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Northeast Wollaston Lake Project: Quaternary Investigations of The
Northeast Wollaston Lake Project: Quaternary Investigations of the Cochrane River (NTS map sheets 64L-10, -11, -14, and -15) and Charcoal Lake (NTS map sheets 64L-9 and -16) Areas J.S. Smith Smith, J.S. (2006): Northeast Wollaston Lake Project: Quaternary investigations of the Cochrane River (NTS map sheets 64L- 10, -11, -14, and -15) and Charcoal Lake (NTS map sheets 64L-9 and -16) areas; in Summary of Investigations 2006, Volume 2, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2006-4.2, CD-ROM, Paper A-6, 15p. Abstract Quaternary geological investigations were initiated in the Cochrane River–Charcoal Lake area (NTS map sheets 64L-9 -10, -11, -14, -15, and -16) as part of the multidisciplinary, multi-year Wollaston Lake Project. The Quaternary component involves 1:50 000-scale surficial geological mapping, collection of ice-flow indicators, and a regional till sampling program. Drift cover is extensive and includes till, organics, and glaciofluvial terrains as the main surficial units. Glacial landforms include hummocky stagnant ice-contact drift, thick blankets and plains, streamlined forms, and boulder fields. Large esker systems extend over the entire map area. These features are attributed to a slowly retreating ice margin, at which there was an abundance of meltwater that flowed both in channels and occasionally as turbulent sheet flows. Multiple ice-flow directions were documented; however, the ice-flow history remains preliminary as age relationships were only identified at five sites. The main regional ice flow was towards the south-southwest (207º). Initial flow ranged between the west-southwest to southwest (258º to 235º), and was followed by a southward (190º) flow before the main flow was established. -
Recording the Reindeer Lake
CONTEXTUALIZING THE REINDEER LAKE ROCK ART A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Master of Arts in the Department of Archaeology and Anthropology University of Saskatchewan Saskatoon By Perry Blomquist © Copyright Perry Blomquist, April 2011. All rights reserved. PERMISSION TO USE In presenting this thesis/dissertation in partial fulfillment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis/dissertation in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis/dissertation work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis/dissertation or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis/dissertation. Requests for permission to copy or to make other uses of materials in this thesis/dissertation in whole or part should be addressed to: Head of the Department of Archaeology and Anthropology University of Saskatchewan Saskatoon, Saskatchewan, S7N 5B1 Canada OR Dean College of Graduate Studies and Research University of Saskatchewan 107 Administration Place Saskatoon, Saskatchewan S7N 5A2 Canada i ABSTRACT The rock art that is found in the region of Reindeer Lake, Saskatchewan is part of a larger category of rock art known as the Shield Rock Art Tradition. -
Phase 1 Geoscientific Desktop Preliminary Assessment, Terrain and Remote Sensing Study
Phase 1 Geoscientific Desktop Preliminary Assessment, Terrain and Remote Sensing Study NORTHERN VILLAGE OF PINEHOUSE, SASKATCHEWAN APM-REP-06144-0060 NOVEMBER 2013 This report has been prepared under contract to the NWMO. The report has been reviewed by the NWMO, but the views and conclusions are those of the authors and do not necessarily represent those of the NWMO. All copyright and intellectual property rights belong to the NWMO. For more information, please contact: Nuclear Waste Management Organization 22 St. Clair Avenue East, Sixth Floor Toronto, Ontario M4T 2S3 Canada Tel 416.934.9814 Toll Free 1.866.249.6966 Email [email protected] www.nwmo.ca PHASE 1 DESKTOP GEOSCIENTIFIC PRELIMINARY ASSESSMENT TERRAIN AND REMOTE SENSING STUDY NORTHERN VILLAGE OF PINEHOUSE, SASKATCHEWAN November 2013 Prepared for: G.W. Schneider, M.Sc., P.Geo. Golder Associates Ltd. 6925 Century Ave, Suite 