BULLETIN No. 88
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Dukes County Intelligencer
Journal of History of Martha’s Vineyard and the Elizabeth Islands THE DUKES COUNTY INTELLIGENCER VOL. 55, NO. 1 WINTER 2013 Left Behind: George Cleveland, George Fred Tilton & the Last Whaler to Hudson Bay Lagoon Heights Remembrances The Big One: Hurricane of ’38 Membership Dues Student ..........................................$25 Individual .....................................$55 (Does not include spouse) Family............................................$75 Sustaining ...................................$125 Patron ..........................................$250 Benefactor...................................$500 President’s Circle ......................$1000 Memberships are tax deductible. For more information on membership levels and benefits, please visit www.mvmuseum.org To Our Readers his issue of the Dukes County Intelligencer is remarkable in its diver- Tsity. Our lead story comes from frequent contributor Chris Baer, who writes a swashbuckling narrative of two of the Vineyard’s most adventur- ous, daring — and quirky — characters, George Cleveland and George Fred Tilton, whose arctic legacies continue to this day. Our second story came about when Florence Obermann Cross suggested to a gathering of old friends that they write down their childhood memories of shared summers on the Lagoon. The result is a collective recollection of cottages without electricity or water; good neighbors; artistic and intellectual inspiration; sailing, swimming and long-gone open views. This is a slice of Oak Bluffs history beyond the more well-known Cottage City and Campground stories. Finally, the Museum’s chief curator, Bonnie Stacy, has reminded us that 75 years ago the ’38 hurricane, the mother of them all, was unannounced and deadly, even here on Martha’s Vineyard. — Susan Wilson, editor THE DUKES COUNTY INTELLIGENCER VOL. 55, NO. 1 © 2013 WINTER 2013 Left Behind: George Cleveland, George Fred Tilton and the Last Whaler to Hudson Bay by Chris Baer ...................................................................................... -
Paleocene Alkaline Volcanism in the Nares Strait Region Related to Strike-Slip Tectonics
Paleocene Alkaline Volcanism in the Nares Strait Region Related to Strike-slip Tectonics Solveig Estrada & Detlef Damaske Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany ([email protected]) The tectonic development of the North Atlantic, the Labrador Sea/Baffin Bay and the Eurasian Basin of Arctic Ocean led to relative movements between the Greenland Plate and the North American Plate. There has been a debate for many years, whether the Nares Strait between northwest Greenland and Ellesmere Island marks an ancient plate boundary in terms of a left-lateral transform fault (Wegener Fault) or whether there was no movement between Greenland and Ellesmere Island at all. New data were acquired during joint German-Canadian geological field work on northeast Ellesmere Island 1998-2000 (Mayr 2008), followed in 2001 by a geoscience cruise in Nares Strait (Tessensohn et al. 2006). Indications for sinistral strike-slip movements followed by compressive tectonics were found at the western margin of northern Nares Strait (Saalmann et al. 2005). Paleogene basins on Judge Daly Promontory, northeast Ellesmere Island, are bounded by a complex pattern of strike-slip and thrust faults. The clastic sediments in the basins are rich in volcanogenic material. Volcanic pebbles within the Cape Back basin near Nares Strait are derived from lava flows and ignimbrites of a continental rift-related, strongly differentiated, highly incompatible element enriched, alkaline volcanic suite (Estrada et al. 2009). 40Ar/39Ar amphibole and alkali feldspar ages indicate that volcanism was active around 61–58 Ma and was probably contemporaneous with sedimentation within the Paleogene pull-apart basins on Judge Daly Promontory formed by sinistral strike-slip tectonics parallel to the present-day Nares Strait. -
The Quest for the Northwest Passage
NOVA DANIA THE QUEST FOR THE NORTHWEST PASSAGE SUZANNE CARLSON With considerable envy, the seventeenth century King of Denmark, Christian IV, watched the scramble to discover the elusive passage over Polar regions to lay claim to the riches of Cathay. This article will follow the fate of Christian’s early seventeenth century New World foothold, Nova Dania, through the cartographic record, speculating on what and when the Danes might have known about the then frozen northwest passage. An essential piece in this story is the amazing tale of Jens Munk, a merchant adventurer in the King’s service. For the cyber traveler, opportunities have reached a new zenith with Google Earth (FIGURE 1). I find myself cruising at 35,000 feet over the Alps, the Arabian Desert, up the Dania Nova Amazon, and to one of my favorite armchair destinations, FIGURE 2. JUSTUS DANCKERT’S TOTIUS AMERICAE DESCRIPTIO, the Arctic. With your AMSTERDAM, CA. 1680. VESTERGOTLANDS MUSEET, GOTHENBURG, SWEDEN Google joy stick, PART I - MAPPING NOVA DANIA you are able to glide with ease through the newly open waters With addictive zeal I searched map after map until I finally of the Northwest spotted it again: this time with the name reversed into Nova Passage. Dania (New Denmark). And there was more. Mer Cristian, Mare Christianum, or Christians Sea, depending on the Before the days of FIGURE 1. NORTHERN CANADA AND language appeared in what is now Fox Basin. Later, Nova GREENLAND. GOOGLE EARTH, 2006 satellite imaging, we Dania abandoned its Latin pretensions and became Nouvelle were content with and Denmarque and, as time went on, its location began to fascinated by maps, maps of unknown exotic places, maps wander—north into Buttons Bay, west into the interior, and showing nations or would-be empires. -
Contemporary Inuit Drawing
Cracking the Glass Ceiling: Contemporary Inuit Drawing Nancy Campbell A DISSERTATION SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN ART HISTORY, YORK UNIVERSITY TORONTO, ONTARIO. January 2017 © Nancy Campbell, 2017 Abstract The importance of the artist’s voice in art historical scholarship is essential as we emerge from post-colonial and feminist cultural theory and its impact on curation, art history, and visual culture. Inuit art has moved from its origins as an art representing an imaginary Canadian identity and a yearning for a romantic pristine North to a practice that presents Inuit identity in their new reality. This socially conscious contemporary work that touches on the environment, religion, pop culture, and alcoholism proves that Inuit artists can respond and are responding to the changing realities in the North. On the other side of the coin, the categories that have held Inuit art to its origins must be reconsidered and integrated into the categories of contemporary art, Indigenous or otherwise, in museums that consider work produced in the past twenty years to be contemporary as such. Holding Inuit artists to a not-so-distant past is limiting for the artists producing art today and locks them in a history that may or may not affect their work directly. This dissertation examines this critical shift in contemporary Inuit art, specifically drawing, over the past twenty years, known as the contemporary period. The second chapter is a review of the community of Kinngait and the role of the West Baffin Eskimo Cooperative in the dissemination of arts and crafts. -
Chapter 8 Polar Bear Harvesting in Baffin Bay and Kane Basin: a Summary of Historical Harvest and Harvest Reporting, 1993 to 2014
Chapter 8 SWG Final Report CHAPTER 8 POLAR BEAR HARVESTING IN BAFFIN BAY AND KANE BASIN: A SUMMARY OF HISTORICAL HARVEST AND HARVEST REPORTING, 1993 TO 2014 KEY FINDINGS Both Canada (Nunavut) and Greenland harvest from the shared subpopulations of polar • bears in Baffin Bay and Kane Basin. During 1993-2005 (i.e., before quotas were introduced in Greenland) the combined • annual harvest averaged 165 polar bears (range: 120-268) from the Baffin Bay subpopulation and 12 polar bears (range: 6-26) from Kane Basin (for several of the years, harvest reported from Kane Basin was based on an estimate). During 2006-2014 the combined annual harvest averaged 161 (range: 138-176) from • Baffin Bay and 6 (range: 3-9) polar bears from Kane Basin. Total harvest peaked between 2002 and 2005 coinciding with several events in harvest • reporting and harvest management in both Canada and Greenland. In Baffin Bay the sex ratio of the combined harvest has remained around 2:1 (male: • females) with an annual mean of 35% females amongst independent bears. In Kane Basin the sex composition of the combined harvest was 33% females overall for • the period 1993-2014. The estimated composition of the harvest since the introduction of a quota in Greenland is 44% female but the factual basis for estimation of the sex ratio in the harvest is weak. In Greenland the vast majority of bears are harvested between January and June in Baffin • Bay and Kane Basin whereas in Nunavut ca. 40% of the harvest in Baffin Bay is in the summer to fall (August – November) while bears are on or near shore. -
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. -
Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K of 95I4674 85L
Natural Resources Ressources naturelles Canada Canada CurrentCurrent and and Upcoming Upcoming NGR NGR Program Program Activities Activities in in British British Columbia, Columbia, NationalNational Geochemical Geochemical Reconnaissance Reconnaissance NorthwestNorthwest Territories, Territories, Yukon Yukon Territory Territory and and Alberta, Alberta, 2005-06 2005-06 ProgrProgrammeamme National National de de la la Reconnaissance Reconnaissance Géochimique Géochimique ActivitésActivités En-cours En-cours et et Futures Futures du du Programme Programme NRG NRG en en Colombie Colombie Britannique, Britannique, P.W.B.P.W.B. Friske, Friske,S.J.A.S.J.A. Day, Day, M.W. M.W. McCurdy McCurdy and and R.J. R.J. McNeil McNeil auau Territoires Territoires de du Nord-Ouest, Nord-Ouest, au au Territoire Territoire du du Yukon Yukon et et en en Alberta, Alberta, 2005-06 2005-06 GeologicalGeological Survey Survey of of Canada Canada 601601 Booth Booth St, St, Ottawa, Ottawa, ON ON 11 Area: Edéhzhie (Horn Plateau), NT 55 Area: Old Crow, YT H COLU Survey was conducted in conjunction with Survey was conducted in conjunction with and funded by IS M EUB IT B and funded by NTGO, INAC and NRCAN. NORTHWEST TERRITORIES R I the Yukon Geological Survey and NRCAN. Data will form A 124° 122° 120° 118° 116° B Alberta Energy and Utilities Board Data will form the basis of a mineral potential GEOSCIENCE 95N 85O the basis of a mineral potential evaluation as part of a 95O 85N evaluation as part of a larger required 95P 85M larger required Resource Assessment. OFFICE .Wrigley RESEARCH ANALYSIS INFORMATION Resource Assessment. .Wha Ti G 63° YUKON 63° Metals in the Environment (MITE) E Y AGS ESS Program: O E ESS Program: Metals in the Environment V .Rae-Edzo L R GSEOLOGICAL URVEY Survey Type: Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K OF 95I4674 85L Survey Type: Stream Sediment, stream M Year of Collection: 2004 and 2005 A C K ENZI E R 2 62° I V water, bulk stream sediment (HMCs and KIMs). -
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. -
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. -
The Southampton Island Marine Ecosystem Project 2019 Cruise
Southampton Island The Southampton Island Marine Ecosystem Project 2019 Cruise Report 5-29 August MV William Kennedy SIMEP 2019 Cruise Report Table of Contents Section 1. Introduction .................................................................................................... 1 Section 2. Physical Oceanography .................................................................................. 6 Section 3. Biogeochemistry .......................................................................................... 14 Section 4. Phytoplankton .............................................................................................. 20 Section 5. Kelp .............................................................................................................. 28 Section 6. Zooplankton and Fish .................................................................................. 38 Section 7. Sediments ..................................................................................................... 44 Appendix: Ship Log ...................................................................................................... 49 Appendix: Phyto Net Log ............................................................................................. 71 Appendix: Sediment stations ........................................................................................ 79 SIMEP 2019 Cruise Report Section 1. Introduction Climate warming is forcing rapid change to Canada’s marine Arctic icescape (Hochheim and Barber 2010) and its associated ecosystem, -
NTI IIBA for Conservation Areas Cultural Heritage and Interpretative
NTI IIBA for Phase I: Cultural Heritage Resources Conservation Areas Report Cultural Heritage Area: Dewey Soper and Interpretative Migratory Bird Sanctuary Materials Study Prepared for Nunavut Tunngavik Inc. 1 May 2011 This report is part of a set of studies and a database produced for Nunavut Tunngavik Inc. as part of the project: NTI IIBA for Conservation Areas, Cultural Resources Inventory and Interpretative Materials Study Inquiries concerning this project and the report should be addressed to: David Kunuk Director of Implementation Nunavut Tunngavik Inc. 3rd Floor, Igluvut Bldg. P.O. Box 638 Iqaluit, Nunavut X0A 0H0 E: [email protected] T: (867) 975‐4900 Project Manager, Consulting Team: Julie Harris Contentworks Inc. 137 Second Avenue, Suite 1 Ottawa, ON K1S 2H4 Tel: (613) 730‐4059 Email: [email protected] Report Authors: Philip Goldring, Consultant: Historian and Heritage/Place Names Specialist Julie Harris, Contentworks Inc.: Heritage Specialist and Historian Nicole Brandon, Consultant: Archaeologist Note on Place Names: The current official names of places are used here except in direct quotations from historical documents. Names of places that do not have official names will appear as they are found in the source documents. Contents Maps and Photographs ................................................................................................................... 2 Information Tables .......................................................................................................................... 2 Section -
ARCTIC Exploration the SEARCH for FRANKLIN
CATALOGUE THREE HUNDRED TWENTY-EIGHT ARCTIC EXPLORATION & THE SeaRCH FOR FRANKLIN WILLIAM REESE COMPANY 409 Temple Street New Haven, CT 06511 (203) 789-8081 A Note This catalogue is devoted to Arctic exploration, the search for the Northwest Passage, and the later search for Sir John Franklin. It features many volumes from a distinguished private collection recently purchased by us, and only a few of the items here have appeared in previous catalogues. Notable works are the famous Drage account of 1749, many of the works of naturalist/explorer Sir John Richardson, many of the accounts of Franklin search expeditions from the 1850s, a lovely set of Parry’s voyages, a large number of the Admiralty “Blue Books” related to the search for Franklin, and many other classic narratives. This is one of 75 copies of this catalogue specially printed in color. Available on request or via our website are our recent catalogues: 320 Manuscripts & Archives, 322 Forty Years a Bookseller, 323 For Readers of All Ages: Recent Acquisitions in Americana, 324 American Military History, 326 Travellers & the American Scene, and 327 World Travel & Voyages; Bulletins 36 American Views & Cartography, 37 Flat: Single Sig- nificant Sheets, 38 Images of the American West, and 39 Manuscripts; e-lists (only available on our website) The Annex Flat Files: An Illustrated Americana Miscellany, Here a Map, There a Map, Everywhere a Map..., and Original Works of Art, and many more topical lists. Some of our catalogues, as well as some recent topical lists, are now posted on the internet at www.reeseco.com.