The Antarctic Sun, January 21, 2001
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THE MOUNT EREBUS TRAGEDY Air New Zealand DC10-30 ZK-NZP, Flight NZ901 Th 28 November 1979
THE MOUNT EREBUS TRAGEDY Air New Zealand DC10-30 ZK-NZP, Flight NZ901 th 28 November 1979 A REVIEW WAVERLEY PARSONS Graduate Certificate in Antarctic Studies 2003 1 TABLE OF CONTENTS ABSTRACT ................................................................................................................... 2 Introduction ................................................................................................. 3 Prelude: Before the Flight of NZ901 .......................................................... 4 Flight Preparation .......................................................................................................... 4 The Flight Path ............................................................................................................... 5 The Accident ............................................................................................... 7 Sector Whiteout ............................................................................................................. 8 Discovery of Wreckage ............................................................................................... 10 ‘Operation Overdue’ .................................................................................................... 12 The Aftermath ...........................................................................................14 The Offical Aircraft Accident Report – ‘Chippindale’s Report’ ................................. 14 The Royal Commission of Inquiry ............................................................................. -
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. -
Mcmurdo STATION MODERNIZATION STUDY Building Shell & Fenestration Study
McMURDO STATION MODERNIZATION STUDY Building Shell & Fenestration Study April 29, 2016 Final Submittal MCMURDO STATION MODERNIZATION STUDY | APRIL 29, 2016 MCMURDO STATION MODERNIZATION STUDY | APRIL 29, 2016 2 TABLE OF CONTENTS Section 1: Overview PG. 7-51 Team Directory PG. 8 Project Description PG. 9 Methodology PG. 10-11 Design Criteria/Environmental Conditions PG. 12-20 (a) General Description (b) Environmental Conditions a. Wind b. Temp c. RH d. UV e. Duration of sunlight f. Air Contaminants (c) Graphic (d) Design Criteria a. Thermal b. Air Infiltration c. Moisture d. Structural e. Fire Safety f. Environmental Impact g. Corrosion/Degradation h. Durability i. Constructability j. Maintainability k. Aesthetics l. Mechanical System, Ventilation Performance and Indoor Air Quality implications m. Structural implications PG. 21-51 Benchmarking 3 Section 2: Technical Investigation and Research PG. 53-111 Envelope Components and Assemblies PG. 54-102 (a) Components a. Cladding b. Air Barrier c. Insulation d. Vapor Barrier e. Structural f. Interior Assembly (b) Assemblies a. Roofs b. Walls c. Floors Fenestration PG. 103-111 (a) Methodology (b) Window Components Research a. Window Frame b. Glazing c. Integration to skin (c) Door Components Research a. Door i. Types b. Glazing Section 3: Overall Recommendation PG. 113-141 Total Configured Assemblies PG. 114-141 (a) Roofs a. Good i. Description of priorities ii. Graphic b. Better i. Description of priorities ii. Graphic c. Best i. Description of priorities ii. Graphic 4 (b) Walls a. Good i. Description of priorities ii. Graphic b. Better i. Description of priorities ii. Graphic c. Best i. Description of priorities ii. -
Reconstructions of Antarctic Topography Since the Eocene–Oligocene T Boundary ⁎ Guy J.G
Palaeogeography, Palaeoclimatology, Palaeoecology 535 (2019) 109346 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Reconstructions of Antarctic topography since the Eocene–Oligocene T boundary ⁎ Guy J.G. Paxmana, , Stewart S.R. Jamiesona, Katharina Hochmuthb,c, Karsten Gohlb, Michael J. Bentleya, German Leitchenkovd,e, Fausto Ferracciolif a Department of Geography, Durham University, Durham, UK b Alfred Wegener Institute Helmholtz-Center for Polar and Marine Sciences, Bremerhaven, Germany c School of Geography, Geology and the Environment, University of Leicester, Leicester, UK d Institute for Geology and Mineral Resources of the World Ocean, St. Petersburg, Russia e Institute of Earth Sciences, St. Petersburg State University, St. Petersburg, Russia f British Antarctic Survey, Cambridge, UK ABSTRACT Accurate models of past Antarctic ice sheet behaviour require realistic reconstructions of the evolution of bedrock topography. However, other than a preliminary attempt to reconstruct Antarctic topography at the Eocene–Oligocene boundary, the long-term evolution of Antarctica's subglacial topography throughout its glacial history has not previously been quantified. Here, we derive new reconstructions of Antarctic topography for four key time slices in Antarctica's climate andglacial history: the Eocene–Oligocene boundary (ca. 34 Ma), the Oligocene–Miocene boundary (ca. 23 Ma), the mid-Miocene climate transition (ca. 14 Ma), and the mid- Pliocene warm period (ca. 3.5 Ma). To reconstruct past topography, we consider a series of processes including ice sheet loading, volcanism, thermal subsidence, horizontal plate motion, erosion, sedimentation and flexural isostatic adjustment, and validate our models where possible using onshore and offshore geological constraints. Our reconstructions show that the land area of Antarctica situated above sea level was ~25% larger at the Eocene–Oligocene boundary than at the present-day. -
Polar Ice Coring and IGY 1957-58 in This Issue
NEWSLETTER OF T H E N A T I O N A L I C E C O R E L ABORATORY — S CIE N C E M A N AGE M E N T O FFICE Vol. 3 Issue 1 • SPRING 2008 Polar Ice Coring and IGY 1957-58 In this issue . An Interview with Dr. Anthony J. “Tony” Gow Polar Ice Coring and IGY 1957-58 From the early 1950’s through the mid-1960’s, U.S. polar ice coring research was led by two U.S. Army An Interview with Dr. Tony Gow .... 1 Corps of Engineers research labs: the Snow, Ice, and Permafrost Research Establishment (SIPRE), and Upcoming Meetings ...................... 2 later, the Cold Regions Research and Engineering Laboratory (CRREL). One of the high-priority research Greenland Science projects recommended by the U.S. National Academy of Sciences/National Committee for IGY 1957-58 and Education Week ..................... 3 was to deep core drill into polar ice sheets for scientific purposes. To this end, SIPRE was tasked with Ice Core Working Group developing and running the entire U.S. ice core drilling and research program. Following the successful Members ....................................... 3 pre-IGY pilot drilling trials at Site-2 NW Greenland in 1956 (305 m) and 1957 (411 m), the SIPRE WAIS Divide turned their attention to deep ice core drilling in Antarctica for IGY 1957-58. Dr. Anthony J. (Tony) Ice Core Update ............................ 5 Gow (CRREL, retired) was one of the scientists on the project. In March 2008, the NICL-SMO had Ice Cores and POLAR-PALOOZA the opportunity to sit down with Dr. -
Federal Register/Vol. 84, No. 78/Tuesday, April 23, 2019/Rules
Federal Register / Vol. 84, No. 78 / Tuesday, April 23, 2019 / Rules and Regulations 16791 U.S.C. 3501 et seq., nor does it require Agricultural commodities, Pesticides SUPPLEMENTARY INFORMATION: The any special considerations under and pests, Reporting and recordkeeping Antarctic Conservation Act of 1978, as Executive Order 12898, entitled requirements. amended (‘‘ACA’’) (16 U.S.C. 2401, et ‘‘Federal Actions to Address Dated: April 12, 2019. seq.) implements the Protocol on Environmental Justice in Minority Environmental Protection to the Richard P. Keigwin, Jr., Populations and Low-Income Antarctic Treaty (‘‘the Protocol’’). Populations’’ (59 FR 7629, February 16, Director, Office of Pesticide Programs. Annex V contains provisions for the 1994). Therefore, 40 CFR chapter I is protection of specially designated areas Since tolerances and exemptions that amended as follows: specially managed areas and historic are established on the basis of a petition sites and monuments. Section 2405 of under FFDCA section 408(d), such as PART 180—[AMENDED] title 16 of the ACA directs the Director the tolerance exemption in this action, of the National Science Foundation to ■ do not require the issuance of a 1. The authority citation for part 180 issue such regulations as are necessary proposed rule, the requirements of the continues to read as follows: and appropriate to implement Annex V Regulatory Flexibility Act (5 U.S.C. 601 Authority: 21 U.S.C. 321(q), 346a and 371. to the Protocol. et seq.) do not apply. ■ 2. Add § 180.1365 to subpart D to read The Antarctic Treaty Parties, which This action directly regulates growers, as follows: includes the United States, periodically food processors, food handlers, and food adopt measures to establish, consolidate retailers, not States or tribes. -
