Navigated Waters in Alberta
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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 -
Summer 2018 Vol
Summer 2018 Vol. 45 No. 2 Quarterly Journal of the Wilderness Canoe Association Image from the “Heart and Stroke” calendar. AGAWA! Story and photos by Jeff McColl This report, which is a little different than what you are used flow river, but you can’t really call it a “wild” river because to reading in Nastawgan , is an accumulation of information of changes due to logging and because of the railway tracks. I’ve collected during more than 30 years of running the Finding evidence of logging has become much harder in the Agawa. last 10 years as the forests and river reclaimed the area. We all know someone who has become smitten by a par - Finding out information on the Agawa and many other ticular area, and when I started paddling the Agawa I did not watersheds in Algoma is much easier now than when I think it would happen to me. started. The Historical Forestry Database online at the Sault I became aware of the Agawa in 1976, on the way west Ste. Marie Public Library is amazing! Many maps are over to compete in the White Water Nationals, when I crossed 100 years old and still incredibly accurate. over it on the Highway 17 bridge. The Agawa is a natural- The First Nations Peoples of this area deserve credit for guiding early surveyors through this area, even though their history was oral. Pictographs at Agawa rock reveal that the First Nations were there for thou - sands of years. Access to the river for paddlers can be a little complicated now because the passenger train stopped running in 2015. -
Intermediate & Advanced Lake Solo Charles Burchill
Intermediate & Advanced Lake Solo Charles Burchill March 19, 2017 This document covers the material required for Paddle Canada Lake Canoe Intermediate and Advanced Solo Skills courses and was developed based on the Paddle Canada Lake Canoe Program Manual (6th edition 2013). Some items have been updated in this manual from the Paddle Canada website 2015. This document should not be used alone but in conjunction with the PC resource material, program manual, stroke resource manual and other supporting documentation. It is not a complete resource manual for all conditions, paddling styles, equipment, or knowledge – there is a brief list of additional resources available at the end of the document for more information. This work is licensed under the Creative Commons Attribution-NonCommercial- NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ or send a letter to Creative Commons, 444 Castro Street, Suite 900, Mountain View, California, 94041, USA. Charles Burchill [email protected], the primary author, must be notified of corrections, updates, changes, and distribution of this document. Use of any organization, methods, information, or equipment in this document should not be taken as an endorsement or acceptance by the author or an editor. Individuals using this document for reference must take responsibility for any use of the material; it is the responsibility of the individual to determine if they are qualified to take on any outing and can accurately assess the conditions and their abilities in relation to their own safety.. The author/publisher/editors of this document will accept no responsibility for injury or loss associated with using information in this publication. -
LITTLE SMOKY LANDSLIDE, ALBERTA Corey R
CHARACTERIZING COMPLEX DEEP SEATED LANDSLIDE DEFORMATION USING CORNER REFLECTOR INSAR (CR-INSAR): LITTLE SMOKY LANDSLIDE, ALBERTA Corey R. Froese Alberta Geological Survey, Edmonton, Alberta, Canada, [email protected] Valentin Poncos1, Roger Skirrow2, Mohamed Mansour3, Derek Martin3 1Canadian Centre for Remote Sensing, Ottawa, Ontario 2Alberta Infrastructure and Transportation, Edmonton, Alberta 3Department of Civil and Environmental Engineering, University of Alberta, Edmonton, RÉSUMÉ Les glissements de terre rétrogressifs et profonds le long des parois de la vallée de la rivière Little Smoky, dans le nord- ouest de l'Alberta, ont mené à un entretien continu notable sur l’autoroute 49 au cours des 50 dernières années. Bien que les zones de vitesse plus élevées localisées aient résulté en une enquête et une surveillance spécifiques du site, les configurations de déformation générales des parois de la vallée restent difficiles à comprendre. Des études précédentes et une reconnaissance du champ ont mis l’accent sur une série de glissements plus actifs et plus récents, en superposition sur des glissements moins actifs et plus anciens, menant à la complexité des modèles de déformation et de vélocité. Puisque la végétation est importante sur ce site, une série de 18 réflecteurs à écho renforcé satellitaires ont été construits et installés sur les parois, le long des deux côtés de la vallée, à l’automne 2006 de sorte à fournir une série de sources ponctuelles où les déformations de niveau subcentimétrique peuvent être mesurées avec un niveau de confiance élevé au moyen de la technologie InSAR. La première année des données a démontré des tendances manifestes des réflecteurs à se déplacer dans la ligne de visée du satellite. -
Status of the Arctic Grayling (Thymallus Arcticus) in Alberta
Status of the Arctic Grayling (Thymallus arcticus) in Alberta: Update 2015 Alberta Wildlife Status Report No. 57 (Update 2015) Status of the Arctic Grayling (Thymallus arcticus) in Alberta: Update 2015 Prepared for: Alberta Environment and Parks (AEP) Alberta Conservation Association (ACA) Update prepared by: Christopher L. Cahill Much of the original work contained in the report was prepared by Jordan Walker in 2005. This report has been reviewed, revised, and edited prior to publication. It is an AEP/ACA working document that will be revised and updated periodically. Alberta Wildlife Status Report No. 57 (Update 2015) December 2015 Published By: i i ISBN No. 978-1-4601-3452-8 (On-line Edition) ISSN: 1499-4682 (On-line Edition) Series Editors: Sue Peters and Robin Gutsell Cover illustration: Brian Huffman For copies of this report, visit our web site at: http://aep.alberta.ca/fish-wildlife/species-at-risk/ (click on “Species at Risk Publications & Web Resources”), or http://www.ab-conservation.com/programs/wildlife/projects/alberta-wildlife-status-reports/ (click on “View Alberta Wildlife Status Reports List”) OR Contact: Alberta Government Library 11th Floor, Capital Boulevard Building 10044-108 Street Edmonton AB T5J 5E6 http://www.servicealberta.gov.ab.ca/Library.cfm [email protected] 780-427-2985 This publication may be cited as: Alberta Environment and Parks and Alberta Conservation Association. 2015. Status of the Arctic Grayling (Thymallus arcticus) in Alberta: Update 2015. Alberta Environment and Parks. Alberta Wildlife Status Report No. 57 (Update 2015). Edmonton, AB. 96 pp. ii PREFACE Every five years, Alberta Environment and Parks reviews the general status of wildlife species in Alberta. -
Canoe Trip: North to Athabasca by David Curran
Canoe Trip: North To Athabasca By David Curran Canoe Trip: North To Athabasca.PDF - Are you searching for Canoe Trip: North To Athabasca By David Curran Books? Now, you will be happy that at this time Canoe Trip: North To Athabasca PDF is available at our online library. With our complete resources, you could find by David Curran Canoe Trip: North To Athabasca PDF or just found any kind of Books for your readings everyday. You could find and download any books you like and save it into your disk without any problem at all. There is a lot of books, user manual, or guidebook that related to by David Curran Canoe Trip: North To Athabasca PDF, such as : seo for wordpress: how to get your website on page #1 of google...fast!, man vs. child: one dad’s guide to the weirdness of parenting, the crystal world, introduction to programming with java a problem solving approach, katherine elizabeth, full of grace, microsoft® sql server™ 2000 high availability, diabetic smoothie recipes: top 365 diabetic friendly easy to make/blend delicious smoothie recipes, casual game design: designing play for the gamer in all of us, the frozen water trade: a true story, twice taken, java software solutions: foundations of program design, how to write a novel the easy way: using the pulp fiction method to write better novels, fruit trees in small spaces: abundant harvests from your own backyard, quick & easy greek yogurt recipes: 47 delicious "almost vegetarian" greek yogurt dishes for breakfast, lunch, and dinner, patterns of the hypnotic techniques of milton h. -
University of Alberta Edmonton, Alberta
University of Alberta Fall and Winter Movements of Arctic grayling (Thymallus arcticus (Pallas)) in the Little Smoky River, Alberta A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Science Department of Biological Sciences Edmonton, Alberta FalI 1997 National Libr;try Bibliothèque nationale l*l of Canada du Canada Acquisitions and Acquisitions et Bibliographie Services services bibliographiques 395 Wellington Street 395, tue Wellington Ottawa ON K1A ON4 ûüawaON K1AON4 Canada Canada YwrlSle vmdkhmce Our No NMenlllrhence The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant à la National Library of Canada to Bibliothèque nationale du Canada de reproduce, loan, disûi'bute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfiche/film, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des extraits substantiels may be printed or othemise de celle-ci ne doivent êeimprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation, ABSTRACT Fall and winter movements of Arctic grayling from a 78 km reach of a river systern were evaluated using radiotelemetry. The rnovements of 30 fish were monitored weekly from August 31 to November 16, 1993 and biweekly from November 16, 1993 to January 15, 1994. -
