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160-621: The canyon was formed during the Miocene period (23.7–5.3 million years ago) by the river cutting into the uplifting Interior Plateau. From the northern Cariboo to Fountain , the river follows the line of the huge Fraser Fault, which runs on a north–south axis and meets the Yalakom Fault a few miles downstream from Lillooet . Exposures of lava flows are present in cliffs along the Fraser Canyon. They represent volcanic activity in

320-457: A "designated group," along with women, visible minorities , and people with physical or mental disabilities. First Nations are not defined as a visible minority by the criteria of Statistics Canada . 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 and

480-542: A broader aridification trend. The EMCI ended 18 million years ago, giving way to the Middle Miocene Warm Interval (MMWI), the warmest part of which was the MMCO that began 16 million years ago. As the world transitioned into the MMCO, carbon dioxide concentrations varied between 300 and 500 ppm. Global annual mean surface temperature during the MMCO was about 18.4 °C. MMCO warmth was driven by

640-551: A change in the public perception of the residential school system, as well as official government apologies, and a (controversial) legal settlement. Colonization had a significant impact on First Nations diet and health. According to the historian Mary-Ellen Kelm, "inadequate reserve allocations, restrictions on the food fishery, overhunting, and over-trapping" alienated First Nations from their traditional way of life, which undermined their physical, mental, emotional, and spiritual health. As Canadian ideas of progress evolved around

800-529: A clade of large terrestrial predatory crocodyliformes distantly related to modern crocodilians, from which they likely diverged over 180 million years ago, are known from the Miocene of South America. The last Desmostylians thrived during this period before becoming the only extinct marine mammal order. The pinnipeds , which appeared near the end of the Oligocene, became more aquatic. A prominent genus

960-570: A cooler, drier climate. C 4 grasses, which are able to assimilate carbon dioxide and water more efficiently than C 3 grasses, expanded to become ecologically significant near the end of the Miocene between 6 and 7 million years ago, although they did not expand northward during the Late Miocene. The expansion of grasslands and radiations among terrestrial herbivores correlates to fluctuations in CO 2 . One study, however, has attributed

1120-534: A few handholds – were compared to goat-tracks. North of Lytton , it is followed by BC Highway 12 , then from Lillooet to Pavilion by BC Highway 99 (the farther end of the Sea-to-Sky Highway , though not carrying that name in this area). The British Columbia Railway (now operated by the CN) line follows the same stretch of canyon from Lillooet to just beyond Pavilion]. Between there and

1280-781: A few miles. These include Marble Canyon , Churn Creek , the Chilcotin River, the Bridge River , Seton Lake and Cayoosh Creek , the Stein River , the Nahatlatch River , the Coquihalla River and the innumerable smaller creeks flanking the river between Kanaka Bar and Yale. The Canadian Pacific Railway has at least 30 tunnels in its Yale to Lytton section with one up to half a mile in length. The Fraser Canyon Highway Tunnels were constructed from

1440-486: A good analogue for future warmer climates caused by anthropogenic global warming , with this being especially true of the global climate during the Middle Miocene Climatic Optimum (MMCO), because the last time carbon dioxide levels were comparable to projected future atmospheric carbon dioxide levels resulting from anthropogenic climate change was during the MMCO. The Ross Sea margin of

1600-435: A good model for a "living fossil". Eucalyptus fossil leaves occur in the Miocene of New Zealand , where the genus is not native today, but have been introduced from Australia . Both marine and continental fauna were fairly modern, although marine mammals were less numerous. Only in isolated South America and Australia did widely divergent fauna exist. In Eurasia, genus richness shifted southward to lower latitudes from

1760-598: A major expansion of Antarctic glaciers. This severed the connection between the Indian Ocean and the Mediterranean Sea and formed the present land connection between Afro-Arabia and Eurasia. The subsequent uplift of mountains in the western Mediterranean region and a global fall in sea levels combined to cause a temporary drying up of the Mediterranean Sea (known as the Messinian salinity crisis ) near

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1920-480: A major expansion of grass-grazer ecosystems . Herds of large, swift grazers were hunted by predators across broad sweeps of open grasslands , displacing desert, woodland, and browsers . The higher organic content and water retention of the deeper and richer grassland soils , with long-term burial of carbon in sediments, produced a carbon and water vapor sink. This, combined with higher surface albedo and lower evapotranspiration of grassland, contributed to

2080-678: A neutral Indian state in the American Old Northwest, and made this demand as late as 1814 at the peace negotiations at Ghent. The Americans rejected the idea, the British dropped it, and Britain's Indian allies lost British support. In addition, the Indians were no longer able to gather furs in American territory. Abandoned by their powerful sponsor, Great Lakes-area natives ultimately assimilated into American society, migrated to

2240-531: A reference to the colour of the rocks when it rains, or the name of a community built on the cliffsides here during the Fraser Canyon Gold Rush . At the site that once housed railway workers, a tourist attraction built in 1971 takes visitors across Hell's Gate via an aerial tramway . At Siska , a few minutes south of Lytton, there are the Cisco bridges —a pair of railway bridges at the throat of

2400-532: A right of access." More than 6,000 First Nations, Inuit and Métis served with British forces during First World War and Second World War . A generation of young native men fought on the battlefields of Europe during the Great War and approximately 300 of them died there. When Canada declared war on Germany on September 10, 1939, the native community quickly responded to volunteer. Four years later, in May 1943,

2560-719: A rocky gorge. From south to north, the Canadian Pacific has been on the west side of the canyon, while the Canadian National has been on the east side. At Siska, the two railways switch sides: the CP—160-metre-long (520 ft) truss bridge—crosses to the east, the CN—on an 250-metre (810 ft) steel-arched bridge over the CP—is now on the west. The two railways now have an agreement to allow directional running through

2720-679: A shantytown of the same name, much of which was on catwalks on the ramparts of its dark-rock cliffs. Nearly all tributaries of the Fraser have canyons of varying scale; the few exceptions include the Pitt and the Chilliwack in the Lower Fraser Valley. The Thompson Canyon , from Lytton to Ashcroft , is a sequence of large canyons of its own, some of them also named, although most British Columbians and travellers think of it as part of

2880-602: A significant drop in atmospheric carbon dioxide levels. Both continental and oceanic thermal gradients in mid-latitudes during the Early Miocene were very similar to those in the present. Global cooling caused the East Asian Summer Monsoon (EASM) to begin to take on its modern form during the Early Miocene. From 22.1 to 19.7 Ma, the Xining Basin experienced relative warmth and humidity amidst

3040-700: A significant local decline along the northeastern coast of Australia during the Tortonian, most likely due to warming seawater. Cetaceans attained their greatest diversity during the Miocene, with over 20 recognized genera of baleen whales in comparison to only six living genera. This diversification correlates with emergence of gigantic macro-predators such as megatoothed sharks and raptorial sperm whales . Prominent examples are O. megalodon and L. melvillei . Other notable large sharks were O. chubutensis , Isurus hastalis , and Hemipristis serra . Crocodilians also showed signs of diversification during

3200-704: A variant of Métis . The Métis as of 2013 predominantly speak English , with French a strong second language, as well as numerous Aboriginal tongues. Métis French is best preserved in Canada, Michif in the United States, notably in the Turtle Mountain Indian Reservation of North Dakota , where Michif is the official language of the Métis that reside on this Chippewa reservation. The encouragement and use of Métis French and Michif

