Witchekan Lake First Nation Source Water Protection Plan
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Wollaston Road
WOLLASTON LAKE ROAD ENVIRONMENTAL IMPACT STATEMENT Biophysical Environment 4.0 Biophysical Environment 4.1 INTRODUCTION This section provides a description of the biophysical characteristics of the study region. Topics include climate, geology, terrestrial ecology, groundwater, surface water and aquatic ecology. These topics are discussed at a regional scale, with some topics being more focused on the road corridor area (i.e., the two route options). Information included in this section was obtained in full or part from direct field observations as well as from reports, files, publications, and/or personal communications from the following sources: Saskatchewan Research Council Canadian Wildlife Service Beverly and Qamanirjuaq Caribou Management Board Reports Saskatchewan Museum of Natural History W.P. Fraser Herbarium Saskatchewan Environment Saskatchewan Conservation Data Centre Environment Canada Private Sector (Consultants) Miscellaneous publications 4.2 PHYSIOGRAPHY Both proposed routes straddle two different ecozones. The southern portion is located in the Wollaston Lake Plain landscape area within the Churchill River Upland ecoregion of the Boreal Shield ecozone. The northern portion is located in the Nueltin Lake Plain landscape area within the Selwyn Lake Upland ecoregion of the Taiga Shield ecozone (Figure 4.1). (SKCDC, 2002a; Acton et al., 1998; Canadian Biodiversity, 2004; MDH, 2004). Wollaston Lake lies on the Precambrian Shield in northern Saskatchewan and drains through two outlets. The primary Wollaston Lake discharge is within the Hudson Bay Drainage Basin, which drains through the Cochrane River, Reindeer Lake and into the Churchill River system which ultimately drains into Hudson Bay. The other drainage discharge is via the Fond du Lac River to Lake Athabasca, and thence to the Arctic Ocean. -
The Archaeology of Brabant Lake
THE ARCHAEOLOGY OF BRABANT LAKE A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfilment of the Requirements for the Degree of Master of Arts in the Department of Anthropology and Archaeology University of Saskatchewan Saskatoon By Sandra Pearl Pentney Fall 2002 © Copyright Sandra Pearl Pentney All rights reserved. PERMISSION TO USE PERMISSION TO USE In presenting this thesis in partial fulfilment 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 in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis 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 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. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Anthropology and Archaeology University of Saskatchewan Saskatoon, Saskatchewan (S7N 5B 1) ABSTRACT Boreal forest archaeology is costly and difficult because of rugged terrain, the remote nature of much of the boreal areas, and the large expanses of muskeg. -
The Cultural Ecology of the Chipewyan / by Donald Stewart Mackay.
ThE CULTURAL ECOLOGY OF TkE CBIPE%YAN UONALD STEhAkT MACKAY b.A., University of british Columbia, 1965 A ThESIS SUBMITTED IN PAhTIAL FULFILLMENT OF THE HEObIRCMENTS FOR THE DEGREE OF MASTER OF ARTS in the department of Sociology and Anthropology @ EONALD STECART MACKAY, 1978 SIMON F hAShR UNlVERSITY January 1978 All rights reserved. This thesis may not be reproduced in whole or in, part, by photocopy or other means, without permission of the author. APPROVAL Name : Donald Stewart Mackay Degree: Master of Arts Title of Thesis: The Cultural Ecology of the Chipewyan Examining Cormnit tee : Chairman : H. Sharp Senior Supervisor- - N. Dyck C.B. Crampton . Fisher Departme'nt of Biological Sciences / ,y/y 1 :, Date Approved: //!,, 1 U The of -- Cultural Ecology .- --------the Chipewyan ----- .