Shackleton Range Traverse Lock Back for This Work
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fifth World Forestry Congress
Proceedings of the Fifth World Forestry Congress VOLUME 1 RE University of Washington, Seattle, Washington United States of America August 29September 10, 1960 The President of the United States of America DWIGHT D. EISENHOWER Patron Fifth World Forestry Congress III Contents VOLUME 1 Page Chapter1.Summary and Recommendations of the Congress 1 Chapter 2.Planning for the Congress 8 Chapter3.Local Arrangements for the Congress 11 Chapter 4.The Congress and its Program 15 Chapter 5.Opening Ceremonies 19 Chapter6. Plenary Sessions 27 Chapter 7.Special Congress Events 35 Chapitre 1.Sommaire et recommandations du Congrès 40 Chapitre 2.Preparation des plans en vue du Congrès 48 Chapitre 3.Arrangements locaux en vue du Congrès 50 Chapitre 4.Le Congrès et son programme 51 Chapitre 5.Cérémonies d'ouverture 52 Chapitre 6.Seances plénières 59 Chapitre 7.Activités spéciales du Congrès 67 CapItullo1. Sumario y Recomendaciones del Congreso 70 CapItulo 2.Planes para el Congreso 78 CapItulo 3.Actividades Locales del Congreso 80 CapItulo 4.El Congreso y su Programa 81 CapItulo 5.Ceremonia de Apertura 81 CapItulo 6.Sesiones Plenarias 88 CapItulo 7.Actos Especiales del Congreso 96 Chapter8. Congress Tours 99 Chapter9.Appendices 118 Appendix A.Committee Memberships 118 Appendix B.Rules of Procedure 124 Appendix C.Congress Secretariat 127 Appendix D.Machinery Exhibitors Directory 128 Appendix E.List of Financial Contributors 130 Appendix F.List of Participants 131 First General Session 141 Multiple Use of Forest Lands Utilisation multiple des superficies boisées Aprovechamiento Multiple de Terrenos Forestales Second General Session 171 Multiple Use of Forest Lands Utilisation multiple des superficies boisées Aprovechamiento Multiple de Terrenos Forestales Iv Contents Page Third General Session 189 Progress in World Forestry Progrés accomplis dans le monde en sylviculture Adelantos en la Silvicultura Mundial Section I.Silviculture and Management 241 Sessions A and B. -
Friedrich-Alexander Universität Erlangen-Nürnberg
Petrologische und Geochemische Untersuchungen an ultramafischen und mafischen Gesteinen der Shackleton Range, Ost-Antarktis Zeugen des Zusammenschlusses Gondwanas und letzte Relikte eines einstigen Ozeans? Der Naturwissenschaftlichen Fakultät/ Dem Fachbereich Geographie und Geowissenschaften der Friedrich-Alexander-Universität Erlangen-Nürnberg zur Erlangung des Doktorgrades Dr. rer. Nat. vorgelegt von Tanja Romer aus Illertissen i Als Dissertation genehmigt von der Naturwissenschaftlichen Fakultät/ vom Fachbereich Geographie und Geowissenschaften der Friedrich-Alexander-Universität Erlangen-Nürnberg Tag der mündlichen Prüfung: 01.06.2017 Vorsitzende/r des Promotionsorgans: Prof. Dr. Georg Kreimer Gutachter/in: Prof. Dr. Esther Schmädicke Prof. Dr. Reiner Klemd ii Zusammenfassung Im östlichen Teil der Antarktis liegt die Shackleton Range. Es handelt sich hierbei um ein Kollisionsorogen, das nach heutigen Erkenntnissen der panafrikanischen Orogenese zugeordnet wird. Hinweise darauf finden sich im nördlichen Bereich (z.B. Haskard Highlands) der Shackleton Range. Hier treten granatführende, ultramafische Gesteine als Linsen, eingeschlossen in hochgradig metamorphen Gneisen auf. Die Linsen setzen sich hauptsächlich aus granat- und/oder spinell-führenden Pyroxeniten und untergeordnet auch Peridotiten zusammen. Die nähere Umgebung der Linsen wird vor allem durch Amphibolite dominiert. Die Pyroxenite enthalten teilweise eine Verwachsung von Granat und Olivin und sind damit ein eindeutiger Indikator für eine eklogitfazielle Metamorphose in diesem Bereich. Weiterhin zeugen sie als ultramafische Gesteine von einer möglichen Suturzone. In dieser Forschungsarbeit konnte mittels Mikrosondenanalytik an Granat, Ortho- und Klinopyroxen, Spinell, Olivin und Amphibol für die ultramafischen Gesteine ein Teil des im Uhrzeigersinn verlaufenden P-T-Pfads rekonstruiert werden. Thermobarometrische Berechnungen ergaben maximale Metamorphosetemperaturen von 800 bis 850 °C. Die maximal erreichten Drücke dürften zwischen 20 bis 23 kbar gelegen haben. -
Petrogenesis of the Metasediments from the Pioneers Escarpment, Shackleton Range, Antarctica
Polarforschung 63 (2/3): 165-182,1993 (erschienen 1995) Petrogenesis of the Metasediments from the Pioneers Escarpment, Shackleton Range, Antarctica By Norbcrt W. Roland', Martin Olcsch2 and Wolfgang Schubert' Summary: During the GEISHA expedition (Geologische Expedition in die during apre-Ross metarnorphic event or orogeny. The Ross Orogeny at about Shackleton Range 1987/88), the Pioneers Escarpment was visited and sampled 500 Ma probably just led to the weak greensehrst facies overprint that is evi extensively for the first time. Most of the rock types eneountered represent dent in the rocks of the Pioneers Group. amphibolite faeies metamorphics, but evidence for granulite facies conditions was found in cores of garnet. These conelitions must have been at least partly Finally, sedimentation resumed in the area of the present Shacklcton Range, or reached during the peak of metamorphism. at least in the eastern part of the Pioneers Escarpment, probably when detritus from erosion of the basement (Read Group and Pioneers Group) was deposi For the Pioneers Escarpment a varicolored succession of sedimentary anel bi ted, forming sandstones and greywackes of possibly Jurassie age. There is no modal volcanic origin is typical. It comprises: indication that these sediments belong to the former Turnpike Bluff Group. quartzites muscovite quartzite, sericite quartzite, fuchsite quartzite, garnet quartz schists etc.; Zusammenfassung: Während GEISHA (Geologische Expedition in die Shack pelites: mica schists and plagiocJase 01' plagioclase-microcline gneisses, alu leton Range 1987/88) wurde erstmals das Pioneers Escarpment der Shackleton minous schists; Range intensiver beprobt. Es treten Überwiegend Metamorphire der Amphibo marls and carbonates: grey meta-limestones, carbonaceous guartzites, but also litfazies auf. -
Page 1 0° 10° 10° 110° 110° 20° 20° 120° 120° 30° 30° 130° 130° 40
Bouvet I 50° 40° 30° 20° 10° 0° (Norway) 10° 20° 30° 40° 50° Marion I Prince Edward I e PRINCE EDWARD ISLANDS ea Ic (South Africa) t of S exten ) aximum 973-82 M rage 1 60° ar ave (10 ye SOUTH 60° SOUTH GEORGIA (UK) SANDWICH Crozet Is ISLANDS (France) (UK) R N 60° E H O T C U Antarctic Circle E H A A K O N A G V I O EO I S A N D T H E S O U T H E R N O C E A N R a Laurie I G ( t E V S T k A Powell I J . r u 70° ORCADAS (ARGENTINA) O E A S o b N A l L F lt d Stanley N B u a Coronation I R N r A N Rawson SIGNY (UK) E A I n Y ( U C A g g A G M R n K E E A E a i S S K R A T n V a Edition 6 SOUTH ORKNEY ST M Y I ) e E y FALKLAND ISLANDS (UK) R E S 70° N L R ø ISLANDS O A R E E A v M N N S Z a l Y I A k a IS ) L L i h EN BU VO ) v n ) IA id e A IM A O S e rs I L MAITRI N S r F L a a S QUARISEN E U B n J k L S F R i - e S ( r ) U (INDIA) v Kapp Norvegia P t e m s a N R U s i t ( u R i k A Puerto Deseado Selbukta a D e R u P A r V Y t R b A BORGMASSIVET s E A l N m (J A V FIMBULHEIME E l N y Comodoro Rivadavia u S N o r t IS A H o RIISER LARSENISEN u H t Clarence I J N K Z n E w W E o R Elephant I W E G E T IN o O D m d N E S T SØR-RONDANE z n R I V nH t Y O ro a y 70° t S E R E e O u S L P sl a P N A R e RS L I B y A r H O e e G See Inset d VESTFJELLA LL C G b AV g it en o E H n NH M n s o J N e n EIA a h d E C s e NE T W E M F S e S n I R n r u T h King George I t a b i N m N O d i E H r r N a Joinville I A O B . -
The Stratigraphy of the Ohio Range, Antarctica
