Early History of Petroleum Exploration Offshore Norway and Its Impact on Geoscience Teaching and Research
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Jens Esmark's Mountain Glacier Traverse 1823 À the Key to His
bs_bs_banner Jens Esmark’s mountain glacier traverse 1823 À the key to his discovery of Ice Ages GEIR HESTMARK Hestmark, G. 2018 (January): Jens Esmark’s mountain glacier traverse 1823 À the key to his discovery of Ice Ages. Boreas, Vol. 47, pp. 1–10. https://doi.org/10.1111/bor.12260. ISSN 0300-9483. The discovery of Ice Ages is one of the most revolutionary advances made in the Earth sciences. In 1824 Danish- Norwegian geoscientist Jens Esmark published a paper stating that there was indisputable evidence that Norway and other parts of Europe had previously been covered by enormous glaciers carving out valleys and fjords, in a cold climate caused by changes in the eccentricity of Earth’s orbit. Esmark and his travel companion Otto Tank arrived at this insight byanalogous reasoning: enigmatic landscape features theyobserved close to sea level alongtheNorwegian coast strongly resembled features they observed in the front of a retreating glacier during a mountain traverse in the summer of 1823. Which glacier they observed up close has however remained a mystery, and thus an essential piece of information in the story of this discovery has been missing. Based on previously unknown archive sources, supplemented by field study, I here identify the key locality as the glacier Rauddalsbreen. This is the northernmost outlet glacier from Jostedalsbreen, the largest glacier in mainland Europe. Here the foreland exposed byglacier retreat since the Little Ice Age maximum around AD 1750 contains a rich collection of glacial deposits and erosional forms. The point of enlightenment is more precisely identified to be a specific moraine and its distal sandur at 61°53026″N, 7°26043″E. -
Jens Esmark – Meteorologist
1 2 Jens Esmark’s Christiania (Oslo) meteorological observations 3 1816-1838: The first long term continuous temperature record 4 from the Norwegian capital homogenized and analysed 5 6 7 Geir Hestmark1 and Øyvind Nordli2 8 9 1 Centre for Ecological and Evolutionary Synthesis, CEES, Department of 10 Biosciences, Box 1066 Blindern, University of Oslo, N-0316 Oslo, Norway 11 2 Norwegian Meteorological Institute (MET Norway), 12 Research and Development Department, Division for Model and Climate Analysis, 13 P.O. Box 43 Blindern, N-0313 Oslo, Norway 14 15 Correspondence to: Geir Hestmark ([email protected]) 16 17 Abstract 18 In 2010 we rediscovered the complete set of meteorological observation protocols 19 made by professor Jens Esmark (1762-1839) during his years of residence in the 20 Norwegian capital of Oslo (then Christiania). From 1 January 1816 to 25 January 21 1839 Esmark at his house in Øvre Voldgate in the morning, early afternoon and 22 late evening recorded air temperature with state of the art thermometers. He also 23 noted air pressure, cloud cover, precipitation and wind directions, and 24 experimented with rain gauges and hygrometers. From 1818 to the end of 1838 he 25 twice a month provided weather tables to the official newspaper Den norske 26 Rigstidende, and thus acquired a semi-official status as the first Norwegian state 27 meteorologist. This paper evaluates the quality of Esmark’s temperature 28 observations, presents new metadata, new homogenization and analysis of monthly 29 means. Three significant shifts in the measurement series were detected, and 30 suitable corrections are proposed. -
Glacial Geomorphology☆ John Menzies, Brock University, St
Glacial Geomorphology☆ John Menzies, Brock University, St. Catharines, ON, Canada © 2018 Elsevier Inc. All rights reserved. This is an update of H. French and J. Harbor, 8.1 The Development and History of Glacial and Periglacial Geomorphology, In Treatise on Geomorphology, edited by John F. Shroder, Academic Press, San Diego, 2013. Introduction 1 Glacial Landscapes 3 Advances and Paradigm Shifts 3 Glacial Erosion—Processes 7 Glacial Transport—Processes 10 Glacial Deposition—Processes 10 “Linkages” Within Glacial Geomorphology 10 Future Prospects 11 References 11 Further Reading 16 Introduction The scientific study of glacial processes and landforms formed in front of, beneath and along the margins of valley glaciers, ice sheets and other ice masses on the Earth’s surface, both on land and in ocean basins, constitutes glacial geomorphology. The processes include understanding how ice masses move, erode, transport and deposit sediment. The landforms, developed and shaped by glaciation, supply topographic, morphologic and sedimentologic knowledge regarding these glacial processes. Likewise, glacial geomorphology studies all aspects of the mapped and interpreted effects of glaciation both modern and past on the Earth’s landscapes. The influence of glaciations is only too visible in those landscapes of the world only recently glaciated in the recent past and during the Quaternary. The impact on people living and working in those once glaciated environments is enormous in terms, for example, of groundwater resources, building materials and agriculture. The cities of Glasgow and Boston, their distinctive street patterns and numerable small hills (drumlins) attest to the effect of Quaternary glaciations on urban development and planning. It is problematic to precisely determine when the concept of glaciation first developed. -
Historical Mineral Collections in the Silver Mining Town of Kongsberg, Norway
Historical mineral collections in the silver mining town of Kongsberg, Norway F.S. Nordrum & B.I. Berg F.S. Nordrum & Berg, B.I. Historical mineral collections in the silver mining town of Kongsberg, Nor• way. In: Winkler Prins, CF. & Donovan, S.K. (eds.), VII International Symposium 'Cultural Heritage in Geosciences, Mining and Metallurgy: Libraries - Archives - Museums': "Museums and their collections", Leiden (The Netherlands), 19-23 May 2003. Scripta Geológica Special Issue, 4: 229-235, 4 figs.; Leiden, August 2004. F.S. Nordrum & B.I. Berg, Norwegian Mining Museum, P.O. Box 18, NO-3602 Kongsberg, Norway ([email protected]; [email protected]). Key words — old geological collections, silver mines, mining officers, mining academy, Kongsberg. The discovery of native silver deposits at Kongsberg, Norway, in 1623 created interest for silver speci• mens and mineral collecting, also among mining officers. Large collections were donated by J. Hiort, M.T. Brünnich and J. Esmark to the Mining Academy at Kongsberg. The Academy's collections were in 1814 transferred to the University of Oslo. From 1841 The Kongsberg Silver Mines built up their own collections. Contents Introduction 229 Early mineral collections at Kongsberg 230 The Kongsberg Silver Mines' mineral collection (1841-1958) 233 Acknowledgements 234 References 234 Introduction The Kongsberg Silver Mines were established in 1623 and the Kongsberg mining town was founded in 1624 by the Danish-Norwegian king Christian IV. The ore, dominated by native silver, was a sensation at the time. Specimens of native silver became popular collecting items. Most fine specimens, however, went to members of the royalty in Copenhagen. -
Hans Morten Thrane Esmark (Figure 11)
Thorium-Lovoya, Langesundfj ord, Norway James L. Marshall Beta Eta '71 and Virginia R. Marshall Department of Chemistry, University of North Texas, Denton TX 76203-5070; jimm@unt. edu; Computer Technology, Denton ISD, Denton TX 76201 About 100 kilometers to the southwest of 0 Oslo (Figure 1) lies the Langesund, one of the beautiful fjords that encircle the coast Oslo of Norway (Figure 2). This area was home to Henrik Ibsen, the well-known nineteenth cen- tury playwright who lived in Skien at the north- ernmost reaches of this fjord. Hundreds of islands dot this inlet-measuring in size from a square kilometer to a mere boulder poking out of the water-rendering a boat necessary for a local traveler (Figure 3). One fateful day in early 1829, the pastor of Figure 1. The southeast part of Norway (identified by the tessara, expanded in the next figure) played an Brevik was rowing around the rocky islands of important part in the discovery of some of the more unusual elements. the Langesundfjord, hunting for ducks.' As he Oslo drifted around Loveya Island (see Figure 4), he thing they had seen before, and noticed a black mineral in the pegmatite boul- the two Esmarks realized this Kongsberg ders. Curious, he eased his boat by the craggy might be something new. Esmark 10 ) km rishus shore and scrambled ashore. He chipped off senior sent a sample to Jbns (He) some of the crystals and took them back to his Jakob Berzelius, the famous parish. The glimmering mineral that the pastor chemist in Stockholm, for a more Brevik collected would later be known as thorite, complete analysis, who later that Knaben (Th, La ThSiO 4 (Figure 5), and thereby begins the story year discovered thorium in the Mine of the discovery of a new element. -
