Winnipeg lies at the bottom of the Red River Valley, a low-lying flood plain with an extremely flat topography. [1] This valley was formed by the ancient glacial Lake Agassiz which has rich deposits of black soil. Winnipeg is on the eastern edge of the Canadian Prairies in Western Canada; it is known as the 'Gateway to the West'. It is relatively close to many large Canadian Shield lakes and parks, as well as Lake Winnipeg (the Earth's twelfth largest freshwater lake). [2] Winnipeg is bordered by tallgrass prairie to the west and south and the aspen parkland to the northeast.
Winnipeg is fairly isolated in that the closest city with equal or greater population is Minneapolis–Saint Paul, Minnesota (metro population of 3,317,308), which is 733 km (455 mi) southeast from the city.[ citation needed ] According to the Census geographic units of Canada, the city has a total area of 464.01 km2 (179.16 sq mi) and an elevation of 240 m (790 ft). [3]
The city has a humid continental climate with wide temperature contrasts between winter and summer, and greater precipitation in summer. Mean January temperature is −16.4 °C (2.5 °F), and mean July temperature is 19.7 °C (67.5 °F). Average annual precipitation is 521.1 mm (20.52 in); snow falls on 53 days and lies on 132 days in an average year.
Winnipeg has three major rivers: the Red River, the Assiniboine River, and the Seine River. The Red River is a Canadian heritage river. [4] Because of Winnipeg's extremely flat topography and substantial snowfall, Winnipeg is subject to severe flooding. The Red River reached its greatest flood height in 1826. The Red River Floodway protects the city from flooding.
According to the 2001 Census, there are 230 neighbourhoods in Winnipeg. [5] Downtown Winnipeg, the city's economic core, is centred on the intersection of Portage Avenue and Main Street (reputed to be one of the windiest in Canada). [6] Downtown Winnipeg covers an area of about one square mile (2.5 km2) and is the fastest growing high-income neighbourhood in the city.[ citation needed ] More than 72,000 people work downtown, and over 40,000 students attend classes at its universities and colleges.[ citation needed ] The past few decades have seen downtown undergo major revitalization efforts; since 1999, over Can$1.2 billion has been invested.[ citation needed ]
In Winnipeg, there are 10 buildings that stand taller than 85 m (279 ft). The tallest building in the city is the newer 33-storey, 128 m (420 ft) 201 Portage. [7] The second tallest building in the city is the Richardson Building, standing at 124 m (407 ft) tall with 34 storeys. [8]
Downtown Winnipeg's Exchange District is named after the area's original grain exchange from 1880 to 1913. [9] The 30-block district received National Historic Site of Canada status in 1997; it includes North America's most extensive collection of early 20th-century terracotta and cut stone architecture, 62 of downtown Winnipeg's 86 heritage structures, [9] Stephen Juba Park, and Old Market Square, home to Winnipeg Jazz and Fringe Festivals. [9] Other major downtown areas include The Forks, Central Park, Broadway-Assiniboine and Chinatown. Many of Downtown Winnipeg's major buildings are linked with the Winnipeg Walkway skywalk. [10]
Various residential neighbourhoods surround downtown in all directions, but expansion is greatest to the south and west, and has tended to follow the course of the two major rivers. The urbanized area in Winnipeg is about 25 km (16 mi) from east to west and 20 km (12 mi) from north to south, although several areas remain underdeveloped. The largest park in the city, Assiniboine Park next to the affluent neighbourhood of Tuxedo, houses the Assiniboine Park Zoo and the Leo Mol Sculpture Garden, Other large city parks include Kildonan Park, St. Vital Park, and Fort Whyte Centre. The major commercial areas in the city are Polo Park (West End and St. James), Kildonan Crossing (Transcona and East Kildonan), South St. Vital, Garden City (West Kildonan) and the Corydon strip.
Osborne Village is Winnipeg's most densely populated neighbourhood, [11] as well as the second most densely populated neighbourhood in Western Canada. [12] It was voted the Best Place to Live in Uptown Magazine's 2008 Best of List. [13] Osborne Village is a complex urban community with a rich heritage and diverse built forms. It's appreciated as a desirable location in which to live, work, and play. As such, it continues to experience development interest. Popular annual events include the Canada Day Festival. Osborne Village is home to one of Winnipeg's most vibrant collection of stores and restaurants with over 175 businesses calling Osborne Village home.
Little Italy is a vibrant Italian district. Located on Corydon Avenue, between Stafford Street in the west, and Pembina Highway in the east it is home to many boutiques and some of the city's finest restaurants and Gelato.[ citation needed ]
Saint Boniface is the centre of much of the Franco-Manitoban community. It features such landmarks as the Cathédrale de Saint Boniface (St. Boniface Cathedral), Boulevard Provencher, the Provencher Bridge, Esplanade Riel, St. Boniface Hospital, the Collège universitaire de Saint-Boniface and the Royal Canadian Mint. It covers the southeast part of the city and has a population of 65,000.
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The city uses the grid plan but there are several different grids in place, as the city was originally thirteen separate municipalities and each developed under different circumstances and under different rules. Although it is common for roadways running north–south to be called "streets" and those running east–west to be called "avenues", the practice is far from universal, and few roadways run in a precise cardinal direction; an "east-west" road may run at a 45-degree angle from true east–west. Attempts in the early 20th century to bring order to the system by giving numerical names to the streets failed; all roadways in the city have proper names, some of which are repeated. (There is, for instance, a Wellington Crescent in River Heights and a Wellington Avenue in the West End, and a Killarney Avenue in Fort Garry and a Killarney Street in St. Vital.)
There is also no universal address numbering system in place. Address numbers usually increase as the distance from either the Red or Assiniboine rivers increases, but this is by no means uniform, even within a specific district. These peculiarities can cause serious problems for newcomers and visitors, especially in the older areas of the city, and may even affect postal and other deliveries.
Many of the main thoroughfares in Winnipeg are wide due to the spring soil conditions and the historical use of the Red River ox cart which created wide ruts in the (then) muddy roads. Portage Avenue has four lanes of traffic in each direction plus a central boulevard for much of its run through Winnipeg. Few thoroughfares, however, are as wide as the freeways seen in other Canadian cities (such as the 401 in Toronto or Deerfoot Trail in Calgary). Residential streets are commonly significantly narrower than streets in other Western Canadian cities, so narrow that parking is only possible on one side of the street.
Winnipeg lies in the middle of the North American continent on a low-lying, flat plain. Due to its location in the Canadian Prairies, and its distance from both mountains and oceans, it has an extreme humid continental climate (Köppen Dfb, [14] Plant Hardiness Zone 3b-4a [15] [16] [17] ), in that there are great differences between summer and winter temperatures. The openness of the prairies leaves Winnipeg exposed to numerous weather systems including blizzards and cold Arctic high pressure systems, known as the polar high. Winnipeg has four distinct seasons, with short transitional periods between winter and summer.
