DOCSLIB.ORG

December 13, 2016 'Longyearbyen at Its Best:' Modern Tragedies, Triumphs Part of Traditional Tributes During Syttende Mai Celebration Page 7

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
December 13, 2016 'Longyearbyen at Its Best:' Modern Tragedies, Triumphs Part of Traditional Tributes During Syttende Mai Celebration Page 7 FREE Weather summary Cloudy with snow and rain this weekend and next week, with very strong winds at times. icepeople Full forecast page 3 The world's northernmost alternative newspaper Vol. 8, Issue 33 December 13, 2016 www.icepeople.net 'Longyearbyen at its best:' Modern tragedies, triumphs part of traditional tributes during Syttende Mai celebration Page 7 “ To believe that the governor can rescue people out, regardless of circumstances, is wrong. There is no guarantee for that. - Per Andreassen, police lieutenant Svalbard governor's office ” DAG ARNE HUSDAL / LONGYEARBYEN LOKALSTYRE A classic view of Longyearbyen recently became the city's government's Facebook portrait. Norway's government has since released a statistical one. Late update: 12 apartments vacated again due to building, infrastructure damage. Paint by numbers icepeople.net Cold, hard stats add up to compelling portrait of recent drastic change in 'This is Svalbard 2016' By MARK SABBATINI front. Adventdalen in operation. In 2015 there were Editor Those conclusions are part of the "This is about 300 different businesses in Longyear- Tourism and mining have essentially Svalbard 2016" report released this month by byen, Ny-Ålesund and Svea, divided into swamped positions in terms of their economic Statistics Norway. While the document's pre- many different industries, a growth of over 70 importance. Many more foreigners and far sentation is remarkably similar to the initial percent since 2007." See DOCK, page 12 fewer Norwegians are filling those jobs, and report released in 2009 – much of the text is Mining accounted for 30 percent of the on a temporary or part-time basis for less the same with updated numbers plugged in – jobs and half of the total economic output, ac- money than traditional wage earners. The it's a striking tale about how Svalbard's has cording to the 2009 report that used figures presence and stability of wildlife and natural changed more dramatically in many ways dur- from the previous two years. But coal produc- elements have gone haywire in all directions. ing the past eight years than it did during pre- tion dropped by nearly 75 percent between And the community has taken many steps to- vious century. then and 2015, and the shift in jobs has been ward what is considered normal - which plen- "Mining is no longer Svalbard's heart," equally momentous. ty of locals will doubtlessly consider an af- the report declares. "There is only Mine 7 in See NUMBERS, page 4 Related coverage: • Letters to the Future: grope and change...7 Rocky outlook • Fleeing Svalbard is easy – sort of……....11 98% of Svalbard’s inland glaciers to shrink 90% or more by 2100? By MARK SABBATINI nating glaciers shrinking by at least 90 percent, Editor if climate change continues on its current pace, Svalbard will likely see “an almost com- according to a recently published study. SWISSEDUC.CH plete deglaciation” of many of its inland areas There is, however, considerable debate Inland glaciers in Nordenskiöldland will be among MAKSYM BOREIKO by the year 2100, with virtually all land-termi- See SHRINK, page 8 the first to disappear, according to a new study. You're a mean oneSee REALITY, Cookie page monstrosity4 Manic miner Sketchy scene IMAGE COURTESTY OF SNØHETTA Is this the Too much for 'Bipolar' film Is this the Arctic A twin-dock floating pier, seen here in an artist's Grinch of even a steel lives up to its in the era of illustration, is being proposed for Longyearbyen. Svalbard? stomach name Trump? Page 2 Page 3 Page 5 Page 7 https://us- mg6.mail.yahoo.c om/neo/ launch?.rand=epm v8hf4ja5bp# Page 2 December 13, 2016 Who's to blame and how A rare December sunrise in Svalbard? to express your wrath Editor Mark Sabbatini Bag lady Marion Prudhon Principal of principles Kristan Hutchison Psychiatrist Irene Gallion Accomplice Get some real dirt on icepeople! Jeff Newsom Our global headquarters available for rent during the March 20 eclipse! Sleeps three on actual Mailing address furnishings (double bed and sofa), plus a few can squeeze in on the floor. Washing machine, turbo Icepeople wi-fi and about a 5-10 minute walk to most places. Plus, you'll be helping provide our pitiful little Vei 210 -2- 13 newspaper with desperately needed funds. Contact [email protected] for details. Longyearbyen, Svalbard 9170 Norway Telephone MARK SABBATINI / ICEPEOPLE Norway: +47 41 51 46 38 Or is the moon made of brunost? Or is Mother Nature simply caving in to the fact that orange is all U.S. +1 (970) 673-4472 the rage at the moment? Obviously in this post-truth world it can't be