S. BRIAN Mccann (1935–2004)
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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. -
Page 1 So Gr Renandode Onlagrenje Sopssjc Sprapb0496 #125472 One
ᓄᓇᕘᒥ ᐊᕙᑎᓕᕆᔨᒃᑯᑦ ᑲᑎᒪᔨᖏᑦᑎᒍᑦ ᑐᒃᓯᖅᑑᑦ ᕿᒥᕐᕈᔭᒃᓴᖅ #125472 One Ocean Expeditions - Arctic 2019 cruise season ᑐᒃᓯᖅᑑᑕᐅᔪᖅ New ᖃᓄᐃᑦᑑᓂᖓ: ᐱᓕᕆᐊᕆᔭᐅᔪᒪᔫᑉ ᐳᓚᕋᖅᑐᓕᕆᓂᖅ ᖃᓄᐃᑦᑑᓂᖓ: ᐅᓪᓗᖓ 5/30/2019 5:47:04 PM ᑐᒃᓯᖅᑑᑎᓕᐊᕕᓂᐅᑉ: Period of operation: from 0001-01-01 to 0001-01-01 ᑲᔪᓯᒃᑲᐃᔨᐅᓂᐊᕋᓱᒋᔭᐅᔪᑦ: from 0001-01-01 to 0001-01-01 ᐱᓕᕆᐊᖃᕈᒪᔪᖅ: Aaron Lawton One Ocean Expeditions 38141 2nd Ave Squamish British Columbia V8B 0A6 Canada ᐅᖄᓚᐅᑏᑦ: 6043904900, ᓱᑲᔪᒃᑯᑦ: ᑐᓴᐅᒪᔭᒃᓴᑦ ᖃᓄᐃᑦᑑᑎᓂᒃ ᐱᓕᕆᐊᖃᕐᓂᐊᕆᐊᖓᓐᓂᒃ ᖃᓪᓗᓈᑎᑐᑦ: Expedition cruise tourism in the Canadian Arctic with a maximum of 146 passengers and 25 staff from around the world. We plan to operate 5 voyages in Nunavut on the RCGS Resolute from July 2019 through to September 2019. Ship visits are concentrated in ice- free zones and in arctic communities. Visits ashore last generally no longer than three hours.Our ship, the RCGS Resolute will drift or drop anchor while passengers disembark into small inflatable zodiacs. Passengers will cruise in zodiacs or will land on shore where appropriate. ᐅᐃᕖᑎᑐᑦ: Description du Projet :Nos opérons un vaisseau de tourisme style expédition capable de transporter un maximum de 146 passagers et 25 employés que nous employons de partout dans le monde. Nous planifions opérer 5 voyages dans le Nunavut en 2019 abord le RCGS Resolute à partir du mois de juillets jusqu’au mois de septembre. Les visites à bateau sont concentrées dans les zones d’eau libre ou se trouve la plupart des communautés de L’arctique. Nos visites ne durent pas plus que trois heures. ᐃᓄᒃᑎᑐᑦ: ᐱᓕᕆᐊᒃᓴᐃᑦ ᐅᓂᒃᑳᖏᑦ:ᐅᒥᐊᕐᔪᐊᒃᑯ ᐳᓚᕋᑦᑐᓕᕆᓂ ᑲᓇᑕᐅᑉ ᐅᑭᐅᖅᑕᖅᑑ ᐃᒪᖓᓂ ᐳᓚᕋᑎᓂ ᓂᕆᐅᒋᔭᐅᔪ 146 ᐊᑭᓖᓯᒪᔪᑦ ᐳᓚᕋᑏᑦ 25ᓂ ᐳᓚᕋᑐᓕᕆᔨᓂ ᐃᖃᓇᐃᔭᖅᑎᖃᕋᔭᖅᑐᑦ ᓄᓇᕐᔪᐊᒥᖓᕈᓘᔭᕋᔭᖅᐳᑦ. -
Instructions Nautiques
Volume 1, quatneme edition DFO - Libra I MPO - Bibllothequel II I II lill 1111111 II II 14062957 INSTRUCTIONS NAUTIQUES ARCTIQUE CANADIEN VK 808 157 V.1 1994 Peches Fisheries et Oceans and Oceans Canadi t - LSANS CANIOC\ '1471rognyme C!:•(iermel)n Rimouski (01,14bed 35:_ 484 TOL et fax ,418) `,723-18,31 marinas, topographiques et mattes VK 808 157 V.1 1994 Service hydrographique d.. Instructions nautiques : Arctique canadien, vol. 1 179860 14062957 c.1 INSTRUCTIONS NAUTIQUES-ARCTIQUE CANADIEN Volume 1 Photographie de couyerture — Brise- glace NGCC George R. Pearkes escortant les remorqueurs Angus Sherwood et Johnny Hope. Le Service hydrographique du Canada produit et distribue des Cartes marines, des Instructions nautiques, des Guides nautiques et des Tables des mardes des voies navigables du Canada. Les usagers de cette publication sont pries de signaler les dangers nouvellement reperes, les changements des aides a la navigation, l'existence de nouveaux hauts-fonds ou chenaux, les erreurs d'impression ou autres renseignements utiles a la correction des cartes marines et des publications hydrographiques touchant les eaux canadiennes au : Directeur general Service hydrographique du Canada Ministere des Peches et des Oceans Ottawa (Ontario) K 1 A 0E6 Les Instructions nautiques, Guides nautiques, Tables des maries, Tables des niveaux de l'eau, Rapports des activites et Marine Sciences Papers sont publies par la Direction generale des communications pour le Service hydrographique du Canada. On peut se procurer ces publications par le Groupe Communication Canada — Edition ou au Service hydrographique du Canada. YGO INSTRUCTIONS NAUTIQUES ARCTIQUE CANADIEN VOL. 1 QUATRIEME EDITION 1994 Ministere des Vetches et des Oceans Ottawa, Canada ©Ministre des Approvisionnements et Services Canada 1994 En vente par la poste au : Groupe Communication Canada — Edition Ottawa, Canada K1A 0S9 ou chez votre libraire ou au Bureau de distribution des cartes marines Ministere des Peches et des Oceans C.P. -
Marine Navigationalert
