Historical Records and Relics from the North Greenland Coast
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Aglooka Advisor Spring 2019
Aglooka Advisor Spring 2019 Issue No. 8 Aglooka Advisor Spring 2019 Issue No.8 President’s Report page 4 Eric Marwick: an obituary page 6 Polar Exploration: article by John Ramwell page 7 Dr John Rae Commemorated on an Unusual Scale: links to an article by Rognvald Boyd on the JRS website page 8 Two Art Exhibitions: article by Sigrid Appleby page 9 RICS honours John Rae: report by Fiona Gould page 10 Hall of Clestrain: archaeological report by Dan Lee page 10 Memories of Two Canadians: article by Anne Clark page 11 An Unexpected Guest: newspaper report from 1858 submitted by Fiona Sutherland page 12 Take the Torch: book review page 13 Arctic Return Expedition: update by David Reid page 14 Poster Competition: results page 15 Notices page 16 Photo on front cover by John Welburn, ABIPP, showing roof patches, new guttering and heavy-duty plastic covering on windows. - 2 - Patrons Dr Peter St John, The Earl of Orkney Ken McGoogan, Author Ray Mears, Author & TV Presenter Bill Spence, Lord Lieutenant of Orkney Sir Michael Palin Magnus Linklater CBE Board of Trustees (in alphabetical order by surname) Andrew Appleby — Jim Chalmers — Anna Elmy — Neil Kermode — Fiona Lettice Mark Newton — Norman Shearer Committee President — Andrew Appleby Chairman — Norman Shearer Honorary Secretary — Anna Elmy Honorary Treasurer — Fiona Lettice Webmaster and Social Media — Mark Newton Membership Secretary — Fiona Gould Administrative Secretary — Julie Cassidy Registered Office The John Rae Society 7 Church Road Stromness Orkney KW16 3BA Tel: 01856 851414 e-mail: [email protected] Newsletter Editor — Fiona Gould The views expressed in this newsletter are those of the authors and not necessarily those of the Editor or the Board of Trustees of the John Rae Society. -
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. -
The Origin, Development, and History of the Norwegian Seventh-Day Adventist Church from the 1840S to 1889" (2010)
Andrews University Digital Commons @ Andrews University Dissertations Graduate Research 2010 The Origin, Development, and History of the Norwegian Seventh- day Adventist Church from the 1840s to 1889 Bjorgvin Martin Hjelvik Snorrason Andrews University Follow this and additional works at: https://digitalcommons.andrews.edu/dissertations Part of the Christian Denominations and Sects Commons, Christianity Commons, and the History of Christianity Commons Recommended Citation Snorrason, Bjorgvin Martin Hjelvik, "The Origin, Development, and History of the Norwegian Seventh-day Adventist Church from the 1840s to 1889" (2010). Dissertations. 144. https://digitalcommons.andrews.edu/dissertations/144 This Dissertation is brought to you for free and open access by the Graduate Research at Digital Commons @ Andrews University. It has been accepted for inclusion in Dissertations by an authorized administrator of Digital Commons @ Andrews University. For more information, please contact [email protected]. Thank you for your interest in the Andrews University Digital Library of Dissertations and Theses. Please honor the copyright of this document by not duplicating or distributing additional copies in any form without the author’s express written permission. Thanks for your cooperation. ABSTRACT THE ORIGIN, DEVELOPMENT, AND HISTORY OF THE NORWEGIAN SEVENTH-DAY ADVENTIST CHURCH FROM THE 1840s TO 1887 by Bjorgvin Martin Hjelvik Snorrason Adviser: Jerry Moon ABSTRACT OF GRADUATE STUDENT RESEARCH Dissertation Andrews University Seventh-day Adventist Theological Seminary Title: THE ORIGIN, DEVELOPMENT, AND HISTORY OF THE NORWEGIAN SEVENTH-DAY ADVENTIST CHURCH FROM THE 1840s TO 1887 Name of researcher: Bjorgvin Martin Hjelvik Snorrason Name and degree of faculty adviser: Jerry Moon, Ph.D. Date completed: July 2010 This dissertation reconstructs chronologically the history of the Seventh-day Adventist Church in Norway from the Haugian Pietist revival in the early 1800s to the establishment of the first Seventh-day Adventist Conference in Norway in 1887. -
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. -
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). -
Geology of Greenland Bulletin 185, 67-93
Sedimentary basins concealed by Acknowledgements volcanic rocks The map sheet was compiled by J.C. Escher (onshore) In two areas, one off East Greenland between latitudes and T.C.R. Pulvertaft (offshore), with final compilation 72° and 75°N and the other between 68° and 73°N off and legend design by J.C. Escher (see also map sheet West Greenland, there are extensive Tertiary volcanic legend). In addition to the authors’ contributions to the rocks which are known in places to overlie thick sedi- text (see Preface), drafts for parts of various sections mentary successions. It is difficult on the basis of exist- were provided by: L. Melchior Larsen (Gardar in South ing seismic data to learn much about these underlying Greenland, Tertiary volcanism of East and West Green- sediments, but extrapolation from neighbouring onshore land); G. Dam (Cretaceous–Tertiary sediments of cen- areas suggests that oil source rocks are present. tral West Greenland); M. Larsen (Cretaceous–Tertiary Seismic data acquired west of Disko in 1995 have sediments in southern East Greenland); J.C. Escher (map revealed an extensive direct hydrocarbon indicator in of dykes); S. Funder (Quaternary geology); N. Reeh the form of a ‘bright spot’ with a strong AVO (Amplitute (glaciology); B. Thomassen (mineral deposits); F.G. Versus Offset) anomaly, which occurs in the sediments Christiansen (petroleum potential). Valuable comments above the basalts in this area. If hydrocarbons are indeed and suggestions from other colleagues at the Survey are present here, they could either have been generated gratefully acknowledged. below the basalts and have migrated through the frac- Finally, the bulletin benefitted from thorough reviews tured lavas into their present position (Skaarup & by John Korstgård and Hans P. -
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. -
Frederick J. Krabbé, Last Man to See HMS Investigator Afloat, May 1854
The Journal of the Hakluyt Society January 2017 Frederick J. Krabbé, last man to see HMS Investigator afloat, May 1854 William Barr1 and Glenn M. Stein2 Abstract Having ‘served his apprenticeship’ as Second Master on board HMS Assistance during Captain Horatio Austin’s expedition in search of the missing Franklin expedition in 1850–51, whereby he had made two quite impressive sledge trips, in the spring of 1852 Frederick John Krabbé was selected by Captain Leopold McClintock to serve under him as Master (navigation officer) on board the steam tender HMS Intrepid, part of Captain Sir Edward Belcher’s squadron, again searching for the Franklin expedition. After two winterings, the second off Cape Cockburn, southwest Bathurst Island, Krabbé was chosen by Captain Henry Kellett to lead a sledging party west to Mercy Bay, Banks Island, to check on the condition of HMS Investigator, abandoned by Commander Robert M’Clure, his officers and men, in the previous spring. Krabbé executed these orders and was thus the last person to see Investigator afloat. Since, following Belcher’s orders, Kellett had abandoned HMS Resolute and Intrepid, rather than their return journey ending near Cape Cockburn, Krabbé and his men had to continue for a further 140 nautical miles (260 km) to Beechey Island. This made the total length of their sledge trip 863½ nautical miles (1589 km), one of the longest man- hauled sledge trips in the history of the Arctic. Introduction On 22 July 2010 a party from the underwater archaeology division of Parks Canada flew into Mercy Bay in Aulavik National Park, on Banks Island, Northwest Territories – its mission to try to locate HMS Investigator, abandoned here by Commander Robert McClure in 1853.3 Two days later underwater archaeologists Ryan Harris and Jonathan Moore took to the water in a Zodiac to search the bay, towing a side-scan sonar towfish. -
Postglacial Isobases from Northern Ellesmere Island and Greenland
Document generated on 09/23/2021 9:47 a.m. Géographie physique et Quaternaire Postglacial Isobases from Northern Ellesmere Island and Greenland: New Data Isobases postglaciaires du nord de l’île d’Ellesmere et du Groenland : nouvelles données Postglaziale Isobasen vom Norden der Ellesmere-lnsel und Grönland: neue Daten John England and Jan Bednarski Volume 40, Number 3, 1986 Article abstract Over seventy new 14C dates on former relative sea levels from Hall Land, URI: https://id.erudit.org/iderudit/032650ar northwest Greenland, and Clements Markham Inlet, northern Ellesmere DOI: https://doi.org/10.7202/032650ar Island, are combined with previous data to revise the regional isobases for this area. These isobases show : 1) a centre of maximum postglacial emergence See table of contents over northwest Greenland extending to; 2) an intervening cell of lower emergence over northeast Ellesmere Island which was isostatically-dominated by the Greenland Ice Sheet; in turn, extending to 3) a higher centre of Publisher(s) emergence over the Grant Land Mountains, northernmost Ellesmere Island, associated with the independent history of local ice caps there. Radiocarbon Les Presses de l'Université de Montréal dates from raised marine shorelines show a 2000 year lag between glacial unloading on northwest Greenland and northernmost Ellesmere Island. This ISSN lag in glacioisostatic adjustments suggests a considerable range in the glacier response times and/or glacioclimatic regimes in this area. Throughout the area 0705-7199 (print) the last ice limit was ca. 5-60 km beyond present ice margins. Maximum 1492-143X (digital) emergence at these ice limits is marked by shorelines built into a full glacial sea which range from 124 m asl in Clements Markham Inlet to 150 m asl in Hall Explore this journal Land. -
Greenland Explorer
GREENLAND EXPLORER Valleys and Fjords EXPEDITION IN BRIEF The Trip Overview Meet locals along the west coast of Greenland and experience traditional Inuit settlements Visit the Ilulissat Icefjord, a UNESCO World Heritage Site The west coast of Greenland is Europe’s final frontier, and sailing along it is Explore historic places from Norse the best way to sample its captivating history, enthralling wildlife and distinct and Viking eras culture. Explore places from the Norse and Viking eras, experience the Spot arctic wildlife, such as whales, birds and seals Ilulissat Icefjord—a UNESCO World Heritage Site— and visit two Greenland Cruise in a Zodiac to get up close to communities, encountering an ancient culture surviving in a modern world. glaciers, fjords, icebergs and more For trip inquiries, speak to our Polar Travel Advisers at 1. 844.205.0837 | Visit QuarkExpeditions.com for more details or get a free quote here. and geography of Greenland, your next Itinerary stop. Join expedition staff on deck and on the bridge as they look out for whales and seabirds, get to know your fellow Ban Bay GREENLAND DAY 1 | ARRIVE IN guests or simply take in the natural REYKJAVIK, ICELAND ARCTIC beauty that surrounds you. CIRCLE Arrive in the Icelandic capital in the Eqip Sermia Ilulissat morning and make your way to your DAY 4 | EAST GREENLAND Sisimiut Kangerlussuaq Experience a true arctic ghost town Itilleq included hotel. You will have the day Scoresby Sund to explore the city on your own. In when we visit the abandoned settlement Nuuk of Skjoldungen, where inhabitants the evening, join us at your hotel for a Skjoldungen Denmark Strait welcome briefing. -
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. -
The Greenlander of Today 5
Top-Sukkertoppen, a west Greenland settlement, is located on rocky terrain. It is the centre of a valuablesealing and cod-salting industry. Bottom-Godthaab, capital of Greenland, was founded by the Danish missionary Hans Egede in 1721. This view shows the older part of the town including the hospital to the left. .. THE GREENLANDER OFTODAY* By Eske Brun. The Greenland Administration, Copenhagen, Denmark. SHOULD like to begin by saying something about the first and most I serious error generally made about Greenland, and the one which is, I think, the most difficult to eradicate: It is popularly believed that it is cold in Greenland, so cold that wherever and whenever you are there you are frozen stiff, and that there is nothing there but ice and snow. This idea of Greenland as an enormous lump of ice is largely due to the ice-cap. Five-sixths of Greenland’s two million square kilometers are covered by this ice-cap. There is so much ice there that, if it melted, the oceans and seasall over theworld would rise eight meters. The existence of the ice-cap is not due to any excessive cold in Greenland, but mainly to the considerable height of the country, the average height of the surface of the ice-cap being about 2000 meters, and to the heavy snowfall. Paradoxical as it may seem ,the ice-cap is thicker in southern Greenland than in northern Greenland, because the snowfall is heavier in the south. The largest continuous tracts of land not covered with ice are to be found in Peg-yland on the northern coast of the country.