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The Regional Distribution of Zeolites in the Basalts of the Faroe Islands and the Significance of Zeolites As Palaeo- Temperature Indicators
The regional distribution of zeolites in the basalts of the Faroe Islands and the significance of zeolites as palaeo- temperature indicators Ole Jørgensen The first maps of the regional distribution of zeolites in the Palaeogene basalt plateau of the Faroe Islands are presented. The zeolite zones (thomsonite-chabazite, analcite, mesolite, stilbite-heulandite, laumontite) continue below sea level and reach a depth of 2200 m in the Lopra-1/1A well. Below this level, a high temperature zone occurs characterised by prehnite and pumpellyite. The stilbite-heulan- dite zone is the dominant mineral zone on the northern island, Vágar, the analcite and mesolite zones are the dominant ones on the southern islands of Sandoy and Suðuroy and the thomsonite-chabazite zone is dominant on the two northeastern islands of Viðoy and Borðoy. It is estimated that zeolitisa- tion of the basalts took place at temperatures between about 40°C and 230°C. Palaeogeothermal gradients are estimated to have been 66 ± 9°C/km in the lower basalt formation of the Lopra area of Suðuroy, the southernmost island, 63 ± 8°C/km in the middle basalt formation on the northernmost island of Vágar and 56 ± 7°C/km in the upper basalt formation on the central island of Sandoy. A linear extrapolation of the gradient from the Lopra area places the palaeosurface of the basalt plateau near to the top of the lower basalt formation. On Vágar, the palaeosurface was somewhere between 1700 m and 2020 m above the lower formation while the palaeosurface on Sandoy was between 1550 m and 1924 m above the base of the upper formation. -
The Whaling Station Við Áir
May 2007 The Whaling Station við Áir Provisional report on the conservation of the whaling station as a maritime museum MENTAMÁLARÁÐIÐ The Whaling Station við Áir Provisional report on the conservation of the whaling station as a maritime museum Mentamálaráðið The Faroese Ministry of Culture Hoyvíksvegur 72 Fo-100 Tórshavn Faroe Islands Tel +298 306500 www.mmr.fo May 2007 2 Tórshavn May 21, 2007 For the attention of the Minister of Culture, In the autumn of 2006 the Minister of Culture, Jógvan á Lakjuni, appointed a committee to consider the conservation of the Whaling Station við Áir. It was charged with submitting a report to the Minister in spring 2007. The committee concludes that the Whaling Station við Áir should be preserved as an example of the industrial society, which developed in the Faroes in the late 19th century. Whaling was of great social importance at the time and stations were set up throughout the world, seven were located in the Faroes. Today virtually all whaling has ceased, hence most of these stations have disappeared. Preserving the Whaling Station við Áir is therefore also important from a global perspective. The buildings við Áir have survived by chance, but it is thanks to visionaries in Sundalagið, the local area, and Føroya Fornminnissavn (Faroese National Museum) that much of the whaling equipment still exists. It will therefore be possible to restore the Whaling Station nearly to its original condition, not for industrial purposes, but in order to create a maritime museum and cultural activity centre við Áir. Time has clearly taken its toll on the buildings, however, and if the Station is to be conserved, immediate efforts to safeguard both the buildings and equipment are required. -
Review of the Survey's Activities in 1988
