Geological Survey of Canada Commission Gbologique Du Canada

Total Page:16

File Type:pdf, Size:1020Kb

Geological Survey of Canada Commission Gbologique Du Canada Geological Survey of Canada Commission gbologique du Canada , PAPER 87-7 GEOLOGICAL SURVEY OF CANADA RADIOCARBON DATES XXVll W. BLAKE, JR. GEOLOGICAL SURVEY OF CANADA PAPER 87-7 GEOLOGICAL SURVEY OF CANADA RADIOCARBON DATES XXVll W. BLAKE, JR. Energy, Mines and ~nergie,Mines et 1*1 Resources Canada Ressources Canada @ Minister of Supply and Services Canada 1988 Available in Canada through authorized bookstore agents and other bookstores or by mail from Canadian Government Publishing Centre Supply and Services Canada Ottawa, Canada KIA OS9 and from Geological Survey of Canada offices: 601 Booth Street Ottawa, Canada KIA OE8 3303-33rd Street N.W., Calgary, Alberta T2L 2A7 100 West Pender Street Vancouver, B.C. V8L 4B2 A deposit copy of this publication is also available for reference in public libraries across Canada Cat. No. M44-8717E Canada: $5.00 ISBN 0-660-12776-8 Other countries: $6.00 Price subject to change without notice CONTENTS AbstracWR6sum6 Introduction Acknowledgments Geological samples Eastern Canada Newfoundland Nova Scotia New Brunswick Quebec Ontario Western Canada Manitoba British Columbia Northern Canada, mainland Yukon Territory Northwest Territories Northern Canada, Arctic Archipelago Coronation GulfIVictoria Island Banks Island Baffin Island Northern Baffin Bay Devon-. - Island Coburg Island Southern Ellesmere Island West-central Ellesmere Island East-central Ellesmere Island Cocked Hat Island Bathurst Island Melville Island Prince Patrick Island United States of America Archeologlcawashin7- samples Eastern Canada Newfoundland Labrador Nova Scotia Ontario Northern Canada. Arctic Archipelago- - Devon Island Southern Ellesmere Island Skraeling Island Haa Island East-central Ellesmere Island References Index Tables 1. Monthly average count for background during the period August 1, 1986 to November 17,1986. 2. Monthly average count (No) for oxalic acid standard during the period August 1, 1986 to November 17,1986. 3. Number of one-day counts used to determine average counting rates for background and oxalic acid standard during the report period. 4. Number of monthly background and standard gas preparations used during the report period. The present date list, GSC XXVII, is the sixteenth to be published directly in the Geological Survey's Paper series. Lists prior to GSC XI1 were published first in the journal Radiocarbon and were reprinted as GSC Papers. The lists through 1967 (GSC VI) were given new pagination, whereas lists VII to XI (1968 to 1971) were reprinted with the same pagination. GEOLOGICAL SURVEY OF CANADA RADIOCARBON DATES XXVII Abstract This list presents 380 radiocarbon age determinations made by the Radiocarbon Dating Laboratory. Age determinations (323) on geological samples from various areas are as follows: Newfoundland (24); Nova Scotia (2); New Brunswick (2); Quebec (15); Ontario (36); Manitoba (12); British Columbia (57); Yukon Territory (10); Northwest Territories, mainland (43); Northwest Territories, Arctic Archipelago (121); Washington (1). Age determinations (57) on archeological samples are as follows: Newfoundland (1); Labrador (3); Nova Scotia (1); Ontario (5); Northwest Territories, Arctic Archipelago (47). Tables I and 2 summarize details of background and standard for the 2 L and 5 L counters during the period from August 1, 1986 to November 17, 1986; Table 3 gives the number of counts used to determine the average background and standard counting rates; and Table 4 lists the number of different background and standard gas preparations used for counting. Resume Ce rapport presente les resultats de 380 datations effectuees par le Laboratoire de datation au radiocarbone. Les datations (323) effectuees sur les echantillons geologiques proviennent des regions suivantes: Ile de Terre Neuve (24); Nouvelle-Ecosse (2); Nouveau-Brunswick (2); Quebec (15); Ontario (36); Manitoba (12); Colombie- Britannique (57); Yukon (10); Territoires du Nord-Ouest, continent (43); Territoires du Nord-Ouest, archipel Arctique (121); Washington (1). Les datations (57) effectuees sur les echantillons archeologiques sont: Ile de Terre-Neuve (I); Labrador (3); Nouvelle-Ecosse (1); Ontario (5); Territoires du Nord-Ouest, archipel Arctique (47). Tableaux 1 et 2 resument les valeurs de mouvement propre et de I'etalonnage des compteurs 2 L et 5 L, pour la periode allant du 1 aout 1986 au 17 novembre 1986; le tableau 3 donne le nombre de coups utilises pour determiner la moyenne des faux d'impulsions du mouvement propre et de I'etalonnage; et, le tableau 4 presente le nombre de preparations de gaz pour le mouvement propre et pour I'etalonnage utilisees pour le comptage. INTRODUCTION1 Table 1. Monthly average count for background during the period August 1, 1986 to November 17, 1986 During the period from August, 1986 through November 1986, both the 2 L counter (Dyck and 2 L Counter 5 L Counter Fyles, 1962) and the 5 L counter (Dyck et al., 1965) (2 atm) (1 atm) were operated continuously. The 2 L counter was Month cpm* cpm* operated at 2 atmospheres (atrn), and the 5 L counter August, 1986 1.593 + 0.027 3.343 f 0.039 was operated at 1 atmosphere throughout this September 1.805 + 0.066 3.613 f 0.097 period. October 2.018 f 0.047 4.040 k 0.101 The average background and oxalic acid November 2.204 + 0.032 4.359 + 0.096 standard counting rates which were used for age calculations are shown in Tables 1 and 2, *cpm = counts per minute respectively. On a monthly basis, the counting rates were within statistical limits. Table 3 lists the number of one-day counts used to determine the average background and oxalic acid standard Sample gas preparation and purification were counting rates for the period noted above, and carried out as described in Lowdon et aI. (1977). Table 4 gives the number of different background Carbon dioxide gas proportional counting techniques and (oxalic acid) standard-gas preparations used. have been discussed by Dyck (1967). For a recent 1 Data for the tables in the introduction were supplied by R.N. McNeely, Laboratory Supervisor since November 1981. The introduction follows the style developed by J.A. Lowdon. The date list has been compiled by W. Blake. Jr. from descriptions of samples and interpretations of age determinations provided by the collectors and submitters. Table 2. Monthly average count (No)* for oxalic acid O.O%o for marine shells. All 13C112C determinations standard during the period August 1, 1986 to were made on aliquots of the sample gas used for age November 17, 1986 determinations. Since 1975 all 13C112C ratios have 2 L Counter 5 L Counter been determined under contract by Professor P. Fritz (2 atm) (1 atm) and R.J. Drimmie of the Department of Earth Month CPm CPm Sciences, University of Waterloo, Waterloo, Ontario, August 1986 18.151 + 0.100 28.190 f 0.128 or by Waterloo Isotope Analysts, Inc., Kitchener, September 18.056 + 0.159 28.183 f 0.210 Ontario (R.J. Drimmie, chief analyst) using the same October 18.107 + 0.107 28.368 f 0.173 equipment as at the University of Waterloo. Prior to November 18.041 f 0.138 28.301 + 0.195 that time some 13C112C ratios were determined by the GSC Geochronology Section (R.K. Wanless, Head) and by Teledyne Isotopes, Westwood, New Jersey. *No = 0.95 of the net counting rate of the NBS oxalic acid standard Acknowledgments Appreciation is expressed to I.M. Robertson (1964 to Table 3. Number of one-day counts used to present), S.M. Chartrand (1969 to 19761, determine average counting rates for background and oxalic acid standard during the report period J.E. Tremblay (1976 to 1980), and A.M. Telka (1980 to 1986), and L.M. Mail16 (1986 to present) for the Background Standard preparation, purification, and counting o< samples in Month 2L 5L 2L 5L the laboratory. Supervision of laboratory operations August 1986 4 4 3 3 has been as follows: W. Dyck (1960 to 1965), September 4 4 3 3 J.A. Lowdon (1965 to 1981), and R.N. McNeely (1981 October 4 4 3 3 to present). November 3 2 1 1 Identification of materials used for dating or associated with the material being dated has been carried out by the following specialists, to whom Table 4. Number of monthly background and standard gas preparations used dur~ngthe report period I extend my sincere thanks: R.J. Mott, L.D. Farley- Gill (L.D. Wilson), and H. Jett6 (wood); N.F. Alley, Background Standard Department of Mines and Energy, South Australia, Month 2L 5L 2L 5L Eastwood, South Australia (formerly Ministry of the Environment, Province of British Columbia, August 1986 2 3 2 2 Victoria), J.E. Shepperd, formerly University of September 2 2 2 2 October 2 2 2 2 British Columbia, Vancouver, and R.J. Mott (pollen); November 2 2 1 1 J.P. Smol, Queen's University, Kingston (algae); S. Lichti-Federovich (diatoms and pollen); J.V. Matthews, Jr. (plant macrofossils and fossil review of laboratory operations the reader is referred arthropods); N.F. Alley (plant macrofossils); to Lowdon (1985). J.A. Janssens, University of Minnesota, Age calculations during the report period were Minneapolis, Minnesota, and W.A. Weber, done on a CDC Cyber 70 SerieslModel74 computer. University of Colorado, Boulder, Colorado (mosses); Calculations are based on a 14C half-life of 5568 f 30 M. Kuc, formerly GSC, Ottawa (mosses and plant years and 0.95 of the activity of the NBS oxalic acid macrofossils); A.H. Clarke, Jr. and M.F.I. Smith, standard. Ages are quoted in radiocarbon years both formerly National Museum of Natural Sciences, before 'present' (BP), where 'present' is taken to Ottawa, J.E. Dale, formerly GSC, now Queen's be 1950. The error assigned to each age has been University, Kingston, Ontario, the late W.H. Dall, calculated using only the counting errors of sample, U.S.
Recommended publications
  • Application Exempt Pursuant to NLCA 12
    NIRB File No.: 05AN089 Previous CWS File Nos.: NUN-MBS-14-10, NUN-NWA-14-06 Previous PC File Nos.: QNP-2008-C25108 DFO File No.: NU-07-0045 The Honourable Leona Aglukkaq Minister of Environment Government of Canada c/o Mia Pelletier, A/Habitat Specialist Canadian Wildlife Services P.O. Box 1870 Iqaluit, NU X0A 0H0 Sent via email: [email protected]; [email protected] Re: Application Exempt from the Requirement for Screening pursuant to Section 12.4.3 of the NLCA: Quark Expeditions’ “Quark Canadian Arctic 2015” Project, Kitikmeot and Qikiqtani (North and South Baffin) Regions Dear Mia Pelletier: On April 16, 2015 the Nunavut Impact Review Board (NIRB or Board) received an application from the Canadian Wildlife Service (CWS) for a new CWS Bird Sanctuary permit and CWS National Wildlife Area permit for Quark Expeditions’ “Quark Canadian Arctic 2015” project proposal. On April 24, 2015 the NIRB received a positive conformity determination (North Baffin Regional Land Use Plan) from the Nunavut Planning Commission for this file. Please be advised that the original project proposal (NIRB File No.: 05AN089) was received by the NIRB from the CWS on May 30, 2005 and was screened in accordance with Part 4, Article 12 of the Nunavut Land Claims Agreement (NLCA). On July 6, 2005 the NIRB issued a NLCA 12.4.4(a) screening decision to the Minister of Environment, Government of Canada, which indicated that the proposed project could proceed subject to the NIRB’s recommended project- specific terms and conditions. On April 25, 2008 the NIRB received an application for an amendment and renewal from the CWS to Quark Expeditions’ National Wildlife Area entry permit and a new CWS Bird Sanctuary permit for the above mentioned project.
    [Show full text]
  • Western Elements in the Early Thule Culture of the Eastern High Arctic PETER SCHLEDERMANN' and KAREN Mccullough'
    ARCTIC VOL. 33, NO. 4 (DECEMBER l-), P. 833-841 Western Elements in the Early Thule Culture of the Eastern High Arctic PETER SCHLEDERMANN' and KAREN McCULLOUGH' ABSTRACT. Excavations of Thule culture wintersites in the Bache Peninsula regionon the east coastof Ellesmere Island have yielded a numberof finds which indicate a strong relationship to cultural developments in the Bering Sea region. Specific elements under discussion include dwelling styles, clay pottery, needle cases, a brow band and harpoon heads. Evidence is presented suggesting an initial arrivalof the Thule cultureInuit in the eastern Arctic around 1050 A.D. INTRODUCTION Much has been writtenabout the origins and expansionof the Thule culture into the Canadian Arctic. That this event took place as a result of population move- ment and migration from the west is never seriously contested. However, the timing and causes of this movement are subjects of continuing debate. During the past three summers, excavations have taken placeon several Thule culture winter sites in the Bache Peninsula region onthe east coast of Ellesmere Island (Fig. 1). The winter settlements, containing approximately 150 house ruins distributed over 12 sites, span a 500 to 600 year occupation period which ended about 1700 A.D. The retreat of the Thule culture Inuit fromthis region to the more viable Thuledistrict in northwest Greenland probably marksthe final abandonment of the Canadian High Arctic as a semi-permanent settlement area. Research into the early Thule culture occupation in the study area has been one of several primary objectives, particularly in relation to the temporal and spatial &hities of the NQgdlit and Ruin Island phases initially described by Holtved (1944; 1954).
    [Show full text]
  • A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W
    ARCTIC VOL. 60, NO. 1 (MARCH 2007) P. 1–6 A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W. PARK1 and DOUGLAS R. STENTON2 (Received 13 June 2006; accepted in revised form 31 July 2006) ABSTRACT. In 1999 a team of geologists discovered an archaeological site near Cape Southwest, Axel Heiberg Island. On the basis of its location and the analysis of two artifacts removed from the site, the discoverers concluded that it was a hastily abandoned campsite created by Hans Krüger’s German Arctic Expedition, which was believed to have disappeared between Meighen and Amund Ringnes islands in 1930. If the attribution to Krüger were correct, the existence of this site would demonstrate that the expedition got farther on its return journey to Bache Peninsula than previously believed. An archaeological investigation of the site by the Government of Nunavut in 2004 confirmed its tentative attribution to the German Arctic Expedition but suggested that it is not a campsite, but the remains of a deliberately and carefully constructed cache. The finds suggest that one of the three members of the expedition may have perished before reaching Axel Heiberg Island, and that the survivors, in order to lighten their sledge, transported valued but heavy items (including Krüger’s geological specimens) to this prominent and well-known location to cache them, intending to return and recover them at some later date. Key words: German Arctic Expedition, Hans Krüger, archaeology, geology, Axel Heiberg Island, Nunavut RÉSUMÉ. En 1999, une équipe de géologues a découvert un lieu d’importance archéologique près du cap Southwest, sur l’île Axel Heiberg.
    [Show full text]
  • Examining Precontact Inuit Gender Complexity and Its
    EXAMINING PRECONTACT INUIT GENDER COMPLEXITY AND ITS DISCURSIVE POTENTIAL FOR LGBTQ2S+ AND DECOLONIZATION MOVEMENTS by Meghan Walley B.A. McGill University, 2014 A thesis submitted to the School of Graduate Studies In partial fulfillment of the requirements for the degree of Master of Arts Department of Archaeology Memorial University of Newfoundland May 2018 St. John’s, Newfoundland and Labrador 0 ABSTRACT Anthropological literature and oral testimony assert that Inuit gender did not traditionally fit within a binary framework. Men’s and women’s social roles were not wholly determined by their bodies, there were mediatory roles between masculine and feminine identities, and role-swapping was—and continues to be—widespread. However, archaeologists have largely neglected Inuit gender diversity as an area of research. This thesis has two primary objectives: 1) to explore the potential impacts of presenting queer narratives of the Inuit past through a series of interviews that were conducted with Lesbian Gay Bisexual Transgender Queer/Questioning and Two-Spirit (LGBTQ2S+) Inuit and 2) to consider ways in which archaeological materials articulate with and convey a multiplicity of gender expressions specific to pre-contact Inuit identity. This work encourages archaeologists to look beyond categories that have been constructed and naturalized within white settler spheres, and to replace them with ontologically appropriate histories that incorporate a range of Inuit voices. I ACKNOWLEDGEMENTS First and foremost, qujannamiik/nakummek to all of the Inuit who participated in interviews, spoke to me about my work, and provided me with vital feedback. My research would be nothing without your input. I also wish to thank Safe Alliance for helping me identify interview participants, particularly Denise Cole, one of its founding members, who has provided me with invaluable insights, and who does remarkable work that will continue to motivate and inform my own.
    [Show full text]
  • Hot Rocks from Cold Places: a Field, Geochemical and Geochronological Study from the High Arctic Large Igneous P Rovince (HALIP) at Axel Heiberg Island, Nunavut
    ! !"#$%"&'($)*"+$,"-.$/-0&1(2$3$451-.6$71"&81+5&0-$09.$ 71"&8*"9"-":5&0-$;#<.=$)*"+$#81$!5:8$3*&#5&$>0*:1$ ?:91"<($/*"@59&1$A!3>?/B$0#$3C1-$!15D1*:$?(-09.6$ E<90@<#$ $ $ by Cole Girard Kingsbury A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Earth Sciences Ottawa – Carleton Geoscience Centre and Carleton University Ottawa, Ontario © 2016 Cole Girard Kingsbury ! ! !"#$%&'$() ) ) ) ) ) ) ) ) ) ) The geology of the Arctic is greatly influenced by a period of widespread Cretaceous magmatic activity, the High Arctic Large Igneous Province (HALIP). Two major tholeiitic magmatic pulses characterize HALIP: an initial 120 -130 Ma pulse that affected Arctic Canada and formally adjacent regions of Svalbard (Norway) and Franz Josef Land (Russia). In Canada, this pulse fed lava flows of the Isachsen Formation. A second 90-100 Ma pulse that apparently only affected the Canadian side of the Arctic, fed flood basalts of the Strand Fiord Formation. The goal of this thesis is to improve understanding of Arctic magmatism of the enigmatic HALIP through field, remote sensing, geochemical and geochronology investigations of mafic intrusive rocks collected in the South Fiord area of Axel Heiberg Island, Nunavut, and comparison with mafic lavas of the Isachsen and Strand Fiord Formations collected from other localities on the Island. Ground-based and remote sensing observations of the South Fiord area reveal a complex network of mafic sills and mainly SSE-trending dykes. Two new U-Pb baddeleyite ages of 95.18 ± 0.35 Ma and 95.56 ± 0.24 Ma from South Fiord intrusions along with geochemical similarity confirm these intrusions (including the SSE-trending dykes) are feeders for the Strand Fiord Formation lavas.
    [Show full text]
  • A Historical and Legal Study of Sovereignty in the Canadian North : Terrestrial Sovereignty, 1870–1939
    University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 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 A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 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 ucpress@ ucalgary.ca 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 specificwork without breaching the artist’s copyright.
    [Show full text]
  • Research Cruise Report: Mission HLY031
    Research Cruise Report: Mission HLY031 Conducted aboard USCGC Healy In Northern Baffi n Bay and Nares Strait 21 July –16 August 2003 Project Title: Variability and Forcing of Fluxes through Nares Strait and Jones Sound: A Freshwater Emphasis Sponsored by the US National Science Foundation, Offi ce of Polar Programs, Arctic Division Table of Contents Introduction by Chief Scientist . 4 Science Program Summary . 6 Science Party List . 7 Crew List . 8 Science Component Reports CTD-Rosette Hydrography . 9 Internally recording CTD . 29 Kennedy Channel Moorings . 33 Pressure Array . 41 Shipboard ADCP . 47 Bi-valve Retrieval . 51 Coring . 55 Seabeam Mapping . 65 Aviation Science Report . 71 Ice Report . 79 Weather Summary . 91 Inuit Perspective . 95 Photojournalist Perspective . 101. Website Log . 105 Chief Scientist Log . 111 Recommendations . .125 Introduction Dr. Kelly Kenison Falkner Chief Scientist Oregon State University In the very early hours of July 17, 2003, I arrived at collected via the ship’s Seabeam system and the underway the USCGC Healy moored at the fueling pier in St. John’s thermosalinograph system was put to good use throughout Newfoundland, Canada to assume my role as chief scientist much of the cruise. for an ambitious interdisciplinary mission to Northern Part of our success can be attributed to luck with Mother Baffi n Bay and Nares St. This research cruise constitutes Nature. Winds and ice worked largely in our favor as we the inaugural fi eld program of a fi ve year collaborative wound our way northward. Our winds were generally research program entitled Variability and Forcing of moderate and out of the south and the ice normal to light.
    [Show full text]
  • Canadian Arctic North Greenland
    SPECIAL OFFER -SAVE £300 PER PERSON THE CANADIAN ARCTIC & NORTH GREENLAND AN EXPLORATION OF THE HIGH ARCTIC ABOARD THE HANSEATIC INSPIRATION 4 TH TO 23RD AUGUST 2023 Sisimiut or this expedition we are delighted to be working with our associates at Ice conditions determine FHapag-Lloyd Cruises and their five-star vessel, the Hanseatic Inspiration. the course This unusual voyage combines the remote Canadian Arctic with its diverse Ellesmere Island Hans Island Pim Island wildlife, history and rich Inuit culture with Greenland’s west coast of great ares trait mith ound towering cliffs, walls of glacial ice, winding fjords, vast icesheets and flowing Etah iorapaluk glaciers. evon Island aanaa ape ork The expedition begins with five days of exploration of the CanadianArctic. Lying north of mainland Canada, the Canadian Arctic Archipelago consists of CANADA 94 major islands and forms the world’s largest High Arctic land area. Here we Baffin Island GRNLAND follow in the footsteps of the legendary explorers including Amundsen, Baffin and Franklin, who over the course of 300 years risked their lives to search the Arctic for the fabled Northwest Passage between the Atlantic and the Pacific ummanna Oceans. Our journey continues to coastal Greenland, one of the last great Ilulissat wilderness areas where man has made little difference to the landscape and isko a isimiut tourists are still a rarity. It is a marvel to behold; for most visitors their first angerlussua encounter with Greenland is a humbling experience as they witness nature in Arctic ircle the raw and look out across a magnificent Arctic world.
    [Show full text]
  • 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.
    [Show full text]
  • Wolf-Sightings on the Canadian Arctic Islands FRANK L
    ARCTIC VOL. 48, NO.4 (DECEMBER 1995) P. 313–323 Wolf-Sightings on the Canadian Arctic Islands FRANK L. MILLER1 and FRANCES D. REINTJES1 (Received 6 April 1994; accepted in revised form 13 March 1995) ABSTRACT. A wolf-sighting questionnaire was sent to 201 arctic field researchers from many disciplines to solicit information on observations of wolves (Canis lupus spp.) made by field parties on Canadian Arctic Islands. Useable responses were obtained for 24 of the 25 years between 1967 and 1991. Respondents reported 373 observations, involving 1203 wolf-sightings. Of these, 688 wolves in 234 observations were judged to be different individuals; the remaining 515 wolf-sightings in 139 observations were believed to be repeated observations of 167 of those 688 wolves. The reported wolf-sightings were obtained from 1953 field-weeks spent on 18 of 36 Arctic Islands reported on: no wolves were seen on the other 18 islands during an additional 186 field-weeks. Airborne observers made 24% of all wolf-sightings, 266 wolves in 48 packs and 28 single wolves. Respondents reported seeing 572 different wolves in 118 separate packs and 116 single wolves. Pack sizes averaged 4.8 ± 0.28 SE and ranged from 2 to 15 wolves. Sixty-three wolf pups were seen in 16 packs, with a mean of 3.9 ± 2.24 SD and a range of 1–10 pups per pack. Most (81%) of the different wolves were seen on the Queen Elizabeth Islands. Respondents annually averaged 10.9 observations of wolves ·100 field-weeks-1 and saw on average 32.2 wolves·100 field-weeks-1· yr -1 between 1967 and 1991.
    [Show full text]
  • Geographical Report of the Crocker Land Expedition, 1913-1917
    5.083 (701) Article VL-GEOGRAPHICAL REPORT OF THE CROCKER LAND EXPEDITION, 1913-1917. BY DONALD B. MACMILLAN CONTENTS PAGE INTRODUCTION......................................................... 379 SLEDGE TRIP ON NORTH POLAR SEA, SPRING, 1914 .......................... 384 ASTRONOMICAL OBSERVATIONS-ON NORTH POLAR SEA, 1914 ................ 401 ETAH TO POLAR SEA AND RETURN-MARCH AVERAGES .............. ........ 404 WINTER AND SPRING WORK, 1915-1916 ............. ......................... 404 SPRING WORK OF 1917 .................................... ............ 418 GENERAL SUMMARY ....................................................... 434 INTRODUCTJON The following report embraces the geographical work accomplished by the Crocker Land Expedition during -four years (Summer, 19.13, to Summer, 1917) spent at Etah, NortJaGreenland. Mr. Ekblaw, who was placed in charge of the 1916 expeditin, will present a separate report. The results of the expedition, naturally, depended upon the loca tion of its headquarters. The enforced selection of Etah, North Green- land, seriously handicapped the work of the expedition from start to finish, while the. expenses of the party were more than doubled. The. first accident, the grounding of the Diana upon the coast of Labrador, was a regrettable adventure. The consequent delay, due to unloading, chartering, and reloading, resulted in such a late arrival at Etah that our plans were disarranged. It curtailed in many ways the eageimess of the men to reach their objective point at the head of Flagler Bay, te proposed site of the winter quarters. The leader and his party being but passengers upon a chartered ship was another handicap, since the captain emphatically declared that he would not steam across Smith Sound. There was but one decision to be made, namely: to land upon the North Greenland shore within striking distance of Cape Sabine.
    [Show full text]
  • ESTIMATING PEARY CARIBOU (Rangifer Tarandus Pearyi) and MUSKOX (Ovibos Moschatus) NUMBERS, COMPOSITION and DISTRIBUTIONS on the HIGH ARCTIC ISLANDS of NUNAVUT
    ESTIMATING PEARY CARIBOU (Rangifer tarandus pearyi) AND MUSKOX (Ovibos moschatus) NUMBERS, COMPOSITION AND DISTRIBUTIONS ON THE HIGH ARCTIC ISLANDS OF NUNAVUT Mitch Campbell1 1Regional Wildlife Biologist, Department of Environment, Government of Nunavut, P.O. Box 120, Arviat, NU X0C 0E0 2006 Status Report, No. 19 Campbell, M. 2006. Estimating Peary caribou (Rangifer tarandus pearyi) and muskox (Ovibos moschatus) numbers, composition and distributions on Ellesmere Island, Nunavut. Government of Nunavut, Department of Environment, Status report: 19, Iqaluit, 12 pp. SUMMARY REPORT TO NUNAVUT CO-MANAGERS Prepared By: Mitch W. Campbell Regional Biologist Department of Environment Wildlife Research Division P.O. 120 Arviat, Nu X0C 0E0 Ph: (867)857-2828 Fax: (867)857-2986 E-mail: [email protected] June 15th, 2006 Title: Estimating Peary Caribou (Rangifer tarandus pearyi) and Muskox (Ovibos moschatus) Numbers, Composition and Distributions on Ellesmere Island, Nunavut. Summary: The scientific study of Peary caribou and Muskox on Nunavut’s high arctic islands has been ongoing since May 2000. The data collected thus far on West Devon Island, Bathurst Island and Ellesmere Island are being analyzed and archived. The resulting file report will include a history of scientific study of Peary Caribou, the methods used during these studies, the population estimates of all surveys up to and including the 2006 Ellesmere survey, an analysis of satellite collar movement data, a resource selection analysis examining Peary caribou habitat, a summary of IQ collected by GN Biologists and a in-depth section pulling all aspects of the report into comprehensive management recommendations for the future study and continued co-management of Peary Caribou in Nunavut.
    [Show full text]