7 Bar L. Hereford Ranch Moose Creek, MB November 22, 1961
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Chapter 4 – Project Setting
Chapter 4 – Project Setting MINAGO PROJECT i Environmental Impact Statement TABLE OF CONTENTS 4. PROJECT SETTING 4-1 4.1 Project Location 4-1 4.2 Physical Environment 4-2 4.3 Ecological Characterization 4-3 4.4 Social and Cultural Environment 4-5 LIST OF FIGURES Figure 4.1-1 Property Location Map ......................................................................................................... 4-1 Figure 4.4-1 Communities of Interest Surveyed ....................................................................................... 4-6 MINAGO PROJECT ii Environmental Impact Statement VICTORY NICKEL INC. 4. PROJECT SETTING 4.1 Project Location The Minago Nickel Property (Property) is located 485 km north-northwest of Winnipeg, Manitoba, Canada and 225 km south of Thompson, Manitoba on NTS map sheet 63J/3. The property is approximately 100 km north of Grand Rapids off Provincial Highway 6 in Manitoba. Provincial Highway 6 is a paved two-lane highway that serves as a major transportation route to northern Manitoba. The site location is shown in Figure 4.1-1. Source: Wardrop, 2006 Figure 4.1-1 Property Location Map MINAGO PROJECT 4-1 Environmental Impact Statement VICTORY NICKEL INC. 4.2 Physical Environment The Minago Project is located within the Nelson River sub-basin, which drains northeast into the southern end of the Hudson Bay. The Minago River and Hargrave River catchments, surrounding the Minago Project Site to the north, occur within the Nelson River sub-basin. The William River and Oakley Creek catchments at or surrounding the Minago Project Site to the south, occur within the Lake Winnipeg sub-basin, which flows northward into the Nelson River sub-basin. The topography in these watersheds varies between elevation 210 and 300 m.a.s.l. -
Wallace Mining and Mineral Prospects in Northern
r Geology V f .ibrary TN 27 7A3V/1 WALLACE MINING AND MINERAL PROSPECTS IN NORTHERN MANITOBA THE LIBRARY OF THE UNIVERSITY OF CALIFORNIA LOS ANGELES University of British Columbia D. REED LIBRARY The RALPH o DEPARTMENT OF GEOLOGY UNIVERSITY OF CALIFORNIA LOS ,-XGELES, CALIF. Northern Manitoba Bulletins Mining and Mineral Prospects in Northern Manitoba BY R. C. WALLACE PUBLISHED BY AUTHORITY OF GOVERNMENT OP MANITOBA OFFICE OF COMMISSIONER OF NORTHERN MANITOBA The Pas, Manitoba Northern Manitoba Bulletins Mining and Mineral Prospects in Northern Manitoba BY R. C. WALLACE PUBLISHED BY AUTHORITY OF GOVERNMENT OF MANITOBA OFFICE OF COMMISSIONER OF NORTHERN MANITOBA The Pas, Manitoba CONTENTS Chapter Page I. Introductory 5 II. Geological features ... 7 III. History of Mining Development 12 IV. Metallic Deposits: (A) Mineral belt north of The Pas .... 20 (1) Flin Flon and Schist Lake Districts. .... ....20 (2) Athapapuskow Lake District ..... ....27 (3) Copper and Brunne Lake Districts .....30 (4) Herb and Little Herb Lake Districts .... .....31 (5) Pipe Lake, Wintering Lake and Hudson Bay Railway District... 37 (B) Other mineral areas .... .....37 V. Non-metallic Deposits 38 (a) Structural materials 38 (ft) Fuels 38 (c) Other deposits. 39 VI. The Economic Situatior 40 VII. Bibliography 42 Appendix: Synopsis of Regulations governing the granting of mineral rights.. ..44 NORTHERN MANITOBA NORTHERN MANITOBA Geology Library INTRODUCTORY CHAPTER I. INTRODUCTORY Scope of Bulletin The purpose of this bulletin is to give a short description of the mineral deposits, in so far as they have been discovered and developed, in the territory which was added to the Province of Manitoba in the year 1912. -
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province -
Bedrock Geology Compilation Map Series: Grand Rapids NTS
Manitoba Industry, Trade and Mines Geological Survey MARGINAL NOTES B.G.C.M. Series Grand Rapids, NTS 63G, 1:250 000 The Grand Rapids map sheet (NTS 63G) is underlain by Paleozoic carbonate formations, with the QUATERNARY exception of minor Precambrian bedrock exposures in the northeast corner. The Paleozoic strata Pervasive glacial erosion carved the Grand Rapids area into an outcrop-dominated landscape. Sediment O O represent a portion of the northeastern flank of the Williston Basin and dip gently to the southwest. Recent 100 0 O 98 0 4 000 ’ 0 ’ 0 5 000 cover is restricted to the south along The Pas Moraine and, most likely, to the area north of Lake 50 30 99 0 30 50 glaciation has modified the exposed Paleozoic bedrock. The rocks outcrop in a region known as the O O Interlake, and the Grand Rapids area is where many of Manitoba's caves