- ---A <*PI-: (sign-ir ~re) - Donald Stewart Mackay --- (na~t) March 14, 1978. (date ) AESTRACT This study is concerned with the persistence of human life on the edge of the Canadian Barren Grounds. The Chipewyan make up the largest distinct linguistic and cultural group and are the most easterly among the Northern Athapaskan Indians, or Dene. Over many centuries, the Chipewyan have maintained a form of social life as an edge-of-the-forest people and people of the Barren Grounds to the west of Hudson Bay. The particular aim of this thesis is to attempt, through a survey of the ecological and historical 1iterature , to elucidate something of the traditional adaptive pattern of the Chipewyan in their explcitation of the subarc tic envirorient . Given the fragmentary nature of much of the historical evidence, our limited understanding of the subarctic environment, and the fact that the Chipewyan oecumene (way of looking at life) is largely denied to the modern observer, we acknowledge that this exercise in ecological and historical reconstruction is governed by serious hazards and limitations. -
Requirements Department of Geography
A GEOGRAPHICAL STUDY OF· THE COMMERCIAL FISHING INDUSTRY IN NORTHERN SASKATCHEWAN: AN EXAMPLE OF RESOURCE DEVELOPMENT A Thesis Submitted to the Faculty of Graduate Studies in Partial FUlfilment of the Requirements for the Degree of Master of Arts in the Department of Geography by Gary Ronald Seymour Saskatoon, Saskatchewan . 1971. G.R. Seymour Acknowledgements The author is grateful to the many people in the Geography Department, University of Saskatchewan, in government and in the fishing industry who provided valuable information and advice in the preparation of this thesis. The author is particularly indebted to: Dr. J.H. I Richards and E.N. Shannon, Department of Geography, Univer�ity of Saskatchewan; G. Couldwell and P. Naftel, Fisheries Branch, Department of Natural Resources, Saskatchewan and F.M. Atton, Chief Biologist, Fisheries Branch, Department of Natural Resources, Saskatoon. Gratitude is also expressed to the Institute of Northern Studies, University of Saskatchewan whose financial assistance made collection of field data for this thesis possible. A special debt of gratitude is extended to my advisor, Dr. R.M. Bone of the Geography Department, University of Saskatchewan, whose willing direction and advice provided valuable assistance in the organization and writing of the thesis. i Table of Contents Page I. INTRODUCTION • • • • • • • • • • • • • • • • • • • • • 1 II. THE RESOURCE BASE • • • • • • • • • • • • • • • • • • 3 Factors Affecting Total Productivity •••••• 3 Methods of Commercial Fishing •••• • • • • • • 7 1) Summer -
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. -
Reindeer Lake) Area, Northeastern La Ronge Domain
Geology of the Birch Point (Reindeer Lake) Area, Northeastern La Ronge Domain Ralf 0. Maxeiner Maxeiner, R.O. ( 1998): Geology of the Birch Point (Reindeer Lake) area. northeastern La Ronge Domain; in Summary of Investigations 1998. Saskatchewan Geological Survey. Sask. Energy Mines, Misc. Rep. 98-4. In 1996, the Saskatchewan Geological Survey initiated Mineral Resources {Innes et al., 1964). Fox and a mapping project in the southern Reindeer Lake area, Johnston ( 1980) discussed the characteristics of a belt aimed at providing I :20 000 scale coverage of the "La of ultramafic rocks that cross the map sheet. An Ronge-Lynn Lake Bridge" (Maxeiner, 1996, 1997; aeromagnetic map of the Southend area at I :63,360 Harper, 1996, 1997; Corrigan et al., 1997). During the scale was issued in 1965. past summer, mapping between the 1996 and 1997 map sheets covered an approximately 340 km 2 area centered on Birch Point, Reindeer Lake, about 30 km northeast of Southend and 210 km northeast of the 2. General Geology town of La Ronge (Figure I). This year's map area offers a unique cross-section through the northwestern part of the Reindeer Zone, Mapping by the Geological Survey of Canada (GSC) at from the Central Metavolcanic Belt of the La Ronge I :50 000 was carried out in adjoining areas to the east Domain into the Burntwood Group of the Kisseynew and south (Corrigan et al., this volume), and also Domain (Figure I). From northwest to southeast the extended farther north as part of a regional study study area is underlain by the following supracrustal designed to enhance understanding of the lithotectonic assemblages (Figure 2): evolution of the northwestern Reindeer Zone within the Trans-Hudson Orogen. -
History of Mining in Saskatchewan
