Svalbard Golden Light Scenic Special
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Surface Magnetic Anomaly Study on the Eastern Part of the Forlandsundet Graben
Surface magnetic anomaly study on the eastern part of the Forlandsundet Graben A. A. KRASIL'ScIKOV*, A. P. KUBANSKIJ'* and Y. OHTA Krasil'Stikov, A. A,, Kubanskij, A. P. & Ohta, Y. 1995: Surface magnetic anomaly study on the eastern part of the Forlandsundet Graben. Polar Research 14(1), 55-68. A surface magnetic survey was carried out by use of a proton magnetometer over wide strandflats along the eastern coast of Forlandsundet, western Spitsbergen, to decipher subsurface structures and lithologies. Distinctive linear high-anomaly segments and zones were recognised on the magnetic anomaly maps. These zones coincide well with the eastern marginal fault of the Tertiary Forlandsundet Graben and associated faults north of St. Jonsfjorden, while they reflect bedrock lithologies in the south. The high-anomaly segments, which constitute the zones, are locally aligned in a left-stepping. en echelon arrangement within the zones, indicating a dextral transpressional stress regime on the eastern marginal fault of the graben during a certain time. Sudden termination and bends of the segments define a later transverse fault system. A. A. Kradftikou and A. P. Kubanskij, Polar Marine Geological Expedition, ul. Pobeda, 24, 189510 Lomonosou. Russia; Y. Ohta, Norwegian Polar Institute, P.O. Box 5072 Majorstua. N-0301 Oslo, Norway. Introduction Kleinspehn & Teyssier (1992), Gabrielsen et al. (1992) and Lepvrier (1992), and various esti- Pronounced coastal plains have developed on the mations of the subsurface geology have been pro- eastern coast of Forlandsundet, 1.5-6 km in posed. width, extending N-S for approximately 75 km The areas have complex structures resulting from Engelskbukta to the northern side of Isfjor- from Caledonian thrusting which was overprinted den (Fig. -
Spitsbergen & the Svalbard Archipelago 2019
Field Guides Tour Report The Norwegian Arctic: Spitsbergen & the Svalbard Archipelago 2019 Jun 26, 2019 to Jul 6, 2019 John Coons & Doug Gochfeld For our tour description, itinerary, past triplists, dates, fees, and more, please VISIT OUR TOUR PAGE. Polar Bear. What more is there to say? Actually there is much more to be said for this most-wanted iconic Arctic mammal. This female, who could have been pregnant by the looks of her, was as at home on the pack ice as one could imagine her being anywhere. After a nap, she curiously approached the ship, before eventually sauntering off across the windswept, seemingly desolate sea ice which stretched to the horizon, and indeed beyond the limits of our sight. This was certainly the most anticipated moment by many of the participants on the ship, and with good reason. What a majestic creature! Photo by guide Doug Gochfeld. The Arctic. That word is one of the most evocative of any which describes a region on this planet. There aren’t many places where you can easily access it, and none of those are as far north as Svalbard. Our journey not only got us up to some of the farthest north tundra, but it also brought us into the Arctic sea ice itself. It all started with a flight from Oslo, the culturally rich capital of the northern kingdom of Norway, across the ocean where the Norwegian and Barents Seas meet, to Longyearbyen, the only substantial settlement on the Svalbard Archipelago. The windswept “city,” along the southern shores of Isfjorden, was established as a coal mining settlement many moons ago, but nowadays there is only one very insignificant mine still active, and it has transformed into a tourism & research-centric town. -
Census of Breeding Seabirds on the Northwest Coast of Svalbard 1973 and 1978
Census of breeding seabirds on the northwest coast of Svalbard 1973 and 1978 CHRISTIAN KEMPF AND BENO~TSI~ER Kempf, C. & Sittler, B. 1988: Census of breeding seabirds on the northwest coast of Svalbard 1973 and 1978. Polar Research 6, 195-203. The western coast of Svalbard is one of the world's most important seabird regions (Belopol'skij 1961; L0venskiold 1964; Norderhaug et al. 1977), due to the favourable water temperatures, light regime and amounts of mineral salts (Norderhaug et al. 1977). Seabirds have been censused several times in this area (Kristoffersen 1962; Larsen 1965; Dhondt et al. 1969; Voisin 1970; Norderhaug 1974; Sendstad 1978; Alendal et al. 1982). Except for Larsen (1965), there is no comprehensive and quantitative survey of any part of northwestern Svalbard. Further east, Jepsen & Mobrek (1983) surveyed the area between GrPhuken and Nordaustlandet. Recent concern about the potentially detrimental effects of planned oil exploration and increased human activities in the high Arctic has emphasized the need for more information on the ecology in these regions. This paper provides more comprehensive data on seabird populations in northwestern Svalbard, between southern Prins Karls Forland and Verlegenhuken. The results supplement the studies carried out in 1978 and 1979 by Jepsen & Mobzk (1983) between Verlegenhuken and Kong Karls Land. Chrbtian Kempf and Benoit Sittler, Groupe de Recherches en Ecologie Arctique, 68660 Rombach le Franc, France; December 1986 (reuised September 1988). General area description In 1978, a party of 9 people with base camp at Sorgattet (between Magdalenefjorden and The northwest coast of Svalbard is deeply Smeerenburgfjorden) conducted surveys in indented, with rocky peninsulas rising to 300- Kongsfjorden and Albert I Land (9-13 July), 800 m a.s.1. -
1. Philippe D'auvergne's Glacier Amsterdamøya, Smeerenburg View
1. Philippe d’Auvergne’s Glacier Amsterdamøya, Smeerenburg View east across Smeerenburgfjorden from Smeerenburgsletta. Inserted historical images from left to right, top: 1693 version of Jan Jansz map of “Hollantsche Bay” as published by Hendrick Donker in his De nieuwe geoctroyeerde verbeterde en vermeerdede stuurmans zee-spiegel: T Eerste en tweede deel Van de Nieuwe Stu- urmans Zee-Spiegel. Verlichtende de Noordsche, Ostersche, en Westersche Ship- Vaert, Amsterdam (courtesy, National Library, Portugal). Jan Jan- sz, 1651, “De Hollantsche ofte Mourits-Bay” engraved map published in De Lichtende Columne ofte Zee-Spiegel by Jan Jansz, Amsterdam, 1651 (this version from Wieder 1919). This is the first printed local map of the whaling area in northwest Spitsbergen. To identify the plate of the 1651 version of this map number 22 1/2 is printed in the lower right corner. It also seems to be the first map where two glaciers are each marked as “ysbergh”. Judging from their positions it is most likely todays Kenne- dybreen (left) and Frambreen. Pieter Goos, 1657, “Spitzberga” in De Lichtende Co- lumne ofte Zee-Spiegel originally published by Jan Jansz, Amsterdam, 1651 (cour- tesy, National Library, Spain). Below from left to right: John Clevely’s 1774 ver- sion of “View of an iceberg” in Spitsbergen (courtesy, British Museum). Clevely’s version of the glacier is based on a sketch by Philippe d’Auvergne. The chart of the area made by Constantine Phipps in 1773 and W. Byrne’s print of the “View of an iceberg” based on the sketch by Philippe d’Auvergne as published in 1774 in A voy- age towards the North Pole, undertaken by His Majesty’s Command 1773 by Constantine John Phipps. -
Iron and Manganese Speciation and Cycling in Glacially Influenced High-Latitude Fjord Sediments
Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 141 (2014) 628–655 www.elsevier.com/locate/gca Iron and manganese speciation and cycling in glacially influenced high-latitude fjord sediments (West Spitsbergen, Svalbard): Evidence for a benthic recycling-transport mechanism Laura M. Wehrmann a,b,⇑, Michael J. Formolo b,1, Jeremy D. Owens a,2, Robert Raiswell c, Timothy G. Ferdelman b, Natascha Riedinger a, Timothy W. Lyons a a Department of Earth Sciences, University of California, Riverside, CA, USA b Biogeochemistry Department, Max Planck Institute for Marine Microbiology, Bremen, Germany c School of Earth and Environment, Leeds University, Leeds, UK Received 16 August 2013; accepted in revised form 9 June 2014; available online 20 June 2014 Abstract Glacial environments may provide an important but poorly constrained source of potentially bioavailable iron and man- ganese phases to the coastal ocean in high-latitude regions. Little is known about the fate and biogeochemical cycling of gla- cially derived iron and manganese in the coastal marine realm. Sediment and porewater samples were collected along transects from the fjord mouths to the tidewater glaciers at the fjord heads in Smeerenburgfjorden, Kongsfjorden, and Van Keulen- fjorden along Western Svalbard. Solid-phase iron and manganese speciation, determined by sequential chemical extraction, could be linked to the compositions of the local bedrock and hydrological/weathering conditions below the local glaciers. The concentration and sulfur isotope composition of chromium reducible sulfur (CRS) in Kongs- and Van Keulenfjorden sedi- ments largely reflect the delivery rate and isotope composition of detrital pyrite originating from adjacent glaciers. -
Protected Areas in Svalbard – Securing Internationally Valuable Cultural and Natural Heritage Contents Preface
Protected areas in Svalbard – securing internationally valuable cultural and natural heritage Contents Preface ........................................................................ 1 – Moffen Nature Reserve ......................................... 13 From no-man’s-land to a treaty and the Svalbard – Nordaust-Svalbard Nature Reserve ...................... 14 Environmental Protection Act .................................. 4 – Søraust-Svalbard Nature Reserve ......................... 16 The history of nature and cultural heritage – Forlandet National Park .........................................18 protection in Svalbard ................................................ 5 – Indre Wijdefjorden National Park ......................... 20 The purpose of the protected areas .......................... 6 – Nordenskiöld Land National Park ........................ 22 Protection values ........................................................ 7 – Nordre Isfjorden National Park ............................ 24 Nature protection areas in Svalbard ........................10 – Nordvest-Spitsbergen National Park ................... 26 – Bird sanctuaries ..................................................... 11 – Sassen-Bünsow Land National Park .................... 28 – Bjørnøya Nature Reserve ...................................... 12 – Sør-Spitsbergen National Park ..............................30 – Ossian Sars Nature Reserve ................................. 12 Svalbard in a global context ..................................... 32 – Hopen Nature Reserve -
A Working Stratigraphy for Central Western Oscar Il Land, Spitsbergen
Leslie Kanat and Alan Morris A working stratigraphy for central western Oscar Il Land, Spitsbergen NORSK POLARINSTITUTT OSLO 1988 Leslie Kanat and Alan Morris A working stratigraphy for central western Oscar Il Land, Spitsbergen ------�.... _-_ .... _---- NORSK POLARINSTITUTT OSLO 1988 Cooer page. Deformation in the Chaotic Zone. Two textural oceurrcnccs of veining are common in dolostonc within the Chaotic Zonc. In this drawing, fine grained, rccrystallizcd catadastic quartz (stipp1c) was injcctcd by later quartz vcin (strained) within a massive dolomitic host. The fine graincd texture (stipplc) is typ;cal for quartz in whieh catacl.sis was followcd by rccrystallization accommodated dislocation crcep. Scale bar: 0.5 mm. ISBN 82-90307-52-7 Norsk Polarinstitutt. Printed December 1988 Rolfstangveien 12, 1330 Oslo Lufthavn, Primcd in Great Bruam by Page Bros (Norwkhi Lld Norway Contents Abstract " ,.. ,.... , ........ , .. ,."." ..", ... "... '"",.,., ..."".""""""""".,.",." .. " .....",."""",'.'.', .. '"".","' .... ',, ' .. , , ,., " ,,'. 5 Introduction ,.', , ,."" .. , ,., .. ,., " '" ,.. "'."" ,.""."".,.... , .. "."".",.,.,., ..", .. , ..."."",."."""",.".,.""",.""""""""""", 7 Strandtlat strip rocks (CAR)", .... ... ".""".""." ........ "", .................... , ....... " ... " ... , ...... ,."... ""., .. ,,, 8 Bullbreen Group ..., ",.""., ,.,.... , , .... , .. ,.,.. ' " ..., , .., ,.,.,., ",.. , ,.. , ,.'.", .." ,.,'... , ,... , , .., , .. , ,.. " .. '".. "., ",.", ."., "'" ,.. ", ,., 9 Holmesletfjella Formation (BHI-6)" ...., ..." ,' -
Shipwreck at Cape Flora: the Expeditions of Benjamin Leigh Smith, England’S Forgotten Arctic Explorer
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2013 Shipwreck at Cape Flora: The Expeditions of Benjamin Leigh Smith, England’s Forgotten Arctic Explorer Capelotti, P. J. University of Calgary Press Capelotti, P.J. "Shipwreck at Cape Flora: The Expeditions of Benjamin Leigh Smith, England’s Forgotten Arctic Explorer". Northern Lights Series No. 16. University of Calgary Press, Calgary, Alberta, 2013. http://hdl.handle.net/1880/49458 book http://creativecommons.org/licenses/by-nc-nd/3.0/ Attribution Non-Commercial No Derivatives 3.0 Unported Downloaded from PRISM: https://prism.ucalgary.ca University of Calgary Press www.uofcpress.com SHIPWRECK AT CAPE FLORA: THE EXPEDITIONS OF BENJAMIN LEIGH SMITH, ENGLAND’S FORGOTTEN ARCTIC EXPLORER P.J. Capelotti ISBN 978-1-55238-712-2 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 [email protected] 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 specific work without breaching the artist’s copyright. -
Svalbard Islands SAFARI OVERVIEW
CHEESEMANS’ ECOLOGY SAFARIS 555 North Santa Cruz Avenue Los Gatos, CA 95030-4336 USA (800) 527-5330 (408) 741-5330 [email protected] cheesemans.com Svalbard Islands Realm of the Polar Bear June 23 to July 6, 2020 Polar bear viewing from the Zodiac SAFARI OVERVIEW Sail through Norway’s Arctic past glaciers lit by the midnight sun to find a most mythic predator: the polar bear. This polar adventure is to the famed Svalbard Archipelago of northern Norway. Located between the North Pole and Norway, these islands are home to one of the greatest concentrations of polar bears on Earth. This region remains wild and pristine with its vast mountains, dramatic fjords, massive glaciers, and picturesque icebergs coupled with a myriad of Arctic wildlife. The primary mission of professional photographer leader Scott Davis is to provide you with skills and opportunities to produce quality images of unique Arctic wildlife and beautiful landscapes. HIGHLIGHTS • Adventure north of the Arctic Circle to seek out polar bears in 24 hours of daylight. • Zodiac cruise up to the base of striking cliffs to view nesting seabird colonies. • Slip into Svalbard’s many inlets and straits where larger ships cannot access. • Search for beluga whales, blue whales, humpback whales, and walrus. • Improve your photography skills with biologist-turned-professional-photographer Scott Davis. LEADERS: Scott Davis and Samuel Blanc. Cheesemans’ Ecology Safaris Page 1 of 10 Itinerary Updated: December 2018 DAYS: 14, including estimated travel time. 10 nights aboard our ship. GROUP SIZE: 12. COST: $12,300 per person, single occupancy (each person has a private cabin if they choose), not including airfare. -
Important Bird Areas and Potential Ramsar Sites in Europe
cover def. 25-09-2001 14:23 Pagina 1 BirdLife in Europe In Europe, the BirdLife International Partnership works in more than 40 countries. Important Bird Areas ALBANIA and potential Ramsar Sites ANDORRA AUSTRIA BELARUS in Europe BELGIUM BULGARIA CROATIA CZECH REPUBLIC DENMARK ESTONIA FAROE ISLANDS FINLAND FRANCE GERMANY GIBRALTAR GREECE HUNGARY ICELAND IRELAND ISRAEL ITALY LATVIA LIECHTENSTEIN LITHUANIA LUXEMBOURG MACEDONIA MALTA NETHERLANDS NORWAY POLAND PORTUGAL ROMANIA RUSSIA SLOVAKIA SLOVENIA SPAIN SWEDEN SWITZERLAND TURKEY UKRAINE UK The European IBA Programme is coordinated by the European Division of BirdLife International. For further information please contact: BirdLife International, Droevendaalsesteeg 3a, PO Box 127, 6700 AC Wageningen, The Netherlands Telephone: +31 317 47 88 31, Fax: +31 317 47 88 44, Email: [email protected], Internet: www.birdlife.org.uk This report has been produced with the support of: Printed on environmentally friendly paper What is BirdLife International? BirdLife International is a Partnership of non-governmental conservation organisations with a special focus on birds. The BirdLife Partnership works together on shared priorities, policies and programmes of conservation action, exchanging skills, achievements and information, and so growing in ability, authority and influence. Each Partner represents a unique geographic area or territory (most often a country). In addition to Partners, BirdLife has Representatives and a flexible system of Working Groups (including some bird Specialist Groups shared with Wetlands International and/or the Species Survival Commission (SSC) of the World Conservation Union (IUCN)), each with specific roles and responsibilities. I What is the purpose of BirdLife International? – Mission Statement The BirdLife International Partnership strives to conserve birds, their habitats and global biodiversity, working with people towards sustainability in the use of natural resources. -