and karst features are located. Winnipeg, where peatlands dominate. No information is available within the area regarding preLate 54 0 54 0 LEGEND ISOPACH MAPS STRUCTURE CONTOUR MAPS SML Wisconsinan glaciation, although multiple glacial striations and discontinuous older sediments may be SA N The map sheet is blanketed by up to 60 m of glacial till, lake sediments and glacial outwash deposits (see SA present. SA 'Surficial Geology' and 'Overburden Thickness' inset maps). The north basin of Lake Winnipeg occupies N Little Playgreen WESTERN CANADA SEDIMENTARY BASIN McMartin (2000) documented two late Wisconsinan glacial advances in the Flin Flon area, first towards SML Lake a significant portion of the sheet. -
Lake Diefenbaker: the Prairie Jewel
Journal of Great Lakes Research 41 Supplement 2 (2015) 1–7 Contents lists available at ScienceDirect Journal of Great Lakes Research journal homepage: www.elsevier.com/locate/jglr Lake Diefenbaker: The prairie jewel Introduction with intakes that are 34 m below FSL. The proportion of inflowing water that flows out of Gardiner Dam varies from ~70% in low flow years (e.g., 2001 average flow was 84 m3 s−1)toover97%inhigh fl 3 −1 Fighting drought with a dam: Lake Diefenbaker, the reservoir of ow years (e.g., 2005; 374 m s ; Hudson and Vandergucht, 2015) fl life-giving water.CBC's Norman DePoe. with a median proportional out ow of ~94%. Additional water losses in- clude net evaporation, which can represent over 10% in dry years, irriga- On the broad expanse of flat land of the northern Great Plains of tion, and direct use from the reservoir. From the Qu'Appelle Dam, Lake Canada lies a large, narrow, river-valley reservoir, Lake Diefenbaker. Diefenbaker water is transferred out of the natural catchment and re- The reservoir was developed for multiple benefits including the irriga- leased down the Qu'Appelle River to supply southern regions of the tion of ~2000 km2 of land in Central Saskatchewan, the generation of province. With a mean depth of 22 m, the water residence time, though hydroelectricity, a source of drinking water, flood control, water for in- variable, is typically just over a year (Donald et al., 2015; Hudson and dustry and livestock, and recreation. This semi-arid region has an aver- Vandergucht, 2015). -
Copyright © November 2018 Erin Yaremko
Failed Partnership to Future Partnership: An Examination of Social Impacts Moving from Institutional Failure to Partner with Indigenous Communities to a New Model of Partnership A Thesis submitted to the Faculty of Graduate Studies of The University of Manitoba In partial fulfilment of the requirements of the degree of MASTER OF ARTS Department of History University of Manitoba Winnipeg Copyright © November 2018 Erin Yaremko 0 Acknowledgement of Treaty Territory and Positionality I acknowledge that I reside and work on treaty 1 and treaty 5 territory, the traditional territories of the Anishinaabeg (Ojibway), Muskeko-ininiwak (Cree), Dakota and Nakota peoples, and the homeland of the Red River Métis Nation. As a settler descendant I acknowledge the continuation of modern colonial barriers First Nations continue to face, and am consciously aware of the white privilege I carry. I commit myself to building reciprocal partnerships and alliances to further the growth of the Indigenous perspective in historical source. I come to this research and work with anticolonial, anti-racist world views and commit myself to furthering my own personal growth and understanding of Indigenous methodology and world views through continual alliance with each Nation I am fortunate to partner with. My early upbringing through inner city volunteer positions and further work in areas of social justice facilitated the growth of my passion for social justice-based research and work in partnership with other cultural groups. Past work in partnership with the Japanese Canadian based project Landscapes of Injustice helped foster my understanding of large social justice- based research projects. Work in partnership with the Japanese Manitoban and Japanese Saskatchewan communities furthered my understanding of colonization in Canada and the trauma caused by western society. -
NOR-MAN Regional Health Authority 2009/2010 Community Health Assessment Report
