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Ramsar Sites in Order of Addition to the Ramsar List of Wetlands of International Importance
Ramsar sites in order of addition to the Ramsar List of Wetlands of International Importance RS# Country Site Name Desig’n Date 1 Australia Cobourg Peninsula 8-May-74 2 Finland Aspskär 28-May-74 3 Finland Söderskär and Långören 28-May-74 4 Finland Björkör and Lågskär 28-May-74 5 Finland Signilskär 28-May-74 6 Finland Valassaaret and Björkögrunden 28-May-74 7 Finland Krunnit 28-May-74 8 Finland Ruskis 28-May-74 9 Finland Viikki 28-May-74 10 Finland Suomujärvi - Patvinsuo 28-May-74 11 Finland Martimoaapa - Lumiaapa 28-May-74 12 Finland Koitilaiskaira 28-May-74 13 Norway Åkersvika 9-Jul-74 14 Sweden Falsterbo - Foteviken 5-Dec-74 15 Sweden Klingavälsån - Krankesjön 5-Dec-74 16 Sweden Helgeån 5-Dec-74 17 Sweden Ottenby 5-Dec-74 18 Sweden Öland, eastern coastal areas 5-Dec-74 19 Sweden Getterön 5-Dec-74 20 Sweden Store Mosse and Kävsjön 5-Dec-74 21 Sweden Gotland, east coast 5-Dec-74 22 Sweden Hornborgasjön 5-Dec-74 23 Sweden Tåkern 5-Dec-74 24 Sweden Kvismaren 5-Dec-74 25 Sweden Hjälstaviken 5-Dec-74 26 Sweden Ånnsjön 5-Dec-74 27 Sweden Gammelstadsviken 5-Dec-74 28 Sweden Persöfjärden 5-Dec-74 29 Sweden Tärnasjön 5-Dec-74 30 Sweden Tjålmejaure - Laisdalen 5-Dec-74 31 Sweden Laidaure 5-Dec-74 32 Sweden Sjaunja 5-Dec-74 33 Sweden Tavvavuoma 5-Dec-74 34 South Africa De Hoop Vlei 12-Mar-75 35 South Africa Barberspan 12-Mar-75 36 Iran, I. R. -
Anvil Boulders and Lithic Reduction on Southern Victoria Island, Northwest Territories JACK BRINK’
ARCTIC VOL. 45, NO. 2 (JUNE 1992) P. 138-144 Anvil Boulders and Lithic Reduction on Southern Victoria Island, Northwest Territories JACK BRINK’ (Received II December 1990; accepted in revised form I5 August 1991) ABSTRACT. This paper reports on an unusual archaeological feature discovered at the Cadfael site (NiNg-17) on southeastern Victoria Island. TWO large boulders apparently served as anvil stones on which quartzite cobbleswere fractured. Lithic debris remained in situ on and around the boulders, preserving the materials and spatial arrangements as abandoned by the last flintknappers. Analysis ofone boulder and the associated artifacts demon- strates that a bipolar technology was employed to split cobbles, presumably to obtain large flakes for use as, or for making into, tools. As far as is known, no similar features have been reported in the literature on the Canadian Arctic, although potential candidates exist on Baffin Island and at Great Bear Lake. The age and cultural affiliation of the Cadfael site anvil boulders are undetermined; however an association with the Late Dorset culture, dating to about lo00 years ago, seemsmost likely. Key words: arctic archaeology, lithic technology, Dorsetculture, Victoria Island RÉSUMÉ. Cette communication concerne la d6couverte d’un aménagement archéologique plutôt inhabituel trouvé au site Cadfael (NiNg-17), situé au sud de l’île Victoria. Deux grosses pierres y auraient apparemment servies d’enclumes où l’on aurait cassé des galets de quartzite. Les débris lithiques étaient restés in situ sur et autour des grosses roches, préservant ainsi le materiel et les arrangements spatiaux tels qu’abandonnés par les derniers artisans de la pierre. -
Lesser Snow Goose EN
Introduction This bird • has evolved a strong serrated bill and tongue to cut and tear the roots of bulrushes and sedges • often has a rusty orange face, because its feathers have been stained by iron in the earth where the bird feeds • is probably the most abundant goose in Canada • unlike most other waterfowl, usually nests in large colonies with densities of up to 2 000 pairs per square kilometre Description The Lesser Snow Goose Chen caerulescens caerulescens has two different appearances, white phase and blue phase. The plumage of white-phase geese is almost completely white, except for black wing tips. The blue-phase goose has a white head, a bluish colour on the feathers of the lower back and flanks, and a body that ranges in colour from very pale, almost white, to very dark. Both the white- and blue-phase snow geese frequently have rusty orange faces, because their feathers have been stained by iron in the earth where the birds feed. The downy goslings of the white-phase geese are yellow, those of the blue phase nearly black. By two months of age the young birds of both colour phases are grey with black wing tips, although the immature blue-phase birds are generally a darker grey and have some light feathers on the chin and throat, which can become stained like those of the adults. The goslings have mostly lost their grey coloring by the following spring; in April and May they may only show a few flecks of darker coloring on their head and neck, and a few grey feathers on their wings that distinguish them from adults. -
Proceedings Template
Canadian Science Advisory Secretariat (CSAS) Research Document 2020/032 Central and Arctic Region Ecological and Biophysical Overview of the Southampton Island Ecologically and Biologically Significant Area in support of the identification of an Area of Interest T.N. Loewen1, C.A. Hornby1, M. Johnson2, C. Chambers2, K. Dawson2, D. MacDonell2, W. Bernhardt2, R. Gnanapragasam2, M. Pierrejean4 and E. Choy3 1Freshwater Institute Fisheries and Oceans Canada 501 University Crescent Winnipeg, MB R3T 2N6 2North/South Consulting Ltd. 83 Scurfield Blvd, Winnipeg, MB R3Y 1G4 3McGill University. 845 Sherbrooke Rue, Montreal, QC H3A 0G4 4Laval University Pavillon Alexandre-Vachon 1045, , av. of Medicine Quebec City, QC G1V 0A6 July 2020 Foreword This series documents the scientific basis for the evaluation of aquatic resources and ecosystems in Canada. As such, it addresses the issues of the day in the time frames required and the documents it contains are not intended as definitive statements on the subjects addressed but rather as progress reports on ongoing investigations. Published by: Fisheries and Oceans Canada Canadian Science Advisory Secretariat 200 Kent Street Ottawa ON K1A 0E6 http://www.dfo-mpo.gc.ca/csas-sccs/ [email protected] © Her Majesty the Queen in Right of Canada, 2020 ISSN 1919-5044 Correct citation for this publication: Loewen, T. N., Hornby, C.A., Johnson, M., Chambers, C., Dawson, K., MacDonell, D., Bernhardt, W., Gnanapragasam, R., Pierrejean, M., and Choy, E. 2020. Ecological and Biophysical Overview of the Southampton proposed Area of Interest for the Southampton Island Ecologically and Biologically Significant Area. DFO Can. Sci. Advis. Sec. Res. -
3.1.9 Wildlife and Wildlife Habitat This Section of the Document Focuses On
EIRB File No. 02/10-05 May 2011 ISSUED FOR USE 215 3.1.9 Wildlife and Wildlife Habitat This section of the document focuses on terrestrial mammals likely to be found within the local and regional study area and is based on a review of background information and traditional knowledge as well as the results of field studies. As defined under the IFA, “wildlife” means all fauna in a wild state other than reindeer. Section 3.1.9 considers terrestrial mammals and Section 3.1.10 considers birds. 3.1.9.1 Terrestrial Mammals There are 34 species of terrestrial mammals potentially occurring in the Regional Study Area for the proposed Highway (Table 3.1.9-1). The local and regional abundance and distribution of these species varies considerably depending on habitat availability and access to terrain suitable for various life history phases, such as calving and denning. No terrestrial mammal species were assessed as “at risk” under the NWT General Status Ranking Program (GNWT ENR 2011a). TABLE 3.1.9-1 TERRESTRIAL MAMMALS POTENTIALLY OCCURRING WITHIN THE REGIONAL STUDY AREA Common Name Scientific Name NWT General Status Rank Cinereus Shrew (Masked Shrew) Sorex cinereus Secure Dusky Shrew Sorex monticolus Secure Arctic Shrew Sorex arcticus Secure Tundra Shrew Sorex tundrensis Undetermined Barren-ground Shrew Sorex ugyunak Undetermined Snowshoe Hare Lepus americanus Secure Arctic Hare Lepus arcticus Secure Arctic Ground Squirrel Spermophilus parryii Secure Red Squirrel Tamiasciurus hudsonicus Secure Beaver Castor canadensis Secure Northern Red-backed -
Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012
Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012 Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012 Cover Photos (clockwise from top left): Doug Steinke, Doug Steinke, John Conkin, Jeff Coats, Tim Moser, Tim Moser, Doug Steinke Arctic Goose Joint Venture Technical Committee. 2008. Arctic Goose Joint Venture Strategic Plan: 2008 - 2012. Unpubl. Rept. [c/o AGJV Coordination Office, CWS, Edmonton, Alberta]. 112pp. Strategic Plan 2008 – 2012 Table of Contents INtroductioN ................................................................................................................ 7 ACCOMPLISHMENts AND FUTURE CHALLENGES .................................................... 9 Past Accomplishments ....................................................................................................... 9 Banding ...................................................................................................................... 9 Surveys ..................................................................................................................... 10 Research ................................................................................................................... 10 Future Challenges ........................................................................................................... 11 INformatioN NEEDS AND Strategies to ADDRESS THEM ............................ 12 Definitions of Information Needs.................................................................................... 12 Strategies for Meeting the Information -
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. .......................................................................................................................... -
A Review of Information on Fish Stocks and Harvests in the South Slave Area, Northwest Territories
A Review of Information on Fish Stocks and Harvests in the South Slave Area, Northwest Territories DFO L b ary / MPO Bibliotheque 1 1 11 0801752111 1 1111 1 1 D.B. Stewart' Central and Arctic Region Department of Fisheries and Oceans Winnipeg, Manitoba R3T 2N6 'Arctic Biological Consultants Box 68, St. Norbert Postal Station 95 Turnbull Drive Winnipeg, MB, R3V 1L5. 1999 Canadian Manuscript Report of Fisheries and Aquatic Sciences 2493 Canadian Manuscript Report of Fisheries and Aquatic Sciences Manuscript reports contain scientific and technical information that contributes to existing knowledge but which deals with national or regional problems. Distribution is restricted to institutions or individuals located in particular regions of Canada. However, no restriction is placed on subject matter, and the series reflects the broad interests and policies of the Department of Fisheries and Oceans, namely, fisheries and aquatic sciences. Manuscript reports may be cited as full publications. The correct citation appears above the abstract of each report. Each report is abstracted in Aquatic Sciences and Fisheries Abstracts and indexed in the Department's annual index to scientific and technical publications. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports (Biological Series) of the Fisheries Research Board of Canada. Numbers 901-1425 were issued as Manuscript Reports of the Fisheries Research Board of Canada. Numbers 1426-1550 were issued as Department of Fisheries and the Environment, Fisheries and Marine Service Manuscript Reports. -
SLAVE MÉTIS ALLIANCE PO Box 2301 Yellowknife, NT X1A 2P7
SLAVE MÉTIS ALLIANCE PO Box 2301 Yellowknife, NT X1A 2P7 July 4, 2019 Mackenzie Valley Review Board 200 Scotia Centre, 5102-50th Ave Yellowknife, NT X1A 2N7 To: Kate Mansfield & Catherine Fairbairn Re: Review Board Information Requests to Parties for Diavik EA1819-01 As requested for the Diavik Environmental Assessment (EA1819-01), the Mackenzie Valley Environmental Impact Review Board (Review Board) issued two information request to several parties, including the North Slave Métis Alliance. This letter specifically addresses Information Request 1: Potential impacts to cultural use of Lac de Gras Area 1. Please describe how your group used the Lac de Gras area culturally (including the hunting, fishing, trapping, gathering, and travel) before mining started there. As this question pertains to the land use prior to the development of Diavik Diamond Mine, this information was collected and provided to the regulators during the initial environmental assessment of the mine. Please see the attached “Appendix A: Can’t Live Without Work” by North Slave Metis Alliance (1999). 2. Please describe how your group would use and feel about the Lac de Gras area under the following scenarios: a) reconnecting empty pits and underground mine workings with Lac de Gras at closure (that is, Diavik’s current closure plan for the mine), b) putting processed kimberlite into the pits and underground mine workings before reconnecting them to Lac de Gras (that is, the proposed activities for this environmental assessment), c) putting processed kimberlite into the pits and underground mine workings and not reconnecting them with Lac de Gras. During a community meeting, NSMA members expressed that their interest was to have the Diavik mine site (not just the pits) return to pre-development condition as much as practicable, in such a way that the area would be the cleanest and safest environment possible for humans and wildlife. -
