Watershed Resiliency and Restoration Program Grant Approval Fact Sheet
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The Little Bow Gets Bigger – Alberta's Newest River
ALBERTA WILDERNESS Article ASSOCIATION Wild Lands Advocate 13(1): 14 - 17, February 2005 The Little Bow Gets Bigger – Alberta’s Newest River Dam By Dr. Stewart B. Rood, Glenda M. Samuelson and Sarah G. Bigelow The Little Bow/Highwood Rivers Project includes Alberta’s newest dam and provides the second major water project to follow the Oldman River Dam. The controversy surrounding the Oldman Dam attracted national attention that peaked in about 1990, and legal consideration up to the level of the Supreme Court over federal versus provincial jurisdiction and the nature and need for environmental impact analysis. A key outcome was that while environmental matters are substantially under provincial jurisdiction, rivers involve fisheries, navigation, and First Nations issues that invoke federal responsibility. As a consequence, any major water management project in Canada requires both provincial and federal review. At the time of the Oldman Dam Project, three other proposed river projects in Alberta had received considerable support and even partial approval. Of these, the Pine Coulee Project was the first to advance, probably partly because it was expected to be the least controversial and complex. That project involved the construction of a small dam on Willow Creek, about an hour south of Calgary. A canal from that dam diverts water to be stored in a larger, offstream reservoir in Pine Coulee. That water would then be available for release back into Willow Creek during the late summer when flows are naturally low but irrigation demands are high. Pine Coulee was generally a dry prairie coulee and reservoir flooding did not inundate riparian woodlands or an extensive stream channel. -
Preliminary Soil Survey of the Peace River-High Prairie-Sturgeon Lake
PROVINCE OF ALBERTA Research Council of Alberta. Report No. 31. University of Alberta, Edmonton, Alberta. SOIL SURVEY DIVISION Preliminary Soi1 Survey of The Peace River-High Prairie- Sturgeon Lake Area BY F. A. WYATT Department of Soils University of Alberta, Edmonton, Alberta (Report published by the University of Alberta at the request of Hon. Hugh W. Allen, Minister of Lands and Mines) 1935 Price 50 cents. LETTER OF TRANSMITTAL. , DR. R. C. WALLACE, Director of Research, Resedrch Cowuil of Alberta, University of Alberta, Edmonton, Alberta. Sir:- 1 beg to submit a report entitled “Preliminary Soi1 Survey of the Peace River-High Prairie-Sturgeon Lake Area,” prepared in co- operation with Dr. J. L. Doughty, Dr. A. Leahey and Mr. A. D. Paul. A soi1 map in colors accompanies this report. This report is compiled from five adjacent surveys c,onducted between the years 1928 and 1931. It includes a11 of two and parts of the other three surveys. The area included in the report is about 108 miles square with McLennan as the approximate geographical tenter. Respectfully submitted, F. A. WYATT. Department of Soils, University of, Alberta, Edmonton, Alberta, April 15th, 1935. .-; ‘- TABLE OF CONTENTS PAGE Description of area ...............................................................................................................................................1 Drainage ........................................................................................................................................................................2 Timber -
Information Package Watercourse
Information Package Watercourse Crossing Management Directive June 2019 Disclaimer The information contained in this information package is provided for general information only and is in no way legal advice. It is not a substitute for knowing the AER requirements contained in the applicable legislation, including directives and manuals and how they apply in your particular situation. You should consider obtaining independent legal and other professional advice to properly understand your options and obligations. Despite the care taken in preparing this information package, the AER makes no warranty, expressed or implied, and does not assume any legal liability or responsibility for the accuracy or completeness of the information provided. For the most up-to-date versions of the documents contained in the appendices, use the links provided throughout this document. Printed versions are uncontrolled. Revision History Name Date Changes Made Jody Foster enter a date. Finalized document. enter a date. enter a date. enter a date. enter a date. Alberta Energy Regulator | Information Package 1 Alberta Energy Regulator Content Watercourse Crossing Remediation Directive ......................................................................................... 4 Overview ................................................................................................................................................. 4 How the Program Works ....................................................................................................................... -
Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005
Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005 CONSERVATION REPORT SERIES The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. CONSERVATION REPORT SERIES 25% Post Consumer Fibre When separated, both the binding and paper in this document are recyclable Sport Fish Distribution and Relative Abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005 Jason Blackburn Alberta Conservation Association 2nd floor, YPM Place, 530 – 8th Street South Lethbridge, Alberta, Canada T1J 2J8 Report Series Co‐editors PETER AKU KELLEY KISSNER Alberta Conservation Association 50 Tuscany Meadows Cres. NW #101, 9 Chippewa Rd Calgary, AB T3A 5K6 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data, Technical ISBN printed: 978‐0‐7785‐7731‐7 ISBN online: 978‐0‐7785‐7732‐4 Publication No.: T/199 Disclaimer: This document is an independent report prepared by the Alberta Conservation Association. The authors are solely responsible for the interpretations of data and statements made within this report. Reproduction and Availability: This report and its contents may be reproduced in whole, or in part, provided that this title page is included with such reproduction and/or appropriate acknowledgements are provided to the authors and sponsors of this project. Suggested Citation: Blackburn, J. 2007. Sport fish distribution and relative abundance on the Lower Red Deer River from Dickson Dam to Joffre, Alberta, 2005. -
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta Submitted to: Submitted by: SSRB Water Storage Opportunities AMEC Environment & Infrastructure, Steering Committee a Division of AMEC Americas Limited Lethbridge, Alberta Lethbridge, Alberta 2014 amec.com WATER STORAGE OPPORTUNITIES IN THE SOUTH SASKATCHEWAN RIVER BASIN IN ALBERTA Submitted to: SSRB Water Storage Opportunities Steering Committee Lethbridge, Alberta Submitted by: AMEC Environment & Infrastructure Lethbridge, Alberta July 2014 CW2154 SSRB Water Storage Opportunities Steering Committee Water Storage Opportunities in the South Saskatchewan River Basin Lethbridge, Alberta July 2014 Executive Summary Water supply in the South Saskatchewan River Basin (SSRB) in Alberta is naturally subject to highly variable flows. Capture and controlled release of surface water runoff is critical in the management of the available water supply. In addition to supply constraints, expanding population, accelerating economic growth and climate change impacts add additional challenges to managing our limited water supply. The South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009) identified re-management of existing reservoirs and the development of additional water storage sites as potential solutions to reduce the risk of water shortages for junior license holders and the aquatic environment. Modelling done as part of that study indicated that surplus water may be available and storage development may reduce deficits. This study is a follow up on the major conclusions of the South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009). It addresses the provincial Water for Life goal of “reliable, quality water supplies for a sustainable economy” while respecting interprovincial and international apportionment agreements and other legislative requirements. -
A Taxonomic and Ecologic Study of the Riverbottom Forest on St
Great Basin Naturalist Volume 36 Number 3 Article 1 9-30-1976 A taxonomic and ecologic study of the riverbottom forest on St. Mary River, Lee Creek, and Belly River in southwestern Alberta, Canada Robert K. Shaw Cardston, Alberta, Canada Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Shaw, Robert K. (1976) "A taxonomic and ecologic study of the riverbottom forest on St. Mary River, Lee Creek, and Belly River in southwestern Alberta, Canada," Great Basin Naturalist: Vol. 36 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol36/iss3/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. The Great Basin Naturalist Published at Provo, Utah, by Brigham Young University Volume 36 September 30, 1976 No. 3 A TAXONOMIC AND ECOI.OGIC STUDY OF THE RIVERBOTTOM FOREST ON ST. MARY RIVER, LEE CREEK, AND BELLY RIVER IN SOUTHW^ESTERN ALBERTA, CANADA Robert K. Shawi Abstr.\ct. — The riverbottom forest community of St. Mary River. Lee Creek, and Belly River in southvvestern Alberta. Canada, is a unique ecological entity characterized by poplar species hav- ing their major Alberta distribution along these streams. Stands in the community are dominated by three tree species, six shrub species, and nine herb species. Establishment of the community is dependent on climate and substrate; destruction is the result of progressive lateral stream-flow erosion. -
Bow River Basin State of the Watershed Summary 2010 Bow River Basin Council Calgary Water Centre Mail Code #333 P.O