100 Mississauga, Ontario Canada L5N 7K2 Nuclear Waste Management Organization 22 St. Clair Avenue East 6th Floor Toronto, Ontario Canada M4T 2S3 NWMO Report Number: APM-REP-06144-0060 Prepared by: D.P. van Zeyl, M.Sc. L.A. Penner, M.Sc., P.Eng., P.Geo. J.D. Mollard and Associates (2010) Limited 810 Avord Tower, 2002 Victoria Avenue Regina, Saskatchewan Canada S4P 0R7 Terrain Report, Pinehouse, Saskatchewan November 2013 EXECUTIVE SUMMARY In March 2012, the Northern Village of Pinehouse, Saskatchewan, expressed interest in continuing to learn more about the Nuclear Waste Management Organization (NWMO) nine-step site selection process, and requested that a preliminary assessment be conducted to assess the potential suitability of the Pinehouse area for safely hosting a deep geological repository (Step 3). -
Far North Geomapping Initiative: Bedrock Geology of the Snyder Lake Area, Northwestern Manitoba (Part of NTS 64N5) by P.D
GS-1 Far North Geomapping Initiative: bedrock geology of the Snyder Lake area, northwestern Manitoba (part of NTS 64N5) by P.D. Kremer, C.O. Böhm and N. Rayner1 Kremer, P.D., Böhm, C.O. and Rayner, N. 2011: Far North Geomapping Initiative: bedrock geology of the Snyder Lake area, northwestern Manitoba (part of NTS 64N5); in Report of Activities 2011, Manitoba Innovation, Energy and Mines, Manitoba Geological Survey, p. 6–17. Summary The Wollaston Domain, The Manitoba Geological Survey’s Far North Geo- which forms part of the base- mapping Initiative continued in the summer of 2011 with ment sequence to the Proterozoic bedrock and surfi cial geological mapping in the Snyder Athabasca Basin in northeastern Lake area, in the northwestern corner of the province. Saskatchewan, locally contains basement-hosted uncon- The Snyder Lake area is largely underlain by medium- formity-related world-class uranium deposits (e.g., Mil- to upper-amphibolite–grade metasedimentary rocks of lennium deposit). A number of uranium occurrences in the Wollaston Supergroup, including psammitic, semi- Saskatchewan are associated with particular strata of the pelitic, pelitic, and lesser amounts of calcsilicate gneiss Wollaston Supergroup (e.g., graphitic pelite of the Daly and marble. Southeast and northwest of Snyder Lake, the Lake Group, calcsilicate and calcareous arkose of the sedimentary succession is fl anked by intrusive rocks of Geikie River Group, Yeo and Delaney, 2007). As a result, potential Archean age that were metamorphosed at upper the Wollaston Domain in northwestern Manitoba has seen a recent increase in exploration activity. Regional map- amphibolite- to granulite-facies conditions. -
Winter Roads in Manitoba
CGU HS Committee on River Ice Processes and the Environment 12th Workshop on the Hydraulics of Ice Covered Rivers Edmonton, AB, June 19-20, 2003 Winter Roads in Manitoba Don Kuryk Department of Transportation & Government Services 16th Floor – 215 Garry Street Winnipeg, Manitoba, R3C 3Z1 [email protected] Winter roads have connected isolated northern communities for over 50 years. Originally, winter roads were constructed by private contractors. Since 1979, the Department of Transportation has been overseeing the construction and maintenance of winter roads through contracts with Indian Bands and other local groups. The winter road network in Manitoba spans a length of 2178 km and services 30 communities (approximately 29000 people). It is extremely important for the shipment of goods, employment of locals and travel between communities. With the certainty of climate change and expected temperature increases of 4-6°C by the end of this century, there is a real threat to the seasonal operation of winter roads. The inevitable climate change from greenhouse gas emissions will result in later freeze-ups, earlier spring melts and more frost-free days. The implications of this climate change would be detrimental to the winter road network. An example of these implications was the airlifts required in 1998 to transport essential supplies to several communities as a result of drastic changes in the climate predominately due to El Nino. This shortened the winter road season and didn’t allow some of the routes to be constructed at all. 1. Introduction Winter roads originated over 50 years ago as a private operation until the government took over the network in 1971. -
Wollaston Lake, Uranium Mines Straddling on a Continental
Sentinel Vision EVT-503 Wollaston Lake, uranium mines straddling on a 15 August 2019 continental drainage divide Sentinel-1 CSAR IW acquired on 05 June 2015 at 00:34:07 UTC ... Sentinel-2 MSI acquired on 05 July 2019 at 18:19:29 UTC Author(s): Sentinel Vision team, VisioTerra, France - [email protected] 2D Layerstack Keyword(s): Lake, hydrology, mine, pollution, urban planning, Canada. Fig. 1 - S3 SLSTR (19.05.2019) - S5,S3,S2 colour composite - Wollaston Lake lies between Lake Athabasca & the western tip of Hudson bay. 3D view Fig. 2 - S1 (19.12.2016) - vv,vh,ndi(vh,vv) colour composite - Ice expanding during December. 3D view Fig. 3 - S1 (20.03.2018) - vv,vh,ndi(vh,vv) colour composite - Wollaston Lake covered in ice. 3D view Wollaston Lake lies in the wooded Shield country of north-east Saskatchewan, Canada. The lake has an average depth of 20.6 m and a maximum depth of 71 m. Its content is estimated at 75 km³. The water level is at an altitude of 398 m and its shoreline is 1475 km. The catchment area of the lake is 23 310 km² large. The lake is frozen between November and June. Fig. 4 - S1 (01.04.2018) - vv,vh,ndi(vh,vv) colour composite - Two weeks later, long thin cracks run along the lake's surface. 3D view To the north-west, about 10% of the lake's water drains via the Fond Du Lac River into Lake Athabasca and the Mackenzie River system which ultimately drains into the Arctic Ocean; to the north-east it drains via the Cochrane River into Reindeer Lake and the Churchill River system into Hudson Bay. -
Taiga Shield Ecozone Kazan River Upland Ecoregion Taiga Shield Ecozone the Taiga Shield Ecozone Lies on Either Side of Hudson Bay
Terrestrial Ecozones, Ecoregions, and Ecodistricts of Manitoba An Ecological Stratification of Manitoba’s Natural Landscapes Research Branch Technical Bulletin 1998-9E R.E. Smith, H. Veldhuis, G.F. Mills, R.G. Eilers, W.R. Fraser, and G.W. Lelyk Land Resource Unit Brandon Research Centre, Research Branch Agriculture and Agri-Food Canada Taiga Shield Ecozone Kazan River Upland Ecoregion Taiga Shield Ecozone The Taiga Shield Ecozone lies on either side of Hudson Bay. The eastern segment occupies the central part of Quebec and Labrador, and the western seg- ment occupies portions of north- ern Manitoba, Saskatchewan, Alberta and the south-eastern area of the continental North- west Territories, and the south- ern part of Nunavut. Character- istic of the zone are the open and often stunted conifer dominated forests, and the Precambrian shield with its shallow soils and many lakes. Climate The ecoclimate of the ecozone is classified as Subarctic, is a common occurrence in summer, especially in areas which is characterized by relatively short summers with with the stronger continental climate conditions. prolonged daylight, and long, very cold winters. Mean annual temperature in the area west of Hudson Bay is as Mean annual precipitation ranges from 200 to 500 mm low as -9.0oC, but it ranges from -1oC to -5oC in Quebec west of Hudson Bay, while east of Hudson Bay it ranges and Labrador, with some areas in Labrador having mean from 500 to 800 mm, to over 1000 mm locally along the annual temperatures as high as 1oC. A few degrees of frost Labrador coast. Selected Climate Data1 (Annual Means) for the Taiga Shield Ecozone Temperature Precipitation Degree Days Frost Free Period Station (oC) (>5oC) (days) Rain(mm) Snow(cm) Total(mm) Brochet A -4.9 261.8 167.5 427.1 952.0 97.0 Ennadai Lake -9.3 173.7 117.1 266.7 595.0 78.0 Uranium City A -3.5 204.9 197.9 344.8 1111.0 106.0 Yellowknife A -5.4 150.2 135.4 266.7 1027.0 111.0 1 Canadian Climate Normals, 1951-1980. -
Cochrane River
Autumn 1990 Vol. 17 No.3 Quarterly Journal of the Wilderness Canoe Association COCHRANE RIVER Article: Dave Bober Photos: Dave Bober and Ralph Zaffrann Old Crow can make the crossing from Wollaston to Reindeer Traffic on Wollaston was nil, except for the barge that Lake in less than thirty-two air kilometres, but rivers have a serves the several fish plants. The pristine beauty of this lake, mind of their own. The Cochrane River takes her sweet time, the largest within the borders of Saskatchewan, was insulted a detour of over three hundred twenty kilometres that will several years ago by the construction of the Rabbit Lake carry a wilderness canoeist into that superb little stick Mine Road. However, few recreational boaters risk the un- country, the domain of the sand eskers. pleasant remoteness of that road, so canoeist's still have the Having read Tyrell, Oberholtzer, Downes, and Klein, three great lake pretty much to themselves. of us eagerly paddled across Hidden Bay on Wollaston Lake in On our first full day we did about 38 kilometres in late July 1988. Even the cold summer rain was a relief after the almost ideal conditions for crossing big water-cloudy, cool, gruelling 430-km drive up from La Ronge. Our trio consisted of and easy showers. The calmness and translucence of the lake Ralph Zaffrann, a retired engineer from Rochester, New York; surface added a mystical quality to the many islands that Al Anuta, an engineering professor from Phoenix, Arizona; and seemed to loom before us like little mountains floating on an myself, a farmer from Hudson Bay, Saskatchewan. -
Phase 1 Geoscientific Desktop Preliminary Assessment, Lineament Interpretation
Phase 1 Geoscientific Desktop Preliminary Assessment, Lineament Interpretation NORTHERN VILLAGE OF PINEHOUSE, SASKATCHEWAN APM-REP-06144-0062 NOVEMBER 2013 This report has been prepared under contract to the NWMO. The report has been reviewed by the NWMO, but the views and conclusions are those of the authors and do not necessarily represent those of the NWMO. All copyright and intellectual property rights belong to the NWMO. For more information, please contact: Nuclear Waste Management Organization 22 St. Clair Avenue East, Sixth Floor Toronto, Ontario M4T 2S3 Canada Tel 416.934.9814 Toll Free 1.866.249.6966 Email [email protected] www.nwmo.ca PHASE 1 GEOSCIENTIFI C DESKTOP PRELIMINARY ASSESSMENT LINEAMENT INTERPRETATION NORTHERN VILLAGE OF PINEHOUSE, SASKATCHEWAN NWMO REPORT NUMBER: APM-REP-06144-0062 November 2013 Prepared for: G.W. Schneider, M.Sc., P.Geo. Golder Associates Ltd. 6925 Century Avenue, Suite 100 Mississauga, Ontario Canada L5N 7K2 Nuclear Waste Management Organization (NWMO) 22 St. Clair Avenue East 6th Floor Toronto, Ontario Canada M4T 2S3 Prepared by: Jason Cosford, Ph.D., P.Geo. L.A. Penner, M.Sc. P.Eng., P.Geo. J.D. Mollard and Associates (2010) Limited 810 Avord Tower, 2002 Victoria Avenue Regina, Saskatchewan Canada S4P 0R7 Lineament Interpretation, Pinehouse, Saskatchewan November 2013 EXECUTIVE SUMMARY In March 2012, the Northern Village of Pinehouse, Saskatchewan, expressed interest in continuing to learn more about the Nuclear Waste Management Organization’s (NWMO) nine- step site selection process, and requested that a preliminary assessment be conducted to assess potential suitability of the Pinehouse area for safely hosting a deep geological repository (Step 3). -
Spring 2006 Ii
Spring 2014 Vol. 41 No. 1 Quarterly Journal of the Wilderness Canoe Association Above Kazan Falls (from L to R: George Luste, Mike Good, John Martin, John Blackborow) Reindeer Lake to Baker Lake 1974 Following the 1894 route of Joseph Burr Tyrrell Story by John Martin Photos by John Martin and George Luste In January 1974, George Luste walked into my office and and tame rivers in southern Ontario, so this opportunity was proposed a canoe trip of over 800 miles, from Reindeer Lake immediately intriguing and I soon agreed. I had only been at on the Saskatchewan/Manitoba border to Baker Lake in the the University of Toronto for a year and it amazes me now Barren Lands during the upcoming summer. While I had that I got away with an eight-week absence from the lab so been