Sr-126 Drilling Through the Greenland Ice Sheet
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Re-Introducing Sports Stores
780-594-4414 5118 50 Avenue, Cold Lake Helping you is what we do! www.northernlightsrealestate.com Approved Relocation Supplier Nous offrons un service bilingue Northern Lights Realty Ltd. INDEPENDENTLY OWNED AND OPERATED Volume 54 Number 5 www.couriernews.ca February 2, 2021 Re-introducing Sports Stores Joy Smith Joy Smith Introducing the newest member of the Col Sports Stores has a wide variety of outdoor activity equipment for the Defence Team to borrow, J.J. Parr Sports Centre staff, Megan Garrett. including several six-man ice fishing tents (pictured) as well as a few 4-man tents. Ice fishing Megan is the new Sports Stores Technician. gear included! JOY SMITH, REPORTER 4 Wing Cold Lake maintains several kilometres fishing gear are limited and they book up fast, so plan of groomed Cross Country Ski trails at the Cold ahead. A new face will be greeting patrons of the Col Lake Golf and Winter Club. Cross country ski boots, Pick up and returns to Sports Stores are by J.J. Parr Sports Centre Sports Stores. Megan Garrett skis and poles are available in a limited number appointment only as per COVID-19 regulations. has joined the PSP team as the new Sports Stores of sizes for children as well as adults. No helmets Military members and members of the Defence Team Technician. Raised in Moose Jaw, Megan made her are provided. can sign out equipment and gear necessary. Members way to Cold Lake via New Brunswick and British If skiing isn’t your speed then give snow shoeing signing out equipment will be asked to complete some Columbia, then returning to Moose Jaw to wait out a try. -
Ice Businesses at Turners Falls, Massachusetts Turners Falls Reporter
Ice Businesses at Turners Falls Ice Businesses at Turners Falls, Massachusetts Reported in the Turners Falls Reporter for the years in this compilation. August, 2017 Page 1 of 24 Ed Gregory Ice Businesses at Turners Falls Ice Businesses at Turners Falls, Massachusetts Reported in the Turners Falls Reporter for the years in this compilation Pages of the Turners Falls Reporter given in this compilation are verbatim. Grammar, Punctuation and Spelling are as in the archetype. Evident edits are displayed via [sic]1 Composed, printed & bound by Ed Gregory August, 2017 1 Thus; so. Used to indicate that a quoted passage, especially one containing an error or unconventional spelling, has been retained in its original form or written intentionally. August, 2017 Page 2 of 24 Ed Gregory Ice Businesses at Turners Falls Content - Year 1873 4 1913 18 1874 4 1914 19 1875 4 1915 19 1876 No editions available for 1876 or, from January,1877 to April, 1877 1877 4 1916 19 1878 4 1917 20 1879 5 1918 20 1880 No ice info. 1919 21 1881 5 1920 21 1882 5 1921 22 1883 6 1922 22 1884 7 -end- 1885 7 1886 7 1887 8 1888 8 1889 9 1890 9 1891 9 1892 9 1893 10 1894 10 1895 10 1896 11 1897 11 1898 11 1899 12 1900 12 1901 13 1902 13 1903 14 1904 14 1905 14 1906 14 1907 15 1908 15 1909 16 1910 17 1911 17 1912 17 August, 2017 Page 3 of 24 Ed Gregory Ice Businesses at Turners Falls Ice Businesses at Turners Falls, Massachusetts as reported in the Turners Falls Reporter for the years 1872 to 1922. -
Udenrigspolitisk Redegørelse 2018
EM/2018/14 Udenrigspolitisk Redegørelse 2018 Billede: National Aeronautics and Space Administration (NASA) EM 2018/14 Sags nr. 2018 – 2195 EM 2018/14 Side 1 af 86 1. Indledning For at sikre Grønlands synlighed og interesser internationalt, er det vigtigt at vores land er en aktiv aktør i den internationale politik. Det er derfor vigtigt med en nødvendig repræsentation i vores primære samarbejdslande, samt videre vigtigt at deltage og markere sig i internationale møder og konferencer. Jeg havde således fornøjelsen, sammen med Udenrigsminister Anders Samuelsen, den 22. og 23. maj 2018, at markere 10 året for vedtagelsen af Ilulissat erklæringen, en absolut skelsættende begivenhed for vores land og Arktisk og en erklæring som har været med til at sikre fred og stabilitet i den arktiske region. Foruden værterne deltog repræsentanter fra USA, Canada, Rusland, Finland, Sverige, Norge, Island og Færøerne samt repræsentanter for ICC og Samerådet. Alle medlemslandene fra Arktisk Råd, samt de 6 oprindelige folks organisationer repræsenteret i Arktisk Råd, var således inviteret til markeringen, således en større kreds, end de 5 arktiske kyststater, der vedtog erklæringen tilbage i 2008. Denne udvidelse af kredsen blev gennemført med henblik på større medinddragelse af de aktører, som implementerer principperne i erklæringen. På ministermødet blev vigtigheden af at fokusere på den arktiske befolkning fremhævet. Vores mest fremtrædende opgave i Arktisk er at vi som folk er med til at lede dialogen om, og udviklingen af, vores region. Den grønlandske repræsentation i Reykjavik er nu under etablering, og forventes endelig officielt åbnet i 4. kvartal af 2018. Repræsentationen forventes at bidrage til at vedligeholde og udvide de eksisterende samarbejder med Island, samt styrke de politiske og handelsmæssige forbindelser. -
The Criteria for the Choice of the Fluid for Ice Deep
r_ r: r] FGRffirereM&Hffi : I bv P. G. Ta lalayt'z and N. S. Gun destrup2 I St.Peters b urg Stote Mining Institute 21 I Line,2 St.Petersburg 199026, Russia 2[]niversi4, of Copenhagen, Deportntent of Geophysics JuliaT Maries Vej 30, DK-2100 Copenhagen O, Denmark i l K*t /;'/88//,}?4= t}=ii ri/ n H- ,i ii lj'j E\UE llUlrli , 9+ \5- \s;.( Copenhagen 1999 \ I CONTENTS Introduction …………………………………………………………………………… 3 1. Types of hole fluids for deep ice core drilling …………………………………… 5 Classification of ice drilling fluids Petroleum oil products Densifiers Alcohols, esters and other organic liquids Silicon oils 2. Density and fluid top ……………………………………………………………… 13 General considerations Fluid top Density profile of ice Approximate density profile of fluid Real density profile of fluid Density profile of two-compound fluid Hydrostatic pressure and density profile in GISP2 bore-hole at Summit, Greenland Pressure difference and choice of the fluid density Choice of the fluid density for 3000-m bore-hole at Central Greenland 3. Bore-hole closure rate …………………………………………………………….. 37 Bore-hole closure and drilling technology Ice creep Flow parameter A Enhancement coefficient Glen’s Law power n Glen’s Law and the rate of the bore-hole closure Prognosis of the bore-hole closure 4. Viscosity …………………………………………………………………………… 48 General considerations The rational values of average drill’s lowering/hoisting rate Fluid viscosity and free drill’s lowering rate Viscosity of drilling fluid versus temperature Viscosity of drilling fluid versus pressure Resume 5. Frost-resistance …………………………………………………………………... 64 6. Stability …………………………………………………………………………… 67 Stability of drilling fluids during storage and transportation Stability of drilling fluids in bore-hole 1 7. -
Exploring Greenland: Science and Technology in Cold War Settings Matthias Heymann, Henrik Knudsen, Maiken L
Document generated on 09/28/2021 8:37 a.m. Scientia Canadensis Canadian Journal of the History of Science, Technology and Medicine Revue canadienne d'histoire des sciences, des techniques et de la médecine Exploring Greenland: Science and Technology in Cold War Settings Matthias Heymann, Henrik Knudsen, Maiken L. Lolck, Henry Nielsen, Kristian H. Nielsen and Christopher J. Ries Comparative Issues in the History of Circumpolar Science and Article abstract Technology This paper explores a vacant spot in the Cold War history of science: the Volume 33, Number 2, 2010 development of research activities in the physical environmental sciences and in nuclear science and technology in Greenland. In the post-war period, URI: https://id.erudit.org/iderudit/1006149ar scientific exploration of the polar areas became a strategically important DOI: https://doi.org/10.7202/1006149ar element in American and Soviet defence policy. Particularly geophysical fields like meteorology, geology, seismology, oceanography, and others profited greatly from military interest. While Denmark maintained formal sovereignty See table of contents over Greenland, research activities were strongly dominated by U.S. military interests. This paper sets out to summarize the limited current state of knowledge about activities in the environmental physical sciences in Publisher(s) Greenland and their entanglement with military, geopolitical, and colonial interests of both the USA and Denmark. We describe geophysical research in CSTHA/AHSTC the Cold War in Greenland as a multidimensional colonial endeavour. In a period of decolonization after World War II, Greenland, being a Danish colony, ISSN became additionally colonized by the American military. Concurrently, in a 0829-2507 (print) period of emerging scientific internationalism, the U.S. -
The Abandoned Ice Sheet Base at Camp Century, Greenland, in a Warming Climate
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2016 The abandoned ice sheet base at Camp Century, Greenland, in a warming climate Colgan, William ; Machguth, Horst ; MacFerrin, Mike ; Colgan, Jeff D ; van As, Dirk ; MacGregor, Joseph A Abstract: In 1959 the U.S. Army Corps of Engineers built Camp Century beneath the surface of the northwestern Greenland Ice Sheet. There they studied the feasibility of deploying ballistic missiles within the ice sheet. The base and its wastes were abandoned with minimal decommissioning in 1967, under the assumption they would be preserved for eternity by perpetually accumulating snowfall. Here we show that a transition in ice sheet surface mass balance at Camp Century from net accumulation to net ablation is plausible within the next 75 years, under a business-as-usual anthropogenic emissions scenario (Representative Concentration Pathway 8.5). Net ablation would guarantee the eventual remobilization of physical, chemical, biological, and radiological wastes abandoned at the site. While Camp Century and four other contemporaneous ice sheet bases were legally established under a Danish-U.S. treaty, the potential remobilization of their abandoned wastes, previously regarded as sequestered, represents an entirely new pathway of political dispute resulting from climate change. DOI: https://doi.org/10.1002/2016GL069688 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-126150 Journal Article Published Version The following work is licensed under a Creative Commons: Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) License. -
The Multiscale Structure of Antarctica Part I : Inland Ice
Title The Multiscale Structure of Antarctica Part I : Inland Ice Faria, Sérgio H.; Kipfstuhl, Sepp; Azuma, Nobuhiko; Freitag, Johannes; Weikusat, Ilka; Murshed, M. Mangir; Kuhs, Author(s) Werner F. 低温科学, 68(Supplement), 39-59 Citation Physics of Ice Core Records II : Papers collected after the 2nd International Workshop on Physics of Ice Core Records, held in Sapporo, Japan, 2-6 February 2007. Edited by Takeo Hondoh Issue Date 2009-12 Doc URL http://hdl.handle.net/2115/45430 Type bulletin (article) Note I. Microphysical properties, deformation, texture and grain growth File Information LTS68suppl_005.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP The Multiscale Structure of Antarctica Part I: Inland Ice Sergio H. Faria -t , Sepp Kipfstuhl .. , Nobuhiko Azuma ... , Johannes Frei tag •• , Ilka Weikusat .. , M. Mangir MU fshed • , Werner F. Kuhs • * cze. Sect. a/Crystallography, Universityo[Gotlingen. COl/illgen, GermallY ** Alfred iVegener illslirurejor Po/arand Marille Research, BremerllOl'ell, Germany *** Dept. of Mechanical Engineerillg, Nagaoka Universit), ofTec1l11ology, Nagaoka. Japa" Abstract: The dynamics of polar ice sheets is strongly often imposes a terrible dilemma. A typical example is innuenced by a complex coupling of intrinsic structures. the disparity in the vocabularies used by geoscientists Some of these structures are extremely small, like dislo and materials scientists to describe the same microstruc cation walls and micro-inclusions: others occur in a wide IU ral features in polycrystals. In an allempt to be system range of scales, like stratigraphic features; and there are atic without being completely discrepant with the exist also those coll055al structures as large as megadunes :md ing literature. -
Mountain Springs (1890-1948)
Mountain Springs (1890-1948) The Early Years Bowmans Creek for the Lehigh Valley Railroad. Apparently, Splash Dam No. 1 was used as a splash dam at least through 1895, but it was not suc- The ice industry at Mountain Springs may not have been intentionally cessful. The fall in the creek was too steep and the twisting creek bed designed. Harveys Lake would have been the natural site for a major ice caused the released water to rush ahead of the logs, and too often the industry, but the Wright and Barnum patents to the lake discouraged its logs became stranded along the shore instead of being carried down- development. Indeed, Splash Dam No. 1 at Bean Run was developed by stream to the mill. Albert Lewis, not for the ice industry, but as an extension of his lumber With the completion and sale by Lewis to the Lehigh Valley of the rail- industry at Stull downstream on Bowmans Creek. road along the creek in 1893, a splash dam was not critical to carry the In October 1890, the Albert Lewis Lumber and Manufacturing logs to mill. His company ran log railroad lines into the forest lands to Company began construction of a log and timber dam on Bowmans haul timber to the Lehigh Valley line and then down to Stull. Lewis then Creek, near Bean Run, a small stream which runs into the creek. The ini- converted Splash Dam No. 1 to icecutting in the mid-1890s, an industry tial dam site was a failure; the creek bed was too soft to support a dam. -
THE NORTHERN ENGINEER Applied Science & Technology in the North Editor Carla Helfferich
THE NORTHERN ENGINEER applied science & technology in the north Editor Carla Helfferich Editorial Advisor Lee Leonard Associate Editor Barbara Matthews Subscription Manager/Typesetting Teri Lucara Finance Officer Neta Stilkey Editorial Board John Bates Deputy Commissioner, DOTPF Juneau Joseph M. Colonel! Woodward-Clyde Consultants Anchorage Mark Fryer Consulting Engineers Anchorage Paul Goodwin Variance Corporation Anchorage Keith B. Mather Vice Chancellor for Research, UAF Janet Matheson Architect Fairbanks John M. Miller Geophysical Institute, UAF Tunis Wentink, Jr. Geophysical Institute, UAF John Zarling Mechanical Engineering, UAF The Northern Engineer, Vol. 14, No. 3 THE NORTHERN ENGINEER VOLUME 14, NUMBER 3 FALL 1982 CONTENTS Of Ice and Men: The Symposium for Ice Drilling Technology Philip Marshall. ........................................ .4 Mountain Lodge Roof Design in the Arctic-Alpine Zone Robert G. Albrecht .....................................11 Inflation and Alaska's Residential Energy Conservation Loans ·.'' . Ted G. Eschenbach .....................................14 J ,Jc Solar-Powered Signals at Remote Railroad Crossings Chuck Gentry .........................................20 The Production of Calcium and Magnesium Acetates as Alternative De-Icing Agents Michael J. Economides, Russell D. Ostermann and Bertrand Theuveny .....................................22 Changes in Chena River Water Quality Timothy Tilsworth and Paul L. Bateman.....................29 High-Speed Gravel Roads Matthew Reckard ......................................38 -
Ice Cutting at Bantam Lake N
Ice House Ruins Tour Map Follow the Lake Trail (L = yellow blaze) Round trip ~ 1 mile Ice Cutting at Bantam Lake Berkshire Ice Company 1908-1927 Museum and Parking Lot Southern New England Ice Company 1927-1929 Lake Trail 8 6 7 5 4 3 2 1 Before the advent of the refrigerator, people kept food from spoiling by placing it in an icebox—a wooden cabinet with shelves for perishables and a large compartment for a block N of ice to keep everything cold. Where did this ice come Bantam Lake from? It was cut from lakes and ponds in the winter in re- gions where the temperatures were below freezing for ex- tended periods of time. Ice blocks were cut by farmers for Photos are courtesy of the Morris Historical Society and the family use and by crews employed by large commercial Bantam Historical Society with special thanks to Lee Swift and concerns. Both occurred at Bantam Lake. The commercial Betsy Antonucci. operation was centered on the north shore and involved White Memorial Foundation one of the largest ice block storage facilities in southern 71 Whitehall Road, P.O. Box 368 New England. The company even had railroad service Litchfield, CT 06763 making the distribution of ice to distant cities possible. (860) 567-0857 www.whitememorialcc.org 2014 West side of ice house showing box car and men shoveling snow from the tracks 8. The railroad line – This spur (now the beginning of the Butter- nut Brook Trail) led out to the main line of the Shepaug Railroad near the Lake Station. -
EAA2021 Sessions 14 July-1.Pdf
ORGANISERS 27th EAA Annual Meeting (Kiel Virtual, 2021) - Sessions Names, titles and affiliations are reproduced as submitted by the session organisers and/or authors. Language and wording were not revised. Technical editing: Kateřina Kleinová (EAA) Design and layout: Kateřina Kleinová (EAA) Design cover page: Janine Cordts (Institut für Ur- und Frühgeschichte Universität Kiel) European Association of Archaeologists Prague, June 2021 © European Association of Archaeologists, 2021 Tuesday 7 September 2021 #EAA2021 5 UNDERSTANDING PREHISTORIC DEMOGRAPHY Time: 9:00 - 16:30 CEST, 7 September 2021 Theme: 5. Assembling archaeological theory and the archaeological sciences Format: Regular session Organisers: Armit, Ian (University of York) - Damm, Charlotte (University of Tromso) - Črešnar, Matija (University of Ljubljana) ABSTRACTS 9:00 INTRODUCTION 9:15 THE COLOGNE PROTOCOL: ESTIMATING PAST POPULATION DENSITIES Schmidt, Isabell (University of Cologne) - Hilpert, Johanna (Kiel University - CAU) - Kretschmer, Inga (Landesamt für Denkmalpflege Stuttgart) - Peters, Robin (Landschaftsverband Rheinland) - Broich, Manue - Schiesberg, Sara - Vo- gels, Oliver - Wendt, Karl Peter - Zimmermann, Andreas - Maier, Andreas (University of Cologne) 9:30 DWELLINGS, SETTLEMENT ORGANISATION AND POPULATION FLUCTUATIONS: A MULTI-SCALAR CASE STUDY FROM ARCTIC NORWAY Damm, Charlotte (Arctic University of Norway) 9:45 EXPLORING LOCAL GEOGRAPHICAL CONDITIONS UNDERPINNING REGIONAL DEMOGRAPHIC CHANGE AMONG HUNTER-FISHER-GATHERERS IN SOUTHWEST COASTAL NORWAY (11,500-4300 CAL BP) Lundström, Victor - Bergsvik, Knut (University Museum, University of Bergen) 10:00 TERRITORIES, STRATEGIES AND TWO GENERATIONS Odgaard, Ulla (Independent researcher) 10:15 POPULATION DYNAMICS AND THE EXPANSION OF AGRICULTURE. ASSESSING THE RADIOCARBON GAPS DURING THE NEOLITHIZATION PROCESS IN THE WESTERN MEDITERRANEAN Cortell-Nicolau, Alfredo (Departament de Prehistòria, Arqueologia i Història Antiga. Universitat de València) - Crema, Enrico (Department of Archaeology. -
Descriptive Text to the 1995 Geological Map of Greenland, 1:2 500 000
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 18 2009 Greenland from Archaean to Quaternary Descriptive text to the 1995 Geological map of Greenland, 1:2 500 000. 2nd edition Niels Henriksen, A.K. Higgins, Feiko Kalsbeek and T. Christopher R. Pulvertaft GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 18 Keywords Archaean, Caledonides, Cenozoic, economic geology, geological map, Greenland, ice sheet, Mesozoic, offshore, orogenic belts, Palaeozoic, petroleum, Phanerozoic, Proterozoic, sedimentary basins. Cover illustration The cover design depicts mountains of the East Greenland Caledonian fold belt. The view, west of Mestersvig (located on map, page 4), is north over Bersærkerbræ and the northern part of the Stauning Alper to Kong Oscar Fjord with Traill Ø in the right backgro- und. The mountains up to 1800 m high are of the Neoproterozoic Eleonore Bay Supergroup. To the right: first author Niels Henriksen, for many years head of geological mapping at GGU/GEUS, and participant in field work in Greenland for more than 45 years. Frontispiece: facing page Major Caledonian syncline involving reactivated Archaean basement gneisses containing amphibolite bands. Overlying rusty coloured Mesoproterozoic metasediments (Krummedal supracrustal sequence) just visible in tight core of the fold. The intensity of deformation in the syncline clearly increases towards the core, where the basement gneisses become more strongly foliated. Some of the amphibolite bands were derived from cross-cutting basic intrusions, which are still discernable in the less severely deformed parts of the Archaean basement (Fig. 17, p. 31). The height of the section is c. 2000 m.