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Optical Timeline by Tony Oursler
Optical Timeline by Tony Oursler 1 Iris is thought to be derived from the RED Symyaz leads the fallen angels. Archimedes (c. 287212 b.c.) is said to Greek word for speaker or messenger. According to Enoch, they came to earth have used a large magnifying lens or Seth, the Egyptian god most associated of their own free will at Mount Hermon, burning-glass, which focused the suns Fifth century b.c. Chinese philosopher with evil, is depicted in many guises: descending like stars. This description rays, to set fire to Roman ships off Mo Ti, in the first description of the gives rise to the name Lucifer, “giver of Syracuse. camera obscura, refers to the pinhole as a black pig, a tall, double-headed figure light.” “collection place” and “locked treasure with a snout, and a serpent. Sometimes And now there is no longer any “I have seen Satan fall like lightning room.” he is black, a positive color for the difficulty in understanding the images in from heaven.” (Luke 10:1820) Egyptians, symbolic of the deep tones of mirrors and in all smooth and bright Platos Cave depicts the dilemma of fertile river deposits; at other times he is surfaces. The fires from within and from the uneducated in a graphic tableau of red, a negative color reflected by the without communicate about the smooth light and shadow. The shackled masses parched sands that encroach upon the surface, and from one image which is are kept in shadow, unable to move crops. Jeffrey Burton Russell suggests variously refracted. -
Expressions of Climate Perturbations in Western Ugandan Crater Table 3
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Open Access Open Access Clim. Past Discuss., 9, 5183–5226, 2013 Climate www.clim-past-discuss.net/9/5183/2013/ Climate CPD doi:10.5194/cpd-9-5183-2013 of the Past of the Past © Author(s) 2013. CC Attribution 3.0 License. Discussions 9, 5183–5226, 2013 Open Access Open Access This discussion paper is/has been under review for the journal ClimateEarth of the System Past (CP). Earth System Expressions of Please refer to the corresponding final paper in CP if available. Dynamics Dynamics climate perturbations Discussions in western Ugandan Open Access ExpressionsGeoscientific of climate perturbationsGeoscientific inOpen Access crater Instrumentation Instrumentation K. Mills et al. western UgandanMethods and crater lake sedimentMethods and Data Systems Data Systems records during the last 1000 yr Discussions Open Access Open Access Title Page Geoscientific 1,2 1Geoscientific 1 3 4 K. Mills , D. B. Ryves , N. J. Anderson , C. L. BryantModel, and -
The Agrarian Life of the North 2000 Bc–Ad 1000 Studies in Rural Settlement and Farming in Norway
The Agrarian Life of the North 2000 bc–ad 1000 Studies in Rural Settlement and Farming in Norway Frode Iversen & Håkan Petersson Eds. THE AGRARIAN LIFE OF THE NORTH 2000 BC –AD 1000 Studies in rural settlement and farming in Norway Frode Iversen & Håkan Petersson (Eds.) © Frode Iversen and Håkan Petersson, 2017 ISBN: 978-82-8314-099-6 This work is protected under the provisions of the Norwegian Copyright Act (Act No. 2 of May 12, 1961, relating to Copyright in Literary, Scientific and Artistic Works) and published Open Access under the terms of a Creative Commons CC-BY 4.0 License (http://creativecommons.org/licenses/by/4.0/). This license allows third parties to freely copy and redistribute the material in any medium or format as well as remix, transform or build upon the material for any purpose, including commercial purposes, provided the work is properly attributed to the author(s), including a link to the license, and any changes that may have been made are thoroughly indicated. The attribution can be provided in any reasonable manner, however, in no way that suggests the author(s) or the publisher endorses the third party or the third party’s use of the work. Third parties are prohibited from applying legal terms or technological measures that restrict others from doing anything permitted under the terms of the license. Note that the license may not provide all of the permissions necessary for an intended reuse; other rights, for example publicity, privacy, or moral rights, may limit third party use of the material. -
Bulk Mineralogy of Lunar Crater Central Peaks Via Thermal Infrared Spectra from the Diviner Lunar Radiometer - a Study of the Moon’S Crustal Composition at Depth
