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176-558: The history of Canada covers the period from the arrival of the Paleo-Indians to North America thousands of years ago to the present day. The lands encompassing present-day Canada have been inhabited for millennia by Indigenous peoples , with distinct trade networks, spiritual beliefs, and styles of social organization. Some of these older civilizations had long faded by the time of the first European arrivals and have been discovered through archeological investigations. From

352-530: A Canadian culture that has also been strongly influenced by its linguistic, geographic and economic neighbour, the United States . Since the conclusion of the Second World War , Canada's strong support for multilateralism and internationalism has been closely related to its peacekeeping efforts . Archeological and Indigenous genetic evidence indicate that North and South America were

528-525: A North American fur trade monopoly was granted to Pierre Du Gua, Sieur de Mons . The fur trade became one of the main economic ventures in North America. Du Gua led his first colonization expedition to an island located near the mouth of the St. Croix River . Among his lieutenants was a geographer named Samuel de Champlain , who promptly carried out a major exploration of the northeastern coastline of what

704-884: A Native American source population related to the Ainu ancestors, the Jōmon . Paleo-Indian skeletons in the Americas such as Kennewick Man (Washington State), Hoya Negro skeleton (Yucatán), Luzia Woman and other skulls from the Lagoa Santa site (Brazil), Buhl Woman (Idaho), Peñon Woman III , two skulls from the Tlapacoya site (Mexico City), and 33 skulls from Baja California have exhibited certain craniofacial traits distinct from most modern Native Americans, leading physical anthropologists to posit an earlier "Paleoamerican" population wave. The most basic measured distinguishing trait

880-409: A band of Reformers under the leadership of William Lyon Mackenzie took up arms in a disorganized and ultimately unsuccessful series of small-scale skirmishes around Toronto, London , and Hamilton . In Lower Canada, a more substantial rebellion occurred against British rule. Both English- and French-Canadian rebels, sometimes using bases in the neutral United States, fought several skirmishes against

1056-677: A branch of Ancient East Asians migrated to Northeastern Siberia, and mixed with descendants of the ANE, leading to the emergence of Ancient Paleo-Siberian and Native American populations in Extreme Northeastern Asia. However, the Beringian standstill hypothesis is not supported by paternal DNA evidence, which may reflect different population histories for paternal and maternal lineages in Native Americans, which

1232-615: A daughter population of ancient East Asians, who they encountered around 25,000 years ago, which led to the emergence of Native American ancestral populations. However, the exact location where the admixture took place is unknown, and the migratory movements that united the two populations are a matter of debate. One theory supposes that Ancient North Eurasians migrated south to East Asia , or Southern Siberia , where they would have encountered and mixed with ancient East Asians. Genetic evidence from Lake Baikal in Russia supports this area as

1408-751: A durable and extensive geographic feature connecting Siberia with Alaska. With the rise of sea level after the Last Glacial Maximum (LGM), the Beringian land bridge was again submerged. Estimates of the final re-submergence of the Beringian land bridge based purely on present bathymetry of the Bering Strait and eustatic sea level curve place the event around 11,000 years BP (Figure 1). Ongoing research reconstructing Beringian paleogeography during deglaciation could change that estimate and possible earlier submergence could further constrain models of human migration into North America. The onset of

1584-634: A federated country in its own right. (According to James Bowden, writing in The Dorchester Review , "Ottawa turned its back on 'Dominion' in the 1940s and 1950s," impelled by what historian C.P. Champion referred to as "neo-nationalism.") Federation emerged from multiple impulses: the British wanted Canada to defend itself; the Maritimes needed railroad connections, which were promised in 1867; English-Canadian nationalism sought to unite

1760-710: A federation. This was especially pushed by the liberal Reform movement of Upper Canada and the French-Canadian Parti rouge in Lower Canada who favoured a decentralized union in comparison to the Upper Canadian Conservative party and to some degree the French-Canadian Parti bleu , which favoured a centralized union. Using the lure of the Canadian Pacific Railway , a transcontinental line that would unite

1936-575: A great difference in the number of men at 2,034 versus 1,181 women. By the early 1700s the New France settlers were well established along the shores of the St. Lawrence River and parts of Nova Scotia, with a population of around 16,000. However, new arrivals stopped coming from France in the proceeding decades, meaning that the English and Scottish settlers in Newfoundland, Nova Scotia, and

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2112-760: A group of settlers led by Paul Chomedey de Maisonneuve , who founded Ville-Marie, the precursor to present-day Montreal . In 1663 the French crown took direct control of the colonies from the Company of New France . Although immigration rates to New France remained very low under direct French control, most of the new arrivals were farmers, and the rate of population growth among the settlers themselves had been very high. The women had about 30 per cent more children than comparable women who remained in France. Yves Landry says, "Canadians had an exceptional diet for their time." This

2288-482: A lineage found among Native Americans and Han Chinese, emerged around 20,000 BP, constraining the emergence of D4h3 to post-LGM. Age estimates based on Y-chromosome micro-satellite diversity place origin of the American Haplogroup Q1a3a (Y-DNA) at around 15,000 to 10,000 BP. Greater consistency of DNA molecular evolution rate models with each other and with archaeological data may be gained by

2464-462: A long groove called a "flute". The spear points would typically be made by chipping a single flake from each side of the point. The point was then tied onto a spear of wood or bone. As the environment changed with the ice age ending around 17–13 Ka BP on short, and around 25–27 Ka BP on the long, many animals migrated overland to take advantage of the new sources of food. Humans following these animals, such as bison, mammoth and mastodon, thus gained

2640-404: A lure for coastal migration. Reconstruction of the southern Beringian coastline also suggests potential for a highly productive coastal marine environment. Pollen data indicate a warm period culminating between 17,000 and 13,000 BP followed by cooling between 13,000 and 11,500 BP. Coastal areas deglaciated rapidly as coastal alpine glaciers, then lobes of Cordilleran ice, retreated. The retreat

2816-505: A much earlier date, possibly 40,000 years ago, followed by a much later second wave of immigrants. The Clovis First theory, which dominated thinking on New World anthropology for much of the 20th century, was challenged in the 2000s by the secure dating of archaeological sites in the Americas to before 13,000 years ago. The archaeological sites in the Americas with the oldest dates that have gained broad acceptance are all compatible with an age of about 15,000 years. This includes

2992-537: A much wider geographical distribution, but mostly in the central and southern part of the continent. The haplogroup most commonly associated with Amerindian genetics is Haplogroup Q-M3 . Y-DNA , like ( mtDNA ), differs from other nuclear chromosomes in that the majority of the Y chromosome is unique and does not recombine during meiosis . This allows the historical pattern of mutations to be easily studied. The pattern indicates Indigenous Amerindians experienced two very distinctive genetic episodes: first with

3168-680: A separate colony— New Brunswick —was created in 1784; followed in 1791 by the division of Quebec into the largely French-speaking Lower Canada ( French Canada ) along the St. Lawrence River and the Gaspé Peninsula and an anglophone Loyalist Upper Canada , with its capital settled by 1796 in York (present-day Toronto ). After 1790 most of the new settlers were American farmers searching for new lands; although generally favourable to republicanism, they were relatively non-political and stayed neutral in

3344-955: A single animal species: the bison (an early cousin of the American bison ). The earliest known of these bison-oriented hunting traditions is the Folsom tradition . Folsom peoples traveled in small family groups for most of the year, returning yearly to the same springs and other favored locations on higher ground. There they would camp for a few days, perhaps erecting a temporary shelter, making and/or repairing some stone tools, or processing some meat, then moving on. Paleo-Indians were not numerous, and population densities were quite low. Paleo-Indians are generally classified by lithic reduction or lithic core "styles" and by regional adaptations. Lithic technology fluted spear points, like other spear points, are collectively called projectile points . The projectiles are constructed from chipped stones that have

3520-774: A transcontinental railway—voted no in 1869, and did not join Canada until 1949. In 1873, John A. Macdonald ( First Prime Minister of Canada ) created the North-West Mounted Police (now the Royal Canadian Mounted Police ) to help police the Northwest Territories . Specifically the Mounties were to assert Canadian sovereignty to prevent possible American encroachments into the area. The Mounties' first large-scale mission

3696-489: A variety of flora. Paleo-Indian groups were efficient hunters and carried a variety of tools. These included highly efficient fluted-style spear points, as well as microblades used for butchering and hide processing. Projectile points and hammerstones made from many sources are found traded or moved to new locations. Stone tools were traded and/or left behind from North Dakota and Northwest Territories , to Montana and Wyoming . Trade routes also have been found from