This dissertation has been 65—1200 microfilmed exactly as received LONG, William Ellis, 1930- THE STRATIGRAPHY OF THE OHIO RANGE, ANTARCTICA. The Ohio State University, Ph.D., 1964 G eology University Microfilms, Inc., Ann Arbor, Michigan THE STRATIGRAPHY OF THE OHIO RANGE, 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 William Ellis Long, B.S., Rl.S. The Ohio State University 1964 Approved by A (Miser Department of Geology PLEASE NOTE: Figure pages are not original copy* ' They tend tc "curl11. Filled in the best way possible. University Microfilms, Inc. Frontispiece. The Ohio Range, Antarctica as seen from the summit of ITIt. Glossopteris. The cliffs of the northern escarpment include Schulthess Buttress and Darling Ridge. The flat area above the cliffs is the Buckeye Table. ACKNOWLEDGMENTS The preparation of this paper is aided by the supervision and advice of Dr. R. P. Goldthwait and Dr. J. M. Schopf. Dr. 5. B. Treves provided petrographic advice and Dir. G. A. Doumani provided information con cerning the invertebrate fossils. Invaluable assistance in the fiBld was provided by Mr. L. L. Lackey, Mr. M. D. Higgins, Mr. J. Ricker, and Mr. C. Skinner. Funds for this study were made available by the Office of Antarctic Programs of the National Science Foundation (NSF grants G-13590 and G-17216). The Ohio State Univer sity Research Foundation and Institute of Polar Studies administered the project (OSURF Projects 1132 and 1258). Logistic support in Antarctica was provided by the United States Navy, especially Air Development Squadron VX6. -
^Ol N E 20% Number
^ol n e 20% Number ( (-,()RI)()N OGD _P07ING ROi 5E HALIFAX, CANADA NEW -i. ENN, CO;' N't.I`IR:i I' M O[-,'SC H(;ER. TIE NYA I II',l> t; t , 1 11i!.1 . SWITZERLAND 'k,7 $. Y . YALE UNIVER,S NEW HAVEN, CONNECTICUT 06520 RADIOCARBON Editor: MINZE STUIVER Managing Editor: RENEE S KRA Published by THE AMERICAN JOURNAL OF SCIENCE Editors: JOHN RODGERS, JOHN H OSTROM, AND PHILIP M ORVILLE Managing Editor: MARIE C CASEY Published three times a year, in Winter, Spring, and Summer, at Yale University, New Haven, Connecticut 06520. Subscription rate $45.00 (for institutions), $30.00 (for individuals), available only in whole volumes. All correspondence and manuscripts should be addressed to the Managing Editor, RADIOCARBON, Box 2161, Yale Station, New Haven, Connecticut 06520. INSTRUCTIONS TO CONTRIBUTORS Manuscripts of radiocarbon papers should follow the recommendations in Sugges- tions to Authors, 5th ed.* All copy (including the bibliography) must be typewritten in double space. Manuscripts for vol 21, no. 1 must be submitted in duplicate before September 1, 1978, for vol 21, no. 2 before January 1, 1979. General or technical articles should follow the recommendations above and the editorial style of the American Journal of Science. Descriptions of samples, in date lists, should follow as closely as possible the style shown in this volume. Each separate entry (date or series) in a date list should be considered an abstract, prepared in such a way that descriptive material is distinguished from geologic or archaeologic interpretation, but description and interpretation must be both brief and informative, emphasis placed on significant comments. -
The Shackleton Range of East Antarctica
General Information Project Title: The Shackleton Range of East Antarctica: unravelling a complex geological history via an integrated geochronological, geochemical and geophysical approach Lead Institution: BAS Department / School / Institute Geology & Geophysics CASE Partner Organisations CASP, West Building, Madingley Road, [OPTIONAL] Cambridge, CB3 0UD. Leave blank if not applicable End-user Collaborations [OPTIONAL] Leave blank if not applicable Project Team The first supervisor should be from the lead institution. The Second Supervisor should be from a second IAPETUS2 organisation Supervisor 1 Name Dr Teal Riley Organisation BAS Email [email protected] Biography URL https://WWW.bas.ac.uk/profile/trr/ Supervisor 2 Name Dr Nick Gardiner Organisation University of St Andrews Email [email protected] Biography URL https://WWW.st-andrews.ac.uk/earth- sciences/people/njg7 Supervisor 3 (if applicable) Name Dr Fausto Ferraccioli Organisation BAS Email [email protected] Biography URL https://WWW.bas.ac.uk/profile/ffe/ Supervisor 4 (if applicable) Name Organisation Choose an item. Email