30% SW-COC-002397 Bow River Basin State of the Watershed Summary 2010 Bow River Basin Council Calgary Water Centre Mail Code #333 P.O. Box 2100 Station M Calgary, AB Canada T2P 2M5 Street Address: 625 - 25th Ave S.E. Bow River Basin Council Mark Bennett, B.Sc., MPA Executive Director tel: 403.268.4596 fax: 403.254.6931 email: [email protected] Mike Murray, B.Sc. Program Manager tel: 403.268.4597 fax: 403.268.6931 email: [email protected] www.brbc.ab.ca Table of Contents INTRODUCTION 2 Overview 4 Basin History 6 What is a Watershed? 7 Flora and Fauna 10 State of the Watershed OUR SUB-BASINS 12 Upper Bow River 14 Kananaskis River 16 Ghost River 18 Seebe to Bearspaw 20 Jumpingpound Creek 22 Bearspaw to WID 24 Elbow River 26 Nose Creek 28 WID to Highwood 30 Fish Creek 32 Highwood to Carseland 34 Highwood River 36 Sheep River 38 Carseland to Bassano 40 Bassano to Oldman River CONCLUSION 42 Summary 44 Acknowledgements 1 Overview WELCOME! This State of the Watershed: Summary Booklet OVERVIEW OF THE BOW RIVER BASIN LET’S TAKE A CLOSER LOOK... THE WATER TOWERS was created by the Bow River Basin Council as a companion to The mountainous headwaters of the Bow our new Web-based State of the Watershed (WSOW) tool. This Comprising about 25,000 square kilometres, the Bow River basin The Bow River is approximately 645 kilometres in length. It begins at Bow Lake, at an River basin are often described as the booklet and the WSOW tool is intended to help water managers covers more than 4% of Alberta, and about 23% of the South elevation of 1,920 metres above sea level, then drops 1,180 metres before joining with the water towers of the watershed. -
South Saskatchewan River Basin Adaptation to Climate Variability Project
South Saskatchewan River Basin Adaptation to Climate Variability Project Climate Variability and Change in the Bow River Basin Final Report June 2013 This study was commissioned for discussion purposes only and does not necessarily reflect the official position of the Climate Change Emissions Management Corporation, which is funding the South Saskatchewan River Basin Adaptation to Climate Variability Project. The report is published jointly by Alberta Innovates – Energy and Environment Solutions and WaterSMART Solutions Ltd. This report is available and may be freely downloaded from the Alberta WaterPortal website at www.albertawater.com. Disclaimer Information in this report is provided solely for the user’s information and, while thought to be accurate, is provided strictly “as is” and without warranty of any kind. The Crown, its agents, employees or contractors will not be liable to you for any damages, direct or indirect, or lost profits arising out of your use of information provided in this report. Alberta Innovates – Energy and Environment Solutions (AI-EES) and Her Majesty the Queen in right of Alberta make no warranty, express or implied, nor assume any legal liability or responsibility for the accuracy, completeness, or usefulness of any information contained in this publication, nor that use thereof infringe on privately owned rights. The views and opinions of the author expressed herein do not necessarily reflect those of AI-EES or Her Majesty the Queen in right of Alberta. The directors, officers, employees, agents and consultants of AI-EES and the Government of Alberta are exempted, excluded and absolved from all liability for damage or injury, howsoever caused, to any person in connection with or arising out of the use by that person for any purpose of this publication or its contents. -
Sediment Fingerprinting in the Lower Little Bow River Using Cs-137 As a Tracer
Melody Caron et al. Sediment fingerprinting in the Lower Little Bow River Sediment fingerprinting in the Lower Little Bow River using Cs-137 as a tracer Melody Caron Department of Soil Science, University of Manitoba David A. Lobb Department of Soil Science, Watershed Systems Research Program, University of Manitoba Jim J. Miller Lethbridge Research and Development Centre, Agriculture and Agri-Food Canada Kui Liu Department of Soil Science, University of Manitoba Phillip N. Owens Environmental Science Program, University of Northern British Columbia The Lower Little Bow River watershed is a source of irrigation water for southeast Alberta. However, sediment in the river can be detrimental to both irrigation pump equipment and the health of the river. In order to understand and manage how sedi- ment moves through a watershed, a study of sediment sources was conducted along a reach of the Lower Little Bow River employing fingerprinting techniques. The radionuclide cesium-137 was used as a tracer to determine whether the sediment in the river is being generated by surface or subsurface erosion processes. The main sources of sediment were found from subsur- face erosion of an irrigation return-flow channel, coulee walls, and the river’s stream banks. This demonstrates that subsurface erosion is the principle generator of sediment in the Lower Little Bow. Through measurement of multiple points along the reach, the study also determined that the composition of the suspended sediment load did not change as it moved downstream in the river. Keywords: soil erosion, sedimentation, sediment fingerprinting, cesium-137, irrigation, Alberta Introduction tion, where an increase in nutrient concentration causes exces- The sources of suspended sediments in watersheds can be identi- sive algal growth on the surface of water (Barthod et al. -