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3872-506: Is a long-standing open question. While advances in archaeology , Pleistocene geology , physical anthropology , and DNA analysis have progressively shed more light on the subject, significant questions remain unresolved. The " Clovis first theory" refers to the hypothesis that the Clovis culture represents the earliest human presence in the Americas about 13,000 years ago. Evidence of pre-Clovis cultures has accumulated and pushed back

4048-551: Is general agreement that the Americas were first settled from Asia, the pattern of migration and the place(s) of origin in Eurasia of the peoples who migrated to the Americas remain unclear. The traditional theory is that Ancient Beringians moved when sea levels were significantly lowered due to the Quaternary glaciation , following herds of now-extinct Pleistocene megafauna along ice-free corridors that stretched between

4224-540: Is less than 100%. The HTLV virus genome has been mapped, allowing identification of four major strains and analysis of their antiquity through mutations. The highest geographic concentrations of the strain HLTV-1 are in sub-Saharan Africa and Japan. In Japan, it occurs in its highest concentration on Kyushu . It is also present among African descendants and native populations in the Caribbean region and South America. It

4400-627: Is not uncommon and has been observed in other populations. A 2019 study suggested that Native Americans are the closest living relatives to 10,000-year-old fossils found near the Kolyma River in northeastern Siberia. A study published in July 2022 suggested that people in southern China may have contributed to the Native American gene pool, based on the discovery and DNA analysis of 14,000-year-old human fossils. The contrast between

4576-467: Is now Quebec City , one of the earliest permanent settlements, which would become the capital of New France. He took personal administration over the city and its affairs and sent out expeditions to explore the interior. Champlain became the first known European to encounter Lake Champlain in 1609. By 1615, he had travelled by canoe up the Ottawa River through Lake Nipissing and Georgian Bay to

4752-511: Is now Western Canada , would have allowed migration before the beginning of the Holocene . However, a 2016 study has argued against this, suggesting that the peopling of North America via such a corridor is unlikely to significantly pre-date the earliest Clovis sites. The study concludes that the ice-free corridor in what is now Alberta and British Columbia "was gradually taken over by a boreal forest dominated by spruce and pine trees" and that

4928-596: Is now the United States. In the spring of 1605, under Samuel de Champlain, the new St. Croix settlement was moved to Port Royal (today's Annapolis Royal, Nova Scotia ). Samuel de Champlain also landed at Saint John Harbour on June 24, 1604 (the feast of St. John the Baptist) and is where the city of Saint John, New Brunswick , and the Saint John River gets their name. In 1608 Champlain founded what

5104-664: Is one of the five mtDNA haplogroups found in Indigenous Americans. Native Americans mostly belong to the X2a clade, which has never been found in the Old World . According to Jennifer Raff , X2a probably originated in the same Siberian population as the other four founding maternal lineages, and that there is no compelling reason to believe it is related to X lineages found in Europe or West Eurasia. The Kennewick man fossil

5280-809: Is rare in Central America and North America. Its distribution in the Americas has been regarded as due to importation with the slave trade. The Ainu have developed antibodies to HTLV-1, indicating its endemicity to the Ainu and its antiquity in Japan. A subtype "A" has been defined and identified among the Japanese (including Ainu ), and among Caribbean and South American isolates. A subtype "B" has been identified in Japan and India. In 1995, Native Americans in coastal British Columbia were found to have both subtypes A and B. Bone marrow specimens from an Andean mummy about 1500 years old were reported to have shown

5456-537: Is the dolichocephaly of the skull. Some modern isolated populations such as the Pericúes of Baja California and the Fuegians of Tierra del Fuego exhibit that same morphological trait. Other anthropologists advocate an alternative hypothesis that evolution of an original Beringian phenotype gave rise to a distinct morphology that was similar in all known Paleoamerican skulls, followed by later convergence towards

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5632-693: The 1930 Imperial Conference and the passing of the Statute of Westminster in 1931 recognized that Canada had become co-equal with the United Kingdom. The Patriation of the Constitution in 1982 marked the removal of legal dependence on the British parliament. Canada currently consists of ten provinces and three territories and is a parliamentary democracy and a constitutional monarchy . Over centuries, elements of Indigenous, French, British and more recent immigrant customs have combined to form

5808-499: The Alexander Archipelago . The now-submerged coastal plain has potential for more refugia. Pollen data indicate mostly herb/shrub tundra vegetation in unglaciated areas, with some boreal forest towards the southern end of the range of Cordilleran ice. The coastal marine environment remained productive, as indicated by fossils of pinnipeds . The highly productive kelp forests over rocky marine shallows may have been

5984-531: The Algonquian and Iroquoian peoples. The Algonquian language is believed to have originated in the western plateau of Idaho or the plains of Montana and moved with migrants eastward, eventually extending in various manifestations all the way from Hudson Bay to what is today Nova Scotia in the east and as far south as the Tidewater region of Virginia . Speakers of eastern Algonquian languages included

6160-773: The American Revolution , there was some sympathy for the American cause among the Acadians and the New Englanders in Nova Scotia. Neither party joined the rebels, although several hundred individuals joined the revolutionary cause. An invasion of Quebec by the Continental Army in 1775, with a goal to take Quebec from British control, was halted at the Battle of Quebec by Guy Carleton , with

6336-740: The Appalachian Mountains to the Rocky Mountains . France and Spain kept the Treaty of Fontainebleau secret from other countries until 1764. However under the Treaty of Paris, the eastern side of the Mississippi river basin became British territory. Great Britain returned to France its most important sugar-producing colony, Guadeloupe , which the French considered more valuable than Canada. (Guadeloupe produced more sugar than all

6512-542: The Arctic archipelago , the distinctive Paleo-Eskimos known as Dorset peoples , whose culture has been traced back to around 500 BCE, were replaced by the ancestors of today's Inuit by 1500 CE. This transition is supported by archeological records and Inuit mythology that tells of having driven off the Tuniit or 'first inhabitants'. Inuit traditional laws are anthropologically different from Western law . Customary law

6688-507: The Atlantic coast communities and sailed into the St. Lawrence River , trading and making alliances with First Nations , as well as establishing fishing settlements such as in Percé (1603). As a result of France's claim and activities in the colony of Canada, the name Canada was found on international maps showing the existence of this colony within the St. Lawrence river region. In 1604,

6864-533: The Atlantic provinces . Official tradition deemed the first landing site to be at Cape Bonavista , Newfoundland, although other locations are possible. After 1497 Cabot and his son Sebastian Cabot continued to make other voyages to find the Northwest Passage , and other explorers continued to sail out of England to the New World, although the details of these voyages are not well recorded. Based on

7040-473: The Bering Strait from North Asia into the Americas over a land bridge ( Beringia ). This bridge existed from 45,000 to 12,000 BCE (47,000–14,000 BP ). Small isolated groups of hunter-gatherers migrated alongside herds of large herbivores far into Alaska . From c.  16,500  – c.  13,500 BCE ( c.  18,500  – c.  15,500 BP), ice-free corridors developed along

7216-480: The British Columbia Interior to the coast of California . The glaciers that covered the northern half of the continent began to gradually melt, exposing new land for occupation around 17,500–14,500 years ago. At the same time as this was occurring, worldwide extinctions among the large mammals began. In North America, camelids and equids eventually died off, the latter not to reappear on

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7392-811: The Buttermilk Creek Complex in Texas, the Meadowcroft Rockshelter site in Pennsylvania and the Monte Verde site in southern Chile. Archaeological evidence of pre- Clovis people points to the South Carolina Topper Site being 16,000 years old, at a time when the glacial maximum would have theoretically allowed for lower coastlines. It has often been suggested that an ice-free corridor, in what

7568-695: The Dakelh (Carrier) and the Tsilhqot'in . The inlets and valleys of the British Columbia Coast sheltered large, distinctive populations, such as the Haida , Kwakwaka'wakw and Nuu-chah-nulth , sustained by the region's abundant salmon and shellfish. These peoples developed complex cultures dependent on the western red cedar that included wooden houses, seagoing whaling and war canoes and elaborately carved potlatch items and totem poles . In