The city averages 521.1 mm (20.52 in) of precipitation per year, although this can vary greatly from year to year. [18]
Climate data for Winnipeg (Winnipeg James Armstrong Richardson International Airport) WMO ID: 71852; coordinates 49°55′N97°14′W / 49.917°N 97.233°W ; elevation: 238.7 m (783 ft); 1991–2020 normals, extremes 1872–present [a] | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high humidex | 6.3 | 11.1 | 28.0 | 34.1 | 40.2 | 46.1 | 47.3 | 45.5 | 45.9 | 34.3 | 23.9 | 9.3 | 47.3 |
Record high °C (°F) | 7.8 (46.0) | 11.7 (53.1) | 23.7 (74.7) | 34.3 (93.7) | 37.8 (100.0) | 38.3 (100.9) | 42.2 (108.0) | 40.6 (105.1) | 38.8 (101.8) | 31.1 (88.0) | 23.9 (75.0) | 11.7 (53.1) | 42.2 (108.0) |
Mean daily maximum °C (°F) | −11.4 (11.5) | −8.8 (16.2) | −0.9 (30.4) | 10.0 (50.0) | 18.1 (64.6) | 23.3 (73.9) | 25.8 (78.4) | 25.4 (77.7) | 19.6 (67.3) | 10.4 (50.7) | 0.1 (32.2) | −8.2 (17.2) | 8.6 (47.5) |
Daily mean °C (°F) | −16.3 (2.7) | −14.1 (6.6) | −6.1 (21.0) | 3.8 (38.8) | 11.1 (52.0) | 17.1 (62.8) | 19.5 (67.1) | 18.7 (65.7) | 13.3 (55.9) | 5.1 (41.2) | −4.4 (24.1) | −12.7 (9.1) | 2.9 (37.2) |
Mean daily minimum °C (°F) | −21.2 (−6.2) | −19.3 (−2.7) | −11.2 (11.8) | −2.5 (27.5) | 4.2 (39.6) | 10.9 (51.6) | 13.2 (55.8) | 11.9 (53.4) | 6.9 (44.4) | −0.2 (31.6) | −8.8 (16.2) | −17.3 (0.9) | −2.8 (27.0) |
Record low °C (°F) | −44.4 (−47.9) | −45.0 (−49.0) | −38.9 (−38.0) | −27.8 (−18.0) | −11.7 (10.9) | −6.1 (21.0) | 1.1 (34.0) | −1.1 (30.0) | −8.3 (17.1) | −20.6 (−5.1) | −36.7 (−34.1) | −47.8 (−54.0) | −47.8 (−54.0) |
Record low wind chill | −56.4 | −57.1 | −49.4 | −35.8 | −20.8 | −7.9 | 0.0 | 0.0 | −11.5 | −24.2 | −48.1 | −50.6 | −57.1 |
Average precipitation mm (inches) | 18.0 (0.71) | 13.3 (0.52) | 25.5 (1.00) | 32.5 (1.28) | 69.5 (2.74) | 74.3 (2.93) | 76.6 (3.02) | 74.3 (2.93) | 53.2 (2.09) | 38.1 (1.50) | 24.7 (0.97) | 19.4 (0.76) | 519.2 (20.44) |
Average rainfall mm (inches) | 0.2 (0.01) | 3.8 (0.15) | 8.8 (0.35) | 19.9 (0.78) | 66.2 (2.61) | 79.3 (3.12) | 89.0 (3.50) | 80.9 (3.19) | 46.6 (1.83) | 33.8 (1.33) | 7.2 (0.28) | 0.5 (0.02) | 436.1 (17.17) |
Average snowfall cm (inches) | 25.0 (9.8) | 11.8 (4.6) | 19.2 (7.6) | 13.6 (5.4) | 4.1 (1.6) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 0.0 (0.0) | 4.2 (1.7) | 21.1 (8.3) | 27.2 (10.7) | 126.2 (49.7) |
Average precipitation days (≥ 0.2 mm) | 11.9 | 8.8 | 9.1 | 8.4 | 12.9 | 13.4 | 11.9 | 11.3 | 10.7 | 9.8 | 9.9 | 11.6 | 129.8 |
Average rainy days (≥ 0.2 mm) | 0.47 | 1.0 | 2.6 | 5.3 | 12.9 | 13.1 | 11.9 | 11.3 | 10.5 | 7.2 | 2.9 | 0.75 | 79.9 |
Average snowy days (≥ 0.2 cm) | 12.2 | 7.8 | 7.6 | 3.2 | 0.82 | 0.0 | 0.0 | 0.0 | 0.0 | 2.1 | 8.7 | 11.6 | 53.9 |
Average relative humidity (%) (at 1500 LST) | 72.7 | 71.0 | 67.9 | 49.1 | 47.8 | 54.6 | 55.7 | 52.3 | 54.7 | 61.0 | 72.6 | 76.5 | 61.3 |
Mean monthly sunshine hours | 114.7 | 133.9 | 181.9 | 241.4 | 285.2 | 276.3 | 308.3 | 281.4 | 189.0 | 147.4 | 93.9 | 99.5 | 2,352.9 |
Percent possible sunshine | 42.9 | 47.2 | 49.5 | 58.6 | 59.8 | 56.6 | 62.6 | 62.8 | 49.8 | 44.1 | 34.4 | 39.2 | 50.6 |
Source: Environment and Climate Change Canada (sun 1981–2010) [19] [20] [21] [22] |
Climate data is also available for downtown Winnipeg, with a weather station located at The Forks. This data demonstrates the urban heat island effect cities have on moderating temperatures compared to airport weather stations.