3360-491: A wide range of chemical effects, including severe mercury poisoning. They suffered low birth rates, skewed birth-gender ratio, and health effects among the population. This led to legislation and eventually the Indian Health Transfer Policy that provided a framework for the assumption of control of health services by First Nations people, and set forth a developmental approach to transfer centred on

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3520-651: A zone of low rainfall in the Late Miocene. The Indian Plate continued to collide with the Eurasian Plate , creating new mountain ranges and uplifting the Tibetan Plateau , resulting in the rain shadowing and aridification of the Asian interior. The Tian Shan experienced significant uplift in the Late Miocene, blocking westerlies from coming into the Tarim Basin and drying it as a result. At

3680-575: Is a misnomer, given to Indigenous peoples of North America by European explorers who erroneously thought they had landed in the East Indies . The use of the term Native Americans , which the government and others have adopted in the United States, is not common in Canada. It refers more specifically to the Indigenous peoples residing within the boundaries of the US. The parallel term Native Canadian

3840-498: Is a term used to identify Indigenous peoples in Canada who are neither Inuit nor Métis . Traditionally, First Nations in Canada were peoples who lived south of the tree line , and mainly south of the Arctic Circle . There are 634 recognized First Nations governments or bands across Canada. Roughly half are located in the provinces of Ontario and British Columbia . Under Charter jurisprudence , First Nations are

4000-595: Is considered a canyon town and to be the southern outlet of the canyon because the highway became more difficult from that point; the river is navigable to Yale). Between the Spuzzum and Boston Bar was known in the gold rush as the Big Canyon or Black Canyon; there are several named subcanyons of the Big Canyon, most famously Hells Gate Canyon (in some descriptions the Black Canyon is below Hell's Gate). Above

4160-651: Is growing due to outreach within the five provincial Métis councils after at least a generation of steep decline. Canada's Indian and Northern Affairs define Métis to be those persons of mixed First Nation and European ancestry. Allied with the French, the first nations of the Wabanaki Confederacy of Acadia fought six colonial wars against the British and their native allies (See the French and Indian Wars , Father Rale's War and Father Le Loutre's War ). In

4320-423: Is navigable between Boston Bar and Lillooet and also between Big Bar Ferry and Prince George and beyond, although rapids at Soda Canyon and elsewhere were still difficult waters for the many steamboats which piloted the river in the 19th and early 20th centuries. The first sternwheeler to pass the rapids was Skuzzy , which was built with a multiple-compartment hull to preserve her from sinking from rock damage. She

4480-786: Is not commonly used, but Native (in English) and Autochtone (in Canadian French ; from the Greek auto , own, and chthon , land) 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. Bands and nations may have slightly different meanings. Within Canada,

4640-513: Is not well defined. The earliest accounts of contact occurred in the late 10th century, between the Beothuk and Norsemen . According to the Sagas of Icelanders , the first European to see what is now Canada was Bjarni Herjólfsson , who was blown off course en route from Iceland to Greenland in the summer of 985 or 986 CE. The first European explorers and settlers of what is now Canada relied on

4800-568: Is on the west coast of Vancouver Island . In pre-contact and early post-contact times, the number of nations was much greater, but smallpox and other consequences of contact resulted in the disappearance of groups, and the absorption of others into neighbouring groups. The Nuu-chah-nulth are relations of the Kwakwaka'wakw , the Haisla , and the Ditidaht . The Nuu-chah-nulth language is part of

4960-596: Is passed on through oral tradition of the Squamish indigenous peoples of the Pacific Northwest Coast . Prior to colonization and the introduction of writing had only oral tradition as a way to transmit stories, law, and knowledge across generations. The writing system established in the 1970s uses the Latin alphabet as a base. Knowledgeable elders have the responsibility to pass historical knowledge to

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5120-513: Is the only tunnel that does not have lights, while the China Bar tunnel is the only tunnel that requires ventilation. The China Bar and Alexandra tunnels have warning lights that are activated by cyclists before they enter the tunnels. This was required because the tunnels are curved. It is expected that the Ferrabee tunnel will get the same warning lights as it too is curved. At the mouth of

5280-495: The Citizenship Act was amended to grant formal citizenship to Status Indians and Inuit, retroactively as of January 1947. In 1960, First Nations people received the right to vote in federal elections without forfeiting their Indian status. By comparison, Native Americans in the United States had been allowed to vote since the 1920s. In his 1969 White Paper , then- Minister of Indian Affairs , Jean Chrétien , proposed

5440-628: The Atlantic coast. Together with other Anicinàpek, they arrived at the "First Stopping Place" near Montreal. While the other Anicinàpe peoples continued their journey up the St. Lawrence River , the Algonquins settled along the Ottawa River ( Kitcisìpi ), an important highway for commerce, cultural exchange, and transportation. A distinct Algonquin identity, though, was not realized until after

5600-608: The British Parliament's Slavery Abolition Act finally abolished slavery in all parts of the British Empire . Historian Marcel Trudel has documented 4,092 recorded slaves throughout Canadian history, of which 2,692 were Aboriginal people, owned by the French, and 1,400 blacks owned by the British, together owned by approximately 1,400 masters. Trudel also noted 31 marriages took place between French colonists and Aboriginal slaves. British agents worked to make

5760-697: The Cowichan and Fraser rivers, and those from Saskatchewan managed to produce good harvests. Since 1881, those First Nations people living in the prairie provinces required permits from Indian Agents to sell any of their produce. Later the government created a pass system in the old Northwest Territories that required indigenous people to seek written permission from an Indian Agent before leaving their reserves for any length of time. Indigenous people regularly defied those laws, as well as bans on Sun Dances and potlatches, in an attempt to practice their culture. The 1930 Constitution Act or Natural Resources Acts

5920-547: The District of Saskatchewan under Riel against the Dominion of Canada, which they believed had failed to address their concerns for the survival of their people. In 1884, 2,000 Cree from reserves met near Battleford to organize into a large, cohesive resistance. Discouraged by the lack of government response but encouraged by the efforts of the Métis at armed rebellion, Wandering Spirit and other young militant Cree attacked

6080-668: The Great Lakes and the Illinois Country . The alliance involved French settlers on the one side, and on the other side were the Abenaki, Odawa, Menominee , Ho-Chunk (Winnebago), Mississaugas , Illiniwek , Huron- Petun , Potawatomi etc. It allowed the French and the Indians to form a haven in the middle- Ohio valley before the open conflict between the European powers erupted. In the Royal Proclamation of 1763 ,

6240-481: The International Commission on Stratigraphy : Regionally, other systems are used, based on characteristic land mammals; some of them overlap with the preceding Oligocene and following Pliocene Epochs: Continents continued to drift toward their present positions. Of the modern geologic features, only the land bridge between South America and North America was absent, although South America

6400-707: The Liberals began to back away from the 1969 White Paper, particularly after the Calder case decision in 1973. After the Canadian Supreme Court recognized that indigenous rights and treaty rights were not extinguished, a process was begun to resolve land claims and treaty rights and is ongoing today. In 1970, severe mercury poisoning , called Ontario Minamata disease , was discovered among Asubpeeschoseewagong First Nation and Wabaseemoong Independent Nations people, who lived near Dryden, Ontario . There

6560-552: The Makah tribe practising death by starvation as punishment and Pacific coast tribes routinely performing ritualized killings of slaves as part of social ceremonies into the mid-1800s. Slave-owning tribes of the fishing societies, such as the Yurok and Haida lived along the coast from what is now Alaska to California . Fierce warrior indigenous slave-traders of the Pacific Northwest Coast raided as far south as California. Slavery