Escape from the Great Plains the Icelanders in North Dakota and Alberta
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Great Plains Quarterly Great Plains Studies, Center for Fall 1983 Escape From The Great Plains The Icelanders In North Dakota And Alberta Howard Palmer University of Calgary Follow this and additional works at: https://digitalcommons.unl.edu/greatplainsquarterly Part of the Other International and Area Studies Commons Palmer, Howard, "Escape From The Great Plains The Icelanders In North Dakota And Alberta" (1983). Great Plains Quarterly. 1695. https://digitalcommons.unl.edu/greatplainsquarterly/1695 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. ESCAPE FROM THE GREAT PLAINS THE ICELANDERS IN NORTH DAKOTA AND ALBERTA HOWARD PALMER Immigration historians in Canada and the United One important feature of this movement that States are becoming aware of the need to look they do not highlight is the extent to which at immigration history within the larger context it included European immigrants and their of North American history. Canadian immi children who had settled earlier in the United gration patterns have been affected, indirectly, States but decided to move on as new oppor almost as much by American immigration pol tunities opened up in Canada. The Hrst sizable icy as by Canadian policy. Within many ethnic settlements of Hungarians, Slovaks, Lithuan groups in North America, there has been a ians, Czechs, Danes, Finns, Norwegians, Swedes, significant exchange of people and cultural Icelanders, Dutch, Welsh, and Hutterites on patterns between Canada and the United the Canadian prairies did not come directly States. -
High Streamflow Advisory Update River Basins Currently With
High Streamflow Advisory Update Issued at 1:30 PM - June 11, 2010 Issued by River Forecast Centre River Basins Currently with Advisories Hay Peace Information in addition to this advisory may be found at: Athabasca High http://www.environment.alberta.ca/forecasting/forecasterscomments Level http://www.environment.alberta.ca/apps/basins Ft. McMurray High Streamflow Advisory – Stream levels are rising or expected to Peace rise rapidly and no major flooding is expected. Minor flooding in low- River lying areas is possible. Anyone situated close to the streams affected Grande Prairie is advised to be cautious of the rising levels. Beaver Flood Watch – Stream levels are rising and will approach or may Edmonton exceed bank full. Flooding of areas adjacent to these streams may North occur. Anyone situated close to the river is advised to take Saskatchewan appropriate precautionary measures. Red Deer Red Deer Flood Warning – Rising stream levels will result in flooding of areas adjacent to the streams affected. Anyone situated close to the river Calgary South Bow Saskatchewan should take appropriate measures to avoid flood damage. Medicine Hat Lethbridge Oldman Milk Streamflow Advisory Overview for Alberta Advisories apply to streams and their tributaries unless otherwise noted. ♦ Up to 50 mm of precipitation fell, with local amounts of up to 60 mm, in the North Saskatchewan and Red Deer River basins on Wednesday and Thursday. ♦ No significant precipitation is forecast in these areas over the next few days. ♦ Conditions are being monitored – -
JOURNAL of ALBERTA POSTAL HISTORY Issue
JOURNAL OF ALBERTA POSTAL HISTORY Issue #22 Edited by Dale Speirs, Box 6830, Calgary, Alberta T2P 2E7, or [email protected] Published in February 2020. POSTAL HISTORY OF RED DEER RIVER BADLANDS: PART 2 by Dale Speirs This issue deals with the northern section of the Red Deer River badlands of south-central Alberta from Kneehill canyon to Rosedale. The badlands portion of the river stretches for 200 kilometres, gouged out by glacial meltwaters. The badlands are the richest source of Late Cretaceous dinosaurs in the world. Originally settled by homesteaders, the coal industry dominated from the 1920s to its death in the 1950s. Since then, the tourist industry has grown, with petroleum and agriculture strong. 2 Part 1 appeared in JAPH #13. Index To Post Offices. Aerial 44 Beynon 30 Cambria 47 Carbon 56 Drumheller 7 Fox Coulee 20 Gatine 51 Grainger 60 Hesketh 53 Midlandvale 13 Nacmine 17 Newcastle Mine 16 Rosebud Creek/Rosebud 33 Rosedale 40 Rosedale Station 40 Wayne 26 3 DRUMHELLER MUNICIPALITY The economic centre of the Red Deer River badlands is Drumheller, with a population of about 8,100 circa 2016. Below is a modern map of the area, showing Drumheller’s central position in the badlands. It began in 1911 as a coal mining village and grew rapidly during the heyday of coal. After World War Two, when railroads converted to diesel and buildings were heated with natural gas, Drumheller went into a decades-long decline. The economic slump was finally reversed by the construction of the Royal Tyrrell Museum of Palaeontology, the world’s largest fossil museum and a major international tourist destination.