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East Jordan, Michigan, Thursday, May 6, 1954 Ten Cents
\ -/. pecial Northern Michigan Progress Issue . "HOME OF THE SWANS" VOLUME 58 NUMBER 18 EAST JORDAN, MICHIGAN, THURSDAY, MAY 6, 1954 TEN CENTS OVER THE Marie Nielsen Tops All Officers Returned BACK FENCE County Dress Revue BY MARSHALL The largest crowd ever to wit• inent was in clothing work with MAYOR MAKES ANNUAL ness a county 4-H Achievement 109 making garments, Health It snowed so hard Monday program was present at the East Improvement was next with 72, right it pushed the mushrooms Jordan high school Tuesday eve• Handicraft with 71, knitting 37, back into the ground . Troop• ning, April 27. One hundred four- Conservation 37, Tractor Main• er Moon of the State Police Post girls took part in a Dress Revue tenance 14, Personal Grooming ai Gaylord has been transferred in a program planned and direct• 9, Personal Accounts 7, Home to Wakefield in the upper pen• CITY ENTS ed by Mrs. William Malpass of Improvement 5, Junior Leader• insula. He stopped in East Jor• East Jordan and her committee. ship 2, and there was 1 Electri• dan on his way and said: "Jen• cal member and 1 chrocheting On Monday evening, exhibits * * * ny Barnett served me my first member. were brought in and were viewed AG. SOCIETY QUITS cup of coffee in East Jordan six The Dress Revue winner was j.ears ago and now she is serving all day Tuesday by parents and Masonic Lodge To Construct friends of 4-H members and East Marie Nielsen, age 17, daughter my last here." . Sorry to see of Mr. -
Of Penguins and Polar Bears Shapero Rare Books 93
OF PENGUINS AND POLAR BEARS Shapero Rare Books 93 OF PENGUINS AND POLAR BEARS EXPLORATION AT THE ENDS OF THE EARTH 32 Saint George Street London W1S 2EA +44 20 7493 0876 [email protected] shapero.com CONTENTS Antarctica 03 The Arctic 43 2 Shapero Rare Books ANTARCTIca Shapero Rare Books 3 1. AMUNDSEN, ROALD. The South Pole. An account of “Amundsen’s legendary dash to the Pole, which he reached the Norwegian Antarctic Expedition in the “Fram”, 1910-1912. before Scott’s ill-fated expedition by over a month. His John Murray, London, 1912. success over Scott was due to his highly disciplined dogsled teams, more accomplished skiers, a shorter distance to the A CORNERSTONE OF ANTARCTIC EXPLORATION; THE ACCOUNT OF THE Pole, better clothing and equipment, well planned supply FIRST EXPEDITION TO REACH THE SOUTH POLE. depots on the way, fortunate weather, and a modicum of luck”(Books on Ice). A handsomely produced book containing ten full-page photographic images not found in the Norwegian original, First English edition. 2 volumes, 8vo., xxxv, [i], 392; x, 449pp., 3 folding maps, folding plan, 138 photographic illustrations on 103 plates, original maroon and all full-page images being reproduced to a higher cloth gilt, vignettes to upper covers, top edges gilt, others uncut, usual fading standard. to spine flags, an excellent fresh example. Taurus 71; Rosove 9.A1; Books on Ice 7.1. £3,750 [ref: 96754] 4 Shapero Rare Books 2. [BELGIAN ANTARCTIC EXPEDITION]. Grande 3. BELLINGSHAUSEN, FABIAN G. VON. The Voyage of Fete Venitienne au Parc de 6 a 11 heurs du soir en faveur de Captain Bellingshausen to the Antarctic Seas 1819-1821. -
Canadian Arctic 1987
Canadian Arctic 1987 TED WHALLEY Ellesmere Island has, at Cape Columbia, the northern-most land in the world, at latitude about 83.1°. It is a very mountainous island, particularly on the north west and the east sides, and its mountains almost reach the north coast - the northern-most mountains in the world. It was from here that most of the attempts to reach the North Pole have started, including that of Peary - reputedly, but perhaps not actually, the first man to reach the Pole. Nowadays, tourist flights to the Pole by Twin Otter from Resolute Bay are common, but are somewhat expensive. The topography of Ellesmere is dominated by several large and small ice-caps which almost bury the mountains, and only the Agassiz Ice-Cap, which is immediately west of Kane Basin, has a name. On the north-west side there are two large and unnamed ice-caps, the larger of which straddles 82°N and the smaller straddles 8I.5°N. There is also a large unnamed ice-cap immediately west of Smith Sound, a smaller one on the south-east tip of Ellesmere Island, and another north of the settlement of Grise Fiord on the south coast. The north coast of Ellesmere was the home of great ice shelves, but, at about the turn of the century, the ice shelves started to break off and float away as so-called 'ice islands' that circulated for many decades around the arctic ocean, and still do. They have often been used as natural platforms for scientific expeditions. Perhaps nine-tenths of the original ice shelves have floated away. -
NORTH Aberdeen’S Circumpolar Collections
University of Aberdeen Marischal Museum and Special Libraries & Archives NORTH Aberdeen’s Circumpolar Collections Rambles among the fields and fjords, from Thomas Forrester, Norway in 1848 and 1849 (London: Longman, 1850). Lib R 91(481) Fore This view looking up to the Shagtols- Tind, the highest mountain in Norway, reaching the height of 7670 English feet, beneath a bell-shaped snowy valley penetrated into the mountains, and closed by a vast glacier…[the view taken from]… the most splendid fir- forest I have yet met with. An Information Document University of Aberdeen Development Office King’s College Aberdeen Scotland, UK t. +44 (0)1224 272281 f. +44 (0)1224 272271 www.abdn.ac.uk/giving 1 CONTENTS PAGE INTRODUCTION 3 IDEAS OF THE NORTH Maps 3 Marvels 3 Magicians 4 Monsters 6 An ‘imagined north’ 6 ABERDEEN AND THE ARCTIC Treasures 7 Scientists 7 Explorers 7 Drama in the Arctic 8 Commerce and adventure 8 TRAVEL AND TOPOGRAPHY Orkney and Shetland 10 Russia and Siberia 11 Iceland 12 Scandinavia 13 Northern Japan 14 The American Arctic 15 CONCLUSION 19 HOLDINGS AS INDICATED IN THE TEXT 20 2 A significant number of alumni in the University A cartographic pioneer of the sixteenth century, of Aberdeen’s long history have found that the Gerald Mercator, made a single map of The compass needle drew them to the north. As Lands under the Pole, complete with an explorers, settlers, missionaries, or employees imaginary landmass at the North Pole, while of the Hudson’s Bay Company, graduates of in the seventeenth century, Blaeu’s Regions the two ancient colleges which make up the Beneath the North Pole tries to accommodate modern university have been conspicuous in the latest geographical knowledge with many circumpolar connections. -
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$3*&$>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. -
The Life and Letters of a Royal Navy Surgeon, Edward Lawton Moss MD
REVIEWS • 109 why they are the crème de la crème. Chapters 7a and 7b pic- plateau of Washington Irving Island off the entrance to ture and describe some of these items. Chapter 7c, entitled Dobbin Bay on the east coast of Ellesmere Island. Much to “Gems Showcase,” is a visual feast. No fewer than 43 pages their surprise, they discovered two ancient-looking stone are devoted to images, almost all in colour, of polar material cairns on the plateau, but failed to locate any evidence of such as notices of various kinds, postcards, covers, and let- who might have built them. Moss made a quick sketch of ters. This section alone is worth the price of the book. the two cairns, a sketch he later back in England turned into The ultimate goal of many philatelists is to exhibit their a colour painting, now kept at the Scott Polar Institute in collections and, they hope, to earn a commensurate award. Cambridge. The drawing and the mention of the cairns in Chapter eight outlines the differences between showing one’s the expedition diaries resulted in our own investigation of collection and exhibiting it. Although many of the processes the plateau in July 1979. By then, numerous finds of Norse involved in showing a polar exhibit are the same as those artifacts in nearby 12th century Inuit house ruins strongly of exhibiting a general postal history collection, the author suggested that the builders of the old cairns could have been explains the differences in some detail. If an exhibit is to Norse explorers from Greenland (McCullough and Schled- do well in competition, planning, deciding what to include, ermann, 1999). -
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. -
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. -
Hudson Bay Ice Conditions
Hudson Bay Ice Conditions ERIC W. DANIELSON, JR.l ABSTRACT.Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western, northern, and eastern edges of the Bay; the pattern seems to be a result of local topography, cur- rents, and persistent winds. Final melting occurs in August. Freeze-up commences in October, along the northwestern shore, and proceeds southeastward. The entire Bay is ice-covered by early January,except for persistent shore leads. RÉSUMÉ. Conditions de la glace dans la mer d’Hudson. A partir de l’analyse de neuf années de reconnaissances aériennes et d’autres données, on a pu déduire des moyennes mensuelles de distribution de la glace pour la mer d’Hudson. L‘informa- tion est présentte sous formes de cartes et de discussion des Cléments significatifs. On y voit que la débâcle progresse vers le sud à partir des marges ouest, nord et est dela mer; cette séquence sembleêtre le résultat de la topographielocale, des courants et .des vents dominants. La fonte se termine en aofit. L’enge€wommence en octobre le long de la rive nord-ouest et progresse vers le sud-est. Sauf pow les chenaux côtiers persistants, la mer est entihrement gelée au début de janvier. INTRODUCTION In many respects, ice cover is a basic hydrometeorological variable. In Hudson Bay (Fig. 1) it might be considered the most basic of all, as it influences all other conditions so decisively. -
Americanlegionvo1356amer.Pdf (9.111Mb)
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Submission to The
SUBMISSION TO THE NUNAVUT WILDLIFE MANAGEMENT BOARD FOR Information: Decision: X Issue: Southampton Island (SHI) Caribou Management Background: • The Southampton Island caribou herd was in decline beginning in June 2003, and by June 2011 had declined to levels unable to sustain the estimated subsistence harvest. • The main cause of the decline was a reproductive disease termed Brucellosis. This disease causes severe reproductive declines within caribou populations, negatively impacting birth rates in females and sperm production in reproductive males through testicular tissue damage. • Though the disease is thought to have caused the decline, intra-territorial sales of caribou meat from SHI to primarily Baffin Communities dramatically accelerated the decline in 2010 and 2011. • The establishment of a TAH helped control this intra-territorial sale, helping to stabilize the population. • Management actions have proven effective thus far but all parties are very concerned about finding a way to control the intra-territorial sale of caribou meat if we are to secure the herds future. Current Status • The SHI caribou population has increased from an estimated 7,287 caribou in May 2013 to 12,297 caribou in May 2015. • Both the Department of Environment (DOE) and the Coral Harbour Hunters and Trappers Organization (HTO) believe this increase is at least in part related to an emigration event detected by Coral Harbour hunters in the winter of 2013/2014 from mainland Nunavut. • DOE is currently comparing genetic profiles of recent caribou samples with pre- immigration samples in an attempt to confirm this immigration event. • Additionally both Coral Harbour harvesters and DOE survey crews have detected an increase in calf observations between the 2012/13 harvesting season and the present suggesting an increase in productivity over the same period. -
Late Wisconsinan Glaciation of Southern Eureka Sound: Evidence for Extensive Innuitian Ice in the Canadian High Arctic During Th
Quaternary Science Reviews 19 (2000) 1319}1341 Late Wisconsinan glaciation of southern Eureka Sound: evidence for extensive Innuitian ice in the Canadian High Arctic during the Last Glacial Maximum Colm OD Cofaigh! *, John England!, Marek Zreda" !Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E3 "Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona 85721, USA Abstract Southern Eureka Sound was originally proposed as the centre of an Innuitian Ice Sheet in the Canadian High Arctic at the Last Glacial Maximum (LGM) based largely on the pattern of Holocene emergence. This paper focuses on the glacial geological evidence for such an ice sheet in the region. Granite dispersal trains and ice-moulded bedrock record regional, westward #ow of warm-based ice into Eureka Sound from SE Ellesmere Island. Regional ice was coalescent with local ice domes on inter-"ord peninsulas. Marine limit in the form of raised deltas, beaches and washing limits formed during deglaciation of the regional ice. Throughout southern Eureka Sound, marine limit dates )9.2 ka BP, indicating that ice commenced retreat during the early Holocene. Ice-divides were located along the highlands of central Ellesmere and Axel Heiberg islands, from which ice inundated Eureka Sound, #owing north and south along the channel. Regional radiocarbon dates on marine limit show that deglaciation occurred in two steps. Initial break-up and radial retreat of ice from Eureka Sound to the inner "ords was rapid and preceded stabilisation along adjacent coastlines and at "ord heads. Two-step deglaciation is also re#ected in di!erences in glacial geomorphology between the inner and outer parts of many "ords.