Bulk mineralogy of Lunar crater central peaks via thermal infrared spectra from the Diviner Lunar Radiometer - A study of the Moon’s crustal composition at depth Eugenie Song A thesis submitted in partial fulfillment of the requirements for the degree of Master of Sciences University of Washington 2012 Committee: Joshua Bandfield Alan Gillespie Bruce Nelson Program Authorized to Offer Degree: Earth and Space Sciences 1 Table of Contents List of Figures ............................................................................................................................................... 3 List of Tables ................................................................................................................................................ 3 Abstract ......................................................................................................................................................... 4 1 Introduction .......................................................................................................................................... 5 1.1 Formation of the Lunar Crust ................................................................................................... 5 1.2 Crater Morphology ................................................................................................................... 7 1.3 Spectral Features of Rock-Forming Silicates in the Lunar Environment ................................ 8 1.4 Compositional Studies of Lunar Crater Central Peaks ........................................................... -
The Cultural Impact of Science in the Early Twentieth Century
In the early decades of the twentieth century, engagement with science was commonly used as an emblem of modernity. This phenomenon is now attracting increasing attention in different historical specialties. Being Modern builds on this recent scholarly interest to explore engagement with science across culture from the end of the nineteenth century to approximately 1940. Addressing the breadth of cultural forms in Britain and the western world from the architecture of Le Corbusier to working class British science fiction, Being Modern paints a rich picture. Seventeen distinguished contributors from a range of fields including the cultural study of science and technology, art and architecture, English The Cultural Impact of culture and literature examine the issues involved. The book will be a valuable resource for students, and a spur to scholars to further examination of culture as an Science in the Early interconnected web of which science is a critical part, and to supersede such tired formulations as ‘Science and culture’. Twentieth Century Robert Bud is Research Keeper at the Science Museum in London. His award-winning publications in the history of science include studies of biotechnology and scientific instruments. Frank James and Morag Shiach James and Morag Frank Robert Greenhalgh, Bud, Paul Edited by Paul Greenhalgh is Director of the Sainsbury Centre at the University of East Anglia, Edited by and Professor of Art History there. He has published extensively in the history of art, design, and the decorative arts in the early modern period. Robert Bud Paul Greenhalgh Frank James is Professor of History of Science at the Royal Institution and UCL. -
938 607072Main Whenbiosphe
| THIS PAGE INTENTIONALLY BLANK by Michael Meltzer NASA SP-2011- 4234 Library of Congress Cataloging-in-Publication Data Meltzer, Michael. When biospheres collide : a history of NASA’s planetary protection programs / by Michael Meltzer. p. cm. -- (NASA SP ; 2011-4234) Includes bibliographical references and index. 1. Space pollution. 2. Space environment. 3. Outer space-- Exploration--Environmental aspects. 4. Environmental protection-- Moral and ethical aspects. I. Title. TL1499.M45 2010 363.739--dc22 2008005759 CONTENTS List of Figures vii List of Tables xi Preface xiii Foreword xv Acknowledgments xix Chapter 1: Why We Must Protect Planetary Environments 1 Chapter 2: In the Beginning: The Need for Planetary Protection Is Recognized 15 Chapter 3: Developing Effective Planetary Protection Approaches 77 Chapter 4: Back Contamination: The Apollo Approach 113 Chapter 5: Planetary Protection for Mars: The Viking Experience 247 Chapter 6: Small Bodies of the Solar System 301 Chapter 7: Return to Mars 359 Chapter 8: Do We Have the Right To Contaminate? The Ethical and Legal Aspects of Planetary Protection 433 Chapter 9: Conclusion 457 Appendices 461 A. Detailed Planetary Protection Requirements 461 B. The Impact of “Faster, Better, Cheaper” on Planetary Protection Priorities 471 C. Biohazard Identification: The Synergism Between Bioterror Prevention and Planetary Protection Research 474 D. Committees, Organizations, and Facilities Important to the Development of Planetary Protection 476 E. Timeline of Important Planetary Protection–Related Events 481 F. Planetary Protection Approaches Used on Various Missions 484 Acronyms and Abbreviations 493 The NASA History Series 497 Index 515 v THIS PAGE INTENTIONALLY BLANK LIST OF FIGURES Image Page Description 2.1 17 Joshua Lederberg in a laboratory at the University of Wisconsin, October 1958. -
Tony Oursler's Optical Timeline
Optical Timeline by Tony Oursler 1 Iris is thought to be derived from the RED Symyaz leads the fallen angels. Archimedes (c. 287212 b.c.) is said to Greek word for speaker or messenger. According to Enoch, they came to earth have used a large magnifying lens or Seth, the Egyptian god most associated of their own free will at Mount Hermon, burning-glass, which focused the suns Fifth century b.c. Chinese philosopher with evil, is depicted in many guises: descending like stars. This description rays, to set fire to Roman ships off Mo Ti, in the first description of the gives rise to the name Lucifer, “giver of Syracuse. camera obscura, refers to the pinhole as a black pig, a tall, double-headed figure light.” “collection place” and “locked treasure with a snout, and a serpent. Sometimes And now there is no longer any “I have seen Satan fall like lightning room.” he is black, a positive color for the difficulty in understanding the images in from heaven.” (Luke 10:1820) Egyptians, symbolic of the deep tones of mirrors and in all smooth and bright Platos Cave depicts the dilemma of fertile river deposits; at other times he is surfaces. The fires from within and from the uneducated in a graphic tableau of red, a negative color reflected by the without communicate about the smooth light and shadow. The shackled masses parched sands that encroach upon the surface, and from one image which is are kept in shadow, unable to move crops. Jeffrey Burton Russell suggests variously refracted. -
Expressions of Climate Perturbations in Western Ugandan Crater Lake Sediment Records During the Last 1000 Years
Supplement of Clim. Past, 10, 1581–1601, 2014 http://www.clim-past.net/10/1581/2014/ doi:10.5194/cp-10-1581-2014-supplement © Author(s) 2014. CC Attribution 3.0 License. Supplement of Expressions of climate perturbations in western Ugandan crater lake sediment records during the last 1000 years K. Mills et al. Correspondence to: K. Mills ([email protected]) 1 Mills et al – Supplementary Material 2 1 Results 3 1.1 Core correlation and chronological analyses 4 1.1.1 Lake Nyamogusingiri 5 Core correlation. Four cores were collected from Lake Nyamogusingiri: two Kajak cores 6 (NCR1 0-29 cm; NCR2 0-35 cm) and two Russian cores (NCR1C1 0-85 cm; NCR2C1 0-100 7 cm). Only the longer Kajak core (NCR2) was used for analysis as it provided a larger overlap 8 with the top of the Russian cores (8 cm). During the retrieval of core NCR1C1 the core 9 chamber failed to close correctly and sediments were lost. As the integrity of this core was 10 compromised NCR1C1 was not considered for analysis. The second core drive (NCR2C1) 11 was successful and selected for analysis. 12 Due to the lack of any obvious defining stratigraphic or sedimentological indicators (e.g. 13 banding) in the Nyamogusingiri cores, cores were first correlated on the basis of the field 14 calculations of the coring depths. This correlation was subsequently corrected and finalised 15 based on the loss-on-ignition and diatom analysis (Figure S1), with Thalassiosira rudolfi 16 being a key species in the confirmation of the overlap (Figure 4a, main text). -
Expressions of Climate Perturbations in Western Ugandan Crater Lake Sediment Records During the Last 1000 Years
Clim. Past, 10, 1581–1601, 2014 www.clim-past.net/10/1581/2014/ doi:10.5194/cp-10-1581-2014 © Author(s) 2014. CC Attribution 3.0 License. Expressions of climate perturbations in western Ugandan crater lake sediment records during the last 1000 years K. Mills1,2,*, D. B. Ryves1, N. J. Anderson1, C. L. Bryant3, and J. J. Tyler4 1Department of Geography, Loughborough University, Loughborough, Leics LE11 3TU, UK 2School of Science and Engineering, University of Ballarat, Ballarat, Vic 3350, Australia 3NERC Radiocarbon Facility, Scottish Enterprise Technology Park, East Kilbride, Scotland G75 0QF, UK 4School of Earth and Environmental Sciences, University of Adelaide, Adelaide, SA 5001, Australia *current address: British Geological Survey, Keyworth, Nottingham NG12 5GG, UK Correspondence to: K. Mills ([email protected]) Received: 15 August 2013 – Published in Clim. Past Discuss.: 10 September 2013 Revised: 26 June 2014 – Accepted: 3 July 2014 – Published: 27 August 2014 Abstract. Equatorial East Africa has a complex regional the main phase of the Little Ice Age (LIA) (ca. AD 1600– patchwork of climate regimes, sensitive to climate fluctua- 1800), whereas the diatom response from the shallower Lake tions over a variety of temporal and spatial scales during Kyasanduka is more complex (with groundwater likely play- the late Holocene. Understanding how these changes are ing a key role), and may be driven more by changes in silica recorded in and interpreted from biological and geochemi- and other nutrients, rather than by lake level. The sensitivity cal proxies in lake sedimentary records remains a key chal- of these two Ugandan lakes to regional climate drivers breaks lenge to answering fundamental questions regarding the na- down in ca. -
Progress Report 1997-1999 Department of Physics Comisión Nacional De Energía Atómica
Progress Report 1997-1999 Department of Physics Comisión Nacional de Energía Atómica Elena M. Godfrin – Rubén Weht Editors Graciela Mastrogiacomo Secretary Buenos Aires – Argentina 2000 INDEX Introduction 1 Nuclear Physics Nuclear Spectroscopy 3 Heavy Ion Physics and Accelerator Mass Spectrometry 10 Astrophysics Astroparticles 15 Pierre Auger Project 17 Applied and Atomic Physics Structural coatings, Surfaces Studies and Ion Implementation 21 Condensed Matter 23 Solar Energy 31 Theoretical Physics 35 Data Communication, Data Acquisition and Computational Facilities 39 Contribution to Conferences 41 Publications 63 Establishment of National Standards 79 Theses 81 Special Works 85 Scientific Cooperation Programs 87 Visitors and Visits 89 Grants and Awards 93 Teaching 95 Personnel 97 Introduction This report describes the activities of the Physics Department for the three-year period 1997-99. It includes basic and applied research, both experimental and theoretical, in areas of nuclear and condensed matter physics and solar energy, technical developments, services and teaching activities at all levels. Other areas of interest are chaos, complex systems, high-Tc superconductivity, astrophysics, intermediate energies and surface physics. The Department maintains strong research ties with the international scientific community and a great part of its research is conducted in collaboration with scientists from all over the world. It is worthwhile to mention the participation of several of our staff researchers in the Pierre Auger Project, an international project involving scientists from many countries, led by Dr. James W. Cronin. Its objective is the installation of two observatories for studying the highest-energy cosmic rays observed on earth, one in the United States and the other in Argentina. -
Book of Abstracts
23rd International Radiocarbon Conference June 17-22 2018 Trondheim Book of Abstracts 23rd International Radiocarbon Conference 2 Table of Content Table of Content ..................................................................................................................................................................... 2 Oral Presentations .................................................................................................................................................................. 3 Poster Presentations ............................................................................................................................................................. 99 Poster Session 1 ................................................................................................................................................................ 99 Poster Session 2 .............................................................................................................................................................. 188 Author Index ....................................................................................................................................................................... 277 3 23rd International Radiocarbon Conference Oral Presentations Updated program, 2018-06-15 Radiocarbon 2018 schedule: Speakers Time Sunday Monday Tuesday 17-06-18 18-06-18 19-06-18 08:00 Front desk Registration 08:30 M. Sarnthein, 302 Opening ceremony 09:00 A. McNichol, 307 E. Boaretto 09:30 R. Hopkins, 110 NTNU welcoming -
Astrobiology and the Potential for Life on Europa, Hand Et
Hand et al.: Potential for Life on Europa 589 Astrobiology and the Potential for Life on Europa Kevin P. Hand NASA Jet Propulsion Laboratory/California Institute of Technology Christopher F. Chyba Princeton University John C. Priscu Montana State University, Bozeman Robert W. Carlson NASA Jet Propulsion Laboratory/California Institute of Technology Kenneth H. Nealson University of Southern California The high likelihood that Europa harbors a contemporary, global, subsurface liquid water ocean makes it a top target in our search for life beyond Earth. Europa’s chondritic composition, rocky seafloor, and radiolytically processed surface may also play an important role in the habita- bility of Europa. Here we review the availability and cycling of biologically essential elements, the availability of energy to power life, and the conditions on Europa that could be conducive to the origin of life. We also address the survivability and detection of possible biosignatures on the surface, and possible search strategies for future orbiting and landed missions. 1. ORIGINS AND HABITABILITY, by the attributes listed in the periphery of Fig. 1. This chap- PAST AND PRESENT ter concerns the details of these attributes so that our physi- cal, chemical, and geological understanding of Europa can 1.1. Introduction guide our biological assessment of this world. We do not address in detail the case for liquid water on Europa, as that Europa may be the premier place in the solar system to search for both extant life and a second origin of life. The discovery of extant life beyond Earth would provide criti- cal information about the fundamental nature of life and the breadth of possible biological processes.