The 1773 Phipps Expedition Towards the North Pole ANN SAVOURS (MRS
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- . - - - . -. � ..;/, 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? .... -
Foraminifera1 Stratigraphy of Raised Marine Deposits, Representing Isotope Stage 5, Prins Karls Forland, Western Sval Bard
Foraminifera1 stratigraphy of raised marine deposits, representing isotope stage 5, Prins Karls Forland, western SVal bard HELENE BERGSTEN. TORBJORN ANDERSON and OLAFUR INGOLFSSON Bergsten, H., Andersson. T. & Ingolfsson, 0. 1998: Foraminiferd stratigraphy of raised marine deposits, representing isotope stage 5. Prins Karls Forland, western Svalbard. Polar Research 17(1). 81-91. Two raised marine sequences from Prim Karls Forland, western Svalbard, interpreted to have been deposited during part of isotope substage Se (Eemian) and substage 5a, were studied for foraminifera content. Time constraints are given by I4C ages, infrared stimulated luminescence age estimates and amino acid ratios in suhfossil marine molluscs. A diamicton (unit B) separates the two marine sequences and reflects an advancement of local glaciers sometime late in isotope stage 5. The two marine sequences contain diverse benthic foraminifera1 faunas, indicating periods of a relatively warm and seasonally ice-free marine shelf environment. Compared to the lowermost sequence (unit A), the upper marine sequence (unit C) seems to reflect a more shallow environment that could have resulted from the global lowering of the sea level towards the end of isotope stage 5. Our results further emphasise the problem of biostratigraphic distinction between interglacial and interstadial deposits at high latitudes, with temperature conditions for substage Sa close to those of substage 5e and present conditions. Helene Bergsten, Torbjorn Andersson and Olufur Ingdlfsson, Earth Sciences Centre, Goteborg University, Box 460, S-405 30 Goteborg, Sweden. Introduction Chronology and glacial history The Poolepynten site is situated on Prins Karls Sediments in the Poolepynten sections are ex- Forland, western Svalbard at N78'27'El l"40' posed in up to 10 metre high coastal cliffs over a (Fig. -
Seacare Authority Exemption
EXEMPTION 1—SCHEDULE 1 Official IMO Year of Ship Name Length Type Number Number Completion 1 GIANT LEAP 861091 13.30 2013 Yacht 1209 856291 35.11 1996 Barge 2 DREAM 860926 11.97 2007 Catamaran 2 ITCHY FEET 862427 12.58 2019 Catamaran 2 LITTLE MISSES 862893 11.55 2000 857725 30.75 1988 Passenger vessel 2001 852712 8702783 30.45 1986 Ferry 2ABREAST 859329 10.00 1990 Catamaran Pleasure Yacht 2GETHER II 859399 13.10 2008 Catamaran Pleasure Yacht 2-KAN 853537 16.10 1989 Launch 2ND HOME 856480 10.90 1996 Launch 2XS 859949 14.25 2002 Catamaran 34 SOUTH 857212 24.33 2002 Fishing 35 TONNER 861075 9714135 32.50 2014 Barge 38 SOUTH 861432 11.55 1999 Catamaran 55 NORD 860974 14.24 1990 Pleasure craft 79 199188 9.54 1935 Yacht 82 YACHT 860131 26.00 2004 Motor Yacht 83 862656 52.50 1999 Work Boat 84 862655 52.50 2000 Work Boat A BIT OF ATTITUDE 859982 16.20 2010 Yacht A COCONUT 862582 13.10 1988 Yacht A L ROBB 859526 23.95 2010 Ferry A MORNING SONG 862292 13.09 2003 Pleasure craft A P RECOVERY 857439 51.50 1977 Crane/derrick barge A QUOLL 856542 11.00 1998 Yacht A ROOM WITH A VIEW 855032 16.02 1994 Pleasure A SOJOURN 861968 15.32 2008 Pleasure craft A VOS SANTE 858856 13.00 2003 Catamaran Pleasure Yacht A Y BALAMARA 343939 9.91 1969 Yacht A.L.S.T. JAMAEKA PEARL 854831 15.24 1972 Yacht A.M.S. 1808 862294 54.86 2018 Barge A.M.S. -
ESG Perspectives June 2019 Svalbard Sojourn an Arctic
June 2019 ESG Perspectives ™ SVALBARD SOJOURN: AN ARCTIC EXPERIENCE by Bob Smith, President & CIO islands are 60% glaciated with some of the world’s fastest-moving glaciers. The balance of the region is 30% barren ground, and 10% is covered with very low ground vegetation. In contrast to other Arctic regions, the Svalbard has no indigenous population and there is no historical evidence that the Vikings settled in the area during their time. In fact, it was the 1596 Dutch expedition of Willem Barents who discovered and drew maps of the region before his ship was crushed by freezing sea ice leading to his untimely death. However, the work of this expedition survived, and it led to the exploration of the region by other European countries over the Photo of Bob Smith in Kungsfjord, Svalbard centuries. This eventually gave rise to the exploitation It is said that what happens in the Arctic doesn’t stay of the natural resources of the region as a destination in the Arctic. That is because this region provides for whalers, fur trappers, and seal hunters, as well as essential global climate regulation and substantial other animal-based products. With the industrialization ecosystem benefits to humanity outside and beyond of Europe and the arrival of steel-hulled ships in the its boundaries. Indeed, the Arctic environment, and early 1900s, this region also eventually became a source human society and its economic activities are deeply for industrial minerals and, in particular, coal. connected to each other, representing a pivotal link in a complex adaptive global ecosystem. -
Locating South China in Rodinia and Gondwana: a Fragment of Greater India Lithosphere?
Locating South China in Rodinia and Gondwana: A fragment of greater India lithosphere? Peter A. Cawood1, 2, Yuejun Wang3, Yajun Xu4, and Guochun Zhao5 1Department of Earth Sciences, University of St Andrews, North Street, St Andrews KY16 9AL, UK 2Centre for Exploration Targeting, School of Earth and Environment, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia 3State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 4State Key Laboratory of Biogeology and Environmental Geology, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China 5Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China ABSTRACT metamorphosed Neoproterozoic strata and From the formation of Rodinia at the end of the Mesoproterozoic to the commencement unmetamorphosed Sinian cover (Fig. 1; Zhao of Pangea breakup at the end of the Paleozoic, the South China craton fi rst formed and then and Cawood, 2012). The Cathaysia block is com- occupied a position adjacent to Western Australia and northern India. Early Neoproterozoic posed predominantly of Neoproterozoic meta- suprasubduction zone magmatic arc-backarc assemblages in the craton range in age from ca. morphic rocks, with minor Paleoproterozoic and 1000 Ma to 820 Ma and display a sequential northwest decrease in age. These relations sug- Mesoproterozoic lithologies. Archean basement gest formation and closure of arc systems through southeast-directed subduction, resulting is poorly exposed and largely inferred from the in progressive northwestward accretion onto the periphery of an already assembled Rodinia. presence of minor inherited and/or xenocrys- Siliciclastic units within an early Paleozoic succession that transgresses across the craton were tic zircons in younger rocks (Fig. -
Early Maritime Navigation Unit Plan
EARLY MARITIME NAVIGATION UNIT PLAN Compelling How did advances in marine navigation, from the 13th century C.E. through the 18th century Question C.E., help to catapult Western Europe into global preeminence? C3 Historical Thinking Standards – D2.His.1.9-12. Evaluate how historical events and developments were shaped by unique circumstances of time and place as well as broader historical contexts. Standards C3 Historical Thinking Standards – D2.His.2.9-12. and Analyze change and continuity in historical eras. Practices Common Core Content Standards – CCSS.ELA-LITERACY.WHST.9-10.1.B Develop claim(s) and counterclaims fairly, supplying data and evidence for each while pointing out the strengths and limitations of both claim(s) and counterclaims in a discipline-appropriate form and in a manner that anticipates the audience's knowledge level and concerns. Staging the How do advances in marine navigation technology help nations develop and sustain world Question influence? Supporting Supporting Supporting Supporting Question 1 Question 2 Question 3 Question 4 Why has the sea been What is navigation and How does being posed How did STEM confer crucial to the fate of what special challenges with a challenge lead us to advantages to a society’s nations, empires, and does the sea pose to innovation and progress? ability to navigate the civilizations? travelers? world’s oceans? Formative Formative Formative Formative Performance Task 1 Performance Task 2 Performance Task 3 Performance Task 4 1) Look at the planet’s 1) In pairs ask your 1) Compass Lesson Plan 1) Drawing connections to physical geography, partner to draw you a (Lesson is located below the last three questions, all the Print Documents) build an argument that map from school to a view the Longitude video the sea was better at specific location in your Discover how the (07:05 min) connecting cultures town. -
Chapter 1 Svalbard, 3 Chapter 2 Outline History of Geological Research, 16 Chapter 3 Svalbard's Geological Frame, 23
Downloaded from http://mem.lyellcollection.org/ by guest on September 25, 2021 PART 1 Introduction Chapter 1 Svalbard, 3 Chapter 2 Outline history of geological research, 16 Chapter 3 Svalbard's geological frame, 23 Mid-season view of the glaciers Comfortlessbreen (on the left) and Aavartsmarkbreen (beyond). The rocks are Early Vendian with Varanger tillites. Stratigraphic sections are generally worked along the glacier margins either by porterage from the shore (in this case Egelskbukta) or by sledge from the interior. Photo M. J. Hambrey (SP. 455). Late season view from the east over the terminal crevassed glacier Monacobreen. In this case access up the glacier is almost impossible because the lower reaches are deeply crevassed and the glacier terminates in ice-cliffs in inner Liefdefjorden. The glacier beyond offers an easy route westward. Photo P. W. Webb, CSE 1989. Downloaded from http://mem.lyellcollection.org/ by guest on September 25, 2021 View from Ossian Sarsfjellet at the eastern end of Kongsfjorden towards the mountains of Broggerhalvoya which are reflected in the fjord. The intervening fjord carries a scatter of small bergs which have calved from the glacier cliffs of Kronebreen and Kongsbreen respectively to north and south of the photographer. The concentration of ice depends on wind and tide and is navigable with care in a slow moving boat. The small bergs melt rapidly in the summer. Photo M. J. Hambrey (SP96.122) 1996. The CSE motorboat Salterella in mid-Kongsfjorden seen when looking out to sea with the landmark Kapp Mitra to the right where the rocks are Caledonian metamorphosed basement of pre-Vendian rocks. -
Cambridge University Press 978-0-521-76518-3 — the Making of the Modern Admiralty C
Cambridge University Press 978-0-521-76518-3 — The Making of the Modern Admiralty C. I. Hamilton Index More Information Index Accountant-General, 60; of the Navy Arbuthnot, Charles, 97–8 (from 1832): 65, 125, 138, 146, Army Staff, 222 189–93, 295 (see also estimates); Arnold-Forster, H. O., 198, 217 staff, 164, 188, 192 Asquith, H. H., 224 administrative board, 31 Assistant Secretary for Finance Duties Admiralty (see also Admiralty Office; (see also Secretariat), 192 Board of Admiralty; Childers, H. C. E.; Aube, H.-L.-T., 172 First and Second (Permanent) Auckland, George Eden, Earl of, 119, 134 Secretaries; Geddes, E.; Goschen, Awdry, Richard, 191, 201, 205 George; Graham, Sir James; ‘mob from the North’; Naval Staff; Navy Bacon, Sir Reginald, (Kt. 1916), 215 Board; Navy Pay Office; Principal Baddeley, Vincent, (Kt. 1921), 205, 206, 259 Officers; Private Office; Victualling Balfour, A. J., 237, 238 Board; Secretariat; Sick and Hurt Ballard, G. A., 222, 223 Office; Sixpenny Office; Transport Bank of England, 28 Office; War Staff): administration/ Barham, Lord, see Middleton, Charles policy divide, 266–7, 275, 279, 288, Barnaby, Nathaniel (Kt. 1885), 136, 162, 307; attacks on, 312; civil–military 173, 194–5 division in (see also Godfrey, John), Barrow, John (cr. baronet, 1835) (see also 68–9, 279, 289, 297–302, 313, 314; Second Secretary): 6, 12, 52, 57, 63; committees, 110–11, 120–3, 186–9, administration and policy of, 41, 51, 215; communications, 176, 220, 64, 68–9, 75, 93, 100–1, 103, 152, 248–50; demobilisation, 274, 276; 163; and Benthamism, 54; and development, 2–3, 23, 234–6; J. -
Memoirs of Hydrography
MEMOIRS 07 HYDROGRAPHY INCLUDING Brief Biographies of the Principal Officers who have Served in H.M. NAVAL SURVEYING SERVICE BETWEEN THE YEARS 1750 and 1885 COMPILED BY COMMANDER L. S. DAWSON, R.N. I 1s t tw o PARTS. P a r t II.—1830 t o 1885. EASTBOURNE: HENRY W. KEAY, THE “ IMPERIAL LIBRARY.” iI i / PREF A CE. N the compilation of Part II. of the Memoirs of Hydrography, the endeavour has been to give the services of the many excellent surveying I officers of the late Indian Navy, equal prominence with those of the Royal Navy. Except in the geographical abridgment, under the heading of “ Progress of Martne Surveys” attached to the Memoirs of the various Hydrographers, the personal services of officers still on the Active List, and employed in the surveying service of the Royal Navy, have not been alluded to ; thereby the lines of official etiquette will not have been over-stepped. L. S. D. January , 1885. CONTENTS OF PART II ♦ CHAPTER I. Beaufort, Progress 1829 to 1854, Fitzroy, Belcher, Graves, Raper, Blackwood, Barrai, Arlett, Frazer, Owen Stanley, J. L. Stokes, Sulivan, Berard, Collinson, Lloyd, Otter, Kellett, La Place, Schubert, Haines,' Nolloth, Brock, Spratt, C. G. Robinson, Sheringham, Williams, Becher, Bate, Church, Powell, E. J. Bedford, Elwon, Ethersey, Carless, G. A. Bedford, James Wood, Wolfe, Balleny, Wilkes, W. Allen, Maury, Miles, Mooney, R. B. Beechey, P. Shortland, Yule, Lord, Burdwood, Dayman, Drury, Barrow, Christopher, John Wood, Harding, Kortright, Johnson, Du Petit Thouars, Lawrance, Klint, W. Smyth, Dunsterville, Cox, F. W. L. Thomas, Biddlecombe, Gordon, Bird Allen, Curtis, Edye, F. -
Downloaded from Brill.Com10/01/2021 12:06:24AM Via Free Access History of Science Scholars in Action
Scholars in Action - 9789004243910 Downloaded from Brill.com10/01/2021 12:06:24AM via free access History of Science Scholars in Action and Medicine Library The Practice of Knowledge and the Figure of the Savant in the 18th Century VOLUME 34/1 Volume 1 Scientific and Learned Cultures and Edited by André Holenstein, Hubert Steinke, and Martin Stuber Their Institutions Editor In collaboration with M. Feingold Philippe Rogger California Institute of Technology VOLUME 9 LEIDEN • BOSTON The titles published in this series are listed at brill.com/slci 2013 - 9789004243910 Downloaded from Brill.com10/01/2021 12:06:24AM via free access History of Science Scholars in Action and Medicine Library The Practice of Knowledge and the Figure of the Savant in the 18th Century VOLUME 34/1 Volume 1 Scientific and Learned Cultures and Edited by André Holenstein, Hubert Steinke, and Martin Stuber Their Institutions Editor In collaboration with M. Feingold Philippe Rogger California Institute of Technology VOLUME 9 LEIDEN • BOSTON 2013 - 9789004243910 Downloaded from Brill.com10/01/2021 12:06:24AM via free access This is an open access title distributed under the terms of the CC BY-NC-ND 4.0 license, which permits any non-commercial use, distribution, and reproduction in any medium, provided no alterations are made and the original author(s) and source are credited. Further information and the complete license text can be found at https://creativecommons.org/licenses/by-nc-nd/4.0/ The terms of the CC license apply only to the original material. The use of material from other sources (indicated by a reference) such as diagrams, illustrations, photos and text samples may require further permission from the respective copyright holder. -
