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Diavik's Northern Business Commitment
Diavik’s Business Commitment Northern Partners, Northern Success Diavik’s Northern Business Commitment Very early in the development of the Diavik Diamonds As of September 30, 2001, Diavik Diamond Mines Inc. Project, we recognized the importance that a project like ours had awarded to northern companies some $650 million would have on Canada's North, in particular the Northwest of the $850 million value of our contracts. Within the Territories and West Kitikmeot Region of Nunavut. We northern dollar figure, Aboriginal joint ventures therefore committed ourselves to supporting northern accounted for over $450 million, or three quarters of economic development through the provision of meaningful northern spending. training, employment and business opportunities. Diavik When we imagine what may lay beyond the Diavik further expressed its commitments through a Socio-Economic Diamond Mine, we see Diavik Diamond Mines Inc. as Monitoring Agreement with the Government of the Northwest having played an important part in contributing to a Territories and through five Participation Agreements with our northern business community with more capacity, neighbouring Aboriginal communities. broader business reach, and greater economic prosperity. On the business side, we have taken a number of steps to make The pages that follow showcase some of the many our commitments a reality. We have embedded our northern businesses participating in the Diavik commitments in our corporate culture through the Diamonds Project. They, and so many others, have been development of a Northern Business Participation Policy, our welcome and able partners in providing meaningful which expresses our commitment to support northerners in opportunities for northern business development and developing long-lasting and sustainable business capabilities. -
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. -
Compendium of Research in the Northwest Territories 2014
Compendium of Research in the Northwest Territories 2014 www.nwtresearch.com This publication is a collaboration between the Aurora Research Institute, the Department of Environment and Natural Resources, Fisheries and Oceans Canada and the Prince of Wales Northern Heritage Centre. Thank you to all who submitted a summary of research or photographs, and helped make this publication possible. Editor: Ashley Mercer Copyright © 2015 ISSN: 1205-3910 Printed by Aurora Research Institute Foreword Welcome to the 2014 Compendium of Research in the Northwest Territories. This year marked a special anniversary for the Aurora Research Institute and northern research. Fifty years ago, the Inuvik Research Laboratory was built and has served as a hub for research in the western arctic ever since. The Lab, as it was known, was first built as an initiative of the Canadian federal government in the newly established community of Inuvik. It remains on the same site today, but in 2011, a new modern multi-purpose facility opened to continue to support research in the north. We have included a brief history of the Lab and its impact in this edition of the Compendium to mark its long lasting importance to many researchers and community members. As part of the 50th anniversary celebration, the Aurora Research Institute team undertook a full set of NWT-wide celebrations. We celebrated the history, capacity and growth of research in the NWT that touched all corners of the territory and beyond. We honoured the significant scientific contributions that have taken place in the NWT over the past 50 years, and the role of NWT researchers, technicians and citizens in these accomplishments. -
2018 Yellowknife Geoscience Forum Abstract and Summary Volume
2018 Abstract and Summary Volume Cover photograph Carcajou River, NWT; Viktor Terlaky, Senior Petroleum Geologist at the Northwest Territories Geological Survey The picture was taken following a rainstorm along Carcajou River, NWT, which resulted in a spectacular rainbow across the river valley. In the background are outcrops of the Late Devonian Imperial Formation, interpreted to be submarine turbidite deposits. The light bands are sandstone bodies intercalated with the darker shale intervals, representing periodic activity in sedimentation. Compiled by D. Irwin, S.D. Gervais, and V. Terlaky Recommended Citation: Irwin, D., Gervais, S.D., and Terlaky, V. (compilers), 2018. 46th Annual Yellowknife Geoscience Forum Abstracts; Northwest Territories Geological Survey, Yellowknife, NT. YKGSF Abstracts Volume 2018. - TECHNICAL PROGRAM - 2018 YELLOWKNIFE GEOSCIENCE FORUM ABSTRACTS AND SUMMARIES I Contents ordered by first author (presenting author in bold) Abstracts – Oral Presentations IBAS – to Regulate or Not: What is the Rest of Canada Doing? Abouchar, J. .......................................................................................................................... 1 Seabridge Discovers New Gold Zones at Courageous Lake Adam, M.A. ........................................................................................................................... 1 Gold Mineralisation at the Fat Deposit, Courageous Lake, Northwest Territories Adam, M.A. .......................................................................................................................... -
Ancient Knowledge of Ancient Sites: Tracing Dene Identity from the Late Pleistocene and Holocene Christopher C
11 Ancient Knowledge of Ancient Sites: Tracing Dene Identity from the Late Pleistocene and Holocene Christopher C. Hanks The oral traditions of the Dene of the Mackenzie Valley contain some intriguing clues to cul tural identity associated with natural events that appear to have occurred at the end of the Pleisto cene and during the early Holocene. The Yamoria cycle describes beaver ponds that filled the ancient basins of postglacial lakes, while other narratives appear to describe the White River ash fall of 1250 B.P. This paper examines Dene views of the past and begins the task of relating them to the archaeological and geomorphological literature in an attempt to understand the cultural per spectives contained in these two different views of “history.” STORIES, NOT STONE TOOLS, UNITE US The Chipewyan, Sahtu Dene, Slavey, Hare, Mountain Dene, Dogrib, and Gwich’in are the Athapaskan-speaking people of the Northwest Territories. Collectively they refer to themselves as the Dene. Their shared cultural identity spans four distinct languages and four major dialects, and is spread from Hudson's Bay to the northern Yukon. Based on archaeological culture histories, there are relatively few strands of evidence that suggest a close relationship between these groups (Clark 1991; Hanks 1994). However, by using oral traditions, the archaeological record, linguistic theories, and the geological record, it can be argued that in the distant past the ancestors of the Dene lived as one group in the mountains along the Yukon-Alaskan border (Abel 1993: 9). For some archaeologists, the Athapaskan arrival east of the Cordilleran is implied by the appearance of a microlithic technology 6000-5000 B.P. -
OROGRAPHY 11 Just North of Edmonton a Height of Land Turns the Waters to Flow North Into the Great Mackenzie River, Over 2,500 M
OROGRAPHY 11 Just north of Edmonton a height of land turns the waters to flow north into the great Mackenzie river, over 2,500 miles long, whose valley with its low elevation above the sea is the outstanding feature of the Northwest Territories. In this watershed the terrain becomes less smooth with prominent elevations in the Caribou, Horn, and Franklin mountains and the clay soils of the prairies give way to more of sand and gravel. Great Slave and Great Bear lakes, each half as large again as lake Ontario and less elevated above the sea than lake Erie, are notable features; north and east of these two great lakes the country comes within the Canadian Shield* and the rock with some shallow overburden slopes gently down to the Arctic ocean without any large uplifts to break the monotony. Going east again, in the more northerly part there is encountered the orographical influence of Hudson bay which, indenting the continent so deeply and with rivers running in from west, south, and east, has an enormous drainage basin mainly in Manitoba, Ontario, and Quebec. Practically all of this great basin, excepting the Nelson River drainage, is included in the Canadian Shield, the surface characteristic of which is hard rock either exposed or overlain with shallow soil generally confining agriculture to the valleys or small basins. With only small areas in northeastern Quebec rising above 2,000 feet in elevation, there are no great eminences, but the surface is generally accidented by many hills and hollows with countless numbers of lakes and streams. -
Yellowknife Periphery Area Région Périphérique De Yellowknife Public Engagement Summary Report Rapport Sur La Consultation Publique November 2016 Novembre 2016