Northern Tier National High Adventure Program Boy Scouts of America
Northern Tier National High Adventure Program Boy Scouts of America 2012 EXPEDITION & ROUTE PLANNING GUIDE TABLE OF CONTENTS Introduction 1 Policies 2 & 3 Contact Information 3 Safety Afloat and Safe Swim Defense Plans 4 Risk Advisory and Prevention of Problems 5 & 6 Fiscal Information 7 - 9 Crew Information 10 Physical Conditioning and Preparation 11 Expedition Planning Information 12 - 15 Charles L. Sommers Wilderness Canoe Base – Ely Minnesota 16 - 35 Prices, Crew Size, Camping Permits, Permit Fees 16 & 17 Canadian Customs, U.S. Customs, Special Restrictions, RABC 18 General Base Information 19 How to Get to the Ely Base 20 Map to Base 21 Detailed Transportation, Off Base Accommodations and Attractions 22 Fishing 22 & 23 Routes 24 Boundary Waters Canoe Area Wilderness Routes 25 - 28 Quetico Provincial Park Routes 29 - 33 Ely to Atikokan Routes 34 & 35 Donald Rogert Canoe Base – Atikokan, Ontario 36 - 59 Prices, Crew Size, Camping Permits, Permit Fees 36 & 37 Canadian Customs, U.S. Customs, Special Restrictions 37 General Base Information 38 Shuttle Into and Out of the Wilderness 38 & 39 How to Get to the Atikokan Base 39 Map to Base 40 Ground Transportation Services, Driving Times 41 Off Base Accommodations and Attractions 42 Fishing 42 Routes, Comparison of Parks 43 – 44 Ground Shuttle Information, Float Plane Options 45 Quetico Provincial Park Routes 46 – 49 Crown Lands Routes 50 – 54 Atikokan to Ely Routes 55 & 56 Canadian Fishing Expedition 57 & 58 Canadian Kayaking Trek 59 Northern Expeditions Canoe Base – Bissett, Manitoba 60 -
Development of a Snowmelt Runoff Model for the Lower Smoky River
Development of a Snowmelt Runoff Model for the Lower Smoky River Centre for Hydrology Report No. 13 John Pomeroy, Kevin Shook, Xing Fang, Tom Brown and Chris Marsh Centre for Hydrology, University of Saskatchewan 117 Science Place, Saskatoon, Saskatchewan, S7N 5C8 1 Development of a Snowmelt Runoff Model for the Lower Smoky River Centre for Hydrology Report No. 13 John Pomeroy, Kevin Shook, Xing Fang, Tom Brown and Chris Marsh Centre for Hydrology, University of Saskatchewan 117 Science Place, Saskatoon, SK S7N 5C8 March 15, 2013 Contract No. 130051. Prepared for Alberta Environment and Sustainable Resource Development, Edmonton Prepared by John Pomeroy, Kevin Shook, Xing Fang, Tom Brown and Chris Marsh © Centre for Hydrology, University of Saskatchewan, Saskatoon, Saskatchewan 2 3 Table of Contents Executive Summary ............................................................................................................................6 List of Figures .....................................................................................................................................7 List of Tables ......................................................................................................................................8 List of Acronyms .................................................................................................................................9 1. Introduction................................................................................................................................. 12 1.1 Overview -
Update on the Little Smoky Landslide
UPDATE ON THE LITTLE SMOKY LANDSLIDE Roger Skirrow, Alberta Infrastructure and Transportation, Edmonton, Alberta, Canada Don Proudfoot, Thurber Engineering Ltd, Edmonton, Alberta, Canada Corey Froese, AMEC Earth & Environmental, Edmonton, Alberta, Canada Stan Thomson, Professor Emeritus, University of Alberta, Edmonton, Alberta, Canada ABSTRACT The Little Smoky River valley is cut into a preglacial channel infilled with very soft deposits. Valley slope instability is pervasive and very deeply seated. Highway 49 crosses the valley along an alignment that involves long sidehill traverses connected by a relatively low level bridge crossing. The south bridge abutment and land-based piers, and a significant portion of the southern valley slope