Heat Flow Variations in the Antarctic Continent
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Integrated Tephrochonology Copyedited
U.S. Geological Survey and The National Academies; USGS OFR-2007-xxxx, Extended Abstract.yyy, 1- Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core N.W. Dunbar,1 W.C. McIntosh,1 A.V. Kurbatov,2 and T.I Wilch 3 1NMGB/EES Department, New Mexico Tech, Socorro NM, 87801, USA ( [email protected] , [email protected] ) 2Climate Change Institute 303 Bryand Global Sciences Center, Orono, ME, 04469, USA ([email protected]) 3Department of Geological Sciences, Albion College, Albion MI, 49224, USA ( [email protected] ) Summary Mount Berlin and Mt. Takahe, two West Antarctica volcanic centers have produced a number of explosive, ashfall generating eruptions over the past 500,000 yrs. These eruptions dispersed volcanic ash over large areas of the West Antarctic ice sheet. Evidence of these eruptions is observed at two blue ice sites (Mt. Waesche and Mt. Moulton) as well as in the Siple Dome and Byrd (Palais et al., 1988) ice cores. Geochemical correlations between tephra sampled at the source volcanoes, at blue ice sites, and in the Siple Dome ice core suggest that at least some of the eruptions covered large areas of the ice sheet with a volcanic ash, and 40 Ar/ 39 Ar dating of volcanic material provides precise timing when these events occurred. Volcanic ash from some of these events expected to be found in the WAIS Divide ice core, providing chronology and inter-site correlation. Citation: Dunbar, N.W., McIntosh, W.C., Kurbatov, A., and T.I Wilch (2007), Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10 th ISAES X, edited by A. -
Tephrochronology: Methodology and Correlations, Antarctic Peninsula Area
Tephrochronology: Methodology and correlations, Antarctic Peninsula Area Mats Molén Thesis in Physical Geography 30 ECTS Master’s Level Report passed: November 9 2012 Supervisor: Rolf Zale Tephrochronology: Methodology and correlations, Antarctic Peninsula Area Abstract Methods for tephrochronology are evaluated, in the following way: Lake sediments <500 years old from three small Antarctic lakes were analysed for identification of tephras. Subsamples were analysed for a) grain size, and identification and concentration of volcanogenic grains, b) identification of tephra horizons, c) element abundance by EPMA WDS/EDS and LA-ICP-MS, and d) possible correlations between lakes and volcanoes. Volcanogenic minerals and shards were found all through the sediment cores in all three lakes, in different abundances. A high background population of volcanogenic mineral grains, in all samples, made the identification of tephra horizons difficult, and shards could only be distinguished by certainty after chemical analysis of elements. The tephra layers commonly could not be seen by the naked eye, and, hence they are regarded as cryptotephras. Because of the small size of recent eruptions in the research area, and the travel distance of ash, most shards are small and difficult to analyse. Nine possible tephra horizons have been recorded in the three lakes, and preliminary correlations have been made. But because of analytical problems, the proposed correlations between the lakes and possible volcanic sources are preliminary. Table of contents 1. Introduction . 1 1.1. Advances and problems of tephrochronology . 1 1.1.1. General observations .. 1 1.1.2. Difficulties in tephrochronology work .. 2 1.1.3. The current research .. 4 1.2. -
Multiple Sources for Tephra from AD 1259 Volcanic Signal in Antarctic Ice
Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino To cite this version: Biancamaria Narcisi, Jean Robert Petit, Barbara Delmonte, Valentina Batanova, Joel Savarino. Mul- tiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. Quaternary Science Reviews, Elsevier, 2019, 210, pp.164-174. 10.1016/j.quascirev.2019.03.005. hal-02350371 HAL Id: hal-02350371 https://hal.archives-ouvertes.fr/hal-02350371 Submitted on 25 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Details Manuscript number JQSR_2019_21 Title MULTIPLE SOURCES FOR TEPHRA FROM AD 1259 VOLCANIC SIGNAL IN ANTARCTIC ICE CORES Abstract Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. -
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). -
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 Majestyʼs 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. -
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. -
Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs Amanda Colleen Lough Washington University in St
Washington University in St. Louis Washington University Open Scholarship All Theses and Dissertations (ETDs) Summer 9-1-2014 Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs Amanda Colleen Lough Washington University in St. Louis Follow this and additional works at: https://openscholarship.wustl.edu/etd Recommended Citation Lough, Amanda Colleen, "Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs" (2014). All Theses and Dissertations (ETDs). 1319. https://openscholarship.wustl.edu/etd/1319 This Dissertation is brought to you for free and open access by Washington University Open Scholarship. It has been accepted for inclusion in All Theses and Dissertations (ETDs) by an authorized administrator of Washington University Open Scholarship. For more information, please contact [email protected]. WASHINGTON UNIVERSITY IN ST. LOUIS Department of Earth and Planetary Sciences Dissertation Examination Committee: Douglas Wiens, Chair Jill Pasteris Philip Skemer Viatcheslav Solomatov Linda Warren Michael Wysession Studies of Seismic Sources in Antarctica Using an Extensive Deployment of Broadband Seismographs by Amanda Colleen Lough A dissertation presented to the Graduate School of Arts and Sciences of Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 2014 St. Louis, Missouri © 2014, Amanda Colleen Lough Table of Contents List of Figures ............................................................................................................................. -
Late Quaternary Volcanic Activity in Marie Byrd Land: Potential 40Ar/39Ar-Dated Time Horizons in West Antarctic Ice and Marine Cores
Late Quaternary volcanic activity in Marie Byrd Land: Potential 40Ar/39Ar-dated time horizons in West Antarctic ice and marine cores T. I. Wilch* Department of Geological Sciences, Albion College, Albion, Michigan 49224 W. C. McIntosh Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, and New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 N. W. Dunbar New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 ABSTRACT More than 12 40Ar/39Ar-dated tephra lay- ies is to determine the basal age of the ice sheet. ers, exposed in bare ice on the summit ice cap The 1968 Byrd Station ice core in the West Late Quaternary volcanic activity at three of Mount Moulton, 30 km from their inferred Antarctic Ice Sheet has an inferred basal age of major alkaline composite volcanoes in Marie source at Mount Berlin, range in age from 492 only 74 ka (Hammer et al., 1994). The exten- Byrd Land, West Antarctica, is dominated by to 15 ka. These englacial tephra layers provide sive lateral flow of ice from the ice divide area explosive eruptions, many capable of deposit- a minimum age of 492 ka for the oldest iso- to Byrd Station may have removed or disturbed ing ash layers as regional time-stratigraphic topically dated ice in West Antarctica. This much of the basal ice record. Consequently, the horizons in the West Antarctic Ice Sheet and well-dated section of locally derived glacial ice 74 ka date of the Byrd core provides only a in Southern Ocean marine sediments. -
The Antarctic Sun, December 19, 1999
On the Web at http://www.asa.org December 19, 1999 Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program Ski-plane crashes at AGO-6 By Aaron Spitzer The Antarctic Sun Two pilots escaped injury Sunday when their Twin Otter aircraft crashed during takeoff from an isolated landing site in East Antarctica. The plane, a deHavilland Twin Otter turboprop owned by Kenn Borek Air Ltd. and chartered to the U.S. Antarc- tic Program, was taking off around 3:15 p.m. Sunday when it caught a ski in the snow and tipped sideways. A wing hit the ground and the plane suffered Congratulations, it’s a helicopter! extensive damage. A New Zealand C-130 delivers a Bell 212 helicopter to the ice runway last week. The new The accident occurred on a tempo- arrival took the place of the Royal New Zealand Air Force helo used in the first part of the rary skiway at Automated Geophysical season. Photo by Ed Bowen. Observatory 6, located in Wilkes Land, about 800 miles northwest of McMurdo. The pilots had flown to the site earlier in the day from McMurdo Station to drop Testing tainted waters off two runway groomers, who were preparing the strip for the arrival of an By Josh Landis LC-130 Hercules ski-plane. The Antarctic Sun On Monday afternoon, another Kenn Borek Twin Otter, chartered to the Most scientists come to Antarctica because it gives them a chance to do their Italian Antarctic Program at Terra Nova work in the most pristine conditions on Earth. -
Volcanic Rocks of the Ross Island Area Blende Trachyte Porphyry Or of Olivine Basalt Por- Phyry