Climate data for Winnipeg (The Forks) WMO ID: 71579; coordinates 49°53′18″N97°07′46″W / 49.88833°N 97.12944°W ; elevation: 230.0 m (754.6 ft); 1999-2020 | |||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Mean daily maximum °C (°F) | −10 (14) | −8.5 (16.7) | 0.1 (32.2) | 10.3 (50.5) | 17.7 (63.9) | 23.4 (74.1) | 26.7 (80.1) | 25.4 (77.7) | 19.9 (67.8) | 10.5 (50.9) | 1.1 (34.0) | −7.5 (18.5) | 9.1 (48.4) |
Mean daily minimum °C (°F) | −17.9 (−0.2) | −17.2 (1.0) | −9.1 (15.6) | −0.3 (31.5) | 6.7 (44.1) | 13.2 (55.8) | 16.5 (61.7) | 14.9 (58.8) | 9.7 (49.5) | 2.4 (36.3) | −6 (21) | −14.7 (5.5) | −0.1 (31.7) |
Source: Environment and Climate Change Canada [23] |
Typical winter phenomena include the bonspiel (January) thaw, ice fog, and the aurora borealis. The city is virtually assured of having a white Christmas as there is only one 25 December on record in the last century where there was no snow on the ground. Out of Canada's 100 largest cities, Winnipeg's winter is the tenth coldest with an average low of −20.2 °C (−4.4 °F). [24] From December through February the maximum daily temperature exceeds 0 °C (32 °F), on average, for only 10 days and the minimum daily temperature falls below −20 °C (−4 °F) on 49 days.
Summers are typically warm and generally not overly humid, with average humidity levels around 50% from June to August. Occasionally, humidex readings exceed 40. The trees will usually be in full bloom by late May and do not lose their leaves until early October. Winnipeg's growing season lasts from 25 May to 22 September; [25] and temperatures frequently hover in the mid to high twenties Celsius (77F to 86F). The city frequently gets thunderstorms during the summer, averaging 27 per season. [26] The city can occasionally have short blasts of hot weather like on 23 August 2011 the temperature reached 37.2 °C (99.0 °F). [27] The temperature reaches at or above 30 °C (86 °F) 14 times a year, which is ranked the 16th highest in Canada, just above Toronto, Ontario. [28] The highest temperature ever recorded in Winnipeg (since commencement of record-keeping in 1873) was 42.2 °C (108.0 °F) on 11 July 1936; [29] and the hottest temperature recorded in the past 50 years was 38.7 °C (101.7 °F) on 6 August 1988 and again on 1 August 1989. The highest humidex reading was 48 on 25 July 2007. [30]
The weather during these seasons is highly variable, and rapidly changing. For example, temperatures in Winnipeg in April have ranged from −6.3 to 34.3 °C (20.7 to 93.7 °F), and in October from −6 to 30.5 °C (21.2 to 86.9 °F). The city often receives an Indian summer, when summer weather returns briefly after the first frosts, usually in late September or sometimes October. Some Septembers can have gorgeous weather, like in September 2009 Winnipeg only saw 4 days with daytime highs below 20 °C (68 °F) at the Forks weather station. [31]
Winnipeg is one of Canada's sunniest cities, and the weather in all seasons is characterized by an abundance of sunshine. In July and August combined, Winnipeg has 60 out of 62 days with measurable sunshine; and has an annual average of 306 days a year with measurable sunshine. [32] November is the least sunny month while July and August are the most sunny months. [32] Winnipeg is ranked second for Canada's clearest skies year-round, sixth sunniest city year-round, and second for sunniest city in Canada in spring and winter. [18] Winnipeg is sunnier in the summer, spring, and winter than any Canadian city east of it. [33] Winnipeg has short daylight hours in the winter and long daylight hours in the summer. On the shortest day of the year (21 December) Winnipeg only has 8 hours and 5 minutes of daylight with the sun setting at 4:29pm and doesn't rise until 8:24am. [34] On 21 June (the longest day of the year) Winnipeg has 16 hours and 21 minutes of daylight with twilight ending at 10:25pm and twilight starting at 4:35am. [34]
