WHAT's NEW in the CGA Shanghai, July 2002
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Management Plan for Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND
Management Plan For Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND 1. Description of values to be protected In 1985, two areas at Cape Bird, Ross Island were designated as SSSI No. 10, Caughley Beach (Recommendation XIII-8 (1985)) and SPA No. 20, New College Valley (Recommendation XIII-12 (1985)), following proposals by New Zealand that these areas should be protected because they contained some of the richest stands of moss and associated microflora and fauna in the Ross Sea region of Antarctica. This is the only area on Ross Island where protection is specifically given to plant assemblages and associated ecosystems. At that time, SPA No. 20 was enclosed within SSSI No. 10, in order to provide more stringent access conditions to that part of the Area. In 2000, SSSI No. 10 was incorporated with SPA No. 20 by Measure 1 (2000), with the former area covered by SPA No. 20 becoming a Restricted Zone within the revised SPA No. 20. The boundaries of the Area were revised from the boundaries in the original recommendations, in view of improved mapping and to follow more closely the ridges enclosing the catchment of New College Valley. Caughley Beach itself was adjacent to, but never a part of, the original Area, and for this reason the entire Area was renamed as New College Valley, which was within both of the original sites. The Area was redesignated by Decision 1 (2002) as Antarctic Specially Protected Area (ASPA) No. 116 and a revised Management Plan was adopted through Measure 1 (2006). -
Geology of Hut Point Peninsula, Ross Island
significantly below their Curie temperatures (approxi- Wilson, R. L., and N. D. Watkins. 1967. Correlation of mately 550°C.). petrology and natural magnetic polarity in Columbia Plateau basalts. Geophysical Journal of the Royal Astro- Previous work (Pucher, 1969; Stacey and Banerjee, nomical Society, 12(4): 405-424. 1974) indicates that the CRM intensity acquired in a low field is significantly less than the TRM intensity. It thus would appear that if a CRM induced at temperatures considerably below the Curie tempera- Geology of Hut Point Peninsula, ture, contributes a significant proportion to the ob- Ross Island served NRM intensity, too low an intensity value will be assigned to the ancient field. Although it is too early to report a firm value for PHILIP R. KYLE the intensity of the ancient field during the imprint- Department of Geology ing of unit 13 and related flows, we think that the Victoria University strength of the ambient field was more likely to Wellington, New Zealand have been about 0.5 oe (based on samples at about 141 meters) than about 0.1 oe (based on samples SAMUEL B. TREVES 122.18 and 126.06 meters). The virtual dipole Department of Geology moment (Smith, 1967b) calculated for an estimated University of Nebraska field intensity of 0.5 oe at the site is 7 X 10 25 gauss Lincoln, Nebraska 68508 cubic centimeters. This is larger than the value of 5.5 X 1025 gauss cubic centimeters (Smith, 1967b) Hut Point Peninsula is about 20 kilometers long calculated on the basis of paleointensity experiments and 2 to 4 kilometers wide. -
University Microfilms, a XEROX Company, Ann Arbor, Michigan