History of Mining In Saskatchewan Early Mining in Saskatchewan The earliest mining occurred when earth’s inhabitants started using various stones for tools or certain clays for cooking vessels. The earliest recorded occupation in Saskatchewan was around 9000 B.C. at the Niska site in the southern part of the province. Ample evidence of the use of stone tools, arrow heads, and spear heads, etc. has been found in the area. Much of the material used by these early inhabitants was imported or traded from other regions of North America. The study of the stone tools provides us with information about the people’s work, their history, their religion, their travels and their relationships with other groups or nations. Stone is readily available throughout most of Saskatchewan. This was especially important for Saskatchewan’s First Nations people who moved their camps frequently in search for food. The stones available were not all suitable for tools and they needed a constant supply of stone material that broke cleanly or was hard enough for pounding. Consequently, they made regular trips to the source areas or traded with people who lived near the sources. For these early residents of our province, the exchange of goods was more than just a means of acquiring things. Bartering and gift exchange was a means of creating and reinforcing relationships between individuals, families and nations. For thousands of years, goods have been exchanged through networks that extended across North America. Although perishable goods were also traded, our records are in the form of shell or stone artefacts. -
Lawrence Bay Lodge on Reindeer Lake, Saskatchewan
Lawrence Bay Lodge on Reindeer Lake, Saskatchewan Lawrence Bay Airways & Outposts 2020 www.lawrencebay.com 701-262-4560 www.lawrencebay.com • 701-262-4560 Original Lodge built in 1971. Lodge today, 2020. OUR 50TH YEAR I owe a lot of our success at Lawrence Bay Lodge to my late wife, Verdean, who stuck by me in the early, lean years and supported all my crazy ideas. Our success in the future will be on the shoulders of my son and daughter, working with me. They have both grown up at Lawrence Bay Lodge and together have more experience in the business than anyone I know. By initiating catch and release in 1981, we have insured our fantastic fishing for the future. Quality of fishing at Lawrence Bay Lodge is as good now as it was in 1971. Thanks to our wonderful guests and excellent staff that have helped make this all possible. Your Hosts, Mindy, Phil and Randy www.lawrencebay.com • 701-262-4560 WHY CHOOSE LAWRENCE BAY LODGE FOR YOUR FISHING & HUNTING CAMP? Reindeer Lake is one of the most productive lakes in the north because it drains a very large portion of northeast Saskatchewan and northwest Manitoba; consequently the food source for gamefish is very good, better than most of the smaller lakes. The proof is in the fish! At Reindeer Lake and the surrounding outpost camps, you will find that the Northern Pike, Lake Trout, and Walleyes in our area are very heavy for their length, with the smaller heads and large stocky bodies. The lakes in our area have a large number of islands with many bays and large wood flats for big Northern Pike. -
The Six Seasons of the Woodland Cree: a Lesson to Support Science 10
The Six Seasons of the Woodland Cree: A Lesson to Support Science 10 by Duane Johnson 2008 Teaching Materials from the Stewart Resources S106.22 Centre These lessons were developed by the following team of teachers, Elders, and cultural advisors: Yvonne Chamakese, David Hlady, Anna-Leah King, Duane Johnson, Marcia Klein, Lana Lorensen, Sally Milne, Joseph Naytowhow, Lamarr Oksasikewiyin, Stuart Prosper, Ron Ray, Ted View, John Wright, and Laura Wasacase. Support was provided by Dean Elliott from the Ministry of Education, and Margaret Pillay from the Saskatchewan Professional Development Unit. All resources used in these lessons are available through the Stewart Resources Centre: http://www.stf.sk.ca/services/stewart_resources_centre/online_catalogue_unit_plans/index .html Information regarding the protocol when inviting Elders into the classroom can be found in the document: Elders in the Classroom by Anna-Leah King (attached as Appendix A). Further information can be found in the Saskatchewan Learning document: Aboriginal Elders and Community Workers in Schools. Table of Contents Overview ......................................................................................................................... 