Mapping Our World: Terra Incognita to Australia
XIV Mapping our world The maps seemed to have a life which was essentially XV paradoxical, being both ancient and contemporary in the same moment. They showed recognisable worlds which had been changed by more recent knowledge and cartographic handiwork, and yet preserved the past in the Matthew Flinders, General Chart of Terra Australis Maps are perhaps the most intriguing and revealing of immediacy and colour of the present. or Australia: showing the parts explored between 1798 visual documents. Their presence is felt from the first The thoughtful gaze of viewers was generously reciprocated and 1803 by M. Flinders Commr. of H.M.S. Investigator experience of a school atlas or globe to Google maps of by the rich, storied surfaces of the encyclopaedic array of (detail), London, 1814 (corrected to 1822) our backyards and streets. The form and content of maps charts, globes and atlases. Whether they visited because NATIONAL LIBRARY OF AUSTRALIA, CANBERRA, have changed markedly over the centuries, and Mapping TOOLEY COLLECTION, MAP T 1494 they loved maps, were map collectors, or just wanted Our World: Terra Incognita to Australia takes as one of its to experience the rarity and splendour of a memorable starting points this fascinating story of transformation: cartographic exhibition was hard to determine. The maps the development of cartography since the first speculative in these exhibitions seemed to make viewers slow down, maps emerged from the ancient world. Piece by piece, and perhaps travel a little way with the mapmaker, beyond through imagination and exploration, the world has aspects of cartography and history and into the realm of been charted, often at great cost, and now in the early the imagination. -
The Quest for Longitude
FOR IMMEDIATE RELEASE Press Contacts: Garland Scott, (202) 675-0342, [email protected] Esther French, (202) 675-0326, [email protected] Press Tour: Wednesday, March 18, 10:30 am Reservations requested, [email protected] New Exhibition—Ships, Clocks & Stars: The Quest for Longitude The solution to one of the greatest technical challenges of the eighteenth century Produced by the National Maritime Museum, Greenwich, London Proudly sponsored by United Technologies Corporation On exhibit March 19 – August 23, 2015 Washington, DC— For centuries, longitude (east-west position) was a matter of life and death at sea. Ships that went off course had no way to re-discover their longitude. With no known location, they might smash into underwater obstacles or be forever lost at sea. The award-winning exhibition, Ships, Clocks & Stars: The Quest for Longitude, produced by the National Maritime Museum in Greenwich, London, celebrates the 300th anniversary of the British Longitude Act of 1714, which offered huge rewards for any practical way to determine longitude at sea. The longitude problem was so difficult that—despite that incentive—it took five decades to solve it. Through extraordinary, historic materials—many from the collection of the National Maritime Museum—the exhibition tells the story of the clockmakers, astronomers, naval officers, and others who pursued the long "quest for longitude" to ultimate success. John Harrison’s work in developing extremely advanced marine timekeepers, which was vital to finally solving the problem of longitude, took place against a backdrop of almost unprecedented collaboration and investment. Featured in this complex and fascinating history are the names of Galileo, Isaac Newton, Captain James Cook, and William Bligh of HMS Bounty.