|Area||Ranked 7th among provinces|
|• Total||651,036 km2 (251,366 sq mi)|
|Coastline||0 km (0 mi)|
|Borders||Alberta, Manitoba, Northwest Territories, Montana and North Dakota|
|Highest point|| Cypress Hills |
1,468 metres (4,816 ft)
|Lowest point|| Lake Athabasca |
213 metres (699 ft)
|Longest river||Saskatchewan River|
|Largest lake|| Lake Athabasca |
The geography of Saskatchewan (suskăchuwun"), is unique among the provinces and territories of Canada in some respects. It is one of only two landlocked regions (Alberta is the other) and it is the only region whose borders are not based on natural features like lakes, rivers or drainage divides. The borders of Saskatchewan, which make it very nearly a trapezoid, were determined in 1905 when it became a Canadian province. Saskatchewan has a total area of 651,036 square kilometres (251,366 sq mi) of which 591,670 km2 (228,450 sq mi) is land and 59,366 km2 (22,921 sq mi) is water.
Geography is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of the Earth and planets. The first person to use the word γεωγραφία was Eratosthenes. Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be.
Saskatchewan is a prairie and boreal province in western Canada, the only province without a natural border. It has an area of 651,900 square kilometres (251,700 sq mi), nearly 10 percent of which is fresh water, composed mostly of rivers, reservoirs, and the province's 100,000 lakes.
The provinces and territories of Canada are sub-national governments within the geographical areas of Canada under the authority of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada —were united to form a federated colony, becoming a sovereign nation in the next century. Over its history, Canada's international borders have changed several times, and the country has grown from the original four provinces to the current ten provinces and three territories. Together, the provinces and territories make up the world's second-largest country by area.
The province's name comes from the Saskatchewan River, whose Cree name is: kisiskatchewani sipi, meaning "swift flowing river".
The Saskatchewan River is a major river in Canada, about 550 kilometres (340 mi) long, flowing roughly eastward across Saskatchewan and Manitoba to empty into Lake Winnipeg. Through its tributaries the North Saskatchewan and South Saskatchewan, its watershed encompasses much of the prairie regions of central Canada, stretching westward to the Rocky Mountains in Alberta and northwestern Montana in the United States. It reaches 1,939 kilometres (1,205 mi) to its farthest headwaters on the Bow River, a tributary of the South Saskatchewan in Alberta.
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 classified as 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.
Saskatchewan can be divided into three regions: grassland (part of the Great Plains) in the south, aspen parkland in the center, and forest in the north. The forest region lies partly on the northern part of the Great Plains and partly on the Canadian Shield. Its principal rivers are the Assiniboine River, and North and South Saskatchewan Rivers.
Grasslands are areas where the vegetation is dominated by grasses (Poaceae); however, sedge (Cyperaceae) and rush (Juncaceae) families can also be found along with variable proportions of legumes, like clover, and other herbs. Grasslands occur naturally on all continents except Antarctica. Grasslands are found in most ecoregions of the Earth. For example, there are five terrestrial ecoregion classifications (subdivisions) of the temperate grasslands, savannas, and shrublands biome (ecosystem), which is one of eight terrestrial ecozones of the Earth's surface.
The Great Plains is the broad expanse of flat land, much of it covered in prairie, steppe, and grassland, that lies west of the Mississippi River tallgrass prairie in the United States and east of the Rocky Mountains in the U.S. and Canada. It embraces:
Aspen parkland refers to a very large area of transitional biome between prairie and boreal forest in two sections, namely the Peace River Country of northwestern Alberta crossing the border into British Columbia, and a much larger area stretching from central Alberta, all across central Saskatchewan to south central Manitoba and continuing into small parts of the US states of Minnesota and North Dakota. Aspen parkland consists of groves of aspen poplars and spruce interspersed with areas of prairie grasslands, also intersected by large stream and river valleys lined with aspen-spruce forests and dense shrubbery. This is the largest boreal-grassland transition zone in the world and is a zone of constant competition and tension as prairie and woodlands struggle to overtake each other within the parkland.
Saskatchewan is bordered on the west by Alberta, on the north by the Northwest Territories, on the east by Manitoba, and on the south by the U.S. states of Montana and North Dakota.
Saskatchewan is a trapezoid. Its western border runs concurrent with the 4th meridian or the 110°W longitude, separating Saskatchewan from the province of Alberta. This border extends in length for 1,225 kilometres (761 mi) and was established in 1905 when both provinces were formed.
The meridian 110° west of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, North America, the Pacific Ocean, the Southern Ocean, and Antarctica to the South Pole.