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6720-559: The Middle Miocene Climate Transition (MMCT). Abrupt increases in opal deposition indicate this cooling was driven by enhanced drawdown of carbon dioxide via silicate weathering. The MMCT caused a sea surface temperature (SST) drop of approximately 6 °C in the North Atlantic. The drop in benthic foraminiferal δ O values was most noticeable in the waters around Antarctica, suggesting cooling

6880-586: The North Saskatchewan River and purchased a great deal of European trade goods through Cree middlemen from the Hudson's Bay Company . The lifestyle of this group was semi-nomadic, and they followed the herds of bison during the warmer months. They traded with European traders, and worked with the Mandan , Hidatsa , and Arikara tribes. In the earliest oral history , the Algonquins were from

7040-418: The North-West Territories . Offended by the concepts of the treaties, Cree chiefs resisted them. Big Bear refused to sign Treaty 6 until starvation among his people forced his hand in 1882. His attempts to unite Indigenous nations made progress. In 1884 the Métis (including the Anglo-Métis) asked Louis Riel to return from the United States, where he had fled after the Red River Rebellion , to appeal to

7200-489: The Old World . Around the end of this epoch, the ancestors of humans had split away from the ancestors of the chimpanzees and had begun following their own evolutionary path during the final Messinian Stage (7.5–5.3 Ma) of the Miocene. As in the Oligocene before it, grasslands continued to expand, and forests to dwindle. In the seas of the Miocene, kelp forests made their first appearance and soon became one of Earth's most productive ecosystems. The plants and animals of

7360-424: The Three Sisters ( maize / beans / squash ), the Iroquois became powerful because of their confederacy. Gradually the Algonquians adopted agricultural practises enabling larger populations to be sustained. The Assiniboine were close allies and trading partners of the Cree, engaging in wars against the Gros Ventres alongside them, and later fighting the Blackfoot. A Plains people, they went no further north than

7520-405: The Treaty of Tordesillas , these two kingdoms decided to draw the dividing line running north–south, 370 leagues (from 1,500 to 2,200 km (930 to 1,370 mi) approximately depending on the league used) west of the Cape Verde Islands. Land to the west would be Spanish, to the east Portuguese. Given the uncertain geography of the day, this seemed to give the "new founde isle" to Portugal. On

7680-477: The Wakashan language group. In 1999 the discovery of the body of Kwäday Dän Ts'ìnchi provided archaeologists with significant information on indigenous tribal life prior to extensive European contact. Kwäday Dän Ts'ìnchi (meaning "Long Ago Person Found" in Southern Tutchone ), or "Canadian Ice Man", is a naturally mummified body that a group of hunters found in Tatshenshini-Alsek Provincial Park in British Columbia. Radiocarbon dating of artifacts found with

7840-448: The carbon cycle occurred approximately 6 Ma, causing continental carbon reservoirs to no longer expand during cold spells, as they had done during cold periods in the Oligocene and most of the Miocene. At the end of the Miocene, global temperatures rose again as the amplitude of Earth's obliquity increased, which caused increased aridity in Central Asia. Around 5.5 Ma, the EAWM underwent a period of rapid intensification. Life during

8000-482: The 1502 Cantino map , Newfoundland appears on the Portuguese side of the line (as does Brazil). An expedition captured about 60 Aboriginal people as slaves who were said to "resemble gypsies in colour, features, stature and aspect; are clothed in the skins of various animals ...They are very shy and gentle, but well formed in arms and legs and shoulders beyond description ...." Some captives, sent by Gaspar Corte-Real , reached Portugal. The others drowned, with Gaspar, on

8160-424: The 17th, 18th and 19th centuries and Europeans , mainly French. The Métis were historically the children of French fur traders and Nehiyaw women or, from unions of English or Scottish traders and Northern Dene women ( Anglo-Métis ). The Métis spoke or still speak either Métis French or a mixed language called Michif . Michif , Mechif or Métchif is a phonetic spelling of the Métis pronunciation of Métif ,

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8320-622: The 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of Discovery 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 an understanding of ancient cultures and historic peoples. Collectively, First Nations (Indians), Inuit, and Métis peoples constitute Indigenous peoples in Canada , Indigenous peoples of

8480-410: The 19th century, the Canadian Indian residential school system was intended to force the assimilation of Aboriginal and First Nations people into European-Canadian society. The purpose of the schools, which separated children from their families, has been described by commentators as "killing the Indian in the child." Funded under the Indian Act by Indian and Northern Affairs Canada, a branch of

8640-445: The 20th century of cultural genocide and ethnocide . There was widespread physical and sexual abuse . Overcrowding, poor sanitation, and a lack of medical care led to high rates of tuberculosis , and death rates of up to 69%. Details of the mistreatment of students had been published numerous times throughout the 20th century, but following the closure of the schools in the 1960s, the work of indigenous activists and historians led to

8800-414: The Americas , or " first peoples ". First Nation as a term became officially used by the government beginning in 1980s to replace the term Indian band in referring to groups of Indians with common government and language. The First Nations people had begun to identify by this term during 1970s activism, in order to avoid using the word Indian , which some considered offensive. No legal definition of

8960-449: The Atlantic coast were the Beothuk , Maliseet , Innu , Abenaki and Mi'kmaq . The Blackfoot Confederacy resides in the Great Plains of Montana and Canadian provinces of Alberta , British Columbia and Saskatchewan . The name Blackfoot came from the dye or paint on the bottoms of their leather moccasins . One account claimed that the Blackfoot Confederacies walked through the ashes of prairie fires, which in turn blackened

9120-491: The Beothuk disappeared entirely. There are reports of contact made before Christopher Columbus between the first peoples and those from other continents. Even in Columbus' time there was much speculation that other Europeans had made the trip in ancient or contemporary times; Gonzalo Fernández de Oviedo y Valdés records accounts of these in his General y natural historia de las Indias of 1526, which includes biographical information on Columbus. Aboriginal first contact period

9280-406: The Big Canyon there are the Lillooet Canyon, Fountain Canyon, Glen Fraser Canyon, Moran Canyon, High Bar Canyon, French Bar Canyon and more all the way up to Soda Creek Canyon near Quesnel . Upstream from there the river flows in wider country, but in the Robson Valley between Prince George and Tête Jaune Cache , the river enters the Grand Canyon of the Fraser . The Black Canyon was the site of

9440-422: The British agents discouraged any warlike activities or raids on American settlements, but the Americans became increasingly angered, and this became one of the causes of the War of 1812 . In the war, the great majority of First Nations supported the British, and many fought under the aegis of Tecumseh . But Tecumseh died in battle in 1813 and the Indian coalition collapsed. The British had long wished to create

9600-417: The British ceded the Old Northwest to the United States in the Treaty of Paris in 1783, it kept fortifications and trading posts in the region until 1795. The British then evacuated American territory, but operated trading posts in British territory, providing weapons and encouragement to tribes that were resisting American expansion into such areas as Ohio, Indiana, Michigan, Illinois and Wisconsin. Officially,

9760-471: The British recognized the treaty rights of the indigenous populations and resolved to only settle those areas purchased lawfully from the indigenous peoples. Treaties and land purchases were made in several cases by the British, but the lands of several indigenous nations remain unceded and/or unresolved. First Nations routinely captured slaves from neighbouring tribes. Sources report that the conditions under which First Nations slaves lived could be brutal, with

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9920-408: The Canyon, an archeological site documents the presence of the Stó:lō people in the area from the early Holocene period, 8,000 to 10,000 years ago after the retreat of the Fraser Glacier . Research farther upriver at the Keatley Creek Archaeological Site , near Pavilion, is dated to 8000 BP, when a huge lake filled what is now the canyon above Lillooet, created by a slide a few miles south of