5 Review af the Survey's activities in 1988 Martin Ghisler Director During 1988 GGU started two major field projects in geological series. In addition the programme will in Greenland, one in North-East Greenland, and another clude a preliminary evaluation of the mineral potential in West Greenland in the Disko Bugt area. In addition of the area and, combined with existing aeromagnetic petroleum geological investigations in Jameson Land and planned marine-seismic surveys, will contribute to a and glacio-hydrological studies in West Greenland con better understanding of the geology and hydrocarbon tinued. A total of 84 participants were engaged in the potential of the off-shore area. field work. In 1988, 23 participants from GGU and 6 from the The scientific and technical staff at GGU in Copen Geodetic Institute were supported by helicopter from a hagen continued research on material collected in base camp north of Daneborg, 300 km north of Mesters Greenland; total staff including administrative person Vig. The main activities were concentrated on the crys nel numbers at present 108. A 10 per cent reduction of talline rocks of the Caledonides between 75° and 76°N the staff is forecast over the next four years, combined and were accompanied by more detailed studies south with an additional reduction of the budget by 14 per of 75°N on the sedimentary features of the late Pre cent. Accordingly, decreasing activity in both field work cambrian Eleonore Bay Group, the palaeontology of in Greenland and laboratory work in Copenhagen is Lower Palaeozoic strata, and the sedimentological and expected. -
North Atlantic Marine Mammal Commission
North Atlantic Marine Mammal Commission ANNUAL REPORT 1995 Layout & editing: NAMMCO Secretariat Printing: Peder Norbye Grafisk, Tromsø, Norway ISSN 1025-2045 ISBN 82-91578-00-1 © North Atlantic Marine Mammal Commission 1995 Søndre Tollbugate 9, Postal address: University of Tromsø, 9037 Tromsø Tel.: +47 77 64 59 08, Fax: +47 77 64 59 05, Email: [email protected] Preface The North Atlantic Marine Mammal Commission was established in 1992 by an Agreement signed in Nuuk, Greenland on the 9th of April between the Faroe Islands, Greenland, Iceland and Norway. The objective of the Commission, as stated in the Agreement, is to “... contribute through regional consultation and cooperation, to the conservation, rational management and study of marine mammals in the North Atlantic.” The Council, which is the decision-making body of the Commission, held its inaugural meeting in Tórshavn, Faroe Islands, 10-11 September 1992 (NAMMCO/1), and has convened four times since: in Tromsø, Norway 19-20 January 1993 (NAMMCO/2); Reykjavik, Iceland, 1-2 July 1993 (NAMMCO/3); Tromsø, Norway 24-25 February 1994 (NAMMCO/4); and most recently in Nuuk, Greenland, 21-23 February 1995 (NAMMCO/5). The present volume contains proceedings from NAMMCO/5 - the fifth meeting of the Council, which was held at the Hotel Hans Egede in Nuuk, Greenland 21-23 February 1995 (Section 1), as well as the reports of the 1995 meetings of the Management Committee (Section 2) and the Scientific Committee (Section 3), which presented their conclusions to the Council at its fifth meeting. Included as an annex to the Management Committee report is the report of the second meeting of the Working Group on Inspection and Observation. -
Hiking, Guided Walks, Visit Tórshavn FO-645 Æðuvík, Tel
FREE COPY TOURIST GUIDE 2018 www.visitfaroeislands.com #faroeislands Download the free app FAROE ISLANDS TOURIST GUIDE propellos.dk EXPERIENCE UP CLOSE We make it easy: Let 62°N lead the way to make the best of your stay on the Faroe Islands - we take care of practical arrangements too. We assure an enjoyable stay. Let us fly you to the Faroe Islands - the world’s most desireable island community*) » Flight Photo: Joshua Cowan - @joshzoo Photo: Daniel Casson - @dpc_photography Photo: Joshua Cowan - @joshzoo » Hotel » Car rental REYKJAVÍK » Self-catering FAROE ISLANDS BERGEN We fly up to three times daily throughout the year » Excursions directly from Copenhagen, and several weekly AALBORG COPENHAGEN EDINBURGH BILLUND » Package tours flights from Billund, Bergen, Reykjavik and » Guided tours Edinburgh - directly to the Faroe Islands. In the summer also from Aalborg, Barcelona, » Activity tours Book Mallorca, Lisbon and Crete - directly to the » Group tours your trip: Faroe Islands. BARCELONA Read more and book your trip on www.atlantic.fo MALLORCA 62n.fo LISBON CRETE *) Chosen by National Geographic Traveller. GRAN CANARIA Atlantic Airways Vága Floghavn 380 Sørvágur Faroe Islands Tel +298 34 10 00 PR02613-62N-A5+3mmBleed-EN-01.indd 1 31/05/2017 11.40 Explanation of symbols: Alcohol Store Airport Welcome to the Faroe Islands ................................................................................. 6 Aquarium THE ADVENTURE ATM What to do .................................................................................................................. -