Saskatchewan's eastern border includes minor measurement errors from the 1880s, so that it does not lie perfectly on the 102°W longitude, but rather it is slightly west of that meridian from 60°N parallel to 55°47'N, then slightly east of that until the Canada–United States border – an irregular line (rather than a straight one) for its 1,225-kilometre (761 mi) distance. When Saskatchewan was formed in 1905, Manitoba and the District of Keewatin were the neighboring areas to the east. Manitoba was enlarged in 1912 north to the 60th parallel, becoming Saskatchewan's only eastern neighbor. This remaining section of the border was determined by survey between 1961 and 1972.
The meridian 102° west of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, North America, the Pacific Ocean, the Southern Ocean, and Antarctica to the South Pole.
The 60th parallel north is a circle of latitude that is 60 degrees north of Earth's equator. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean.
The Canada–United States border, officially known as the International Boundary, is the longest international border in the world between two countries. It is shared between Canada and the United States, the second- and fourth/third largest countries by area, respectively. The terrestrial boundary is 8,891 kilometres (5,525 mi) long, of which 2,475 kilometres (1,538 mi) is Canada's border with Alaska. Eight Canadian provinces and territories, and thirteen U.S. states are located along the border.
Saskatchewan's southern border with the United States sits approximately on the 49th parallel, as agreed in the Treaty of 1818 —though minor measurement errors during the 1870s International Boundary Survey result in some variance between the actual Canada–United States border and the 49th parallel. This boundary was not formally established until the 1867 survey. This border extends 627 kilometres (390 mi) across southern Saskatchewan.
The 49th parallel north is a circle of latitude that is 49° north of Earth's equator. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean.
The Convention respecting fisheries, boundary and the restoration of slaves between the United States of America and the United Kingdom of Great Britain and Ireland, also known as the London Convention, Anglo-American Convention of 1818, Convention of 1818, or simply the Treaty of 1818, was an international treaty signed in 1818 between the above parties. Signed during the presidency of James Monroe, it resolved standing boundary issues between the two nations. The treaty allowed for joint occupation and settlement of the Oregon Country, known to the British and in Canadian history as the Columbia District of the Hudson's Bay Company, and including the southern portion of its sister district New Caledonia.
The Northwest Territories is north of the 60th parallel which forms the northern border of the province. 445 kilometres (277 mi) across northern Saskatchewan. The aforementioned measurement errors in the 1880s surveys place the Saskatchewan/Manitoba border approximately 400 metres (440 yd) west of the 102nd meridian and the accurately measured Northwest Territories/Nunavut border, just missing a true quadripoint of the Saskatchewan/Manitoba/Northwest Territories/Nunavut borders.This border extends
The geology of Saskatchewan can be divided into two main geological regions, the Pre-Cambrian or Canadian shield and the Phanerozoic or Western Canada Sedimentary Basin. Within the Canadian shield exists the Athabasca sedimentary basin. Meteorite impacts have altered the natural geological formation processes. The Quaternary period is the most recent geological process when the prairies were affected by glacial events. 35 kilometres (22 mi) in diameter.There are six notable meteorite or comet impact craters in Saskatchewan. Carswell, Deep Bay and Gow Lake have affected the Canadian Shield area of the north. In the southern Phanerozoic crater are the Viewfield, Elbow and Maple Creek structures. The Carswell structure is largest astrobleme at
Archaeologists have dated the first human settlements to 9,500 BCE. The four groups inhabiting the area at the time of the first European contact were the Cree, Assiniboine, Salteaux and Dene.Henry Kelsey of the Hudson's Bay Company is considered the first European person to see this area. The earliest trading posts were made by the French; however, the first permanent settlement was established at Cumberland House in 1774 by the HBC. In addition, several more ports were set up by British fur traders among the area's waterways. The forested area of the Canadian Shield was the favoured area for early settlement, and the economy was heavily dependent on hunting and trapping.
In 1870, the Hudson's Bay Company sold Rupert's Land and ceded its rights to the Canadian Government. [ citation needed ] Additional native peoples and Métis (people of mixed French and indigenous Canadian ancestry), led by Louis Riel, rebelled between 1884 and 1885 and were suppressed.The region became a part of the Northwest Territories. The majority of the Canadians of indigenous descent in the Northwest Territories sold their lands to the government in the 1870s and were settled on reservations.
