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Hudson Bay

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Hudson Bay
Hudson bay large.svg
Hudson Bay, Canada
Hudson Bay 2008-07-21 by Aqua.jpg
LocationCanada
Coordinates60°N 86°W / 60°N 86°W / 60; -86 (Hudson Bay)[1]Coordinates: 60°N 86°W / 60°N 86°W / 60; -86 (Hudson Bay)[1]
Native name
Ocean/sea sourcesArctic Ocean, North Atlantic Ocean
Catchment area3,861,400 km2 (1,490,900 sq mi)
Basin countriesCanada and the United States
Max. length1,370 km (850 mi)
Max. width1,050 km (650 mi)
Surface area1,230,000 km2 (470,000 sq mi)
Average depth100 m (330 ft)
Max. depth270 m (890 ft)[2]
Frozenmid-December to mid-June
IslandsIslands of Hudson Bay
SettlementsRankin Inlet, Arviat, Puvirnituq, Churchill

Hudson Bay (Southern East Cree: ᐐᓂᐯᒄ, romanized: Wînipekw; Northern East Cree: ᐐᓂᐹᒄ, romanized: Wînipâkw; Inuktitut: ᑲᖏᖅᓱᐊᓗᒃ ᐃᓗᐊ, romanizedKangiqsualuk ilua[3] or Inuktitut: ᑕᓯᐅᔭᕐᔪᐊᖅ, romanizedTasiujarjuaq;[4] French: baie d'Hudson), sometimes called Hudson's Bay (usually historically), is a large body of saltwater in northeastern Canada with a surface area of 1,230,000 km2 (470,000 sq mi). It is located north of Ontario, west of Quebec, northeast of Manitoba and southeast of Nunavut, but politically entirely part of Nunavut.[5] It is an inland marginal sea of the Arctic Ocean. It drains a very large area, about 3,861,400 km2 (1,490,900 sq mi),[6] that includes parts of southeastern Nunavut, Alberta, Saskatchewan, Ontario, Quebec, all of Manitoba, and parts of the U.S. states of North Dakota, South Dakota, Minnesota, and Montana. Hudson Bay's southern arm is called James Bay.

The Eastern Cree name for Hudson and James Bay is Wînipekw (Southern dialect) or Wînipâkw (Northern dialect), meaning muddy or brackish water. Lake Winnipeg is similarly named by the local Cree, as is the location for the city of Winnipeg.

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French language

French language

French is a Romance language of the Indo-European family. It descended from the Vulgar Latin of the Roman Empire, as did all Romance languages. French evolved from Gallo-Romance, the Latin spoken in Gaul, and more specifically in Northern Gaul. Its closest relatives are the other langues d'oïl—languages historically spoken in northern France and in southern Belgium, which French (Francien) largely supplanted. French was also influenced by native Celtic languages of Northern Roman Gaul like Gallia Belgica and by the (Germanic) Frankish language of the post-Roman Frankish invaders. Today, owing to France's past overseas expansion, there are numerous French-based creole languages, most notably Haitian Creole. A French-speaking person or nation may be referred to as Francophone in both English and French.

Canada

Canada

Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, making it the world's second-largest country by total area, with the world's longest coastline. It is characterized by a wide range of both meteorologic and geological regions. The country is sparsely inhabited, with most residing south of the 55th parallel in urban areas. Canada's capital is Ottawa and its three largest metropolitan areas are Toronto, Montreal, and Vancouver.

Manitoba

Manitoba

Manitoba is a province of Canada at the longitudinal centre of the country. It is Canada's fifth-most populous province, with a population of 1,342,153 as of 2021, of widely varied landscape, from arctic tundra and the Hudson Bay coastline in the north to dense boreal forest, large freshwater lakes, and prairie grassland in the central and southern regions.

Inland sea

Inland sea

An inland sea is a continental body of water which is very large in area and is either completely surrounded by dry land or connected to an ocean by a river, strait or "arm of the sea". An inland sea will generally have higher salinity than a freshwater lake, but usually lower salinity than seawater.

Arctic Ocean

Arctic Ocean

The Arctic Ocean is the smallest and shallowest of the world's five major oceans. It spans an area of approximately 14,060,000 km2 (5,430,000 sq mi) and is known as the coldest of all the oceans. The International Hydrographic Organization (IHO) recognizes it as an ocean, although some oceanographers call it the Arctic Mediterranean Sea. It has been also been described as an estuary of the Atlantic Ocean. It is also seen as the northernmost part of the all-encompassing World Ocean.

Hudson Bay drainage basin

Hudson Bay drainage basin

The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about 3,861,400 square kilometres (1,490,900 sq mi), the basin is almost totally in Canada, with a small portion in the United States . The watershed's connection to the Labrador Sea is at the Hudson Strait's mouth between Resolution Island in the Qikiqtaaluk Region and Cape Chidley on the Labrador Peninsula. The watershed's headwaters to the south-west are on the Continental Divide of the Americas, bounded at Triple Divide Peak to the south, and Snow Dome to the north. The western and northern boundary of the watershed is the Arctic Divide, and the southern and eastern boundary is the Laurentian Divide.

Alberta

Alberta

Alberta is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada. The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds.

Minnesota

Minnesota

Minnesota is a state in the Upper Midwestern region of the United States. It is the 12th largest U.S. state in area and the 22nd most populous, with over 5.75 million residents. Minnesota is home to western prairies, now given over to intensive agriculture; deciduous forests in the southeast, now partially cleared, farmed, and settled; and the less populated North Woods, used for mining, forestry, and recreation. Roughly a third of the state is covered in forests, and it is known as the "Land of 10,000 Lakes" for having over 14,000 bodies of fresh water covering at least ten acres. More than 60% of Minnesotans live in the Minneapolis–Saint Paul metropolitan area, known as the "Twin Cities", the state's main political, economic, and cultural hub. With a population of about 3.7 million, the Twin Cities is the 16th largest metropolitan area in the U.S. Other minor metropolitan and micropolitan statistical areas in the state include Duluth, Mankato, Moorhead, Rochester, and St. Cloud.

James Bay

James Bay

James Bay is a large body of water located on the southern end of Hudson Bay in Canada. Both bodies of water extend from the Arctic Ocean, of which James Bay is the southernmost part. Despite bordering the Canadian provinces of Quebec and Ontario, the bay and the islands within it, the largest of which is Akimiski Island, are politically part of Nunavut.

Cree language

Cree language

Cree is a dialect continuum of Algonquian languages spoken by approximately 117,000 people across Canada, from the Northwest Territories to Alberta to Labrador. If considered one language, it is the aboriginal language with the highest number of speakers in Canada. The only region where Cree has any official status is in the Northwest Territories, alongside eight other aboriginal languages. There, Cree is spoken mainly in Fort Smith and Hay River.

Lake Winnipeg

Lake Winnipeg

Lake Winnipeg is a very large, relatively shallow 24,514-square-kilometre (9,465 sq mi) lake in North America, in the province of Manitoba, Canada. Its southern end is about 55 kilometres (34 mi) north of the city of Winnipeg. Lake Winnipeg is Canada's sixth-largest freshwater lake and the third-largest freshwater lake contained entirely within Canada, but it is relatively shallow excluding a narrow 36 m (118 ft) deep channel between the northern and southern basins. It is the eleventh-largest freshwater lake on Earth. The lake's east side has pristine boreal forests and rivers that were in 2018 inscribed as Pimachiowin Aki, a UNESCO World Heritage Site. The lake is 416 km (258 mi) from north to south, with remote sandy beaches, large limestone cliffs, and many bat caves in some areas. Manitoba Hydro uses the lake as one of the largest reservoirs in the world. There are many islands, most of them undeveloped.

Cree

Cree

The Cree are a North American Indigenous people. They live primarily in Canada, where they form one of the country's largest First Nations.

Description

The bay is named after Henry Hudson, an Englishman sailing for the Dutch East India Company, and after whom the river that he explored in 1609 is also named. Hudson Bay encompasses 1,230,000 km2 (470,000 sq mi), making it the second-largest water body using the term "bay" in the world (after the Bay of Bengal). The bay is relatively shallow and is considered an epicontinental sea, with an average depth of about 100 m (330 ft) (compared to 2,600 m (8,500 ft) in the Bay of Bengal). It is about 1,370 km (850 mi) long and 1,050 km (650 mi) wide.[7] On the east it is connected with the Atlantic Ocean by Hudson Strait; on the north, with the Arctic Ocean by Foxe Basin (which is not considered part of the bay), and Fury and Hecla Strait.

Hudson Bay is often considered part of the Arctic Ocean:[8] the International Hydrographic Organization, in its 2002 working draft[9] of Limits of Oceans and Seas, defined Hudson Bay, with its outlet extending from 62.5 to 66.5 degrees north (just a few miles south of the Arctic Circle) as being part of the Arctic Ocean, specifically "Arctic Ocean Subdivision 9.11". Other authorities include it in the Atlantic,[10] in part because of its greater water budget connection with that ocean.[11][12][13][14][15]

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Hudson Bay drainage basin

Hudson Bay drainage basin

The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about 3,861,400 square kilometres (1,490,900 sq mi), the basin is almost totally in Canada, with a small portion in the United States . The watershed's connection to the Labrador Sea is at the Hudson Strait's mouth between Resolution Island in the Qikiqtaaluk Region and Cape Chidley on the Labrador Peninsula. The watershed's headwaters to the south-west are on the Continental Divide of the Americas, bounded at Triple Divide Peak to the south, and Snow Dome to the north. The western and northern boundary of the watershed is the Arctic Divide, and the southern and eastern boundary is the Laurentian Divide.

Henry Hudson

Henry Hudson

Henry Hudson was an English sea explorer and navigator during the early 17th century, best known for his explorations of present-day Canada and parts of the northeastern United States.

Dutch East India Company

Dutch East India Company

The United East India Company was a chartered company established on 20 March 1602 by the States General of the Netherlands amalgamating existing companies into the first joint-stock company in the world, granting it a 21-year monopoly to carry out trade activities in Asia. Shares in the company could be bought by any resident of the United Provinces and then subsequently bought and sold in open-air secondary markets. It is sometimes considered to have been the first multinational corporation. It was a powerful company, possessing quasi-governmental powers, including the ability to wage war, imprison and execute convicts, negotiate treaties, strike its own coins, and establish colonies.

Hudson River

Hudson River

The Hudson River is a 315-mile (507 km) river that flows from north to south primarily through eastern New York. It originates in the Adirondack Mountains of Upstate New York and flows southward through the Hudson Valley to the New York Harbor between New York City and Jersey City, eventually draining into the Atlantic Ocean at Lower New York Bay. The river serves as a physical boundary between the states of New Jersey and New York at its southern end. Farther north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Even as far north as the city of Troy, the flow of the river changes direction with the tides.

Bay

Bay

A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or even another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action.

Bay of Bengal

Bay of Bengal

The Bay of Bengal is the northeastern part of the Indian Ocean, bounded on the west and northwest by India, on the north by Bangladesh, and on the east by Myanmar and the Andaman and Nicobar Islands of India. Its southern limit is a line between Sangaman Kanda, Sri Lanka, and the north westernmost point of Sumatra, Indonesia. It is the largest water region called a bay in the world. There are countries dependent on the Bay of Bengal in South Asia and Southeast Asia. During the existence of British India, it was named the Bay of Bengal after the historic Bengal region. At the time, the Port of Kolkata served as the gateway to the Crown rule in India. Cox's Bazar, the longest sea beach in the world and Sundarbans, the largest mangrove forest and the natural habitat of the Bengal tiger, are located along the bay.

Hudson Strait

Hudson Strait

The Hudson Strait links the Atlantic Ocean and the Labrador Sea to Hudson Bay in Canada. This strait lies between Baffin Island and Nunavik, with its eastern entrance marked by Cape Chidley in Newfoundland and Labrador and Resolution Island off Baffin Island. The strait is about 750 km long with an average width of 125 km, varying from 70 km at the eastern entrance to 240 km at Deception Bay.

Arctic Ocean

Arctic Ocean

The Arctic Ocean is the smallest and shallowest of the world's five major oceans. It spans an area of approximately 14,060,000 km2 (5,430,000 sq mi) and is known as the coldest of all the oceans. The International Hydrographic Organization (IHO) recognizes it as an ocean, although some oceanographers call it the Arctic Mediterranean Sea. It has been also been described as an estuary of the Atlantic Ocean. It is also seen as the northernmost part of the all-encompassing World Ocean.

Foxe Basin

Foxe Basin

Foxe Basin is a shallow oceanic basin north of Hudson Bay, in Nunavut, Canada, located between Baffin Island and the Melville Peninsula. For most of the year, it is blocked by sea ice and drift ice made up of multiple ice floes.

Fury and Hecla Strait

Fury and Hecla Strait

Fury and Hecla Strait is a narrow Arctic seawater channel located in the Qikiqtaaluk Region of Nunavut, Canada.

International Hydrographic Organization

International Hydrographic Organization

The International Hydrographic Organization (IHO) is an intergovernmental organisation representing hydrography. As of May 2022, the IHO comprised 98 Member States.

Arctic Circle

Arctic Circle

The Arctic Circle is one of the two polar circles, and the most northerly of the five major circles of latitude as shown on maps of Earth. Its southern equivalent is the Antarctic Circle.

History

Canada, routes of explorers, 1497 to 1905
Canada, routes of explorers, 1497 to 1905

The search for a western route to Cathay and the Indies, which had been actively pursued since the days of Columbus and the Cabots, in the latter part of the 15th century, directly resulted in the first sighting of Hudson Bay by Europeans.[16] English explorers and colonists named Hudson Bay after Sir Henry Hudson who explored the bay beginning August 2, 1610, on his ship Discovery.[17]: 170  On his fourth voyage to North America, Hudson worked his way around Greenland's west coast and into the bay, mapping much of its eastern coast. Discovery became trapped in the ice over the winter, and the crew survived onshore at the southern tip of James Bay. When the ice cleared in the spring, Hudson wanted to explore the rest of the area, but the crew mutinied on June 22, 1611. They left Hudson and others adrift in a small boat. The fate of Hudson and the crew members stranded with him is unknown, but historians have found no evidence that they survived for long afterward.[17]: 185  In May 1612, Sir Thomas Button sailed from England with two ships to look for Henry Hudson, and to continue the search for the Northwest Passage to Asia.[16]

In 1668, Nonsuch reached the bay and traded for beaver pelts, leading to the creation of the Hudson's Bay Company (HBC), which still bears the historic name.[18] The HBC negotiated a trading monopoly from the English crown for the Hudson Bay watershed, called Rupert's Land.[19]: 4  France contested this grant by sending several military expeditions to the region, but abandoned its claim in the Treaty of Utrecht (April 1713).[20]

During this period, the HBC built several factories (forts and trading posts) along the coast at the mouth of the major rivers (such as Fort Severn, Ontario; York Factory, Churchill; and the Prince of Wales Fort). The strategic locations were bases for inland exploration. More importantly, they were trading posts with Indigenous peoples who came to them with furs from their trapping season. The HBC shipped the furs to Europe and continued to use some of these posts well into the 20th century.

HBC's trade monopoly was abolished in 1870, and it ceded Rupert's Land to Canada, an area of approximately 3,900,000 km2 (1,500,000 sq mi), as part of the Northwest Territories.[19]: 427  In 1912, the western shore south of 60° and all the eastern shore were transferred to the adjacent provinces, but the bay and offshore islands remained part of the Northwest Territories. Starting in 1913, the bay was extensively charted by the Canadian government's CSS Acadia to develop it for navigation.[21] This mapping progress led to the establishment of Churchill, Manitoba, as a deep-sea port for wheat exports in 1929, after unsuccessful attempts at Port Nelson.

The Port of Churchill was an important shipping link for trade with Europe and Russia until its closure in 2016 by owner OmniTRAX.[22] The port and the Hudson Bay Railway were then sold to the Arctic Gateway Group—a consortium of First Nations, local governments, and corporate investors—in 2018.[23] On July 9, 2019, ships on missions to resupply arctic communities began stopping at the port for additional cargo,[24] and the port began shipping grain again on September 7, 2019.[25]

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Cathay

Cathay

Cathay is a historical name for China that was used in Europe. During the early modern period, the term Cathay initially evolved as a term referring to what is now Northern China, completely separate and distinct from China, which was a reference to southern China. As knowledge of East Asia increased, Cathay came to be seen as the same polity as China as a whole. The term Cathay became a poetic name for China.

Christopher Columbus

Christopher Columbus

Christopher Columbus was an Italian explorer and navigator from the Republic of Genoa who completed four voyages across the Atlantic Ocean sponsored by the Catholic Monarchs of Spain, opening the way for the widespread European exploration and European colonization of the Americas. His expeditions were the first known European contact with the Caribbean and Central and South America.

John Cabot

John Cabot

John Cabot was an Italian navigator and explorer. His 1497 voyage to the coast of North America under the commission of Henry VII of England is the earliest-known European exploration of coastal North America since the Norse visits to Vinland in the eleventh century. To mark the celebration of the 500th anniversary of Cabot's expedition, both the Canadian and British governments elected Cape Bonavista, Newfoundland as representing Cabot's first landing site. However, alternative locations have also been proposed.

Discovery (1602 ship)

Discovery (1602 ship)

Discovery or Discoverie was a small 20-ton, 38-foot (12 m) long "fly-boat" of the British East India Company, launched before 1602. It was one of the three ships on the 1606–1607 voyage to the New World for the English Virginia Company of London. The journey resulted in the founding of Jamestown in the new Colony of Virginia.

Greenland

Greenland

Greenland is an island country in North America and part of the Kingdom of Denmark. It lies between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three countries that form the Kingdom of Denmark, the others being Denmark and the Faroe Islands; the citizens of all these countries are citizens of Denmark and of the European Union. The capital of Greenland is Nuuk.

James Bay

James Bay

James Bay is a large body of water located on the southern end of Hudson Bay in Canada. Both bodies of water extend from the Arctic Ocean, of which James Bay is the southernmost part. Despite bordering the Canadian provinces of Quebec and Ontario, the bay and the islands within it, the largest of which is Akimiski Island, are politically part of Nunavut.

Nonsuch (1650 ship)

Nonsuch (1650 ship)

Nonsuch was the ketch that sailed into Hudson Bay in 1668-1669 under Zachariah Gillam, in the first trading voyage for what was to become the Hudson's Bay Company two years later. Originally built as a merchant ship in 1650, and later the Royal Navy ketch HMS Nonsuch, the vessel was sold to Sir William Warren in 1667. The name means "none such", i.e. "unequalled". The ship was at the time considered smaller than many others but was specifically selected because of her small size so that when she arrived in Hudson Bay and James Bay she could be sailed up-river and taken out of water so the thick ice of the bay wouldn't crush her.

Hudson's Bay Company

Hudson's Bay Company

The Hudson's Bay Company is a Canadian retail business group. A fur trading business for much of its existence, it became the largest and oldest corporation in Canada, and now owns and operates retail stores across the country. The company's namesake business division is Hudson's Bay, commonly referred to as The Bay.

Kingdom of England

Kingdom of England

The Kingdom of England existed on the island of Great Britain from 12 July 927, when it unified from various Anglo-Saxon kingdoms, until 1 May 1707, when it united with Scotland to form the Kingdom of Great Britain.

Drainage basin

Drainage basin

A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the drainage divide, made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern.

List of Anglo-French conflicts on Hudson Bay

List of Anglo-French conflicts on Hudson Bay

The Anglo-French conflicts on Hudson Bay were a series of conflicts in the 17th and 18th centuries between England and France for control over the area around the Hudson Bay.

Factory (trading post)

Factory (trading post)

Factory was the common name during the medieval and early modern eras for an entrepôt – which was essentially an early form of free-trade zone or transshipment point. At a factory, local inhabitants could interact with foreign merchants, often known as factors. First established in Europe, factories eventually spread to many other parts of the world. The origin of the word factory is from Latin factorium 'place of doers, makers'.

Geography and climate

Map including Hudson Bay
Map including Hudson Bay

Extent

The International Hydrographic Organization defines the northern limit of Hudson Bay as follows:[26]

A line from Nuvuk Point (62°21′N 78°06′W / 62.350°N 78.100°W / 62.350; -78.100) to Leyson Point, the Southeastern extreme of Southampton Island, through the Southern and Western shores of Southampton Island to its Northern extremity, thence a line to Beach Point (66°03′N 86°06′W / 66.050°N 86.100°W / 66.050; -86.100) on the Mainland.

Climate

Polar bear walks on newly formed ice in early November at Hudson Bay.
Polar bear walks on newly formed ice in early November at Hudson Bay.

Northern Hudson Bay has a polar climate (Köppen: ET) being one of the few places in the world where this type of climate is found south of 60 °N, going farther south towards Quebec, where Inukjuak is still dominated by the tundra. From Arviat, Nunavut, to the west to the south and southeast prevails the subarctic climate (Köppen: Dfc). This is because in the central summer months, heat waves can advance from the hot land and make the weather milder, with the result that the average temperature surpasses 10 °C or 50 °F. At the extreme southern tip of the extension known as James Bay arises a humid continental climate with a longer and generally hotter summer. (Köppen: Dfb)[27] The average annual temperature in almost the entire bay is around 0 °C (32 °F) or below. In the extreme northeast, winter temperatures average as low as −29 °C or −20.2 °F.[28]

The Hudson Bay region has very low year-round average temperatures. The average annual temperature for Churchill at 59°N is −6 °C or 21.2 °F and Inukjuak, facing cool westerlies in summer at 58°N, an even colder −7 °C or 19.4 °F. By comparison, Magadan, in a comparable position at 59°N on the Eurasian landmass in the Russian Far East and with a similar subarctic climate, has an annual average of −2.7 °C or 27.1 °F.[29] Vis-à-vis geographically closer Europe, contrasts stand much more extreme. Arkhangelsk at 64°N in northwestern Russia has an average of 2 °C or 36 °F,[30] while the mild continental coastline of Stockholm at 59°N on the shore of an analogous large hyposaline marine inlet – the Baltic Sea – has an annual average of 8 °C or 46 °F.[31]

Water temperature peaks at 8–9 °C (46.4–48.2 °F) on the western side of the bay in late summer. It is largely frozen over from mid-December to mid-June, when it usually clears from its eastern end westwards and southwards. A steady increase in regional temperatures over the last 100 years has been reflected in a lengthening of the ice-free period, which was as short as four months in the late 17th century.[32]

Climate data for Arviat Airport (1981–2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) −1.5
(29.3)
−1.5
(29.3)
3.5
(38.3)
4.0
(39.2)
14.5
(58.1)
30.8
(87.4)
33.9
(93.0)
30.0
(86.0)
23.0
(73.4)
18.1
(64.6)
2.1
(35.8)
−0.4
(31.3)
33.9
(93.0)
Average high °C (°F) −25.4
(−13.7)
−24.2
(−11.6)
−18
(0)
−9.1
(15.6)
−1.2
(29.8)
7.7
(45.9)
15.1
(59.2)
14.2
(57.6)
7.3
(45.1)
−1
(30)
−12
(10)
−20.3
(−4.5)
−5.6
(21.9)
Daily mean °C (°F) −29.3
(−20.7)
−28.3
(−18.9)
−22.8
(−9.0)
−14
(7)
−4.3
(24.3)
4.4
(39.9)
11.1
(52.0)
10.8
(51.4)
4.8
(40.6)
−3.6
(25.5)
−16.1
(3.0)
−24.1
(−11.4)
−9.3
(15.3)
Average low °C (°F) −33.1
(−27.6)
−32.4
(−26.3)
−27.5
(−17.5)
−18.7
(−1.7)
−7.4
(18.7)
1.0
(33.8)
7.0
(44.6)
7.3
(45.1)
2.2
(36.0)
−6.2
(20.8)
−20.1
(−4.2)
−27.9
(−18.2)
−13
(9)
Record low °C (°F) −48.3
(−54.9)
−47
(−53)
−41.5
(−42.7)
−36.7
(−34.1)
−26.7
(−16.1)
−11
(12)
−4
(25)
−0.6
(30.9)
−8.3
(17.1)
−26
(−15)
−34
(−29)
−42.5
(−44.5)
−48.3
(−54.9)
Average precipitation mm (inches) 10.1
(0.40)
6.6
(0.26)
11.4
(0.45)
12.5
(0.49)
18.2
(0.72)
29.6
(1.17)
36.7
(1.44)
56.0
(2.20)
44.0
(1.73)
24.5
(0.96)
18.6
(0.73)
18.3
(0.72)
286.5
(11.28)
Average rainfall mm (inches) 0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.5
(0.02)
6.1
(0.24)
26.3
(1.04)
36.7
(1.44)
56.0
(2.20)
41.2
(1.62)
7.6
(0.30)
0.0
(0.0)
0.0
(0.0)
174.4
(6.87)
Average snowfall cm (inches) 10.1
(4.0)
6.6
(2.6)
11.4
(4.5)
12.1
(4.8)
12.1
(4.8)
3.2
(1.3)
0.0
(0.0)
0.0
(0.0)
2.8
(1.1)
16.9
(6.7)
18.8
(7.4)
18.3
(7.2)
112.4
(44.3)
Average precipitation days (≥ 0.2 mm) 7.4 7.2 9.1 7.1 7.6 8.0 8.9 14.1 12.6 10.8 10.3 8.1 111.3
Average rainy days (≥ 0.2 mm) 0.0 0.0 0.0 0.3 2.0 7.4 8.9 14.1 11.6 2.8 0.0 0.0 47.0
Average snowy days (≥ 0.2 cm) 7.4 7.2 9.1 7.0 5.8 0.8 0.0 0.0 1.1 8.2 10.3 8.1 65.0
Average relative humidity (%) 69.1 69.9 74.4 79.8 84.6 76.8 72.7 74.7 74.6 84.1 80.7 73.3 76.2
Source: Environment Canada[33][34]
Climate data for Churchill Airport (1981–2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 1.7
(35.1)
1.8
(35.2)
9.0
(48.2)
28.2
(82.8)
28.9
(84.0)
32.2
(90.0)
34.0
(93.2)
36.9
(98.4)
29.2
(84.6)
21.7
(71.1)
7.2
(45.0)
3.0
(37.4)
36.9
(98.4)
Average high °C (°F) −21.9
(−7.4)
−20.2
(−4.4)
−13.9
(7.0)
−5.1
(22.8)
2.9
(37.2)
12.0
(53.6)
18.0
(64.4)
16.8
(62.2)
9.5
(49.1)
1.6
(34.9)
−9
(16)
−17.8
(0.0)
−2.3
(27.9)
Daily mean °C (°F) −26
(−15)
−24.5
(−12.1)
−18.9
(−2.0)
−9.8
(14.4)
−1
(30)
7.0
(44.6)
12.7
(54.9)
12.3
(54.1)
6.4
(43.5)
−1.2
(29.8)
−12.7
(9.1)
−21.9
(−7.4)
−6.5
(20.3)
Average low °C (°F) −30.1
(−22.2)
−28.8
(−19.8)
−23.9
(−11.0)
−14.4
(6.1)
−5
(23)
2.0
(35.6)
7.3
(45.1)
7.7
(45.9)
3.2
(37.8)
−3.9
(25.0)
−16.4
(2.5)
−25.9
(−14.6)
−10.7
(12.7)
Record low °C (°F) −45.6
(−50.1)
−45.4
(−49.7)
−43.9
(−47.0)
−33.3
(−27.9)
−25.2
(−13.4)
−9.4
(15.1)
−2.2
(28.0)
−2.2
(28.0)
−11.7
(10.9)
−24.5
(−12.1)
−36.1
(−33.0)
−43.9
(−47.0)
−45.6
(−50.1)
Average precipitation mm (inches) 18.7
(0.74)
16.6
(0.65)
18.1
(0.71)
23.6
(0.93)
30.0
(1.18)
44.2
(1.74)
59.8
(2.35)
69.4
(2.73)
69.9
(2.75)
48.4
(1.91)
35.5
(1.40)
18.4
(0.72)
452.5
(17.81)
Average rainfall mm (inches) 0.0
(0.0)
0.0
(0.0)
0.4
(0.02)
1.1
(0.04)
16.1
(0.63)
41.0
(1.61)
59.8
(2.35)
69.3
(2.73)
66.0
(2.60)
20.9
(0.82)
1.3
(0.05)
0.1
(0.00)
276.0
(10.87)
Average snowfall cm (inches) 21.7
(8.5)
19.3
(7.6)
20.4
(8.0)
24.9
(9.8)
15.5
(6.1)
3.3
(1.3)
0.0
(0.0)
0.0
(0.0)
4.2
(1.7)
29.8
(11.7)
39.2
(15.4)
22.9
(9.0)
201.2
(79.2)
Average precipitation days (≥ 0.2 mm) 11.9 10.2 11.0 8.9 10.2 12.0 13.9 15.4 15.9 15.7 15.5 11.9 152.6
Average rainy days (≥ 0.2 mm) 0.09 0.05 0.45 1.4 5.1 10.7 13.9 14.9 14.5 6.5 0.91 0.24 67.5
Average snowy days (≥ 0.2 cm) 11.9 10.3 11.1 8.3 6.7 1.5 0.0 0.06 2.6 11.6 15.6 12.3 92.1
Mean monthly sunshine hours 79.7 117.7 177.8 198.2 197.0 243.0 281.7 225.9 112.0 58.1 55.3 53.1 1,799.5
Percent possible sunshine 36.2 45.1 48.7 45.8 37.7 44.3 51.6 47.2 29.0 18.2 23.5 26.7 37.8
Source: Environment Canada[35][36][37]
Climate data for Coral Harbour Airport (1981–2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high humidex −0.6 −1.9 −0.5 4.4 8.9 22.8 32.8 30.1 19.9 7.6 3.7 3.2 32.8
Record high °C (°F) −0.6
(30.9)
−1.1
(30.0)
0.0
(32.0)
5.0
(41.0)
9.4
(48.9)
23.3
(73.9)
28.0
(82.4)
26.1
(79.0)
18.5
(65.3)
7.6
(45.7)
4.0
(39.2)
3.4
(38.1)
28.0
(82.4)
Average high °C (°F) −25.5
(−13.9)
−25.5
(−13.9)
−20.4
(−4.7)
−10.9
(12.4)
−2.9
(26.8)
6.4
(43.5)
14.7
(58.5)
11.7
(53.1)
4.6
(40.3)
−3
(27)
−11.9
(10.6)
−20.1
(−4.2)
−6.9
(19.6)
Daily mean °C (°F) −29.6
(−21.3)
−29.7
(−21.5)
−25.2
(−13.4)
−16.1
(3.0)
−6.7
(19.9)
3.1
(37.6)
10.0
(50.0)
7.7
(45.9)
1.7
(35.1)
−6.1
(21.0)
−16.1
(3.0)
−24.4
(−11.9)
−11
(12)
Average low °C (°F) −33.7
(−28.7)
−33.9
(−29.0)
−29.9
(−21.8)
−21.1
(−6.0)
−10.5
(13.1)
−0.3
(31.5)
5.3
(41.5)
3.6
(38.5)
−1.2
(29.8)
−9.1
(15.6)
−20.3
(−4.5)
−28.6
(−19.5)
−15
(5)
Record low °C (°F) −52.8
(−63.0)
−51.4
(−60.5)
−49.4
(−56.9)
−39.4
(−38.9)
−31.1
(−24.0)
−15.6
(3.9)
−1.1
(30.0)
−3.3
(26.1)
−17.2
(1.0)
−34.4
(−29.9)
−40.6
(−41.1)
−48.9
(−56.0)
−52.8
(−63.0)
Record low wind chill −69.5 −69.3 −64.3 −55.1 −39.7 −23.2 −8.2 −11.8 −23.7 −43.7 −54.8 −64.2 −69.5
Average precipitation mm (inches) 9.5
(0.37)
7.0
(0.28)
11.2
(0.44)
18.2
(0.72)
19.0
(0.75)
27.6
(1.09)
34.1
(1.34)
59.4
(2.34)
45.4
(1.79)
33.8
(1.33)
22.9
(0.90)
14.8
(0.58)
302.9
(11.93)
Average rainfall mm (inches) 0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.4
(0.02)
4.3
(0.17)
20.8
(0.82)
34.1
(1.34)
58.9
(2.32)
36.7
(1.44)
7.2
(0.28)
0.5
(0.02)
0.0
(0.0)
163.0
(6.42)
Average snowfall cm (inches) 9.6
(3.8)
7.1
(2.8)
11.3
(4.4)
18.2
(7.2)
14.9
(5.9)
6.9
(2.7)
0.0
(0.0)
0.6
(0.2)
8.6
(3.4)
26.7
(10.5)
22.9
(9.0)
14.8
(5.8)
141.6
(55.7)
Average precipitation days (≥ 0.2 mm) 8.5 6.7 9.0 9.5 10.4 9.6 9.6 12.6 11.2 14.6 13.0 10.4 125.1
Average rainy days (≥ 0.2 mm) 0.0 0.0 0.0 0.2 1.8 7.2 9.6 12.5 8.2 3.6 0.6 0.1 43.8
Average snowy days (≥ 0.2 cm) 8.6 6.6 9.0 9.5 9.4 3.3 0.0 0.3 4.3 13.1 12.9 10.4 87.3
Average relative humidity (%) 64.9 64.2 67.5 73.8 80.3 73.9 63.1 68.9 75.6 84.8 77.6 69.7 72.0
Mean monthly sunshine hours 37.9 112.1 187.4 240.2 239.9 262.2 312.3 220.4 109.8 70.8 47.9 18.8 1,859.7
Percent possible sunshine 22.4 47.0 51.6 53.2 42.0 41.9 51.2 43.3 27.9 23.3 24.3 13.9 36.8
Source: Environment Canada Canadian Climate Normals 1981–2010[38]
Climate data for Inukjuak (1971–2000)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high humidex −0.6 2.4 4.4 6.5 16.0 32.4 34.0 28.4 19.8 12.2 7.2 1.4 34.0
Record high °C (°F) 0.6
(33.1)
5.0
(41.0)
3.9
(39.0)
7.2
(45.0)
23.3
(73.9)
30.0
(86.0)
27.8
(82.0)
25.6
(78.1)
22.8
(73.0)
16.7
(62.1)
8.3
(46.9)
16.1
(61.0)
30.0
(86.0)
Average high °C (°F) −21
(−6)
−21.6
(−6.9)
−16.3
(2.7)
−7.1
(19.2)
1.2
(34.2)
8.4
(47.1)
13.2
(55.8)
12.5
(54.5)
7.7
(45.9)
2.0
(35.6)
−4.2
(24.4)
−15
(5)
−3.4
(25.9)
Daily mean °C (°F) −24.8
(−12.6)
−25.8
(−14.4)
−21.2
(−6.2)
−11.7
(10.9)
−1.9
(28.6)
4.6
(40.3)
9.4
(48.9)
9.2
(48.6)
5.1
(41.2)
−0.3
(31.5)
−7.4
(18.7)
−18.9
(−2.0)
−7
(19)
Average low °C (°F) −28.6
(−19.5)
−29.9
(−21.8)
−26.1
(−15.0)
−16.3
(2.7)
−5.1
(22.8)
0.8
(33.4)
5.5
(41.9)
5.9
(42.6)
2.5
(36.5)
−2.6
(27.3)
−10.6
(12.9)
−22.7
(−8.9)
−10.6
(12.9)
Record low °C (°F) −46.1
(−51.0)
−49.4
(−56.9)
−45
(−49)
−34.4
(−29.9)
−25.6
(−14.1)
−9.4
(15.1)
−6.7
(19.9)
−2.8
(27.0)
−11.1
(12.0)
−22.8
(−9.0)
−33.9
(−29.0)
−43.3
(−45.9)
−49.4
(−56.9)
Record low wind chill −60 −58 −55 −46 −36 −15 −7 −5 −12 −31 −47 −55 −60
Average precipitation mm (inches) 14.4
(0.57)
11.6
(0.46)
15.5
(0.61)
22.6
(0.89)
27.0
(1.06)
38.2
(1.50)
60.1
(2.37)
61.1
(2.41)
70.1
(2.76)
58.6
(2.31)
50.6
(1.99)
30.3
(1.19)
459.9
(18.11)
Average rainfall mm (inches) 0.0
(0.0)
0.1
(0.00)
0.1
(0.00)
3.6
(0.14)
12.6
(0.50)
33.6
(1.32)
59.5
(2.34)
61.1
(2.41)
62.2
(2.45)
28.2
(1.11)
3.2
(0.13)
0.4
(0.02)
264.6
(10.42)
Average snowfall cm (inches) 15.0
(5.9)
12.0
(4.7)
16.1
(6.3)
19.4
(7.6)
14.6
(5.7)
4.4
(1.7)
1.0
(0.4)
0.0
(0.0)
7.5
(3.0)
32.6
(12.8)
50.0
(19.7)
32.0
(12.6)
204.5
(80.5)
Average rainy days (≥ 0.2 mm) 0.09 0.04 0.09 1.2 4.5 8.5 12.8 15.1 16.2 8.6 1.2 0.13 68.5
Average snowy days (≥ 0.2 cm) 10.8 9.2 9.3 9.9 8.4 3.6 0.26 0.13 5.0 15.6 20.3 15.3 107.8
Mean monthly sunshine hours 63.5 122.5 182.5 183.2 159.4 209.4 226.0 171.7 97.9 50.4 31.8 35.2 1,533.5
Percent possible sunshine 28.6 46.7 49.9 42.5 30.6 38.4 41.6 36.0 25.4 15.8 13.4 17.5 32.2
Source: Environment Canada[39]
Climate data for Kuujjuarapik Airport (1981−2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 3.3
(37.9)
9.4
(48.9)
11.1
(52.0)
21.9
(71.4)
32.0
(89.6)
33.9
(93.0)
37.0
(98.6)
33.3
(91.9)
33.9
(93.0)
23.9
(75.0)
11.8
(53.2)
7.2
(45.0)
37.0
(98.6)
Average high °C (°F) −18.7
(−1.7)
−17.5
(0.5)
−10.8
(12.6)
−2
(28)
6.2
(43.2)
12.4
(54.3)
15.9
(60.6)
16.1
(61.0)
11.2
(52.2)
5.1
(41.2)
−2.1
(28.2)
−11.1
(12.0)
0.4
(32.7)
Daily mean °C (°F) −23.3
(−9.9)
−22.9
(−9.2)
−16.7
(1.9)
−7.2
(19.0)
1.6
(34.9)
7.2
(45.0)
11.1
(52.0)
11.8
(53.2)
8.0
(46.4)
2.4
(36.3)
−4.9
(23.2)
−15
(5)
−4
(25)
Average low °C (°F) −27.8
(−18.0)
−28.3
(−18.9)
−22.6
(−8.7)
−12.3
(9.9)
−3
(27)
2.0
(35.6)
6.2
(43.2)
7.6
(45.7)
4.7
(40.5)
−0.3
(31.5)
−7.6
(18.3)
−18.7
(−1.7)
−8.3
(17.1)
Record low °C (°F) −49.4
(−56.9)
−48.9
(−56.0)
−45
(−49)
−33.9
(−29.0)
−25
(−13)
−7.8
(18.0)
−2.2
(28.0)
−1.1
(30.0)
−6.1
(21.0)
−15
(5)
−28.9
(−20.0)
−46.1
(−51.0)
−49.4
(−56.9)
Average precipitation mm (inches) 27.9
(1.10)
22.7
(0.89)
23.2
(0.91)
23.7
(0.93)
33.5
(1.32)
59.6
(2.35)
75.8
(2.98)
91.6
(3.61)
109.3
(4.30)
81.6
(3.21)
65.9
(2.59)
46.1
(1.81)
660.8
(26.02)
Average rainfall mm (inches) 0.05
(0.00)
0.64
(0.03)
2.1
(0.08)
6.9
(0.27)
19.9
(0.78)
55.1
(2.17)
75.9
(2.99)
91.6
(3.61)
106.5
(4.19)
53.4
(2.10)
9.4
(0.37)
0.65
(0.03)
422.0
(16.61)
Average snowfall cm (inches) 29.3
(11.5)
22.8
(9.0)
22.1
(8.7)
17.3
(6.8)
14.3
(5.6)
4.4
(1.7)
0.0
(0.0)
0.0
(0.0)
2.9
(1.1)
29.4
(11.6)
58.5
(23.0)
47.9
(18.9)
248.8
(98.0)
Average precipitation days (≥ 0.2 mm) 17.2 14.0 12.7 11.3 12.2 12.1 13.9 16.5 20.8 21.6 22.0 21.3 195.5
Average rainy days (≥ 0.2 mm) 0.17 0.38 1.0 3.2 6.9 10.6 13.9 16.5 20.0 14.1 3.6 0.41 90.9
Average snowy days (≥ 0.2 cm) 17.2 13.9 12.5 9.6 7.0 2.8 0.0 0.0 2.0 12.1 20.6 21.2 118.9
Mean monthly sunshine hours 71.7 112.7 155.8 165.2 166.4 205.0 213.5 163.7 81.8 64.4 34.2 40.0 1,474.3
Percent possible sunshine 29.6 41.5 42.5 39.0 33.2 39.4 41.0 35.2 21.3 19.8 13.5 17.8 31.2
Source: Environment Canada[40]
Climate data for Rankin Inlet Airport (1981–2010)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high humidex −3 −4.4 1.1 2.5 13.4 26.3 32.2 31.8 21.8 11.7 1.4 0.8 32.2
Record high °C (°F) −2.5
(27.5)
−4.4
(24.1)
1.3
(34.3)
3.4
(38.1)
14.1
(57.4)
26.1
(79.0)
28.9
(84.0)
30.5
(86.9)
20.6
(69.1)
11.8
(53.2)
1.5
(34.7)
0.9
(33.6)
30.5
(86.9)
Average high °C (°F) −27.3
(−17.1)
−26.1
(−15.0)
−20.6
(−5.1)
−11.1
(12.0)
−2.4
(27.7)
7.9
(46.2)
14.9
(58.8)
13.1
(55.6)
6.3
(43.3)
−1.9
(28.6)
−13
(9)
−21.9
(−7.4)
−6.9
(19.6)
Daily mean °C (°F) −30.8
(−23.4)
−29.9
(−21.8)
−25
(−13)
−15.6
(3.9)
−5.8
(21.6)
4.2
(39.6)
10.5
(50.9)
9.7
(49.5)
3.8
(38.8)
−4.6
(23.7)
−17
(1)
−25.7
(−14.3)
−10.5
(13.1)
Average low °C (°F) −34.4
(−29.9)
−33.6
(−28.5)
−29.2
(−20.6)
−20.1
(−4.2)
−9
(16)
0.5
(32.9)
6.1
(43.0)
6.2
(43.2)
1.3
(34.3)
−7.3
(18.9)
−20.9
(−5.6)
−29.4
(−20.9)
−14.2
(6.4)
Record low °C (°F) −46.1
(−51.0)
−49.8
(−57.6)
−43.4
(−46.1)
−35.7
(−32.3)
−23.8
(−10.8)
−9.4
(15.1)
−1.9
(28.6)
−1.4
(29.5)
−9
(16)
−27.4
(−17.3)
−36.5
(−33.7)
−43.6
(−46.5)
−49.8
(−57.6)
Record low wind chill −66.8 −70.5 −64.4 −53.6 −35.9 −17.6 −5.3 −8.8 −18.1 −42.7 −55.3 −62.4 −70.5
Average precipitation mm (inches) 8.7
(0.34)
8.2
(0.32)
12.3
(0.48)
19.9
(0.78)
19.5
(0.77)
26.6
(1.05)
42.0
(1.65)
57.4
(2.26)
42.9
(1.69)
38.0
(1.50)
21.7
(0.85)
12.8
(0.50)
310.1
(12.21)
Average rainfall mm (inches) 0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
1.1
(0.04)
7.0
(0.28)
22.1
(0.87)
41.9
(1.65)
57.2
(2.25)
39.1
(1.54)
12.9
(0.51)
0.3
(0.01)
0.1
(0.00)
181.8
(7.16)
Average snowfall cm (inches) 8.9
(3.5)
8.5
(3.3)
12.5
(4.9)
19.2
(7.6)
13.0
(5.1)
4.6
(1.8)
0.1
(0.0)
0.2
(0.1)
3.8
(1.5)
25.5
(10.0)
22.4
(8.8)
13.3
(5.2)
131.9
(51.9)
Average precipitation days (≥ 0.2 mm) 7.8 6.6 9.0 8.5 8.7 7.7 10.4 13.2 12.7 14.9 12.6 10.0 122.1
Average rainy days (≥ 0.2 mm) 0.0 0.0 0.0 0.7 2.3 6.3 10.4 13.2 10.5 4.2 0.4 0.1 48.4
Average snowy days (≥ 0.2 cm) 7.8 6.7 9.0 8.2 7.1 2.0 0.1 0.1 3.3 12.4 12.5 10.0 79.3
Average relative humidity (%) 66.2 67.3 71.3 79.0 82.3 72.3 66.6 70.6 76.3 84.5 78.4 70.2 73.7
Source: Environment Canada Canadian Climate Normals 1981–2010[41]

Waters

In late spring (May), large chunks of ice float near the eastern shore of the bay, while the centre of the bay remains frozen to the west. Between 1971 and 2007, the length of the ice-free season increased by about seven days in the southwestern part of the Hudson Bay, historically the last area to thaw.
In late spring (May), large chunks of ice float near the eastern shore of the bay, while the centre of the bay remains frozen to the west. Between 1971 and 2007, the length of the ice-free season increased by about seven days in the southwestern part of the Hudson Bay, historically the last area to thaw.

Hudson Bay has a lower average salinity level than that of ocean water. The main causes are the low rate of evaporation (the bay is ice-covered for much of the year), the large volume of terrestrial runoff entering the bay (about 700 km3 (170 cu mi) annually, the Hudson Bay watershed covering much of Canada, many rivers and streams discharging into the bay), and the limited connection with the Atlantic Ocean and its higher salinity.[42] Sea ice is about three times the annual river flow into the bay, and its annual freezing and thawing significantly alters the salinity of the surface layer. Although its exact effects are not fully understood currently, the cyclonic storms in the bay are responsible for synoptic variability of salinity along the coast.[43]

One consequence of the lower salinity of the bay is that the freezing point of the water is higher than in the rest of the world's oceans, thus decreasing the time that the bay remains ice-free. The increase of river inflows during the winter has decreased the season of sea ice by more than 1 month since the 1960s.[44]

The lower salinity of the bay also has effects on the distribution and prevalence of common marine life such as micro algae. Research has shown that the lower salinity of the Hudson Bay limits the growth of micro algae, which causes a notable change in biomass along the bay's salinity gradient.[45]

Shores

The western shores of the bay are a lowland known as the Hudson Bay Lowlands which covers 324,000 km2 (125,000 sq mi). The area is drained by a large number of rivers and has formed a characteristic vegetation known as muskeg. Much of the landform has been shaped by the actions of glaciers and the shrinkage of the bay over long periods of time. Signs of numerous former beachfronts can be seen far inland from the current shore. A large portion of the lowlands in the province of Ontario is part of the Polar Bear Provincial Park, and a similar portion of the lowlands in Manitoba is contained in Wapusk National Park, the latter location being a significant polar bear maternity denning area.[46]

In contrast, most of the eastern shores (the Quebec portion) form the western edge of the Canadian Shield in Quebec. The area is rocky and hilly. Its vegetation is typically boreal forest, and to the north, tundra.

Measured by shoreline, Hudson Bay is the largest bay in the world (the largest in area being the Bay of Bengal).

The distinctive arculate segment on the eastern shore of Hudson Bay is referred to as the Nastapoka arc.

Islands

There are many islands in Hudson Bay, mostly near the eastern coast. All the islands, including those in James Bay, are part of Nunavut and lie in the Arctic Archipelago. Several are disputed by the Cree.[47] One group of islands is the Belcher Islands. Another group includes the Ottawa Islands.

Discover more about Geography and climate related topics

International Hydrographic Organization

International Hydrographic Organization

The International Hydrographic Organization (IHO) is an intergovernmental organisation representing hydrography. As of May 2022, the IHO comprised 98 Member States.

Köppen climate classification

Köppen climate classification

The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, German climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification.

Inukjuak

Inukjuak

Inukjuak is a northern village located on Hudson Bay at the mouth of the Innuksuak River in Nunavik, in the Nord-du-Québec region of northern Quebec, Canada. Its population is 1,821 as of the 2021 Canadian Census. An older spelling is Inoucdjouac; its former name was Port Harrison.

Arviat

Arviat

Arviat is a predominantly Inuit hamlet located on the western shore of Hudson Bay in the Kivalliq Region of Nunavut, Canada. Arviat is derived from the Inuktitut word arviq meaning "Bowhead whale". Earlier in history, its name was Tikirajualaaq, and Ittaliurvik,.

Nunavut

Nunavut

Nunavut is the largest and northernmost territory of Canada. It was separated officially from the Northwest Territories on April 1, 1999, via the Nunavut Act and the Nunavut Land Claims Agreement Act, which provided this territory to the Inuit for independent government. The boundaries had been drawn in 1993. The creation of Nunavut resulted in the first major change to Canada's political map in half a century since the province of Newfoundland was admitted in 1949.

James Bay

James Bay

James Bay is a large body of water located on the southern end of Hudson Bay in Canada. Both bodies of water extend from the Arctic Ocean, of which James Bay is the southernmost part. Despite bordering the Canadian provinces of Quebec and Ontario, the bay and the islands within it, the largest of which is Akimiski Island, are politically part of Nunavut.

Humid continental climate

Humid continental climate

A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot summers and cold winters. Precipitation is usually distributed throughout the year but often does have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid. The cooler Dfb, Dwb, and Dsb subtypes are also known as hemiboreal climates.

Churchill, Manitoba

Churchill, Manitoba

Churchill is a town in northern Manitoba, Canada, on the west shore of Hudson Bay, roughly 140 km (87 mi) from the Manitoba–Nunavut border. It is most famous for the many polar bears that move toward the shore from inland in the autumn, leading to the nickname "Polar Bear Capital of the World," and to the benefit of its burgeoning tourism industry.

59th parallel north

59th parallel north

The 59th parallel north is a circle of latitude that is 59 degrees north of the Earth's equatorial plane. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean.

58th parallel north

58th parallel north

The 58th parallel north is a circle of latitude that is 58 degrees north of the Earth's equatorial plane. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean.

Magadan

Magadan

Magadan is a port town and the administrative center of Magadan Oblast, Russia, located on the Sea of Okhotsk in Nagayev Bay and serving as a gateway to the Kolyma region.

Arkhangelsk

Arkhangelsk

Arkhangelsk, also known in English as Archangel and Archangelsk, is a city and the administrative center of Arkhangelsk Oblast, Russia. It lies on both banks of the Northern Dvina near its mouth into the White Sea. The city spreads for over 40 kilometres (25 mi) along the banks of the river and numerous islands of its delta. Arkhangelsk was the chief seaport of medieval and early modern Russia until 1703, when it was replaced by the newly-founded Saint Petersburg.

Geology

Hudson Bay occupies a large structural basin, known as the Hudson Bay basin, that lies within the Canadian Shield. The collection and interpretation of outcrop, seismic and drillhole data for exploration for oil and gas reservoirs within the Hudson Bay basin found that it is filled by, at most, 2,500 m (8,200 ft) of Ordovician to Devonian limestone, dolomites, evaporites, black shales, and various clastic sedimentary rocks that overlie less than 60 m (200 ft) of Cambrian strata that consist of unfossiliferous quartz sandstones and conglomerates, overlain by sandy and stromatolitic dolomites. In addition, a minor amount of terrestrial Cretaceous fluvial sands and gravels are preserved in the fill of a prominent ring-like depression about 325–650 km (202–404 mi) across created by the dissolution of Silurian evaporites during the Cretaceous Period.[48][49][50][51]

From the large quantity of published geologic data that has been collected as the result of hydrocarbon exploration, academic research, and related geologic mapping, a detailed history of the Hudson Bay basin has been reconstructed.[49] During the majority of the Cambrian Period, this basin did not exist. Rather, this part of the Canadian Shield area was still topographically high and emergent. It was only during the later part of the Cambrian that the rising sea level of the Sauk marine transgression slowly submerged it. During the Ordovician, this part of the Canadian Shield continued to be submerged by rising sea levels except for a brief middle Ordovician marine regression. Only starting in the Late Ordovician and continuing into the Silurian did the gradual regional subsidence of this part of the Canadian Shield form the Hudson Bay basin. The formation of this basin resulted in the accumulation of black bituminous oil shale and evaporite deposits within its centre, thick basin-margin limestone and dolomite, and the development of extensive reefs that ringed the basin margins that were tectonically uplifted as the basin subsided. During Middle Silurian times, subsidence ceased and this basin was uplifted. It generated an emergent arch, on which reefs grew, that divided the basin into eastern and western sub-basins. During the Devonian Period, this basin filled with terrestrial red beds that interfinger with marine limestone and dolomites. Before deposition was terminated by marine regression, Upper Devonian black bituminous shale accumulated in the south-east of the basin.[48][49][50][51]

The remaining history of the Hudson Bay basin is largely unknown as a major unconformity separates Upper Devonian strata from glacial deposits of the Pleistocene. Except for poorly known terrestrial Cretaceous fluvial sands and gravels that are preserved as the fills of a ring of subsided strata around the centre of this basin, strata representing this period of time are absent from the Hudson Bay basin and the surrounding Canadian Shield.[48][51]

The Precambrian Shield underlying Hudson Bay and in which Hudson Bay basin formed is composed of two Archean proto-continents, the Western Churchill and Superior cratons. These cratons are separated by a tectonic collage that forms a suture zone between these cratons and the Trans-Hudson Orogen. The Western Churchill and Superior cratons collided at about 1.9–1.8 Ga in the Trans-Hudson orogeny. Because of the irregular shapes of the colliding cratons, this collision trapped between them large fragments of juvenile crust, a sizable microcontinent, and island arc terranes, beneath what is now the centre of modern Hudson Bay as part of the Trans-Hudson Orogen. The Belcher Islands are the eroded surface of the Belcher Fold Belt, which formed as a result of the tectonic compression and folding of sediments that accumulated along the margin of the Superior Craton before its collision with the Western Churchill Craton.[52][53]

Map of post-glacial rebound. Hudson Bay is in the region of the most rapid uplift.
Map of post-glacial rebound. Hudson Bay is in the region of the most rapid uplift.

Hudson Bay and the associated structural basin lies within the centre of a large free-air gravity anomaly that lies within the Canadian Shield. The similarity in areal extent of the free-air gravity anomaly with the perimeter of the former Laurentide Ice Sheet that covered this part of Laurentia led to a long-held conclusion that this perturbation in the Earth's gravity reflected still ongoing glacial isostatic adjustment to the melting and disappearance of this ice sheet. Data collected over Canada by the Gravity Recovery and Climate Experiment (GRACE) satellite mission allowed geophysicists to isolate the gravity signal associated with glacial isostatic adjustment from longer–time scale process of mantle convection occurring beneath the Canadian Shield. Based upon this data, geophysicists and other Earth scientists concluded that the Laurentide Ice Sheet was composed of two large domes to the west and east of Hudson Bay. Modelling glacial isostatic adjustment using the GRACE data, they concluded that ≈25 to ≈45% of the observed free-air gravity anomaly was due to ongoing glacial isostatic adjustment, and the remainder likely represents longer time-scale effects of mantle convection.[54]

Southeastern semicircle

Earth scientists have disagreed about what created the semicircular feature known as the Nastapoka arc that forms a section of the shoreline of southeastern Hudson Bay. Noting the paucity of impact structures on Earth in relation to the Moon and Mars, Carlyle Smith Beals[55] proposed that it is possibly part of a Precambrian extraterrestrial impact structure that is comparable in size to the Mare Crisium on the Moon. In the same volume, John Tuzo Wilson[56] commented on Beals' interpretation and alternately proposed that the Nastapoka arc may have formed as part of an extensive Precambrian continental collisional orogen, linked to the closure of an ancient ocean basin. The current general consensus is that it is an arcuate boundary of tectonic origin between the Belcher Fold Belt and undeformed basement of the Superior Craton created during the Trans-Hudson orogeny. This is because no credible evidence for such an impact structure has been found by regional magnetic, Bouguer gravity, or other geologic studies.[52][53] However, other Earth scientists have proposed that the evidence of an Archean impact might have been masked by deformation accompanying the later formation of the Trans-Hudson orogen and regard an impact origin as a plausible possibility.[57][58]

Discover more about Geology related topics

Canadian Shield

Canadian Shield

The Canadian Shield, also called the Laurentian Plateau, is a geologic shield, a large area of exposed Precambrian igneous and high-grade metamorphic rocks. It forms the North American Craton, the ancient geologic core of the North American continent. Glaciation has left the area with only a thin layer of soil, through which exposures of igneous bedrock resulting from its long volcanic history are frequently visible. As a deep, common, joined bedrock region in eastern and central Canada, the Shield stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada and most of Greenland; it also extends south into the northern reaches of the United States.

Hydrocarbon exploration

Hydrocarbon exploration

Hydrocarbon exploration is the search by petroleum geologists and geophysicists for deposits of hydrocarbons, particularly petroleum and natural gas, in the Earth's crust using petroleum geology.

Ordovician

Ordovician

The Ordovician is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period 485.4 million years ago (Mya) to the start of the Silurian Period 443.8 Mya.

Limestone

Limestone

Limestone is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of CaCO3. Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life.

Evaporite

Evaporite

An evaporite is a water-soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution. There are two types of evaporite deposits: marine, which can also be described as ocean deposits, and non-marine, which are found in standing bodies of water such as lakes. Evaporites are considered sedimentary rocks and are formed by chemical sediments.

Clastic rock

Clastic rock

Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus, chunks, and smaller grains of rock broken off other rocks by physical weathering. Geologists use the term clastic to refer to sedimentary rocks and particles in sediment transport, whether in suspension or as bed load, and in sediment deposits.

Conglomerate (geology)

Conglomerate (geology)

Conglomerate is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay.

Cretaceous

Cretaceous

The Cretaceous is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin creta, "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation Kreide.

Fluvial processes

Fluvial processes

In geography and geology, fluvial processes are associated with rivers and streams and the deposits and landforms created by them. When the stream or rivers are associated with glaciers, ice sheets, or ice caps, the term glaciofluvial or fluvioglacial is used.

Geologic map

Geologic map

A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults, folds, are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features.

Cambrian

Cambrian

The Cambrian Period is the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period 485.4 mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of lagerstätte sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Cambrian biology surpasses that of some later periods.

Marine transgression

Marine transgression

A marine transgression is a geologic event during which sea level rises relative to the land and the shoreline moves toward higher ground, which results in flooding. Transgressions can be caused by the land sinking or by the ocean basins filling with water or decreasing in capacity. Transgressions and regressions may be caused by tectonic events such as orogenies, severe climate change such as ice ages or isostatic adjustments following removal of ice or sediment load.

Economy

The Arctic Bridge shipping route (blue line) is hoped to link North America to markets in Europe and Asia using ice-free routes across the Arctic Ocean
The Arctic Bridge shipping route (blue line) is hoped to link North America to markets in Europe and Asia using ice-free routes across the Arctic Ocean

Arctic Bridge

The longer periods of ice-free navigation and the reduction of Arctic Ocean ice coverage have led to Russian and Canadian interest in the potential for commercial trade routes across the Arctic and into Hudson Bay. The so-called Arctic Bridge would link Churchill, Manitoba, and the Russian port of Murmansk.[59]

Port

The biggest port in the Hudson bay is the city of Churchill, which lies on the river with the same name, Churchill River. The Port of Churchill is a privately owned port on Hudson Bay in Churchill, Manitoba, Canada. Routes from the port connect to the North Atlantic through the Hudson Strait. As of 2008, the port had four deep-sea berths capable of handling Panamax-size vessels for the loading and unloading of grain, bulk commodities, general cargo, and tanker vessels. The port is connected to the Hudson Bay Railway, which shares the same parent company, and cargo connections are made with the Canadian National Railway system at HBR's southern terminus in The Pas. It is the only port of its size and scope in Canada that does not connect directly to the country's road system; all goods shipped overland to and from the port must travel by rail.

The port was originally owned by the Government of Canada but was sold in 1997 to the American company OmniTRAX to run privately. In December 2015, OmniTRAX announced it was negotiating a sale of the port, and the associated Hudson Bay Railway, to a group of First Nations based in northern Manitoba.[60][61] With no sale finalized by July 2016, OmniTRAX shut down the port and the major railroad freight operations in August 2016.[62] The railway continued to carry cargo to supply the town of Churchill itself until the line was damaged by flooding on May 23, 2017. The Port and the Hudson Bay Railway were sold to Arctic Gateway Group—a consortium of First Nations, local governments, and corporate investors—in 2018.[63] On July 9, 2019, ships on missions to resupply arctic communities began stopping at the port for additional cargo,[64] and the port began shipping grain again on September 7, 2019.[65]

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Market (economics)

Market (economics)

In economics, a market is a composition of systems, institutions, procedures, social relations or infrastructures whereby parties engage in exchange. While parties may exchange goods and services by barter, most markets rely on sellers offering their goods or services to buyers in exchange for money. It can be said that a market is the process by which the prices of goods and services are established. Markets facilitate trade and enable the distribution and allocation of resources in a society. Markets allow any tradeable item to be evaluated and priced. A market emerges more or less spontaneously or may be constructed deliberately by human interaction in order to enable the exchange of rights of services and goods. Markets generally supplant gift economies and are often held in place through rules and customs, such as a booth fee, competitive pricing, and source of goods for sale.

Arctic Bridge

Arctic Bridge

The Arctic Bridge or Arctic Sea Bridge is a seasonal sea route approximately 6,700 kilometres long linking Russia to Canada, specifically the Russian port of Murmansk to the Hudson Bay port of Churchill, Manitoba.

Murmansk

Murmansk

Murmansk is a port city and the administrative center of Murmansk Oblast in the far northwest part of Russia. It sits on both slopes and banks of a modest ria or fjord, Kola Bay, an estuarine inlet of the Barents Sea. Its bulk is on the east bank of the inlet. It is in the north of the rounded Kola Peninsula which covers most of the oblast. The city is 108 kilometres (67 mi) from the border with Norway and 182 kilometres (113 mi) from the border with Finland.

Churchill, Manitoba

Churchill, Manitoba

Churchill is a town in northern Manitoba, Canada, on the west shore of Hudson Bay, roughly 140 km (87 mi) from the Manitoba–Nunavut border. It is most famous for the many polar bears that move toward the shore from inland in the autumn, leading to the nickname "Polar Bear Capital of the World," and to the benefit of its burgeoning tourism industry.

Hudson Strait

Hudson Strait

The Hudson Strait links the Atlantic Ocean and the Labrador Sea to Hudson Bay in Canada. This strait lies between Baffin Island and Nunavik, with its eastern entrance marked by Cape Chidley in Newfoundland and Labrador and Resolution Island off Baffin Island. The strait is about 750 km long with an average width of 125 km, varying from 70 km at the eastern entrance to 240 km at Deception Bay.

Panamax

Panamax

Panamax and New Panamax are terms for the size limits for ships travelling through the Panama Canal. The limits and requirements are published by the Panama Canal Authority (ACP) in a publication titled "Vessel Requirements". These requirements also describe topics like exceptional dry seasonal limits, propulsion, communications, and detailed ship design.

Hudson Bay Railway (1997)

Hudson Bay Railway (1997)

Hudson Bay Railway is a Canadian short line railway operating over 1,300 kilometres (810 mi) of track in northeastern Saskatchewan and northern Manitoba.

Canadian National Railway

Canadian National Railway

The Canadian National Railway Company is a Canadian Class I freight railway headquartered in Montreal, Quebec, which serves Canada and the Midwestern and Southern United States.

Government of Canada

Government of Canada

The government of Canada is the body responsible for the federal administration of Canada. A constitutional monarchy, the Crown assumes distinct roles: the executive, as the Crown-in-Council; the legislative, as the Crown-in-Parliament; and the judicial, as the Crown-on-the-Bench. Three institutions—the Privy Council, the Parliament, and the judiciary, respectively—exercise the powers of the Crown.

OmniTRAX

OmniTRAX

OmniTRAX, Inc. is a transportation and transportation infrastructure holding company based in Denver, Colorado, in the United States. It primarily owns or operates railroads, with a network of 25 regional and shortline railroads in 12 U.S. states and three Canadian provinces. It is one of the largest privately owned railroad companies in the United States. The firm also invests in, develops, and operates ports, multimodal transportation terminals, and industrial parks.

First Nations in Canada

First Nations in Canada

First Nations is a term used to identify Indigenous Canadian peoples 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.

Arctic Gateway Group

Arctic Gateway Group

Arctic Gateway Group LP is a limited partnership that owns and operates the Port of Churchill and the Hudson Bay Railway, which connects The Pas to Churchill, Manitoba. It was originally formed as a public-private partnership; with a fifty percent share held by Missinippi Rail, a consortium of northern Manitoba First Nations and local governments, and the private share split between Toronto-based Fairfax Financial Holdings and Regina-based grains company AGT Food and Ingredients. Fairfax and AGT transferred their shares of Arctic Gateway to OneNorth in March 2021, meaning that Arctic Gateway is completely owned by the local governments and Indigenous partners.

Coastal communities

The coast of Hudson Bay is extremely sparsely populated; there are only about a dozen communities. Some of these were founded as trading posts in the 17th and 18th centuries by the Hudson's Bay Company, making them some of the oldest settlements in Western Canada. With the closure of the HBC posts and stores, although many are now run by The North West Company,[66] in the second half of the 20th century, many coastal villages are now almost exclusively populated by Cree and Inuit. Two main historic sites along the coast were York Factory and Prince of Wales Fort.

Communities along the Hudson Bay coast or on islands in the bay are (all populations are as of 2016):

Military development

The Hudson's Bay Company built forts as fur trade strongholds against the French or other possible invaders. One example is York Factory with angled walls to help defend the fort. In the 1950s, during the Cold War, a few sites along the coast became part of the Mid-Canada Line, watching for a potential Soviet bomber attack over the North Pole. The only Arctic deep-water port in Canada is the Port of Churchill, located at Churchill, Manitoba.

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Cree

Cree

The Cree are a North American Indigenous people. They live primarily in Canada, where they form one of the country's largest First Nations.

Inuit

Inuit

Inuit are a group of culturally similar indigenous peoples inhabiting the Arctic and subarctic regions of Greenland, Labrador, Quebec, Nunavut, the Northwest Territories, and Alaska. Inuit languages are part of the Eskimo–Aleut languages, also known as Inuit-Yupik-Unangan, and also as Eskaleut. Inuit Sign Language is a critically endangered language isolate used in Nunavut.

Prince of Wales Fort

Prince of Wales Fort

The Prince of Wales Fort is a historic bastion fort on Hudson Bay across the Churchill River from Churchill, Manitoba, Canada.

Arviat

Arviat

Arviat is a predominantly Inuit hamlet located on the western shore of Hudson Bay in the Kivalliq Region of Nunavut, Canada. Arviat is derived from the Inuktitut word arviq meaning "Bowhead whale". Earlier in history, its name was Tikirajualaaq, and Ittaliurvik,.

Chesterfield Inlet, Nunavut

Chesterfield Inlet, Nunavut

Chesterfield Inlet is a hamlet located on the western shore of Hudson Bay, Kivalliq Region, in Nunavut, Canada, at the mouth of Chesterfield Inlet. Igluligaarjuk is the Inuktitut word for "place with few houses", it is the oldest community in Nunavut. The community is served by air, Chesterfield Inlet Airport, and by an annual supply known as sealift.

Coral Harbour

Coral Harbour

Coral Harbour, is a small Inuit community that is located on Southampton Island, Kivalliq Region, in the Canadian territory of Nunavut. Its name is derived from the fossilized coral that can be found around the waters of the community which is situated at the head of South Bay. The name of the settlement in Inuktitut is Salliq, sometimes used to refer to all of Southampton Island. The plural Salliit, means large flat island(s) in front of the mainland.

Churchill, Manitoba

Churchill, Manitoba

Churchill is a town in northern Manitoba, Canada, on the west shore of Hudson Bay, roughly 140 km (87 mi) from the Manitoba–Nunavut border. It is most famous for the many polar bears that move toward the shore from inland in the autumn, leading to the nickname "Polar Bear Capital of the World," and to the benefit of its burgeoning tourism industry.

Fort Severn First Nation

Fort Severn First Nation

Fort Severn First Nation is a Western Swampy Cree First Nation band government located on the Severn River near Hudson Bay. It is the most northern community in Ontario, Canada. In 2001, the population was 401, consisting of 90 families in an area of 40 square kilometres. The legal name of the reserve is Fort Severn 89, with the main settlement of Fort Severn.

Akulivik

Akulivik

Akulivik is an Inuit village in Nunavik, in northern Quebec, Canada. It is located on a peninsula that juts southwesterly into Hudson Bay across from Smith Island, Nunavut (Qikirtajuaq). Akulivik lies 1,850 km north of Montreal.

Inukjuak

Inukjuak

Inukjuak is a northern village located on Hudson Bay at the mouth of the Innuksuak River in Nunavik, in the Nord-du-Québec region of northern Quebec, Canada. Its population is 1,821 as of the 2021 Canadian Census. An older spelling is Inoucdjouac; its former name was Port Harrison.

Kuujjuarapik

Kuujjuarapik

Kuujjuarapik is the southernmost northern village at the mouth of the Great Whale River on the coast of Hudson Bay in Nunavik, Quebec, Canada. Almost 1000 people, mostly Cree, live in the adjacent village of Whapmagoostui. The community is only accessible by air, Kuujjuarapik Airport and, in late summer, by boat. The nearest Inuit village is Umiujaq, about 160 km (99 mi) north-northeast of Kuujjuarapik. The police services in Kuujjuaraapik are provided by the Nunavik Police Service, formerly the Kativik Regional Police Force. Like most other northern villages in Quebec, there is an Inuit reserved land of the same name, Kuujjuarapik. However, unlike most other Inuit reserved lands, the Inuit reserved land of Kuujjuarapik is not adjacent to its eponymous northern village; rather, it is located considerably farther north and in fact borders on the Inuit reserved land of Umiujaq.

Puvirnituq

Puvirnituq

Puvirnituq is a northern village in Nunavik, on the Povungnituk River near its mouth on Hudson Bay in northern Quebec, Canada. Its population was 2,129 as of the 2021 Canadian census.

Source: "Hudson Bay", Wikipedia, Wikimedia Foundation, (2023, March 21st), https://en.wikipedia.org/wiki/Hudson_Bay.

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See also
References
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General sources
  • Atlas of Canada, online version.
  • Some references of geological/impact structure interest include:
    • Rondot, Jehan (1994). "Recognition of eroded astroblemes". Earth-Science Reviews 35, 4, pp. 331–365.
    • Wilson, J. Tuzo (1968). "Comparison of the Hudson Bay arc with some other features". In: Science, History and Hudson Bay, v. 2. Beals, C. S. (editor), pp. 1015–1033.
External links

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