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. -
Ron Hartman and the Lucerne Valley Meteorites by Robert Verish Ron Hartman and the Lucerne Valley Meteorites
Meteorite Times Magazine Contents by Editor Featured Monthly Articles Accretion Desk by Martin Horejsi Jim's Fragments by Jim Tobin Meteorite Market Trends by Michael Blood Bob's Findings by Robert Verish IMCA Insights by The IMCA Team Micro Visions by John Kashuba Meteorite Calendar by Anne Black Meteorite of the Month by Editor Tektite of the Month by Editor Terms Of Use Materials contained in and linked to from this website do not necessarily reflect the views or opinions of The Meteorite Exchange, Inc., nor those of any person connected therewith. In no event shall The Meteorite Exchange, Inc. be responsible for, nor liable for, exposure to any such material in any form by any person or persons, whether written, graphic, audio or otherwise, presented on this or by any other website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. does not endorse, edit nor hold any copyright interest in any material found on any website, web page or other cyber location linked to from this website. The Meteorite Exchange, Inc. shall not be held liable for any misinformation by any author, dealer and or seller. In no event will The Meteorite Exchange, Inc. be liable for any damages, including any loss of profits, lost savings, or any other commercial damage, including but not limited to special, consequential, or other damages arising out of this service. © Copyright 2002–2011 The Meteorite Exchange, Inc. All rights reserved. No reproduction of copyrighted material is allowed by any means without prior written permission of the copyright owner. -
Mt. Erebus: Mt
8 7 Mt. Erebus Image Gallery. Image Erebus Mt. Pennycook, Jean of courtesy Photo hut. point up into the sky! the into up point and melt ice the makes steam The rock. the in Opening to an ice tower near the lower Erebus Erebus lower the near tower ice an to Opening They look like icicles that that icicles like look They cracks through sides the out comes volcano the it freezes into pillars. pillars. into freezes it of inside the from Steam hot. very is volcano moves into the cold air, air, cold the into moves the of inside the But long. year all ice and ice. When the hot steam steam hot the When ice. snow by covered is Erebus Mt. that means This forms caves made out of of out made caves forms Antarctica. near is It place. cold a is Island Ross MT. EREBUS: A SURPRISING VOLCANO SURPRISING A EREBUS: MT. VOLCANO SURPRISING A EREBUS: MT. http://beyondpenguins.nsdl.org ABOUT THE AUTHOR Jessica Fries-Gaither Issue 9: Earth’s Changing Surface Elementary Resource Specialist, (December 2008) The Ohio State University Copyright December 2008 – The Ohio State University Jessica taught at the elementary level (grades 4-6) Supported by the National and middle school (grades 5-8 math and science) Science Foundation in Memphis, TN and Anchorage, AK. Her work with MT. EREBUS: Beyond Penguins and Polar Bears involves creating Licensed Under a Creative Commons license. A SURPRISING VOLCANO and managing content for the magazine and blog. http://creativecommons.org/licenses/by-sa/3.0/ BY JESSICA FRIES-GAITHER Find this story and others at: DECEMBER 2008 http://beyondpenguins.nsdl.org/information.php?topic=stories Flesch - Kincaid RL = 3.7 13 2 60 °S ANTARCTICA like to study volcanoes, too? volcanoes, study to like about what happens deep inside it. -
Living and Working at USAP Facilities
Chapter 6: Living and Working at USAP Facilities CHAPTER 6: Living and Working at USAP Facilities McMurdo Station is the largest station in Antarctica and the southermost point to which a ship can sail. This photo faces south, with sea ice in front of the station, Observation Hill to the left (with White Island behind it), Minna Bluff and Black Island in the distance to the right, and the McMurdo Ice Shelf in between. Photo by Elaine Hood. USAP participants are required to put safety and environmental protection first while living and working in Antarctica. Extra individual responsibility for personal behavior is also expected. This chapter contains general information that applies to all Antarctic locations, as well as information specific to each station and research vessel. WORK REQUIREMENT At Antarctic stations and field camps, the work week is 54 hours (nine hours per day, Monday through Saturday). Aboard the research vessels, the work week is 84 hours (12 hours per day, Monday through Sunday). At times, everyone may be expected to work more hours, assist others in the performance of their duties, and/or assume community-related job responsibilities, such as washing dishes or cleaning the bathrooms. Due to the challenges of working in Antarctica, no guarantee can be made regarding the duties, location, or duration of work. The objective is to support science, maintain the station, and ensure the well-being of all station personnel. SAFETY The USAP is committed to safe work practices and safe work environments. There is no operation, activity, or research worth the loss of life or limb, no matter how important the future discovery may be, and all proactive safety measures shall be taken to ensure the protection of participants. -
Ellsworth Mountains Tween Depths of 54 and 85 Meters, Slightly Less Saline Conditions Are Indicated, with Freshwater Dilution of About 15 Percent
only at depths of 249 to 279 and 339 to 350 meters. having a source to the east in McMurdo Sound. The occurrence of rare (Eocene) (?) Radiolaria in Preliminary results indicate fluctuations of mineral a sample at a depth of 198.42 meters can be inter- and rock components consistent with changes in preted only as due to reworking or contamination. provenance between a Taylor Valley source and a Holes 4 and 4A, Lake Vanda (micropaleontology). Ross Sea source. Microfabric analyses are being H. Y. Ling examined 13 samples at various depths made of the diamicton units to determine fabric from 70.25 meters to approximate core bottom. strength, the assumption being that basal tills The examination failed to show Radiolaria or sili- deposited by grounded ice are likely to display coil agellates. moderate to strong fabrics whereas glacial-marine Hole 8, New Harbor (micropaleontology). H. Y. Ling drift is not likely to have a fabric. Fabrics are examined 24 samples. Radiolaria were noted at a weak or absent in most diamicton units. But they depth of about 24 meters in unit 1 (medium to are well developed between about 114 and 123 coarse sand and gravel) and between 54 and 132 meters, suggesting grounded ice. Scanning electron meters in unit 2 (diamicton). The number of speci- microscope studies of surface textures and sand mens so far recovered is too low to permit posi- grains from the core are being used as a further tive age identification of the sediments. A few aid in distinguishing grains from glacial, nongla- Eocene and Miocene forms were observed, but are cial, and mixed environments. -
No Turning Back • Rothera Fire • Kayaking the Antarctic • Summer Tours • 2003 Solar Eclipse • Tangan Expedition!
The Journal of the New Zealand Antarctic Society Vol 19, No. 2, 2001 No Turning Back • Rothera Fire • Kayaking the Antarctic • Summer Tours • 2003 Solar Eclipse • Tangan Expedition! Antarctic COVER PICTURE CONTENTS Kayaking in Antarctica SCAR Symposium Rothera Fire Plans to Locate Endurance Solar Eclipse in 2003 Cover photograph: New Zealand kayakers in the Letter to the Editor Antarctic Peninsula north of Enterprise Island. Photo: Graham Charles. The story of last season's Terrorist Attacks Affect Antarctic Planning epic trip is summarised in Antarctic, Vol. 18, no. 3 & 4, p. 58. More photographs opposite. Adventure Tourism Volume 19, No. 2, 2001 No Turning Back - Colin Monteath Issue No. 177 ANTARCTIC is published quarterly by the Over My Shoulder - Dogs on Ice New Zealand Antarctic Society Inc., ISSN 0003-5327. Please address all editorial enquiries to The Editor, NZ Antarctic Society, PO Box 404, Christchurch, or Review - A First Rate Tragedy email: [email protected]. Printed by Herald Communications, 52 Bank Street, Timaru, New Zealand. Review - Antarctica Unveiled Tribute - W. Frank Ponder Science - Tangaroa Explores Ross Sea Science - First Foucault Pendulum at Pole Antarctic Rubbish Volome 19, No. 2,2001 Antarctic NEWS Seals, Subglacial Lakes and Ultra-violet Radiation Highlights of the eighth SCAR Biology Symposium By Dr Clive Howard-Williams here were APIS, Subglacial lakes and The symposium also hosted a UV Radiation. workshop and several lectures on the The eighth SCAR international Bi The results of the Antarctic Pack Ice status of the Earth's latest unexplored ology Symposium was held in Am Seals (APIS) programme are appear large ecosystem: the sub-glacial lakes sterdam between 27 August and 5 ing in the literature, following the beneath the 3.5 km thick Antarctic ice September 2001.