Årsmelding 1976
UNIVERSITETET I BERGEN ÅRSMELDING 1976 FRA DET AKADEMISKE KOLLEGIUM UTGITT AV UNIVERSITETSDIREKTØREN REDAKSJON AVDELING FOR OPPLYSNINGSVIRKSOMHET Qmslagsbilde: De prekliniske institutter, Arstadvollen. Bygningen ble tatt i bruk høstsemesterct 1966, og den er tegnet av arkitektenc MNAL Gunnar Fougner og Einar MyklcVust. Anatomisk, Biokjemisk og Fysiologisk institutt har sine lokaler her. ISBN-82-7127U30-3 Innhold Det akademiske kollegium 5 Bergens Museumsråd 5 Universitetets personale 5 Minneord 5 Avskjed i nåde 6 Utncvninger av professorcr og dosentcr 7 Administrasjonen 14 Oversikt over personalet 17 Forholdstall 19 Studerende ved Universitetet i Bergen 20 Nye studenter 1976 20 Registrerte studentcr 22 Fagoversikt 22 Eksamenet' og grader 28 Doktorgrader 28 Licentiatgrader 29 Magistergrader 30 Hislorisk-filosofisk embetseksamen 32 Matematisk-naturvitenskapelig embetseksamen 40 Samfunnsvitenskapelig embetseksamen 47 Psykologisk embetseksamen 49 Juridisk embetseksamen 52 Medisinsk embetseksamen 53 Odontologisk embetseksamen 54 Bygninger 55 Publikasjoncr 55 Årsfesten 55 De vitenskapelige samlingene 56 Representasjon 57 Rektors representasjon 57 Representasjon i styrer og utvalg 57 Legaler og fond dl! Legaler og fond som luner lii eller blir Myri av L'niviiMt ni i Bergen i>2 Utdeling av legaler og fond dl Æresbevisninger ... 6't Prisoppgåver d*i Gåver ti') Regnskap 7(1 Det historisk-tilosofiske fakultet 75 De enkelte instituttet- 75 Det materuatisk-naturvitcnskapeligc fakultet 113 De enkelte institutter 113 Det medisinske fakultet 198 De enkelte institutter 198 Det odontologiske fakultet 273 De enkelte institutter 273 Det samfunnsvitenskapelige fakultet 284 De enkelte institutter 284 Avdeling for elektronisk databehandling 312 Avdeling for helsekontroll 318 Det pedagogiske seminar 319 Opplysningsarbeid 323 Sommerkurs 329 Universitetsbiblioteket 333 DET AKADEMISKE KOLLEGIUM UNIVERSITETETS PERSONALE Professor Arnc-Johan Henrichsen, rektor. -
Ice Age Megafauna and Time Notes Contents
Ice Age megafauna and time notes Contents 1 Ice age 1 1.1 Origin of ice age theory ........................................ 1 1.2 Evidence for ice ages ......................................... 2 1.3 Major ice ages ............................................ 3 1.4 Glacials and interglacials ....................................... 4 1.5 Positive and negative feedback in glacial periods ........................... 5 1.5.1 Positive feedback processes ................................. 5 1.5.2 Negative feedback processes ................................. 5 1.6 Causes of ice ages ........................................... 5 1.6.1 Changes in Earth’s atmosphere ................................ 6 1.6.2 Position of the continents ................................... 6 1.6.3 Fluctuations in ocean currents ................................ 7 1.6.4 Uplift of the Tibetan plateau and surrounding mountain areas above the snowline ...... 7 1.6.5 Variations in Earth’s orbit (Milankovitch cycles) ....................... 7 1.6.6 Variations in the Sun’s energy output ............................. 8 1.6.7 Volcanism .......................................... 8 1.7 Recent glacial and interglacial phases ................................. 8 1.7.1 Glacial stages in North America ............................... 8 1.7.2 Last Glacial Period in the semiarid Andes around Aconcagua and Tupungato ........ 9 1.8 Effects of glaciation .......................................... 9 1.9 See also ................................................ 10 1.10 References ............................................. -
IAEA TECDOC SERIES World Thorium Occurrences, Deposits and Resources