Winnipeg has moderate precipitation with 513.7 mm (20.22 in) of precip per year. [18] There is measurable rainfall on 76.9 days throughout the year, and 54.7 days with snowfall. [18] Most of the precipitation occurs in the warmer months, with June being the wettest month and February being the driest. Droughts can take place in the region, however they do not happen as frequently as cities further west like Calgary or Swift Current. During the winter Winnipeg will get precipitation mostly in the form of snow, with 36 days of snow falling from December to February. Even in the winter there is occasional rainfall with 2.5 days on average of rainfall during December to February. [32] Other forms of winter precipitation include ice, sleet, and freezing rain. Snow cover usually lasts from November till March, about 132 days or 36% of the year;. [35] The city frequently gets thunderstorms during the summer, averaging 27 days a year with thunderstorms. [26]
Winnipeg has a reputation for being a windy city with the intersection of Portage and Main being called the windiest intersection in Canada; [36] however, Winnipeg is only the 12th windiest city in Canada, just below Hamilton, Ontario. [37] The average annual wind speed is 16.9 km/h (10.5 mph), predominantly from the south but the city has experienced wind gusts of up to 129 km/h (80 mph). [18] April is the windiest month, and July the least windy. Tornadoes do occur in the area, particularly in the late spring and summer months, however they are not frequent. [38] A Fujita scale F5 tornado struck Elie (just 30 km (19 mi) west of Winnipeg) in 2007; this was the strongest tornado ever recorded in Canada. [39]
Because of its flat topography and substantial snowfall, Winnipeg is subject to severe flooding. The Red River reached its greatest flood height in 1826, and this event still remains the highest flood stage of the last two hundred years.
A major flood in 1950 caused a State of Emergency to be declared and the Canadian Army was brought in to protect residents and property. Because of the flood, 100,000 residents were evacuated from their homes and approximately 10,000 homes were destroyed, along with many hospitals, schools and businesses. The flood prompted the Government of Manitoba, under former premier Dufferin Roblin, to build the Red River Floodway. The floodway is colloquially referred to as Duff's Ditch, and is a 47 km (29 mi) long diversion channel that protects Winnipeg from flooding. [40]
Construction on the floodway project began 6 October 1962 and cost $63 million. The project resulted in excavation of approximately 76.5 million cubic metres of earth. Completed in March 1968, it has successfully prevented over $10 billion in flood damages. [40] The flood control system prevented flooding in 1974 and 1979 when water levels neared record levels. However, in the 1997 Red River flood, water threatened the city's relatively unprotected southwest corner. Flood control dikes were reinforced and raised using sandbags and the threat was averted. Winnipeg suffered limited damage compared to cities without flood control structures, such as Grand Forks, North Dakota.
Other related water diversion projects farther away from Winnipeg include the Portage Diversion (also known as the Assiniboine River Floodway) and the Shellmouth Reservoir.
