A Proposal to Fully Protect the South Sandwich Islands
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Region 19 Antarctica Pg.781
Appendix B – Region 19 Country and regional profiles of volcanic hazard and risk: Antarctica S.K. Brown1, R.S.J. Sparks1, K. Mee2, C. Vye-Brown2, E.Ilyinskaya2, S.F. Jenkins1, S.C. Loughlin2* 1University of Bristol, UK; 2British Geological Survey, UK, * Full contributor list available in Appendix B Full Download This download comprises the profiles for Region 19: Antarctica only. For the full report and all regions see Appendix B Full Download. Page numbers reflect position in the full report. The following countries are profiled here: Region 19 Antarctica Pg.781 Brown, S.K., Sparks, R.S.J., Mee, K., Vye-Brown, C., Ilyinskaya, E., Jenkins, S.F., and Loughlin, S.C. (2015) Country and regional profiles of volcanic hazard and risk. In: S.C. Loughlin, R.S.J. Sparks, S.K. Brown, S.F. Jenkins & C. Vye-Brown (eds) Global Volcanic Hazards and Risk, Cambridge: Cambridge University Press. This profile and the data therein should not be used in place of focussed assessments and information provided by local monitoring and research institutions. Region 19: Antarctica Description Figure 19.1 The distribution of Holocene volcanoes through the Antarctica region. A zone extending 200 km beyond the region’s borders shows other volcanoes whose eruptions may directly affect Antarctica. Thirty-two Holocene volcanoes are located in Antarctica. Half of these volcanoes have no confirmed eruptions recorded during the Holocene, and therefore the activity state is uncertain. A further volcano, Mount Rittmann, is not included in this count as the most recent activity here was dated in the Pleistocene, however this is geothermally active as discussed in Herbold et al. -
Of Penguins and Polar Bears Shapero Rare Books 93
OF PENGUINS AND POLAR BEARS Shapero Rare Books 93 OF PENGUINS AND POLAR BEARS EXPLORATION AT THE ENDS OF THE EARTH 32 Saint George Street London W1S 2EA +44 20 7493 0876 [email protected] shapero.com CONTENTS Antarctica 03 The Arctic 43 2 Shapero Rare Books ANTARCTIca Shapero Rare Books 3 1. AMUNDSEN, ROALD. The South Pole. An account of “Amundsen’s legendary dash to the Pole, which he reached the Norwegian Antarctic Expedition in the “Fram”, 1910-1912. before Scott’s ill-fated expedition by over a month. His John Murray, London, 1912. success over Scott was due to his highly disciplined dogsled teams, more accomplished skiers, a shorter distance to the A CORNERSTONE OF ANTARCTIC EXPLORATION; THE ACCOUNT OF THE Pole, better clothing and equipment, well planned supply FIRST EXPEDITION TO REACH THE SOUTH POLE. depots on the way, fortunate weather, and a modicum of luck”(Books on Ice). A handsomely produced book containing ten full-page photographic images not found in the Norwegian original, First English edition. 2 volumes, 8vo., xxxv, [i], 392; x, 449pp., 3 folding maps, folding plan, 138 photographic illustrations on 103 plates, original maroon and all full-page images being reproduced to a higher cloth gilt, vignettes to upper covers, top edges gilt, others uncut, usual fading standard. to spine flags, an excellent fresh example. Taurus 71; Rosove 9.A1; Books on Ice 7.1. £3,750 [ref: 96754] 4 Shapero Rare Books 2. [BELGIAN ANTARCTIC EXPEDITION]. Grande 3. BELLINGSHAUSEN, FABIAN G. VON. The Voyage of Fete Venitienne au Parc de 6 a 11 heurs du soir en faveur de Captain Bellingshausen to the Antarctic Seas 1819-1821. -
South Georgia and Antarctic Odyssey
South Georgia and Antarctic Odyssey 30 November – 18 December 2019 | Greg Mortimer About Us Aurora Expeditions embodies the spirit of adventure, travelling to some of the most wild opportunity for adventure and discovery. Our highly experienced expedition team of and remote places on our planet. With over 28 years’ experience, our small group voyages naturalists, historians and destination specialists are passionate and knowledgeable – they allow for a truly intimate experience with nature. are the secret to a fulfilling and successful voyage. Our expeditions push the boundaries with flexible and innovative itineraries, exciting Whilst we are dedicated to providing a ‘trip of a lifetime’, we are also deeply committed to wildlife experiences and fascinating lectures. You’ll share your adventure with a group education and preservation of the environment. Our aim is to travel respectfully, creating of like-minded souls in a relaxed, casual atmosphere while making the most of every lifelong ambassadors for the protection of our destinations. DAY 1 | Saturday 30 November 2019 Ushuaia, Beagle Channel Position: 20:00 hours Course: 83° Wind Speed: 20 knots Barometer: 991 hPa & steady Latitude: 54°49’ S Wind Direction: W Air Temp: 6° C Longitude: 68°18’ W Sea Temp: 5° C Explore. Dream. Discover. —Mark Twain in the soft afternoon light. The wildlife bonanza was off to a good start with a plethora of seabirds circling the ship as we departed. Finally we are here on the Beagle Channel aboard our sparkling new ice-strengthened vessel. This afternoon in the wharf in Ushuaia we were treated to a true polar welcome, with On our port side stretched the beech forested slopes of Argentina, while Chile, its mountain an invigorating breeze sweeping the cobwebs of travel away. -
Dubai 2020: Dreamscapes, Mega Malls and Spaces of Post-Modernity
Dubai 2020: Dreamscapes, Mega Malls and Spaces of Post-Modernity Dubai’s hosting of the 2020 Expo further authenticates its status as an example of an emerging Arab city that displays modernity through sequences of fragmented urban- scapes, and introvert spaces. The 2020 Expo is expected to reinforce the image of Dubai as a city of hybrid architectures and new forms of urbanism, marked by technologically advanced infrastructural systems. This paper revisits Dubai’s spaces of the spectacle such as the Burj Khalifa and themed mega malls, to highlight the power of these spaces of repre- sentation in shaping Dubai’s image and identity. INTRODUCTION MOHAMED EL AMROUSI Initially, a port city with an Indo-Persian mercantile community, Dubai’s devel- Abu Dhabi University opment along the Creek or Khor Dubai shaped a unique form of city that is con- stantly reinventing itself. Its historic adobe courtyard houses, with traditional PAOLO CARATELLI wind towers-barjeel sprawling along the Dubai Creek have been fully restored Abu Dhabi University to become heritage houses and museums, while their essential architectural vocabulary has been dismembered and re-membered as a simulacra in high-end SADEKA SHAKOUR resorts such as Madinat Jumeirah, the Miraj Hotel and Bab Al-Shams. Dubai’s Abu Dhabi University interest to make headlines of the international media fostered major investment in an endless vocabulary of forms and fragments to create architectural specta- cles. Contemporary Dubai is experienced through symbolic imprints of multiple policies framed within an urban context to project an image of a city offers luxu- rious dreamscapes, assembled in discontinued urban centers. -
Biodiversity: the UK Overseas Territories. Peterborough, Joint Nature Conservation Committee
Biodiversity: the UK Overseas Territories Compiled by S. Oldfield Edited by D. Procter and L.V. Fleming ISBN: 1 86107 502 2 © Copyright Joint Nature Conservation Committee 1999 Illustrations and layout by Barry Larking Cover design Tracey Weeks Printed by CLE Citation. Procter, D., & Fleming, L.V., eds. 1999. Biodiversity: the UK Overseas Territories. Peterborough, Joint Nature Conservation Committee. Disclaimer: reference to legislation and convention texts in this document are correct to the best of our knowledge but must not be taken to infer definitive legal obligation. Cover photographs Front cover: Top right: Southern rockhopper penguin Eudyptes chrysocome chrysocome (Richard White/JNCC). The world’s largest concentrations of southern rockhopper penguin are found on the Falkland Islands. Centre left: Down Rope, Pitcairn Island, South Pacific (Deborah Procter/JNCC). The introduced rat population of Pitcairn Island has successfully been eradicated in a programme funded by the UK Government. Centre right: Male Anegada rock iguana Cyclura pinguis (Glen Gerber/FFI). The Anegada rock iguana has been the subject of a successful breeding and re-introduction programme funded by FCO and FFI in collaboration with the National Parks Trust of the British Virgin Islands. Back cover: Black-browed albatross Diomedea melanophris (Richard White/JNCC). Of the global breeding population of black-browed albatross, 80 % is found on the Falkland Islands and 10% on South Georgia. Background image on front and back cover: Shoal of fish (Charles Sheppard/Warwick -
Chapter 4 Tectonic Reconstructions of the Southernmost Andes and the Scotia Sea During the Opening of the Drake Passage
123 Chapter 4 Tectonic reconstructions of the Southernmost Andes and the Scotia Sea during the opening of the Drake Passage Graeme Eagles Alfred Wegener Institute, Helmholtz Centre for Marine and Polar Research, Bre- merhaven, Germany e-mail: [email protected] Abstract Study of the tectonic development of the Scotia Sea region started with basic lithological and structural studies of outcrop geology in Tierra del Fuego and the Antarctic Peninsula. To 19th and early 20th cen- tury geologists, the results of these studies suggested the presence of a submerged orocline running around the margins of the Scotia Sea. Subse- quent increases in detailed knowledge about the fragmentary outcrop ge- ology from islands distributed around the margins of the Scotia Sea, and later their interpretation in light of the plate tectonic paradigm, led to large modifications in the hypothesis such that by the present day the concept of oroclinal bending in the region persists only in vestigial form. Of the early comparative lithostratigraphic work in the region, only the likenesses be- tween Jurassic—Cretaceous basin floor and fill sequences in South Geor- gia and Tierra del Fuego are regarded as strong enough to be useful in plate kinematic reconstruction by permitting the interpretation of those re- gions’ contiguity in mid-Mesozoic times. Marine and satellite geophysical data sets reveal features of the remaining, submerged, 98% of the Scotia 124 Sea region between the outcrops. These data enable a more detailed and quantitative approach to the region’s plate kinematics. In contrast to long- used interpretations of the outcrop geology, these data do not prescribe the proximity of South Georgia to Tierra del Fuego in any past period. -
Developing UAV Monitoring of South Georgia and the South Sandwich Islands’ Iconic Land-Based Marine Predators
fmars-08-654215 May 26, 2021 Time: 18:32 # 1 ORIGINAL RESEARCH published: 01 June 2021 doi: 10.3389/fmars.2021.654215 Developing UAV Monitoring of South Georgia and the South Sandwich Islands’ Iconic Land-Based Marine Predators John Dickens1*, Philip R. Hollyman1, Tom Hart2, Gemma V. Clucas3, Eugene J. Murphy1, Sally Poncet4, Philip N. Trathan1 and Martin A. Collins1 1 British Antarctic Survey, Natural Environment Research Council, Cambridge, United Kingdom, 2 Department of Zoology, University of Oxford, Oxford, United Kingdom, 3 Cornell Lab of Ornithology, Cornell University, Ithaca, NY, United States, 4 South Georgia Survey, Stanley, Falkland Islands Many remote islands present barriers to effective wildlife monitoring in terms of Edited by: challenging terrain and frequency of visits. The sub-Antarctic islands of South Georgia Wen-Cheng Wang, National Taiwan Normal University, and the South Sandwich Islands are home to globally significant populations of seabirds Taiwan and marine mammals. South Georgia hosts the largest breeding populations of Antarctic Reviewed by: fur seals, southern elephant seals and king penguins as well as significant populations of Gisele Dantas, wandering, black-browed and grey-headed albatross. The island also holds important Pontifícia Universidade Católica de Minas Gerais, Brazil populations of macaroni and gentoo penguins. The South Sandwich Islands host the Sofie Pollin, world’s largest colony of chinstrap penguins in addition to major populations of Adélie KU Leuven Research & Development, Belgium and macaroni penguins. A marine protected area was created around these islands in *Correspondence: 2012 but monitoring populations of marine predators remains a challenge, particularly John Dickens as these species breed over large areas in remote and often inaccessible locations. -
West Antarctica: Tectonics and Paleogeography