IAEA-TECDOC-1877 IAEA-TECDOC-1877 IAEA TECDOC SERIES World Thorium Occurrences, Deposits and Resources Deposits and Resources Thorium Occurrences, World IAEA-TECDOC-1877 World Thorium Occurrences, Deposits and Resources International Atomic Energy Agency Vienna ISBN 978–92–0–103719–0 ISSN 1011–4289 @ WORLD THORIUM OCCURRENCES, DEPOSITS AND RESOURCES The following States are Members of the International Atomic Energy Agency: AFGHANISTAN GERMANY PAKISTAN ALBANIA GHANA PALAU ALGERIA GREECE PANAMA ANGOLA GRENADA PAPUA NEW GUINEA ANTIGUA AND BARBUDA GUATEMALA PARAGUAY ARGENTINA GUYANA PERU ARMENIA HAITI PHILIPPINES AUSTRALIA HOLY SEE POLAND AUSTRIA HONDURAS PORTUGAL AZERBAIJAN HUNGARY QATAR BAHAMAS ICELAND REPUBLIC OF MOLDOVA BAHRAIN INDIA BANGLADESH INDONESIA ROMANIA BARBADOS IRAN, ISLAMIC REPUBLIC OF RUSSIAN FEDERATION BELARUS IRAQ RWANDA BELGIUM IRELAND SAINT LUCIA BELIZE ISRAEL SAINT VINCENT AND BENIN ITALY THE GRENADINES BOLIVIA, PLURINATIONAL JAMAICA SAN MARINO STATE OF JAPAN SAUDI ARABIA BOSNIA AND HERZEGOVINA JORDAN SENEGAL BOTSWANA KAZAKHSTAN SERBIA BRAZIL KENYA SEYCHELLES BRUNEI DARUSSALAM KOREA, REPUBLIC OF SIERRA LEONE BULGARIA KUWAIT SINGAPORE BURKINA FASO KYRGYZSTAN SLOVAKIA BURUNDI LAO PEOPLE’S DEMOCRATIC SLOVENIA CAMBODIA REPUBLIC SOUTH AFRICA CAMEROON LATVIA SPAIN CANADA LEBANON SRI LANKA CENTRAL AFRICAN LESOTHO SUDAN REPUBLIC LIBERIA CHAD LIBYA SWEDEN CHILE LIECHTENSTEIN SWITZERLAND CHINA LITHUANIA SYRIAN ARAB REPUBLIC COLOMBIA LUXEMBOURG TAJIKISTAN CONGO MADAGASCAR THAILAND COSTA RICA MALAWI TOGO CÔTE D’IVOIRE MALAYSIA TRINIDAD -
Centre for Ecological and Evolutionary Synthesis University of Oslo
Centre for Ecological and Evolutionary Synthesis University of Oslo The Editor, Climate of the Past Date: 17 October 2016 Dear Editor, Thank you for your comment 14 October on our paper on Jens Esmark’s Christiania-series. Re your wish to include Hertzberg’s data from Ullensvang by the Hardangerfjord: It would really have been a great advantage if we had a reliable series overlapping Esmark’s series in the opposite direction to Stockholm. The problem with Hertzberg’s observations is that the original data are lost. It is however known that Hertzberg observed various times during the day, from three to six times. For each day he calculated a “daily mean value”. However, these values are not real daily means. It seems that he considered day temperature more important than night temperature, and it is not known how he performed his calculations. With varying observation time during the day it is very likely that Hertzberg’s “daily means” are inhomogenous. Also, Hertzberg was often on voyages so that there are gaps in his series. These were filled by Birkeland by the help of other stations, it is not clear which. It is understandable that MET Norway has given the digitalization of Hertzberg’s “daily means” low priority so they are not digitized. It would be easy for us to plot the annual means calculated by Birkeland in Fig. 12, but we are reluctant to do so because wee are afraid that it could mislead readers rather than add value to our article. Birkeland was a pioneer for his time, so all honor to him. -
Thorium-L0v0ya, Langesundfjord, Norway
,, 11,, , I ii ' "' ~-------- - -- Thorium-L0V0ya, Langesundfjord, Norway James L. Marshall Beta Eta '71 and Virginia R. Marshall Department of Chemistry, University of North Texas, Denton TX 76203-5070; [email protected]; Computer Technology, Denton ISO, Denton TX 76201 bout 100 kilometers to the southwest of "~ Oslo (Figure 1) lies the Langesund, one of ~ Athe beautiful fjords that encircle the coast Oslo of Norway (Figure 2). This area was home to Henrik Ibsen, the well-known nineteenth cen tury playwright who lived in Skien at the north ernmost reaches of this fjord. Hundreds of islands dot this inlet-measuring in size from a square kilometer to a mere boulder poking out of the water-rendering a boat necessary for a local traveler (Figure 3). One fateful day in early 1829, the pastor of Figure 1. The southeast part of Nmway (identified by the tcssam, c;i.pandcd in the next figure) played an Brevik was rowing around the rocky islands of important part in the discovery of some of the more wwsua/ c/emmts. the Langesundfjord, hunting for ducks.' As he drifted around L0v0)'a Island (see Figure 4), he thing they had seen before, and noticed a black mineral in the pegmatite boul the two Esmarks realized this ders. Curious, he eased his boat by the craggy might be something new. Esmark I 100 km I shore and scrambled ashore. He chipped off senior sent a sample to Jons some of the crystals and took them back to his Jakob Berzelius, the famous parish. The glimmering mineral that the pastor chemist in Stockholm, for a more collected would later be known as thorite, complete analysis, who later that Knaben ThSi04 (Figure 5), and thereby begins the story year discovered thorium in the Mine of the discovery of a new element. -
Jens Esmark, Datolite..And Thulite
To discover, yes, but to publish...? Jens Esmark, datolite..and thulite Geir Hestmark Introduction In August 1806 German geologist Johann Friedrich Ludwig Hausmann (1782-1859), arrived at Kongsberg on a trip through Scandinavia, and here met Jens Esmark (1762-1839) who held a position as Assessor in the central mining administration - the Oberbergamt - and also served as Inspector and lecturer in mineralogy, geology (geognosy) and physics at the Berg-Seminarium, the mining academy established in connection with the Silver Mines at Kongsberg in 1757. In his Scandinavian travelogue Hausmann described Esmark as an excellent geognost, and outstanding in many other skills. "Esmark possesses a very instructive collection for the external characters of the minerals for the needs of his lectures, and many splendid Nordic minerals, among which many new are probably present, of which the closer examination and publication every mineralogist so more must be desirous, as Esmark's sharp eye has already demonstrated itself through several interesting discoveries, among others that of the datolite." "Esmark besitzt eine sehr instruktive Sammlung filr die iiusseren Kennzeichen der Fossifien zum Behuf seiner Vorlesungen und viele treffliche, nordischen Mineralien, unter welche manche neue sich befinden dilrfen, auf deren niihere Untersuchung und Bekanntmachung jeder Mineralog um so begieriger seyn muss, da sich Esmark's Scharfblick schon durch mehrere interessante Entdeckungen, wie u. A. durch die des Dato/iths bewiihrt hat." (Hausmann 1811-18, Vol. 2: 38). Esmark's discovery of datolite poses a number interesting questions regarding the discovery, credit for and publication of new minerals. Collection The collection of datolite happened on an inspection trip Esmark made from mid-June to mid-July 1804 in the company of his colleague at the Oberbergamt, Assessor Ole Henckel (1748-1824) to the Egeland Iron Work close to Ris0r town on the south Norwegian coast (Doc 1). -
ÅRBOK for UNIVERSITETSMUSEET I BERGEN 2 011 ÅRBOK for Universitetsmuseet I Bergen 2011
ÅRBOK FOR UNIVERSITETSMUSEET i BERGEN 2 011 ÅRBOK FOR Universitetsmuseet i Bergen 2011 UNIVERSITETET I BERGEN REDAKTØR INNHOLD Jo Høyer Forord – Universitetsmuseet i Bergen 4 [email protected] FRIDTJOF NANSEN OG BERGENS MUSEUM Fridtjof Nansen som konservator ved Bergens Museum 6 FORFATTERE Karen Helle Karen Blaauw Helle Per Harald Salvesen «Nansens makkverk» 17 Professor emeritus, Institutt for biomedisin, UiB Førsteamanuensis i botanikk, Arboretet og Botanisk hage, [email protected] Universitetsmuseet i Bergen Endre Willassen [email protected] Endre Willassen Fridtjof Nansen and the Nobel Prize in Physiology or Medicine of 1906 25 Professor i zoologi, De naturhistoriske samlinger, Per Åsen Ortwin Bock Universitetsmuseet i Bergen Førstekonservator og leder av Botanisk avdeling, Agder [email protected] Naturmuseum og Botaniske Hage Fridtjof Nansen og Nobelprisen i medisin i 1906 (norsk sammendrag) 33 [email protected] Ortwin Bock Ortwin Bock Dr. med Ortwin Bock, Ph.D (Ox), pensjonert lege, Cape Town, Gordon Turner-Walker MIDDELALDERENS BERGEN – ET SENTRUM I PERIFERIEN Sør-Afrika Konservator og prosjektleder for Hvalprosjektet ved [email protected] Universitetsmuseet i Bergen, Associate Professor ved National Ora et labora – be og arbeid 35 Yunlin University of Science and Technology, Taiwan Alf Tore Hommedal [email protected] Alf Tore Hommedal Førsteamanuensis i arkeologi, De kulturhistoriske samlinger, Universitetsmuseet i Bergen Trond Lødøen Å skrive med stil 51 [email protected]