Winnipeg is situated where tall grass prairie meets aspen parkland and is not very far from boreal coniferous forests of the rocky Canadian Shield. The tall grass prairie areas are notable for its endangered western prairie fringed orchid. [41] [42] Some prairie grasses include big bluestem and spear grasses; and wildflowers include aster, goldenrod, prairie crocus and lady's-slipper. [43] Some birds found around Winnipeg include ferruginous and Swainson's hawks; screech and great horned owls; as well as Canada geese and mallards. [43] Winnipeg is also home of the largest remaining mature urban elm forest in North America. [44] Some species of Winnipeg's 8 million trees include elm, ash, maple, oak, poplar, basswood, willow, birch, spruce, pine, cedar, as well as some fruit trees and shrubs. [44] The Red River is the home of a number of species of fish including catfish, goldeye, and walleye.
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. Manitoba has a 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.
Winnipeg is the capital and largest city of the province of Manitoba in Canada. It is centred on the confluence of the Red and Assiniboine rivers, near the longitudinal centre of North America. As of 2021, Winnipeg had a city population of 749,607 and a metropolitan population of 834,678, making it Canada's sixth-largest city and eighth-largest metropolitan area.
The Red River, also called the Red River of the North to differentiate it from the Red River in the south of the continent, is a river in the north-central United States and central Canada. Originating at the confluence of the Bois de Sioux and Otter Tail rivers between the U.S. states of Minnesota and North Dakota, it flows northward through the Red River Valley, forming most of the border of Minnesota and North Dakota and continuing into Manitoba. It empties into Lake Winnipeg, whose waters join the Nelson River and ultimately flow into Hudson Bay.
Brandon is the second-largest city in the province of Manitoba, Canada. It is located in the southwestern corner of the province on the banks of the Assiniboine River, approximately 214 kilometres (133 mi) west of the provincial capital, Winnipeg, and 120 kilometres (75 mi) east of the Saskatchewan border. Brandon covers an area of 77.41 km2 (29.89 sq mi) with a population of 51,313, and a census metropolitan area population of 54,268. It is the primary hub of trade and commerce for the Westman Region as well as parts of southeastern Saskatchewan and northern North Dakota, an area with a population of over 190,000 people.
The Red River Floodway is an artificial flood control waterway in Western Canada. It is a 47 km (29 mi) long channel which, during flood periods, takes part of the Red River's flow around the city of Winnipeg, Manitoba to the east and discharges it back into the Red River below the dam at Lockport. It can carry floodwater at a rate of up to 140,000 cubic feet per second (4,000 m3/s), expanded in the 2000s from its original channel capacity of 90,000 cubic feet per second (2,500 m3/s).
The Assiniboine River is a 1,070-kilometre (660 mi) long river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris, and Whitesand Rivers.
The Red River flood of 1997 was a major flood that occurred in April and May 1997 along the Red River of the North in Minnesota, North Dakota, and southern Manitoba. It was the most severe flood of the river since 1826. The flood reached throughout the Red River Valley, affecting the cities of Fargo and Winnipeg, but none so greatly as Grand Forks and East Grand Forks, where floodwaters reached more than 3 miles (4.8 km) inland. They inundated virtually everything in the twin communities. Total damages for the Red River region were US$3.5 billion. The flood was the result of abundant snowfall and extreme temperatures.
Portage la Prairie is a small city in the Central Plains Region of Manitoba, Canada. As of 2016, the population was 13,304 and the land area of the city was 24.68 square kilometres (9.53 sq mi).
Selkirk is a city in the western Canadian province of Manitoba, located on the Red River about 22 kilometres (14 mi) northeast of Winnipeg, the provincial capital. It has a population of 10,504 as of the 2021 census.
The Forks is a historic site, meeting place, and green space in downtown Winnipeg located at the confluence of the Red River and the Assiniboine River.
The Shellmouth Reservoir is a man-made reservoir on the Assiniboine River in Manitoba and Saskatchewan, Canada.
The 1950 Red River flood was a devastating flood that took place along the Red River in The Dakotas and Manitoba from April 15 to June 12, 1950. Damage was particularly severe in the city of Winnipeg and its environs, which were inundated on May 5, also known as Black Friday to some residents.
