Geographical Report of the Crocker Land Expedition, 1913-1917
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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. -
Hope To"Solve Earth's Final Puzzle-Icy Crocker Land
HOPE TO" SOLVE EARTH'S FINAL PUZZLE-ICY CROCKER LAND Donald B. MacMillan and His Hardy Band Will Be in Wireless Touch with Civilization in Their Search for the Undis¬ Er/e277Zo J&*y»7èk. is invariably good.a tact ittOStOd b) Continent Which and Tradition their symmetrical bodies and perfect covered Theory health. Admiral Peary tella of having seen only one Ks«iulmau kllol u« all hi» Place North of Alaska and Siberia. yuan ol soso latkm oil tbem." Smith Sound was rocentl] swept by an of sad most Of the In¬ his l ¦. [«. i.i «.. smenU bj th« «¦ ¦¦. si "phleini«' typhoid, Wlf.L. the spirit of adventure ev after I'eary had reported finding habitant..about i_ men snd r*> ostaga* the land he had named after one of hi i.'i« «'tri«' Compan) In Bcheneetady, die? were tna.ie ill. It is I" II« red to have so i- that the physl it will h« a station capable ot trans* Will there ever be a time whi patrons, it »Brooklyn been brought to Smith gotind by one of u enemies bava asserted thst sli "r. milting messages al least LUV milis, and n « ii ...,II fear to go forth to face clan's the missionaries from goutta Gi«.inland. further north than Crock«r »«ml »«a of coursa «>f reeetvlag them from *m> known perils to snatch the laurel as ., th< .tire ex¬ .¦. for Taking this warning - «listan. The point «hosiii OlBtSI lame'.' only a gu« will be VSCClnsted against ty¬ The that a eontinent. or at luí¬ quarters is si the bead of riaglei Bai pedition The answer of the centuries has bei theory ol before leaving New fork, ".«1 ta ai an archipelago, must exist in that Ml m Kane Basin, on the essl eoaal phoid "Xu"' la spite of the toll of life will vacillate all th« :.-., amain is on the w irk of lJr Lsnd, This is In Isl H I doctor liuil«, men have gone forth into the ui known wast«» based Qrant .<< Hi- Unite« from lh< \>"'- upon reuching Smith BSUad. -
Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped. -
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. -
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. -
Peary Arctic Club Expedition to the North Pole, 1908-9 Author(S): Robert E
Peary Arctic Club Expedition to the North Pole, 1908-9 Author(s): Robert E. Peary and R. A. Harris Source: The Geographical Journal, Vol. 36, No. 2 (Aug., 1910), pp. 129-144 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1777691 Accessed: 08-05-2016 16:09 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 143.89.105.150 on Sun, 08 May 2016 16:09:32 UTC All use subject to http://about.jstor.org/terms The Geographical Journal. No. 2. AUGUST, 1910. VOL. XXXVI. PEARY ARCTIC CLUB EXPEDITION TO THE NORTH POLE, 1908-9.* By COMMANDER ROBERT E. PEARY. THE last North Polar Expedition of the Peary Arctic Club t left New York harbour on July 6, 1908, in the steamer Roosevelt, built by the club especially for Arctic work, and commanded by Captain Robert A. Bartlett. The members of the expedition were as follows, a total of 22: Commander R. E. Peary, U.S.N., Commander of the expedition; Captain R. -
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. -
ARCTIC CHANGE 2014 8-12 December - Shaw Centre - Ottawa, Canada
ARCTIC CHANGE 2014 8-12 December - Shaw Centre - Ottawa, Canada Oral Presentation Abstracts Arctic Change 2014 Oral Presentation Abstracts ORAL PRESENTATION ABSTRACTS TEMPORAL TREND ASSESSMENT OF CIRCULATING conducted when possible. Results: Maternal levels of Hg and MERCURY AND PCB 153 CONCENTRATIONS AMONG PCB 153 significantly decreased between 1992 and 2013. NUNAVIMMIUT PREGNANT WOMEN (1992-2013) Overall, concentrations of Hg and PCB 153 among pregnant women decreased respectively by 57% and 77% over the last Adamou, Therese Yero (12) ([email protected]), M. Riva (12), E. Dewailly (12), S. Dery (3), G. Muckle (12), R. two decades. In 2013, concentrations of Hg and PCB 153 were Dallaire (12), EA. Laouan Sidi (1) and P. Ayotte (1,2,4) respectively 5.2 µg/L and 40.36 µg/kg plasma lipids (geometric means). Discussion: Our results suggest a significant decrease (1) Axe santé des populations et pratiques optimales en santé, of Hg and PCB 153 maternal levels from 1992 to 2013. Centre de Recherche du Centre Hospitalier Universitaire de Geometric mean concentrations of Hg and PCB 153 measured Québec, Québec,Québec, G1V 2M2 in 2013 were below Health Canada guidelines. The decline (2) Université Laval, Québec, Québec, G1V 0A6 observed could be related to measures implemented at regional, (3) Nunavik Regional Board of Health and Social Services, Kuujjuaq, Québec national and international levels to reduce environmental (4) Institut National de Santé Publique du Québec (INSPQ), pollution by mercury and PCB and/or a significant decrease Québec, G1V 5B3 of seafood consumption by pregnant women. These results have to be interpreted with caution. -
Antoniades.2005A.Pdf
Journal of Paleolimnology (2005) 33: 349–360 Ó Springer 2005 -1 Quantitative estimates of recent environmental changes in the Canadian High Arctic inferred from diatoms in lake and pond sediments Dermot Antoniades1,*, Marianne S.V. Douglas1 and John P. Smol2 1Department of Geology, University of Toronto, 22 Russell St., Toronto ON, M5S 3B1, Canada 2Paleoecological Environmental Assessment and Research Lab (PEARL), Department of Biology, Queen’s University, Kingston ON, K7L 3N6, Canada; *Author for correspondence (e-mail: dermot.antoniades@ utoronto.ca) Received 26 May 2004; accepted in revised form 4 November 2004 Key words: Arctic, Climate, Diatoms, Ellef Ringnes Island, Ellesmere Island, Environmental change, Limnology, pH, Proxies Abstract Diatoms were examined in three lacustrine sediment records from Alert, northern Ellesmere Island, and from Isachsen, Ellef Ringnes Island. Diatom assemblages changed markedly since the mid-19th century following relatively stable community composition that spanned centuries to millennia. Three different assemblages, primarily composed of Fragilaria pinnata, Diadesmis spp., or Pinnularia spp., dominated the pre-1850 period at the three sites, but were replaced with different, more diverse assemblages in recent sediments. These species shifts occurred in the mid- to late-19th century in the Isachsen sites, and in the mid- to late-20th century in our Alert site. This difference in timing appears to be a result of the different sensitivities of lakes and ponds to environmental change, rather than of site-specific chemical properties. Reconstructions of pH using diatom inference models indicated increases from 0.5 to 0.8 pH units at these sites over this period of assemblage change. The diatom-inferred pH record from Alert showed agreement with measured climate data from Alert over the last 30 years.