Biography URL Supervisor 5 (if applicable) Name Organisation Choose an item. Email Biography URL CASE Partners If applicable, add any CASE Partners here Name [optional] Dr Michael FlowerdeW Organisation CASP Email [email protected] Biography URL https://casp.org.uk/people/michael-floWerdeW End-user Collaborations If applicable, add any End-user Collaborations here Name [optional] Organisation Email Biography URL In Collaboration with Add any non-IAPETUS University collaboration partners here. [OPTIONAL] Leave blank if not applicable Name Organisation Email Biography URL Project Details The information provided here will be used to create the project advertisement online and in pdf format. -
New Last Glacial Maximum Ice Thickness Constraints for The
Edinburgh Research Explorer New Last Glacial Maximum Ice Thickness constraints for the Weddell Sea Embayment, Antarctica Citation for published version: Nichols, KA, Goehring, BM, Balco, G, Johnson, JS, Hein, A & Todd, C 2019, 'New Last Glacial Maximum Ice Thickness constraints for the Weddell Sea Embayment, Antarctica', Cryosphere. https://doi.org/10.5194/tc-13-2935-2019 Digital Object Identifier (DOI): 10.5194/tc-13-2935-2019 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: Cryosphere Publisher Rights Statement: © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 09. Oct. 2021 The Cryosphere, 13, 2935–2951, 2019 https://doi.org/10.5194/tc-13-2935-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. New Last Glacial Maximum ice thickness constraints for the Weddell Sea Embayment, Antarctica Keir A. Nichols1, Brent M. -
Clastos Con Calcimicrobios Y Arqueociatos Procedentes De
Estudios Geológicos julio-diciembre 2019, 75(2), e112 ISSN-L: 0367-0449 https://doi.org/10.3989/egeol.43586.567 Calcimicrobial-archaeocyath-bearing clasts from marine slope deposits of the Cambrian Mount Wegener Formation, Coats Land, Shackleton Range, Antarctica Clastos con calcimicrobios y arqueociatos procedentes de depósitos marinos del talud de la Formación cámbrica del Monte Wegener, Coats Land, Cordillera de Shackleton Antártida M. Rodríguez-Martínez1, A. Perejón1, E. Moreno-Eiris1, S. Menéndez2, W. Buggisch3 1Universidad Complutense de Madrid, Departamento de Geodinámica, Estratigrafía y Paleontología, Madrid, Spain. Email: [email protected], [email protected], [email protected]; ORCID ID: http://orcid.org/0000-0002-4363-5562, http://orcid.org/0000-0002-6552-0416, http://orcid.org/0000-0003-2250-4093 2Museo Geominero, Instituto Geológico y Minero de España (IGME), Ríos Rosas, 23, 28003 Madrid, Spain. Email: [email protected]; ORCID ID: Silvia Menéndez: http://orcid.org/0000-0001-6074-9601 3GeoZentrum Nordbayern. Friedrich-Alexander-University of Erlangen-Nürnberg (FAU). Schlossgarten 5, 91054 Erlangen, Germany. ABSTRACT The carbonate clasts from the Mount Wegener Formation provide sedimentological, diagenetic and palaeonto- logical evidences of the destruction and resedimentation of a hidden/unknown Cambrian carbonate shallow-water record at the Coats Land region of Antarctica. This incomplete mosaic could play a key role in comparisons and biostratigraphic correlations between the Cambrian record of the Transantarctic Mountains, Ellsworth-Whitmore block and Antarctic Peninsula at the Antarctica continent. Moreover, it represents a key record in future palaeobio- geographic reconstructions of South Gondwana based on archaeocyathan assemblages. Keywords: Calcimicrobes; Archaeocyaths; Shackleton Range; Antarctica; Gondwana. -
Emergence of the Shackleton Range from Beneath the Antarctic
