Nunavut Mineral Exploration, Mining and Geoscience Overview 2014
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Modelling Population Mobility in Southern Baffin Island's Past
MODELLING POPULATION MOBILITY IN SOUTHERN BAFFIN ISLAND’S PAST USING GIS AND LANDSCAPE ARCHAEOLOGY by Jeffrey Phillip Stup 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 Department of Anthropology University of Manitoba Winnipeg, Manitoba Copyright © 2015 by Jeffrey Phillip Stup Abstract Evidence of chert stone tools on southern Baffin Island of Canada dates back thousands of years, yet most of these materials are found far from coastal areas of use. In the central interior lakes region of Baffin Island, chert can be found but this area is extremely remote and hard to access. If past human populations moved inland from the coast to acquire chert toolstone and pursue seasonally specific subsistence-related activities, many archaeological sites should exist between these respective locales. Historically, it has been difficult to locate such intermediate sites given the expansive of the landscape and the logistical challenges of surveying it. In this study, free and open-source geospatial data were used in geographic information systems (GIS) to predict archaeological site formation and potential inland travel routes. The models created link the archaeologically dense coastal and inland regions. These were constructed with a landscape archaeology theoretical approach and validated by comparisons to Inuit ethnographic accounts of interior-bound pathways. A new archaeological-GIS method was created, using a flood allocation function on a ‘humanistic’ cost surface. This ‘mobility-shed’ method generates vast networks of areas most conducive to human movement, aids in solving problems about past human population movements for Baffin Island history, for an ongoing chert provenance study, and will lead to future research through ground-truthing and more in-depth geospatial studies. -
Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped. -
NUNAVUT a 100 , 101 H Ackett R Iver , Wishbone Xstrata Zinc Canada R Ye C Lve Coal T Rto Nickel-Copper-PGE 102, 103 H Igh Lake , Izo K Lake M M G Resources Inc
150°W 140°W 130°W 120°W 110°W 100°W 90°W 80°W 70°W 60°W 50°W 40°W 30°W PROJECTS BY REGION Note: Bold project number and name signifies major or advancing project. AR CT KITIKMEOT REGION 8 I 0 C LEGEND ° O N umber P ro ject Operato r N O C C E Commodity Groupings ÉA AN B A SE M ET A LS Mineral Exploration, Mining and Geoscience N Base Metals Iron NUNAVUT A 100 , 101 H ackett R iver , Wishbone Xstrata Zinc Canada R Ye C lve Coal T rto Nickel-Copper-PGE 102, 103 H igh Lake , Izo k Lake M M G Resources Inc. I n B P Q ay q N Diamond Active Projects 2012 U paa Rare Earth Elements 104 Hood M M G Resources Inc. E inir utt Gold Uranium 0 50 100 200 300 S Q D IA M ON D S t D i a Active Mine Inactive Mine 160 Hammer Stornoway Diamond Corporation N H r Kilometres T t A S L E 161 Jericho M ine Shear Diamonds Ltd. S B s Bold project number and name signifies major I e Projection: Canada Lambert Conformal Conic, NAD 83 A r D or advancing project. GOLD IS a N H L ay N A 220, 221 B ack R iver (Geo rge Lake - 220, Go o se Lake - 221) Sabina Gold & Silver Corp. T dhild B É Au N L Areas with Surface and/or Subsurface Restrictions E - a PRODUCED BY: B n N ) Committee Bay (Anuri-Raven - 222, Four Hills-Cop - 223, Inuk - E s E E A e ER t K CPMA Caribou Protection Measures Apply 222 - 226 North Country Gold Corp. -
Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K of 95I4674 85L