exhibited movements shortly after construction in 1957. Stabilization efforts were undertaken at that time, as documented by Hayley and Thomson, 1975. Over the past 30 years more movements have occurred on both valley slopes. Numerous investigations and studies were undertaken on both valley slopes, and both slopes are being monitored at discrete instrumented locations. An InSAR study was completed to provide a widescale interpretation of the valley movements. This paper provides an overview of the salient issues and a discussion of short term and long-term mitigation options. RÉSUMÉ Le Little Smoky River Valley est coupé en canal preglacial infilled avec les dépôts très mous. L'instabilité de pente de vallée est dominante et très profondément assise. La Route 49 traverse la vallée le long d'un alignement qui implique de longues traversées reliées par un croisement de pont de niveau relativement bas. La butée du sud de pont et les piliers sur terre, et une partie significative de la pente méridionale de vallée ont montré des mouvements peu de temps après la construction en 1957. -
River Ice Observation Report River Forecast Centre April 10, 2014
River Ice Observation Report River Forecast Centre April 10, 2014 2013 – 2014 Peace River Report No. 31 An observation flight located the Peace River ice front at km 273.1 (22 km upstream of Dunvegan) this morning. This is approximately 100 km further upstream than the average position. It has been receding at a rate of approximately 8 km a day for the last 6 days. The jam at the mouth of the Little Smoky River released last night into the Smoky River ice cover. A localized ice run pushed through to Watino yesterday evening. The Smoky River ice cover downstream of the Little Smoky River has deteriorated into a repeating series of short stretches of intact ice, open water and small ice accumulations. A small accumulation of ice has backed up against the more intact ice cover at the mouth of the Smoky River, but has not affected the Peace River ice cover. Water levels have remained low, even during periods of high snowmelt runoff and ice movement. The ice cover on the lower Smoky River is expected to continue to melt and erode over the course of the day. A contributed observation reported moving ice on the Heart River near Nampa this afternoon. This is expected to pass through the Town of Peace River later this afternoon. The channel through Town is free of ice. Temperatures are forecasted to cool to below the seasonal average for the next several days. This is expected to slow the recession of the Peace River ice front. The flood protection dyke in downtown Peace River was repaired last night, following the intentional breach to lower water levels in the downtown core on Tuesday night. -
Conservation Blueprint of Northern Alberta
Conservation Blueprint of Northern Alberta Prioritizing areas for protected areas planning Conservation Blueprint of Northern Alberta Conservation Blueprint of Northern Alberta Prioritizing areas for protected areas planning Alison Ronson Danielle Pendlebury Columbian ground squirrel- Danielle Pendlebury © 2015 Canadian Parks and Wilderness Society, Northern Alberta Conservation Blueprint of Northern Alberta: Prioritizing areas for protected areas planning ISBN: 978-0-9949229-1-5 Published by the Canadian Parks and Wilderness Society, Northern Alberta. All rights reserved under International and Pan-American Copyright Conventions. No part of this book may be reproduced in any form or by any electronic or mechanical means, including information storage and retrieval systems, without prior written permission from the Canadian Parks and Wilderness Society, Northern Alberta. The maps in this report are for illustrative purposes only. Do not rely on these maps for a precise indication of routes, locations of features, or as a guide to navigation. Canadian Parks and Wilderness Society, Northern Alberta PO Box 52031, Edmonton, Alberta, T6G 2T5 www.cpawsnab.org Book design by Christy Campos and Danielle Pendlebury Printed in Canada on recycled paper (100% post-consumer waste) certified by the Forest Stewardship Council Acknowledgements CPAWS Northern Alberta is grateful to the Alberta Ecotrust Foundation and TD Friends of the Environment Foundation for funding the development and printing of the Conservation Blueprint of Northern Alberta. CPAWS Northern Alberta would like to thank the following individuals for their invaluable advice, guidance, and support during the development and execution of the Conservation Blueprint project: Dr. Rick Schneider and Dr. Scott Neilson at the University of Alberta, Dr.