Edinburgh Research Explorer Emergence of the Shackleton Range from beneath the Antarctic Ice Sheet due to glacial erosion Citation for published version: Sugden, D, Fogwill, CJ, Hein, AS, Stuart, FM, Kerr, AR & Kubik, PW 2014, 'Emergence of the Shackleton Range from beneath the Antarctic Ice Sheet due to glacial erosion', Geomorphology, pp. 1-22. https://doi.org/10.1016/j.geomorph.2013.12.004 Digital Object Identifier (DOI): 10.1016/j.geomorph.2013.12.004 Link: Link to publication record in Edinburgh Research Explorer Document Version: Peer reviewed version Published In: Geomorphology General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 01. Oct. 2021 NOTICE: this is the author's final version of a work that was accepted for publication in Geomorphology. Changes resulting from the publishing process, such as editing, corrections and structural formatting may not be reflected in this document. A definitive version of this document is due to be published in Geomorphology by Elsevier (2014). Emergence of the Shackleton Range from beneath the Antarctic Ice Sheet due to glacial erosion a b a c a d D.E. -
New Last Glacial Maximum Ice Thickness Constraints for the Weddell Sea Embayment, Antarctica
The Cryosphere, 13, 2935–2951, 2019 https://doi.org/10.5194/tc-13-2935-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. New Last Glacial Maximum ice thickness constraints for the Weddell Sea Embayment, Antarctica Keir A. Nichols1, Brent M. Goehring1, Greg Balco2, Joanne S. Johnson3, Andrew S. Hein4, and Claire Todd5 1Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA 2Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA 3British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 4School of GeoSciences, University of Edinburgh, Drummund Street, Edinburgh, EH8 9XP, UK 5Department of Geosciences, Pacific Lutheran University, Tacoma, WA 98447, USA Correspondence: Keir A. Nichols ([email protected]) Received: 27 March 2019 – Discussion started: 14 May 2019 Revised: 12 September 2019 – Accepted: 2 October 2019 – Published: 8 November 2019 Abstract. We describe new Last Glacial Maximum (LGM) surements indicate that the long-lived nuclide measurements ice thickness constraints for three locations spanning the of previous studies were influenced by cosmogenic nuclide Weddell Sea Embayment (WSE) of Antarctica. Samples col- inheritance. Our inferred LGM configuration, which is pri- lected from the Shackleton Range, Pensacola Mountains, and marily based on minimum ice thickness constraints and thus the Lassiter Coast constrain the LGM thickness of the Slessor does not constrain an upper limit, indicates a relatively mod- Glacier, Foundation Ice Stream, and grounded ice proximal est contribution to sea level rise since the LGM of < 4.6 m, to the modern Ronne Ice Shelf edge on the Antarctic Penin- and possibly as little as < 1.5 m. -
1905 and 1906
REPORT OF THE STATE GEOLOGIST ON THE Mineral Industries and Geology of Certain Areas OF VERMONT. 1905- (906. FIFTH OF THIS SERIES. GEORGE H. PERKINS, Ph. D. State Geologist and Professor of Geology., University of Vermont MONTFELIER, VT.. ARGUS AND PATRIOT PiIsSS. 19(R. List of Plates. PAGE 8 I. Typical Slate Quarry, Pawlet ................................ H. Slate Quarry .................. .... ... ... ..... ...... ......... 14 III. Carriers in use in Slate Quarry ........................... CONTENTS. IV. Slate Carriers (Omitted) ............. ..... ..... ............. .ii V. Machine for Trimming Roofing Slate ... ....... ........ ..... 17 VI. Machine for Sawing Slate ......................... .......... 18 VII. Machine for Planing Slate ................................. 18 VIII. Chain Planer for Slate .................................... PAGE 21 INTRODUCTION . ............................................. IX. BoutwellMilne.VarnUm Company's Quarry, Barre, No. I Vi 22 MINERAL RE5OTjiçps ............................................. X. BoutwellMilne-Var11um Company's Quarry, Barre, No. 2 1 24 BUILDING ANT) & Morse Granite Quarry. Barre . .................. ORNAMENTAl, Svoxrs ...................... 4 XI. Wetmore Woodbury ...................... 26 Marble.................. ..................................... XII. Fletcher Granite Quarry, 4 49 Limestol] e Photomicrograph of Aniphibolite ......................... ............................... 7 XIII. Sl Photomicrograph of Amphibolite ......................... 50 ate.......................................................