The arrival of settlements and the rail lines also brought agricultural economies and development in the Central Lowlands Area. The Great Plains or Palliser Triangle area to the south was mainly used for ranching economies. In the beginning of the 20th century, Saskatchewan farmers created cooperative organizations to maintain grain marketization. During the drought and depression of the 1930s, the population decreased as immigration nearly ended and numerous families left. During World War II, conservation programs and the increased demand for grain revived the economy.
Being in the centre of North America, Saskatchewan is far removed from the moderating effects of any large body of water and therefore has a temperate continental climate, Köppen climate classification types BSk, Dfb and Dfc. Hot to warm summers and cold winters mean that the annual temperature range can be up to 65 °C. On average, Saskatchewan has 211 days per year when the temperature drops below freezing. Plough winds, Supercell hail or high precipitation rain storms and tornadoes are eventful summer occurrences. Midale reached 45 °C (113 °F) on July 5, 1937, the highest recorded temperature in Canada.
Compared to average values from all thirteen Canadian provinces and territories, 145 centimetres (57 in)), the fourth-lowest total precipitation (428 millimetres (16.9 in)) and the second-hottest summer (22.5 °C (72.5 °F)). The number of frost-free days ranges from 95 days in the north (Prince Albert, for example) to as high as 124 days in the south (Estevan).Saskatchewan is the sunniest province or territory year round (2206 hours per year), has the second-lowest annual snowfall (
Saskatchewan's capital is Regina. Its most populous city is Saskatoon. Other major cities include Estevan, Flin Flon (part), Humboldt, Lloydminster (part), Melfort, Melville, Moose Jaw, North Battleford, Prince Albert, Swift Current, Weyburn, and Yorkton.
The native flora of the Saskatchewan includes vascular plants, plus additional species of other plants and plant-like organisms such as algae, lichens and other fungi, and mosses.Non-native species of plants are recorded as established outside of cultivation in Saskatchewan, of these some non-native species remain beneficial for gardening, and agriculture, where others have become invasive, noxious weeds. Saskatchewan is committed to protecting species at risk in Canada. The growing season has been studied and classified into plant hardiness zones depending on length of growing season and climatic conditions. Biogeographic factors have also been divided into ecoregions and floristic kingdoms across Saskatchewan, and natural vegetation varies depending on elevation, moisture, soil and weather. The study of ethnobotany uncovers the interrelation between humans and plants and the various ways people have used plants for economic reasons, food, medicine and technological developments.
The Government of Saskatchewan has declared 3 indigenous plants as provincial symbols.
The fauna of Saskatchewan include many land and aquatic species. From the multiplicity of invertebrates and vertebrates two have been chosen as symbols of Saskatchewan, the white-tailed deer and the sharp-tailed grouse.Cenozoic vertebrate fossils reveal the geological evolution of the interior plains and its prehistoric biogeography. Today, Saskatchewan's ecosystems range from the sub-arctic tundra of the Canadian Shield in north Saskatchewan to aspen parkland, and grassland prairie. Fauna inhabit areas unique to their own specific and varied breeding, foraging and nesting requirements. With a large land and water area, and small population density, the ecoregions of Saskatchewan provide important habitat for many animals, both endangered and not.
Naturalists observing wildlife have enumerated shrinking and growing wildlife populations. They advocate programs and methods to preserve or re-introduce endangered species and identify programs of control for outbreaks of wildlife populations.
A broad diversity of wildlife habitats are preserved as parks and reserves protecting the feeding and breeding grounds of protected and indigenous fauna of Saskatchewan.
The total area of freshwater is 59,366 km2. There are two main river basins, the Nelson and Churchill River Basins, both of which drain into Hudson Bay.
Qu'Appelle and Souris, the North and South Saskatchewan, confluence is east of Prince Albert becoming the Saskatchewan which are all a part of the Nelson river basin. The Churchill River connects lakes and streams through the lower portion of the Canadian shield.Rupert's Land a historical political division of Canada comprised all lands of the Hudson Bay drainage system between the years 1670 to 1870.
Frenchman River does not flow east to Hudson Bay, but rather south to the Missouri River, which is part of the Missouri river basin catchment area. The Mackenzie River basin of north Saskatchewan flows north draining into the Arctic Ocean, which belongs to the Mackenzie river basin drainage area.
There are over 10 thousand lakes across Saskatchewan, the main lake region being north of the tree line in the Canadian Shield.
Saskatchewan's largest lake is Lake Athabasca which sits astride the Saskatchewan – Alberta border. The second in size is Reindeer Lake which is located on the Saskatchewan – Manitoba border. Other lakes of notable size would be Wollaston, Cree, Frobisher, and Lac La Ronge. 220 metres (720 ft) is located in Reindeer Lake at the Deep Bay Structure site which was created by a meteor impact.The deepest water point
Saskatchewan is also home to preserved wetlands which are partially submerged areas of land.
Saskatchewan's waterways also contain bogs, as well as the salt water lakes. Quill Lake is Canada's largest saltwater lake, Chaplin Lake is a Western Hemispheric Shorebird Reserve Network and Little Manitou, an ehdorheic lake, is a popular tourist resort. Brine shrimp siheries have existed on sodium magnesium sulphate lakes such as Chaplin, Frederick, Ingebright, and Little Manitou lakes.
Saskatchewan has 34 provincial parks that provide for recreational use or preserve wilderness, special environments or sites of historic importance.
The province is also home to two of Canada's 36 National Parks. Grasslands National Park, which covers 907 square kilometres (350 sq mi) in southernmost part of the province, was established in 1981. The other is Prince Albert National Park covering 3,874 square kilometres (1,496 sq mi) in central Saskatchewan, which was established in 1927.
The economy of Saskatchewan has been associated with agriculture resulting in the moniker Bread Basket of Canadaand Bread Basket of the World. According to the Government of Saskatchewan, approximately 95% of all items produced in Saskatchewan, depend on the basic resources available within the province. Various grains, livestock, oil and gas, potash, uranium, wood and their spin off industries fuel the economy.
Saskatchewan's GDP in 2006 was approximately C$45.922 billion.
The geography of Canada describes the geographic features of Canada, the world's second largest country in total area.
The Canadian Shield, also called the Laurentian Plateau, or Bouclier canadien (French), is a large area of exposed Precambrian igneous and high-grade metamorphic rocks that forms the ancient geological core of the North American continent. Composed of igneous rock resulting from its long volcanic history, the area is covered by a thin layer of soil. With a deep, common, joined bedrock region in eastern and central Canada, it stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada; it also extends south into the northern reaches of the United States. Human population is sparse, and industrial development is minimal, while mining is prevalent.
Alberta is a Canadian province. Located in Western Canada, the province has an area of 661,190 square kilometres (255,290 sq mi) and is bounded to the south by the U.S. state of Montana along 49° north for 298 kilometres (185 mi); to the east at 110° west by the province of Saskatchewan for 1,223 kilometres (760 mi); and at 60° north the Northwest Territories for 644 kilometres (400 mi). The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west.
The Canadian Prairies is a region in Western Canada. It includes the Canadian portion of the Great Plains and the Prairie Provinces, namely Alberta, Saskatchewan, and Manitoba. These provinces are partially covered by grasslands, plains, and lowlands, mostly in the southern regions. The northernmost reaches of the Canadian Prairies are less well known. They are marked by forests and more variable topology. If the region is defined to include areas only covered by prairie land, the corresponding region is known as the Interior Plains. Geographically, the Canadian prairies extend to northeastern British Columbia, but this province is not included in a political manner.
The Churchill River is a major river in Alberta, Saskatchewan and Manitoba, Canada. From the head of the Churchill Lake it is 1,609 kilometres (1,000 mi) long. It was named after John Churchill, 1st Duke of Marlborough and governor of the Hudson's Bay Company from 1685 to 1691.
Meadow Lake is a city in the boreal forest of northwestern Saskatchewan, Canada. Its location is about 246 kilometres (153 mi) northeast of Lloydminster and 156 kilometres (97 mi) north of North Battleford. On November 9, 2009, it officially became Saskatchewan's 14th city.
Eastend is a town in southwest Saskatchewan, Canada. It is situated approximately 55 kilometres (34 mi) north from the Montana border and 85 kilometres (53 mi) from the Alberta border.
The North Saskatchewan River is a glacier-fed river that flows from the Canadian Rockies continental divide east to central Saskatchewan, where it joins with another major river to make up the Saskatchewan River. Its water flows eventually into the Hudson Bay.
Whitewood is a town in the Canadian province of Saskatchewan. It is located approximately 175 kilometres (109 mi) east of Regina on the Trans-Canada Highway Sk Hwy 1. It is situated at the crossroads of two major highways systems – the Trans-Canada, which runs east and west, and Sk Hwy 9, which runs north and south from the US border to Hudson Bay, Saskatchewan. Located midway between Brandon, Manitoba and Regina, Whitewood was and continues to be an ideal place to stop and rest.