Natural Resources Ressources naturelles Canada Canada CurrentCurrent and and Upcoming Upcoming NGR NGR Program Program Activities Activities in in British British Columbia, Columbia, NationalNational Geochemical Geochemical Reconnaissance Reconnaissance NorthwestNorthwest Territories, Territories, Yukon Yukon Territory Territory and and Alberta, Alberta, 2005-06 2005-06 ProgrProgrammeamme National National de de la la Reconnaissance Reconnaissance Géochimique Géochimique ActivitésActivités En-cours En-cours et et Futures Futures du du Programme Programme NRG NRG en en Colombie Colombie Britannique, Britannique, P.W.B.P.W.B. Friske, Friske,S.J.A.S.J.A. Day, Day, M.W. M.W. McCurdy McCurdy and and R.J. R.J. McNeil McNeil auau Territoires Territoires de du Nord-Ouest, Nord-Ouest, au au Territoire Territoire du du Yukon Yukon et et en en Alberta, Alberta, 2005-06 2005-06 GeologicalGeological Survey Survey of of Canada Canada 601601 Booth Booth St, St, Ottawa, Ottawa, ON ON 11 Area: Edéhzhie (Horn Plateau), NT 55 Area: Old Crow, YT H COLU Survey was conducted in conjunction with Survey was conducted in conjunction with and funded by IS M EUB IT B and funded by NTGO, INAC and NRCAN. NORTHWEST TERRITORIES R I the Yukon Geological Survey and NRCAN. Data will form A 124° 122° 120° 118° 116° B Alberta Energy and Utilities Board Data will form the basis of a mineral potential GEOSCIENCE 95N 85O the basis of a mineral potential evaluation as part of a 95O 85N evaluation as part of a larger required 95P 85M larger required Resource Assessment. OFFICE .Wrigley RESEARCH ANALYSIS INFORMATION Resource Assessment. .Wha Ti G 63° YUKON 63° Metals in the Environment (MITE) E Y AGS ESS Program: O E ESS Program: Metals in the Environment V .Rae-Edzo L R GSEOLOGICAL URVEY Survey Type: Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K OF 95I4674 85L Survey Type: Stream Sediment, stream M Year of Collection: 2004 and 2005 A C K ENZI E R 2 62° I V water, bulk stream sediment (HMCs and KIMs). -
Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands. -
Baffin Island: Field Research and High Arctic Adventure, 1961-1967
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2016-02 Baffin Island: Field Research and High Arctic Adventure, 1961-1967 Ives, Jack D. University of Calgary Press Ives, J.D. "Baffin Island: Field Research and High Arctic Adventure, 1961-1967." Canadian history and environment series; no. 18. University of Calgary Press, Calgary, Alberta, 2016. http://hdl.handle.net/1880/51093 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca BAFFIN ISLAND: Field Research and High Arctic Adventure, 1961–1967 by Jack D. Ives ISBN 978-1-55238-830-3 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at [email protected] Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specific work without breaching the artist’s copyright. -
Summary of the Hudson Bay Marine Ecosystem Overview
i SUMMARY OF THE HUDSON BAY MARINE ECOSYSTEM OVERVIEW by D.B. STEWART and W.L. LOCKHART Arctic Biological Consultants Box 68, St. Norbert P.O. Winnipeg, Manitoba CANADA R3V 1L5 for Canada Department of Fisheries and Oceans Central and Arctic Region, Winnipeg, Manitoba R3T 2N6 Draft March 2004 ii Preface: This report was prepared for Canada Department of Fisheries and Oceans, Central And Arctic Region, Winnipeg. MB. Don Cobb and Steve Newton were the Scientific Authorities. Correct citation: Stewart, D.B., and W.L. Lockhart. 2004. Summary of the Hudson Bay Marine Ecosystem Overview. Prepared by Arctic Biological Consultants, Winnipeg, for Canada Department of Fisheries and Oceans, Winnipeg, MB. Draft vi + 66 p. iii TABLE OF CONTENTS 1.0 INTRODUCTION.........................................................................................................................1 2.0 ECOLOGICAL OVERVIEW.........................................................................................................3 2.1 GEOLOGY .....................................................................................................................4 2.2 CLIMATE........................................................................................................................6 2.3 OCEANOGRAPHY .........................................................................................................8 2.4 PLANTS .......................................................................................................................13 2.5 INVERTEBRATES AND UROCHORDATES.................................................................14 -
Arviat, ᐊᕐᕕᐊᑦ, “Place of the Bowhead Whale”
Arviat, ᐊᕐᕕᐊᑦ, “Place of the bowhead whale” Kugaaruk, ᑰᒑᕐᔪ, “Little stream” Introduction Kugaaruk is located on the southwest shore of the Simpson Peninsula, on the east side of Pelly Bay in the Kitikmeot region. In 2016 the population was 933. The wildlife economy plays an important role in Kugaaruk, with many residents supporting themselves by hunting, fishing, trapping, and gathering. Community members also participate in wage-based economic activities1. Important coastal resources in the Kugaaruk region include bowhead whales, narwhals, seals, polar bears, and Arctic char, with residents sometimes travelling long distances to reach hunting and fishing grounds2. The community’s hunting and fishing area includes Pelly Bay, Boothia Peninsula, Committee Bay, Rae Strait, and The Gulf of Boothia2. Current there are no national or territorial parks located near Kugaaruk, however, several fishing and hunting camps exist nearby. Community Restoration Priorities 1. The restoration of key fishing rivers and monitoring of water quality and fish health in local waterbodies, as water levels are too low, and rivers are drying up - remediation action and new infrastructure will be required; and 2. Observed changes in water quality and fish health in some areas have been noted for awhile. A community-led water quality and fish health monitoring programs should be put in place. Community Map and Workshop Highlights The CRN research team visited the community in March 2019. Literature Review Kugaaruk is characterized by coastal mountains and well-vegetated lowlands with several lakes, rivers, and ponds throughout the region, which provide important habitat for a variety of plants and animals2. Land-fast lead systems are areas of separated land-fast ice and pack ice and can be found throughout this region2. -
Technical Report on the Gold and Base Metal Potential of the Sy Property, Nunavut, Canada
NTS 65 I/04 to I/06 and J/01 TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA Completed By: APEX Geoscience Ltd. Suite 200, 9797-45 Avenue Edmonton, Alberta, Canada T6E 5V8 Completed For: Corsa Capital Ltd. Suite 1440, 625 Howe Street Vancouver, BC V6C 2T6 December 4th, 2007 M.B. Dufresne, M.Sc., P.Geol. TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA TABLE OF CONTENTS PAGE SUMMARY...................................................................................................................... 1 INTRODUCTION AND TERMS OF REFERENCE.......................................................... 3 RELIANCE ON OTHER EXPERTS................................................................................. 3 PROPERTY LOCATION AND DESCRIPTION ............................................................... 4 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY............................................................................................................ 8 HISTORY ........................................................................................................................ 8 GEOLOGICAL SETTING .............................................................................................. 15 Regional Geology ............................................................................................... 15 Property Geology ............................................................................................... 16 DEPOSIT -
198 13. Repulse Bay. This Is an Important Summer Area for Seals