Chapter 2 West Antarctica: Tectonics and Paleogeography The origin of West Antarctica (WANT) can be traced back to the Terra Australis orogenesis that began between 520 Ma and 510 Ma—shortly after the terminal suturing of Gondwana (Boger 2011). The onset of this event was responsible for the termination of passive margin sedimentation along much of the Pacific margin of Gondwana and marks the beginning of widespread and broadly coeval deforma- tion and arc-type plutonism. It also began a long-lived process of accretion that added much of the crust that defines eastern Australia, West Antarctica (domain 5 of Boger 2011, Fig. 2.1), and western South America (Cawood 2005, 2009). Post-Gondwana accretionary growth—the Terra Australis and Gondwanide Orogenies—The suturing of the West Gondwana and Australo–Antarctic plates along the Kuunga Orogen brought to an end the long-lived process of convergence between the pre-collision components of Gondwana. The result was a reconfigura- tion of the early to middle Cambrian plate system and the consequent transfer of ocean floor consumption from between the pre-Gondwana cratons to the outboard Pacific margin of newly formed Gondwana supercontinent (Cawood2005 ). This led to the establishment of the accretionary Terra Austrais Orogen (Cawood 2005), a general name given to the orogenic belt that stretched continuously from north- ern South America to northern Australia and which began in the early to middle Cambrian and lasted until the late Carboniferous. In Antarctica Terra Australis (Ross) orogenesis also deformed and variably metamorphosed the pre-Gondwana passive margin (Fig. 2.2). The Gondwana supercontinent underwent a sequential fragmentation over approximately 165 Ma. -
An Assessment for Fisheries Operating in South Georgia and South Sandwich Islands
FAO International Plan of Action-Seabirds: An assessment for fisheries operating in South Georgia and South Sandwich Islands by Nigel Varty, Ben Sullivan and Andy Black BirdLife International Global Seabird Programme Cover photo – Fishery Patrol Vessel (FPV) Pharos SG in Cumberland Bay, South Georgia This document should be cited as: Varty, N., Sullivan, B. J. and Black, A. D. (2008). FAO International Plan of Action-Seabirds: An assessment for fisheries operating in South Georgia and South Sandwich Islands. BirdLife International Global Seabird Programme. Royal Society for the Protection of Birds, The Lodge, Sandy, Bedfordshire, UK. 2 Executive Summary As a result of international concern over the cause and level of seabird mortality in longline fisheries, the United Nations Food and Agricultural Organisation (FAO) Committee of Fisheries (COFI) developed an International Plan of Action-Seabirds. The IPOA-Seabirds stipulates that countries with longline fisheries (conducted by their own or foreign vessels) or a fleet that fishes elsewhere should carry out an assessment of these fisheries to determine if a bycatch problem exists and, if so, to determine its extent and nature. If a problem is identified, countries should adopt a National Plan of Action – Seabirds for reducing the incidental catch of seabirds in their fisheries. South Georgia and the South Sandwich Islands (SGSSI) are a United Kingdom Overseas Territory and the combined area covered by the Territorial Sea and Maritime Zone of South Georgia is referred to as the South Georgia Maritime Zone (SGMZ) and fisheries within the SGMZ are managed by the Government of South Georgia and South Sandwich Islands (GSGSSI) within the framework of the Convention on the Conservation of Antarctic Marine Living (CCAMLR). -
Redacted for Privacy Abstract Approved: John V
AN ABSTRACT OF THE THESIS OF MIAH ALLAN BEAL for the Doctor of Philosophy (Name) (Degree) in Oceanography presented on August 12.1968 (Major) (Date) Title:Batymety and_Strictuof_thp..4rctic_Ocean Redacted for Privacy Abstract approved: John V. The history of the explordtion of the Central Arctic Ocean is reviewed.It has been only within the last 15 years that any signifi- cant number of depth-sounding data have been collected.The present study uses seven million echo soundings collected by U. S. Navy nuclear submarines along nearly 40, 000 km of track to construct, for the first time, a reasonably complete picture of the physiography of the basin of the Arctic Ocean.The use of nuclear submarines as under-ice survey ships is discussed. The physiography of the entire Arctic basin and of each of the major features in the basin