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Diamond Jenness (1886-1969)
Diamond Jenness (1886-1969) HENRY B. COLLINS and WILLIAM E. TAYLOR Jr. Canada’smost distinguished anthropologist, Dr. Diamond Jenness, formerly Chiefof the Division of Anthropology, National Museums of Canada, and Honorary Associate of the Arctic Institute of North America, died peacefully at his home in the Gatineau Hills near Ottawa on 29 November, 1969. He was one of that rapidly-vanishing, virtually extinct kind - the all round anthropolo- gist, who, working seriously, turned out first-class publications in all four major branches of the discipline : ethnology, linguistics, archaeology, and physical anthropology. One must also add a fifth: applied anthropology, a fitting designa- tion for theseries of monographs on Eskimo administration in Alaska, Canada, and Greenland which he wrote after his retirement and which were published by the Arctic Institute between 1962 and 1968. Diamond Jennesswas born in Wellington,New Zealand, on 10 February 1886, and attended Victoria University College, one of the four branches of the University ofNew Zealand, wherehe graduated withfirst class honours in classics in 1908. Later he studied at Balliol College, Oxford, under one of the outstanding ethnologists of the time, Professor R. R. Marett. He received both a B.A. in Lit. Hum. and a diploma in Anthropology at Oxford in 1911. In 191 1-12 he was designated Oxford Scholar in Papua and was sent by the Uni- versity to make anthropological studies among the Northern d’Entrecasteaux, a primitive tribe dwelling on the islands of the D’Entrecasteaux Archipelago off the east coast of New Guinea. The results of this first field-work were published by Oxford University (1 920a). -
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. -
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. -
Ethnobotany of the Kiluhikturmiut Inuinnait of Kugluktuk, Nunavut, Canada
Research Communicaon Ethnobotany of the Kiluhikturmiut Inuinnait of Kugluktuk, Nunavut, Canada Jonathan Duffy Davis1, Sandra Anne Banack2 Author address: 1Fullerton Arboretum, California State University, Fullerton, CA 92831, 2Instute for Ethnomedicine, P.O. Box 3464, Jackson, WY 83001 Received: September 24, 2012 Volume: 3:78‐90 Published: December 29, 2012 © 2012 Society of Ethnobiology Abstract: The disparity in floral diversity between tropical and arcc regions is reflected in a paucity of ethnobotanical research among arcc cultures. The Kiluhikturmiut Inuinnait are an Inuit subpopulaon who inhabit the Kikmeot Region of the Territory of Nunavut in Canada’s Arcc. We conducted an ethnobotanical survey in the Inuinnait hamlet of Kugluktuk to document the tradional uses of plants as food, materials, and medicine. Data were gathered through unstructured interviews, parcipant observaon, purposive sampling, and voucher‐specimen collecon of all plants used. Uses were documented for 23 plant species/types contained in 14 families. Nine species/types were eaten, six species/types were used as materials, and 12 species were used for medicine. Villagers shared common knowledge of plants used for food and materials; however, knowledge of medicinal plants was restricted to a single healer. We argue that specialized knowledge such as the use of medicinal plants is important to document especially when the number individuals using this knowledge is dwindling. Abstract: Pitquhiigut piruqhimayut qauyihaivluk qanuq inuit atuqtauvagait atungauyanik niqiuvluk, -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
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). -
Polar Continental Shelf Program Science Report 2019: Logistical Support for Leading-Edge Scientific Research in Canada and Its Arctic
Polar Continental Shelf Program SCIENCE REPORT 2019 LOGISTICAL SUPPORT FOR LEADING-EDGE SCIENTIFIC RESEARCH IN CANADA AND ITS ARCTIC Polar Continental Shelf Program SCIENCE REPORT 2019 Logistical support for leading-edge scientific research in Canada and its Arctic Polar Continental Shelf Program Science Report 2019: Logistical support for leading-edge scientific research in Canada and its Arctic Contact information Polar Continental Shelf Program Natural Resources Canada 2464 Sheffield Road Ottawa ON K1B 4E5 Canada Tel.: 613-998-8145 Email: [email protected] Website: pcsp.nrcan.gc.ca Cover photographs: (Top) Ready to start fieldwork on Ward Hunt Island in Quttinirpaaq National Park, Nunavut (Bottom) Heading back to camp after a day of sampling in the Qarlikturvik Valley on Bylot Island, Nunavut Photograph contributors (alphabetically) Dan Anthon, Royal Roads University: page 8 (bottom) Lisa Hodgetts, University of Western Ontario: pages 34 (bottom) and 62 Justine E. Benjamin: pages 28 and 29 Scott Lamoureux, Queen’s University: page 17 Joël Bêty, Université du Québec à Rimouski: page 18 (top and bottom) Janice Lang, DRDC/DND: pages 40 and 41 (top and bottom) Maya Bhatia, University of Alberta: pages 14, 49 and 60 Jason Lau, University of Western Ontario: page 34 (top) Canadian Forces Combat Camera, Department of National Defence: page 13 Cyrielle Laurent, Yukon Research Centre: page 48 Hsin Cynthia Chiang, McGill University: pages 2, 8 (background), 9 (top Tanya Lemieux, Natural Resources Canada: page 9 (bottom -
Tab 6 Estimating the Abundance Of
SUBMISSION TO THE NUNAVUT WILDLIFE MANAGEMENT BOARD FOR Information: X Decision: Issue: South Baffin Island Caribou Abundance Survey, 2012 and Proposed Management Recommendations Background: Caribou are a critical component of the boreal and arctic ecosystems. They are culturally significant to local communities and provide an important source of food. In some areas, there is still uncertainty on population trends because of the lack of scientific information due to difficult logistics and remoteness. This is particularly true for Baffin Island, where three sub-populations of Barrenground caribou (Rangifer tarandus groenlandicus) are hypothesized, though little is known about their abundance and trends over time (Ferguson and Gauthier 1992). In the past 60 years, only discrete portions of their range have been surveyed and no robust quantitative estimates at the sub-population level were ever derived. For over a decade Inuit from communities on northern Baffin Island, and more recently from across the entire island, have reported declines in caribou numbers, although no quantitative estimates are available. In total 10 communities, representing half of all Nunavummiut, traditionally or currently harvest Baffin Island caribou. At the same time, climate change, including increased arctic temperatures and precipitation, and anthropogenic activities connected to mineral exploration and mining are potentially negatively impacting caribou and their range. Due to the risk of these cumulative negative effects, and the importance of these caribou to communities, the Department of Environment undertook, in 2012, a quantitative caribou abundance aerial survey of South Baffin Island with the support of the NWMB and co- management partners. This area represents the most abundant area of caribou on Baffin Island. -
Real Estate Tax Commitment Book
Brooksville Real Estate Tax Commitment Book - 6.700 06/23/2021 8:54 AM 2021 Commitment Page 1 Account Name & Address Land Building Exemption Assessment Tax 60 VERSANT POWER 2,550,500 0 0 2,550,500 17,088.35 P.O. BOX 932 BANGOR ME 04402-0932 000-000 73 RUSS, JOEL B 213,500 58,000 0 271,500 1,819.05 RUSS, CAROLYN Acres 0.34 P.O. BOX 137 WALPOLE ME 04573 147 UNDERCLIFF RD 001-001 B6118P42 09/19/2013 B2504P242 751 MAINE COAST HERITAGE 14,200 0 0 14,200 95.14 TRUST, ONE BOWDOIN MILL ISLAND Acres 1.50 SUITE 201 TOPSHAM ME 04086 UNDERCLIFF RD 001-002 B1468P422 919 ROBINSON, RUTH L 24,000 0 0 24,000 160.80 110 UNDERCLIFF ROAD Acres 50.00 UNDERCLIFF FARM BROOKSVILLE ME 04642 UNDERCLIFF RD 001-003 B5569P162 01/25/2011 B4968P217 03/11/2008 B1277P449 578 HUNT-KASARJIAN REBECCA 36,900 1,000 0 37,900 253.93 44 RAY AVE Acres 8.00 BELLINGHAM MA 02019 33 MCGEES HILL RD 001-004 B1207P516 633 KOMINSKY, ANDREW LEWIS 216,100 129,200 0 345,300 2,313.51 KOMINSKY, JULIA REVA Acres 1.30 168 W BROADWAY BANGOR ME 04401 115 WEIR COVE RD 001-005 B6262P345 08/05/2014 B4671P73 12/29/2006 B1537P381 Land Building Exempt Total Tax Page Totals: 3,055,200 188,200 0 3,243,400 21,730.78 Subtotals: 3,055,200 188,200 0 3,243,400 21,730.78 Brooksville Real Estate Tax Commitment Book - 6.700 06/23/2021 8:54 AM 2021 Commitment Page 2 Account Name & Address Land Building Exemption Assessment Tax 634 KOMINSKY, ANDREW LEWIS 22,800 0 0 22,800 152.76 KOMINSKY, JULIA REVA Acres 0.30 168 W BROADWAY BANGOR ME 04401 113 WEIR COVE RD 001-006 B1537P381 918 ROBINSON, RUTH 5,900 0 0 5,900 39.53 110 UNDERCLIFF ROAD Acres 0.22 HARBORSIDE ME 04642 ISLAND IN WEIR COVE 001-007 B2779P558 251 CLIFFORD, PD (HEIRS) 34,700 22,400 0 57,100 382.57 C/O DARON CLIFFORD Acres 0.25 6 BUITLER ACRES LN BLUE HILL ME 04614 120 WEIR COVE RD 001-008 776 MERRICK, TONI RUSSELL 185,200 35,700 0 220,900 1,480.03 P.O. -
Canada's Arctic Marine Atlas
Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King -
Canadian Arctic Expedition 1913-18
REPORT OF THE CANADIAN ARCTIC EXPEDITION 1913-18 VOLUME XIII: ESKIMO FOLK-LORE PART A: MYTHS AND TRADITIONS FROM NORTHERN ALASKA, THE MACKENZIE DELTA AND COR ONATION GULF. By D. JENNESS SOUTHERN PARTY, 1913-16 OTTAWA F. A. ACLAND PRINTER TO THE KING'S MOST EXCELLENT MAJESTY 111M Issued November 15, 1924 Report of the Canadian Arctic Expedition, 1913-18. VOLUME I: GENERA.L INTRODUCTION, NARRATIVE, ETC. Part A: NORTHERN PARTY, 1913-18 •..........•....................•••••••...• . (To be prepared). Part B: SOUTHERN PARTY, 1913-16. By Rudolph Martin Andel"llOn ............... (In preparation) VOLUME D: MA.MMA.LS A.ND BIBDS Part A: MAMMALS OF WESTERN ARCTIC AMERICA. · ................................•...........•.••••.•••••••••••••••••••..• (1 n prepaTlltion). Part B: BIRDS OF WESTERN ARCTIC AMERICA. · ............... ',' .......... '.............................................. (In prepllration). VOLUME m: INSECTS INTRODUCTION. By C. Gordon Hewitt ......•.••••.•••...•.••. V.Slled December 10,1910). Part A: COLLEMBOLA. By Justus W. FoIBOm ....•....••.....••..••••••.••.•.. (I•• lled JlIly 10, 1919). Part B: NEUROPTEROlP INSECTS. By Nathan Bank•.•••.....•.•.••••.. (I,.lIed JIII,l II, 1919). Part C: DIPTERA. Crane-flies. By Charles P. Alexander. Mosquitoes. By HarriBOn G. Dyar. ' Diptera(excluding Tipulidm and Culicidm). By J. R. Mallooh ....... (I.. lIed JIIIIl 14, 1919). Part D: MALLOPHAGA AND ANOPLURA. Mallophaga. By A. W. Baker. Anoplura. By G. F. Ferris and G. H. F. Nuttall .••.••.•••..•.•. (I"lIed September 11,1919). Part E: COLEOPTERA. Forest Insecta, including Ipidm, Cerambycidm, and Buprestidm. By J. M. Swaine. Carabidm and SilphidlB. By H. C. Fall. CoccinellidlB, Elateridm, ChryBOmelidlB and Rhynchophora (excluding Ipidle). By C. W. Leng. Dytiscidm. By J. D. Sherman, Jr..••.•....•.•••••••••••••.•••. (1"lIed December 11,1919). Part F: HEMIPTERA. By Edward P. VanDuzee .............................. (1 ..lIed JIII,l", 1919). -
Combining Flat Water Paddling Over Tundra Lakes with the Rush of White Water Where It Tumbles Down to the Arctic Ocean
COPPERMINE RIVER Introduction The Coppermine River is an excellent trip for experienced canoeists; combining flat water paddling over tundra lakes with the rush of white water where it tumbles down to the Arctic Ocean. The 640 km (400 mi.) trip from Lac de Gras (shorter if canoeists start at Point or Redrock Lakes) takes voyageurs past the tundra, through the treeline and the famous Coppermine Mountains and back to the tundra again as it winds to the north. This is a fast river with many rapids and whitewater stretches. All falls and many of the larger rapids require portaging. Other rapids demand very good manoeuvre skill and expertise in whitewater canoeing. You are on your own once the plane drops you off. There are no settlements until Coppermine on Coronation Gulf. Those attempting the trip should be experienced canoeists, with knowledge of survival and first aid skills. It is suggested to plan at least three to four weeks in advance for the trip. Access To The Coppermine River There are many large lakes in the headwaters of the Coppermine where canoeists can start a trip. The most popular starting points are Lac de Gras, the Source Lake and the Winter Lake. John Franklin started out from the Winter Lake in the summer of 1821 for the Polar Sea, Point Lake at the foot of Obstruction Rapids, Rawalpindi Lake and Redrock Lake. Starting from the Rawalpindi Lake and Redrock Lake avoids the long lake slogs. However, the trip from Rawalpindi to the Coppermine River at Redrock Lake includes several carries and shallow rivers.