10080-412: The Carolinas all stimulated destructive wars over land with their immediate Indian neighbors...Settlement patterns in New France also curtailed the kind of relentless and destructive expansion and land-grabbing that afflicted many British colonies." The Métis (from French métis – "mixed") are descendants of unions between Cree , Ojibwe , Algonquin , Saulteaux , Menominee and other First Nations in

10240-417: The Central Paratethys, cut off from sources of freshwater input by its separation from the Eastern Paratethys. From 13.36 to 12.65 Ma, the Central Paratethys was characterised by open marine conditions, before the reopening of the Bârlad Strait resulted in a shift to brackish-marine conditions in the Central Paratethys, causing the Badenian-Sarmatian Extinction Event. As a result of the Bârlad Strait's reopening,

10400-435: The Creator, or in the Squamish language keke7nex siyam . He called this man his brother. It was from these two men that the population began to rise and the Squamish spread back through their territory. The Iroquois influence extended from northern New York into what are now southern Ontario and the Montreal area of modern Quebec. The Iroquois Confederacy is, from oral tradition, formed circa 1142. Adept at cultivating

10560-721: The Early to the Middle Miocene. Europe's large mammal diversity significantly declined during the Late Miocene. In the Early Miocene, several Oligocene groups were still diverse, including nimravids , entelodonts , and three-toed equids. As in the previous Oligocene Epoch, oreodonts were still diverse, only to disappear in the earliest Pliocene. During the later Miocene mammals were more modern, with easily recognizable canids , bears , red pandas , procyonids , equids , beavers , deer , camelids , and whales , along with now-extinct groups like borophagine canids , certain gomphotheres , three-toed horses , and hornless rhinos like Teleoceras and Aphelos . The late Miocene also marks

10720-402: The East Antarctic Ice Sheet (EAIS) was highly dynamic during the Early Miocene. The Miocene began with the Early Miocene Cool Event (Mi-1) around 23 million years ago, which marked the start of the Early Miocene Cool Interval (EMCI). This cool event occurred immediately after the Oligocene-Miocene Transition (OMT) during a major expansion of Antarctica's ice sheets, but was not associated with

10880-399: The East Asian Winter Monsoon (EAWM) became stronger synchronously with a southward shift of the subarctic front. Greenland may have begun to have large glaciers as early as 8 to 7 Ma, although the climate for the most part remained warm enough to support forests there well into the Pliocene. Zhejiang, China was noticeably more humid than today. In the Great Rift Valley of Kenya , there

11040-409: The First Nations into military allies of the British, providing supplies, weapons, and encouragement. During the American Revolutionary War (1775–1783) most of the tribes supported the British. In 1779, the Americans launched a campaign to burn the villages of the Iroquois in New York State. The refugees fled to Fort Niagara and other British posts, with some remaining permanently in Canada. Although

11200-421: The First Nations peoples, for resources and trade to sustain a living. The first written accounts of interaction show a predominantly Old world bias, labelling the indigenous peoples as "savages", although the indigenous peoples were organized and self-sufficient. In the early days of contact, the First Nations and Inuit populations welcomed the Europeans, assisting them in living off the land and joining forces with

11360-431: The Fraser Canyon. Other important canyons on tributaries include Coquihalla Canyon , the Bridge River Canyon, Seton Canyon and adjacent Cayoosh Canyon , Pavilion Canyon , Vermilion Canyon (Slok Creek) and Churn Creek Canyon . The Chilcotin River also has several subcanyons, as does the Chilko River , notably Lava Canyon and another Black Canyon. There are other canyons on the Fraser that are not considered part of

11520-403: The Fraser is only one treacherous switchback rapid in a shallow rock gorge, and it has neither the roughness of water nor the depth and severity of canyon as is found in the area south from Big Bar to Lillooet or between Boston Bar and Yale. Almost all of the rivers and creeks feeding the Fraser from Williams Lake south have their own canyons which open onto the Fraser, or are just up side-valleys

11680-681: The French and British in their various battles. It was not until the colonial and imperial forces of Britain and France established dominant settlements and, no longer needing the help of the First Nations people, began to break treaties and force them off the land that the antagonism between the two groups grew. The Portuguese Crown claimed that it had territorial rights in the area visited by Cabot. In 1493 Pope Alexander VI – assuming international jurisdiction – had divided lands discovered in America between Spain and Portugal. The next year, in

11840-460: The LMC; extratropical sea surface temperatures dropped substantially by approximately 7–9 °C. 41 kyr obliquity cycles became the dominant orbital climatic control 7.7 Ma and this dominance strengthened 6.4 Ma. Benthic δ O values show significant glaciation occurred from 6.26 to 5.50 Ma, during which glacial-interglacial cycles were governed by the 41 kyr obliquity cycle. A major reorganisation of

12000-523: The Late Cretaceous, are known from the Miocene of Patagonia, represented by the mole-like Necrolestes . The youngest known representatives of metatherians (the broader grouping to which marsupials belong) in Europe, Asia and Africa are known from the Miocene, including the European herpetotheriid Amphiperatherium , the peradectids Siamoperadectes and Sinoperadectes from Asia, and

12160-705: The Late Miocene, the Earth's climate began to display a high degree of similarity to that of the present day . The 173 kyr obliquity modulation cycle governed by Earth's interactions with Saturn became detectable in the Late Miocene. By 12 Ma, Oregon was a savanna akin to that of the western margins of the Sierra Nevada of northern California . Central Australia became progressively drier, although southwestern Australia experienced significant wettening from around 12 to 8 Ma. The South Asian Winter Monsoon (SAWM) underwent strengthening ~9.2–8.5 Ma. From 7.9 to 5.8 Ma,

12320-676: The Mediterranean Sea to almost completely evaporate. This event is referred to as the " Messinian salinity crisis ". Then, at the Miocene–Pliocene boundary, the Strait of Gibraltar opened, and the Mediterranean refilled. That event is referred to as the " Zanclean flood ". Also during the early Miocene (specifically the Aquitanian and Burdigalian Stages), the apes first evolved, began diversifying, and became widespread throughout

12480-574: The Miocene Epoch was mostly supported by the two newly formed biomes , kelp forests and grasslands . Grasslands allow for more grazers, such as horses , rhinoceroses , and hippos . Ninety-five percent of modern plants existed by the end of this epoch . Modern bony fish genera were established. A modern-style latitudinal biodiversity gradient appeared ~15 Ma. The coevolution of gritty , fibrous, fire-tolerant grasses and long-legged gregarious ungulates with high-crowned teeth , led to

12640-590: The Miocene were recognizably modern. Mammals and birds were well established. Whales , pinnipeds , and kelp spread. The Miocene is of particular interest to geologists and palaeoclimatologists because major phases of the geology of the Himalaya occurred during that epoch, affecting monsoonal patterns in Asia, which were interlinked with glacial periods in the northern hemisphere. The Miocene faunal stages from youngest to oldest are typically named according to

12800-449: The Miocene. The largest form among them was a gigantic caiman Purussaurus which inhabited South America. Another gigantic form was a false gharial Rhamphosuchus , which inhabited modern age India . A strange form, Mourasuchus also thrived alongside Purussaurus . This species developed a specialized filter-feeding mechanism, and it likely preyed upon small fauna despite its gigantic size. The youngest members of Sebecidae ,