are described, illustrated and named. The dominant ocean floor features are three mountain ranges, generally paralleling each other and the 40°E. 140°W. meridian. From the Pacific- side of the Arctic basin toward the Atlantic, they are: The Alpha Cordillera; The Lomonosov Ridge; andThe Nansen Cordillera. The Alpha Cordillera is the widest of the three mountain ranges. It abuts the continental slopes off the Canadian Archipelago and off Asia across more than550of longitude on each slope.Its minimum width of about 300 km is located midway between North America and Asia.In cross section, the Alpha Cordillera is a broad arch rising about two km, above the floor of the basin.The arch is marked by volcanoes and regions of "high fractured plateau, and by scarps500to 1000 meters high.The small number of data from seismology, heat flow, magnetics and gravity studies are reviewed.The Alpha Cordillera is interpreted to be an inactive mid-ocean ridge which has undergone some subsidence. -
The Appropriation Bill 2003
SOUTH GEORGIA AND SOUTH SANDWICH ISLANDS GAZETTE PUBLISHED BY AUTHORITY No. 2 13 June 2013 The following are published in this Gazette – Notices 1 to 10; Supplementary Appropriation (2012) Ordinance 2013 (No 2 of 2013); Appropriation (2013) Ordinance 2013 (No 3 of 2013); Wildlife and Protected Areas (Amendment) Ordinance 2013 (No 4 of 2013); Postal Services (Amendment) Ordinance 2013 (No 5 of 2013); Marine Protected Areas Order 2013 (SR&O No 1 of 2013); Prohibited Areas Order 2013 (SR&O No 2 of 2013); and Coins Order 2013 (SR&O No 3 of 2013). 1 NOTICES terminated sooner. Dated 11 February 2013 No. 1 14 December 2012 N. R. HAYWOOD C.V.O., Commissioner. United Kingdom Statutory Instruments ____________________ Notice is hereby given that the following United Kingdom No. 3 6 May 2013 Statutory Instruments have been published in the United Kingdom by The Stationery Office Limited and are Police Ordinance 1967 available to view at www.legislation.gov.uk: section 5 Enrolment of Police Officer 2012 No 2748 – The Iraq (United Nations Sanctions) 1. The Police Ordinance 1967 (No 9 of 1967, Falkland (Overseas Territories) (Amendment) Order 2012; Islands) applies to South Georgia and the South Sandwich Islands by reference to the Application of Colonies Laws 2012 No 2749 – The Liberia (Restrictive Measures) Ordinance 1967 (No 1of 1967, Falkland Islands). (Overseas Territories) (Amendment) Order 2012; 2. Section 5 of the Ordinance provides that the Police 2012 No 2750 – The Democratic Republic of the Congo Force shall consist of such police officers as may from time (Restrictive Measures) (Overseas Territories) (Amendment) to time be approved by the Commissioner and enrolled in Order 2012; the Force. -
Research Vessel POLARSTERN PS119: 13.04
Research vessel POLARSTERN PS119: 13.04. – 31.05.2019 Punta Arenas ‐ Port Stanley Sixth weekly report: 13. – 19. May, 2019 To the smoking volcano of Saunders Island Like last week, we spent the sixth week in the southernmost area of the South Sandwich Plate, from the back‐arc spreading ridge of the segments 8 and 9 in the west to the Kemp Caldera. The volcano of Kemp Caldera is part of the collision zone with the South American plate to the East. A look to our expedition logo shows symbolically the spreading ridge on the left and flowing to the right the volcanoes, fore‐arc area and subduction zone. The weather conditions, which denied from Sunday to Tuesday morning further dives, permitted not until Tuesday to dive down with ROV QUEST to the seafloor. We used the dive‐free time for the deployment of other sampling gear. On Sunday, 12th of May, we sampled the deepest area of the Kemp caldera with a 3 m long gravity corer and the multi‐corer. The until then surveyed Parasound profiles over the caldera showed in the deepest area narrow sediment layers, whose mineral and chemical composition in references to hydrothermal deposits are of huge interest. With our corers we were able to sample sediment layers of 230 cm depth, which surprised us by their colouring and diverse sediment compositions. Figure 1: Penguins being washed up by a wave’s high to an Figure 2: Analyses of sediment cores in the laboratory of an iceberg following by a steep climb (© Carsten Zillgen). Polarstern.