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Cosmology and Shamanism and Shamanism INTERVIEWING INUIT ELDERS
6507.3 Eng Cover w/spine/bleed 5/1/06 9:23 AM Page 1 INTERVIEWINGCosmology INUIT ELDERS and Shamanism Cosmology and Shamanism INTERVIEWING INUIT ELDERS Mariano and Tulimaaq Aupilaarjuk, Lucassie Nutaraaluk, Rose Iqallijuq, Johanasi Ujarak, Isidore Ijituuq and Michel Kupaaq 4 Edited by Bernard Saladin d’Anglure 6507.5_Fre 5/1/06 9:11 AM Page 239 6507.3 English Vol.4 5/1/06 9:21 AM Page 1 INTERVIEWING INUIT ELDERS Volume 4 Cosmology and Shamanism Mariano and Tulimaaq Aupilaarjuk, Lucassie Nutaraaluk, Rose Iqallijuq, Johanasi Ujarak, Isidore Ijituuq and Michel Kupaaq Edited by Bernard Saladin d’Anglure 6507.3 English Vol.4 5/1/06 9:21 AM Page 2 Interviewing Inuit Elders Volume 4 Cosmology and Shamanism Copyright © 2001 Nunavut Arctic College, Mariano and Tulimaaq Aupilaarjuk, Bernard Saladin d’Anglure and participating students Susan Enuaraq, Aaju Peter, Bernice Kootoo, Nancy Kisa, Julia Saimayuq, Jeannie Shaimayuk, Mathieu Boki, Kim Kangok, Vera Arnatsiaq, Myna Ishulutak, and Johnny Kopak. Photos courtesy Bernard Saladin d’Anglure; Frédéric Laugrand; Alexina Kublu; Mystic Seaport Museum. Louise Ujarak; John MacDonald; Bryan Alexander. Illustrations courtesy Terry Ryan in Blodgett, ed. “North Baffin Drawings,” Art Gallery of Ontario; 1923 photo of Urulu, Fifth Thule Expedition. Cover illustration “Man and Animals” by Lydia Jaypoody. Design and production by Nortext (Iqaluit). All rights reserved. The use of any part of this publication, reproduced, transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, or stored in a retrieval system, without written consent of the publisher is an infringement of the copyright law. ISBN 1-896-204-384 Published by the Language and Culture Program of Nunavut Arctic College, Iqaluit, Nunavut with the generous support of the Pairijait Tigummivik Elders Society. -
The Rock Abrasion Record at Gale Crater: Mars Science Laboratory
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE The rock abrasion record at Gale Crater: Mars 10.1002/2013JE004579 Science Laboratory results from Bradbury Special Section: Landing to Rocknest Results from the first 360 Sols of the Mars Science Laboratory N. T. Bridges1, F. J. Calef2, B. Hallet3, K. E. Herkenhoff4, N. L. Lanza5, S. Le Mouélic6, C. E. Newman7, Mission: Bradbury Landing D. L. Blaney2,M.A.dePablo8,G.A.Kocurek9, Y. Langevin10,K.W.Lewis11, N. Mangold6, through Yellowknife Bay S. Maurice12, P.-Y. Meslin12,P.Pinet12,N.O.Renno13,M.S.Rice14, M. E. Richardson7,V.Sautter15, R. S. Sletten3,R.C.Wiens6, and R. A. Yingst16 Key Points: • Ventifacts in Gale Crater 1Applied Physics Laboratory, Laurel, Maryland, USA, 2Jet Propulsion Laboratory, Pasadena, California, USA, 3Department • Maybeformedbypaleowind of Earth and Space Sciences, College of the Environments, University of Washington, Seattle, Washington, USA, 4U.S. • Can see abrasion textures at range 5 6 of scales Geological Survey, Flagstaff, Arizona, USA, Los Alamos National Laboratory, Los Alamos, New Mexico, USA, LPGNantes, UMR 6112, CNRS/Université de Nantes, Nantes, France, 7Ashima Research, Pasadena, California, USA, 8Universidad de Alcala, Madrid, Spain, 9Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Supporting Information: Austin, Texas, USA, 10Institute d’Astrophysique Spatiale, Université Paris-Sud, Orsay, France, 11Department of • Figure S1 12 fi • Figure S2 Geosciences, Princeton University, Princeton, New Jersey, USA, Centre National de la Recherche Scienti que, Institut 13 • Table S1 de Recherche en Astrophysique et Planétologie, CNRS-Université Toulouse, Toulouse, France, Department of Atmospheric, Oceanic, and Space Science; College of Engineering, University of Michigan, Ann Arbor, Michigan, USA, Correspondence to: 14Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA, 15Lab N. -
Chemical Variations in Yellowknife Bay Formation Sedimentary Rocks
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE Chemical variations in Yellowknife Bay formation 10.1002/2014JE004681 sedimentary rocks analyzed by ChemCam Special Section: on board the Curiosity rover on Mars Results from the first 360 Sols of the Mars Science Laboratory N. Mangold1, O. Forni2, G. Dromart3, K. Stack4, R. C. Wiens5, O. Gasnault2, D. Y. Sumner6, M. Nachon1, Mission: Bradbury Landing P.-Y. Meslin2, R. B. Anderson7, B. Barraclough4, J. F. Bell III8, G. Berger2, D. L. Blaney9, J. C. Bridges10, through Yellowknife Bay F. Calef9, B. Clark11, S. M. Clegg5, A. Cousin5, L. Edgar8, K. Edgett12, B. Ehlmann4, C. Fabre13, M. Fisk14, J. Grotzinger4, S. Gupta15, K. E. Herkenhoff7, J. Hurowitz16, J. R. Johnson17, L. C. Kah18, N. Lanza19, Key Points: 2 1 20 21 12 16 2 • J. Lasue , S. Le Mouélic , R. Léveillé , E. Lewin , M. Malin , S. McLennan , S. Maurice , Fluvial sandstones analyzed by 22 22 23 19 19 24 25 ChemCam display subtle chemical N. Melikechi , A. Mezzacappa , R. Milliken , H. Newsom , A. Ollila , S. K. Rowland , V. Sautter , variations M. Schmidt26, S. Schröder2,C.d’Uston2, D. Vaniman27, and R. Williams27 • Combined analysis of chemistry and texture highlights the role of 1Laboratoire de Planétologie et Géodynamique de Nantes, CNRS, Université de Nantes, Nantes, France, 2Institut de Recherche diagenesis en Astrophysique et Planétologie, CNRS/Université de Toulouse, UPS-OMP, Toulouse, France, 3Laboratoire de Géologie de • Distinct chemistry in upper layers 4 5 suggests distinct setting and/or Lyon, Université de Lyon, Lyon, France, California Institute of Technology, Pasadena, California, USA, Los Alamos National 6 source Laboratory, Los Alamos, New Mexico, USA, Earth and Planetary Sciences, University of California, Davis, California, USA, 7Astrogeology Science Center, U.S. -
Constraints on the Depth and Thermal Vigor of Melting in the Martian Mantle
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE Constraints on the depth and thermal vigor 10.1002/2014JE004745 of melting in the Martian mantle Key Points: Justin Filiberto1 and Rajdeep Dasgupta2 • Mantle potential temperature calculated for Gale Crater rocks 1Department of Geology, Southern Illinois University, Carbondale, Illinois, USA, 2Department of Earth Science, Rice • 1450 ± 70°C may represent global Noachian mantle temperature University, Houston, Texas, USA • Consistent with simple convective cooling of the interior of Mars Abstract Studies of rocks in Gale Crater and clasts within the Martian meteorite breccia Northwest Africa (NWA) 7034 (and paired stones) have expanded our knowledge of the diversity of igneous rocks that make up the Martian crust beyond those compositions exhibited in the meteorite collection or Correspondence to: J. Filiberto, analyzed at any other landing site. Therefore, the magmas that gave rise to these rocks may have been fi[email protected] generated at significantly different conditions in the Martian mantle than those derived from previously studied rocks. Here we build upon our previous models of basalt formation based on rocks analyzed in Citation: Gusev Crater and Meridiani Planum to the new models of basalt formation for compositions from Gale Filiberto, J., and R. Dasgupta (2015), Crater and a clast in meteorite NWA 7034. Estimates for the mantle potential temperature, TP based on Constraints on the depth and thermal vigor of melting in the Martian mantle, Noachian age rock analyses in Gale Crater, Gusev Crater, and Bounce Rock in Meridiani Planum, and a J. Geophys. Res. Planets, 120, vitrophyre clast in NWA 7034 are within error, which suggests that the calculated average TP of 1450 ± 70°C doi:10.1002/2014JE004745. -
Atlantic Walrus Odobenus Rosmarus Rosmarus
COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour. -
Valerie Payre: Resume
Valerie Payre: Resume Payré Valérie 10 rue Saint-Julien Birth Date: 08/06/1991 54000 Nancy, France Place of Birth: Charenton-le-Pont (France) Email: [email protected] Nationality: French Phone: +3361 515 1373 Research Experiences 2018 - today Wiess Postdoctoral Research Associate, EEPS, Rice University, Houston, TX, USA Mentors, Rajdeep Dasgupta and Kirsten Siebach. Oct. 2017 – Mar. Staff Scientist, MSL Science Team Collaborator, ChemCam 2018 Playload Downlink Lead, Centre National de la Recherche Scientifique (CNRS) – IRAP - GeoRessources, Nancy, France 2014 – 2017 Ph.D., MSL Science Team Collaborator, ChemCam Playload Downlink Lead, GeoRessources, Nancy, France Advisors, Cécile Fabre and Violaine Sautter. ‘ChemCam contribution to the understanding of the primitive martian crust and alteration processes occurring at the surface of Mars – Alkaline and metal trace element quantifications using LIBS (Li, Sr, Rb, Ba and Cu)’ Technical skills: Laser Induced Breakdown Spectroscopy (LIBS), samples preparation, igneous glass synthesis, electonic microprobe, SEM, LA-ICP-MS, X-ray computed tomography, univariate calibration, Matlab. Summary: LIBS calibrations of Li, Sr, Rb, Ba, and Cu and major elements using univariate models – Understanding of processes causing elevated Li, Rb, Sr and Ba concentrations along Curiosity traverse in the first 1000 sols - Constrain the origin of copper enrichments at Kimberley – Understanding of the primitive martian crust using Gale igneous alkaline rocks, the igneous clasts from the martian breccia NWA7533/7034, and orbital data – Comparison between the primitive martian crust and the Archean crust - Characterization of Bathurst-like rocks. Feb. – Jun. 2014 Grad. Student Research Assistant, Isotope Stable, IPGP, Paris, France Advisors, Isabelle Martinez and Mathilde Cannat. ‘Carbonation of natural serpentines dragged in the Indian Ocean ridge.’ Technical skills: Microprobe, SEM, DRX, Raman, FIB sampling preparation, TEM, autoclave experiments. -
Mclennan(2014)
Elemental Geochemistry of Sedimentary Rocks at Yellowknife Bay, Gale Crater, Mars S. M. McLennan et al. Science 343, (2014); DOI: 10.1126/science.1244734 This copy is for your personal, non-commercial use only. If you wish to distribute this article to others, you can order high-quality copies for your colleagues, clients, or customers by clicking here. Permission to republish or repurpose articles or portions of articles can be obtained by following the guidelines here. The following resources related to this article are available online at www.sciencemag.org (this information is current as of January 24, 2014 ): Updated information and services, including high-resolution figures, can be found in the online version of this article at: on January 24, 2014 http://www.sciencemag.org/content/343/6169/1244734.full.html Supporting Online Material can be found at: http://www.sciencemag.org/content/suppl/2013/12/05/science.1244734.DC1.html This article cites 53 articles, 13 of which can be accessed free: http://www.sciencemag.org/content/343/6169/1244734.full.html#ref-list-1 This article has been cited by 3 articles hosted by HighWire Press; see: http://www.sciencemag.org/content/343/6169/1244734.full.html#related-urls www.sciencemag.org This article appears in the following subject collections: Planetary Science http://www.sciencemag.org/cgi/collection/planet_sci Downloaded from Science (print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by the American Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005. Copyright 2014 by the American Association for the Advancement of Science; all rights reserved. -
Download Chapter
Chapter 13 The Muskrats of North America Other Than Ondatra zibethicus zibethicus THE FIFTEEN RECOGNIZED FORMS of muskrats having North American ranges outside of the range of 0. z. zibethicus show many differences as to population status, habitats, and geographical distribution. Of these other muskrats, 0. z. cinnamominus - the subspecies with which, next to zibethicus, I have had the most experience - can be notable for its low densities over tremendous areas of the arid and semiarid Great Plains; it may hardly be represented at all for stretches of hundreds of miles, yet seldom does it fail nominally to hold essentially its regular range, and it often reaches typical muskrat abundance m suitable marsh or stream habitats. "\\!estward from the range of cinnamominus extend the ranges of the evidently closely related mergens, occipitalis, and osoyoosensis. The one of these having the smallest range, occipitalis, &hows some behavior differences, whereas the widely distributed osoyoosensis is probably as versatile with respect to habitats and climate as any musk rat subspecies, including zibethicus. It is true that zibethicus in northern Ontario and osoyoosensis at high altitudes in western United States illustrate muskrat adaptability to long cold winters and marginal habitats as well as do any of what may be called the true northern muskrats - obscurus, aquilonius, a/bus, zalophus, and spatulatus. Nevertheless, much may still be learned from this latter group about what constitutes habitability of northern muskrat range and what muskrats can there endure in the way of edge-of-range phenomena. The subspecies macrodon, rivalicius, ripensis, bernardi, goldmani, and pallidus are all natives of warm climates and all have restricted geographic ranges. -
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: -
POSTER SESSION: GENESIS MISSION: TARGET HANDLING and SOLAR WIND ABUNDANCES 6:00 P.M
Tuesday, March 19, 2013 [T601] POSTER SESSION: GENESIS MISSION: TARGET HANDLING AND SOLAR WIND ABUNDANCES 6:00 p.m. Town Center Exhibit Area Allton J. H. Rodriguez M. C. Burkett P. J. Ross D. K. Gonzalez C. P. et al. POSTER LOCATION #1 Recent Optical and SEM Characterization of Genesis Solar Wind Concentrator Diamond-on-Silicon Collector [#2466] Observations of contaminants and irradiation damage on diamond-on-silicon surface and postsubdivision imaging. Burkett P. J. Allton J. A. Clemett S. J. Gonzales C. P. Lauer H. V. Jr et al. POSTER LOCATION #2 Plan for Subdividing Genesis Mission Diamond-on-Silicon 60000 Solar Wind Collector [#2837] Using innovative laser scribing and cleaving techniques, Genesis sample 60000 was subdivided resulting subsamples for allocation and analysis. Lauer H. V. Burket P. J. Rodriguez M. C. Nakamura-Messenger K. Clemett S. J. et al. POSTER LOCATION #3 Laser Subdivision of the Genesis Concentrator Target Sample 60000 [#2691] The Genesis Allocation Committee received a request for ~ 1 cm2 of the target sample 60000. We describe the cutting plan used to provide the allocation. Rodriguez M. R. Allton J. H. Burkett P. J. Gonzalez C. P. POSTER LOCATION #4 Examples of Optical Assessment of Surface Cleanliness of Genesis Samples [#2515] We present recent examples of optically surveyed Genesis samples as part of a cleaning plan intended to create a set of “assessed clean” samples for allocation. Kuhlman K. R. Rodgriguez M. C. Gonzalez C. P. Allton J. H. Burnett D. S. POSTER LOCATION #5 Cleaning Study of Genesis Sample 60487 [#2930] This examination of the efficacy of various cleaning methods was conducted using correlative microscopy of Genesis sample 60487. -
Ideas, 11 | Printemps/Été 2018 Opera in the Arctic: Knud Rasmussen, Inside and Outside Modernity 2
IdeAs Idées d'Amériques 11 | Printemps/Été 2018 Modernités dans les Amériques : des avant-gardes à aujourd’hui Opera in the Arctic: Knud Rasmussen, Inside and Outside Modernity L’Opéra dans l’Arctique : Knud Rasmussen, traversées de la modernité Ópera en el Árctico: Knud Rasmussen, travesías de la modernidad Smaro Kamboureli Electronic version URL: http://journals.openedition.org/ideas/2553 DOI: 10.4000/ideas.2553 ISSN: 1950-5701 Publisher Institut des Amériques Electronic reference Smaro Kamboureli, « Opera in the Arctic: Knud Rasmussen, Inside and Outside Modernity », IdeAs [Online], 11 | Printemps/Été 2018, Online since 18 June 2018, connection on 21 April 2019. URL : http://journals.openedition.org/ideas/2553 ; DOI : 10.4000/ideas.2553 This text was automatically generated on 21 April 2019. IdeAs – Idées d’Amériques est mis à disposition selon les termes de la licence Creative Commons Attribution - Pas d'Utilisation Commerciale - Pas de Modification 4.0 International. Opera in the Arctic: Knud Rasmussen, Inside and Outside Modernity 1 Opera in the Arctic: Knud Rasmussen, Inside and Outside Modernity L’Opéra dans l’Arctique : Knud Rasmussen, traversées de la modernité Ópera en el Árctico: Knud Rasmussen, travesías de la modernidad Smaro Kamboureli I. Early 1920s: under western eyes 1 When Greenlander / Danish ethnographer Knud Rasmussen approached a small Padlermiut camp in what is today the Kivalliq Region of Nunavut, Canada, he was surprised to hear “a powerful gramophone struck up, and Caruso’s mighty voice [ringing] out from his tent” (Rasmussen, K., 1927: 63). It was 1922, and the Inuktitut-speaking Rasmussen was after traditional Inuit knowledge, specifically spiritual and cultural practices. -
An Archaeological View of the Thule / Inuit Occupation of Labrador
AN ARCHAEOLOGICAL VIEW OF THE THULE / INUIT OCCUPATION OF LABRADOR Lisa K. Rankin Memorial University May 2009 AN ARCHAEOLOGICAL VIEW OF THE THULE/INUIT OCCUPATION OF LABRADOR Lisa K. Rankin Memorial University May 2009 TABLE OF CONTENTS I. INTRODUCTION........................................................................................................................1 II. BACKGROUND .........................................................................................................................3 1. The Thule of the Canadian Arctic ......................................................................................3 2. A History of Thule/Inuit Archaeology in Labrador............................................................6 III. UPDATING LABRADOR THULE/INUIT RESEARCH ...................................................15 1. The Date and Origin of the Thule Movement into Labrador ...........................................17 2. The Chronology and Nature of the Southward Expansion...............................................20 3. Dorset-Thule Contact .......................................................................................................28 4. The Adoption of Communal Houses................................................................................31 5. The Internal Dynamics of Change in Inuit Society..........................................................34 IV. CONCLUSION ........................................................................................................................37 V. BIBLIOGRAPHY......................................................................................................................39