In Baffin Bay and Adjacent Waters
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My Dear Beaufort: a Personal Letter from John Ross's Arctic Expedition
ARCTIC VOL. 40, NO. 1 (MARCH 1987) P. 66-77 My Dear Beaufort: A Personal Letter from John Ross’s Arctic Expedition of 1829-33 CLIVE HOLLAND’ and JAMES M. SAVELLE2 (Received 30 January 1986; accepted in revised form 6 October 1986) ABSTRACT. During his four years’ residence in the Canadian Arctic in search of a Northwest Passage in 1829-33, John Ross wrote a private letter to Francis Beaufort, Hydrographer of the Navy. The letter, reproduced here, provides valuable historical insights into many aspects of Ross’s character and of the expedition generally. His feelings of bitterness toward several of his contemporaries, especially John Barrow and William E. Parry, due to the ridicule suffered as a result of the failure of his first arctic voyage in 1818, are especially revealing, as is his apparently uneasy relationship with his nephew and second-in-command, James Clark Ross. Ross’s increasing despair andpessimism with each succeeding enforced wintering and, eventually, the abandonment of the expedition ship Victory are also clearly evident. Finally,the understandable problems of maintaining crew discipline during the final year of the expedition, though downplayed, begin to emerge. Key words: John Ross, arctic exploration, 1829-33 Arctic Expedition, unpublished letter RÉSUMÉ. Durant les quatre années où ilr6sidadans l’Arctique canadien à la recherche du Passage du Nord-Ouest, de 1829 à 1833, John Ross écrivit une lettre personnelle à Francis Beaufort, hydrographe de la marine. Cette lettre, reproduite ici, permet de mieux apprécier du point de vue historique, certains aspects du caractère de Ross et de l’expédition en général. -
Canadian Arctic Through-Flow 2012 Cruise to Nares Strait
Canadian Arctic Through-flow 2012 Cruise to Nares Strait CCGS Henry Larsen August 2-17, 2012 Institute of Ocean Sciences Cruise 2012-20 Humfrey Melling – Chief Scientist Fisheries & Oceans Canada Collaborating Institutions: Institute of Ocean Sciences, University of Delaware, Oxford University, Danish Technical University, Scottish Association for Marine Science 1 Cover photo, courtesy of Jason Box: View looking south across the Petermann ice shelf towards Joe Island, Kennedy Channel and Ellesmere Island at the horizon. Note the small ice-shelf fragments in the foreground and cracks within the protruding lobe of the ice . The photograph taken in 2009, before the large ice islands calved from the shelf in August 2010 and again in July 2012. 2 Report on the Scientific Cruise of CCGS Henry Larsen, August 2012 Canadian Arctic Through-flow CCGS Henry Larsen in Nares Strait August 2-17, 2012 Overview The Canadian Arctic Through-flow (CAT) study embodies ten years’ effort within Canada and the international community to measure flows of seawater and ice through the Canadian Archipelago, between the Arctic and the Atlantic Oceans. CATs is the outgrowth of a pilot effort, the Arctic Canada Watch, established in 1997. Moorings enabling year-round measurements were first placed in western Lancaster Sound and Cardigan Strait in 1998. These carried instruments to measure current, temperature and salinity and utilized innovations to address the unique challenges of observing: 1) current direction near the geomagnetic pole; 2) salinity within the hazardous 30-m zone beneath drifting ice pack. These early installations have been maintained and augmented since 1998. In 2003, a large array of instruments was installed across the third principal path for Canadian Arctic through-flow, Nares Strait. -
Of the Inuit Bowhead Knowledge Study Nunavut, Canada
english cover 11/14/01 1:13 PM Page 1 FINAL REPORT OF THE INUIT BOWHEAD KNOWLEDGE STUDY NUNAVUT, CANADA By Inuit Study Participants from: Arctic Bay, Arviat, Cape Dorset, Chesterfield Inlet, Clyde River, Coral Harbour, Grise Fiord, Hall Beach, Igloolik, Iqaluit, Kimmirut, Kugaaruk, Pangnirtung, Pond Inlet, Qikiqtarjuaq, Rankin Inlet, Repulse Bay, and Whale Cove Principal Researchers: Keith Hay (Study Coordinator) and Members of the Inuit Bowhead Knowledge Study Committee: David Aglukark (Chairperson), David Igutsaq, MARCH, 2000 Joannie Ikkidluak, Meeka Mike FINAL REPORT OF THE INUIT BOWHEAD KNOWLEDGE STUDY NUNAVUT, CANADA By Inuit Study Participants from: Arctic Bay, Arviat, Cape Dorset, Chesterfield Inlet, Clyde River, Coral Harbour, Grise Fiord, Hall Beach, Igloolik, Iqaluit, Kimmirut, Kugaaruk, Pangnirtung, Pond Inlet, Qikiqtarjuaq, Rankin Inlet, Nunavut Wildlife Management Board Repulse Bay, and Whale Cove PO Box 1379 Principal Researchers: Iqaluit, Nunavut Keith Hay (Study Coordinator) and X0A 0H0 Members of the Inuit Bowhead Knowledge Study Committee: David Aglukark (Chairperson), David Igutsaq, MARCH, 2000 Joannie Ikkidluak, Meeka Mike Cover photo: Glenn Williams/Ursus Illustration on cover, inside of cover, title page, dedication page, and used as a report motif: “Arvanniaqtut (Whale Hunters)”, sc 1986, Simeonie Kopapik, Cape Dorset Print Collection. ©Nunavut Wildlife Management Board March, 2000 Table of Contents I LIST OF TABLES AND FIGURES . .i II DEDICATION . .ii III ABSTRACT . .iii 1 INTRODUCTION 1 1.1 RATIONALE AND BACKGROUND FOR THE STUDY . .1 1.2 TRADITIONAL ECOLOGICAL KNOWLEDGE AND SCIENCE . .1 2 METHODOLOGY 3 2.1 PLANNING AND DESIGN . .3 2.2 THE STUDY AREA . .4 2.3 INTERVIEW TECHNIQUES AND THE QUESTIONNAIRE . .4 2.4 METHODS OF DATA ANALYSIS . -
Regional Maps of Locations Mentioned in Global Review of The
Regional Maps of Locations Mentioned in Global Review of the Conservation Status of Monodontid Stocks These maps provide the locations of the geographic features mentioned in the Global Review of the Conservation Status of Monodontid Stocks. Figure 1. Locations associated with beluga stocks of the Okhotsk Sea (beluga stocks 1-5). Numbered locations are: (1) Amur River, (2) Ul- bansky Bay, (3) Tugursky Bay, (4) Udskaya Bay, (5) Nikolaya Bay, (6) Ulban River, (7) Big Shantar Island, (8) Uda River, (9) Torom River. Figure 2. Locations associated with beluga stocks of the Bering Sea and Gulf of Alaska (beluga stocks 6-9). Numbered locations are: (1) Anadyr River Estuary, (2) Anadyr River, (3) Anadyr City, (4) Kresta Bay, (5) Cape Navarin, (6) Yakutat Bay, (7) Knik Arm, (8) Turnagain Arm, (9) Anchorage, (10) Nushagak Bay, (11) Kvichak Bay, (12) Yukon River, (13) Kuskokwim River, (14) Saint Matthew Island, (15) Round Island, (16) St. Lawrence Island. Figure 3. Locations associated with beluga stocks of the Chukchi and Beaufort Seas, Canadian Arctic and West Greenland (beluga stocks 10-12 and 19). Numbered locations are: (1) St. Lawrence Island, (2) Kotzebue Sound, (3) Kasegaluk Lagoon, (4) Point Lay, (5) Wain- wright, (6) Mackenzie River, (7) Somerset Island, (8) Radstock Bay, (9) Maxwell Bay, (10) Croker Bay, (11) Devon Island, (12) Cunning- ham Inlet, (13) Creswell Bay, (14) Mary River Mine, (15) Elwin Bay, (16) Coningham Bay, (17) Prince of Wales Island, (18) Qeqertarsuat- siaat, (19) Nuuk, (20) Maniitsoq, (21) Godthåb Fjord, (22) Uummannaq, (23) Upernavik. Figure 4. Locations associated with beluga stocks of subarctic eastern Canada, Hudson Bay, Ungava Bay, Cumberland Sound and St. -
Space Use and Movement Patterns of North Baffin Caribou
Space Use and Movement Patterns of North Baffin Caribou NWMB Project No. 03-09-01 Field Summary and Progress Report September 2011 1Deborah A. Jenkins and 2Jaylene Goorts 1Wildlife Research Biologist, Baffin Region, DoE, GN 2 Wildlife Technician, Baffin Region, DoE, GN PROJECT LEADER Deborah Jenkins, Baffin Region Wildlife Research Biologist Department of Environment, Government of Nunavut P.O. Box 400, Pond Inlet, Nunavut. Phone: (867) 899-8876 Email: [email protected] ACKNOWLEDGEMENTS This project was funded by the Department of Environment, Government of Nunavut, Baffinland Iron Mines Inc., the Nunavut Wildlife Management Board, and Polar Continental Shelf Project. It was further supported by the Hunters and Trappers Organizations (HTO) from five local communities, Pond Inlet, Arctic Bay, Clyde River, Igloolik and Hall Beach and by Parks Canada. Special thanks to our pilots Louis Drapeau (2008), Matt O’Brian (2009), Elou (2010) and Maltee Dahler (2011) and engineer Jason Simms. The wildlife capture and collaring team of Heli-Horizons, Paul Dubois, Laurier Breton, and Rolland Lemieux were outstanding. Thanks to a team of observers Grigor Hope, Sheatie Tagak, Mitch Campbell, Jaypiti Inutiq, Andrew Maher, Gerry Courtemanche, Susan Breckon, Alex Millar, Jaylene Goorts, and Ben Widdowson. Personnel at the Mary River exploration camp were extremely helpful, particularly, Trevor Myers, Jim Millard, Cheryl Wray, Cliff Pilgrim, Brian Larson, Dalton Head, David McCann, Jeff Bush, Kirk Keller, Roland Landry, Wendy Wiseman, and John McLean. Thanks to the kitchen crew that feed us so well. Finally, a special thanks to Mike Kristjanson and Tim McCagherty at PCSP for their logistical support, Mitch Campbell for lending his collaring expertise when the program was initiated, to Jane Chisholm for her assistance with permits, and to Grigor Hope for technical support. -
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. -
From Science to Survival: Using Virtual Exhibits to Communicate the Significance of Polar Heritage Sites in the Canadian Arctic
Open Archaeology 2016; 2: 209–231 Original Study Open Access Peter Dawson*, Richard Levy From Science to Survival: Using Virtual Exhibits to Communicate the Significance of Polar Heritage Sites in the Canadian Arctic DOI 10.1515/opar-2016-0016 Received January 20, 2016; accepted October 29, 2016 Abstract: Many of Canada’s non-Indigenous polar heritage sites exist as memorials to the Heroic Age of arctic and Antarctic Exploration which is associated with such events as the First International Polar Year, the search for the Northwest Passage, and the race to the Poles. However, these and other key messages of significance are often challenging to communicate because the remote locations of such sites severely limit opportunities for visitor experience. This lack of awareness can make it difficult to rally support for costly heritage preservation projects in arctic and Antarctic regions. Given that many polar heritage sites are being severely impacted by human activity and a variety of climate change processes, this raises concerns. In this paper, we discuss how virtual heritage exhibits can provide a solution to this problem. Specifically, we discuss a recent project completed for the Virtual Museum of Canada at Fort Conger, a polar heritage site located in Quttinirpaaq National Park on northeastern Ellesmere Island (http://fortconger.org). Keywords: Arctic; Heritage, Fort Conger, Virtual Reality, Computer Modeling, Education, Climate Change, Polar Exploration, Digital Archaeology. 1 Introduction Climate change and the emerging geopolitical significance of the Arctic have important implications for Canada’s polar heritage. In many Arctic regions, thawing permafrost, land subsidence, erosion, and flooding are causing irreparable damage to heritage sites associated with Inuit culture, historic Euro-North American exploration, whaling and the fur trade (Blankholm, 2009; BViikari, 2009; Camill, 2005; Hald, 2009; Hinzman et al., 2005; Morten, 2009; Stendel et al., 2008). -
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. -
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. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
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.