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National Science Board, Staff, Divisional Committees And
. APPENDIX I NATIONALSCIENCEBOARD, STAFF, D~VISIONALCOMMMTEESAND ADVISORY PANELS NATIONALSCIENCEBOARD Terms Expire May lo,1956 JOHN W. DAVIS, President (ret.), West Virginia State College, Englewood, N. J. EDWIN B. FRED, President, the University of Wisconsin, Madison, Wis. hJRENCE M. GOULD, President, Carleton College, Northfield, Minn. PAUL M. GROSS: Vice President and Dean of Duke University, Duke University, Durham, N. C. GEORGE D. HUMPHREY, President, the University of Wyoming, Laramie, wyo. 0. W. HYMAN, Vice President, the University of Tennessee, Memphis, Term. FREDERICK A. MIDDLEBUSH,~ President Emeritus, University of Missouri, Columbia, MO. EARL P. STJWENSON,~ President, Arthur D. Little, Inc., Cambridge, Mass. Terms Expire May lo,1958 SOPHIE D. ABERLE,~ Special Research Director, the University of New Mexico, Albuquerque, N. Mex. CHESTER I. BARN~,~ Chairman of the Board, President (ret.), Rocke- feller Foundation, New York, N. Y. ROBERT P. BARNES, Professor of Chemistry, Howard University, Washing- ton, D. C. DETLEV W. BRONIC,~ Vice Chairman of the Board and Chairman of the Executive Committee, President, National Academy of Sciences, Wash- ington, D. C., and President, Rockefeller Institute for Medical Research, New York, N. Y. GERTY T. Coar, Professor of Biological Chemistry, School of Medicine, Washington University, St. Louis, MO. CHARLES DOLLARD, President, Carnegie Corp. of New York, New York, N. Y. ROBERT F. LOEB,~ Bard Professor of Medicine, College of Physicians and Surgeons, Columbia University, New York, N. Y. ANDREY A. POTTER, Dean Emeritus of Engineering, Purdue University, Lafayette, Ind. Terms Expire May 10, 1960 RWER ADAMS, Department of Chemistry and Chemical Engineering, Uni- versity of Illinois, Urbana, Ill. 60 FOURTE ANNUAL REPORT 61 THEODORE M. -
Geochemistry This
TORONTOTORONTO Vol. 8, No. 4 April 1998 Call for Papers GSA TODAY — page C1 A Publication of the Geological Society of America Electronic Abstracts Submission — page C3 Antarctic Neogene Landscapes—In the 1998 Registration Refrigerator or in the Deep Freeze? Annual Issue Meeting — June GSA Today Introduction The present Molly F. Miller, Department of Geology, Box 117-B, Vanderbilt Antarctic landscape undergoes very University, Nashville, TN 37235, [email protected] slow environmental change because it is almost entirely covered by a thick, slow-moving ice sheet and thus effectively locked in a Mark C. G. Mabin, Department of Tropical Environmental Studies deep freeze. The ice sheet–landscape system is essentially stable, and Geography, James Cook University, Townsville, Queensland 4811, Australia, [email protected] Antarctic—Introduction continued on p. 2 Atmospheric Transport of Diatoms in the Antarctic Sirius Group: Pliocene Deep Freeze Arjen P. Stroeven, Department of Quaternary Research, Stockholm University, S-106 91 Stockholm, Sweden Lloyd H. Burckle, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964 Johan Kleman, Department of Physical Geography, Stockholm University, S-106, 91 Stockholm, Sweden Michael L. Prentice, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824 INTRODUCTION How did young diatoms (including some with ranges from the Pliocene to the Pleistocene) get into the Sirius Group on the slopes of the Transantarctic Mountains? Dynamicists argue for emplacement by a wet-based ice sheet that advanced across East Antarctica and the Transantarctic Mountains after flooding of interior basins by relatively warm marine waters [2 to 5 °C according to Webb and Harwood (1991)]. -
Formal and Informal Networks of Knowledge and Etheldred Benett's
Journal of Literature and Science Volume 8, No. 1 (2015) ISSN 1754-646X Susan Pickford, “Social Authorship, Networks of Knowledge”: 69-85 “I have no pleasure in collecting for myself alone”:1 Social Authorship, Networks of Knowledge and Etheldred Benett’s Catalogue of the Organic Remains of the County of Wiltshire (1831) Susan Pickford As with many other fields of scientific endeavour, the relationship between literature and geology has proved a fruitful arena for research in recent years. Much of this research has focused on the founding decades of the earth sciences in the early- to mid-nineteenth century, with recent articles by Gowan Dawson and Laurence Talairach-Vielmas joining works such as Noah Heringman’s Romantic Rocks, Aesthetic Geology (2003), Ralph O’Connor’s The Earth on Show: Fossils and the Poetics of Popular Science, 1802-1856 (2007), Virginia Zimmerman’s Excavating Victorians (2008) and Adelene Buckland’s Novel Science: Fiction and the Invention of Nineteenth-Century Geology (2013), to explore the rhetorical and narrative strategies of writings in the early earth sciences. It has long been noted that the most institutionally influential early geologists formed a cohort of eager young men who, having no tangible interests in the economic and practical applications of their chosen field, were in a position to develop a passionately Romantic engagement with nature, espousing an apocalyptic rhetoric of catastrophes past and borrowing epic imagery from Milton and Dante (Buckland 9, 14-15). However, as Buckland further notes, this argument – though persuasive as far as it goes – fails to take into account the broad social range of participants in the construction of early geological knowledge. -
Forensic Geology
Manuscript for inclusion in the Encyclopedia of Geology, Edited by R.C. Selley, L.R.M Cocks and I.R Plimer, Elsevier, Amsterdam (2004) FORENSIC GEOLOGY K. Pye. Department of Geology, Royal Holloway University of London, Egham, Surrey TW20 0EW, UK Introduction Forensic geology is concerned with the application of geological data and techniques in relation to issues which may come before a court of law. It is closely related to environmental forensics, forensic engineering and forensic archaeology. Environmental forensics is somewhat broader in scope than forensic geology and involves a wider range of environmental data, knowledge and expertise. It frequently involves investigations of environmental problems such as water and air pollution. Forensic engineering also overlaps with environmental forensics and is typically concerned with such issues as ground stability, the failure of buildings and other engineering structures, flooding, wind damage, fires and explosions. All sub-disciplines of the geosciences have potential forensic applications, but sedimentology, mineralogy, petrology, geochemistry, palaeontology and geophysics have so far made the greatest contributions. Shallow geophysical prospecting methods have been widely used by forensic archaeologists and others to locate and characterize clandestine graves and buried objects such as drugs and weapons. However, probably the most widely recognized application of forensic geology is the use of geological materials as trace evidence which can be of value in linking a suspect to a crime scene. In the wider forensic and legal literature, sediment, soil, dust and rock fragments have often been grouped together under the loose term ‘soil’ evidence. 1 Some of the earliest users of geological and soil evidence were in fact not geologists. -
The Wyley History of the Geologists' Association in the 50 Years 1958
THE WYLEY HISTORY OF THE GEOLOGISTS’ ASSOCIATION 1958–2008 Leake, Bishop & Howarth ASSOCIATION THE GEOLOGISTS’ OF HISTORY WYLEY THE The Wyley History of the Geologists’ Association in the 50 years 1958–2008 by Bernard Elgey Leake, Arthur Clive Bishop ISBN 978-0900717-71-0 and Richard John Howarth 9 780900 717710 GAHistory_cover_A5red.indd 1 19/08/2013 16:12 The Geologists’ Association, founded in 1858, exists to foster the progress and Bernard Elgey Leake was Professor of Geology (now Emeritus) in the diffusion of the science of Geology. It holds lecture meetings in London and, via University of Glasgow and Honorary Keeper of the Geological Collections in the Local Groups, throughout England and Wales. It conducts field meetings and Hunterian Museum (1974–97) and is now an Honorary Research Fellow in the School publishes Proceedings, the GA Magazine, Field Guides and Circulars regularly. For of Earth and Ocean Sciences in Cardiff University. He joined the GA in 1970, was further information apply to: Treasurer from 1997–2009 and is now an Honorary Life Member. He was the last The Executive Secretary, sole editor of the Journal of the Geological Society (1972–4); Treasurer (1981–5; Geologists’ Association, 1989–1996) and President (1986–8) of the Geological Society and President of the Burlington House, Mineralogical Society (1998–2000). He is a petrologist, geochemist, mineralogist, Piccadilly, a life-long mapper of the geology of Connemara, Ireland and a Fellow of the London W1J 0DU Royal Society of Edinburgh. He has held research Fellowships in the Universities of phone: 020 74349298 Liverpool (1955–7), Western Australia (1985) and Canterbury, NZ (1999) and a e-mail: [email protected] lectureship and Readership at the University of Bristol (1957–74). -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
So6 NATURE (SEPTEMBER 22, T904
so6 NATURE (SEPTEMBER 22, t904 Is Selenium Radio-active? THE HEART OF SKYE.' lT occurred to me recently that a possible ·method of deciding between the two hypotheses which have been THIS volume of detailed rock-description, raising brought forward to explain radio-activity, namely, that of in its successive chapters questions of profound atomic degradation (Rutherford and Soddy, Ramsay, &c.) interest in philosophic geology, proves that the Geo and that of molecular change (Armstrong and Lowry, Proc. logical Survey of the United Kingdom is confident Roy. Soc., 1903), lay in attempting to realise radio-activity that the scientific spirit should permeate its public in the case of an element well known to undergo molecular work. None of the rocks dealt with possesses at pre change readily, but with an atomic weight small enough sent an economic value; most of the area is untraversed to exclude the probability of an atomic instability such as by roads, and the exposures are not to be sought in is assumed for radium and thorium. Such an element is quarries, but in rain-swept uplands, or high on selenium (at. wt. .79), which suggested itself to me as a desolate mountain-walls. Yet no detail is regarded suitable material to experiment with because, under the as unimportant; the surveyor, for months together, influence of light, it undergoes a remarkable alteration in its electrical resistance and E.M.F. of contact, suggesting leads a life as hard and remote as that of an Alaskatt an allotropic change of an altogether unusual character. pioneer; and the result is a book in which the daily As this change, whatever be its real nature, occurs almost difficulties are concealed, while an array of facts is instantaneously (Bellati and Romanese, A tti R. -
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico)
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico) by Stephen Alexander Daire A Thesis Presented to the Faculty of the USC Graduate School University of Southern California In Partial Fulfillment of the Requirements for the Degree Master of Science (Geographic Information Science and Technology) May 2019 Copyright © 2019 by Stephen Daire “History is just a 25,000-year dash from the trees to the starship; and while it’s going on its wild and woolly but it’s only like that, and then you’re in the starship.” – Terence McKenna. Table of Contents List of Figures ................................................................................................................................ iv List of Tables ................................................................................................................................. xi Acknowledgements ....................................................................................................................... xii List of Abbreviations ................................................................................................................... xiii Abstract ........................................................................................................................................ xvi Chapter 1 Planetary Sciences, Cave Survey, & Human Evolution................................................. 1 1.1. Topic & Area of Interest: Exploration & Survey ....................................................................12 -
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The Evolution of Language: Towards Gestural Hypotheses DIS/CONTINUITIES TORUŃ STUDIES IN LANGUAGE, LITERATURE AND CULTURE Edited by Mirosława Buchholtz Advisory Board Leszek Berezowski (Wrocław University) Annick Duperray (University of Provence) Dorota Guttfeld (Nicolaus Copernicus University) Grzegorz Koneczniak (Nicolaus Copernicus University) Piotr Skrzypczak (Nicolaus Copernicus University) Jordan Zlatev (Lund University) Vol. 20 DIS/CONTINUITIES Przemysław ywiczy ski / Sławomir Wacewicz TORUŃ STUDIES IN LANGUAGE, LITERATURE AND CULTURE Ż ń Edited by Mirosława Buchholtz Advisory Board Leszek Berezowski (Wrocław University) Annick Duperray (University of Provence) Dorota Guttfeld (Nicolaus Copernicus University) Grzegorz Koneczniak (Nicolaus Copernicus University) The Evolution of Language: Piotr Skrzypczak (Nicolaus Copernicus University) Jordan Zlatev (Lund University) Towards Gestural Hypotheses Vol. 20 Bibliographic Information published by the Deutsche Nationalbibliothek The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data is available in the internet at http://dnb.d-nb.de. The translation, publication and editing of this book was financed by a grant from the Polish Ministry of Science and Higher Education of the Republic of Poland within the programme Uniwersalia 2.1 (ID: 347247, Reg. no. 21H 16 0049 84) as a part of the National Programme for the Development of the Humanities. This publication reflects the views only of the authors, and the Ministry cannot be held responsible for any use which may be made of the information contained therein. Translators: Marek Placi ski, Monika Boruta Supervision and proofreading: John Kearns Cover illustration: © ńMateusz Pawlik Printed by CPI books GmbH, Leck ISSN 2193-4207 ISBN 978-3-631-79022-9 (Print) E-ISBN 978-3-631-79393-0 (E-PDF) E-ISBN 978-3-631-79394-7 (EPUB) E-ISBN 978-3-631-79395-4 (MOBI) DOI 10.3726/b15805 Open Access: This work is licensed under a Creative Commons Attribution Non Commercial No Derivatives 4.0 unported license. -
Curren T Anthropology
Forthcoming Current Anthropology Wenner-Gren Symposium Curren Supplementary Issues (in order of appearance) t Humanness and Potentiality: Revisiting the Anthropological Object in the Anthropolog Current Context of New Medical Technologies. Klaus Hoeyer and Karen-Sue Taussig, eds. Alternative Pathways to Complexity: Evolutionary Trajectories in the Anthropology Middle Paleolithic and Middle Stone Age. Steven L. Kuhn and Erella Hovers, eds. y THE WENNER-GREN SYMPOSIUM SERIES Previously Published Supplementary Issues December 2012 HUMAN BIOLOGY AND THE ORIGINS OF HOMO Working Memory: Beyond Language and Symbolism. omas Wynn and Frederick L. Coolidge, eds. GUEST EDITORS: SUSAN ANTÓN AND LESLIE C. AIELLO Engaged Anthropology: Diversity and Dilemmas. Setha M. Low and Sally Early Homo: Who, When, and Where Engle Merry, eds. Environmental and Behavioral Evidence V Dental Evidence for the Reconstruction of Diet in African Early Homo olum Corporate Lives: New Perspectives on the Social Life of the Corporate Form. Body Size, Body Shape, and the Circumscription of the Genus Homo Damani Partridge, Marina Welker, and Rebecca Hardin, eds. Ecological Energetics in Early Homo e 5 Effects of Mortality, Subsistence, and Ecology on Human Adult Height 3 e Origins of Agriculture: New Data, New Ideas. T. Douglas Price and Plasticity in Human Life History Strategy Ofer Bar-Yosef, eds. Conditions for Evolution of Small Adult Body Size in Southern Africa Supplement Growth, Development, and Life History throughout the Evolution of Homo e Biological Anthropology of Living Human Populations: World Body Size, Size Variation, and Sexual Size Dimorphism in Early Homo Histories, National Styles, and International Networks. Susan Lindee and Ricardo Ventura Santos, eds. -
Article James Croll – Aman‘Greater Far Than His Work’ Kevin J
Earth and Environmental Science Transactions of the Royal Society of Edinburgh,1–20, 2021 Article James Croll – aman‘greater far than his work’ Kevin J. EDWARDS1,2* and Mike ROBINSON3 1 Departments of Geography & Environment and Archaeology, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen AB24 3UF, UK. 2 McDonald Institute for Archaeological Research and Scott Polar Research Institute, University of Cambridge, Cambridge, UK. 3 Royal Scottish Geographical Society, Lord John Murray House, 15–19 North Port, Perth PH1 5LU, UK. *Corresponding author. Email: [email protected] ABSTRACT: Popular and scholarly information concerning the life of James Croll has been accumu- lating slowly since the death in 1890 of the self-taught climate change pioneer. The papers in the current volume offer thorough assessments of topics associated with Croll’s work, but this contribution seeks to provide a personal context for an understanding of James Croll the man, as well as James Croll the scho- lar of sciences and religion. Using archival as well as published sources, emphasis is placed upon selected components of his life and some of the less recognised features of his biography.These include his family history, his many homes, his health, participation in learned societies and attitudes to collegiality, finan- cial problems including the failed efforts to secure a larger pension, and friendship. Life delivered a mix- ture of ‘trials and sorrows’, but it seems clear from the affection and respect accorded him that many looked upon James Croll as a ‘man greater far than his work’. KEY WORDS: Croil–Croyle–Croll, family history, friendship, health, homes, income, learned societies, pension. -
Meeting Reports
MEETING REPORTS The long arm of the (geoforensics) law A recent meeting in London Initiative on Forensic Geology (IUGS- remote sensing techniques meant that considered both the conventional IFG) and the two groups are now closely remains could be distinguished from the and unusual applications of linked. seafloor topography and other debris, and enabled the successful recovery geoscience to forensic investigation. Scope of the remains of many of the victims. Alastair Ruffell, Jamie Pringle and Forensic geology emerged in the 19th The research also highlighted just Ruth Morgan discuss the global and 20th centuries with the application how little we currently know about the expansion of forensic geoscience, of analyses of traces of sand, sediment decomposition of human remains in the and how this field is central to and soil to criminal investigations. The marine environment compared to the keeping geoscience at the forefront main questions answered by forensic terrestrial. The challenges of working in of science and public interest. geologists were in establishing whether these ‘extreme’ environments is further a suspect could have been at a crime compounded when the complexity of The term forensic geoscience often scene, or their alibi locations, and assessing the taphonomic processes draws to mind images of a scientist this type of analysis continues today. and establishing a post-mortem analysing dirt on a crime suspect’s However, geoscientific techniques have submersion interval (PMSI) in marine shoes. Important though such analyses also long been deployed in the search environments is addressed. Research are, the field has moved far beyond for buried or sunken items, as well as in in this study sought to establish the key these humble beginnings and now the sampling of inorganic materials at variables in play in this highly variable includes work on spacecraft surfaces, crime scenes.