North Saskatchewan River - wikipedia North Saskatchewan River North Saskatchewan River Headwaters of the North Saskatchewan in Banff National Park Country Canada Provinces Alberta, Saskatchewan Tributaries - left Brazeau River - right Clearwater River, Vermilion River, Battle River Cities Edmonton, AB, North Battleford, SK, Prince Albert, SK Source Rocky Mountains - location Saskatchewan Glacier, Alberta - elevation 2,080 m ( 6,824 ft ) - coordinates 52 ° 09 ′ 22 '' N 117 ° 10 ′ 54 '' W ﻿ / ﻿ 52.15611 ° N 117.18167 ° W ﻿ / 52.15611 ; - 117.18167 Mouth Saskatchewan River - location Saskatchewan River Forks, Saskatchewan - elevation 380 m ( 1,247 ft ) - coordinates 53 ° 14 ′ 07 '' N 105 ° 04 ′ 58 '' W ﻿ / ﻿ 53.23528 ° N 105.08278 ° W ﻿ / 53.23528 ; - 105.08278 Coordinates : 53 ° 14 ′ 07 '' N 105 ° 04 ′ 58 '' W ﻿ / ﻿ 53.23528 ° N 105.08278 ° W ﻿ / 53.23528 ; - 105.08278 Length 1,287 km ( 800 mi ) Basin 122,800 km ( 47,413 sq mi ) Discharge for Prince Albert, Saskatchewan, 53 km ( 33 mi ) from the mouth - average 238 m / s ( 8,405 cu ft / s ) - max 5,660 m / s ( 199,881 cu ft / s ) - min 19 m / s ( 671 cu ft / s ) The North Saskatchewan River drainage basin 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. The Saskatchewan River system is the largest shared between the Canadian provinces of Alberta and Saskatchewan. Its watershed includes most of southern and central Alberta and Saskatchewan. Contents 1 Course 2 Geography 3 Geology 4 History 5 Recreation 6 Fish species 7 Flooding 8 Commercial navigation 9 Dams and hydroelectric development 10 Tributaries 11 Photo gallery 12 See also 13 Further reading 14 References 15 External links Course The North Saskatchewan River has a length of 1,287 kilometres ( 800 mi ), and a drainage area of 122,800 square kilometres ( 47,400 sq mi ). At its end point at Saskatchewan River Forks it has a mean discharge of 245 cubic metres per second ( 8,700 cu ft / s ). The yearly discharge at the Alberta -- Saskatchewan border is more than 7 cubic kilometres ( 1.7 cu mi ). The river begins above 1,800 metres ( 5,900 ft ) at the toe of the Saskatchewan Glacier in the Columbia Icefield, and flows southeast through Banff National Park alongside the Icefields Parkway. At the junction of the David Thompson Highway ( Highway 11 ), it initially turns northeast for 10 kilometres ( 6.2 mi ) before switching to a more direct eastern flow for about 30 kilometres ( 19 mi ). At this point, it turns north where it eventually arrives at Abraham Lake. Bighorn Dam constricts the north end of Abraham Lake, where the North Saskatchewan emerges to track eastward to Rocky Mountain House. At Rocky Mountain House, the river abruptly turns north again for 100 kilometres ( 62 mi ) where it switches east towards Edmonton, Alberta. In Edmonton, the river passes through the centre of the city in a northeasterly direction and out towards Smoky Lake at which point it quickly changes to the southeast and then more to the east as it makes its way to the Alberta -- Saskatchewan boundary. From the border, the river flows southeast between North Battleford and Battleford and on in the direction of Saskatoon. About 40 kilometres ( 25 mi ) northwest of Saskatoon, near Langham, the river veers to the northeast where it passes through the City of Prince Albert. About 30 kilometres ( 19 mi ) downstream of Prince Albert, the North Saskatchewan River joins the South Saskatchewan River at Saskatchewan River Forks to become the Saskatchewan River. From there, the river flows east to Tobin Lake and into Manitoba, eventually emptying into Lake Winnipeg. Geography A view of the river looking south from Edmonton 's Glenora neighbourhood The river course can be divided into five distinct sections. The first, the eastern slopes of the Rocky Mountains, is the smallest area geographically, although the largest in terms of run - off and contributed water flow. The glaciers and perpetual snows of the mountain peaks feed the river year - round. Mountains, with little vegetation, experience fast - melting snow cover. The second section of the river comprises the foothills region. The terrain is hilly and rough, with a deeper and more defined valley. This area is well covered with forest and muskeg, and run - off into the river is much more constant and stable than in the mountains. From Edmonton to the mouth of the Vermilion River, the North Saskatchewan flows through the plains - parkland divide, with occasional stretches of prairie. The North Saskatchewan River valley parks system ; the largest expanses of urban parkland in Canada. Cutting across Edmonton and the Capital Region. The river runs in a well - defined valley with deep cuts in the landscape. The fourth section, from the Vermilion River to Prince Albert is principally prairie with a few small stretches of timber and secondary forest cover. The valley of the river is much wider, and the river itself spreads out across shallow water and flows over many shifting sand bars. Low - lying, flat areas, border the river for much of this section. The final section of the river, from Prince Albert to the Saskatchewan River Forks, has many rapids. The valley is more shallow than the previous sections of the river, and the channel is much better defined. There is little prairie and much tree cover in this section. Geology This section needs expansion. You can help by adding to it. ( May 2011 ) The Bridge River Ash is in the vicinity of the North Saskatchewan River, which erupted from the Mount Meager massif in southwestern British Columbia about 2350 years ago. History The river is shown on a Hudson 's Bay Company map from 1760, labeled as the Beaver River. Its Cree name is kisiskâciwanisîpiy ( swift current ). From this name is derived the name Saskatchewan, used as well for the South Saskatchewan River and the Saskatchewan River ( to which the North Saskatchewan is a major tributary ), and the province of that name. Its Blackfoot name is omaka - ty ( big river ). The North Saskatchewan in Edmonton circa 1913. Note steamboats in the foreground, construction of the High Level Bridge in the background, and mid-river piers for future Walterdale Bridge between. The section of the North Saskatchewan river that falls within the Banff National Park boundaries has been designated a Canadian Heritage River in 1989, for its importance in the development of western Canada. The river demarcates the prairie -- parkland divide for much of its course and acted as a natural boundary between plains Blackfoot and woodland Cree First Nations people for thousands of years. With the westward expansion of the fur trade spearheaded by the North West Company and followed by the Hudson 's Bay Company, the river became an important transportation route for fur trade brigades ' York boats, to which it was especially well suited as it follows an eastern trend toward Hudsons Bay, the entry point for the HBC into Canada. Many fur trade posts were constructed on the river, including Fort Edmonton ( 1795 ) and Rocky Mountain House, the uppermost post reached by canoe navigation. The river 's importance continued after the amalgamation of the Hudson 's Bay Company and the North West Company. The river was plied by a number of steamboats right up to WWI, although for everyday freight the growing web of railway lines in the western prairies eventually replaced them. The river was used commercially for many years - to carry flatboats of settlers goods and construction materials downstream from Edmonton, to float thousands of logs in the annual log drive downstream to Edmonton prior to WWI, as a source of ice blocks for home owners ' iceboxes. Recreation Edmonton 's North Saskatchewan River valley parks system is the largest system of urban parks in North America, and covers both sides of the river valley 's course through Edmonton. Fish species Fish species include : walleye, sauger, yellow perch, northern pike, goldeye, mooneye, lake sturgeon, mountain whitefish, burbot, longnose sucker, white sucker and shorthead redhorse. Flooding Like all rivers, the North Saskatchewan is subject to periodic flooding, beginning with rapid snowmelt in the mountains or prolonged periods of rain in the river basin. With the establishment of permanent communities along the river 's course, and the rise of an administrative / government structure, records exist recording floods in the North Saskatchewan for the past century. The Bighorn Dam, constructed in the early 1970s near Nordegg, Alberta, and the Brazeau Dam, constructed in the mid-1960s, have not reduced flooding potential on the North Saskatchewan River ( Alberta Environment 1981 ) 29 June 1915 cover of the Edmonton Daily Bulletin List of notable flood years This list is incomplete ; you can help by expanding it. Year Edmonton Prince Albert Peak date mean daily flow ( m3 / s ) Peak date Peak flow ( m3 / s ) 1899 18 August 4570 August 3960 1912 10 July 2100 14 July 1980 19 August 1990 25 August 1550 1914 9 June 1750 14 June 1790 1915 29 June 4640 2 July 5300 16 July 2550 21 July 2320 1917 18 May 1860 23 May 1540 1923 25 June 2380 30 June 1640 1925 18 August 2150 23 August 1620 1932 4 June 1870 10 June 2160 1944 16 June 3450 20 June 2940 1948 25 May 1850 31 May 2090 1952 25 June 3540 29 June 2970 1954 8 June 3030 12 June 2790 27 August 2820 1 Sept 2570 1965 29 June 2590 4 July 2460 1969 7 July 1740 13 July 1570 1972 27 June 2970 2 July 2340 -- -- 23 April 3880 1980 7 June 1740 13 June 1680 1982 6 July 1920 13 July 1580 1986 19 July 3990 24 July 3230 1990 4 July 2340 10 July 1890 2005 21 June 2270 27 June 1800 2011 19 June 1800 26 June 2100 2013 23 June 2710 29 June 2200 The flood of 1899 The river peaked at a stage of 12.61 metres ( 41.4 ft ) with an estimated peak instantaneous discharge of 5,100 cubic metres per second ( 180,000 cu ft / s ). North Saskatchewan River flood of 1915 Main article : North Saskatchewan River flood of 1915 The 1915 flood of the North Saskatchewan River was one of the most dramatic in the history of Edmonton. On 28 June, the Edmonton Bulletin reported the river had risen `` 10 feet in as many hours. '' A frantic phone call from Rocky Mountain House alerted local authorities to the flood 's arrival. The Canadian Northern Railway had parked a number of train cars on the city 's Low Level Bridge to protect against the `` tons upon tons of debris '' that had been pushed up against its piers, including a house swept away by the current. Thousands of Edmonton residents watched the flood destroy lumber mills along the city 's river valley. The river peaked at a stage of 13.73 metres ( 45.0 ft ), a rise of 11.5 metres ( 38 ft ) above low flow, with an estimated peak instantaneous discharge of 5,800 cubic metres per second ( 200,000 cu ft / s ). However, based on high water marks and 1D modelling, the actual value may have been closer to 6,300 cubic metres per second ( 220,000 cu ft / s ). The flood of 1986 The river peaked at a stage of 11.5 metres ( 38 ft ) with a peak instantaneous discharge of 4,520 cubic metres per second ( 160,000 cu ft / s ). 2013 Alberta Flooding Along with many other rivers in central and southern Alberta during late June, the North Saskatchewan saw significantly higher water levels and flow rates. The river peaked at a stage of 9.03 m ( 29.6 ft ) with a peak instantaneous discharge of 2,710 cubic metres per second ( 96,000 cu ft / s ) on June 23rd in Edmonton. This is signicantly higher than the Bow River 's peak height at 4.1 metres ( 13 ft ) and peak discharge of 1,750 cubic metres per second ( 62,000 cu ft / s ) on June 21st, that caused widespread flooding in Calgary. However, due to the expansive North Saskatchewan River Valley and natural sanctuary / parkland that surrounds it, the City of Edmonton had only minor, isolated flooding, with virtually no major property damage as a result. Commercial navigation The North Saskatchewan River has always been a major trade route from Hudson Bay and central Canada across the Canadian Prairies to the Canadian Rockies. During the fur trade era, birch bark canoes and York boats travelled up and down the Saskatchewan delivering trade goods and amassing furs for transportation to Europe. The North Saskatchewan also witnessed a lively, although short - lived, era of steamboat shipping during the 1870s, 1880s, and 1890s. The Hudson 's Bay Company ( HBC ) purchased a number of steamboats from companies operating on the Red River and trading at Winnipeg / Fort Garry. The HBC desired to avoid paying the labour costs of fur trade brigades, and hoped steamboat shipping would provide a suitable alternative. Several HBC steamboats navigated the river intermittently for many years, although fluctuating water levels and natural barriers ( rapids and sandbars ) hampered efficient operation. With the arrival of the railroad in Western Canada, steamboat shipping on the North Saskatchewan tapered off, but steamboats operated in the Edmonton area until the economic crash of 1912 - 14. Dams and hydroelectric development A number of dams have been planned and constructed on the North Saskatchewan River and its tributaries. No singular purpose has dominated dam planning in the basin, indeed, hydroelectric development, flood control, and water diversion schemes have all underpinned proposals to construct dams on the river. Planned dams The first hydroelectric development on the North Saskatchewan was planned in 1910 near the Town of Drayton Valley. Funding for the plan came from a British syndicate ; design and construction were to be carried out by the Edmonton Hydro - Electric Power Scheme. The development was shelved after the outbreak of World War I. The La Colle Falls hydroelectric project east of Prince Albert was a half - built failure. Construction began in the 1910s and was later abandoned. The city remained in debt from financing the project until 1960, and the site still attracts tourists today. During the 1960s and 1970s, a major dam was planned on the North Saskatchewan near the Hamlet of Hairy Hill, Alberta, about 160 kilometres ( 100 mi ) downstream from Edmonton. This dam was part of a larger interbasin water diversion conceived by the Alberta Government to transfer water from the Peace, Smoky, and Athabasca rivers to the Saskatchewan River Basin. The planned dam had a maximum height of 65 metres ( 212 ft ), with a crest length of 1.76 kilometres ( 5,760 ft ), which would have created a reservoir capable of holding over 4.9 cubic kilometres ( 4,000,000 acre ⋅ ft ) of water. The reservoir would have affected municipal water works in the City of Fort Saskatchewan, was likely to inundate part of the Saddle Lake Indian Reserve, and would have flooded a number of oil and natural gas fields in the area. The plan was later shelved in light of economic and environmental concerns. Constructed dams The Bighorn Dam was constructed near Nordegg and created Abraham Lake, one of the largest reservoirs in Alberta. The dam was constructed in 1971 by TransAlta. The Bighorn Plant has a generating capacity of 120 megawatts ( MW ), and has an available water supply that allows it to be the largest producer of hydroelectric electricity in Alberta, with an average of 408,000 megawatt hours ( MW. h ) each year. One of the North Saskatchewan 's major tributaries, the Brazeau River, houses the Brazeau Hydroelectric Plant. At 355 MW, the Brazeau Dam is Alberta 's largest hydroelectric facility, and was built in 1965 by TransAlta. Though having a higher peak generating capacity than the Bighorn Dam, the hydrology of the Brazeau means that its average annual electricity production is a slightly smaller 397,000 MW. h. Tributaries Saskatchewan Glacier to Abraham Lake Nigel Creek Alexandra River Norman Creek Rampart Creek Arctomy 's Creek Castleguard River Howse River Glacier River Mistaya River Peyto Lake Owen Creek Thompson Creek Corona Creek Spreading Creek Wildhorse Creek Loudon Creek Siffleur River Escarpment River Two O'Clock Creek Bridge Creek Whiterabbit Creek Abraham Lake to Rocky Mountain House Canyon Creek Cline River Pinto Lake Whitegoat Creek BATUS Creek Hoodoo Creek Allstones Creek Mud Creek Tershishner Creek Crooked Creek Kidd Creek Bighorn River Black Canyon Creek South Creek Dutch Creek Jock Creek Gap Creek Deep Creek Shunda Creek Jack Fish Creek Camp Creek Lundine Creek Lewis Creek Rough Creek Ram River North Ram River Cow Creek Cow Lake Clearwater River Rocky Mountain House to Edmonton Chicken Creek Little Beaver Creek Big Beaver Creek No Name Creek Baptiste River Brazeau River Southesk River, Cardinal River, Blackstone River, Elk River, Nordegg River Sand Creek Wolf Creek Washout Creek Mishow Creek Poplar Modeste Creek Tomahawk Creek Shoal Lakes Creek Wabamum Creek Wabamum Lake Strawberry Creek Weed Creek Willow Creek Cutbank Creek Conjuring Creek Wizard Lake Whitemud Creek Blackmud Creek Mill Creek Ravine Edmonton to Alberta - Saskatchewan Border Rat Creek Oldman Creek Horsehills Creek Ross Creek Sturgeon River Big Lake Redwater River Beaverhill Creek Waskatenau Creek Egg Creek Smoky Creek White Earth Creek Redclay Creek Cucumber Creek Saddlelake Creek Lake Eliza Creek Siler Creek Gideon Lake Death River Antimose Creek Telegraph Creek Moosehills Creek Mooswa Creek Middle Creek Borden Lake, Laurier Lake, Ross Lake, Whitney Lake Frog Creek Alma Creek Vermilion River Chester Creek Two Hills Creek Cabin Lake Mosquito Creek Fulton Creek Saskatchewan Pipestone Creek Oldman Creek Monnery River Muskeg Creek Whitesand Creek Englishman River Big Gulley Creek Birling Creek Turtle Lake River Jackfish River Battle River Cooper Creek Baljennie Creek Eagle Creek Pakrowka Creek Shepherds Creek Turtle Creek Cee Pee Creek Radouga Creek Steep Creek Miners Creek Sturgeon River Little Red River Spruce River Garden River Photo gallery Boating in Edmonton, with a view of the High Level Bridge across the river The Edmonton Light Rail Transit ( LRT ) bridge across the river in central Edmonton Driftwood on the river bank near the Groat Bridge in Edmonton Dudley B. Menzies Bridge ( LRT and pedestrian bridge ) over North Saskatchewan River in Edmonton A view of the North Saskatchewan River Valley from the east end of Edmonton The river covered in a sheet of ice in Edmonton North Saskatchewan River and Abraham Lake from space North Saskatchewan River near Myrnam, Alberta View of the City of North Battleford across the North Saskatchewan River See also List of crossings of the North Saskatchewan River North Saskatchewan River valley parks system List of longest rivers of Canada List of rivers of Saskatchewan Saskatchewan River fur trade Watershed management Further reading Kostash, Myrna ( 2005 ). Reading the River : A Traveller 's Companion to the North Saskatchewan River. Coteau Books. ISBN 978 - 1 - 5505 - 0317 - 3. Retrieved 2016 - 04 - 30. References Jump up ^ `` Saskatchewan River ''. Encyclopædia Britannica. 2006. Retrieved September 22, 2006. Jump up ^ Atlas of Canada. `` Major Rivers in Canada ''. Archived from the original on April 4, 2007. Retrieved 2007 - 05 - 01. Jump up ^ Alberta Environment - Alberta river basins Jump up ^ `` River Valley Parks ''. City of Edmonton. City of Edmonton. Retrieved 31 March 2016. Jump up ^ `` Ribbon of Green Concept Plan : Basic Principles ''. City of Edmonton. City of Edmonton. Archived from the original on 26 March 2016. Retrieved 31 March 2016. Jump up ^ Surveys of the North Saskatchewan River : 1910 - 1915. Edmonton : Government of the Province of Alberta, Department of Water Resources, 1917. Pages 50 - 53. Jump up ^ MacDonald, 3 Jump up ^ Geographic Board of Canada. Place Names of Alberta ( 1928 ) Jump up ^ `` North Saskatchewan River ''. Canadian Heritage River System. 2011. Retrieved 2015 - 07 - 09. Jump up ^ `` Fish Species of Saskatchewan ''. Government of Saskatchewan. Archived from the original on 2015 - 11 - 03. Jump up ^ Mustapha, A.M. ( 1981 ). History of Floods in the North Saskatchewan River Basin ( Report ). Alberta Environment, Environmental Engineering Support Services, Technical Services Division. Jump up ^ Research Council of Alberta, Highways Division. Hydrologic Data on Floods in the North Saskatchewan River. ( Edmonton : Research Council of Alberta, 1965 ). Jump up ^ `` Archived copy ''. Archived from the original on 2007 - 12 - 31. Retrieved 2008 - 01 - 02. Environment Canada, Water Survey of Canada, retrieved 11 January 2009. Jump up ^ The Edmonton Bulletin, 28 June 1915. ^ Jump up to : The Edmonton Bulletin, 29 June 1915. Jump up ^ https://wateroffice.ec.gc.ca/report/historical_e.html?stn=05DF001&mode=Graph&type=h2oArc&results_type=historical&dataType=Daily&parameterType=Level&year=2013&y1Max=1&y1Min=1 Jump up ^ https://wateroffice.ec.gc.ca/report/historical_e.html?stn=05BH004&mode=Table&type=h2oArc&results_type=historical&dataType=Daily&parameterType=Flow&year=2013&y1Max=1&y1Min=1 Jump up ^ Bruce Peel, Steamboats on the Saskatchewan, ( Saskatoon : Prairie Books, 1972 ) Jump up ^ Tom Monto, Old Strathcona - Edmonton 's Southside Roots ( Alhambra Books / Crang Publishing ( 2011 ). Jump up ^ Loosmore, W.S.B. To Trail 's End : Early Settlement in Drayton Valley. Drayton Valley : Drayton Valley and District Historical Society, 1994. Pages 10 - 14. Jump up ^ Saskatchewan Settlement Experience. Sasksettlement.com. Retrieved on 2013 - 07 - 12. Jump up ^ Saskatchewan Settlement Experience. Sasksettlement.com. Retrieved on 2013 - 07 - 12. Jump up ^ Athabasca River Historical Report. albertawater.com. Retrieved on 2018 - 03 - 01. Jump up ^ Prairie Farm Rehabilitation Administration, Engineering Services, Alberta Regional Division. Hariy Hill Dam -- North Saskatchewan River, Engineering Report. Calgary : Saskatchewan - Nelson Basin Board, 1970. ^ Jump up to : `` Bighorn ''. www.transalta.com. Retrieved 2017 - 12 - 26. ^ Jump up to : `` Brazeau ''. www.transalta.com. Retrieved 2017 - 12 - 26. Jump up ^ Milholland, Billie. North Saskatchewan River Guide : Mountain to Prairie a Living Landscape. Edmonton : North Saskatchewan Watershed Alliance, 2002. External links North Saskatchewan Watershed Alliance - designated Watershed Planning and Advisory Council Encyclopedia of Saskatchewan Canadian Heritage Rivers System Rivers Alsek Arctic Red Athabasca Bay du Nord Bloodvein Bonnet Plume Boundary Waters Clearwater Cowichan Detroit Fraser French Grand Hayes Hillsborough Humber Kazan Kicking Horse Main Margaree Mattawa Missinaibi North Saskatchewan Red Rideau Seal Shelburne Soper South Nahanni St. Croix St. Marys Tatshenshini Thames Thelon The Three Rivers Upper Restigouche Yukon Nominated Adams Churchill Coppermine Ottawa Saint John See also American Heritage Rivers Category : American Heritage Rivers Category : Canadian Heritage Rivers Category : Rivers of Canada Hydrography of Alberta Rivers Athabasca Battle Beaver Bow Brazeau Clearwater Crowsnest Elbow Hay Little Bow Milk North Saskatchewan Oldman Peace Pembina Red Deer Slave Smoky South Saskatchewan Waterfalls Athabasca Bow Bridal Veil Crescent Crypt Elbow Lundbreck Panther Sunwapta Lakes Athabasca Beaverhill Bistcho Claire Cold Crowsnest Jackfish Lake La Biche Lesser Slave Pigeon Ste. Anne Sylvan Utikuma Wabamun Reservoirs Abraham Barrier Brazeau Chestermere Kananaskis McGregor Minnewanka Glenmore Milk River Ridge Sikome Gleniffer Glaciers Athabasca Bow Columbia Icefield Crowfoot Hector Peyto Saskatchewan Vulture Wapta Waputik Icefield Other Hay - Zama Wetlands Peace -- Athabasca Delta Whooping Crane Summer Range ( wetlands ) VIAF : 315144237 Retrieved from `` https://en.wikipedia.org/w/index.php?title=North_Saskatchewan_River&oldid=830440316 '' Categories : Canadian Heritage Rivers Rivers of Alberta Rivers of Saskatchewan Saskatchewan River Rivers of the Canadian Rockies Tributaries of Hudson Bay Hidden categories : All articles with dead external links Articles with dead external links from June 2016 All articles with unsourced statements Articles with unsourced statements from July 2015 Coordinates on Wikidata Geobox usage tracking for river type Articles to be expanded from May 2011 All articles to be expanded Articles using small message boxes Articles with unsourced statements from May 2010 Incomplete lists from January 2009 Wikipedia articles with VIAF identifiers Talk Contents About Wikipedia Беларуская ( тарашкевіца ) ‎ Български Català Чӑвашла Čeština Dansk Deutsch Español Esperanto فارسی Français 한국어 Hrvatski Italiano Lietuvių Nederlands 日本 語 Norsk Norsk nynorsk Polski Português Русский Српски / srpski Srpskohrvatski / српскохрватски Svenska Українська 中文 18 more Edit links This page was last edited on 14 March 2018, at 20 : 55. 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Question: where does the saskatchewan river start and end
Answer: central Saskatchewan; from the Canadian Rockies continental divide east to central Saskatchewan; Saskatchewan Glacier, Alberta