Descriptive Text to the 1995 Geological Map of Greenland, 1:2 500 000
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 18 2009 Greenland from Archaean to Quaternary Descriptive text to the 1995 Geological map of Greenland, 1:2 500 000. 2nd edition Niels Henriksen, A.K. Higgins, Feiko Kalsbeek and T. Christopher R. Pulvertaft GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 18 Keywords Archaean, Caledonides, Cenozoic, economic geology, geological map, Greenland, ice sheet, Mesozoic, offshore, orogenic belts, Palaeozoic, petroleum, Phanerozoic, Proterozoic, sedimentary basins. Cover illustration The cover design depicts mountains of the East Greenland Caledonian fold belt. The view, west of Mestersvig (located on map, page 4), is north over Bersærkerbræ and the northern part of the Stauning Alper to Kong Oscar Fjord with Traill Ø in the right backgro- und. The mountains up to 1800 m high are of the Neoproterozoic Eleonore Bay Supergroup. To the right: first author Niels Henriksen, for many years head of geological mapping at GGU/GEUS, and participant in field work in Greenland for more than 45 years. Frontispiece: facing page Major Caledonian syncline involving reactivated Archaean basement gneisses containing amphibolite bands. Overlying rusty coloured Mesoproterozoic metasediments (Krummedal supracrustal sequence) just visible in tight core of the fold. The intensity of deformation in the syncline clearly increases towards the core, where the basement gneisses become more strongly foliated. Some of the amphibolite bands were derived from cross-cutting basic intrusions, which are still discernable in the less severely deformed parts of the Archaean basement (Fig. 17, p. 31). The height of the section is c. 2000 m. -
Man-Dependence of House Sparrows (Passer Domesticus) in the Faroe Islands: Habitat Patch Characteristics As Determinants of Presence and Numbers
Man-dependence of House Sparrows (Passer domesticus) in the Faroe Islands: habitat patch characteristics as determinants of presence and numbers SVEN-AXEL BENGTSON, KIRSTIN ELIASEN, LAURA MARY JACOBSEN, EYDFINN MAGNUSSEN Abstract The House Sparrow (Passer domesticus) began to colonize the Faroe Islands in the mid-1940s and occurs in most built-up areas. Breeding is confined to the discrete human habitations (settle- ments) that form a pattern of patches (”habitat-islands”). In 2002 all settlements were surveyed and the number of pairs of sparrows (total number ca. 2,700 pairs) and amount of vegetation (”green space”) were estimated. The settlements ranged in size from 0.01 km2 (a single farmstead) to 8.72 km2 (the capital) and 68% of them (n=118) were occupied by sparrows. Patch occupancy was positively correlated with both area and amount of vegetation (p < 0.001) but not quite with the degree of isolation (p = 0.15). The latter was crudely scored as a function of distance to nearest Man-dependence of House Sparrows in the Faroe Islands UÊÓÓÇ Dorete - her book, Annales Societatis Scientiarum Færoensis, Suppl. 52, pp. 227-243. Ed. by S. A. Bengtson, P. Buckland, P. H. Enckell and A. M. Fosaa. Faroe University Press. settlement with > 10 pairs (a possible source area) and topography (mainly mountains and open sea). The patch variables area, human population, number of houses and houses were strongly intercor- related. Abundance (number of pairs) of sparrows was positively correlated with the number of houses (r = 0.84, p < 0.001). In all but one of the settlements with < 10 houses sparrows were absent, and also in many of those with 10-60 houses where the scatter swas wide (no significant correlation p = 0.25). -
Geological Survey of Denmark and Greenland Bulletin 19, 2009, 1–26
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 19 2009 Lithostratigraphy of the Cretaceous–Paleocene Nuussuaq Group, Nuussuaq Basin, West Greenland Gregers Dam, Gunver Krarup Pedersen, Martin Sønderholm, Helle H. Midtgaard, Lotte Melchior Larsen, Henrik Nøhr-Hansen and Asger Ken Pedersen GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 19 Keywords Lithostratigraphy, Nuussuaq Group, Cretaceous, Paleocene, West Greenland, Nuussuaq Basin. Cover illustration Sedimentary succession of the Nuussuaq Group at Paatuut on the south coast of Nuussuaq, one of the classical localities for sedi- mentological and palaeontological studies. The photograph shows deep incision of the Paleocene Quikavsak Formation into the Upper Cretaceous Atane Formation. The conspicuous red coloration is due to self-combustion of carbonaceous sediments. The upper part of the succession comprises volcanic rocks of the West Greenland Basalt Group. The height of the mountains is c. 2000 m. Photo: Martin Sønderholm. Frontispiece: facing page View down into the narrow Paatuutkløften gorge on the southern coast of Nuussuaq, where coarse-grained, pale sandstones of the Paleocene Quikavsak Formation fill a major incised valley cut into interbedded mudstones and sandstones of the Cretaceous Atane Formation. Sea-fog often invades the coastal valleys but typically dissipates during the day. Photo: Finn Dalhoff. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Geological Institute, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Jon R. Ineson Editorial secretaries: Jane Holst and Esben W. -
Review of Fossil Floras and Nonmarine Deposits of West Greenland
B. ESKE KOCH Dept. Geology, Aarhus University, Aarhus, Denmar^ Review of Fossil Floras and Nonmarine Deposits of West Greenland Abstract: The sedimentary area of central West Pautut flora sensu stricto. Furthermore, the Atane Greenland comprises, besides marine sediments, a formation (ordinarily accepted as Cenomanian, al- number of plant-bearing, nonmarine, and transi- though this has never been convincingly proven) tional-facies formations. Mainly because of insuf- and the Pautut formation (Senonian) may be ex- ficient field studies and conclusions based on scanty posures of a continuous Senonian sequence along geological information, the generally accepted the south coast of the Nugssuaq Peninsula. The ideas about these formations and their floras have Kmgigtoq constituent of the Pautut flora is a been affected by severe misunderstandings. How- mixture of Cretaceous and Tertiary fossils, which ever, recent geological investigations under the were collected from a landslide. auspices of The Geological Survey of Greenland Recent paleontologic and stratigraphic studies have provided a sounder basis for the stratigraphic are attempts to solve the remaining problems. In interpretations and exposed a number of mistakes, Tertiary stratigraphy, such positive results as de- e.g.: in the Lower Cretaceous Kome formation the fining the age of the classic Upper Atanikerdluk often-cited "oldest" angiosperms are dubious, and floras as early Paleocene have been achieved. Study those of the Upernivik Nses formation may be of the Cretaceous formations has been advanced, younger than assumed by Seward; the Atane flora, especially through the investigation of spores and ordinarily cited as Cenomanian, consists of fossils pollen. These studies have been facilitated by dis- from localities the beds of which are not exactly of coveries of marine zones and new faunal localities. -
Matthew Carl Lamanna
Curriculum Vitae Matthew Carl Lamanna Assistant Curator Section of Vertebrate Paleontology Carnegie Museum of Natural History 4400 Forbes Avenue Pittsburgh, Pennsylvania 15213-4080 (412) 578-2696 (Office) (412) 622-8837 (Fax) Email: [email protected] Internet: http://www.carnegiemnh.org/vp/lamanna.html Education 2004 Ph.D., University of Pennsylvania, Department of Earth and Environmental Science. 1999 M.Sc., University of Pennsylvania, Department of Earth and Environmental Science. 1997 B.Sc., Hobart College, Departments of Geoscience and Biology, cum laude. Research Interests Mesozoic (principally Cretaceous) vertebrate faunas, paleoecology, and paleobiogeography; non-avian and avian dinosaur anatomy, systematics, and phylogeny. Academic and Professional Positions 2013–present Research Associate, Cleveland Museum of Natural History. 2012–present Principal Investigator and Project Director, Antarctic Peninsula Paleontology Project (AP3). 2005–present Adjunct Assistant Professor, Department of Geology and Planetary Science, University of Pittsburgh. 2004–present Assistant Curator, Section of Vertebrate Paleontology, Carnegie Museum of Natural History. 1999–present Paleontologist, Bahariya Dinosaur Project. 1997–present Research Associate, Academy of Natural Sciences of Drexel University (Philadelphia). 1997–1998 Exhibit Design Consultant, Dinosaur Hall, Academy of Natural Sciences (Philadelphia). 1995 Research Assistant, University of New Orleans Lance Dinosaur Project. Field Experience 2016 Unnamed formation, Robertson Island, -
GEUS Bulletin No 9 • 2006
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 9 · 2006 Scientific results from the deepened Lopra-1 borehole, Faroe Islands Edited by James A. Chalmers and Regin Waagstein GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF THE ENVIRONMENT 1 GEUS Bulletin no 9 - 7 juli.pmd 1 07-07-2006, 14:19 Geological Survey of Denmark and Greenland Bulletin 9 Keywords Faroe Islands, Palaeogene basalts, Lopra-1/1A borehole. Cover Maersk Rig 81 on the location of the Lopra-1/1A wells at Suðuroy, Faroe Islands, in August 1996 shortly after the start of drilling. Photo: Regin Waagstein. Frontispiece: facing page Maersk Rig 81 on the location of the Lopra-1/1A wells at Suðuroy, Faroe Islands, in August 1996 shortly after the start of drilling. Photo: Regin Waagstein. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Geological Institute, University of Aarhus; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Geological Institute, University of Copenhagen Scientific editors of this volume: James A. Chalmers and Regin Waagstein Editorial secretaries: Esben W. Glendal and Birgit Eriksen Referees: T. Bidstrup (Denmark), D. Bird (USA), R. Burwood (UK), B. Christenson (New Zealand), A. Förster (Germany), D.S Gold- berg (USA), P. Harvey (UK), S. Jakobsson (Iceland), R. Løvlie (Norway), H. Micheelsen (Norway), J.D.A. Piper (UK), M.A. Rooney (Argentina), D. Tarling (UK), G. van Graas (Norway), R. White (UK), M. Worthington (UK) and an anonymous referee (Denmark) Illustrators: Eva Melskens and Kristian Rasmussen Digital photographic work: Benny M. Schark Graphic production: Knud Gr@phic Consult, Odense, Denmark Printers: Schultz Grafisk, Albertslund, Denmark Receipt/acceptance dates of manuscripts: see end of individual articles Printed: 7 July 2006 ISSN 1604-8156 ISBN 87-7871-179-7 Geological Survey of Denmark and Greenland Bulletin The series Geological Survey of Denmark and Greenland Bulletin replaces Geology of Denmark Survey Bulletin and Geology of Greenland Survey Bulletin. -
Geology and Assessment of Undiscovered Oil and Gas Resources of the West Greenland-East Canada Province, 2008
Geology and Assessment of Undiscovered Oil and Gas Resources of the West Greenland-East Canada Province, 2008 Chapter J of The 2008 Circum-Arctic Resource Appraisal Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey Cover. Fishing boat in the Ilulissat Icefjord, Disko Bay, West Greenland, which is about 250 kilometers north of the Arctic Circle. The fjord is notable for its prolific iceberg production; the fast-moving tidal glacier Sermeq Kujalleq (also called Jakobshavn Isbrae) is a major outlet of the Greenland ice sheet. Photo by Flemming G. Christiansen, Geological Survey of Denmark and Greenland. Geology and Assessment of Undiscovered Oil and Gas Resources of the West Greenland- East Canada Province, 2008 By Christopher J. Schenk Chapter J of The 2008 Circum-Arctic Resource Appraisal Edited by T.E. Moore and D.L. Gautier Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text.