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2016 Heard Island Expedition Project Description
2016 Heard Island Expedition Project Description Definition TITLE BIOGEOCHEMICAL COMPOSITION OF THE SUBGLACIAL REGIME ON HEARD ISLAND USING GLACIAL STREAMS AS REMOTE SAMPLING PROBES Abstract We plan to examine the chemical composition and particulate loads of glacial streams at Heard Island as a probe of the geochemical and geophysical composition of the parent rocks, and the microbiological activity of the subglacial till. Given the impressive size and discharge of many of these streams, and their deposition of large amounts of fine sediment in various lagoons and the ocean, these streams are obviously transporting large amounts of material from underneath the glaciers. Lixiviation and direct solution will add solutes to the meltwater, providing a clear chemical signature in samples taken downstream. In addition, subglacial till is a refugium for microbial life which will be carried in the runoff. This work will consist of collecting samples from as many streams as possible, followed by laboratory characterization of the particulates, solutes, and bioactive components. Principal Investigator Fred Belton Cordell Expeditions Principal Investigator Robert Schmieder Cordell Expeditions Co-Investigator Gavin Marshall Tangaroa Blue Foundation Co-Investigator William Mitchell Cordell Expeditions Co-Investigator Staff U. S. Geological Survey Co-Investigator Carlos Nascimento Biochemist Co-Investigator Patrick Quilty University of Tasmania Co-Investigator Maria Hauger Consultant Co-Investigator Onsite team members Cordell Expeditions Context Background Satellite images of Heard Island taken in 2014 have sufficient resolution to exhibit many glacial melt streams, clearly seen as they approach the shoreline and disappear into the ocean, some entering lagoons depositing large amounts of fine sediment. Most of these streams, especially the longer ones (descending up to 3 km) show classic meanders with periods ca. -
Heard and Mcdonald Islands Australia
HEARD AND MCDONALD ISLANDS AUSTRALIA Heard Island and the McDonald Islands are in the Southern Ocean, approximately 4,100 km south- west of Perth and 1,700 km from the Antarctic continent. Their distinctive conservation value is as one of the world’s rare pristine island ecosystems which have virtually no record of alien species and minimal human impact; also as the only volcanically active subantarctic islands they provide a window into ongoing tectonic activity, geomorphic processes and glacial dynamics. COUNTRY Australia NAME Heard and McDonald Islands NATURAL WORLD HERITAGE SERIAL SITE 1997: Inscribed on the World Heritage List under Natural Criteria viii and ix. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] The UNESCO World Heritage Committee issued the following statement at the time of inscription: Justification for Inscription The Committee inscribed this property under criteria (viii) and (ix). It noted that this site is the only volcanically active sub-Antarctic island and illustrates ongoing geomorphic processes and glacial dynamics in the coastal and submarine environment and sub-Antarctic flora and fauna, with no record of alien species. The Committee repeated its request by the sixteenth session for further documentation on the marine resources of the site. IUCN MANAGEMENT CATEGORY 1a Strict Nature Reserve BIOGEOGRAPHICAL PROVINCE Insulantarctica (7.4.9) GEOGRAPHICAL LOCATION Located in the southern Indian Ocean 4,100 km south-west of Australia and 1,700 km north of Mawson Base, Antarctica. Heard Island is at 53°06'S by 73°30'E with the McDonald Islands 43.5 km west of it at 53°03'S by 72°36'E. -
Origin and Evolution of the Sub-Antarctic Islands: the Foundation
Papersnd a Proceedings of the Royal Society of Tasmania, Volume 141 (1), 2007 35 ORIGIN AND EVOLUTION OF THE SUB-ANTARCTIC ISLANDS: THE FOUNDATION by Patrick G. Quilty (with 23 text-figures and two tables) Quilty, P.G. 2007 (23:xi): Origin and evolution of the sub-Antarctic islands: the foundation.Papers and Proceedings of the Royal Society of Tasmania 141 (1): 35-58. https://doi.org/10.26749/rstpp.141.1.35 ISSN 0080-4703. School of Earth Sciences, University of Tasmania, Private Bag 79, Hobart, Tasmania 7001, Australia. Email: P.Quil [email protected] Sub-Antarctic islands have a diversity of origins in detail but most are volcanic and very young suggesting that they are short-lived and that the distribution would have been very differenta few million years ago. 'They contrast with the common tourist brochure concept of oceanic islands. As the Antarctic Plate is virtually static, the islands seldom show signs of association with long-lived linear island chains and most thus stand alone. Longer-lived islands are either on submarine plateaux or are continental remnants of the dispersion of Gondwana. The islands are classified in relation to raised sea-floor, transform fault, triple junction, subduction zone, submarine plateau, submerged continent or continental. Many are difficult of access and poorly known geologically. Their geological history controls their many other roles such as sites as observatories, or for study of colonisation, evolution and speciation rates. Key Words: Sub-Antarctic islands, geological evolution, Macquarie Island, Balleny Islands, Scott Island, Campbell Island, Antipodes Island, Auckland Islands, Enderby Island, Peter I Island, Islas Diego Ramirez, South Georgia, South Sandwich Islands, Bouvetoya, Gough Island, Marion Island, Prince Edward Island, Iles Crozet, Amsterdam Island, St Paul Island, Kerguelen Plateau, Iles Kerguelen, Heard Island, McDonald Island. -
CHANGES in HEARD ISLAND GLACIERS, KING PENGUINS and Furby SEALS G
Papers and Proceedings of the Royal Society of Tasmania, Volume 133(2), 2000 47 CHANGES IN HEARD ISLAND GLACIERS, KING PENGUINS AND FURby SEALS G. M. Budd SINCE 1947 (with two tables, three text-figures and one plate) BUDD, G.M., 2000 (30:vi): Changes in Heard Island glaciers, king penguins and fur seals since 1947. In Banks M.R. & Brown, M.]. (Eds): HEARD ISLAND Pap. Proc. R. Soc. Tasm. 133 (2): 47-60. https://doi.org/10.26749/rstpp.133.2.47 ISSN 0080-4703. School of Exercise and RS. Sport Science, The University of Sydney, PO Box 170, Lidcombe, NSW, Australia 2141. The purpose of this paper is to summarise and discuss the changes in glaciers, king penguins and fur seals reported by the nine wintering parties and 11 summer expeditions that have visited Heard Island since 1947, with emphasis upon those of the years between 1947 and 1971. These early years were notable for an initial period (1947-55) of minimal change, and a subsequent period(1963-71) of rapid change in which a complex pattern of asynchronous glacier retreat and readvance was observed and the main features of the island's recolonisation by king penguins and fur seals were established. Subsequent expeditions (1980-93) have reported continuing glacier recession, evidently in response to warmer air temperatures, and a continuing exponential increase in king penguins and fur seals. The glacier observations show that the Heard Island glaciers are sensitive indicators of climate change in the Southern Ocean, and of the interactions between climate and glacier topography. The island's recolonisation by king penguins and fur seals is attributed mainly to an improved food supply which may itself, like the glacier recession, be a response to changes in atmospheric and oceanic circulation. -
Heard Island and Mcdonald Islands Australia
HEARD ISLAND AND MCDONALD ISLANDS AUSTRALIA McDonald Island with Meyer Aock in background(G. Johnstone) Heard Island and McDonald Islands (Australia) 11 WORLD HERITAGE NOMINATION - IUCN TECHNICAL EVALUATION HEARD ISLAND AND MCDONALD ISLANDS (AUSTRALIA) 1. DOCUMENTATION (i) IUCNAVCMC Data Sheet(25 references) (ii) Additional Literature Consulted: Keage, P. 1987. Additional Protective Measures for Heard Island and the McDonald Islands. b Conserving the Natural Heritage of the Antarctic Realm. IUCN. 1991. A Strategy for Antarctic Conservation. 85 p; IUCN/SCAR. 1994. Developing The Antarctic Protected Area System. 137~. Clarke, M.R. and P. Dingwall. 1995. Conservation of Islands in the Southern Ocean. IUCN. 18Op.; Thorsell, J. 1993. Which Islands Merit World Heritage Status? Insula No 2; Dingwall, P. 1995. Ranking the World Heritage Values of Islands in the Southern Ocean. Report to IUCN 8p. (iii) Consultations: (1992 evaluation) 7 external reviewers. (Second evaluation) 5 external reviewers including members of the IUCN Antarctic Advisory Committee. (iv) Field Visit: None 2. SUMMARY OF NATURAL VALUES The Territory of Heard Island and McDonald Islands (HIMI), an external territory of Australia, consists of a remote group of islands in the Southern Ocean. The nominated property comprises the islands and all offshore rocks and shoals, out to the 12 nautical mile limit for a total area of 6,734 km’. HIM1 are limestone and volcanic accumulations located on the submarine Kerguelen Plateau. Heard Island is dominated by the Big Ben massif, with the volcanically active 2,745m Mawson Peak (the only active volcano in Australia territory). Heard Island is heavily glaciated, with ice cliffs forming a high percentageof the coastline. -
HEARD ISLAND and the Mcdonald ISLANDS: a WINDOW INTO the KERGUELEN PLATEAU
Papers and Proceedings of the Royal Society of Tasmania, Vulurne 2000 1 HEARD ISLAND AND THE McDONALD ISLANDS: A WINDOW INTO THE KERGUELEN PLATEAU by Patrick G. Quilty and Graeme Wheller (with four text.·flgures) QUILTY, P.G. & WHELLER, G.E., 2000 (30:vi): Heard Island and the McDonald Islands: a window into the Kerguelen Plateau. In Banks, MR & Brown, M.J. (Eds); HEARD ISLAND PAPERS. Pap. Proc. R. Soc. Tasm. 133(2): 1~12. ISSN 0080~4703. School of Earth Sciences, University of Tasmania, GPO Box 252-79, Hobart, Tasmania, Australia 7001 (PGQ); Volcanex International Pty Ltd, Suite 4,286 Macquarie St, South Hobart, Tasmania, Australia 7004 (GW). The modem phase of volcanism on Heard Island probably is younger than one million years and is responsible for building Big Ben, the bulk of the island. The nearby McDonald Islands are less than 100 000 years old and are volcanically active. Big Ben sits on (he Drygalski Formation, a Late Miocenc~Early Pliocene volcanic/marine sediment with glacial influence, which occurs as a generally fiat-lying, diff forming unit over most of Heard Island. The "basement" of Palaeogene limestone crops out mainly on Laurens Peninsula but also sporadically heneath Big Ben and occurs as clasts in volcanics. Historical eruptions of Heard Island, most recently from 1985 to at least 1992 and probahly later, have occurred from Mawson Peak, the summit cone built upon Big Ben, bur young lavas and ash cones afe widespread around the island. Recent volcanic activity is summarised. Heard Island and the McDonald Islands, with the Kerguelen Islands, are exposed parts of the Kerguelen Plateau, possibly the largest submarine plateau on earth, and provide geochemical and isotopic insights into the formation of oceanic plateaux, mantle plume development and the separation of Australia, India and Africa from Antarctica. -
Heard Island and Mcdonald Islands Marine Reserve Management Plan 2014–2024
Australian Antarctic Division Heard Island and McDonald Islands Marine Reserve Management Plan 2014-2024 ISBN: 978-1876934-255 This publication is available on the internet at: http://heardisland.antarctica.gov.au/ It is also available from the Department of Environment at [email protected] or freecall 1800 803 772. This publication should be cited as: Commonwealth of Australia (2014). Heard Island and McDonald Islands Marine Reserve Management Plan 2014-2024, Department of the Environment, Canberra. © Commonwealth of Australia 2014 This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non-commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and enquiries concerning reproduction and rights should be addressed to Department of the Environment, Public Affairs, GPO Box 787, Canberra ACT 2601 or email [email protected]. Disclaimer The contents of this document have been compiled using a range of source materials and are valid as at October 2014. The Australian Government is not liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of the document. All images in this publication by: Dr. Matt Curnock Contents Part 1 Foreword and acknowledgements iii Part 2 A description of the Reserve 3 Part 3 Management plan for the Reserve 13 1. Introductory Background 14 1.1 Proclamation of the Reserve 14 1.2 Conservation significance of the Reserve 14 1.3 Previous management plans 16 1.4 Structure of this management plan 16 2. -
Australian Antarctic Magazine — Issue 25: December 2013
AUSTRALIAN MAGAZINE ISSUE 25 2013 AUSTRALIAN ANTARCTIC ISSUE 2013 MAGAZINE 25 The Australian Antarctic Division, a Division of the Department of the Environment, leads Australia’s Antarctic program and seeks to advance Australia’s Antarctic interests CONTENTS in pursuit of its vision of having ‘Antarctica valued, protected and understood’. It does this by managing Australian government activity in Antarctica, providing transport and SCIENCE logistic support to Australia’s Antarctic research program, maintaining four permanent Australian research stations, and Speeding towards an acid ocean 1 conducting scientific research programs both on land and in Symphony of science 2 the Southern Ocean. Measuring phytoplankton from space 3 Australia’s Antarctic national interests are to: • Preserve our sovereignty over the Australian Antarctic Risk maps chart krill’s demise 4 Territory, including our sovereign rights over the Winter Ice Study on Key Species 6 adjacent offshore areas. • Take advantage of the special opportunities Antarctica Digging up penguin history 8 offers for scientific research. Australian Antarctic Medal Awards 9 • Protect the Antarctic environment, having regard to its special qualities and effects on our region. Penguin Barb 10 • Maintain Antarctica’s freedom from strategic and/or Promiscuous community reveals hidden values 12 political confrontation. • Be informed about and able to influence developments SCIENCE CONFERENCE in a region geographically proximate to Australia. Trans-Tasman meeting of Antarctic minds 14 • Derive any reasonable economic benefits from living and non-living resources of the Antarctic (excluding deriving From science to policy 15 such benefits from mining and oil drilling). Managing the cost of pest eradication 18 Australian Antarctic Magazine seeks to inform the Australian and international Antarctic community about the activities Hot rocks add heat to ice sheet models 20 of the Australian Antarctic program. -
Heard Island, a Case Study
BRYOPHYTE DIVERSITY AND TERRESTRIAL PLANT ECOLOGY IN THE SUBANTARCTIC : HEARD ISLAND, A CASE STUDY Dana Michelle Bergstrom B.Sc. M.Sc. A thesis submitted in fulfillment of the requirements for the degree of Doctor of Philosophy. February, 1993. School of Biological Sciences, Macquarie University. MACQUARIE UNIVERSITY HIGHER DEGREE THESIS (PhD) AUTHOR’S CONSENT This is to certify that I, being a candidate for the degree of Doctor of Philosophy am aware of the policy of the University relating to the retention and use of higher degree theses as contained in the University’s PhD Regulations generally, and in particular, Regulation 21(2). In the light of this policy and the provisions of the above Regulations, I agree to allow a copy of my thesis to be deposited in the University Library for consultation, loan and photocopying forthwith. \............ Z?5:^ ^ “Tr /Signature of Witness Signature of Candidate Dated t h i s .......................oL ... day of . 19 3 The Academic Senate on 10 August 1993 resolved that the candidate had satisfied requirements for admission to this degree. This thesis represents a major part of the prescribed program of study. Certificate of originality I hereby declare that the data and information in this thesis have not been submitted elsewhere for any other degree. Except where expressly acknowledged to the contrary in the text or acknowledgements all the work is my own. Dana Michelle Bergstrom Contents CONTENTS ABSTRACT ACKNOWLEDGMENTS CHAPTER 1 Introduction and description of environments 1.1 Introduction to the Subantarctic Zone and to this project............................................................................... ...1 1.1.1 Subantarctic Zone................................................................................................................................. ...1 1.1.2 Introduction to the project................................................................................................................. -
Climbing Big
HEARD ISLAND – THE CLIMBING OF BIG BEN — By Tim Bowden ‘Heard Island is a very threatening dawn and see the red volcanic cones make their own tent. One thing the place, the sheer malevolence of Heard and the blue lights of the glaciers and meteorologists had worked out was that Island hits you when you go … it is the snow fields going up into the there was no knowing when Big Ben essentially black and white, stark, clouds, the great cliffs and the Sooty would turn on its very occasional good because the black volcanic rock cliffs Albatross calling ... it was absolute days. Their radiosonde balloons revealed rise out of this grey seething sea and magic. And the whole year there just a ‘pretty nasty’ picture of the weather at the wind is blowing and the birds are reinforced that.’ 9000 feet, cold exposed and windy. just floating around in the gale and Béchervaise and his companions screaming. The tops of these black The OIC of the ANARE Heard Island worked out that the Abbottsmith Glacier cliffs are coated with a thick, fifty-foot station in 1953, John Béchervaise, was probably their best route to the or so layer of white glacier ice and writer, mountaineer, photographer, mountain. They found there was an ice - this disappears up into the swirling artist, teacher and historian, was fall on the glacier which they thought mists that are engulfing this great intensely aware of this magnificent they could negotiate, and thought it a mountain. When the mists clear you unclimbed peak, the lure of which good idea to lay down a depot of food, have a nine-thousand-foot mountain loomed exceeding large when the news which they could return to or take from. -
Origin and Evolution of the Sub-Antarctic Islands: the Foundation
Papers and Proceedings ofthe Royal Society of Tasmania, Volume 141 (J j, 2007 35 ORIGIN AND EVOLUTION OF THE SUB-ANTARCTIC ISLANDS: THE FOUNDATION by Patrick G. Quilty (with 23 text-figures and two tables) Quilty, P.G. 2007 (23:xi): Origin and evolution of the sub-Antarctic islands: the foundation. Papers and Proceedings ofthe Royal Society of Tasmania 141 (1): 35-58. ISSN 0080-4703. School of Earth 5ciences, University of Tasmania, Private Bag 79, Hobart, Tasmania 7001, Australia. Email: [email protected] 5ub-Antarctic islands have a diversity of origins in detail but most are volcanic and very young suggesting that they are short-lived and that the distribution would have been very different a few million years ago. "Ihey contrast with the common tourist brochure concept of oceanic islands. As the Antarctic Plate is virtually static, the islands seldom show signs of association with long-lived linear island chains and most thus stand alone. Longer-lived islands are either on submarine plateaux or are continental remnants of the dispersion of Gondwana. The islands are classified in relation to raised sea-floor, transform fault, triple junction, subduction zone, submarine plateau, submerged continent or continental. Many are difficult of access and poorly known geologically. Their geological history controls their many other roles such as sites as observatories, or for study of colonisation, evolution and speciation rates. Key Words: Sub-Antarctic islands, geological evolution, Macquarie Island, Balleny Islands, Scott Island, Campbell Island, Antipodes Island, Auckland Islands, Enderby Island, Peter I Island, Islas Diego Ramirez, South Georgia, South Sandwich Islands, Bouvetoya, Gough Island, Marion Island, Prince Edward Island, lIes Crozet, Amsterdam Island, St Paul Island, Kerguelen Plateau, lIes Kerguelen, Heard Island, McDonald Island. -
Glacier Retreat and Melt-Lake Expansion at Stephenson Glacier
Polar Record 38 (207): 297-308 (2002). Printed in the United Kingdom. 297 Glacier retreat and melt-lake expansion at Stephenson Glacier, Heard Island World Heritage Area Kevin Kiernan and Anne McConnell School of Geography and Environmental Studies, University of Tasmania, Hobart, Tasmania 7005, Australia Received September 2001 ABSTRACT. Historical records, recent observations, and geomorphological evidence indicate that rates of retreat and downwasting of the tidewater Stephenson Glacier, and concurrent expansion of ice-marginal melt-lakes, has increased by an order of magnitude since 1987. Melt-lake expansion is partly the product of greatly accelerated ablation of older, ice-cored twentieth-century moraines. The timing of these changes broadly coincides with reported increases in atmospheric and sea-surface temperatures around other sub-Antarctic islands, but correlates less well with changes along the northern Antarctic Peninsula, where warming has been more rapid. These recent changes in landscape character and geomorphological processes have implications for geodiversity, biodiversity, and cultural heritage values in this World Heritage Area. Ifthe causal climatic warming is anthropogenic, it reinforces the fact that even the most remote and little visited nature conservation reserves may be compromised by off-site human impacts, confronting management authorities with difficult philosophical and practical issues. Contents local climate. A smaller volcanic complex, Laurens Pe Introduction 297 ninsula, extends westwards from Big Ben, and Elephant Physical environment 297 Spit extends -10 km downdrift from the eastern side of the Methods 298 mountain. The mean annual temperature (MAT) recorded Results 298 between 1948 and 1954 when a permanent base was Interpretation of results 304 maintained at Atlas Cove, between Laurens Peninsula and Discussion 305 Big Ben, was 1.3°C, with a seasonal variation in tempera Conclusions 307 ture at sea level of -4°C.