RECREATION MANAGEMENT PLANIFICATION DE LA GESTION PLANNING DES ACTIVITÉS RÉCRÉATIVES Yellowknife Periphery Area Région périphérique de Yellowknife Public Engagement Summary Report Rapport sur la consultation publique November 2016 Novembre 2016 Acknowledgements The Government of the Northwest Territories would like to acknowledge and thank those who took the time to participate in focus groups, complete surveys, attend the open house, or submit written comments. The local knowledge shared at these various public engagement events will inform the decisions to be made about recreation management and make them relevant to the Yellowknife area. Photo Credits Cover photo: Courtesy of the GNWT All other photos: Dillon Consulting Ltd. Table of Contents Executive Summary 1 Introduction ................................................................................................................................................. 5 1.1 Public Engagement Objectives ...................................................................................................................................... 5 1.2 Project Information ........................................................................................................................................................... 6 2 Public Engagement Methods .................................................................................................................. 7 2.1 On-Line Engagement ........................................................................................................................................................ -
A Guide to Mineral Deposits NORTHWEST TERRITORIES 2007 a Guide to Mineral Deposits
A GUIDE TO MINERAL DEPOSITS NORTHWEST TERRITORIES 2007 A Guide to Mineral Deposits of the Northwest Territories Minerals, Oil and Gas Division Department of Industry, Tourism and Investment Government of the Northwest Territories November 2007 Edited by: Christy Campbell Published by: Minerals, Oil and Gas Division Department of Industry, Tourism and Investment Government of the Northwest Territories November 2007 Available from: Minerals, Oil and Gas Division Department of Industry, Tourism and Investment Government of the Northwest Territories 9th Floor, Scotia Centre 600, 5102-50th AVE YELLOWKNIFE NT X1A 3S8 www.iti.gov.nt.ca/mog/index.htm Cover Description: Photos courtesy of Diavik Diamond Mines Inc. and John Veevaert of Trinity Mineral Company. Note: This publication supersedes earlier editions of A Guide to Mineral Deposits of the Northwest Territories, published by Minerals, Oil and Gas Division, Department of Industry, Tourism and Investment, Government of the Northwest Territories. Table of Contents Introduction .................................................................................................................................................. 1 GOLD PROPERTIES .................................................................................................................................. 4 Miramar Con Mine ....................................................................................................................................... 6 Miramar Giant Mine .................................................................................................................................... -
Mobile Core Bathurst Caribou Management Zone
Mobile Core Bathurst Caribou Management Zone The Mobile Core Bathurst Caribou Management Zone exists as a wildlife management zone for barren-ground caribou under the Wildlife Act. You must not hunt inside this zone. How do I find out the boundaries of the Mobile Zone? • Get the most recent map. The map is updated every Thursday. You can get a map from: o Gordon Lake station o McKay Lake check station o Your local or regional ENR office o Your local band, community, government or organization office o ENR North Slave Region FaceBook page https://www.facebook.com/enrnorthslaveregion/ o ENR website http://www.enr.gov.nt.ca/en/services/mobile-core-bathurst-caribou- management-zone • Download the most recent .gpx file for your GPS device to plot the zone boundary at http://www.enr.gov.nt.ca/en/services/mobile-core-bathurst-caribou-management-zone What happens if I’m caught harvesting inside the Mobile Zone? • An officer will investigate the scene. • If the officer determines that the caribou may have been harvested illegally, they will seize the caribou meat. • The officer may ask for a voluntary statement from you for the investigation file. • The officer will write up a violation report, and after an investigation is under way, you will be told the next steps. • If the investigation indicates there has been an illegal harvest in the Mobile Zone, a charge will be laid and you will get a date for a court appearance. • If the officer seizes your meat and ENR is not able to store the meat until the court process is complete: o The officer will write up a disposition order to decide who will receive the meat. -
Yellowknife Geoscience Forum
2016 Yellowknife Geoscience Forum Abstract and Summary Volume Cover photograph Mackenzie Mountains foothills, NWT; Viktor Terlaky, Senior Petroleum Geologist at the Northwest Territories Geological Survey The picture was taken near the Arctic Red River and shows river cuts and thaw slumps in the Peel Plateau area. Old meets new: the river cuts expose Devonian and Cretaceous strata, some of which are the target of investigation as potential unconventional hydrocarbon plays; thaw slumps are caused by permafrost melting and are interpreted to be the consequence of climate change. Compiled by D. Irwin, S.D. Gervais, and V. Terlaky Recommended Citation: Irwin, D., Gervais, S.D., and Terlaky, V. (compilers). 2016. 44th Annual Yellowknife Geoscience Forum Abstracts; Northwest Territories Geological Survey, Yellowknife, NT. YKGSF Abstracts Volume 2016. - TECHNICAL PROGRAM - 2016 YELLOWKNIFE GEOSCIENCE FORUM ABSTRACTS AND SUMMARIES Contents ordered by first author (presenting author in bold) Abstracts - Oral Presentations Qilalugaq Diamond Project, Nunavut – A Unique Locality for Rare ‘Canary’ Yellow Diamonds. Armstrong, K.A. ................................................................................................................................ 1 Insights into Gold Mineralization at the Yellowknife City Gold Project using Synchrotron X-Ray Spectroscopy. Banerjee, N.R., Van Loon, L.L., Gordon, S., Lu, L., Bajwa, C., Flynn, T., Sexton, A., Setterfield, T., Campbell, J., and Carpenter, R. .................................................................................................... -
The Evolution of Inuvialuit Identity in the Modern
inuvialuit rising: the evolution of inuvialuit identity in the modern era Natasha Lyons Department of Archaeology, Simon Fraser University, 8888 University Drive, Burnaby, BC V5A 1S6, Canada; [email protected] abstract The Inuvialuit of the western Canadian Arctic were recognized by the government of Canada as the traditional owners and formal stewards of their territory by the Inuvialuit Final Agreement of 1984. During the pursuit of this claim, its progenitors replaced the Western term ‘Mackenzie Inuit’ with the Inuvialuktun term ‘Inuvialuit’ as the collective identifier of the seven or eight traditional groups of the Mackenzie/Beaufort region. The relationships between these groups, and their notions of collectiv- ity, have a rich and complex history. This paper traces the evolution of Inuvialuit social and cultural identity from precontact times through the modern era. The primary focus, however, is on the forces and influences that have helped to shape contemporary Inuvialuit culture, society, and identity in the twentieth century. keywords: Inuvialuit, identity, community-based research, land claims, Mackenzie River The Inuvialuit are the Inuit of the western Canadian Arctic. in exploring the forces and influences that have helped They have lived along the lower reaches of the Mackenzie to shape the Inuvialuit as a group and how these have River and adjacent coastlines bordering the Beaufort Sea changed over the course of contact history. Identity, as for much longer than recorded in historical documents or discussed below, is a sociopolitical and cultural concept oral history. Their ownership and stewardship of this terri- that has been defined in many ways. I use both the sin- tory was formally recognized by the government of Canada gular ‘identity’ and plural ‘identities’ throughout this in the Inuvialuit Final Agreement of 1984. -
Paper 61-13 Camsell Bend and Root River Map-Areas
PAPER 61-13 CAMSELL BEND AND ROOT RIVER MAP-AREAS, DISTRICT OF MACKENZIE, NORTHWEST TERRITORIES 95Jand K (Report, 2 maps, 2 figures) R. J. W. Douglas and D. K. Norris DEC 5 1961 . _.. Price 50 cents 1961 GEOLOGICAL SURVEY OF CANADA CANADA PAPER 61-13 CAMSELL BEND AND ROOT RIVER MAP-AREAS, DISTRICT OF MACKENZIE, NORTHWEST TERRITORIES 95 J,K By R. J. W. Douglas and D. K. Norris DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA 51310-1 ROGER DUHAMEL, F. R. S. C. QUEEN'S PR INTER AND CONTROLLER OF STATIONERY OTTAWA, 1961 Pri ce 50 ce nts Cat. No. M44-6 1 11 CONTENTS Page Introduction .•••••••••••••••••••••• • • •••••••••••••••.••.•• References • • • • • • . • • • • • • • • • • • • • • • . • • . • • • • • • • • • • 1 Physical features........ ................................ 3 Stratigraphy......... ....... .................... ......... 5 Table of formations • • • • • • • • • . • . • • • . • . • • • • • • • . • • • • • • • 8-9 Palaeozoic •.•• , .............................. • • • • • • 6 Ordovician and older {?) - Sunblood formation ( 1) • • • . • • • • • • • . • • . • • • • • • • • • • • • • • • • • . 6 Ordovician and younger - map-units 2-10, including the Whittaker (3), Delorme (4), Camsell (5), Mount Kindle (7), a nd Sombre (10) formations • • • • • • • . • . • • • • • • • • • • • . • • • • • • • • . • • • . • 7 Middle Devonian and older { ? ) - map-units 11-17, comprising the Arnica {11), Manetoe (12), Fune ral (13), Bear Rock (14), Landry (15), Headless (16), and Nahanni (17) formations....... 14 Upper Devonian - map-units 18-25, including