198 13. Repulse Bay. This is an important summer area for seals (Canadian Wildlife Service 1972) and a primary seal-hunting area for Repulse Bay. 14. Roes Welcome Sound. This is an important concentration area for ringed seals and an important hunting area for Repulse Bay. Marine traffic, materials staging, and construction of the crossing could displace seals or degrade their habitat. 15. Southampton-Coats Island. The southern coastal area of Southampton Island is an important concentration area for ringed seals and is the primary ringed and bearded seal hunting area for the Coral Harbour Inuit. Fisher and Evans Straits and all coasts of Coats Island are important seal-hunting areas in late summer and early fall. Marine traffic, materials staging, and construction of the crossing could displace seals or degrade their habitat. 16.7.2 Communities Affected Communities that could be affected by impacts on seal populations are Resolute and, to a lesser degree, Spence Bay, Chesterfield Inlet, and Gjoa Haven. Effects on Arctic Bay would be minor. Coral Harbour and Repulse Bay could be affected if the Quebec route were chosen. Seal meat makes up the most important part of the diet in Resolute, Spence Bay, Coral Harbour, Repulse Bay, and Arctic Bay. It is a secondary, but still important food in Chesterfield Inlet and Gjoa Haven. Seal skins are an important source of income for Spence Bay, Resolute, Coral Harbour, Repulse Bay, and Arctic Bay and a less important income source for Chesterfield Inlet and Gjoa Haven. 16.7.3 Data Gaps Major data gaps concerning impacts on seal populations are: 1. -
Canadian Heritage Rivers System Management Plan for the Thelon River, N.W.T
CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N.W.T. Sector Tourism I 11-40.12 Plans/Strategies I I I - CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N.W.T. NWT EDT Can The 1990 — CANADIAN HERITAGE RIVERS SYSTEM MANAGEMENT PLAN FOR THE THELON RIVER, N. W.T. Submitted by the Municipality of Baker Lake; the Department of Economic Development and Tourism Government of the Northwest Territories; and the Department of Indian Affairs and Northern Development of Canada 1990 TABLE OF CONTENTS . 1.0 Introduction . 1.1 Thelon Heritage River Nomination . 1 1.2 Regional Setting and River Description . 1 1.3 Canadian Heritage Rivers System . 4 1.4 Purpose of the Management Plan . 4 l.4.1 General Considerations . 4 1.4.2 Objectives of the Thelon River Management Plan. 5 2.0 Background 2.1 History of the Nomination . 6 2.2 Public Support and Consultation . 6 2.3 Present Land Use . 8 2.3. lBaker Lake Inuit Land Use . 8 2.3.2 Land Tenure and Land Claims . 8 2.3.3 Mining and Other Development . 10 3.0 Heritage Values 3.1 Natural Heritage Values . 11 3.2 Human Heritage Values . 12 3.3 Recreational Values . 13 4.0 Planning and Management Program 4.1 Land Use Framework.. ~ . 15 4.1. 1 River Corridor . 15 4.1.2 Areas of Significance . 15 4.1.3 Potential Territorial Parks . 18 4.2 Heritage Management and Protection . 20 4.2.1 Human Heritage . 20 4.2.2 Natural Heritage . 21 4.2. -
Gjoa Haven © Nunavut Tourism
NUNAVUT COASTAL RESOURCE INVENTORY ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut Ministère de l’Environnement Gjoa Haven © Nunavut Tourism ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut NUNAVUT COASTAL RESOURCE INVENTORY • Gjoa Haven INVENTORY RESOURCE COASTAL NUNAVUT Ministère de l’Environnement Nunavut Coastal Resource Inventory – Gjoa Haven 2011 Department of Environment Fisheries and Sealing Division Box 1000 Station 1310 Iqaluit, Nunavut, X0A 0H0 GJOA HAVEN Inventory deliverables include: EXECUTIVE SUMMARY • A final report summarizing all of the activities This report is derived from the Hamlet of Gjoa Haven undertaken as part of this project; and represents one component of the Nunavut Coastal Resource Inventory (NCRI). “Coastal inventory”, as used • Provision of the coastal resource inventory in a GIS here, refers to the collection of information on coastal database; resources and activities gained from community interviews, research, reports, maps, and other resources. This data is • Large-format resource inventory maps for the Hamlet presented in a series of maps. of Gjoa Haven, Nunavut; and Coastal resource inventories have been conducted in • Key recommendations on both the use of this study as many jurisdictions throughout Canada, notably along the well as future initiatives. Atlantic and Pacific coasts. These inventories have been used as a means of gathering reliable information on During the course of this project, Gjoa Haven was visited on coastal resources to facilitate their strategic assessment, two occasions: