when flooding, rain or tides come in, the dried sediment is then re-distributed
Mudflat
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Mudflats near
Oban on
Stewart Island,
New Zealand
Mudflat
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General sketch-map of a tidal plain, showing the typical tripartition in
supratidal,
intertidal and
subtidal zones. The most apparent character of the area is the development of tidal channels, affecting mainly the
intertidal zone. In this case, the tidal flat is protected seaward by a
beach barrier, but in many cases (low-energy
waves and
longshore currents) the tidal flats may directly pass into a shallow marine environment.
Mudflat
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Mudflats in
Brewster, Massachusetts,
United States, extending hundreds of yards offshore at the low tide. The line of seashells in the foreground indicates the
high-water mark.
Mudflat
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Gulls feeding on mudflats in
Skagit Bay,
Washington.
47.
Salt pan (geology)
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Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the Sun. They are found in deserts, and are natural formations, a salt pan forms by evaporation of a water pool such as a lake or pond. This happens in climates where the rate of water exceeds the rate of precipitation. If the water drain into the ground, it remains on the surface until it evaporates. Over thousands of years, the minerals accumulate on the surface and these minerals reflect the Suns rays and often appear as white areas. The crust of salt can conceal a quagmire of mud that can engulf a truck, the Qattara Depression in the eastern Sahara desert contains many such traps which served as strategic barriers during World War II. The Bonneville Salt Flats in Utah, where land speed records have been set, is a well-known salt pan in the arid regions of the western United States. The Etosha pan, in the Etosha National Park in Namibia, is another prominent example of a salt pan, the Salar de Uyuni in Bolivia is the largest salt pan in the world. It contains 50%-70% of the worlds lithium reserves, dry lake Pan Sabkha Salt evaporation pond Salt lake Sink Solonchak Briere, Peter R. Playa, playa lake, sabkha, Proposed definitions for old terms. Lowenstein, Tim K. Lawrence A. Hardie, criteria for the recognition of salt-pan evaporites
Salt pan (geology)
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Salar de Uyuni in
Bolivia
Salt pan (geology)
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Cono de Arita in
Salar de Arizaro,
Salta (
Argentina)
Salt pan (geology)
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Devil's Golf Course,
Death Valley National Park, United States
48.
Estuary
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An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a zone between river environments and maritime environments. They are subject both to marine influences—such as tides, waves, and the influx of saline water—and to riverine influences—such as flows of fresh water and sediment. The inflows of sea water and fresh water provide high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea began to rise about 10. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns, the banks of many estuaries are amongst the most heavily populated areas of the world, with about 60% of the worlds population living along estuaries and the coast. The word estuary is derived from the Latin word aestuarium meaning tidal inlet of the sea, there have been many definitions proposed to describe an estuary. However, this definition excludes a number of water bodies such as coastal lagoons. This broad definition also includes fjords, lagoons, river mouths, an estuary is a dynamic ecosystem having a connection to the open sea through which the sea water enters with the rhythm of the tides. The sea water entering the estuary is diluted by the water flowing from rivers. The pattern of dilution varies between different estuaries and depends on the volume of water, the tidal range. Drowned river valleys are known as coastal plain estuaries. In places where the sea level is rising relative to the land, sea water progressively penetrates into river valleys and this is the most common type of estuary in temperate climates. Well-studied estuaries include the Severn Estuary in the United Kingdom and the Ems Dollard along the Dutch-German border, the width-to-depth ratio of these estuaries is typically large, appearing wedge-shaped in the inner part and broadening and deepening seaward. Water depths rarely exceed 30 m, examples of this type of estuary in the U. S. are the Hudson River, Chesapeake Bay, and Delaware Bay along the Mid-Atlantic coast, and Galveston Bay and Tampa Bay along the Gulf Coast. They are relatively common in tropical and subtropical locations and these estuaries are semi-isolated from ocean waters by barrier beaches. Formation of barrier beaches partially encloses the estuary, with only narrow inlets allowing contact with the ocean waters, bar-built estuaries typically develop on gently sloping plains located along tectonically stable edges of continents and marginal sea coasts. They are extensive along the Atlantic and Gulf coasts of the U. S. in areas with active coastal deposition of sediments, barrier beaches form in shallow water and are generally parallel to the shoreline, resulting in long, narrow estuaries
Estuary
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Estuary of the
Klamath River in
Northern California
Estuary
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River Exe estuary
Estuary
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River Nith estuary
Estuary
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Estuary mouth located in
Darwin,
Northern Territory,
Australia
49.