I I 72-15,173 BEHLING, Robert Edward, 1941- PEDOLOGICAL DEVELOPMENT ON MORAINES OF THE MESERVE GLACIER, ANTARCTICA. The Ohio State University in cooperation with Miami (Ohio) University, Ph.D., 1971 Geology University Microfilms,A XEROX Company , Ann Arbor, Michigan PEDOLOGICAL DEVELOPMENT ON MORAINES OF THE MESERVE GLACIER, ANTARCTICA DISSERTATION Presented In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert E. Behling, B.Sc., M*Sc. ***** The Ohio State University 1971 Approved by Adv Department f Geology PLEASE NOTE: Some pages have indistinct print. Filmed as received. University Microfilms, A Xerox Education Company ACKNOWLEDGEMENTS This study could not have been possible without the cooperation of faculty members of the departments of agronomy, mineralogy, and geology, I wish to thank Dr. R. P. Goldthwait as chairman of my committee, Dr. L. P. Wilding and Dr. R. T. Tettenhorst as members of my reading committee, as well as Dr. C. B. Bull and Dr. K. R. Everett for valuable assistance and criticism of the manuscript. A special thanks is due Dr. K. R. Everett for guidance during that first field season, and to Dr. F. Ugolini who first introduced me to the problems of weathering in cold deserts. Numerous people contributed to this end result through endless discussions: Dr. Lois Jones and Dr. P. Calkin receive special thanks, as do Dr. G. Holdsworth and Maurice McSaveney. Laboratory assistance was given by Mr. Paul Mayewski and R. W. Behling. Field logistic support in Antarctica was supplied by the U.S. -
Polar Geography the Historical Development of Mcmurdo Station
This article was downloaded by: [Texas A&M University] On: 19 August 2010 Access details: Access Details: [subscription number 915031382] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37- 41 Mortimer Street, London W1T 3JH, UK Polar Geography Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t781223423 The historical development of McMurdo station, Antarctica, an environmental perspective Andrew G. Kleina; Mahlon C. Kennicutt IIb; Gary A. Wolffb; Steve T. Sweetb; Tiffany Bloxoma; Dianna A. Gielstraa; Marietta Cleckleyc a Department of Geography, Texas A&M University, College Station, TX, USA b Geochemical and Environmental Research Group, Texas A&M, College Station, TX, USA c Uniondale High School, Uniondale, New York, USA To cite this Article Klein, Andrew G. , Kennicutt II, Mahlon C. , Wolff, Gary A. , Sweet, Steve T. , Bloxom, Tiffany , Gielstra, Dianna A. and Cleckley, Marietta(2008) 'The historical development of McMurdo station, Antarctica, an environmental perspective', Polar Geography, 31: 3, 119 — 144 To link to this Article: DOI: 10.1080/10889370802579856 URL: http://dx.doi.org/10.1080/10889370802579856 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. -
The Antarctic Treaty
! ! ! ! ! ! The Antarctic Treaty ! ! ! ! Measures adopted at the Thirty-ninth Consultative Meeting held at Santiago, Chile 23 May – 1 June 2016 ! ! ! ! ! ! ! ! ! ! Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty November 2017! Cm 9542 © Crown copyright 2017 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit nationalarchives.gov.uk/doc/open-government-licence/version/3 Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH ISBN 978-1-5286-0126-9 CCS1117441642 11/17 Printed on paper containing 75% recycled fibre content minimum Printed in the UK by the APS Group on behalf of the Controller of Her Majesty!s Stationery Office MEASURES ADOPTED AT THE THIRTY-NINTH ANTARCTIC TREATY CONSULTATIVE MEETING Santiago, Chile 23 May – 1 June 2016 The Measures1 adopted at the Thirty-ninth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
Flnitflrclid
flNiTflRClID A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) A New Zealand geochemist, Dr W. F. Giggenbach, descends into the inner crater of Mt Erebus on December 23 last year in an unsuccessful attempt to take gas samples. Behind him in the lava lake of the volcano where the temperature is 1000deg Celsius. On his rucksack he carries titanium gas sampling rods. Photo by Colin Monteath VOl. 8, NO. 1 1 . Wellington, New Zealand, as a magazine. o6pt61*11061% I 979I ' . SOUTH SANDWICH Is SOUTH GEORGIA f S O U T H O R K N E Y I s x \ *#****t ■ /o Orcadas arg \ - aanae s» Novolazarevskaya ussr XJ FALKLAND Is /*Signyl.uK ,,'\ V\60-W / -'' \ Syowa japan SOUTH AMERICA /'' /^ y Borga 7 s a "Molodezhnaya A SOUTH , .a /WEDDELL T\USSR SHETLAND DRONNING MAUD LAND ENOERBY \] / Halley Bay^ ununn n mMUU / I s 'SEA uk'v? COATS Ld LAND JJ Druzhnaya ^General Belgrano arg ANTARCTIC %V USSR *» -» /\ ^ Mawson MAC ROBERTSON LANO\ '■ aust /PENINSULA,' "*■ (see map below) /Sohral arg _ ■ = Davis aust /_Siple — USA Amundsen-Scott / queen MARY LAND gMirny [ELLSWORTH u s a / ; t h u s s i " LANO K / ° V o s t o k u s s r / k . MARIE BYRD > LAND WILKES LAND Scott kOSS|nzk SEA I ,*$V /VICTORIA TERRE ' •|Py»/ LAND AOEilE ,y Leningradskaya X' USSR,''' \ 1 3 -------"';BALLENYIs ANTARCTIC PENINSULA ^ v . : 1 Teniente Matienzo arg 2 Esperanza arc 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg 6 Vicecomodoro Marambio arg ' ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Presidents Frei chile * ? 500 1000 Kilometres 10 Stonington I. -
Hnjtflrcilild
HNjTflRCililD A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) Drillers on the Ross Ice Shelf last season used a new hot water system to penetrate fc. 416m of ice and gain access to the waters of the Ross Sea. Here the rig is at work on an access hole for a Norwegian science rproject. ' U . S . N a v y p h o t o Registered ol Post Office Headquarters, Vol. 8, No. 9. Wellington. New Zealand, as a magazine. SOUTH GEORGIA. •.. SOUTH SANDWICH Is' ,,r circle / SOUTH ORKNEY Is' \ $&?-""" "~~~^ / "^x AFAtKtANOis /^SiJS?UK*"0.V" ^Tl~ N^olazarevskayauss« SOUTH AMERICA / /\ ,f Borg°a ~7^1£^ ^.T, \60'E, /? cnirru „ / \ if sa / anT^^^Mo odezhnaya V/ x> SOUTH 9 .» /WEDDELL \ .'/ ' 0,X vr\uss.aT/>\ & SHETtAND-iSfV, / / Halley Bay*! DRONNING MAUD LAND ^im ^ >^ \ - / l s * S Y 2 < 'SEA/ S Euk A J COATSu k V ' tdC O A T S t d / L A N D ! > / \ Dfu^naya^^eneral Belgrano^RG y\ \ Mawson ANTARCTIC SrV MAC ROBERTSON LAND\ \ aust /PENINSULA'^ (see map below) Sobral arg / t Davis aust K- Siple ■■ [ U S A Amundsen-Scott / queen MARY LAND <JMirny AJELLSWORTH Vets') LAND °Vostok ussr MARIE BYRDNs? vice ShelA^ WIIKES tAND , ? O S S ^ . X V a n d a N z / SEA I JpY/VICTORIA .TERRE ,? ^ P o V t A N D V ^ / A D H J E j / V G E O R G E V L d , , _ / £ ^ . / ,^5s=:»iv-'s«,,y\ ^--Dumont d Urville france Leningradskaya \' / USSB_,^'' \ / -""*BALLENYIs\ / ANTARCTIC PENINSULA 1 Teniente Matienzo arg 2 Esperanza arg 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg. -
The Antarctic Sun, January 2, 2005
Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program January 2, 2005 Bye-bye biplane By Kristan Hutchison Sun staff After three winters parked Photo, poetry and prose festival on a snow berm at the South Pole, a Russian biplane is expected to fly to McMurdo next week. A dozen Russian aircraft mechanics have been work- ing around the clock since Dec. 27 to get the plane ready for its return to the air. Meanwhile, other airplane specialists and Russian jour- nalists stand by at McMurdo Station for the expected arrival of the Antonov 3T biplane on Jan. 5. So far the effort is going extremely well and the repairs are being made more quickly Ventifact and Erebus Deborah Roth than expected, said National Scenic first place Field Coordinator, Berg Field Center Science Foundation represen- Lake Fryxell, Dry Valleys, October 2004, 11 pm McMurdo Station tative George Blaisdell. The photographer of this winning entry in The Antarctic Sun Photo, Poetry and Prose “They found almost no Festival modestly claimed that “the scenery did all the work.” In that way, everyone shares See Biplane on page 13 the same advantage, with Antarctica’s stunning views inspiring us all. This year more than 80 photos and almost 40 pieces of writing were entered in the annual contest. One judge commented: “I must say that the entries get better every year.” See the other winners start- QUOTE OF THE WEEK ing on Page 9. For the best view, look at the photos in full color online at www.polar.org/antsun, where you can also download and print a calendar created from the winning entries. -
2003-2004 Science Planning Summary
2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Table of Contents Project Indexes Project Websites Station Schedules Technical Events Environmental and Health & Safety Initiatives 2003-2004 USAP Field Season Project Indexes Project websites List of projects by principal investigator List of projects by USAP program List of projects by institution List of projects by station List of projects by event number digits List of deploying team members Teachers Experiencing Antarctica Scouting In Antarctica Technical Events Media Visitors 2003-2004 USAP Field Season USAP Station Schedules Click on the station name below to retrieve a list of projects supported by that station. Austral Summer Season Austral Estimated Population Openings Winter Season Station Operational Science Opening Summer Winter 20 August 01 September 890 (weekly 23 February 187 McMurdo 2003 2003 average) 2004 (winter total) (WinFly*) (mainbody) 2,900 (total) 232 (weekly South 24 October 30 October 15 February 72 average) Pole 2003 2003 2004 (winter total) 650 (total) 27- 34-44 (weekly 17 October 40 Palmer September- 8 April 2004 average) 2003 (winter total) 2003 75 (total) Year-round operations RV/IB NBP RV LMG Research 39 science & 32 science & staff Vessels Vessel schedules on the Internet: staff 25 crew http://www.polar.org/science/marine. 25 crew Field Camps Air Support * A limited number of science projects deploy at WinFly. 2003-2004 USAP Field Season Technical Events Every field season, the USAP sponsors a variety of technical events that are not scientific research projects but support one or more science projects. -
Volcanic Activity of Mount Erebus, 1981-1982
believe they are related to the depth, energy release, and mech- infrasound signals, the former representing explosions. There anism of various types of eruptions that are transitional be- is a tendency for the epicenter to scatter along an east-west tween the two end members, that is, between less violent gas trend across the summit of Mount Erebus, parallel to the emissions (roar, without explosive onset) and more violent, Erebus-Terra Nova-Terrror volcanic axis. This trend was also sharp explosions (bang, explosive onset). These source charac- observed in the previous season (1980-81) (Takanami et al. teristics are being investigated by the New Zealand and Jap- 1981). The data suggest that the feeder dike or dikes of the anese team members (e.g., Dibble 1981). Mount Erebus lava lake may have an east-west orientation. A positive correlation of signals seen on the figure-eight in- In summary, over the past 2 years we have observed a high duction loop with volcanic explosions has been noted. The level of very-small-magnitude earthquake activity associated origin of these signals could be twofold: (1) eruption of con- with volcanic processes near the summit of Mount Erebus. ducting magma or ionized gas in the Earths static magnetic Swarm-type activity is typical. An unresolved question is field, and (2) expansion of the area enclosed by the wire loop as whether or not the few events occurring on the outer flanks of the summit crater dilates during explosions. We do not know the Erebus volcano are truly tectonic or are icequakes. Fang yet which of these processes is more important. -
