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Ferraccioli Etal2008.Pdf
Tectonophysics 478 (2009) 43–61 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Magmatic and tectonic patterns over the Northern Victoria Land sector of the Transantarctic Mountains from new aeromagnetic imaging F. Ferraccioli a,⁎, E. Armadillo b, A. Zunino b, E. Bozzo b, S. Rocchi c, P. Armienti c a British Antarctic Survey, Cambridge, UK b Dipartimento per lo Studio del Territorio e delle Sue Risorse, Università di Genova, Genova, Italy c Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy article info abstract Article history: New aeromagnetic data image the extent and spatial distribution of Cenozoic magmatism and older Received 30 January 2008 basement features over the Admiralty Block of the Transantarctic Mountains. Digital enhancement Received in revised form 12 November 2008 techniques image magmatic and tectonic features spanning in age from the Cambrian to the Neogene. Accepted 25 November 2008 Magnetic lineaments trace major fault zones, including NNW to NNE trending transtensional fault systems Available online 6 December 2008 that appear to control the emplacement of Neogene age McMurdo volcanics. These faults represent splays from a major NW–SE oriented Cenozoic strike-slip fault belt, which reactivated the inherited early Paleozoic Keywords: – Aeromagnetic anomalies structural architecture. NE SW oriented magnetic lineaments are also typical of the Admiralty Block and fl Transantarctic Mountains re ect post-Miocene age extensional faults. To re-investigate controversial relationships between strike-slip Inheritance faulting, rifting, and Cenozoic magmatism, we combined the new aeromagnetic data with previous datasets Cenozoic magmatism over the Transantarctic Mountains and Ross Sea Rift. -
Review of the Geology and Paleontology of the Ellsworth Mountains, Antarctica
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 107; doi:10.3133/of2007-1047.srp107 Review of the geology and paleontology of the Ellsworth Mountains, Antarctica G.F. Webers¹ and J.F. Splettstoesser² ¹Department of Geology, Macalester College, St. Paul, MN 55108, USA ([email protected]) ²P.O. Box 515, Waconia, MN 55387, USA ([email protected]) Abstract The geology of the Ellsworth Mountains has become known in detail only within the past 40-45 years, and the wealth of paleontologic information within the past 25 years. The mountains are an anomaly, structurally speaking, occurring at right angles to the Transantarctic Mountains, implying a crustal plate rotation to reach the present location. Paleontologic affinities with other parts of Gondwanaland are evident, with nearly 150 fossil species ranging in age from Early Cambrian to Permian, with the majority from the Heritage Range. Trilobites and mollusks comprise most of the fauna discovered and identified, including many new genera and species. A Glossopteris flora of Permian age provides a comparison with other Gondwana floras of similar age. The quartzitic rocks that form much of the Sentinel Range have been sculpted by glacial erosion into spectacular alpine topography, resulting in eight of the highest peaks in Antarctica. Citation: Webers, G.F., and J.F. Splettstoesser (2007), Review of the geology and paleontology of the Ellsworth Mountains, Antarctica, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K. Cooper and C.R. Raymond et al., USGS Open- File Report 2007-1047, Short Research Paper 107, 5 p.; doi:10.3133/of2007-1047.srp107 Introduction The Ellsworth Mountains are located in West Antarctica (Figure 1) with dimensions of approximately 350 km long and 80 km wide. -
Antarctic Peninsula
Hucke-Gaete, R, Torres, D. & Vallejos, V. 1997c. Entanglement of Antarctic fur seals, Arctocephalus gazella, by marine debris at Cape Shirreff and San Telmo Islets, Livingston Island, Antarctica: 1998-1997. Serie Científica Instituto Antártico Chileno 47: 123-135. Hucke-Gaete, R., Osman, L.P., Moreno, C.A. & Torres, D. 2004. Examining natural population growth from near extinction: the case of the Antarctic fur seal at the South Shetlands, Antarctica. Polar Biology 27 (5): 304–311 Huckstadt, L., Costa, D. P., McDonald, B. I., Tremblay, Y., Crocker, D. E., Goebel, M. E. & Fedak, M. E. 2006. Habitat Selection and Foraging Behavior of Southern Elephant Seals in the Western Antarctic Peninsula. American Geophysical Union, Fall Meeting 2006, abstract #OS33A-1684. INACH (Instituto Antártico Chileno) 2010. Chilean Antarctic Program of Scientific Research 2009-2010. Chilean Antarctic Institute Research Projects Department. Santiago, Chile. Kawaguchi, S., Nicol, S., Taki, K. & Naganobu, M. 2006. Fishing ground selection in the Antarctic krill fishery: Trends in patterns across years, seasons and nations. CCAMLR Science, 13: 117–141. Krause, D. J., Goebel, M. E., Marshall, G. J., & Abernathy, K. (2015). Novel foraging strategies observed in a growing leopard seal (Hydrurga leptonyx) population at Livingston Island, Antarctic Peninsula. Animal Biotelemetry, 3:24. Krause, D.J., Goebel, M.E., Marshall. G.J. & Abernathy, K. In Press. Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science.Leppe, M., Fernandoy, F., Palma-Heldt, S. & Moisan, P 2004. Flora mesozoica en los depósitos morrénicos de cabo Shirreff, isla Livingston, Shetland del Sur, Península Antártica, in Actas del 10º Congreso Geológico Chileno. -
USGS Open-File Report 2007-1047, Short Research Paper 075, 4 P.; Doi: 10.3133/Of2007-1047.Srp075
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 075, doi:10.3133/of2007-1047.srp075 Aeromagnetic search for Cenozoic magmatism over the Admiralty Mountains Block (East Antarctica) 1 2 3 4 5 6 E. Armadillo, F. Ferraccioli, A. Zunino, E. Bozzo, S. Rocchi, and P. Armienti 1Dipartimento per lo Studio del Territorio e delle Sue Risorse, Università di Genova, V.le Benedetto XV 5,16132 Genova, Italy ([email protected]) 2British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 OET, UK ([email protected]) 3Dipartimento per lo Studio del Territorio e delle Sue Risorse, Università di Genova, V.le Benedetto XV 5,16132 Genova, Italy ([email protected]) 4Dipartimento per lo Studio del Territorio e delle Sue Risorse, Università di Genova, V.le Benedetto XV 5,16132 Genova, Italy ([email protected]) 5Dipartimento di Scienze della Terra, Università di Pisa, Via di S. Maria 53-56126, Pisa, Italy ([email protected]) 6Dipartimento di Scienze della Terra, Università di Pisa, Via di S. Maria 53-56126, Pisa, Italy ([email protected]) Abstract Cenozoic magmatic rocks of the Transantarctic Mountains provide an important window on the tectonic and magmatic processes of the West Antarctic Rift System. Previous aeromagnetic investigations in northern Victoria Land have delineated Cenozoic volcanic and intrusive complexes assigned to the McMurdo Volcanic Group and Meander Intrusives over the Transantarctic Mountains. We present a new aeromagnetic anomaly map for the region north of the Mariner Glacier to study the extent and spatial distribution of these Cenozoic rocks over the previously unexplored Admiralty Mountains. -
PDF-TITEL-AA-CHILE-EMPEORSADVENTURE Kopie.Pages
Antarktis Flug-Expeditionen EMPEROR PENGUINS Besuch der Kaiserpinguin-Kolonie in der Gould-Bucht ex Punta Arenas / Chile via Basecamp Union Glaciar POLARADVENTURES Schiffs- und Flug-Expeditionen in Arktis und Antarktis Reiseagentur Heinrich-Böll-Str. 40 * D-21335 Lüneburg * Deutschland Tel +49-4131- 223474 Fax +49-4131-54255 [email protected] www.polaradventures.de Saison 2021/22 Veranstalter Direkt-Angebote ab-bis Punta Arenas (Chile) für individuelle Planungen alle Abfahrten der Saison inkl. englischsprachiger Termine POLARADVENTURES Schiffs- und Flug-Expeditionen in Arktis und Antarktis Reiseagentur * Heinrich-Böll-Str. 40 * D-21335 Lüneburg * Deutschland Tel +49-4131- 223474 Fax +49-4131-54255 [email protected] www.polaradventures.de EMPEROR PENGUINS A PHOTOGRAPHER’S PARADISE Immerse yourself in the sights and sounds of the Gould Bay Emperor Penguin Colony on the remote coast of the Weddell Sea. Camp on the same sea ice where thousands of birds come to raise and feed their young. Photograph majestic emperors and their chicks against a spectacular backdrop of ice cliffs, pressure ridges, and icebergs. Spot petrels and seals amongst the endless white expanse. Fall asleep to a chorus of trumpeting calls and wake to find curious penguins outside your tent. Our remote field camp offers you unparalleled access to the emperors as you witness their amazing adaptations to the Antarctic environment alongside our expert guides. ITINERARY Arrival Day Punta Arenas, Chile Pre-departure Day Luggage Pick-Up & Briefing Day 1 Fly to Antarctica Day 2 Explore Union Glacier Day 3 Fly to Emperor Colony Day 4-6 Live with the Emperors Day 7 Return to Union Glacier Day 8 Explore Union Glacier Day 9 Return to Chile Flexible Departure Day Fly Home *Subject to change based on weather and flight conditions. -
Station Sharing in Antarctica
IP 94 Agenda Item: ATCM 7, ATCM 10, ATCM 11, ATCM 14, CEP 5, CEP 6b, CEP 9 Presented by: ASOC Original: English Station Sharing in Antarctica 1 IP 94 Station Sharing in Antarctica Information Paper Submitted by ASOC to the XXIX ATCM (CEP Agenda Items 5, 6 and 9, ATCM Agenda Items 7, 10, 11 and 14) I. Introduction and overview As of 2005 there were at least 45 permanent stations in the Antarctic being operated by 18 countries, of which 37 were used as year-round stations.i Although there are a few examples of states sharing scientific facilities (see Appendix 1), for the most part the practice of individual states building and operating their own facilities, under their own flags, persists. This seems to be rooted in the idea that in order to become a full Antarctic Treaty Consultative Party (ATCP), one has to build a station to show seriousness of scientific purpose, although formally the ATCPs have clarified that this is not the case. The scientific mission and international scientific cooperation is nominally at the heart of the ATS,ii and through SCAR the region has a long-established scientific coordination body. It therefore seems surprising that half a century after the adoption of this remarkable Antarctic regime, we still see no truly international stations. The ‘national sovereign approach’ continues to be the principal driver of new stations. Because new stations are likely to involve relatively large impacts in areas that most likely to be near pristine, ASOC submits that this approach should be changed. In considering environmental impact analyses of proposed new station construction, the Committee on Environmental Protection (CEP) presently does not have a mandate to take into account opportunities for sharing facilities (as an alternative that would reduce impacts). -
Number 90 RECORDS of ,THE UNITED STATES ANTARCTIC
~ I Number 90 RECORDS OF ,THE UNITED STATES ANTARCTIC SERVICE Compiled by Charles E. Dewing and Laura E. Kelsay j ' ·r-_·_. J·.. ; 'i The National Archives Nat i on a 1 A r c hive s and R e c o rd s S e r vi c e General Services~Administration Washington: 1955 ---'---- ------------------------ ------~--- ,\ PRELIMINARY INVENTORY OF THE RECORDS OF THE UNITED STATES ANTARCTIC SERVICE {Record Group 1 Z6) Compiled by Charles E. Dewing and Laura E. Kelsay The National Archives National Archives and Records Service General Services Administration Washington: 1955 National Archives Publication No. 56-8 i\ FORENORD To analyze and describe the permanently valuable records of the Fed eral Government preserved in the National Archives Building is one of the main tasks of the National Archives. Various kinds of finding aids are needed to facilitate the use of these records, and the first step in the records-description program is the compilation of preliminary inventories of the material in the 270-odd record groups to which the holdings of the National Archives are allocated. These inventories are called "preliminary" because they are provisional in character. They are prepared.as soon as possible after the records are received without waiting to screen out all disposable material or to per fect the arrangement of the records. They are compiled primarily for in ternal use: both as finding aids to help the staff render efficient refer ence service and as a means of establishing administrative control over the records. Each preliminary inventory contains an introduction that briefly states the history and fUnctions of the agency that accumulated the records. -
Mcmurdo Dry Valleys, Southern Victoria Land
Measure 1 (2004) Annex Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND 1. Description of values to be protected and activities to be managed The McMurdo Dry Valleys are characterized as the largest relatively ice-free region in Antarctica with approximately thirty percent of the ground surface largely free of snow and ice. The region encompasses a cold desert ecosystem, whose climate is not only cold and extremely arid (in the Wright Valley the mean annual temperature is –19.8°C and annual precipitation is less than 100 mm water equivalent), but also windy. The landscape of the Area contains glaciers, mountain ranges, ice-covered lakes, meltwater streams, arid patterned soils and permafrost, sand dunes, and interconnected watershed systems. These watersheds have a regional influence on the McMurdo Sound marine ecosystem. The Area’s location, where large-scale seasonal shifts in the water phase occur, is of great importance to the study of climate change. Through shifts in the ice-water balance over time, resulting in contraction and expansion of hydrological features and the accumulations of trace gases in ancient snow, the McMurdo Dry Valley terrain also contains records of past climate change. The extreme climate of the region serves as an important analogue for the conditions of ancient Earth and contemporary Mars, where such climate may have dominated the evolution of landscape and biota. The Area is characterized by unique ecosystems of low biodiversity and reduced food web complexity. However, as the largest ice-free region in Antarctica, the McMurdo Dry Valleys also contain relatively diverse habitats compared with other ice-free areas. -
Mapping Blue-Ice Areas and Crevasses in West Antarctica Using ASTER Images, GPS, and Radar Measurements
CHAPTER 31 Mapping blue-ice areas and crevasses in West Antarctica using ASTER images, GPS, and radar measurements Andre´s Rivera, Fiona Cawkwell, Anja Wendt, and Rodrigo Zamora ABSTRACT from ASTER imagery, with the aim of identifying other landing sites for aircraft, as well as providing Before the satellite era, relatively little was known a detailed map for meteorite seekers. ASTER com- about the interior of the West Antarctic Ice Sheet posite images have also been used to map safe (WAIS). Of special interest are the rock outcrops routes for terrestrial traverses through crevasse associated with blue-ice areas (BIAs), which have zones. High-pass filters enhanced crevasse features, been exploited for logistical purposes as well as but visual analysis proved to be the most reliable being the subject of scientific research. The blue method of identifying all crevasses. ASTER images ice consists of relatively snow-free glacier ice that were superior to microwave imagery for crevasse is undergoing ablation. detection, as the latter can lack sufficient contrast; One of these BIAs is Patriot Hills (80180S, however, only Radarsat imagery provided coverage 81220W) where aircraft with conventional landing of higher latitude regions. Information gleaned gear have been landing for more than 20 years. This from visible imagery can be combined with that is now the main hub supporting large terrestrial of field-based radio-echo sounding and ground- expeditions conducted by Chilean scientists within penetrating radar profiles through the ice to map Antarctica. Kinematic GPS has been used to map internal layers and bedrock topography with the BIAs since 1996, with areas delineated on ASTER objective of enhancing our knowledge of this images since 2001 using both manual and auto- remote region. -
Nsf.Gov OPP: Report of the U.S. Antarctic Program Blue Ribbon
EXECUTIVE SUMMARY MORE AND BETTER SCIENCE IN ANTARCTICA THROUGH INCREASED A LOGISTICAL EFFECTIVENESS Report of the U.S. Antarctic Program Blue Ribbon Panel Washington, D.C. July 23, 2012 This booklet summarizes the report of the U.S. Antarctic Program Blue Ribbon Panel, More and Better Science in Antarctica Through Increased Logistical Effectiveness. The report was completed at the request of the White House office of science and Technology Policy and the National Science Foundation. Copies of the full report may be obtained from David Friscic at [email protected] (phone: 703-292-8030). An electronic copy of the report may be downloaded from http://www.nsf.gov/ od/opp/usap_special_review/usap_brp/rpt/index.jsp. Cover art by Zina Deretsky. Front and back inside covers showing McMurdo’s Dry Valleys in Antarctica provided by Craig Dorman. CONTENTS Introduction ............................................ 1 The Panel ............................................... 2 Overall Assessment ................................. 3 U.S. Facilities in Antarctica ....................... 4 The Environmental Challenge .................... 7 Uncertainties in Logistics Planning ............. 8 Activities of Other Nations ....................... 9 Economic Considerations ....................... 10 Major Issues ......................................... 11 Single-Point Failure Modes ..................... 17 Recommendations ................................. 18 Concluding Observations ....................... 21 U.S. ANTARCTIC PROGRAM BLUE RIBBON PANEL WASHINGTON, -
JOURNAL Number Six
THE JAMES CAIRD SOCIETY JOURNAL Number Six Antarctic Exploration Sir Ernest Shackleton MARCH 2012 1 Shackleton and a friend (Oliver Locker Lampson) in Cromer, c.1910. Image courtesy of Cromer Museum. 2 The James Caird Society Journal – Number Six March 2012 The Centennial season has arrived. Having celebrated Shackleton’s British Antarctic (Nimrod) Expedition, courtesy of the ‘Matrix Shackleton Centenary Expedition’, in 2008/9, we now turn our attention to the events of 1910/12. This was a period when 3 very extraordinary and ambitious men (Amundsen, Scott and Mawson) headed south, to a mixture of acclaim and tragedy. A little later (in 2014) we will be celebrating Sir Ernest’s ‘crowning glory’ –the Centenary of the Imperial Trans-Antarctic (Endurance) Expedition 1914/17. Shackleton failed in his main objective (to be the first to cross from one side of Antarctica to the other). He even failed to commence his land journey from the Weddell Sea coast to Ross Island. However, the rescue of his entire team from the ice and extreme cold (made possible by the remarkable voyage of the James Caird and the first crossing of South Georgia’s interior) was a remarkable feat and is the reason why most of us revere our polar hero and choose to be members of this Society. For all the alleged shenanigans between Scott and Shackleton, it would be a travesty if ‘Number Six’ failed to honour Captain Scott’s remarkable achievements - in particular, the important geographical and scientific work carried out on the Discovery and Terra Nova expeditions (1901-3 and 1910-12 respectively). -
A News Bulletin New Zealand, Antarctic Society
A NEWS BULLETIN published quarterly by the NEW ZEALAND, ANTARCTIC SOCIETY INVETERATE ENEMIES A penguin chick bold enough to frighten off all but the most severe skua attacks. Photo: J. T. Darby. Vol. 4. No.9 MARCH. 1967 AUSTRALIA WintQr and Summer bAsts Scott Summer ila..se enly t Hal'ett" Tr.lnsferrea ba.se Will(,t~ U.S.foAust T.mporArily nen -eper&tianaJ....K5yow... •- Marion I. (J.A) f.o·W. H.I.M.S.161 O_AWN IY DEPARTMENT OF LANDS fa SU_VEY WILLINGTON) NEW ZEALAND! MAR. .•,'* N O l. • EDI"'ON (Successor to IIAntarctic News Bulletin") Vol. 4, No.9 MARCH, 1967 Editor: L. B. Quartermain, M.A., 1 Ariki Road, Wellington, E.2, ew Zealand. Assistant Editor: Mrs R. H. Wheeler. Business Communications, Subscriptions, etc., to: Secretary, ew Zealand Antarctic Society, P.O. Box 2110, Wellington, .Z. CONTENTS EXPEDITIONS Page New Zealand 430 New Zealand's First Decade in Antarctica: D. N. Webb 430 'Mariner Glacier Geological Survey: J. E. S. Lawrence 436 The Long Hot Summer. Cape Bird 1966-67: E. C. Young 440 U.S.S.R. ...... 452 Third Kiwi visits Vostok: Colin Clark 454 Japan 455 ArgenHna 456 South Africa 456 France 458 United Kingdom 461 Chile 463 Belgium-Holland 464 Australia 465 U.S.A. ...... 467 Sub-Antarctic Islands 473 International Conferences 457 The Whalers 460 Bookshelf ...... 475 "Antarctica": Mary Greeks 478 50 Years Ago 479 430 ANTARCTI'C March. 1967 NEW ZEALAND'S FIRST DECAD IN ANTARCTICA by D. N. Webb [The following article was written in the days just before his tragic death by Dexter Norman Webb, who had been appointed Public ReLations Officer, cott Base, for the 1966-1967 summer.