because the moon is being seen through a much thicker layer of Earth's atmosphere when it's on the horizon, which means PRIVATE E-mail orange/red light dominates because it has longer wavelengths than other colors that get scattered. [email protected] Web site www.icepeople.net Icesheet Icepeople is published weekly (or thereabouts) Random bits of the week's weirdness: on Tuesdays (or thereabouts), with printed Plenty of folks have suggested Svalbard as copies available free on a limited basis in an ideal destination for U.S. residents wanting Longyearbyen. Additional printed copies are to flee instead of being ruled by The Don, but available locally and by mail upon request. at least one person is asking Santa to give the Charges are on an "at cost" basis. gift of a much simpler solution – albeit one that Briefly may have people here wishing for a wall. A Copyright stuff demonstrator photographed by Thomas Cully is requesting Santa bring Wiggy Trump back to Cruising: Getting out of Original contents of this publication can be the North Pole while delivering presents. reproduced for non-commercial purposes free Since Santa’s real workshop is actually in danger, but into 'death?' of charge if Icepeople is credited as the Longyearbyen’s abandoned Mine 2B, his Another cruise season is about to embark source. The original writers, photographers suggestion isn’t getting any support here full speed ahead in Svalbard, but the smiles of and other contributors retain their rights to all Mainland town claims to be top (“You can keep your garbage to yourself! Time THOMAS CULLY those greeting passengers aren't being shared published works. for USA to start handling their own problems,” On the naughty list: Or so we presume, since by a lot of industry executives these days. per-person telethon giver, a title are being scatter light more than longer wavelengths was one person’s response on Facebook). The Santa doesn't seem likely to grant his wish They took a blow last month when Britain held by Longyearbyen for years Corrections policy sign-waver might also be exposing himself to a issued a warning telling travelers cruising here bit of ridicule with a second message hanging likely things happen, including the mercury is too dangerous. That warning may be re- When we screw up you'll know about it – on from his neck reading “Cold today? Trump soaring to about nine degrees Celsius in the front page. One of the big complaints promises global warming (and dirty air).” East Longyearbyen at the end of last December…the about newspapers is they tend to bury Coast cities are indeed in a deep freeze this new news gone virtual about Svalbard is how corrections and clarifications deep inside week due to an Arctic air blast, but there’s ex- our reindeer are shrinking and the jokes where few people who read the original article actly a zero percent chance denialists making about Santa therefore needing more of them see them. If we need to fix something, an alert fun of the guy will be persuaded that yes, that’s (see page 9). But while researcher are worried box on the front page will state what story is in due to climate change…Speaking of which, a the shrinkage is a danger to the population, a error and where the full correction is printed. couple weeks ago headlines everywhere were far ominous story about Santa's little helpers declaring Svalbard stood an even or better was revealed Monday by the American Geo- chance of having an average annual temper- physical Union, which states the world’s Submitting material ature above freezing for the first time in largest reindeer herd – at the northernmost recorded history. Now, um, not so much as point of Russia on the Taimyr Peninsula – Letters, columns, photos and other material the community plunged into a deep freeze last has decreased from about one million ani- are welcome, but we can't offer pay for week. Temperatures dropped sharply starting mals in 2000 to 600,000 today, at least in part published items since nobody here is getting last Monday night and remained between minus due to climate change. “There is a substantial paid at the moment. Submissions in electronic 15 and minus 20 degrees until Thursday, ac- decline – and we are also seeing this with other form (text, Word documents, JPEGs, etc.) are cording to the Norwegian Meteorological Insti- wild reindeer declining rapidly in other parts of highly preferred, although typing and/or tute. Temperatures from Friday through Tues- the world,” Andrey Petrov, a researcher at the scanning of items will be considered on a per- day have generally been near or below minus Arctic Center at the University of Northern case basis. We reserve the right to edit 10 degrees Celsius. Of course, the past year has Iowa, told the BBC. As one article about the submissions for length, clarity, accuracy, libel seen a rather large number of staggeringly un- study notes, talk about a real war on Christmas.