paddling a canoe all my life, it had all been on lakes early in my career! The idea was to follow a large part of the 1894 route of Joseph Burr Tyrrell, which, as far as we knew, had not been done by anyone since. As many readers will know, Tyrrell was an acclaimed larger-than-life Canadian who travelled vast regions of the prairies and Barrens as an explorer and geologist for the Canadian Geographic Survey in the 1880s and 90s. In 1893, after descend - ing the Dubawnt to Baker Lake, his party paddled in appalling conditions in October down the coast of Hudson Bay and nearly perished not far north of Churchill. During this trip he had heard from his aboriginal guides of another great northern river, now known as the Kazan, and, undaunted, began to organ - ize an expedition to find and explore it. -
David Norman I{Iiiiam Hiit 8.4., University of Manitoba, Submitted In
HISTORY OF THE REINDEER AI\TD NEJAIiIILTNI LAKE DISTRTCT TO 1820 l\ lì-. \ David Norman I{iIIiam HiIt -t 8.4., University of Manitoba, L987 A Thesis Submitted in partial Fulfillment of the Reguírements for the Degree of Master of Arts at University of Manitoba Department of History 1994 Bibliothèque nationale I*I |f{onatt-iorav du Canada Acquisitions and Direction des acquisitions et Bibliographic Services Branch des services bibliog raphiques 395 Wellington Street 395, rue Well¡ngton Ottawa, Ontario Ottawa (Ontario) K1A ON4 K1A ON4 Yout file Votrc élérence Ou( l¡le Nolrc élércnce The author has granted an L'auteur a accordé une licence irrevocable non-exctusive licence irrévocable et non exclus¡ve allowing the National Library of permettant à la Bibliothèque Ganada to reproduce, loan, nationale du Canada de distribute or sell cop¡es of reprodu¡re, prêter, distribuer ou his/her thesis by any means and vendre des copies de sa thèse in any form or format, making de quelque manière et sous this thesis available to interested quelque forme que ce soit pour persons. mettre des exemplaires de cette thèse à la disposition des personnes intéressées. The author retains ownership of L'auteur conserve la propriété du the copyright in his/her thesis. droit d'auteur qu¡ protège sa Neither the thesis nor substantial thèse. Ni la thèse ni des extraits extracts from it may be printed or substantiels de celle-ci ne otherwise reproduced without doivent être imprimés ou his/her perm¡ss¡on. autrement reproduits sans son autorisation. ISBN 0-612-13190-4 C,anadä -
CU Cameco' Uranium
Sierra Club Canada’s Submisssions to CNSC Cameco’s proposed expansion of the world’s largest Uranium mines and mills in Northern Saskatchewan September 4, 2013 www.sierraclub.ca Acknowledgements Sierra Club Canada is a grassroots volunteer‐driven organization. Our most important work is accomplished by member‐volunteers. We would like to thank the following Sierra Club Canada staff and volunteers for their efforts in filing these submissions: • John Bennett, Executive Director, Sierra Club Canada, www.sierraclub.ca, • Isabelle Brunet, Executive Assistant, Sierra Club Canada, • Benny Cheng, B.Sc, Sierra Club Ontario, Green Energy Campaign, • Dale Dewar, MD, FCFP, Physicians for Global Survival, www.pgs.ca, • Christine Elwell, B.A., LL.B., LL.M., Sierra Club Ontario, Green Energy Campaign, • Jenn Elwell, B.A.,B.Ed.(expected), researcher and map specialist, • David Greenfield, Sierra Club CanadaPrairie Chapter, • D'Arcy Hande, The HUES3 Campaign, (Health Uranium Energy, Sustainability, Solidarity and Survival), www.cleangreensask.ca/Home/huesss‐campaign, • Rick Morrell, Executive Director, Saskatchewan Eco Network, www.econet.ca/, • Candyce and Marius Paul, Committee for Future Generations, http://committeeforfuturegenerations.wordpress.com/, and • Karen Weingeist, Coalition for a Clean Green Saskatchewan. Map Sources are acknowledged. SCC submission on the proposed Cameco expansion of the world’s largest uranium mines and mills. page 2 of 2 Table of Contents Acknowledgements ............................................................................................................................