12960-550: The North American Great Plains and in Argentina . The global trend was towards increasing aridity caused primarily by global cooling reducing the ability of the atmosphere to absorb moisture, particularly after 7 to 8 million years ago. Uplift of East Africa in the late Miocene was partly responsible for the shrinking of tropical rain forests in that region, and Australia got drier as it entered

13120-720: The Oligocene–Miocene transgression. As the southern Andes rose in the Middle Miocene (14–12 million years ago) the resulting rain shadow originated the Patagonian Desert to the east. Far northern Australia was monsoonal during the Miocene. Although northern Australia is often believed to have been much wetter during the Miocene, this interpretation may be an artefact of preservation bias of riparian and lacustrine plants; this finding has itself been challenged by other papers. Western Australia, like today,

13280-547: The Port Royal settlement. Champlain persuaded First Nations to allow him to settle along the St. Lawrence, where in 1608 he would found France's first permanent colony in Canada at Quebec City. The colony of Acadia grew slowly, reaching a population of about 5,000 by 1713. New France had cod -fishery coastal communities, and farm economies supported communities along the St. Lawrence River. French voyageurs travelled deep into

13440-617: The Qiongdongnan Basin in the northern South China Sea indicates the Pearl River was a major source of sediment flux into the sea during the Early Miocene and was a major fluvial system as in the present. During the Oligocene and Early Miocene, the coast of northern Brazil, Colombia, south-central Peru , central Chile and large swathes of inland Patagonia were subject to a marine transgression . The transgressions in

13600-682: The abolition of the Indian Act of Canada, the rejection of Aboriginal land claims , and the assimilation of First Nations people into the Canadian population with the status of "other ethnic minorities" rather than as a distinct group. Harold Cardinal and the Indian Chiefs of Alberta responded with a document entitled "Citizens Plus" but commonly known as the "Red Paper". In it, they explained Status Indians' widespread opposition to Chrétien's proposal. Prime Minister Pierre Trudeau and

13760-497: The activity of the Columbia River Basalts and enhanced by decreased albedo from the reduction of deserts and expansion of forests. Climate modelling suggests additional, currently unknown, factors also worked to create the warm conditions of the MMCO. The MMCO saw the expansion of the tropical climatic zone to much larger than its current size. The July ITCZ, the zone of maximal monsoonal rainfall, moved to

13920-602: The age of 35 ). By 1790 the abolition movement was gaining ground in Canada and the ill intent of slavery was evidenced by an incident involving a slave woman being violently abused by her slave owner on her way to being sold in the United States. The Act Against Slavery of 1793 legislated the gradual abolition of slavery: no slaves could be imported; slaves already in the province would remain enslaved until death, no new slaves could be brought into Upper Canada , and children born to female slaves would be slaves but must be freed at age 25. The act remained in force until 1833 when

14080-472: The aridity of the former. Unequivocally-recognizable dabbling ducks , plovers , typical owls , cockatoos and crows appear during the Miocene. By the epoch's end, all or almost all modern bird groups are believed to have been present; the few post-Miocene bird fossils which cannot be placed in the evolutionary tree with full confidence are simply too badly preserved, rather than too equivocal in character. Marine birds reached their highest diversity ever in

14240-638: The beginning of the Miocene, the northern margin of the Arabian plate, then part of the African landmass, collided with Eurasia; as a result, the Tethys seaway continued to shrink and then disappeared as Africa collided with Eurasia in the Turkish – Arabian region. The first step of this closure occurred 20 Ma, reducing water mass exchange by 90%, while the second step occurred around 13.8 Ma, coincident with

14400-472: The body placed the age of the find between 1450 AD and 1700 AD. Genetic testing showed that he was a member of the Champagne and Aishihik First Nations . Aboriginal people in Canada interacted with Europeans as far back as 1000 AD, but prolonged contact came only after Europeans established permanent settlements in the 17th and 18th centuries. European written accounts noted friendliness on

14560-460: The bottoms of their moccasins. They had migrated onto the Great Plains (where they followed bison herds and cultivated berries and edible roots) from the area of now eastern Canada and the northeastern United States. Historically, they allowed only legitimate traders into their territory, making treaties only when the bison herds were exterminated in the 1870s. Pre-contact Squamish history

14720-514: The canoe routes west and a land route to the west coast. According to the oral history, seven great miigis (radiant/iridescent) beings appeared to the peoples in the Waabanakiing to teach the peoples of the mide way of life. One of the seven great miigis beings was too spiritually powerful and killed the peoples in the Waabanakiing when the people were in its presence. The six great miigis beings remained to teach while

14880-520: The canyon as far as Basque. All eastbound trains—CN, CP, and Via Rail's eastbound Canadian —run on the CP line. All westbound trains—CN, CP, Via Rail's westbound Canadian —use the CN tracks. Just north of Lillooet, narrow rock ledges choke the river just at the confluence of the lower canyon of the Bridge River , forming an obstacle to migrating fish that has made this spot the busiest aboriginal fishing site on

15040-666: The canyon's side-crevasses spanned by bridges and trestles. Prior to the double-tracking of those railways and major upgrades to Highway 1 (the Trans Canada Highway), travel through the canyon was even more precarious than it is now. During the frontier era it was a major obstacle between the Lower Mainland and the Interior Plateau, and the slender trails along its rocky walls – many of them little better than notches cut into granite, with

15200-606: The canyon, notably at Soda Creek , between Williams Lake and Prince George. The official but comparatively diminutive Grand Canyon of the Fraser is in the river's upper stretch through the Rocky Mountain Trench , about 115 km (71 mi) upstream from Prince George and about 20 km (12 mi) upstream from the Fraser's confluence with the Bowron River . Despite its name, the Grand Canyon of

15360-433: The concept of self-determination in health. Through this process, the decision to enter into transfer discussions with Health Canada rests with each community. Once involved in transfer, communities are able to take control of health programme responsibilities at a pace determined by their individual circumstances and health management capabilities. The capacity, experience and relationships developed by First Nations as

15520-501: The construction of the Canadian Pacific Railway brought large numbers of European settlers west who encroached on Indigenous territory. European Canadians established governments, police forces, and courts of law with different foundations from indigenous practices. Various epidemics continued to devastate Indigenous communities. All of these factors had a profound effect on Indigenous people, particularly those from

15680-577: The course of this epoch . The youngest representatives of Choristodera , an extinct order of aquatic reptiles that first appeared in the Middle Jurassic , are known from the Miocene of Europe, belonging to the genus Lazarussuchus , which had been the only known surviving genus of the group since the beginning of the Eocene. The last known representatives of the archaic primitive mammal order Meridiolestida , which dominated South America during

15840-533: The development of agriculture, the surest foundation of a colony in the New World. According to David L. Preston , after French colonisation with Champlain "the French were able to settle in the depopulated St. Lawrence Valley, not directly intruding on any Indian nation's lands. This geographic and demographic fact presents a striking contrast to the British colonies' histories: large numbers of immigrants coming to New England, New York, Pennsylvania, Virginia, and

16000-491: The dividing of the Anicinàpek at the "Third Stopping Place", estimated at 2,000 years ago near present-day Detroit . According to their tradition, and from recordings in birch bark scrolls ( wiigwaasabak ), Ojibwe (an Algonquian-speaking people) came from the eastern areas of North America, or Turtle Island , and from along the east coast. They traded widely across the continent for thousands of years and knew of

16160-631: The early to mid Miocene (23–15 Ma). Oceans cooled partly due to the formation of the Antarctic Circumpolar Current , and about 15 million years ago the ice cap in the southern hemisphere started to grow to its present form. The Greenland ice cap developed later, in the Middle Pliocene time, about 3 million years ago. First Nations in Canada First Nations ( French : Premières Nations )

16320-578: The end of the Miocene due to increased habitat uniformity. The expansion of grasslands in North America also led to an explosive radiation among snakes. Previously, snakes were a minor component of the North American fauna, but during the Miocene, the number of species and their prevalence increased dramatically with the first appearances of vipers and elapids in North America and the significant diversification of Colubridae (including

16480-554: The end of the Miocene. The Paratethys underwent a significant transgression during the early Middle Miocene. Around 13.8 Ma, during a global sea level drop, the Eastern Paratethys was cut off from the global ocean by the closure of the Bârlad Strait, effectively turning it into a saltwater lake. From 13.8 to 13.36 Ma, an evaporite period similar to the later Messinian salinity crisis in the Mediterranean ensued in

16640-637: The enigmatic Saint Bathans Mammal . Microbial life in the igneous crust of the Fennoscandian Shield shifted from being dominated by methanogens to being primarily composed of sulphate-reducing prokaryotes . The change resulted from fracture reactivation during the Pyrenean-Alpine orogeny, enabling sulphate-reducing microbes to permeate into the Fennoscandian Shield via descending surficial waters. Diatom diversity

16800-461: The evolution of both groups into modern representatives. The early Miocene Saint Bathans Fauna is the only Cenozoic terrestrial fossil record of the landmass, showcasing a wide variety of not only bird species, including early representatives of clades such as moa , kiwi and adzebills , but also a diverse herpetofauna of sphenodontians , crocodiles and turtles as well as a rich terrestrial mammal fauna composed of various species of bats and

16960-499: The expansion of grasslands not to a CO 2 drop but to the increasing seasonality and aridity, coupled with a monsoon climate, which made wildfires highly prevalent compared to before. The Late Miocene expansion of grasslands had cascading effects on the global carbon cycle, evidenced by the imprint it left in carbon isotope records. Cycads between 11.5 and 5 million years ago began to rediversify after previous declines in variety due to climatic changes, and thus modern cycads are not

17120-718: The extinction of the last-surviving members of the hyaenodonts . Islands began to form between South and North America in the Late Miocene, allowing ground sloths like Thinobadistes to island-hop to North America. The expansion of silica-rich C 4 grasses led to worldwide extinctions of herbivorous species without high-crowned teeth . Mustelids diversified into their largest forms as terrestrial predators like Ekorus , Eomellivora , and Megalictis and bunodont otters like Enhydriodon and Sivaonyx appeared. Eulipotyphlans were widespread in Europe, being less diverse in Southern Europe than farther north due to

17280-574: The federal government, the schools were run by churches of various denominations – about 60% by Roman Catholics, and 30% by the Anglican Church of Canada and the United Church of Canada , along with its pre-1925 predecessors, Presbyterian , Congregationalist and Methodist churches. The attempt to force assimilation involved punishing children for speaking their own languages or practising their own faiths, leading to allegations in

17440-629: The findings of marine invertebrate fossils of both Atlantic and Pacific affinity in La Cascada Formation . Connection would have occurred through narrow epicontinental seaways that formed channels in a dissected topography . The Antarctic Plate started to subduct beneath South America 14 million years ago in the Miocene, forming the Chile Triple Junction . At first the Antarctic Plate subducted only in

17600-636: The fur trade, conflicts with colonial authorities and settlers and loss of land and a subsequent loss of nation self-suffiency. For example, during the late 1630s, smallpox killed more than half of the Huron , who controlled most of the early fur trade in what became Canada. Reduced to fewer than 10,000 people, the Huron Wendat were attacked by the Iroquois, their traditional enemies. In the Maritimes,

17760-521: The government declared that, as British subjects , all able Indian men of military age could be called up for training and service in Canada or overseas. Following the end of the Second World War, laws concerning First Nations in Canada began to change, albeit slowly. The federal prohibition of potlatch and Sun Dance ceremonies ended in 1951. Provincial governments began to accept the right of Indigenous people to vote. In June 1956, section 9 of

17920-524: The government on their behalf. The government gave a vague response. In March 1885, Riel, Gabriel Dumont , and Honoré Jackson (a.k.a. Will Jackson) set up the Provisional Government of Saskatchewan , believing that they could influence the federal government in the same way as they had in 1869. The North-West Rebellion of 1885 was a brief and unsuccessful uprising by the Métis people of

18080-608: The hinterlands (of what is today Quebec, Ontario, and Manitoba, as well as what is now the American Midwest and the Mississippi Valley ), trading with First Nations as they went – guns, gunpowder, cloth, knives, and kettles for beaver furs. The fur trade kept the interest in France's overseas colonies alive, yet only encouraged a small colonial population, as minimal labour was required. The trade also discouraged

18240-464: The human lineage) appeared in Africa at the very end of the Miocene, including Sahelanthropus , Orrorin , and an early form of Ardipithecus ( A. kadabba ). The chimpanzee–human divergence is thought to have occurred at this time. The evolution of bipedalism in apes at the end of the Miocene instigated an increased rate of faunal turnover in Africa. In contrast, European apes met their end at

18400-606: The lake levels of the Eastern Paratethys dropped as it once again became a sea. The Fram Strait opened during the Miocene and acted as the only throughflow for Atlantic Water into the Arctic Ocean until the Quaternary period. Due to regional uplift of the continental shelf, this water could not move through the Barents Seaway in the Miocene. The modern day Mekong Delta took shape after 8 Ma. Geochemistry of

18560-614: The late 18th century, European Canadians encouraged First Nations to assimilate into the European-based culture, referred to as " Canadian culture ". The assumption was that this was the "correct" culture because the Canadians of European descent saw themselves as dominant, and technologically, politically and culturally superior. There was resistance against this assimilation and many businesses denied European practices. The Tecumseh Wigwam of Toronto, for example, did not adhere to

18720-405: The late 20th century, members of various nations more frequently identify by their tribal or national identity only, e.g., "I'm Haida ", or "We're Kwantlens ", in recognition of the distinct First Nations. First Nations peoples had settled and established trade routes across what is now Canada by 500 BCE – 1,000 CE. Communities developed, each with its own culture, customs, and character. In

18880-491: The mountain ranges flanking the gorge. At Hells Gate , near Boston Bar , the canyon walls rise about 1,000 metres (3,300 ft) above the rapids. Fish ladders along the river's side permit migrating salmon to bypass a rockslide that diverted the river during the blasting of the Canadian Northern Railway line in 1913. The area around Hell's Gate carries the name Black Canyon, which may either be

19040-473: The mouth of the Chilcotin River there are only rough ranching roads, and the terrain is a mix of canyon depths flanked by arid benchland and high plateau. Between Pavilion and Lillooet, the river's gorge is at its maximum depth, with the river throttled through a series of narrow gorges flanked by high cliffs, though still flanked above those cliffs by wide benchlands which stand on the foreshoulder of

19200-631: The name comes from the Greek words μείων ( meíōn , "less") and καινός ( kainós , "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene followed the Oligocene and preceded the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages . The Miocene boundaries are not marked by distinct global events but by regionally defined transitions from

19360-543: The next generation. People lived and prospered for thousands of years until the Great Flood . In another story, after the Flood, they repopulated from the villages of Schenks and Chekwelp , located at Gibsons . When the water lines receded, the first Squamish came to be. The first man, named Tseḵánchten, built his longhouse in the village, and later on another man named Xelálten, appeared on his longhouse roof and sent by

19520-547: The north, increasing precipitation over southern China whilst simultaneously decreasing it over Indochina during the EASM. Western Australia was at this time characterised by exceptional aridity. In Antarctica, average summer temperatures on land reached 10 °C. In the oceans, the lysocline shoaled by approximately half of a kilometre during warm phases that corresponded to orbital eccentricity maxima. The MMCO ended around 14 million years ago, when global temperatures fell in

19680-579: The northeastern coastline of what is now the United States. Under Samuel de Champlain, the Saint Croix settlement moved to Port Royal (today's Annapolis Royal, Nova Scotia ), a new site across the Bay of Fundy , on the shore of the Annapolis Basin , an inlet in western Nova Scotia. Acadia became France's most successful colony to that time. The cancellation of Dugua's fur monopoly in 1607 ended

19840-864: The northwest were the Athapaskan-speaking peoples, Slavey , Tłı̨chǫ , Tutchone-speaking peoples, and Tlingit . Along the Pacific coast were the Haida, Tsimshian , Salish, Kwakiutl , Nuu-chah-nulth , Nisga'a and Gitxsan . In the plains were the Blackfoot, Kainai , Sarcee and Northern Peigan . In the northern woodlands were the Cree and Chipewyan . Around the Great Lakes were the Anishinaabe , Algonquin , Iroquois and Wyandot . Along

20000-633: The ocean as well. If the seventh miigis being stayed, it would have established the Thunderbird doodem . The Nuu-chah-nulth are one of the Indigenous peoples of the Pacific Northwest Coast . The term Nuu-chah-nulth is used to describe fifteen separate but related First Nations, such as the Tla-o-qui-aht First Nations , Ehattesaht First Nation and Hesquiaht First Nation whose traditional home

20160-436: The one returned into the ocean. The six great miigis beings then established doodem (clans) for the peoples in the east. Of these doodem , the five original Anishinaabe doodem were the Wawaazisii ( Bullhead ), Baswenaazhi (Echo-maker, i.e., Crane ), Aan'aawenh ( Pintail Duck ), Nooke (Tender, i.e., Bear ) and Moozoonsii (Little Moose ), then these six miigis beings returned into

20320-523: The origin of many modern genera such as Nerodia , Lampropeltis , Pituophis and Pantherophis ). Arthropods were abundant, including in areas such as Tibet where they have traditionally been thought to be undiverse. Neoisopterans diversified and expanded into areas they previously were absent from, such as Madagascar and Australia. In the oceans, brown algae , called kelp , proliferated, supporting new species of sea life, including otters , fish and various invertebrates . Corals suffered

20480-608: The part of the First Nations, who profited in trade with Europeans. Such trade strengthened the more organized political entities such as the Iroquois Confederation. The Aboriginal population is estimated to have been between 200,000 and two million in the late 15th century. The effect of European colonization was a 40 to 80 percent Aboriginal population decrease post-contact. This is attributed to various factors, including repeated outbreaks of European infectious diseases such as influenza , measles and smallpox (to which they had not developed immunity), inter-nation conflicts over

20640-440: The plains who had relied heavily on bison for food and clothing. Most of those nations that agreed to treaties had negotiated for a guarantee of food and help to begin farming. Just as the bison disappeared (the last Canadian hunt was in 1879), Lieutenant-Governor Edgar Dewdney cut rations to indigenous people in an attempt to reduce government costs. Between 1880 and 1885, approximately 3,000 Indigenous people starved to death in

20800-463: The possible herpetotheriid Morotodon from the late Early Miocene of Uganda. Approximately 100 species of apes lived during this time , ranging throughout Africa, Asia and Europe and varying widely in size, diet, and anatomy. Due to scanty fossil evidence it is unclear which ape or apes contributed to the modern hominid clade, but molecular evidence indicates this ape lived between 18 and 13 million years ago. The first hominins ( bipedal apes of

20960-424: The present-day town. During the Fraser Canyon Gold Rush of 1858–1860, 10,500 miners and an untold number of hangers-on populated its banks and towns. The Fraser Canyon War and the series of events known as McGowan's War occurred during the gold rush. Other important histories connected with the canyon include the building of the Cariboo Wagon Road and the construction of the Canadian Pacific Railway. The river

21120-437: The rest of the province, other than by the difficult wagon road to Lillooet via Fountain. During the automotive age and following the construction of the Canadian Northern Railway in 1904–05, a newer version of the road was built through the canyon. The Fraser Canyon Highway was surveyed in 1920 and constructed in 1924–25 with a through-route available after the completion of the (second) Alexandra Suspension Bridge in 1926. This

21280-403: The return voyage. Gaspar's brother, Miguel Corte-Real , went to look for him in 1502, but also failed to return. In 1604 King Henry IV of France granted Pierre Dugua, Sieur de Mons a fur-trade monopoly. Dugua led his first colonization expedition to an island located near to the mouth of the St. Croix River . Samuel de Champlain , his geographer, promptly carried out a major exploration of

21440-430: The river, from ancient times to the present. Concentrations of First Nations people here, from all tribes of the Interior, were believed to have been in excess of 10,000. Many stretches of the Fraser are named in their own right, starting with the Little Canyon between Yale and Spuzzum , which is officially the lowest reach of the Fraser Canyon (although in regional terms Hope , 32 kilometres (20 mi) farther south,

21600-529: The sale of their lands in 1916 and 1917, the Department of Indian Affairs held back funding necessary for farming until they relented. In British Columbia, the McKenna–McBride Royal Commission was created in 1912 to settle disputes over reserve lands in the province. The claims of Indigenous people were ignored, and the commission allocated new, less valuable lands (reserves) for First Nations. Those nations who managed to maintain their ownership of good lands often farmed successfully. Indigenous people living near

21760-399: The second war, Queen Anne's War , the British conquered Acadia (1710). The sixth and final colonial war between the nations of France and Great Britain (1754–1763), resulted in the French giving up their claims and the British claimed the lands of Canada (New France) . In this final war, the Franco-Indian alliance brought together Americans, First Nations and the French, centred on

21920-496: The small town of Frog Lake , killing Thomas Quinn, an Indian agent , and eight others. Although Big Bear actively opposed the attacks, he was charged and tried for treason and sentenced to three years in prison. After the Red River Rebellion of 1869–1870, Métis moved from Manitoba to the District of Saskatchewan, where they founded a settlement at Batoche on the South Saskatchewan River . In Manitoba settlers from Ontario began to arrive. They pushed for land to be allotted in

22080-462: The southern Chilcotin Group during the Pliocene period and the volcanic vents of their origins have not been discovered. The canyon extends 270 kilometres (170 mi) north of Yale to the confluence of the Chilcotin River . Its southern stretch is a major transportation corridor to the Interior from the Coast , with the Canadian National and Canadian Pacific Railways and the Trans-Canada Highway carved out of its rock faces, with many of

22240-531: The southernmost tip of Patagonia, meaning that the Chile Triple Junction lay near the Strait of Magellan . As the southern part of Nazca Plate and the Chile Rise became consumed by subduction the more northerly regions of the Antarctic Plate begun to subduct beneath Patagonia so that the Chile Triple Junction advanced to the north over time. The asthenospheric window associated to the triple junction disturbed previous patterns of mantle convection beneath Patagonia inducing an uplift of ca. 1 km that reversed