NOR-MAN Regional Health Authority Community Health Assessment Report April 2010 Principal Authors: Catherine Hynes, Regional Manager Decision Support Susan Lockhart, Executive Director of Planning, Research & Development Jamie Simard, Decision Support - Administrative Data Entry / Programmer Dr. Lawrence Elliott, Medical Officer of Health NOR-MAN Regional Health Authority 84 Church Street Flin Flon, Manitoba R8A 1L8 Telephone: (204) 687-1338 Fax: (204) 687-6405 E-mail: [email protected] Website: www.norman-rha.mb.ca A Message from Vivian McKenzie Board Vice-Chair A Message to the Region In accordance with Section 23(2B) of the Regional Health Authorities Consequential Amendment Act, I am pleased to present, on behalf of the Board of Directors of the NOR-MAN Regional Health Authority, a copy of NOR-MAN Regional Health Authority’s 2009/2010 Community Health Assessment. Over one year ago, the NOR-MAN Regional Health Authority Board of Directors appointed the NRHA Community Health Assessment Advisory Committee to complete a comprehensive Community Health Assessment for the region. Building on the work that has been done since the RHA’s inception in 1997 and NRHA’s second comprehensive Community Health Assessment completed in 2004, the goal of the project was to provide a solid base of facts and data to guide future decision-making in the region. Both the Community Health Assessment process and report will assist the NOR-MAN Regional Health Authority’s planning process and form the basis for the development of our NRHA’s 2011 - 2016 Strategic Plan. We hope you find the information useful and we encourage our community partners to use the information for your own planning purposes. -
Moose Lake Settlement Agreement 1990
.. ' \ (fi"'. THIS AGREEMENT made as of this day of 1990. BETWEEN: MOOSE LAKE BAND OF INDIANS as represented by the Chief, Jim Tobacco, and Band Councillors, being Lloyd Easter, John Martin, Sam Ettawakapow, and James Ettawakapow, (hereinafter referred to as the "Band") OF THE FIRST PART, and MOOSE LAKE COMMUNITY COUNCIL, as represented by the Mayor, Ted Bercier and Community Councillors being Francis McKay, John Mercredi, Edward Head, Ralph Buck, ,I"" Patrick Ballantyne, Sr. \_- (Moose Lake Community Council hereinafter referred to as the "Community") OF THE SECOND PART, - and - # MANITOBA HYDRO ELECTRIC BOARD, {hereinafter referred to as "Hydro") OF THE THIRD PART. WHEREAS Hydro built the Project, as hereinafter defined, the construction of which caused the substantial alteration of the water regime on local waterways, including Moose Lake, while providing ongoing benefits to the people of Manitoba through the revenues generated therefrom; ,. " 2 AND WHEREAS there is a continuing impact from such substantial alteration; AND WHEREAS the Government of Manitoba (hereinafter referred to as "Manitoba") and the Government of Canada (hereinafter referred to as "Canada") participated with Hydro in arranging for the management of the ~mpact of the said Project on the Moose Lake Cree; AND WHEREAS the construction of the Project also caused the loss of land and other property of the Moose Lake Cree; AND WHEREAS the loss and taking of such land led to the partial relocation of the Band and the Community in the area of Moose Lake, Manitoba, as well -
Moose Lake March 24, 1956 Mr. Foster Chalmers the Pas, Manitoba Dear Foster
Moose Lake March 24, 1956 Mr. Foster Chalmers The Pas, Manitoba Dear Foster: Mrs. Lamb and I are down here for a couple of weeks visiting Jock and Carol. It is so restful and quiet compared to our busy Pas office, with two telephones ringing and travelers of all description in and out all day. I visit the cattle ranch every other day. Those forty calves and the hundred head of older stuff are much easier to look at at oat chop time than some of the impatient which men that storm around the office wanting to go to Noak Lake or Winisk or James Bay. We thoroughly enjoyed the very pleasant evening spent at your house, even if Eric Law and Dr. Harwood did get into heated argument who has the best cottage at the lake. I never get a chance to write any of my friends while in The Pas. In fact, this is the first letter I have ever written you. I have read all the magazines around here and at the Seven Bar L. Might get started on the Old Testament as we have only a bi-monthly mail here. Only having two winters schooling you will excuse the spelling and composition. If I had ever got out of grade three, I sure as hell would have been in grade four. Norman McKenzie also went to school here. My brother Eric says he remembers the day Norman went to school. I must be getting better as I feel like doing something so will ramble along to you and call this letter “Land Marks in Memories”. -
University of Manitoba Winnipeg, Manitoba May 1980 RELOCATION and SOCIAL CHANGE AMONG THE