Load more

Recommended publications
  • Handbok07.Pdf
    - . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? ....
    [Show full text]
  • Zur Geomorphologie Von S-Dickson Land (W-Spitzbergen) Mit Schwerpunkt Auf Der Quartären Vergletscherungsgeschichte
    Polarforschung 53 (1): 31-57, 1983 Zur Geomorphologie von S-Dickson Land (W-Spitzbergen) mit Schwerpunkt auf der quartären Vergletscherungsgeschichte Von Matthias Kuhle' Zusammenfassung: Die Halbinsel Dicksou Land befindet sich im zentralen West-Spitzhergen zwischen NNE-Ausläufern des Isfjorden. Bei einer klimatischen Firnlinie in 500 m NN sind für das südl. Dickson Land Plateaugletscher mit Auslaßzungen charakteristisch. Die Vertei­ lung speziell der Talgletscher sowie die Variationen der orographischen Firnlinie zeigen eine Abhängigkeit von der Windexposition. Bei einer Gegenüberstellung der nach LICHTENECKER (1938) und VISSER (1938) ermittelten Firnlinienwerte und den nach v. HÖFER (1879) er­ rechneten ergaben sich Differenzen von bis zu 107 m. Generelle Abhängigkeit der Differenzbeträge von den Neigungs- und Streckenrelatio­ nen der Gletscher ober- und unterhalb der realen Firnlinien konnte nachgewiesen werden. Dickson Land befand sich während des spätglazia• len Eisvorstoßes im peripheren Bereich zweier lokaler Vereisungszentren. Eine Übergeordnete Inlandvereisung W-Spitzbergens ist für diesen Zeitraum auszuschließen. Über die Ausbildung eines Kerbta~tems durch subglaziale Schmelzwassererosion wird das Maximum der spätglazialen Vereisungsphase auf die Zeit vor 17 500 B. P. ± r~~~ Jahre datiert. Eine Korrelation postglazialer Gletscherstände mit 14C~datierten marinen Terrassen (FEYLING-HANSSEN & OLSSON 1960, FEYLING­ HANSSEN 1965) war möglich. Unter Berücksichtigung isostatischer Ausgleichsbewegung und der Abweichung errechneter von realen Firn­ linien wurde für ein postglaziales Stadial um 10 400 Jahre B. P. eine klimatische Firnlinie in 265 m Ü. d. M. bei einer absoluten Depression von 246 m gegenüber der rezenten Firnlinie ermittelt. Eine Stagnation um 9650 Jahre B. P, fällt mit einer Firnlinie in 315 m Ü. d. M. (Depres­ sion: 173 m) zusammen. JÜngere Gletscherschwankungen um 1890 entsprachen einer Firnlinie in 415 m NN (Depression: 64 m).
    [Show full text]
  • Spitsbergen Nordaustlandet Polhavet Barentshavet
    5°0'0"E 10°0'0"E 15°0'0"E 20°0'0"E 25°0'0"E 30°0'0"E 35°0'0"E 81°0'0"N Polhavet Prins Oscars Land Orvin Land Vesle Tavleøya Gustav V Land Nordaustlandet Karl XII-øya Phippsøya Sjuøyane Gustav Adolf Land 80°0'0"N Martensøya Parryøya Kvitøyjøkulen Waldenøya Foynøya Nordkappsundet Kvitøya Repøyane Castrénøyane 434 433 ZorgdragerfjordenDuvefjorden Snøtoppen Nordenskiöldbukta Scoresbyøya Wrighttoppen Brennevinsfjorden 432 Laponiahalvøya Damflya Lågøya Storøya Kvitøyrenna Storøysundet Botniahalvøya Sabinebukta Orvin Land 437 Rijpfjorden Prins Lady Franklinfjorden Maudbreen Oscars Franklinsundet Worsleybreen Sverdrupisen 80°0'0"N Land Andrée Land Rijpbreen Albert I Land Norskebanken Ny-Friesland Storsteinhalvøya Olav V Land Franklinbreane James I Land Oscar II Land 401 Hinlopenrenna Haakon VII Land Gustav V Moffen Celsiusberget Murchisonfjorden Land Rijpdalen Søre Russøya Vestfonna Harald V Land Mosselhalvøya Austfonna Sorgfjorden 436 Heclahuken Gotiahalvøya Nordaustlandet Harald V Land Fuglesongen Oxfordhalvøya Breibogen Bragebreen Etonbreen IdunfjelletWahlenbergfjorden 435 Amsterdamøya Reinsdyrflya 427 Raudfjorden Balberget Hartogbukta Danskøya Vasahalvøya Smeerenburgfjorden Valhallfonna 79°0'0"N Ben Nevis 428 Woodfjorden Reuschhalvøya Palanderbukta Gustav Adolf Liefdefjorden Magdalenefjorden Åsgardfonna Albert I Glitnefonna Roosfjella Wijdefjorden Land 430 431 Hoelhalvøya Scaniahalvøya Land Bockfjorden Lomfjorden Hinlopenstretet Vibehøgdene Lomfjordhalvøya Svartstupa Monacobreen 429 Seidfjellet Svartknausflya Bråsvellbreen 402 Lomfjella Vibebukta
    [Show full text]
  • Nasjonsrelaterte Stedsnavn På Svalbard Hvilke Nasjoner Har Satt Flest Spor Etter Seg? NOR-3920
    Nasjonsrelaterte stedsnavn på Svalbard Hvilke nasjoner har satt flest spor etter seg? NOR-3920 Oddvar M. Ulvang Mastergradsoppgave i nordisk språkvitenskap Fakultet for humaniora, samfunnsvitenskap og lærerutdanning Institutt for språkvitenskap Universitetet i Tromsø Høsten 2012 Forord I mitt tidligere liv tilbragte jeg to år som radiotelegrafist (1964-66) og ett år som stasjonssjef (1975-76) ved Isfjord Radio1 på Kapp Linné. Dette er nok bakgrunnen for at jeg valgte å skrive en masteroppgave om stedsnavn på Svalbard. Seks delemner har utgjort halve mastergradsstudiet, og noen av disse førte meg tilbake til arktiske strøk. En semesteroppgave omhandlet Norske skipsnavn2, der noen av navna var av polarskuter. En annen omhandlet Språkmøte på Svalbard3, en sosiolingvistisk studie fra Longyearbyen. Den førte meg tilbake til øygruppen, om ikke fysisk så i hvert fall mentalt. Det samme har denne masteroppgaven gjort. Jeg har også vært student ved Universitetet i Tromsø tidligere. Jeg tok min cand. philol.-grad ved Institutt for historie høsten 2000 med hovedfagsoppgaven Telekommunikasjoner på Spitsbergen 1911-1935. Jeg vil takke veilederen min, professor Gulbrand Alhaug for den flotte oppfølgingen gjennom hele prosessen med denne masteroppgaven om stedsnavn på Svalbard. Han var også min foreleser og veileder da jeg tok mellomfagstillegget i nordisk språk med oppgaven Frå Amarius til Pardis. Manns- og kvinnenavn i Alstahaug og Stamnes 1850-1900.4 Jeg takker også alle andre som på en eller annen måte har hjulpet meg i denne prosessen. Dette gjelder bl.a. Norsk Polarinstitutt, som velvillig lot meg bruke deres database med stedsnavn på Svalbard, men ikke minst vil jeg takke min kjære Anne-Marie for hennes tålmodighet gjennom hele prosessen.
    [Show full text]
  • This Is Svalbard 2014. What the Figures
    14 7 9 92 This is 5 Svalbard 2014 853 14 What the figures say 8 53 © Statistics Norway, December 2014 52 When using material from this publication, Statistics Norway must be cited as the source. 5 ISBN 978-82-537-9036-7 (printed) 2715 ISBN 978-82-537-9037-4 (electronic) 215 What do the figures tell us? Questions about statistics? Through the publication of This is Svalbard, Statistics Norway aims to present a wide- Statistics Norway’s information service answers questions about statistics ranging and readily comprehensible picture of life and society on Svalbard, based on and assists you in finding your way on ssb.no. If required, we can assist available statistics. Statistics Norway has previously published four editions of Sval- you in finding the right expert and we also answer questions bard Statistics in the Official Statistics of Norway series. Statistics from many differ- regarding European statistics. ent sources have been used in order to present a full picture of life in the E-mail: [email protected] archipelago. As of 1/1 /2007, the Norwegian Statistics Act applies to Svalbard, and Telephone: +47 21 09 46 42 Statistics Norway will accordingly be publishing more statistics relating to Svalbard. These will be available on www.ssb.no/en/svalbard/ Oslo/Kongvinger, October 2014 Hans Henrik Scheel Director General This is Svalbard is a free publication and can be ordered by e-mail at: [email protected] A PDF version of the publication can be found here: http://www.ssb.no/en/svalbard Sources: Unless otherwise stated, Statistics Norway is the source.
    [Show full text]
  • Nazewnictwo Geograficzne Ś Wiata
    NAZEWNICTWO GEOGRAFICZNE NAZEWNICTWO GEOGRAFICZNE Ś WIATA Zeszyt 12 Ś WIATA 12. Europa – Cz WIATA 12. Europa Europa Część II ęść II IISBNSBN 9978-83-254-0825-178-83-254-0825-1 GŁÓWWNYNY UURZRZĄD GGEODEZJIEODEZJI I KKARTOGRAFIIARTOGRAFII OOkladka.inddkladka.indd 226767 66/10/10/10/10 110:13:170:13:17 PPMM KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 12 Europa Część II GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2010 EEuropa2.indburopa2.indb 1 66/10/10/10/10 9:49:219:49:21 PPMM KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski , Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Bogumiła Więcław, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Elżbieta Chudorlińska (Belgia, Holandia, Irlandia, Szwajcaria, Szwecja, Wielka Brytania), Andrzej Czerny (Austria, Niemcy), Jarosław Pietrow (Dania, Finlandia, Islandia, Norwegia, Szwecja), Agnieszka Pietrzak (Hiszpania, Malta, Portugalia, Włochy), Maksymilian Skotnicki (Francja), Maciej Zych (Andora, Francja, Gibraltar, Guernsey, Holandia, Jan Mayen, Jersey, Liechtenstein, Luksemburg,
    [Show full text]
  • Geomorphology Outline of the Vicinity of Petuniabukta
    Petuniabukta Geomorphology outline of the vicinity of Petuniabukta Grzegorz Rachlewicz* Institute of Paleogeography and Geoecology, Adam Mickiewicz University, Poznań, Poland The relief of coasts, valleys and mountain massifs the height of 50 m above the valley floor. In the around Petuniabukta reveals a variety of interesting upper part this level is marked by belts of lateral mo- and unique features. Landscape associations are di- raines. The marginal zone is shaped in form of an versified according to their genesis, intensity of asymmetric oval. Maximum heights of frontal geomorphic processes and age. Main stream of this moranic rampart, elevated 20–25 m above the valley branch of research arose here as the aftermath from floor, lined with outwash sediments, are located in Poznań University expeditions in the last three de- the southern wing. Mass movements on slopes of cades. ice-cored moraines are the most intensive here, fill- Main agents in shaping primary features of land- ing up englacial voids and crevasses with de- scape were associated with extensive Quaternary bris-slides and melt-water derived material. Central glaciations finished ultimately 10 ka BP. The traces part of marginal zone is occupied by a depression of at least four major advances of Spitsbergen – with small lakes, drained through a system of Barents Sea ice-sheet were detected in the not far ice-cracks, to the springs on the edge of the marginal Kapp Ekholm section. The most spectacular effects zone. The central part of terminal moraine continues of their activity are large valleys and fiords. The last, up the glacier in the form of supraglacial belt, con- widespread episode of glaciers advances during the necting the Bastion nunatak in the central part of ac- Little Ice Age (LIA – 600–100 BP) was responsible cumulation area with the edge of ice.
    [Show full text]
  • Paraglacial Modifications of Glacial Sediments Over Millennial to Decadal Time-Scales in the High Arctic (Billefjorden, Central Spitsbergen, Svalbard)
    PARAGLACIAL MODIFICATIONS OF GLACIAL SEDIMENTS OVER MILLENNIAL TO DECADAL TIME -SCALES IN THE HIGH ARCTIC ... QUAESTIONES GEOGRAPHICAE 29(3) • 2010 PARAGLACIAL MODIFICATIONS OF GLACIAL SEDIMENTS OVER MILLENNIAL TO DECADAL TIME-SCALES IN THE HIGH ARCTIC (BILLEFJORDEN, CENTRAL SPITSBERGEN, SVALBARD) gr z e g o r z rA c h l e w i c z Adam Mickiewicz University, Institute of Geoecology and Geoinformation, Poznań, Poland Manuscript received July 15, 2010 Revised version August 28, 2010 rA c h l e w i c z g., 2010. Paraglacial modifications of glacial sediments over millennial to decadal time-scales in the high Arctic (Billefjorden, central Spitsbergen, Svalbard). Quaestiones Geographicae 29(3), Poznań 2010, pp Poznań 2010 pp. 59–67, 7 Figs. ISBN 978-83-62662-04-3. ISSN 0137-477X. DOI: 10.2478/v10117-010-0023-4. Ab s t r A c t . The paper discuss the morphologic expression and sedimentological record left after the operation of glacial episodes in the area of Billefjorden, central Spitsbergen, in the period of Late Pleistocene ice-sheet deve- lopment and in the last advance of glaciers in the Little Ice Age (LIA) around the beginning of the 20th century. No evidence is found for other Holocene glacier advances. Paraglacial activity during several millennia erased the surface expression of Pleistocene glacial deposits, leaving a widespread set of reworked material that adopts features of slope, fluvial, aeolian or littoral environments. Glacial features generated during the past century, and still forming in front of retreating glaciers, undergo intense paraglacial modifications limited to the maximum depth of permafrost thaw during the summer.
    [Show full text]
  • SVALBARD-BATHYMETRY.Pdf
    0Ê 30Ê 10Ê 20Ê m SVALBARD Nansen Basin TOPOGRAPHY AND BATHYMETRY 0 Compilation made by ZBIGNIEW PERSKI Geological Visualization Laboratory at Chair of Fundamental Geology -20 Faculty of Earth Sciences UNIVERSITY OF SILESIA Bedzinska 60, 41-200 Sosnowiec POLAND -50 [email protected] -100 DATA SOURCES BATHYMETRY: Ermak Plateau Litke Trough -150 International Bathymetric Chart of the Arctic Ocean (IBCAO). The goal of this initiative is to develop a digital data base that contains all available bathymetric data north of 64 degrees -200 North, for use by mapmakers, researchers, and others whose work requires a detailed and acurate knowledge of the depth and the shape of the Arctic seabed. Initiated in 1997, this undertaking has so far engaged the volunteer efforts of investigators who are affiliated with -250 eleven institutions in eight countries: Canada, Denmark, Germany, Iceland, Norway, Russia, Quest Channel Quest B Sweden, and the USA. The activity has also been endorsed and/or supported financially by Lena Trough -300 the Intergovernmental Oceanographic Commission (IOC), the International Arctic Science 80Ê Kvitùyra Committee (IASC), the International Hydrographic Organization (IHO), the US Office of Naval 80Ê A Research (ONR), and the US National Geophysical Data Center (NGDC). Baie Nordenskiold -400 T http://www.ngdc.noaa.gov/mgg/bathymetry/arctic/arctic.html Hinlopenrenna H AWI Bathymetric Charts of the Fram Strait (AWI BCFS). Based on data from R/V Polarstern multibeam sonar surveys between 1984 and 1997 we produced a high resolution bathymetry Spitsbergen Trough* -500 Y of the central Fram Strait. The area insonified covers approx. 36,500 km2 between 78oN - 80 o o o Norske Bank N and 0 E - 7.5 E.
    [Show full text]
  • Structural Geology Around the Southern Termination of the Lomfjorden Fault Complex, Agardhdalen, East Spitsbergen
    Structural geology around the southern termination of the Lomfjorden Fault Complex, Agardhdalen, east Spitsbergen ARILD ANDRESEN, PÅL HAREMO, EIVIND SWENSSON & STEFFEN G. BERGH Andresen, A., Haremo, P., Swensson, E. & Bergh, S. G.: Structural geology around the southem termination of the Lomfjorden Fault Complex, Agardhdalen, east Spitsbergen. Norsk Geologisk Tidsskrift, Vol. 72. pp. 83-91. Oslo 1992. ISSN 0029-1 96X. Structural observations north and south of Agardhdalen, east central Spitsbergen, demonstrate that the southem termination of the Lomfjorden Fault Complex is characterized by interacting thin-skinned and basement uplifted compressional deformation (up-thrusts). Thin-skinned deformation, characterized by thickening of units due to extensive reverse faulting, is related to at (east one and possibly two decollement zones positioned in the Triassic Sassendalen Group (Lower Decollement Zone) and the Upper Jurassic/Lower Cretaceous Janusfjellet Formation (Upper Decollement Zone), respectively. The reverse faulting, often resulting in duplex structures, is particularly well developed in the Triassic Botneheia Member. Formation of a major east-facing anticline (the Eistraryggen Anticline), involving the entire Mesozoic sequence in the area and possibly most of the pre-Mesozoicfpost-Caledonian cover rocks, post-dates the thin-skinned deformation. It is argued that the Eistraryggen Anticline is developed above a steep west-dipping basement-rooted reverse fault. All structures observed around Agardhdalen, except for some possible syn- to post-depositional Triassic extensional faults, are inferred to be Tertiary in age and to have developed contemporaneously with the West Spitsbergen Foldbelt. During this event, basin inversion of the Ny Friesland Block, bordered by the Billefjorden Fault Zone and the Lomfjorden Fault Complex, took place.
    [Show full text]
  • Reisetagebuch 10.-15
    Spitzbergen Reisetagebuch 10.-15. September 2014: in und um Longyearbyen 15.-24. September 2014: Westküste Spitzbergens mit SV Antigua Die Antigua wurde 1957 in Thorne (UK) gebaut und fuhr über viele Jahre hinweg als Fischereischiff, bis sie in den frühen 1990ern in den Niederlanden von Segelschiff-Liebhabern als Barkentine von Grund auf überholt und für die Passagierfahrt fit gemacht und ausgerüstet wurde. Eine Barkentine (oder Schonerbark) zeichnet sich durch drei Masten mit bestimmten Formen der Takelung aus: 4 Rahsegel am Vormast, 2 Gaffelsegel und Staksegel. 1 Mit Fahrtleiter – Rolf Stange Guide/Fotograf – Alexander Lembke Guide/Geologe – Claus-Peter Gödecke Guide – Kristina Hochauf-Stange und auf der SV Antigua Kapitän – Joachim Schiel Erster Steuermann – Annick Zweiter Steuermann – Linda Koch – Alexander Servicechefin – Nadine Service – Jana Service – Bart Mittwoch, 10. September – Longyearbyen: Ankunft, Skjæringa Um die Mittagszeit erreichten wir nach langer Anreise Longyearbyen, wo Rolf und Peter uns am Flughafen in Empfang nahmen. Mit dem Flughafenbus ging es in den Ort, wo wir uns zunächst im Mary-Ann’s Polarriggen einquartierten, einer Unterkunft mit ganz eigenem Stil, der keine Zweifel offenließ, dass wir in Spitzbergen angekommen waren. Um 16 Uhr versammelten wir uns im Polarriggen, wo Rolf uns noch einmal offiziell begrüßte und sich zusammen mit Alex, Guide mit fotografischem Schwerpunkt, sowie Peter, Guide mit geologischer Orientierung, vorstellte. An- schließend brachen wir zu einer ersten, kleinen Runde im Ort auf. Fast direkt hinter der Unterkunft fanden wir glazial- isostatisch gehobene Strandterrassen mit tausende Jahre alten Muscheln. Ein Anstieg führte zu einem Denkmal für die im Krieg Gefallenen hinauf, von wo wir einen guten Ausblick hatten; Rolf erläuterte kurz die verschiedenen Ortsteile mit ihrer historischen Entwicklung.
    [Show full text]
  • Michael Frank William Holland
    NORSK POLARINSTITUTT SKRIFTER NR. 122 MICHAEL FRANK WILLIAM HOLLAND THE GEOLOGY OF CERTAIN PARTS OF EASTERN SPITSBERGEN NORS K POLAR I N STITUTT OSLO 1961 DET KONGELIGE DEPARTEMENT FOR INDUSTRI OG HANDVERK NO RSK POLARI NSTITUTT Observatoriegt. 1, Oslo, Norway Short account of the publications of Norsk Polarinstitutt. The two series published by Norsk Polarinstitutt,SKRIFTERand MEDDELELSER, were taken over from the former institution, Norges Svalbard- og Ishavs-unders0kel­ ser (NSIU), which was incorporated in Norsk Polarinstitutt, when this was founded in 1948. A third series, Norsk Polarinstitutt -ARBOK, will be published with one volum per year. The first volume will soon appear. SKRIFTER includes scientific papers, published in English, French or German. MEDDELELSER comprises shorter papers, often being reprints from other journals. They are generally in a more popular scale and are mostly published in Norwegian. SKRIFTER has in the past been published under various titles: Nos. 1-11. Resultater av De norske statsunderst0ttede Spitsbergen-ekspe­ disjoner. No. 12. Skrifter om Svalbard og Nordishavet. Nos. 13-81. Skrifter om Svalbard og Ishavet. 82-89. Norges Svalbard- og Ishavs-unders0kelser. Skrifter. 90- . Norsk Polarinstitutt. Skrifter. Further Norsk Polarinstitutt also publishes a special series: NORWEGIAN­ BRITISH-SWEDISH ANTARCTIC EXPEDITION, 1949-52. SCIENTIFIC RESULTS. This series will consist of 6 vols. By now 20 papers are published, and the series will probably be completed within 1963. Topographical and hydrographical surveying also plays an important part of the work done by Norsk Polarinstitutt. A list of the published maps and charts is found on the back page of SKRIFTER. A complete list of publications (including maps and charts) is enclosed in S KRI FTER No.
    [Show full text]