Nan Ummsmmm a N E W S B U L L E T I N
nan UmmSmmm A N E W S B U L L E T I N p u b l i s h e d q u a r t e r l y b y t h e NEW ZEALAND ANTARCTIC SOCIETY (INC) BORGA BASE. A WINTERING STATION OF THE SOUTH AFRICAN NATIONAL ANTARCTIC EXPEDITION IN WESTERN QUEEN MAUD LAND. ESTABLISHED IN MAY. 1969' THE BASE IS 350 KILOMETRES SOUTH OF THE MAIN BASE. SANAE. IT WAS BUILT AT A HEIGHT OF 7920FT IN THE BORGE MASSIF. NEAR THE HULDRESLOITTET NUNATAK, AND IS LOCATED AT 72 DEG 50 MIN S - 3DEG 48 MIN W. South African Geological Survey Photo | '.▶'Hev*^ ■ w. ■_■_ /+:-£*&■ ' •Tf*^*' Registered at Post Office Headquarters. Vol. 7. No. 1 Wellington, New Zealand, as a magazine. March, 1974 e-.i.-. M' AUSTRALIA CHRISTCHURCH NEW ZEALAND TASMANIA /^WsDEPENDENcy^. v£ft\ \**° \ 'Sis \ / - V\ . H i lt l e t te f U ! . ) /y . \\(nz) w |X XrS8* •V, / Byrd (US)* ANTARCTICA, Alferei Sobral (Arg)* />*> -toa \ - ^ING mauo\ « Molodyozhnaya^'^. VO/?way * xA ass** (USSR) (USSR)/^ * I B o r g M a s s i f \ <^*/SI{ny I (UK) DRAWN BY DEPARTMENT OF LANDS 4 SURVEY WELLINGTON. NEW ZEALAND. AUG 1969 3rd EDITION vrii::.T■ e<ui^*[PiiLB(S1Fa(B*d (Successor to "Antarctic News Bulletin") Vol. 7. No. 1 73rd Issue Editor: J. M. CAFFIN, 35 Chepstow Avenue, Christchurch 5. Address all contributions, enquiries, etc., to-the Editor. All Business Communications, Subscriptions, etc., to: Secretary, New Zealand Antarctic Society (Inc.), P.O. Box 1223, Christchurch, N.Z. CONTENTS ARTICLES POLAR CRIMINAL LAW 27, 28, 29 QUAIL ISLAND 31, 32 POLAR ACTIVITIES NEW ZEALAND 2, 3, 4, 5, 6, 7, 8 UNITED KINGDOM 9, 10, 11 AUSTRALIA 19, 20, 21, 22 UNITED STATES 12, 13, 14, 15, 16, 17, 18 SOVIET UNION 30 FRANCE 23, 24 SOUTH AFRICA 25, 26 ARGENTINE ITALY GENERAL TOURISM OBITUARY THE READER WRITES ANTARCTIC BOOKSHELF 34, 35, 36 Winter is always cold in Antarctica; this year it will be colder for the men living there. -
Ross Island Trail System Mcmurdo Station & Scott Base, Antarctica
Ross Island Trail System McMurdo Station & Scott Base, Antarctica Ross Island Trail System Recreational Routes CAL Seasonal Trail Please visit the McMurdo Intranet eFoot Plan site for further route information (route marked with trail signs) markers in mi (km): e.g. 1.22 (1.96) CRL Castle Rock Loop Trail & CRS Castle Rock Summit Trail (9.65 mi / 15.53 km) (0.1 mi / 0.17 km) IR Access Road (shared with vehicles) CRS This trip leads to the prominent landform called Castle Rock, named for its buttress-like shape. The Castle Rock routes are the most ambitious hikes, ski or runs in the McMurdo area. As you traverse across the snow and ice field, you see the prominent 0.11 (0.17) landform of Castle Rock ahead, spectacular views to the north, and the Transantarctic Mountains to the east. The route is also Castle Rock a large loop that extends to Castle Rock and ends at Scott Base. More adventurous hikers may want to attempt the Castle Rock Restricted Road Summit route. This route entails scrambling, exposed rock faces and the use of a fixed line as a handhold and should never be (no recreational travel) attempted without an experienced person in your group. The Castle Rock Summit is only open at certain periods due to safety CASTLE ROCK FALL CRL concerns. January 30, 1995 Check-in/Check-out 1 death (Building 182 Firehouse) HPR Hut Point Ridge Loop Trail 1.33 (2.13) (2.63 mi / 4.24 km) The Hut Point Ridge Loop Trail is one of the newest additions to recreation opportunities in the Ross Island area.