22400-522: The spring of 1957 to 1964 as part of the Trans-Canada Highway project. There are seven tunnels in total, the shortest being approximately 57 metres (187 ft); the longest, however, is approximately 610 metres (2,000 ft) and is one of North America 's longest. They are situated between Yale and Boston Bar . In order from south to north, they are: Yale (completed 1963), Saddle Rock (1958), Sailor Bar (1959), Alexandra (1964), Hell's Gate (1960), Ferrabee (1964) and China Bar (1961). The Hell's Gate tunnel

22560-447: The square concession system of English Canada , rather than the seigneurial system of strips reaching back from a river which the Métis were familiar with in their French-Canadian culture. The history of colonization is complex, varied according to the time and place. France and Britain were the main colonial powers involved, though the United States also began to extend its territory at the expense of indigenous people as well. From

22720-422: The start of the 20th century, the federal Indian policy was directed at removing Indigenous people from their communal lands and encouraging assimilation. Amendments to the Indian Act in 1905 and 1911 made it easier for the government to expropriate reserve lands from First Nations. The government sold nearly half of the Blackfoot reserve in Alberta to settlers. When the Kainai (Blood) Nation refused to accept

22880-459: The term First Nations has come into general use for Indigenous peoples other than Inuit and Métis . Outside Canada, the term can refer to Indigenous Australians , U.S. tribes within the Pacific Northwest , as well as supporters of the Cascadian independence movement . The singular, commonly used on culturally politicized reserves , is the term First Nations person (when gender-specific, First Nations man or First Nations woman ). Since

23040-422: The term exists. Some Indigenous peoples in Canada have also adopted the term First Nation to replace the word band in the formal name of their community. A band is a "body of Indians (a) for whose use and benefit in common lands ... have been set apart, (b) ... moneys are held ... or (c) declared ... to be a band for the purposes of", according to the Indian Act by the Canadian Crown . The term Indian

23200-408: The villages of the Fox nation , a tribe that was an ancient rival of the Miami people and their Algonquian allies. Native (or "pani", a corruption of Pawnee ) slaves were much easier to obtain and thus more numerous than African slaves in New France, but were less valued. The average native slave died at 18, and the average African slave died at 25 (the average European could expect to live until

23360-418: The warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and hominoids into Eurasia. During the late Miocene, the connections between the Atlantic and Mediterranean closed, causing

23520-440: The west coast of South America are thought to be caused by a regional phenomenon while the steadily rising central segment of the Andes represents an exception. While there are numerous registers of Oligocene–Miocene transgressions around the world it is doubtful that these correlate. It is thought that the Oligocene–Miocene transgression in Patagonia could have temporarily linked the Pacific and Atlantic Oceans, as inferred from

23680-404: The west or to Canada, or were relocated onto reservations in Michigan and Wisconsin. Historians have unanimously agreed that the Indians were the major losers in the War of 1812. Living conditions for Indigenous people in the prairie regions deteriorated quickly. Between 1875 and 1885, settlers and hunters of European descent contributed to hunting the North American bison almost to extinction;

23840-425: The widely practiced Lord's Day observance, making it a popular spot, especially on Sundays. Moreover, Canadian policies were at times contradictory, such as through the late 19th century- Peasant Farm Policy that severely restricted farming on reserves, despite this practice being seen as important to assimilation efforts. These kinds of attempts reached a climax in the late 19th and early 20th centuries. Founded in

24000-423: Was Allodesmus . A ferocious walrus , Pelagiarctos may have preyed upon other species of pinnipeds including Allodesmus . Furthermore, South American waters witnessed the arrival of Megapiranha paranensis , which were considerably larger than modern age piranhas . New Zealand 's Miocene fossil record is particularly rich. Marine deposits showcase a variety of cetaceans and penguins , illustrating

24160-496: Was a gradual and progressive trend of increasing aridification, though it was not unidirectional, and wet humid episodes continued to occur. Between 7 and 5.3 Ma, temperatures dropped sharply again in the Late Miocene Cooling (LMC), most likely as a result of a decline in atmospheric carbon dioxide and a drop in the amplitude of Earth's obliquity, and the Antarctic ice sheet was approaching its present-day size and thickness. Ocean temperatures plummeted to near-modern values during

24320-416: Was approaching the western subduction zone in the Pacific Ocean , causing both the rise of the Andes and a southward extension of the Meso-American peninsula. Mountain building took place in western North America , Europe , and East Asia . Both continental and marine Miocene deposits are common worldwide with marine outcrops common near modern shorelines. Well studied continental exposures occur in

24480-405: Was arid, particularly so during the Middle Miocene. Climates remained moderately warm, although the slow global cooling that eventually led to the Pleistocene glaciations continued. Although a long-term cooling trend was well underway, there is evidence of a warm period during the Miocene when the global climate rivalled that of the Oligocene . The climate of the Miocene has been suggested as

24640-516: Was extensive mercury pollution caused by Dryden Chemicals Company's waste water effluent in the Wabigoon - English River system. Because local fish were no longer safe to eat, the Ontario provincial government closed the commercial fisheries run by the First Nation people and ordered them to stop eating local fish. Previously it had made up the majority of their diet. In addition to the acute mercury poisoning in northwestern Ontario , Aamjiwnaang First Nation people near Sarnia , Ontario, experienced

24800-428: Was hereditary, the slaves and their descendants being considered prisoners of war . Some tribes in British Columbia continued to segregate and ostracize the descendants of slaves as late as the 1970s. Among Pacific Northwest tribes about a quarter of the population were slaves. The citizens of New France received slaves as gifts from their allies among First Nations peoples. Slaves were prisoners taken in raids against

24960-514: Was inversely correlated with carbon dioxide levels and global temperatures during the Miocene. Most modern lineages of diatoms appeared by the Late Miocene. There is evidence from oxygen isotopes at Deep Sea Drilling Program sites that ice began to build up in Antarctica about 36 Ma during the Eocene . Further marked decreases in temperature during the Middle Miocene at 15 Ma probably reflect increased ice growth in Antarctica. It can therefore be assumed that East Antarctica had some glaciers during

25120-432: Was known as the Cariboo Highway and Highway 1 until the construction and designation of the Trans-Canada Highway (circa-1962). Miocene The Miocene ( / ˈ m aɪ . ə s iː n , - oʊ -/ MY -ə-seen, -⁠oh- ) is the first geological epoch of the Neogene Period and extends from about 23.03 to 5.333 million years ago (Ma). The Miocene was named by Scottish geologist Charles Lyell ;

25280-464: Was most intense there. Around this time the Mi3b glacial event (a massive expansion of Antarctic glaciers) occurred. The East Antarctic Ice Sheet (EAIS) markedly stabilised following the MMCT. The intensification of glaciation caused a decoherence of sediment deposition from the 405 kyr eccentricity cycle. The MMWI ended about 11 Ma, when the Late Miocene Cool Interval (LMCI) started. A major but transient warming occurred around 10.8-10.7 Ma. During

25440-400: Was part of a shift acknowledging indigenous rights . It enabled provincial control of Crown land and allowed Provincial laws regulating game to apply to Indians, but it also ensured that "Indians shall have the right ... of hunting, trapping and fishing game and fish for food at all seasons of the year on all unoccupied Crown lands and on any other lands to which the said Indians may have

25600-438: Was used to haul equipment and supplies during the construction of the Canadian Pacific Railway, beginning in the 1880s. With the construction of the Canadian Pacific Railway in the 1880s came the destruction of key portions of the Cariboo Wagon Road , as there was no room for both railway and road on the narrow, steep mountainsides above the river. As a result, the towns of Lytton and Boston Bar were cut off from road access with

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