The Portage Diversion is a water control structure on the Assiniboine River near Portage la Prairie, Manitoba, Canada. The project was made as part of a larger attempt to prevent flooding in the Red River Valley. The Portage Diversion consists of two separate gates which divert some of the flow of water in the Assiniboine River to a 29 km long diversion channel that empties into Lake Manitoba near Delta Beach. This helps prevent flooding on the Assiniboine down river from the diversion, including in Winnipeg, where the Assiniboine River meets the Red River.
The geography of Manitoba addresses the easternmost of the three prairie Canadian provinces, located in the longitudinal centre of Canada. Manitoba borders on Saskatchewan to the west, Ontario to the east, Nunavut to the north, and the American states of North Dakota and Minnesota to the south. Although the border with Saskatchewan appears straight on large-scale maps, it actually has many right-angle corners that give the appearance of a slanted line. In elevation, Manitoba ranges from sea level on Hudson Bay to 2727 ft (831 m) on top of Baldy Mountain. The northern sixty percent of the province is on the Canadian Shield. The northernmost regions of Manitoba lie permafrost, and a section of tundra bordering Hudson Bay.
Delta Marsh consists of an extensive open marsh located near the south shore of Lake Manitoba, approximately 24 km north of the town of Portage la Prairie, Manitoba. The marsh extends for nearly 30 km along the shore of the lake, and has a breadth of up to 4 km. The marsh consists of a network of interconnected shallow bays separated from Lake Manitoba by a wooded barrier dune ridge of 300m to 600m width.
The history of flooding in Canada includes floods caused by snowmelt runoff or freshet flooding, storm-rainfall and "flash flooding", ice jams during ice formation and spring break-up, natural dams, coastal flooding on ocean or lake coasts from storm surges, hurricanes and tsunamis. Urban flooding can be caused by stormwater runoff, riverine flooding and structural failure when engineered flood management structures, including dams and levees, prove inadequate to manage the quantities and force of flood waters. Floods can also occur when groundwater levels rise entering buildings cracks in foundation, floors and basements. Flooding is part of the natural environmental process. Flooding along large river systems is more frequent in spring where peak flows are often governed by runoff volume due to rainfall and snowmelt, but can take place in summer with flash floods in urban systems that respond to short-duration, heavy rainfall. Flooding due to hurricanes, or downgraded severe storms, is a concern from August to October when tropical storms can affect Eastern North America. Flood events have had a significant effect on various regions of the country. Flooding is the costliest natural disaster for Canadians. Most home insurance claims in Canada deal with water damage due to sewer back-up, not fire.
The history of Winnipeg comprises its initial population of Aboriginal peoples through its settlement by Europeans to the present day. The first forts were built on the future site of Winnipeg in the 1700s, followed by the Selkirk Settlement in 1812. Winnipeg was incorporated as a city in 1873 and experienced dramatic growth in the late 19th and early 20th centuries. Following the end of World War I, the city's importance as a commercial centre in Western Canada began to wane. Winnipeg and its suburbs experienced significant population growth after 1945, and the current City of Winnipeg was created by the unicity amalgamation in 1972.
The 2009 Red River flood along the Red River of the North in North Dakota and Minnesota in the United States and Manitoba in Canada brought record flood levels to the Fargo-Moorhead area. The flood was a result of saturated and frozen ground, spring snowmelt exacerbated by additional rain and snow storms, and virtually flat terrain. Communities along the Red River prepared for more than a week as the U.S. National Weather Service continuously updated the predictions for the city of Fargo, North Dakota, with an increasingly higher projected river crest. Originally predicted to reach a level of near 43 feet (13 m) at Fargo by March 29, the river in fact crested at 40.84 feet (12.45 m) at 12:15 a.m. March 28, and started a slow decline. The river continued to rise to the north as the crest moved downstream.
This is a timeline of the history of Winnipeg.
The 2011 Souris/Mouse River flood in Canada and the United States occurred in June and was greater than a hundred-year flooding event for the river. The US Army Corps of Engineers estimated the flood to have a recurrence interval of two to five centuries.