ley. This process is due to the presence of an ice- two inches, are abundant. Field observations indicate cemented layer close to the surface (usually less than that they are lag materials that weathering has freed 40 cm) and to frequent (although light) summer from the fine-grained matrix of the anorthoclase snow falls coupled with high humidity. trachyte porphyry flows. On the lower flanks of Particular attention is being paid to soil-profile Mount Erebus, in the saddle between Mounts Terra samples with respect to physical and chemical Nova and Erebus, flows of black-glassy-scoriaceous- weathering and to ionic translocations. A map is porphyritic-anorthoclase trachyte (Kenyte) occur. being prepared to correlate and define the soils, the They resemble the glassy anorthoclase trachyte of surficial geology, and the glacial history of Wright the Cape Royds area (Treves, 1962). Locally, the Valley. black trachyte porphyry overlies a grey, massive trachyte. Loose anorthoclase crystals that weathering References has released from the trachyte are also abundant. Behling, R. E. and P. E. Calkin. 1969. Chemical-physical Mount Discovery: The top of the mountain is weathering, surficial geology, and glacial history of the covered by snow and ice. There are, however, nu- Wright Valley, Victoria Land. Antarctic Journal of the merous outcrops near the summit. Some of these U.S., IV(4): 128-129. were found to consist of trachyte, basalt, and basalt Calkin, P. E., R. E. Behling, and C. Bull. 1970. Glacial porphyry. In general, the trachyte is younger than history of Wright Valley, southern Victoria Land, Ant- arctica. Antarctic Journal of the U.S., V( 1): 22-27. -
The CMS Tumbler
The CMS June Tumbler 2021 The monthly newsletter of the Cascade Mineralogical Society, Inc., Kent, Washington Connect with us! Next Meeting: Website: https://www.cascademineralogicalsociety.org Club Facebook: https://www.facebook.com/CasMinSoc/ June 10, 2021 Show Facebook: https://www.facebook.com/cascadegemandmineralshow 7:00 p.m. Instagram: https://www.instagram.com/cascadegemandmineralshow/ This month remember American Legion Hall to wish a 25406 97th Pl S Happy Birthday to Michelle Patterson on June 2 Kent, WA Leonard Bahr on June 7 Charles Benedict on June 10 The Program is about Isaac Fu on June 11 Charleen Shoemaker on June 11 Picture Stones Michael Watson on June 11 Shelley Opel on June 16 The Show & Tell Becky Patterson on June 21 Theme is something Margaret Squires on June 27 Brenda Haworth on June 29 you've done or acquired in Dick Morgan on June 29 the last 15 months and also remember to wish a Happy Anniversary to Table of Contents Calendar...........................................................3 Robert & Mrs. Waddell on June 8 (7 years) Cartoons...................................................3 & 11 From the Top of the Rock Pile.........................5 Land Use Bills..................................................5 Ice Towers........................................................7 Young Richard's Almanac................................7 Colors Around the World..................................8 May Field Trip Report.......................................9 Field Trips........................................................11 Shows..............................................................12 Except where otherwise noted, material from The Tumbler may be reprinted for non-commercial purposes, provided that the author(s) and source are acknowledged. For commercial use, the author(s) must be contacted for permission; if no contact information is given, contact them via the editor. Tips, suggestions, recipes and experiments printed in this newsletter are the experiences and/or opinions of the individuals submitting them. -
Andrill Mcmurdo Ice Shelf Project
ANDRILL MCMURDO ICE SHELF PROJECT SCIENTIFIC PROSPECTUS image courtesy Josh Landis and the National Science Foundation ANDRILL CONTRIBUTION 4 ANDRILL ISBN: 0-9723550-1-4 Additional copies of this report and other information regarding ANDRILL are available from: ANDRILL Science Management Office 126 Bessey Hall University of Nebraska – Lincoln Lincoln, NE 68588-0341 Phone: 1 + (402) 472-6723 Fax: 1 + (402) 472-6724 Please visit our website at http://andrill.org ANDRILL McMurdo Ice Shelf Project Scientific Prospectus TABLE OF CONTENTS: 1. SUMMARY 1 2. THE ANDRILL PROGRAM: BACKGROUND AND OVERVIEW 2 2.1 The McMurdo Sound Portfolio of Stratigraphic Drilling Objectives 3 3. McMURDO ICE SHELF PROJECT 4 3.1 Introduction 4 3.2 Regional Tectonic and Stratigraphic Setting 6 3.3 Site Survey and a Stratigraphic Interpretation of Target Interval 7 3.3.1 Seismic Stratigraphy 7 3.3.2 Seismic Stratigraphic Interpretation and Age Relationships: A Prognosis for ANDRILL Drilling 8 3.3.3 Faulting and Deformation 9 3.3.4 Bathymetry 9 3.3.5 Oceanography 10 3.3.6 Seafloor and Shallow Sub-seafloor Stratigraphy 10 3.4 Towards a Glacial-Interglacial Depositional Model 11 3.5 Chronostratigraphy 12 4. SCIENTIFIC OBJECTIVES 12 4.1 Overview 12 4.2 Key Climatic Questions to be Addressed 13 5. THE SCIENCE TEAM 14 6. ACKNOWLEDGEMENTS 15 7. REFERENCES 15 Co-Chief Scientists - - Tim Naish1,2 and Ross Powell3 1Institute of Geological and Nuclear Sciences P. O. Box 303068, Lower Hutt, New Zealand. 2Antarctic Research Centre, Victoria University of Wellington P. O. Box 600, Wellington, New Zealand e-mail: [email protected] phone: 64-4-570-4767 3Department of Geology and Environmental Geosciences 312 Davis Hall, Normal Rd, Northern Illinois University De Kalb, IL 60115-2854, U.S.A.