Marsh
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A marsh is a wetland that is dominated by herbaceous rather than woody plant species. Marshes can often be found at the edges of lakes and streams and they are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, Marshes provide a habitat for many species of plants, animals, and insects that have adapted to living in flooded conditions. The plants must be able to survive in wet mud with low oxygen levels, many of these plants therefore have aerenchyma, channels within the stem that allow air to move from the leaves into the rooting zone. Marsh plants also tend to have rhizomes for underground storage and reproduction, familiar examples include cattails, sedges, papyrus and sawgrass. Aquatic animals, from fish to salamanders, are able to live with a low amount of oxygen in the water. Some can obtain oxygen from the air instead, while others can live indefinitely in conditions of low oxygen, Marshes provide habitats for many kinds of invertebrates, fish, amphibians, waterfowl and aquatic mammals. Marshes have extremely high levels of production, some of the highest in the world. Marshes also improve water quality by acting as a sink to filter pollutants, Marshes are able to absorb water during periods of heavy rainfall and slowly release it into waterways and therefore reduce the magnitude of flooding. The pH in marshes tends to be neutral to alkaline, as opposed to bogs, Marshes differ depending mainly on their location and salinity. Both of these factors influence the range and scope of animal and plant life that can survive. The three main types of marsh are salt marshes, freshwater marshes, and freshwater marshes. These three can be found worldwide and each contains a different set of organisms, saltwater marshes are found around the world in mid to high latitudes, wherever there are sections of protected coastline. They are located close enough to the shoreline that the motion of the tides affects them and they flourish where the rate of sediment buildup is greater than the rate at which the land level is sinking. Salt marshes are dominated by specially adapted rooted vegetation, primarily salt-tolerant grasses, salt marshes are most commonly found in lagoons, estuaries, and on the sheltered side of shingle or sandspit. The currents there carry the fine particles around to the side of the spit. These locations allow the marshes to absorb the nutrients from the water running through them before they reach the oceans. Coastal development and urban sprawl has caused significant loss of these essential habitats, although considered a freshwater marsh, this form of marsh is affected by the ocean tides
Marsh
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A marsh along the edge of a small river
Marsh
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Marsh in shallow water on a lakeshore
Marsh
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White water lilies are a typical marsh plant in European areas of deeper water.
Marsh
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Many kinds of birds nest in marshes; this one is a
yellow-headed blackbird.
50.
Swamp
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A swamp is a wetland that is forested. Many swamps occur along rivers where they are critically dependent upon natural water level fluctuations. Other swamps occur on the shores of large lakes, some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inundation. The two main types of swamp are true or swamp forests and transitional or shrub swamps, in the boreal regions of Canada, the word swamp is colloquially used for what is more correctly termed a bog or muskeg. The water of a swamp may be water, brackish water or seawater. Some of the worlds largest swamps are found along rivers such as the Amazon, the Mississippi. Swamps are characterized by slow-moving to stagnant waters and they are usually associated with adjacent rivers or lakes. Swamps are features of areas with very low topographic relief, historically, humans have drained swamps to provide additional land for agriculture and to reduce the threat of diseases borne by swamp insects and similar animals. Many swamps have also undergone intensive logging, requiring the construction of drainage ditches and these ditches and canals contributed to drainage and, along the coast, allowed salt water to intrude, converting swamps to marsh or even to open water. Large areas of swamp were therefore lost or degraded, louisiana provides a classic example of wetland loss from these combined factors. Europe has probably lost nearly half its wetlands, New Zealand lost 90 percent of its wetlands over a period of 150 years. Ecologists recognise that swamps provide valuable ecological services including flood control, fish production, water purification, carbon storage, in many parts of the world authorities protect swamps. In parts of Europe and North America, swamp restoration projects are becoming widespread, often the simplest steps to restoring swamps involve plugging drainage ditches and removing levees. Swamps and other wetlands have traditionally held a very low property value compared to fields, prairies and they have a reputation for being unproductive land that cannot easily be utilized for human activities, other than perhaps hunting and trapping. Farmers, for example, typically drained swamps next to their fields so as to more land usable for planting crops. Many societies now realize that swamps are important to providing fresh water and oxygen to all life. Indeed, floodplain swamps are important in fish production. Government environmental agencies are taking steps to protect and preserve swamps, in Europe, major effort is being invested in the restoration of swamp forests along rivers
Swamp
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A freshwater swamp in
Florida
Swamp
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A
black alder swamp in
Germany
Swamp
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Swamp in southern Louisiana
Swamp
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A small swamp in the
Padstow, New South Wales.
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