Highway 2 is a provincial highway in the Canadian province of Saskatchewan. It is the longest Saskatchewan Highway, at 809 km (503 mi). The highway is partially divided and undivided. However, only about 18 kilometres (11 mi) near Moose Jaw, 11 kilometres (7 mi) near Chamberlain, and 21 kilometres (13 mi) near Prince Albert are divided highway. Highway 2 is a major north-south route, beginning at the Canada–US border at the Port of West Poplar River, and Opheim, Montana customs checkpoints. Montana Highway 24 continues south. The town of La Ronge delimits the northern terminus with Highway 102 continuing north. It passes through the major cities of Moose Jaw in the south and Prince Albert in the north. Highway 2 overlaps Highway 11 between the towns of Chamberlain and Findlater. This 11 kilometres (7 mi) section of road is a wrong-way concurrency. The highway ends at La Ronge, where it becomes Highway 102.
Highway 6 is a paved undivided major provincial highway in the Canadian province of Saskatchewan. It runs from Montana Highway 16 at the Canada–US border near the Canada customs port of Regway to Highway 55 near Choiceland. Highway 6 is about 523 km (325 mi) long. The CanAm Highway comprises Saskatchewan Highways from south to north: SK 35, Sk 39, Sk 6, Sk 3, as well as Sk 2. 330 kilometres (210 mi) of Saskatchewan Highway 6 contribute to the CanAm Highway between Corinne and Melfort.
Highway 3 is a major provincial paved undivided highway in the Canadian province of Saskatchewan. It runs from the Alberta border, where it continues west as Alberta Highway 45, to the Manitoba border, and then continues east as Highway 77. Highway 3 is about 615 km (382 mi.) long. The CanAm Highway comprises Saskatchewan Highways 35, 39, 6, 2, as well as 2. 59.7 miles (96.1 km) of Saskatchewan Highway 3 contribute to the CanAm Highway between Melfort and Prince Albert.
Volcanology of Canada includes lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes, calderas, diatremes, and maars, along with examples of more less common volcanic forms such as tuyas and subglacial mounds. It has a very complex volcanological history spanning from the Precambrian eon at least 3.11 billion years ago when this part of the North American continent began to form.
The economy of Saskatchewan has been associated with agriculture resulting in the moniker "Bread Basket of Canada" and Bread Basket of the World. According to the Government of Saskatchewan, approximately 95% of all items produced in Saskatchewan, depend on the basic resources available within the province. Various grains, livestock, oil and gas, potash, uranium, wood and their spin off industries fuel the economy.
The geology of Saskatchewan can be divided into two main geological regions, the Precambrian Canadian Shield and the Phanerozoic Western Canadian Sedimentary Basin. Within the Precambrian shield exists the Athabasca sedimentary basin. Meteorite impacts have altered the natural geological formation processes. The prairies were most recently affected by glacial events in the Quaternary period.
The native flora of Saskatchewan includes vascular plants, plus additional species of other plants and plant-like organisms such as algae, lichens and other fungi, and mosses. Non-native species of plants are recorded as established outside of cultivation in Saskatchewan, of these some non-native species remain beneficial for gardening, and agriculture, where others have become invasive, noxious weeds. Saskatchewan is committed to protecting species at risk in Canada. The growing season has been studied and classified into plant hardiness zones depending on length of growing season and climatic conditions. Biogeographic factors have also been divided into vegetative zones, floristic kingdoms, hardiness zones and ecoregions across Saskatchewan, and natural vegetation varies depending on elevation, moisture, soil type landforms, and weather. The study of ethnobotany uncovers the interrelation between humans and plants and the various ways people have used plants for economic reasons, food, medicine and technological developments. The Government of Saskatchewan has declared 3 indigenous plants as provincial symbols.
The Fauna of Saskatchewan include several diverse land and aquatic animal species. From the multiplicity of invertebrates and vertebrates, two have been chosen as symbols of Saskatchewan. Cenozoic vertebrate fossils reveal the geological evolution of the interior plains and its prehistoric biogeography. Today, Saskatchewan's ecosystems range from the sub-arctic tundra of the Canadian Shield in north Saskatchewan to aspen parkland, the Mid-Continental Canadian forests in the centre of the province and grassland prairie. Fauna inhabit areas unique to their own specific and varied breeding, foraging and nesting requirements. With a large land and water area, and small population density, the ecoregions of Saskatchewan provide important habitat for many animals, both endangered and not. Naturalists observing wildlife have enumerated shrinking and growing wildlife populations. They advocate programs and methods to preserve or re-introduce endangered species and identify programs of control for outbreaks of wildlife populations. A broad diversity of wildlife habitats are preserved as parks and reserves protecting the feeding and breeding grounds of protected and indigenous fauna of Saskatchewan.