7744-629: The French and Indian War , an event called the Expulsion of the Acadians or le Grand Dérangement . The "expulsion" resulted in approximately 12,000 Acadians being shipped to destinations throughout Britain's North America and to France, Quebec and the French Caribbean colony of Saint-Domingue . The first wave of the expulsion of the Acadians began with the Bay of Fundy Campaign (1755) and

7920-404: The Gulf of Venezuela to the high mountains and valleys. The population using them were hunter-gatherers that seemed to remain within a certain circumscribed territory. El Jobo points were probably the earliest, going back to c.  14,200  – c.  12,980 BP and they were used for hunting large mammals. In contrast, the fish-tail points, dating to c. 11,000 B.P. in Patagonia , had

8096-636: The Laurentide and Cordilleran ice sheets . An alternative proposed scenario involves migration, either on foot or using boats , down the Pacific coast to South America. Evidence of the latter would have been submerged by a sea-level rise of more than a hundred meters following the end of the Last Glacial Period . The time range of the peopling of the Americas remains a source of substantial debate. Conventional estimates have it that humans reached North America at some point between 15,000 and 20,000 years ago. However, some groups of humans may have reached South America as early as 25,000 years ago. One of

8272-403: The Laurentide and Cordilleran ice sheets. Another route proposed is that, either on foot or using boats , they migrated down the Pacific coast to South America as far as Chile . Any archaeological evidence of coastal occupation during the last Ice Age would now have been covered by the sea level rise , up to a hundred metres since then. The precise date for the peopling of the Americas

8448-478: The Laurentide Ice Sheet and spread rapidly southward, occupying both North and South America by 12,000 to 14,000 years ago. The earliest populations in the Americas, before roughly 10,000 years ago, are known as Paleo-Indians . Indigenous peoples of the Americas have been linked to Siberian populations by proposed linguistic factors , the distribution of blood types , and in genetic composition as reflected by molecular data, such as DNA . While there

8624-431: The Mi'kmaq and Abenaki of the Maritime region of Canada and likely the extinct Beothuk of Newfoundland . The Ojibwa and other Anishinaabe speakers of the central Algonquian languages retain an oral tradition of having moved to their lands around the western and central Great Lakes from the sea, likely the Atlantic coast. According to oral tradition, the Ojibwa formed the Council of Three Fires in 796 CE with

8800-421: The North American extinction event that occurred at the end of the Pleistocene. Their genome , however, contains evidence of a bottleneck – something that can be used to test hypothesis on migrations between the two continents. Early human groups were largely nomadic , relying on following food sources for survival. Mobility was part of what made humans successful. As nomadic groups, early humans likely followed

8976-431: The Odawa and the Potawatomi . The Five Nations of the Iroquois (Haudenosaunee) were centred from at least 1000 CE in northern New York, but their influence extended into what is now southern Ontario and the Montreal area of modern Quebec. They spoke varieties of Iroquoian languages. The Iroquois Confederacy , according to oral tradition, was formed in 1142 CE. In addition, there were other Iroquoian-speaking peoples in

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9152-478: The Pacific coast and valleys of North America . This allowed land animals, followed by humans, to migrate south into the interior of the continent. The people went on foot or used boats along the coastline. The dates and routes of the peopling of the Americas remain subjects of ongoing debate. It is likely there were three waves of ancient settlers from the Bering Sea to the America continent. Stone tools , particularly projectile points and scrapers , are

9328-404: The Portuguese Empire . In 1506, King Manuel I of Portugal created taxes for the cod fisheries in Newfoundland waters. João Álvares Fagundes and Pero de Barcelos established fishing outposts in Newfoundland and Nova Scotia around 1521 CE; however, these were later abandoned, with the Portuguese colonizers focusing their efforts on South America. The extent and nature of Portuguese activity on

9504-445: The Puget lowlands up to 16,800 BP. Even during the maximum extent of coastal ice, unglaciated refugia persisted on present-day islands, that supported terrestrial and marine mammals. As deglaciation occurred, refugia expanded until the coast became ice-free by 15,000 BP. The retreat of glaciers on the Alaskan Peninsula provided access from Beringia to the Pacific coast by around 17,000 BP. The ice barrier between interior Alaska and

9680-403: The Sea of Okhotsk , shows a marked shift from tree and shrub pollen to herb pollen prior to 30,000 BP, as herb tundra replaced boreal forest and shrub steppe going into the LGM. A similar record of tree/shrub pollen being replaced with herb pollen as the LGM approached was recovered near the Kolyma River in Arctic Siberia. The abandonment of the northern regions of Siberia due to rapid cooling or

9856-465: The Tlingit , who lived on the islands of southern Alaska and northern British Columbia . The Na-Dene language group is believed to be linked to the Yeniseian languages of Siberia. The Dene of the western Arctic may represent a distinct wave of migration from Asia to North America. The Interior of British Columbia was home to the Salishan language groups such as the Shuswap (Secwepemc) , Okanagan and southern Athabaskan language groups, primarily

10032-442: The Treaty of Tordesillas , the Spanish Crown claimed it had territorial rights in the area visited by John Cabot in 1497 and 1498 CE. However, Portuguese explorers like João Fernandes Lavrador would continue to visit the north Atlantic coast, which accounts for the appearance of " Labrador " on maps of the period. In 1501 and 1502 the Corte-Real brothers explored Newfoundland (Terra Nova) and Labrador claiming these lands as part of

10208-426: The Ulchis of the lower Amur River region (4 among 87 sampled, or 4.6%), along with Subhaplogroup C1a (1 among 87, or 1.1%). Subhaplogroup C1a is regarded as a close sister clade of the Native American Subhaplogroup C1b. Subhaplogroup D1a has also been found among ancient Jōmon skeletons from Hokkaido The modern Ainu are regarded as descendants of the Jōmon. The occurrence of the Subhaplogroups D1a and C1a in

10384-407: The War of 1812 . In 1785, Saint John, New Brunswick became the first incorporated city in what would later become Canada. The signing of the Treaty of Paris in 1783 formally ended the war. Great Britain made several concessions to the US at the expense of the North American colonies. Notably, the borders between Canada and the United States were officially demarcated; all land south and west of

10560-653: The Wisconsin glaciation , the Earth's ocean water was, to varying degrees over time, stored in glacier ice. As water accumulated in glaciers, the volume of water in the oceans correspondingly decreased, resulting in lowering of global sea level . The variation of sea level over time has been reconstructed using oxygen isotope analysis of deep sea cores, the dating of marine terraces, and high-resolution oxygen isotope sampling from ocean basins and modern ice caps. A drop of eustatic sea level by about 60 to 120 metres (200 to 390 ft) from present-day levels, commencing around 30,000 years Before Present (BP), created Beringia ,

10736-451: The giant beaver , steppe wisent , giant muskox , mastodon , woolly mammoth and ancient reindeer . The Clovis culture , appearing around 11,500 BCE ( c.  13,500 BP) in North America, is one of the most notable Paleo-Indian archaeological cultures. It has been disputed whether the Clovis culture were specialist big-game hunters or employed a mixed foraging strategy that included smaller terrestrial game, aquatic animals, and

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10912-419: 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 Haida Gwaii islands, Old Crow Flats , and the Bluefish Caves contain some of the earliest Paleo-Indian archeological sites in Canada. Ice Age hunter-gatherers of this period left lithic flake fluted stone tools and

11088-412: The republicanism that was common among American immigrants to Canada . The troubling memory of the war and the American invasions etched itself into the consciousness of Canadians as a distrust of the intentions of the United States towards the British presence in North America. The rebellions of 1837 against the British colonial government took place in both Upper and Lower Canada. In Upper Canada,

11264-416: The western frontier . In the former French territory, the new British rulers of Canada first abolished and then later reinstated most of the property, religious, political, and social culture of the French-speaking habitants , guaranteeing the right of the Canadiens to practice the Catholic faith and to the use of French civil law (now Quebec Civil Code ) in the UK's Quebec Act of 1774. During

11440-440: The "Clovis people likely came from the south, not the north, perhaps following wild animals such as bison ". An alternative hypothesis for the peopling of America is coastal migration , which may have been feasible along the deglaciated (but now submerged) coastline of the Pacific Northwest from about 16,000 years ago. Pre-LGM migration across Beringia has been proposed to explain purported pre-LGM ages of archaeological sites in

11616-405: The 1840 Act of Union , and responsible government was achieved in 1848, a few months after it was accomplished in Nova Scotia. The parliament of United Canada in Montreal was set on fire by a mob of Tories in 1849 after the passing of an indemnity bill for the people who suffered losses during the rebellion in Lower Canada. Between the Napoleonic Wars and 1850, some 800,000 immigrants came to

11792-404: The Americas becoming extinct towards the end of the Paleoindian period as part of the Late Pleistocene megafauna extinctions . The potential role of human hunting in the extinctions has been the subject of much controversy. From 8000 to 7000 BCE (10,000–9,000 BP) the climate stabilized, leading to a rise in population and lithic technology advances, resulting in a more sedentary lifestyle during

11968-409: The Americas followed by isolation of the northern population following closure of the ice-free corridor. Evidence of Australo-Melanesians admixture in Amazonian populations was found by Skoglund and Reich (2016). A study of the diversification of mtDNA Haplogroups C and D from southern Siberia and eastern Asia, respectively, suggests that the parent lineage (Subhaplogroup D4h) of Subhaplogroup D4h3,

12144-408: The Americas occurring around 10,000 to 15,000 years after isolation of the small founding population . Another model (Kitchen et al. 2008) proposes that migration into Beringia occurred approximately 36,000 BP, followed by 20,000 years of isolation in Beringia. A third model (Nomatto et al. 2009) proposes that migration into Beringia occurred between 40,000 and 30,000 BP, with a pre-LGM migration into

12320-663: The Americas such as Bluefish Caves and Old Crow Flats in the Yukon Territory , and Meadowcroft Rock Shelter in Pennsylvania. The oldest archaeological sites on the Alaskan side of Beringia date to around 14,000 BP. It is possible that a small founder population had entered Beringia before that time. However, archaeological sites that date closer to the LGM on either the Siberian or the Alaskan side of Beringia are lacking. Biomarker and microfossil analyses of sediments from Lake E5 and Burial Lake in northern Alaska suggest human presence in eastern Beringia as early as 34,000 years ago. These sedimentary analyses have been suggested to be

12496-519: The Americas suggest that Clovis (thus the "Paleo-Indians") time range should be re-examined. In particular, sites such as Cooper's Ferry in Idaho, Cactus Hill in Virginia , Meadowcroft Rockshelter in Pennsylvania , Bear Spirit Mountain in West Virginia , Catamarca and Salta in Argentina , Pilauco and Monte Verde in Chile , Topper in South Carolina , and Quintana Roo in Mexico have generated early dates for wide-ranging Paleo-Indian occupation. Some sites significantly predate

12672-701: The Americas ;portal Peopling of the Americas The peopling of the Americas began when Paleolithic hunter-gatherers ( Paleo-Indians ) entered North America from the North Asian Mammoth steppe via the Beringia land bridge , which had formed between northeastern Siberia and western Alaska due to the lowering of sea level during the Last Glacial Maximum (26,000 to 19,000 years ago). These populations expanded south of

12848-496: The Americas. Due to the evidence that Paleoindians hunted now extinct megafauna (large animals), and that following a period of overlap, most large animals across the Americas became extinct as part of the Late Pleistocene megafauna extinctions , it has been argued by many authors that hunting by Paleoindians was an important factor in the extinctions, though this suggestion is controversial, with other authors placing

13024-811: The Arctic Ocean on the north and the Pacific Ocean on the west. The Colony of Vancouver Island was chartered in 1849, with the trading post at Fort Victoria as the capital. This was followed by the Colony of the Queen Charlotte Islands in 1853, and by the creation of the Colony of British Columbia in 1858 and the Stikine Territory in 1861, with the latter three being founded expressly to keep those regions from being overrun and annexed by American gold miners. The Colony of

13200-521: The British Conquest of Acadia occurred in 1710, resulting in Nova Scotia (other than Cape Breton) being officially ceded to the British by the Treaty of Utrecht , including Rupert's Land, which France had conquered in the late 17th century ( Battle of Hudson's Bay ). As an immediate result of this setback, France founded the powerful Fortress of Louisbourg on Cape Breton Island . Louisbourg

13376-601: The British islands combined, and Voltaire had notoriously dismissed Canada as " Quelques arpents de neige ", " A few acres of snow "). Following the Treaty of Paris, King George III issued the Royal Proclamation of 1763 . The proclamation organized Great Britain's new North American empire and stabilized relations between the British Crown and Aboriginal peoples , formally recognizing aboriginal title, regulated trade, settlement, and land purchases on

13552-592: The British to a settled colony with stronger ties to New England. Britain eventually gained control of Quebec City after the Battle of the Plains of Abraham and the Battle of Fort Niagara in 1759, and finally captured Montreal in 1760. As part of the terms of the Treaty of Paris (1763) , signed after the defeat of New France in the Seven Years' War , France renounced its claims to territory in mainland North America , except for fishing rights off Newfoundland and

13728-520: The Canadian mainland during the 16th century remains unclear and controversial. French interest in the New World began with Francis I of France , who in 1524 sponsored Giovanni da Verrazzano 's navigation of the region between Florida and Newfoundland in hopes of finding a route to the Pacific Ocean . Although the English had laid claims to it in 1497 when John Cabot made landfall somewhere on

13904-699: The Early Archaic period in some regions. Sites in Alaska (eastern Beringia) exhibit some of the earliest evidence of Paleo-Indians, followed by archaeological sites in northern British Columbia , western Alberta and the Old Crow Flats region of the Yukon territory. The Paleo-Indians would eventually flourish all over the Americas. These peoples were spread over a wide geographical area; thus there were regional variations in lifestyles. However, all

14080-711: The Great Lakes, which was formerly a part of the Province of Quebec and included modern-day Michigan, Wisconsin, Illinois, Indiana and Ohio, was ceded to the Americans. Fishing rights were also granted to the United States in the Gulf of St. Lawrence and on the coast of Newfoundland and the Grand Banks . The British ignored part of the treaty and maintained their military outposts in the Great Lakes areas it had ceded to

14256-626: The Hudson's Bay Company claims, and in 1686, Pierre Troyes led an overland expedition from Montreal to the shore of the bay , where they managed to capture a handful of outposts. La Salle 's explorations gave France a claim to the Mississippi River Valley , where fur trappers and a few settlers set up scattered forts and settlements . There were four French and Indian Wars and two additional wars in Acadia and Nova Scotia between

14432-683: The LGM, due to cold and dry conditions. Coastal environments during the Last Glacial Maximum were complex. The lowered sea level, and an isostatic bulge equilibrated with the depression beneath the Cordilleran Ice Sheet, exposed the continental shelf to form a coastal plain. While much of the coastal plain was covered with piedmont glaciers, unglaciated refugia supporting terrestrial mammals have been identified on Haida Gwaii , Prince of Wales Island , and outer islands of

14608-460: The Last Glacial Maximum after 30,000 years BP saw the expansion of alpine glaciers and continental ice sheets that blocked migration routes out of Beringia. By 21,000 years BP, and possibly thousands of years earlier, the Cordilleran and Laurentide ice sheets coalesced east of the Rocky Mountains , closing off a potential migration route into the center of North America. Alpine glaciers in

14784-629: The Last Glacial Maximum, climates in eastern Siberia fluctuated between conditions approximating present day conditions and colder periods. The pre-LGM warm cycles in Arctic Siberia saw flourishes of megafaunas. The oxygen isotope record from the Greenland Ice Cap suggests that these cycles after about 45,000 BP lasted anywhere from hundreds to between one and two thousand years, with greater duration of cold periods starting around 32,000 BP. The pollen record from Elikchan Lake, north of

14960-540: The North American coast (likely either modern-day Newfoundland or Nova Scotia ) and had claimed the land for England on behalf of Henry VII , these claims were not exercised and England did not attempt to create a permanent colony. As for the French, however, Jacques Cartier planted a cross in the Gaspé Peninsula in 1534 and claimed the land in the name of Francis I, creating a region called " Canada "

15136-620: The Pacific coast broke up starting around 16,200 BP. The ice-free corridor to the interior of North America opened between 13,000 and 12,000 BP. Glaciation in eastern Siberia during the LGM was limited to alpine and valley glaciers in mountain ranges and did not block access between Siberia and Beringia. The paleoclimates and vegetation of eastern Siberia and Alaska during the Wisconsin glaciation have been deduced from high resolution oxygen isotope data and pollen stratigraphy . Prior to