RELOCATION AND SOCTAL CHANGE A}4ONG THE ST{AMPY CREE AND METIS OF EASTERVTLLE, MANITOBA JAMES B. WALDRAM A THESTS SUBMITTED TO THE FACULTY OF GRADUATE STUDTES ÏN PARTÏAL FULFILLMENT OF THE REQUTREMENTS FOR THE DEGREE OF MASTER OF ARTS Department of Anthropology University of Manitoba Winnipeg, Manitoba May 1980 RELOCATION AND SOCIAL CHANGE AMONG THE SI^IAMPY CREE AND METIS OF EASTERVILLE, t'lAN IT0BA BY JAMES BURGESS WALDRAM A thesis submitted to the Faculty of Graduate Studies of the University of Manitoba in partial fulfillment of the requirements of the degree of MASTER OF ARTS .jo 1980 Fernrission has been granted to the LIBRARY OF THE UNIVER- SITY OF MANITOBA to lend or sell copies of this thesis, to the NATIONAL LIBRARY OF CANADA to nricrofilnr this thesis and to lend or sell copies of the film, and UNIVERSITY MICROFILMS to publish an abstract of this thesis. The author reserves other publication rights, and neither the thesis nor extensive extracts from it may be printed or other- wise reproduced without the author's written permission. êBFTFêgT. In J,964r â coflllTlunity of Swampy Cree and Metis in Northern Manitoba was forced to relocate when a hydro- electric dam constructed nearby caused a rise in the lake leve1 which flooded out the community. In order to effect the relocation, the l"lanitoba government created an administrative body, known as the Forebay Committee. The purpose of this thesis is to examine the long-term consequences of the relocation for the people involved, and to evaluate the effectiveness of the Forebay Committee in planning and executing this relocat,ion. -
Manitoba, Canada
2019 REGIONAL TRAVEL GUIDE NORTH MB Manitoba, Canada north.travelmanitoba.com Digital. Agile. Transformative. Our people leverage data and technology to solve problems and build a better tomorrow. Vale.com NORTHERN MANITOBA It is a region of the province that is vast and Going back thousands of years, Indigenous mostly untouched, where the waterways have people thrived off this land – its fauna and flora carved their place through the rocks and providing the necessities for survival. With arrival the forests provide refuge to an abundance of the Europeans in 1612 and the development of wildlife. But for those who seek a deeper of the fur trade, Manitoba’s North and its connection, they’ll find the land holds Indigenous people paved the way for a thriving the stories of Indigenous people and the enterprise in commerce that would influence communities here shine with the legends the entire history of the province. The next wave of the past and the potential of the future. of explorers to hit the North were prospectors, Northern Manitoba is a region that stretches as this ancient landscape held treasures from the 53rd parallel to the northern border beneath its surface. Towns were established with Nunavut and the shores of Hudson Bay. and populations grew as mining was a top The landscape here shifts from the coniferous industry for decades. Today, the communities forests of the Canadian Shield, to muskeg – have diversified and are welcoming visitors to boggy land characterized by surface water discover their unique charms and proximity to and slowly decomposing plants – to tundra, incredible wilderness and natural settings. -
Rags to Riches”
“RAGS TO RICHES” Leo Pettipas Manitoba Archaeological Society At the height of the last Ice Age around 18,000 years ago, all of Manitoba was covered by an ice cap some 1,200 metres thick. The weight of this massive burden pushed the underlying land surface downward, in much the same way that the surface of a cushion will sink when someone sits on it. Eventually, the ice sheet began to melt, and by about 7,500 years ago, it had all but disappeared from Manitoba. At first, the melting was especially rapid around the southern margins of the glacier; the last area to become ice-free was the North country around Hudson Bay. In other words, the southern portions of the province became ice-free first, and more and more of the land was released from the pressure of the ice as its edge melted ever northward and the glacier got smaller and smaller over time. The disappearance of the ice sheet gave rise to a process that scientists refer to as “crustal rebound.” Ever since it became free of its glacial burden, the surface of the earth’s crust in the North has been “rebounding” upward toward its original, pre-glacial elevation – just as the cushion will rise upward to its original height after the person gets up off it. Crustal rebound had a strong influence on the natural and human history of the major lakes and rivers that inherited the region from the now-extinct Lake Agassiz. For example, after that great lake disappeared, the Saskatchewan River flowed into Cedar Lake, just as it does now.