Marine Navigation Alert Jeppesen MARINE NAVIGATION ALERTS contain significant information affecting Jeppesen Charts and/or Technology. They are regularly updated at www.jeppesen.com/marinealerts/ Date: October 10 , 2012 Subject: Removal of Canadian charts from C-MAP by Jeppesen products (see Table 1 for a detailed list of charts removed) Affected Products: C-MAP NT, C-MAP NT+, C-MAP (iOS) , C-MAP MAX, C-MAP MAX Pro, C-MAP 4D , C-MAP 4D EMBEDDED, C-MAP MAX EMBEDDED, C-MAP WORLDFOLIO (Passport Charts), C-MAP by Jeppesen MM3D (see Table 2 at the end of this document for a detailed list of affected products) Jeppesen would like to inform its customers operating in Canadian waters that per contractual requirements with the Canadian Hydrographic Service (CHS), Jeppesen has removed select charts from its products which were derived from official CHS paper charts. The Canadian Hydrographic Service (CHS) considers these charts inadequate for conversion to digital format, and for use in digital navigation systems (including GPS Chart Plotters). To minimize the impact of this change, areas where charts were removed have been covered with smaller scale charts, whenever possible. As a consequence of removing these charts, Jeppesen has discontinued a number of cartridge codes (see the list of affected cartridges below). Jeppesen customers in possession of the following cartridges won’t be able to update their products until further notice : C-MAP NT+: M-NA-C126.31, M-NA-C152.31, M-NA-C176.31, M-NA-C178.31, M-NA-C179.31, M-NA-C209.31, M-NA-C210.31, M-NA-C217.31, M-NA-C218.31, M-NA-C219.31, M-NA-C221.31, M-NA-C222.31, M-NA-C250.31 C-MAP MAX: M-NA-M048.21, M-NA-M176.21, M-NA-M178.21, M-NA-M179.21, M-NA-M209.21, M-NA-M210.21, M-NA-M217.21, M-NA-M218.21, M-NA-M219.21, M-NA-M250.21, M-NA- M330.21 C-MAP 4D: M-NA-D048.08, M-NA-D176.08, M-NA-D178.08, M-NA-D179.08, M-NA-D209.08, M- NA-D210.08, M-NA-D217.08, M-NA-D218.08, M-NA-D219.08, M-NA-D250.08, M-NA-D330.08 iOS: M-NA-I048.08 Jeppesen will continue to work with CHS to provide high quality chart coverage as soon as possible. -
1988 Science·Institute Of·The·Northwest·Territories
NORTHWEST· TERRITORIES SCIENTIFIC·RESEARCH · 1988 SCIENCE·INSTITUTE OF·THE·NORTHWEST·TERRITORIES Contents Introduction ... iii Baffin Region ... 1 lnuvik Region ... 23 Keewatin Region ... 33 Kitikmeot Region ... 39 Fort Smith Region . 45 Index by Researcher ... 53 Index by Category ... 55 Research Reports . .. 60 Regional Map ... 64 Introduction Research Licence. The only exceptions are archaeology, which is administered Was the Arctic once a lush tropical envi by the Prince of Wales Northern Heritage ronment inhabited by dinosaurs? Centre in Yellowknife, and studies of land animals, which are licenced through the Who were the people who lived on Elles Wildlife Management Division of the De mere Island in the High Arctic thousands partment of Renewable Resources, also of years ago? in Yellowknife. How prepared are the communities in the The Scientific Research Licences were Eastern Arctic for the economic develop established for a number of reasons. ment that would follow the establishment Generally, it was felt that northern resi of Nunavut? dents should be informed about and invit ed to participate in research that occurs What sort of a fish is an Arctic Cisco? in and around their communities. To this end, scientists are required to discuss Should northerners be worried about their proposed research with local com contaminants in their country food? munity representatives before they begin work. They must also submit reports on Can computers be used to predict their research results when they are fin the way a forest fire will spread? ished and are encouraged to give public presentations where appropriate. In addition, the licencing information is contributed to the Arctic Science and These are just a few of the questions Technology Information System, a com scientists in the N.W.T. -
Queen Elizabeth Islands Game Survey, 1961
•^i.ri.iri^VJU.HIJJ^^^iiH^ Queen Elizabeth Islands Game Survey, 1961 by JOHN S. TENER OCCASIONAL PAPERS No. 4 QUEEN ELIZABETH ISLANDS GAME SURVEY, 1961 by John S. Tener Canadian Wildlife Service Occasional Papers Number 4 National Parks Branch Department of Northern Affairs and National Resources Issued under the authority of the HONOURABLE ARTHUR LAING, P.C, M.P., B.S.A.. Minister of Northern Affairs and National Resources ROGER DUHAMEL, F.R.S.C. Queen's Printer and Controller oi Stationery, Ottawa, 1963 Cat. No. R 69-1/4 CONTENTS 5 ABSTRACT 6 INTRODUCTION 7 OBJECTIVE Personnel, 7 Itinerary, 7 8 METHOD Logistics, 8 Survey design, 8 Survey method, 9 Sources of error, 11 13 RESULTS Caribou and muskoxen on the Islands Devon, 14 Mackenzie King, 28 Cornwallis, 14 Brock, 29 Little Cornwallis, 15 Ellef Ringnes, 29 Bathurst, 15 Amund Ringnes, 30 Melville, 20 Lougheed, 31 Prince Patrick, 23 King Christian, 32 Eglinton, 26 Cornwall, 32 Emerald, 27 Axel Heiberg, 32 Borden, 27 Ellesmere, 33 38 SPECIES SUMMARY Avifauna American and Gyrfalcon, 40 black brant, 38 Peregrine falcon, 41 Snow geese, 39 Rock ptarmigan, 41 Old Squaw, 40 Snowy owl, 41 King eider, 40 Raven, 41 Mammalian fauna Polar bear, 42 Seals, 44 Arctic fox, 43 Peary caribou, 45 Arctic wolf, 44 Muskoxen, 47 49 SUMMARY 50 REFERENCES LIST OF TABLES I Survey intensity of the Islands, 13 II Calculations, estimated caribou population, Bathurst Island, 18 III Calculations, estimated muskox population, Bathurst Island, 19 IV Observations from the ground of four muskox herds, Bracebridge Inlet, -
From Wherever the Fast Ice Edge Is Located in Lancaster Sound Or Barrow Strait, and in an Easterly Direction from M'clure Strait and Amundsen Gulf
from wherever the fast ice edge is located in Lancaster Sound or Barrow Strait, and in an easterly direction from M'Clure Strait and Amundsen Gulf. Figure 7.3.1.8 presents the average date of occurrence for each event as well as the range of dates recorded over 13 years (Gorman 1988). Break-up of the ice cover between each of the geographic locations occurs very rapidly; in the order of days (Dickins 1983; Gorman 1986). In most years, the ice sheet becomes extensively fractured and then breaks into large floes in the order of tens of kilometres (Maxwell 1980). b) Prince of Wales Strait Prince of Wales Strait is one of two channels to be used by the Polar 8 to access the Beaufort Sea from Parry Channel. It is a narrow channel, and concerns were raised during the Beaufort EIS over the effect of icebreaking ships on the ice regime of such channels. The ice regime of Prince of Wales Strait and possible effects of ship traffic were the subject of a discussion paper written by Dickens (1983) on behalf of the proponents of the Beaufort Sea development. The Strait is typically covered by stable landfast ice from late October until mid to late Julf(Dickins 1983; Gorman 1988). Gorman (1988) reported the average date of fracture was July 15 with a range from July 5 to 28 based on 13 years of data. Dickins (1983) divided the ice regime into north and south sections of the channel, separated by the Princess Royal Islands. Break-up begins in the south section and is extremely variable with up to three weeks between first fracturing and major ice movement (Dickins 1983). -
Haughton Astrobleme: a Mid-Cenozoic Impact Crater Devon Island, Canadian Arctic Archipelago
Haughton Astrobleme: A Mid-Cenozoic Impact Crater Devon Island, Canadian Arctic Archipelago T. FRISCH’ and R. THORSTEINSSON’ ABSTRACT. Haughton Astrobleme is a nearly circular impact crater with a diameter of about 16km and a central uplift in Devon Island. Bedrock exposed in the crater comprised the followingmainly carbonate Lower Ordovician to, Upper Silurian formations in order upward: Eleanor River, Bay Fiord, Thumb Mountain, Irene Bay and Allen Bay. The Eleanor River Formation in the centre of the crater is raised about 480 m above its normal stratigraphic position outside the crater. The much shattered and faulted lower Paleozoic rocks within thecrater contrast markedly with the subhorizontal surrounding strata.The AllenBay Formation constitutes surface exposure around all but the easternmost part of the crater’s border where the Thumb Mountain and Irene Bay Formations are exposed. Also exposed in the crater are two newly recognized, and as yet unnamed, formations: a polymict impact breccia that overlies the lower Paleozoic rocks, with marked angular unconformity and crops out over about a quarter of the area of the crater; and a unit of lake sediments near the western border of the crater that lies disconformably on the impact breccia and with angular’unconformity on the lower Paleozoic rocks. The impact breccia is composed chiefly of carbonate rocks, but locally contains clasts of Precambrian crystalline basement from a depth estimated to be at least 1700 m. The basement clasts show varying degrees of shock metamorphism, the highest being that displayed by rocks with vesicular, flow-banded feldspar or quartz glass. Coesite has been identified in a sample of gneiss. -
Seabird Colonies and Distributions Around Devon Island and Vicinity1
Seabird Colonies and Distributions around Devon Island and Vicinity1 DAVID N. NETTLESHIP2 ABSTRACT. Nineteen glaucous gull (Larus hyperboreus) colonies, two Thayer’s gull (L. thayeri) colonies, andthree fulmar (Fulmnrusglacialis) colonies were recorded duringone intensive, and several short,aerial surveys around Devon Island in the summer of 1972. Observations were also made of distributions of seabirds at sea and at colonies on some adjacent islands (Dundas, Margaret, Baillie- Hamilton, and Cornwallis). Only 2 of the 29 colonies examined have been described previously. The greatimportance of LancasterSound to the present and future welfare of arctic seabirdsis discussed. RÉSUMÉ. Les colonies d‘osiseaur demer et leur distribution autourde de Devon et dans son voisinage. Au cours d’une reconnaissance aérienne importante et de plusieurs autres plus courtes autour de l’île de Devon à l’été 1972, on a relevé dix-neuf colonies de Goéland bourgmestre (Larus hyperboreus), deux de Mouette de Thayer (Larus thayeri) et trois de Fulmar boréal(Fulmarus glacialis). On a aussi observé la distribution des oiseaux en meret dans les colonies de quelques îles adjacentes (Dundas, Margaret, Baillie-Hamilton et Cornwallis). Deux seulement de ces 29 colonies ont déjà été décrites. L‘auteur discute de la grande importance du détroit de Lancaster pour le bien-être présent et futur des oiseaux de mer arctiques. PE3IOME. ITomnuu ~~opmuxnmuy e pa&w ocmposa fleaow. B pesynb~a~e 06CJIenOBaHMfi C BO3AyXa JIeTOM 1972 r. OIIElCaHbI XOJIOHHH YaeX (Larus hyperboreus H L. thayeri) M rnymsmefi (Fulmarus glacialis) B paitoHe ocTposa AeBoH. IIpo~o- nnnncb Taxace H~~JIKI~~HHKpacnpeneneHm IITHII B Mope M ICOJIOHM~~Ha cocenxmx OCTpOBaX (AaHRaC, Mapra eT, &&JIJIH-raMHJIbTOH M ~OpHyOJIJIHC).TOnbXO2 y13 29 06~apywe~Hb1xRonOHHg Lm omcaHb1 npexae. -
Arctic & Greenland Expedition Cruise
KANGERLUSSUAQ TO NOME: ARCTIC & GREENLAND EXPEDITION CRUISE Follow the route of explorers that looked for the Northwest Passage, from Frobisher in the 1570s right up to the world’s most important modern day explorer: you. Whether you are a first timer or well-initiated in the region, expect the savage beauty to seduce you time and time again. From crystal clear glaciers to the abundant marine and bird life, this Northwest Passage crossing is both mesmerising and memorable. ITINERARY Day 1 Kangerlussuaq Kangerlussuaq is a settlement in western Greenland in the Qeqqata municipality located at the head of the fjord of the same name (Danish: Søndre Strømfjord). It is Greenland's main air transport hub and the site of Greenland's largest commercial airport. The airport dates from American settlement during and after World War II, when the site was known as Bluie West-8 and Sondrestrom Air Base. The Kangerlussuaq area is also home to Greenland's most diverse terrestrial fauna, including muskoxen, caribou, and gyrfalcons. The settlement's economy and population of 512 is almost entirely reliant on the airport and tourist industry. Day 2 Kangaamiut (Qeqqata) & Evighedsfjord Only 350 people live in the small Greenlandic community of Kangaamiut. Located on the south coast of Timerdlit Island and facing the Davis Strait, Kangaamiut is situated between the mouths of two long fjords: the Kangerlussuatsiaq Fjord (or Evighedsfjorden in Danish) to its south and to its north Kangaamiut Kangerluarsuat Fjord. Founded in 1755, it was called “Sugarloaf” (Sukkertoppen) because of the appearance of three nearby hills. Within roughly an hour of steaming south from Kangerlussuaq Fjord is Evighedsfjord Fjord. -
Richard Et Al. 2001
ARCTIC VOL. 54, NO. 3 (SEPTEMBER 2001) P. 207–222 Summer and Autumn Movements and Habitat Use by Belugas in the Canadian High Arctic and Adjacent Areas P.R. RICHARD,1 M.P. HEIDE-JØRGENSEN,2 J.R. ORR,1 R. DIETZ3 and T.G. SMITH4 (Received 18 November 1999; accepted in revised form 25 January 2001) ABSTRACT. Twenty-one adult belugas (8M, 13F) were live-captured and instrumented with satellite-linked transmitters in the summer and fall of 1996. Twelve were captured in estuaries along the coast of Somerset Island in July and nine were captured in September in Croker Bay, SE Devon Island. This paper reports on the summer and autumn movements and dive depths of these animals from late July 1996 until the last tags ceased transmitting in November 1996. Of the 12 captured in July, 11 provided data for 30–126 days (mean = 84 days). Most of the animals moved rapidly to southern Peel Sound, where they all spent the month of August, making frequent deep dives, some of which were to depths near or at the seabed of the Franklin Trench. The belugas also used several bays along the coast of Prince of Wales Island and another one on Melville Peninsula. They left southern Peel Sound between late August and early September and moved rapidly to the south coast of Devon Island, many using Maxwell Bay and Croker Bay for several days. All belugas instrumented in Croker Bay in September, as well as the summer-tagged individuals that were still transmitting, moved east and north along the south and east coasts of Devon Island, eventually reaching Jones Sound and north Baffin Bay. -
Distribution, Movement and Abundancoef Polar Bears In
ARCTIC VOL. 35. NO. 1 (MARCH lSW), P. 159-189 Distribution, Movement and Abundanceof Polar Bearsin Lancaster Sound, Northwest Territories R.E. SCHWEINSBURG,’ L.J. LEE’ and P.B. LATOUR’ ABSTRACT. Mark-recapture studies show that polar bears are distributed at varying densities throughout Lancaster Sound during winter and spring. Major concentrations occur along the north and south coasts and the transverse floe edge at themouth of the sound. As the ice melts, some bears move west whereas others move to nearby land areas. There is some evidence that as the ice forms, polar bears return from their summer locations to eastern Lancaster Sound.Polar bears of Lancaster Sound are part of the larger population whose western range extends to Barrow Strait, Prince Regent Inlet, Wellington Channel and Jones Sound. The southern and eastern range limits are unknown although this population may extend at least to Clyde River on northeastern Baffin Island and probably to Greenland. Maternity denning appears to be widespread over the study area probably because of the abundance of suitable habitat. We estimated a population of 1031 2236 polar bears in Lancaster Sound during 1979; however, more estimates are needed to determine if this relatively high number is normal for the area. Key words: polar bear, distribution, movement, abundance, Baffin Bay, Lancaster Sound, summer retreat, denning RÉSUMÉ. Les ttudesde “marquage-recapture” dtmontrent que les ours polaires sont rkpartis selon des densittsvariables &traversle dttroit de Lancasterdurant l’hiver et le printemps. Les concentrations les plus importantes se trouvent le long des c6tesnord et sud et sur la bordure transversale de la glace en derive &l’embouchuredu dttroit.