15312-612: The Queen Charlotte Islands and most of the Stikine Territory were merged into the Colony of British Columbia in 1863 (the remainder, north of the 60th Parallel, became part of the North-Western Territory ). The Seventy-Two Resolutions from the 1864 Quebec Conference and Charlottetown Conference laid out the framework for uniting British colonies in North America into a federation. The Resolutions became

15488-620: The Thirteen American Colonies and New France from 1688 to 1763. During King William's War (1688 to 1697), military conflicts in Acadia included the Battle of Port Royal (1690) ; a naval battle in the Bay of Fundy ( Action of July 14, 1696 ); and the Raid on Chignecto (1696) . The Treaty of Ryswick in 1697 ended the war between the two colonial powers of England and France for a brief time. During Queen Anne's War (1702 to 1713),

15664-614: The U.S., and they continued to supply their native allies with munitions. The British evacuated the outposts with the Jay Treaty of 1795, but the continued supply of munitions irritated the Americans in the run-up to the War of 1812. Canadian historians have had mixed views on the long-term impact of the American Revolution. Arthur Lower in the 1950s provided the long-standard historical interpretation that for English Canada

15840-588: The Y lineage specific to South America indicates that certain Amerindian populations have been isolated since the initial colonization of the region. The Na-Dené , Inuit and Indigenous Alaskan populations, however, exhibit haplogroup Q (Y-DNA) mutations that are distinct from other Amerindians with various mtDNA mutations. This suggests that the earliest migrants into the northern extremes of North America and Greenland derived from later migrant populations. Evidence from full genomic studies suggests that

16016-691: The area, including the St. Lawrence Iroquoians , the Erie, and others. On the Great Plains , the Cree or Nēhilawē (who spoke a closely related Central Algonquian language , the plains Cree language ) depended on the vast herds of bison to supply food and many of their other needs. To the northwest were the peoples of the Na-Dene languages , which include the Athapaskan-speaking peoples and

16192-487: The assistance of First Nations and loyalist informants, most notably Laura Secord . The War ended with no boundary changes thanks to the Treaty of Ghent of 1814, and the Rush–Bagot Treaty of 1817. A demographic result was the shifting of the destination of American migration from Upper Canada to Ohio , Indiana and Michigan , without fear of Indigenous attacks. After the war, supporters of Britain tried to repress

16368-523: The assistance of local militias. The defeat of the British army during the Siege of Yorktown in October 1781 signalled the end of Great Britain's struggle to suppress the American Revolution. When the British evacuated New York City in 1783, they took many Loyalist refugees to Nova Scotia, while other Loyalists went to southwestern Quebec. So many Loyalists arrived on the shores of the St. John River that

16544-537: The attempted settlement of Vinland by Leif Erikson around the same period or, more broadly, with Norse exploration of the Americas . Under letters patent from King Henry VII of England , the Italian John Cabot became the first European known to have landed in Canada after the Viking Age . Records indicate that on June 24, 1497, he sighted land at a northern location believed to be somewhere in

16720-557: The authorities. The towns of Chambly and Sorel were taken by the rebels, and Quebec City was isolated from the rest of the colony. Montreal rebel leader Robert Nelson read the " Declaration of Independence of Lower Canada " to a crowd assembled at the town of Napierville in 1838. The rebellion of the Patriote movement was defeated after battles across Quebec. Hundreds were arrested, and several villages were burnt in reprisal. The British government then sent Lord Durham to examine

16896-702: The basis for the London Conference of 1866 , which led to the formation of the Dominion of Canada on July 1, 1867. The term dominion was chosen to indicate Canada's status as a self-governing polity of the British Empire, the first time it was used about a country. With the coming into force of the UK's British North America Act, 1867 (enacted by the British Parliament ), Canada became

17072-617: The beginning of the cooling period that led into the LGM. A compilation of archaeological site dates throughout eastern Siberia suggest that the cooling period caused a retreat of humans southwards. Pre-LGM lithic evidence in Siberia indicate a settled lifestyle that was based on local resources, while post-LGM lithic evidence indicate a more migratory lifestyle. A 2021 discovery of human footprints in relict lake sediments near White Sands National Park in New Mexico demonstrated there

17248-625: The blame on climatic change. In a 2012 survey of archaeologists in The SAA Archaeological Record, 63% of respondents said that megafauna extinctions were likely the result of a "combination of factors". The Archaic period in the Americas saw a changing environment featuring a warmer, more arid climate and the disappearance of the last megafauna. The majority of population groups at this time were still highly mobile hunter-gatherers, but now individual groups started to focus on resources available to them locally. Thus with

17424-706: The brisk market for sea otter pelts in China, thereby launching what became known as the China Trade . In 1789 war threatened between Britain and Spain on their respective rights; the Nootka Crisis was resolved peacefully largely in favour of Britain, the much stronger naval power at the time. In 1793 Alexander MacKenzie , a Scotsman working for the North West Company , crossed the continent and with his Aboriginal guides and French-Canadian crew, reached

17600-699: The centre of Huron country near Lake Simcoe . During these voyages, Champlain aided the Wendat (aka "Hurons") in their battles against the Iroquois Confederacy. As a result, the Iroquois would become enemies of the French and be involved in multiple conflicts (known as the French and Iroquois Wars ) until the signing of the Great Peace of Montreal in 1701. The English, led by Humphrey Gilbert , had claimed St. John's, Newfoundland , in 1583 as

17776-525: The chronology of the controversial Pedra Furada rock shelter in Piauí , Brazil . More recently, studies at the archaeological sites Santa Elina (27000-10000 years BP) in the midwest, and Rincão I (20000-12000 years BP) in southeastern Brazil also show associations of evidence of human presence with sediments dating from before the LGM. A 2003 study dated evidence for the controlled use of fire to before 40,000 years ago. Additional evidence has been adduced from

17952-578: The coastal ranges and the Alaskan Peninsula isolated the interior of Beringia from the Pacific coast. Coastal alpine glaciers and lobes of Cordilleran ice coalesced into piedmont glaciers that covered large stretches of the coastline as far south as Vancouver Island and formed an ice lobe across the Straits of Juan de Fuca by 18,000 BP. Coastal alpine glaciers started to retreat around 19,000 BP while Cordilleran ice continued advancing in

18128-766: The colonies of British North America, mainly from the British Isles , as part of the great migration of Canada . These included Gaelic -speaking Highland Scots displaced by the Highland Clearances to Nova Scotia and Scottish and English settlers to the Canadas, particularly Upper Canada. The Irish Famine of the 1840s significantly increased the pace of Irish Catholic immigration to British North America, with over 35,000 distressed Irish landing in Toronto alone in 1847 and 1848. Spanish explorers had taken

18304-464: The continent until the Spanish reintroduced the horse near the end of the 15th century CE. As the Quaternary extinction event was happening, the late Paleo-Indians would have relied more on other means of subsistence. From c.  10,500  – c.  9,500 BCE ( c.  12,500  – c.  11,500 BP), the broad-spectrum big game hunters of the Great Plains began to focus on

18480-632: The deglaciated landscape increased slowly. The earliest possible viability of the ice-free corridor as a human migration route has been estimated at 11,500 BP. Birch forests were advancing across former herb tundra in Beringia by 17,000 BP in response to climatic amelioration, indicating increased productivity of the landscape. Analyses of biomarkers and microfossils preserved in sediments from Lake E5 and Burial Lake in northern Alaska suggest early humans burned Beringian landscapes as early as 34,000 years ago. The authors of these studies suggest that fire

18656-614: The development of human Y-chromosome DNA haplogroups (yDNA haplogroups ) and human mitochondrial DNA haplogroups (mtDNA haplogroups) characteristic of Native American populations. Models of molecular evolution rates were used to estimate the ages at which Native American DNA lineages branched off from their parent lineages in Asia and to deduce the ages of demographic events. One model (Tammetal 2007) based on Native American mtDNA Haplotypes (Figure 2) proposes that migration into Beringia occurred between 30,000 and 25,000 BP, with migration into

18832-472: The early 21st century, the models of the chronology of migration are divided into two general approaches. The first is the short chronology theory , that the first migration occurred after the LGM, which went into decline after about 19,000 years ago, and was then followed by successive waves of immigrants. The second theory is the long chronology theory, which proposes that the first group of people entered Beringia, including ice-free parts of Alaska, at

19008-454: The early human groups who hunted them. Bison , a type of megafauna, have been identified as an ideal candidate for the tracing of human migrations out of Europe because of both their abundance in North America as well as being one of the first megafauna for which ancient DNA was used to trace patterns of population movement. Unlike other types of fauna that moved between the Americas and Eurasia ( mammoths , horses , and lions ), Bison survived

19184-519: The few areas of agreement is the origin from Siberia , with widespread habitation of the Americas during the end of the Last Glacial Period, and more specifically after the end of the Last Glacial Maximum around 16,000 to 13,000 years before present. The Palaeoindian culture lasts 4000 years, from 12,000 to 8000 BP. It is divided into Early Palaeoindian (12,000-10,000 BP) and Late Palaeoindian (10,000-8000 BP), ending with early events of

19360-501: The first North American English colony by royal prerogative of Queen Elizabeth I . In the reign of King James I , the English established additional colonies in Cupids and Ferryland , Newfoundland , and soon after established the first successful permanent settlements of Virginia to the south. On September 29, 1621, a charter for the foundation of a New World Scottish colony was granted by King James to William Alexander . In 1622,

19536-446: The first people in the Americas diverged from Ancient East Asians about 36,000 years ago and expanded northwards into Siberia, where they encountered and interacted with a different Paleolithic Siberian population (known as Ancient North Eurasians ), giving rise to both Paleosiberian peoples and Ancient Native Americans , which later migrated towards the Beringian region, became isolated from other populations, and subsequently populated

19712-525: The first settlers left Scotland. They initially failed and permanent Nova Scotian settlements were not firmly established until 1629 during the end of the Anglo-French War . These colonies did not last long except the fisheries in Ferryland under David Kirke . In 1631, under Charles I of England , the Treaty of Suza was signed, ending the war and returning Nova Scotia to the French. New France

19888-550: The following Archaic Period . Researchers continue to study and discuss the specifics of Paleo-Indian migration to and throughout the Americas , including the dates and routes traveled. The traditional theory holds that these early migrants moved into Beringia between eastern Siberia and present-day Alaska 17,000 years ago, at a time when the Quaternary glaciation significantly lowered sea levels. These people are believed to have followed herds of now-extinct pleistocene megafauna along ice-free corridors that stretched between

20064-481: The following summer. Cartier had sailed up the St. Lawrence river as far as the Lachine Rapids , to the spot where Montreal now stands. Permanent settlement attempts by Cartier at Charlesbourg-Royal in 1541, at Sable Island in 1598 by Marquis de La Roche-Mesgouez, and at Tadoussac, Quebec in 1600 by François Gravé Du Pont all eventually failed. Despite these initial failures, French fishing fleets visited

20240-401: The food from Eurasia to the Americas – part of the reason why tracing megafaunal DNA is so helpful for garnering insight to these migratory patterns. The grey wolf originated in the Americas and migrated into Eurasia prior to the Last Glacial Maximum – during which it was believed that remaining populations of the grey wolf residing in North America faced extinction and were isolated from

20416-456: The forests and marshes. The fall would have been a busy time because foodstuffs would have to be stored and clothing made ready for the winter. During the winter, coastal fishing groups moved inland to hunt and trap fresh food and furs. Late ice-age climatic changes caused plant communities and animal populations to change. Groups moved and sought new supplies as preferred resources were depleted. Small bands utilized hunting and gathering during

20592-432: The fortress surrendered. The return of Louisbourg to French control by the peace treaty prompted the British to found Halifax in 1749 under Edward Cornwallis . Despite the official cessation of war between the British and French empires with the Treaty of Aix-la-Chapelle , the conflict in Acadia and Nova Scotia continued as Father Le Loutre's War . The British ordered the Acadians expelled from their lands in 1755 during

20768-571: The genetic profiles of the Hokkaido Jōmon skeletons and the modern Ainu illustrates another uncertainty in source models derived from modern DNA samples. The development of high-resolution genomic analysis has provided opportunities to further define Native American subclades and narrow the range of Asian subclades that may be parent or sister subclades. The common occurrence of the mtDNA Haplogroups A, B, C, and D among eastern Asian and Native American populations has long been recognized, along with

20944-635: The geologic association of bones at the Bluefish Cave and Old Crow Flats sites, and the related Bonnet Plume site, have been called into question. No evidence of human remains have been discovered at these sites. In addition to disputed archaeological sites, support for pre-LGM human presence has been found in lake sediment records of northern Alaska. Biomarker and microfossil analyses of sediments from Lake E5 and Burial Lake in suggest human presence in eastern Beringia as early as 34,000 years ago. These analyses are indeed compelling in that they corroborate

21120-609: The ice sheets, the oldest such sites occur in association with the Clovis complex. If humans managed to breach the continental ice sheets significantly before 13,000 BP, there should be clear evidence for it in the form of at least some stratigraphically discrete archaeological components with a relatively high artifact count. So far, no such evidence exists." Genetic studies have used high resolution analytical techniques applied to DNA samples from modern Native Americans and Asian populations regarded as their source populations to reconstruct

21296-534: The individual groups shared a common style of stone tool production, making knapping styles and progress identifiable. This early Paleo-Indian period's lithic reduction tool adaptations have been found across the Americas, utilized by highly mobile bands consisting of approximately 20 to 60 members of an extended family. Food would have been plentiful during the few warm months of the year. Lakes and rivers were teeming with many species of fish, birds and aquatic mammals. Nuts, berries and edible roots could be found in

21472-761: The inferences made from the Bluefish Cave and Old Crow Flats sites. In 2020, evidence emerged for a new pre-LGM site in North-Central Mexico . Chiquihuite cave , an archaeological site in Zacatecas State, has been dated to 26,000 years BP based on numerous lithic artefacts discovered there. However, there is scholarly debate over whether the artifacts should be considered evidence of human activity or if they were formed naturally. No evidence of human DNA or hearth have been unearthed. Pre-LGM human presence in South America rests partly on

21648-514: The initial peopling of the Americas, and secondly with European colonization of the Americas . The former is the determinant factor for the number of gene lineages and founding haplotypes present in today's Indigenous Amerindian populations. Human settlement of the Americas occurred in stages from the Bering sea coast line , with an initial layover on Beringia for the founding population . The micro-satellite diversity and distributions of

21824-472: The lands into one country, dominated by the English language and loyalist culture; many French-Canadians saw an opportunity to exert political control within a new largely French-speaking Quebec and exaggerated fears of possible U.S. expansion northward. On a political level, there was a desire for the expansion of responsible government and elimination of the legislative deadlock between Upper and Lower Canada, and their replacement with provincial legislatures in

22000-667: The last continents into which humans migrated . During the Wisconsin glaciation , 50,000–17,000 years ago, falling sea levels allowed people to move gradually across the Bering land bridge ( Beringia ), from Siberia into northwest North America. At that point, they were blocked by the Laurentide Ice Sheet that covered most of Canada, confining them to Alaska and the Yukon for thousands of years. The exact dates and routes of

22176-442: The late 15th century, French and British expeditions explored, colonized, and fought over various places within North America in what constitutes present-day Canada. The colony of New France was claimed in 1534 with permanent settlements beginning in 1608. France ceded nearly all its North American possessions to the Great Britain in 1763 at the Treaty of Paris after the Seven Years' War . The now British Province of Quebec

22352-405: The lead in the Pacific Northwest coast , with the voyages of Juan José Pérez Hernández in 1774 and 1775. By the time the Spanish determined to build a fort on Vancouver Island , the British navigator James Cook had visited Nootka Sound and charted the coast as far as Alaska, while British and American maritime fur traders had begun a busy era of commerce with the coastal peoples to satisfy

22528-401: The location where the admixture took place. However, a third theory, the "Beringian standstill hypothesis", suggests that East Asians instead migrated north to Northeastern Siberia, where they mixed with ANE, and later diverged in Beringia, where distinct Native American lineages formed. This theory is supported by maternal and nuclear DNA evidence. According to Grebenyuk, after 20,000 BP,

22704-470: The lower Amur region suggests a source population from that region distinct from the Altai-Baikal source populations, where sampling did not reveal those two particular subclades. The conclusions regarding Subhaplogroup D1 indicating potential source populations in the lower Amur and Hokkaido areas stand in contrast to the single-source migration model. Subhaplogroup D4h3 has been identified among Han Chinese . Subhaplogroup D4h3 from China does not have

22880-452: The migration time frame of ice-free corridors, thus suggesting that there were additional coastal migration routes available, traversed either on foot and/or in boats. Geological evidence suggests the Pacific coastal route was open for overland travel before 23,000 years ago and after 16,000 years ago. In South America, the site of Monte Verde indicates that its population was probably territorial and resided in their river basin for most of

23056-409: The modern Native American phenotype. Archaeogenetic studies do not support a two-wave model or the Paleoamerican hypothesis of an Australo-Melanesian origin, and firmly assign all Paleo-Indians and modern Native Americans to one ancient population that entered the Americas in a single migration from Beringia. Only in one ancient specimen (Lagoa Santa) and a few modern populations in the Amazon region,

23232-412: The morphology of Luzia Woman fossil, which was described as Australo-Melanesian . This interpretation was challenged in a 2003 review which concluded the features in question could also have arisen by genetic drift. In November 2018, scientists of the University of São Paulo and Harvard University released a study that contradicts the alleged Australo-Melanesian origin of Luzia. Using DNA sequencing,

23408-427: The most closely related subclades grow more specific. Subhaplogroups D1 and D4h3 have been regarded as Native American specific based on their absence among a large sampling of populations regarded as potential descendants of source populations, over a wide area of Asia. Among the 3,764 samples, the Sakhalin –lower Amur region was represented by 61 Oroks . In another study, Subhaplogroup D1a has been identified among

23584-411: The mouth of the Bella Coola River , completing the first continental crossing north of Mexico, missing George Vancouver 's charting expedition to the region by only a few weeks. In 1821, the North West Company and Hudson's Bay Company merged, with a combined trading territory that was extended by a licence to the North-Western Territory and the Columbia and New Caledonia fur districts, which reached

23760-493: The name big-game hunters . Pacific coastal groups of the period would have relied on fishing as the prime source of sustenance. Archaeologists are piecing together evidence that the earliest human settlements in North America were thousands of years before the appearance of the current Paleo-Indian time frame (before the late glacial maximum 20,000-plus years ago). Evidence indicates that people were living as far east as Beringia before 30,000 BCE (32,000 BP). Until recently, it

23936-422: The nation, Ottawa attracted support in the Maritimes and in British Columbia. In 1866, the Colony of British Columbia and the Colony of Vancouver Island merged into a single Colony of British Columbia . After Rupert's Land was transferred to Canada by Britain in 1870, connecting to the eastern provinces, British Columbia joined Canada in 1871. In 1873, Prince Edward Island joined. Newfoundland—which had no use for

24112-424: The need to complete the Canadian Pacific Railway. It guaranteed Anglophone control of the Prairies and demonstrated the national government was capable of decisive action. However, it lost the Conservative Party most of their support in Quebec and led to a permanent distrust of the Anglophone community on the part of the Francophones. Paleo-Indians Traditional theories suggest that big-animal hunters crossed

24288-489: The oldest pottery excavated to date in Canada. The Hopewell tradition is an Indigenous 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 . The eastern woodland areas of what became Canada were home to

24464-409: The only possibly recoverable remnants of humans living in Alaska during the last Glacial period. At Old Crow Flats, mammoth bones have been found that are broken in distinctive ways indicating human butchery. The radiocarbon dates on these vary between 25,000 and 40,000 BP. Also, stone microflakes have been found in the area indicating tool production. However, the interpretations of butcher marks and

24640-670: The passage of time there is a pattern of increasing regional generalization like the Southwest , Arctic , Poverty , Dalton , and Plano traditions. These regional adaptations would become the norm, with reliance less on hunting and gathering, and a more mixed economy of small game, fish, seasonally wild vegetables, and harvested plant foods. Many groups continued to hunt big game but their hunting traditions became more varied and meat procurement methods more sophisticated. The placement of artifacts and materials within an Archaic burial site indicated social differentiation based upon status in some groups. [REDACTED] Indigenous peoples of

24816-441: The passage of time, there is a pattern of increasing regional generalization (i.e.: Paleo-Arctic , Plano and Maritime Archaic traditions). The Woodland cultural period dates from about 2000 BCE to 1000 CE and is applied to the Ontario, Quebec, and Maritime regions . The introduction of pottery distinguishes the Woodland culture from the previous Archaic-stage inhabitants. The Laurentian-related people of Ontario manufactured

24992-438: The period of the Last Glacial Maximum along with genetic evidence found from early human remains in the Americas provides evidence to support pre-Clovis migrations into the Americas. The Native American source population was formed in Siberia by the mixing of two distinct populations: Ancient North Eurasians and an ancient East Asian (ESEA) population. According to Jennifer Raff, the Ancient North Eurasian population mixed with

25168-418: The possible date of the first peopling of the Americas. Academics generally believe that humans reached North America south of the Laurentide Ice Sheet at some point between 15,000 and 20,000 years ago. Some new controversial archaeological evidence suggests the possibility that human arrival in the Americas may have occurred prior to the Last Glacial Maximum more than 20,000 years ago. During

25344-452: The presence of haplogroup X . As a whole, the greatest frequency of the four Native American associated haplogroups occurs in the Altai - Baikal region of southern Siberia. Some subclades of C and D closer to the Native American subclades occur among Mongolian, Amur, Japanese, Korean, and Ainu populations. With further definition of subclades related to Native American populations, the requirements for sampling Asian populations to find

25520-408: The presence of the A subtype. The finding ignited controversy, with contention that the sample DNA was insufficiently complete for the conclusion and that the result reflected modern contamination. However, a re-analysis indicated that the DNA sequences were consistent with, but not definitely from, the "cosmopolitan clade" (subtype A). The presence of subtypes A and B in the Americas is suggestive of

25696-543: The primary evidence of the earliest human activity in the Americas. Archeologists and anthropologists use surviving crafted lithic flaked tools to classify cultural periods. Scientific evidence links Indigenous Americans to eastern Siberian populations by the distribution of blood types, and genetic composition as indicated by molecular data, such as DNA . There is evidence for at least two separate migrations. Paleoindians lived alongside and hunted many now extinct megafauna (large animals), with most large animals across

25872-421: The rate grew more rapid. The inland Cordilleran and Laurentide ice sheets retreated more slowly than did the coastal glaciers. Opening of an ice-free corridor did not occur until after 13,000 to 12,000 BP. The early environment of the ice-free corridor was dominated by glacial outwash and meltwater, with ice-dammed lakes and periodic flooding from the release of ice-dammed meltwater. Biological productivity of

26048-471: The remains of large butchered mammals. The North American climate stabilized around 8000 BCE (10,000 years ago). 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

26224-438: The rest of the population. This, however, may not be the case. Radiocarbon dating of ancient grey wolf remains found in permafrost deposits in Alaska show a continuous exchange of population from 12,500 radiocarbon years BP to beyond radiocarbon dating capabilities. This indicates that there was viable passage for grey wolf populations to exchange between the two continents. These faunas' ability to exchange populations during

26400-515: The results showed that Luzia's ancestry was entirely Native American. Stones described as probable tools, hammerstones and anvils , have been found in southern California , at the Cerutti Mastodon site , that are associated with a mastodon skeleton which appeared to have been processed by humans. The mastodon skeleton was dated by thorium-230/uranium radiometric analysis, using diffusion–adsorption–decay dating models, to around 130 thousand years ago. No human bones were found and expert reaction

26576-402: The results were counter-revolutionary: [English Canada] inherited, not the benefits, but the bitterness of the Revolution…. English Canada started its life with as powerful a nostalgic shove backward into the past as the Conquest had given to French Canada: two little peoples officially devoted to counter-revolution, to lost causes, to the tawdry ideals of a society of men and masters, and not to

26752-486: The retreat of game species with the onset of the LGM has been proposed to explain the lack of archaeological sites in that region dating to the LGM. The pollen record from the Alaskan side shows shifts between herb/shrub and shrub tundra prior to the LGM, suggesting less dramatic warming episodes than those that allowed forest colonization on the Siberian side. Diverse, though not necessarily plentiful, megafauna were present in those environments. Herb tundra dominated during

26928-400: The same geographic implication as Subhaplotype D1a from Amur-Hokkaido, so its implications for source models are more speculative. Its parent lineage, Subhaplotype D4h, is believed to have emerged in East Asia, rather than Siberia, around 20,000 BP. Subhaplogroup D4h2, a sister clade of D4h3, has also been found among Jōmon skeletons from Hokkaido. D4h3 has a coastal trace in the Americas. X

27104-417: The second wave began after the final Siege of Louisbourg (1758) . Many of the Acadians settled in southern Louisiana , creating the Cajun culture there. Some Acadians managed to hide and others eventually returned to Nova Scotia, but they were far outnumbered by a new migration of New England Planters who settled on the former lands of the Acadians and transformed Nova Scotia from a colony of occupation for

27280-423: The self-reliant freedom alongside of them. Recently Michel Ducharme has agreed that Canada did indeed oppose "republican liberty", as exemplified by the United States and France. However, he says it did find a different path forward when it fought against British rulers after 1837 to secure "modern liberty". That form of liberty focused not on the virtues of citizens but on protecting their rights from infringement by

27456-449: The settlement of the frontier. The war on the border with the United States was characterized by a series of multiple failed invasions and fiascos on both sides. American forces took control of Lake Erie in 1813, driving the British out of western Ontario, killing the Shawnee leader Tecumseh , and breaking the military power of his confederacy . The war was overseen by British army officers like Isaac Brock and Charles de Salaberry with

27632-405: The situation; he stayed in Canada for five months before returning to Britain, bringing with him his Durham Report , which strongly recommended responsible government . A less well-received recommendation was the amalgamation of Upper and Lower Canada for the deliberate assimilation of the French-speaking population. The Canadas were merged into a single colony, the United Province of Canada , by

27808-415: The southern Thirteen Colonies outnumbered the French population approximately ten to one by the 1750s. From 1670, through the Hudson's Bay Company , the English also laid claim to Hudson Bay and its drainage basin, known as Rupert's Land , establishing new trading posts and forts , while continuing to operate fishing settlements in Newfoundland. French expansion along the Canadian canoe routes challenged

27984-531: The spring and summer months, then broke into smaller direct family groups for the fall and winter. Family groups moved every 3–6 days, possibly traveling up to 360 km (220 mi) per year. Diets were often sustaining and rich in protein; clothing was made from a variety of animal hides that were also used for shelter construction. During much of the early and middle Paleo-Indian periods, inland bands are thought to have subsisted primarily through hunting now-extinct megafauna . Large Pleistocene mammals included

28160-407: The state. The War of 1812 was fought between the United States and the British, with the British North American colonies being heavily involved. Greatly outgunned by the British Royal Navy , the American war plans focused on an invasion of Canada (especially what is today eastern and western Ontario ). The American frontier states voted for war to suppress the First Nations raids that frustrated

28336-424: The two small islands of Saint Pierre and Miquelon where its fishermen could dry their fish. France had already secretly transferred its vast Louisiana territory to Spain under the Treaty of Fontainebleau (1762) in which King Louis XV of France had given his cousin King Charles III of Spain the entire area of the drainage basin of the Mississippi River from the Great Lakes to the Gulf of Mexico and from

28512-404: The use of dated fossil DNA to calibrate molecular evolution rates. Although there is no archaeological evidence that can be used to direct support a coastal migration route during the Last Glacial Maximum , genetic analysis has been used to support this thesis. In addition to human genetic lineage, megafaunal DNA lineage can be used to trace movements of megafauna – large mammalian – as well as

28688-428: The word " Dominion " was conferred as the country's title. Over the next eighty-two years, Canada expanded by incorporating other parts of British North America , finishing with Newfoundland and Labrador in 1949. Although responsible government had existed in British North America since 1848, Britain continued to set its foreign and defence policies until the end of World War I . The Balfour Declaration of 1926 ,

28864-744: The year. Some other South American groups, on the other hand, were highly mobile and hunted big-game animals such as gomphotheres and giant sloths . They used classic bifacial projectile point technology, such as Fishtail points . The primary examples are populations associated with El Jobo points ( Venezuela ), fish-tail or Magallanes points (various parts of the continent, but mainly the southern half), and Paijan points ( Peru and Ecuador ) at sites in grasslands, savanna plains, and patchy forests. The dating for these sites ranges from c.  14,000 BP (for Taima-Taima in Venezuela) to c.  10,000 BP. The bi-pointed El Jobo projectile points were mostly distributed in north-western Venezuela; from

29040-557: Was a verifiable human presence in the region dating back to the LGM between 18,000 and 26,000 years ago. Later studies, reported in October 2023, confirmed that the age of the human footprints to be "up to 23,000 years old". The Clovis-first advocates have not accepted the veracity of these findings. In 2022, they said, "The oldest evidence for archaeological sites in the New World with large numbers of artifacts occurring in discrete and minimally disturbed stratigraphic contexts occur in eastern Beringia between 13,000 and 14,200 BP. South of

29216-415: Was accelerated as sea levels rose and floated glacial termini. It has been estimated that the coast range was fully ice-free between 16,000 and 15,000 BP. Littoral marine organisms colonized shorelines as ocean water replaced glacial meltwater. Replacement of herb/shrub tundra by coniferous forests was underway by 15,000 BP north of Haida Gwaii. Eustatic sea level rise caused flooding, which accelerated as

29392-399: Was divided into Upper and Lower Canada in 1791. The two provinces were united as the Province of Canada by the Act of Union 1840 , which came into force in 1841. 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. "Canada" was adopted as the legal name of the new country and

29568-461: Was due to the natural abundance of meat, fish, and pure water; the good food conservation conditions during the winter; and an adequate wheat supply in most years. The 1666 census of New France was conducted by France's intendant , Jean Talon , in the winter of 1665–1666. The census showed a population count of 3,215 Acadians and habitants (French-Canadian farmers) in the administrative districts of Acadia and Canada. The census also revealed

29744-429: Was found to carry the deepest branch of the X2a haplogroup, and he did not have any European ancestry that would be expected for a European origin of the lineage. The Human T cell Lymphotrophic Virus 1 ( HTLV-1 ) is a virus transmitted through exchange of bodily fluids and from mother to child through breast milk. The mother-to-child transmission mimics a hereditary trait, although such transmission from maternal carriers

29920-421: Was generally believed that the first Paleo-Indian people to arrive in North America belonged to the Clovis culture. This archaeological phase was named after the city of Clovis, New Mexico , where in 1936 unique Clovis points were found in situ at the site of Blackwater Draw , where they were directly associated with the bones of Pleistocene animals. Recent data from a series of archaeological sites throughout

30096-544: Was intended to serve as a year-round military and naval base for France's remaining North American empire and to protect the entrance to the St. Lawrence River. Father Rale's War resulted in both the fall of New France's influence in present-day Maine and the British recognition that it would have to negotiate with the Mi'kmaq in Nova Scotia. During King George's War (1744 to 1748), an army of New Englanders led by William Pepperrell mounted an expedition of 90 vessels and 4,000 men against Louisbourg in 1745. Within three months

30272-402: Was mixed; claims of tools and bone processing were called "not plausible" by Prof. Tom Dillehay . The Yana River Rhino Horn site (RHS) has dated human occupation of eastern Arctic Siberia to 31,300 BP. That date has been interpreted by some as evidence that migration into Beringia was imminent, lending credence to occupation of Beringia during the LGM. However, the Yana RHS date is from

30448-434: Was non-existent in Inuit society before the introduction of the Canadian legal system . The Norse , who had settled Greenland and Iceland , arrived around 1000 CE and built a small settlement at L'Anse aux Meadows at the northernmost tip of Newfoundland (carbon dating estimate 990 – 1050 CE). L'Anse aux Meadows, the only confirmed Norse site in North America outside of Greenland, is also notable for its connection with

30624-422: Was not fully restored to French rule until the 1632 Treaty of Saint-Germain-en-Laye . This led to new French immigrants and the founding of Trois-Rivières in 1634. After Champlain's death in 1635, the Roman Catholic Church and the Jesuit establishment became the most dominant force in New France and hoped to establish a utopian European and Aboriginal Christian community. In 1642, the Sulpicians sponsored

30800-410: Was to suppress the second independence movement by Manitoba 's Métis , a mixed-blood people of joint First Nations and European descent, who originated in the mid-17th century. The desire for independence erupted in the Red River Rebellion in 1869 and the later North-West Rebellion in 1885 led by Louis Riel . Suppressing the Rebellion was Canada's first independent military action and demonstrated

30976-505: Was used as means of hunting megafauna. The Indigenous peoples of the Americas have an ascertained archaeological presence in the Americas dating back to about 15,000 years ago. More recent research, however, suggests a human presence dating to between 18,000 and 26,000 years ago, during the Last Glacial Maximum. There remain uncertainties regarding the precise dating of individual sites and regarding conclusions drawn from population genetics studies of contemporary Native Americans. In

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