4 Foundational Objectives.................................................................................................. 4 Timeframe .......................................................................................................................4 Resources .......................................................................................................................4 -
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. -
From the Bush to the Village in Northern Saskatchewan: Contrasting CCF Community Development Projects"
CORE Metadata, citation and similar papers at core.ac.uk Provided by Érudit Article "From the Bush to the Village in Northern Saskatchewan: Contrasting CCF Community Development Projects" David M. Quiring Journal of the Canadian Historical Association / Revue de la Société historique du Canada, vol. 17, n° 1, 2006, p. 151-178. Pour citer cet article, utiliser l'information suivante : URI: http://id.erudit.org/iderudit/016106ar DOI: 10.7202/016106ar Note : les règles d'écriture des références bibliographiques peuvent varier selon les différents domaines du savoir. Ce document est protégé par la loi sur le droit d'auteur. L'utilisation des services d'Érudit (y compris la reproduction) est assujettie à sa politique d'utilisation que vous pouvez consulter à l'URI https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Érudit est un consortium interuniversitaire sans but lucratif composé de l'Université de Montréal, l'Université Laval et l'Université du Québec à Montréal. Il a pour mission la promotion et la valorisation de la recherche. Érudit offre des services d'édition numérique de documents scientifiques depuis 1998. Pour communiquer avec les responsables d'Érudit : [email protected] Document téléchargé le 9 février 2017 10:21 From the Bush to the Village in Northern Saskatchewan: Contrasting CCF Community Development Projects DAVID M. QUIRING Abstract The election of the CCF in 1944 brought rapid change for the residents of northern Saskatchewan. CCF initiatives included encouraging northern aboriginals to trade their semi-nomadic lifestyles for lives in urban settings. The establishment of Kinoosao on Reindeer Lake provides an example of how CCF planners established new villages; community development processes excluded local people. -
Following the Oberholtzer-Magee Expedition, by David F. Pelly
246 • REVIEWS Yoo, J.C., and D’Odorico, P. 2002. Trends and fluctuations in the likely caribou crossings and waited, the Dene [Chipewyan] dates of ice break-up of lakes and rivers in northern Europe: The were more inclined to simply follow the caribou in their effect of the North Atlantic Oscillation. Journal of Hydrology migration, not unlike a pack of wolves” (p. 64). The hostil- 268:100–112. ity between them made it difficult for anyone to find a guide Zhang, X., Vincent, L.A., Hogg, W.D., and Niitsoo, A. 2000. to conduct him through the territory. Temperature and precipitation trends in Canada during the Pelly does a kind of time-travel through the history of the 20th century. Atmosphere-Ocean 38:395–429. area, going back to the time of Samuel Hearne in the 18th century and up to the descriptions of Bill Layman, who is Thomas Huntington still canoeing the area today. The narrative ranges from the Bigelow Laboratory for Ocean Sciences mid-19th century, when the Roman Catholic mission was 180 McKown Point Rd. established in the village of Brochet at the head of Reindeer West Boothbay Harbor, Maine 04575, USA Lake, to the travels of American P.G. Downes, who in 1939 [email protected] covered some of the same route traveled by Oberholtzer and Magee 27 years earlier. Pelly traces centuries of nomadic movement of the Chipewyan, the Inuit, and the Cree as they The Old Way North: following the Ober- followed the caribou across the land, sometimes in co-op- holtzer-Magee expedition.