Diamondiferous Kimberlites on Victoria Island, Canada: a Northern Extension of the Slave Craton
DIAMONDIFEROUS KIMBERLITES ON VICTORIA ISLAND, CANADA: A NORTHERN EXTENSION OF THE SLAVE CRATON Mark Kolebaba1, George Read2, Bernard Kahlert1 and Dave Kelsch1, 1 Diamonds North Resources Ltd, Canada; 2 Canabrava Diamond Corporation, Canada basalt (Natkusiak Formation 723 Ma) and INTRODUCTION agglomerate which make up the Shaler Mountains that are intruded by gabbro sills. The lower sandstone and gabbro units of the Shaler Group are also found Victoria Island, located in the Northwest Territories along the southern coast of Victoria Island, and as and Nunavut in the High Arctic of Canada (Figure 1) small inliers south of Washburn Lake. has been a diamond exploration target since 1993 when exploration companies recognized the possibility Archean age rocks beneath the eastern half of Victoria Island under thin Paleozoic carbonate cover. Much evidence has been collected through work since 1993 that suggests Victoria Island has the potential to become a world-class diamond-producing district. Recent exploration efforts have identified kimberlites with high diamond counts and robust diamond size distributions trending toward large 1 to 2 mm stones from small kimberlite samples. Supportive mineral chemistry including major oxides and trace element analyses suggests a cool geotherm, presence of potential peridotitic diamond sources and a strong diamond bearing eclogite signature. Figure 1: Location and geology map for Victoria Island. GEOLOGY Regional magnetics indicate the basement rocks have been intruded by NW-SE trending Mackenzie (1270 Archean rocks exist in the eastern half of Victoria Ma) and Franklin (720 Ma) diabase dykes and a Island. Paleozoic sediments including dolomite, previously undocumented north-south trending minor limestone, sandstone and shale of the Arctic diabase dyke system dated at 425 Ma (Diamonds Platform have been preserved within post- North Internal Report, 1999). -
CNGO NU Summary-Of-Activities
SUMMARY OF ACTIVITIES 2015 © 2015 by Canada-Nunavut Geoscience Office. All rights reserved. Electronic edition published 2015. This publication is also available, free of charge, as colour digital files in Adobe Acrobat® PDF format from the Canada- Nunavut Geoscience Office website: www.cngo.ca/ Every reasonable effort is made to ensure the accuracy of the information contained in this report, but Natural Resources Canada does not assume any liability for errors that may occur. Source references are included in the report and users should verify critical information. When using information from this publication in other publications or presentations, due acknowledgment should be given to Canada-Nunavut Geoscience Office. The recommended reference is included on the title page of each paper. The com- plete volume should be referenced as follows: Canada-Nunavut Geoscience Office (2015): Canada-Nunavut Geoscience Office Summary of Activities 2015; Canada- Nunavut Geoscience Office, 208 p. ISSN 2291-1235 Canada-Nunavut Geoscience Office Summary of Activities (Print) ISSN 2291-1243 Canada-Nunavut Geoscience Office Summary of Activities (Online) Front cover photo: Sean Noble overlooking a glacially eroded valley, standing among middle Paleoproterozoic age psam- mitic metasedimentary rocks, nine kilometres west of Chidliak Bay, southern Baffin Island. Photo by Dustin Liikane, Carleton University. Back cover photo: Iqaluit International Airport under rehabilitation and expansion; the Canada-Nunavut Geoscience Of- fice, Geological Survey of Canada (Natural Resources Canada), Centre d’études nordiques (Université Laval) and Trans- port Canada contributed to a better understanding of permafrost conditions to support the planned repairs and adapt the in- frastructure to new climatic conditions. Photo by Tommy Tremblay, Canada-Nunavut Geoscience Office. -
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: