River Current Is Published Three Times a Year by Partners for the Sas Katch Ewan River Basin
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South Saskatchewan River Watershed Authority Watershed Stewards Inc
Saskatchewan South Saskatchewan River Watershed Authority Watershed Stewards Inc. Table of Contents 1. Comments from Participants 1 1.1 A message from your Watershed Advisory Committees 1 2. Watershed Protection and You 2 2.1 One Step in the Multi-Barrier Approach to Drinking Water Protection 2 2.2 Secondary Benefits of Protecting Source Water: Quality and Quantity 3 3. South Saskatchewan River Watershed 4 4. Watershed Planning Methodology 5 5. Interests and Issues 6 6. Planning Objectives and Recommendations 7 6.1 Watershed Education 7 6.2 Providing Safe Drinking Water to Watershed Residents 8 6.3 Groundwater Threats and Protection 10 6.4 Gravel Pits 12 6.5 Acreage Development 13 6.6 Landfills (Waste Disposal Sites) 14 6.7 Oil and Gas Exploration, Development, Pipelines and Storage 17 6.8 Effluent Releases 18 6.9 Lake Diefenbaker Water Levels and the Operation of Gardiner Dam 20 6.10 Watershed Development 22 6.11 Water Conservation 23 6.12 Stormwater Discharge 23 6.13 Water Quality from Alberta 25 6.14 Agriculture Activities 26 6.15 Fish Migration and Habitat 27 6.16 Role of Fisheries and Oceans Canada in Saskatchewan 28 6.17 Wetland Conservation 29 6.18 Opimihaw Creek Flooding 31 6.19 Federal Lands 32 7. Implementation Strategy 33 8. Measuring Plan Success - The Yearly Report Card 35 9. Conclusion 36 10. Appendices 37 Courtesy of Ducks Unlimited Canada 1. Comments from Participants 1.1 A message from your Watershed Advisory Committees North “Safe drinking water and a good supply of water are important to ALL citizens. -
The State of Lake Winnipeg
Great Plains Lakes The State of Lake Winnipeg Elaine Page and Lucie Lévesque An Overview of Nutrients and Algae t nearly 25,000 square kilometers, Lake Winnipeg (Manitoba, Canada) is the tenth-largest freshwater lake Ain the world and the sixth-largest lake in Canada by surface area (Figure 1). Lake Winnipeg is the largest of the three great lakes in the Province of Manitoba and is a prominent water feature on the landscape. Despite its large surface area, Lake Winnipeg is unique among the world’s largest lakes because it is comparatively shallow, with a mean depth of only 12 meters. Lake Winnipeg consists of a large, deeper north basin and a smaller, relatively shallow south basin. The watershed is the second-largest in Canada encompassing almost 1 million square kilometers, and much of the land in the watershed is cropland and pastureland for agricultural production. The lake sustains a productive commercial and recreational fishery, with walleye being the most commercially important species in the lake. The lake is also of great recreational value to the many permanent and seasonal communities along the shoreline. The lake is also a primary drinking water source for several communities around the lake. Although Lake Winnipeg is naturally productive, the lake has experienced accelerated nutrient enrichment over the past several decades. Nutrient concentrations are increasing in the major tributaries that flow into Lake Winnipeg (Jones and Armstrong 2001) and algal blooms have been increasing in frequency and extent on the lake, with the most noticeable changes occurring since the mid 1990s. Surface blooms of cyanobacteria have, in some years, covered greater than 10,000 square kilometers of the north basin of the lake Figure 1. -
Land Resources
Relationship with the Land - Resources This map shows one year’s travels of a clan of Amsskaapipikani in the last decade of the nineteenth century. Courtesy of Glenbow Museum Relationship with the Land – Seasonal Round Unit Resource Glenbow Museum Relationship with the Land - Resources Place Names on the Map: 1. Itsiputsimaup – Battle Coulee 2. Katoyissksi – Sweet Grass 3. Aiiyimmikoi – Cypress Hills 4. Pakoki Lake – Pakowki 5. Akaiiniskio – Manyberries 6. Einiotoka’nisi – Buffalo-Bull’s Head 7. Ihkitsitapiksi – Seven Persons 8. Aiiykimmikuyiu – Cypress Hills 9. Nokomis’s – Long Lakes 10. Matokeks oma’nistamoai otsitskiiitapiau – Women’s Society Left their Lodge Pole 11. A’ykomonoasiu – Green Lake 12. A’isinaiypi – Writing on Stone 13. A’kekoksistakskuyi – Women’s Point 14. Ponakiksi – Cut Bank Creek Relationship with the Land – Seasonal Round Unit Resource Glenbow Museum Relationship with the Land - Resources Blackfoot camps were composed of members of an extended family and other people who may have joined the clan. The arrangement of the tipis was not strictly defined in these camps, although all of them faced east. This allowed the morning prayers to travel towards the rising sun, helping it to come above the horizon for another day. Relationship with the Land – Seasonal Round Unit Resource Glenbow Museum Relationship with the Land - Resources Definition of the term – “Seasonal Round” The Blackfoot tribes had an enormous land base they inhabited. Within this territory they had areas where they would travel well over 500 miles during a yearly cycle to hunt, gather and renew religious commitments. Being knowledgeable of their environment and respectful of their gifts from the creator they would carefully select locations or places to travel to in a lifetime. -
Climate in the Lake Winnipeg Watershed and the Level of Lake Winnipeg
Climate in the Lake Winnipeg Watershed and the Level of Lake Winnipeg Prepared for the Manitoba Clean Environment Commission Gregory K. McCullough th 6 February 2015 This document has been prepared at the request of the Clean Environment Commission. The main objective are 1) to describe climatic patterns and inflow history to Lake Winnipeg over the 100 years since widespread, continuous meteorological and hydrometric records were initiated in the early 20th century, and to describe climate patterns predicted for the 21st century, and 2) to describe the effects of trends and variability in climate over the watershed on the water level record in the lake. Finally, there is a brief summary of how regulation since the late 1970s has interacted with these historical relationships. Disclosure In my current employment at the University of Manitoba, I conduct scientific research that is partially funded by Manitoba Hydro, including research related to the effects of climate change and hydro-electric regulation on Hudson Bay. However, none of the research described below was supported by funding from Manitoba Hydro. Lake Winnipeg Climate and Regulation 1 Feb 2015 Greg McCullough i Executive summary Over the last century, the total annual inflow to Lake Winnipeg has ranged by almost 4X from 35,000 to 136,000 cfs. The variability of tributary discharge and underlying climate in the watershed happens at four scales: seasonal, year-to-year, multi-decadal, and long term trends. The level of the lake has varied at all of these scales in rough synchrony with the supply of water from its watershed. Based on analyses reported in scientific literature, over the last century, precipitation has increased in the watersheds of the Winnipeg and Red Rivers. -
Perspectives of Blackfoot Confederacy People
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2021-03-02 Indian Residential Schools: Perspectives of Blackfoot Confederacy People Fox, Terri-Lynn Fox, T.-L. (2021). Indian Residential Schools: Perspectives of Blackfoot Confederacy People (Unpublished doctoral thesis). University of Calgary, Calgary, AB. http://hdl.handle.net/1880/113142 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Indian Residential Schools: Perspectives of Blackfoot Confederacy People by Terri-Lynn Fox (Aai’piihkwikomotaakii) A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN EDUCATIONAL RESEARCH CALGARY, ALBERTA MARCH, 2021 © Terri-Lynn Fox 2021 English Abstract This qualitative research project explored two main themes: the Indian residential school (IRS) settlement agreement for survivors of federally funded and church-run institutions, and the participants’ perspectives (N = 16) on the apology to the survivors and subsequent generations that have been affected. I focus on the First Nation population of southern Alberta, specifically the Blackfoot Confederacy (Siksikaitsitapi). I use a Siksikaitsitapi lens and methodology on their experiences at an IRS, the IRS settlement, the Canadian government’s apology to former students, and the status of reconciliation as a whole. -
Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H. -
The Methodists' Great 1869 Camp Meeting and Aboriginal Conservation Strategies in the North Saskatchewan River Valley
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Great Plains Quarterly Great Plains Studies, Center for 2009 The Methodists' Great 1869 Camp Meeting and Aboriginal Conservation Strategies in The North Saskatchewan River Valley George Colpitts Department of the University of Calgary, in Alberta, Canada Follow this and additional works at: https://digitalcommons.unl.edu/greatplainsquarterly Part of the Other International and Area Studies Commons Colpitts, George, "The Methodists' Great 1869 Camp Meeting and Aboriginal Conservation Strategies in The North Saskatchewan River Valley" (2009). Great Plains Quarterly. 1170. https://digitalcommons.unl.edu/greatplainsquarterly/1170 This Article is brought to you for free and open access by the Great Plains Studies, Center for at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Great Plains Quarterly by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. THE METHODISTS' GREAT 1869 CAMP MEETING AND ABORIGINAL CONSERVATION STRATEGIES IN THE NORTH SASKATCHEWAN RIVER VALLEY GEORGE COLPITTS George McDougall, chairman of the Methodist gent of Wesleyan Methodists and their Native Missions to the Indians of the Northwest affiliates from Fort Edmonton, Pigeon Lake, Territories, kept a large, black book in which he Lac Ste. Anne, Lac La Biche, and Whitefish jotted sermon notes, references to classical and Lake-all located on the most northern and biblical literature and sometimes simply his itin westerly fringes of the northern Great Plains. eraries by horseback from Victoria, the primary Their expedition and other hunts joined by Methodist mission in the far British northwest. Protestant or Roman Catholic missions help Under the "s" tab and labeled "Saskatchewan," identify some of the strategies of competition he noted repeatedly in the 1860s the food crisis and cooperation emerging in the western boreal facing North Saskatchewan residents. -
September 16, 2019 (Updated Web Links February 7, 2020) 1 Proposed
Proposed Nutrient Concentration Objectives and Loading Targets for the Red River at the US/Canada Boundary International Red River Board – Water Quality Committee Background Excessive nutrients such as phosphorus and nitrogen and resulting increase in the frequency and severity of algal blooms is one of the greatest water quality challenges facing the international Red River watershed and downstream Lake Winnipeg. While all jurisdictions within the watershed have various regulatory frameworks, as well as plans and approaches to reduce the contribution of nutrients to water, the development of an enhanced, coordinated, and systematic strategy is desirable. Since September 2011, with the support of the International Joint Commission (including through the International Watershed Initiatives funding), the International Red River Board’s Water Quality Committee has been undertaking work to address nutrients in the Red River. The mission is to develop a collaborative, science and watershed-based approach to managing nutrients in the Red River and its watershed with the goal of restoring and protecting aquatic ecosystem health and water uses in the Red River watershed and Lake Winnipeg. The strategy has a number of guiding principles: Efforts, decisions and outcomes will be based on and supported by scientifically defensible methods and research. An integrated watershed perspective and approach will be used in priority setting and decision making. Coordinated, cooperative and collaborative processes will be used where appropriate and desirable. Notwithstanding, it is understood that jurisdictional independence will be maintained and that jurisdictional participation is voluntary. The strategy and its objectives will be goal/outcome based with particular focus on the protection and/or restoration of aquatic ecosystems and water uses. -
Minnesota Red River Trails
NPS Form 10-900-b 0MB No, 7024-0078 (Jan 1987) ' ^ n >. •• ' M United States Department of the Interior j ; j */i i~i U i_J National Park Service National Register of Historic Places 41990' Multiple Property Documentation Form NATIONAL REGISTER This form is for use in documenting multiple property groups relating to one or several historic contexts. See instructions in Guidelines for Completing National Register Forms (National Register Bulletin 16). Complete each item by marking "x" in the appropriate box or by entering the requested information. For additional space use continuation sheets (Form 10-900-a). Type all entries. A. Name of Multiple Property Listing_______________________________________ Minnesota Red River Trails B. Associated Historic Contexts Minnesota Red River Trails, 1835-1871 C. Geographical Data State of Minnesota I | See continuation sheet D. Certification As the designated authority under the Nal ional Historic Preservation Act of 1966, as amended, I hereby certify that this documentation form meets the National R< gister documentation standards and sets forth requirements for the listing of related ^fo^r^e&-^r\^^r(l \feith the Natii nal Register criteria. This submission meets the procedural and professional requirerrlents^eftirfn in 36 GnWFari 6Q~ tftd-the Secretary of the Interior's Standards for Planning and Evaluation. rJ it fft> Sigriature or certifying official I an R. Stewart Date / / __________________Deputy State-Historic Preservation Officer State or Federal agency and bureau ,,. , , Minnesota Historical Society 1, herebAcertify that this multiple property documentation form has been approved by the National Register as a basis for evaluating related properties for listing in the National Register. -
Clean Water Guide
Clean water. For me. For you. Forever. A hands-on guide to keeping Manitoba’s water clean and healthy. WaterManitoba’s natural treasure Water is Manitoba’s most precious and essential resource. Where the water fl ows Our deep, pristine lakes give us drinking water. As well, our lakes Water is contained in natural geographic regions called watersheds. are beautiful recreation spots enjoyed by thousands of campers, Think of them as large bowls. Sometimes they are grouped together cottagers and fi shers — including many fi shers who earn their living to form larger regions, sometimes they are small and isolated. on our lakes. Watersheds help us protect our water by allowing us to control the spread of pollutants and foreign species from one watershed to Manitoba’s lakes, rivers and wetlands are home to a wide variety another. When we see Manitoba as a network of watersheds, it helps us of fi sh and wildlife. And our rushing rivers generate power for our to understand how actions in one area can affect water in other areas. businesses and light up our homes. Even more important, water is the source Where the water meets the land of all life on earth. It touches every area The strip of land alongside rivers, lakes, streams, dugouts, ponds of our lives. Without it, we could not and even man-made ditches is called a riparian zone or shoreline. thrive — we could not even survive. The trees and vegetation along this strip of land are an important habitat for many kinds of wildlife and the last line of defense between Unfortunately, many of the things pollutants in the ground and our water. -
Red River Trails
Red River Trails by Grace Flandrau ------... ----,. I' , I 1 /7 Red River Trails by Grace Flandrau Compliments of the Great Northern Railway The Red River of the North Red River Trails by Grace Flandrau Foreword There is a certain hay meadow in southwestern Minnesota; curiously enough this low-lying bit of prairie, often entirely submerged, happens to be an important height of land dividing the great water sheds of Hudson's Bay and Mississippi riv,er. I t lies between two lakes: One of these, the Big Stone, gives rise to the Minnesota river, whose waters slide down the long tobog gan of the Mississippi Valley to the Gulf of Mexico; from the other, Lake Traverse, flows the Bois de Sioux, a main tributary of the Red River of the North, which descends for over five. hundred miles through one of the richest valleys in the world to Lake Winnipeg and eventually to Hudson's Bay. In the dim geologic past, the melting of a great glacier ground up limestone and covered this valley with fertile deposits, while the glacial Lake Agassiz subsequently levelled it to a vast flat plain. Occasionally in spring when the rivers are exceptionally high, the meadow is flooded and becomes a lake. Then a boatman, travelling southward from the semi-arctic Hudson's Bay, could float over the divide and reach the Gulf of Mexico entirely by water route. The early travellers gave, romantic names to the rive.rs of the West, none more so, it seems to me, than Red River of the North, 3 with its lonely cadence, its suggestion of evening and the cry of wild birds in far off quiet places. -
Water Quality in the South SK River Basin
Water Quality in the South SK River Basin I AN INTRODUCTION TO THE SOUTH SASKATCHEWAN RIVER BASIN I.1 The Saskatchewan River Basin The South Saskatchewan River joins the North Saskatchewan River to form one of the largest river systems in western Canada, the Saskatchewan River System, which flows from the headwater regions along the Rocky Mountains of south-west Alberta and across the prairie provinces of Canada (Alberta, Saskatchewan, and Manitoba). The Prairie physiographic region is characterized by rich soils, thick glacial drift and extensive aquifer systems, and a consistent topography of broad rolling hills and low gradients which create isolated surface wetlands. In contrast, the headwater region of the Saskatchewan River (the Western Cordillera physiographic region) is dominated by thin mineral soils and steep topography, with highly connected surface drainage systems and intermittent groundwater contributions to surface water systems. As a result, the Saskatchewan River transforms gradually in its course across the provinces: from its oxygen-rich, fast flowing and highly turbid tributaries in Alberta to a meandering, nutrient-rich and biologically diverse prairie river in Saskatchewan. There are approximately 3 million people who live and work in the Saskatchewan River Basin and countless industries which operate in the basin as well, including pulp and paper mills, forestry, oil and gas extraction, mining (coal, potash, gravel, etc.), and agriculture. As the fourth longest river system in North America, the South Saskatchewan River Basin covers an incredibly large area, draining a surface of approximately 405 860 km² (Partners FOR the Saskatchewan River Basin, 2009). Most of the water that flows in the Saskatchewan River originates in the Rocky Mountains of the Western Cordillera, although some recharge occurs in the prairie regions of Alberta and Saskatchewan through year-round groundwater contributions, spring snow melt in March or April, and summer rainfall in May and early July (J.W.