LUNAR SECTION CIRCULAR Vol.56 No.6 June 2019
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Image – Action – Space
Image – Action – Space IMAGE – ACTION – SPACE SITUATING THE SCREEN IN VISUAL PRACTICE Luisa Feiersinger, Kathrin Friedrich, Moritz Queisner (Eds.) This publication was made possible by the Image Knowledge Gestaltung. An Interdisciplinary Laboratory Cluster of Excellence at the Humboldt-Universität zu Berlin (EXC 1027/1) with financial support from the German Research Foundation as part of the Excellence Initiative. The editors like to thank Sarah Scheidmantel, Paul Schulmeister, Lisa Weber as well as Jacob Watson, Roisin Cronin and Stefan Ernsting (Translabor GbR) for their help in editing and proofreading the texts. This work is licensed under a Creative Commons Attribution-NonCommercial-No-Derivatives 4.0 License. For details go to https://creativecommons.org/licenses/by-nc-nd/4.0/. Copyrights for figures have been acknowledged according to best knowledge and ability. In case of legal claims please contact the editors. ISBN 978-3-11-046366-8 e-ISBN (PDF) 978-3-11-046497-9 e-ISBN (EPUB) 978-3-11-046377-4 Library of Congress Control Number: 2018956404 Bibliographic information published by the Deutsche Nationalbibliothek The Deutsche National bibliothek lists this publication in the Deutsche Nationalbibliographie; detailed bibliographic data are available on the internet at http://dnb.dnb.de. © 2018 Luisa Feiersinger, Kathrin Friedrich, Moritz Queisner, published by Walter de Gruyter GmbH, Berlin/Boston The book is published with open access at www.degruyter.com, https://www.doabooks.org and https://www.oapen.org. Cover illustration: Malte Euler Typesetting and design: Andreas Eberlein, aromaBerlin Printing and binding: Beltz Bad Langensalza GmbH, Bad Langensalza Printed in Germany www.degruyter.com Inhalt 7 Editorial 115 Nina Franz and Moritz Queisner Image – Action – Space. -
Glossary Glossary
Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts. -
Astronomy Observation Journal by Target
Astronomy Observation Journal by Target Piero Dalle Pezze May 21, 2017 Abstract This document contains my observation reports by target. This file was generated using Java soft- ware tool AstroJournal (http://pdp10.github.io/AstroJournal/) and pdflatex (http://www.tug.org/texlive/). AstroJournal imports files containing astronomy observation reports. Once imported, it generates a comprehensive LATEX document which is then exported to PDF using the utility pdflatex. Astro- Journal is released under GPL v3 license. Contents 1 Legends 1 2 Basic Statistics 3 3 Solar System 4 3.1 Sun, Star.............................................4 3.2 Moon, Satellite.......................................... 10 3.3 Mercury, Planet.......................................... 16 3.4 Venus, Planet........................................... 16 3.5 Mars, Planet........................................... 17 3.6 Ceres, Asteroid.......................................... 18 3.7 Jupiter, Planet.......................................... 19 3.8 Saturn, Planet.......................................... 24 3.9 Uranus, Planet.......................................... 26 3.10 Neptune, Planet......................................... 27 3.11 Mercury Transit, Planet..................................... 27 3.12 Venus - Jupiter, Planet...................................... 28 4 Milky Way 29 4.1 Milky Way, Galaxy........................................ 29 5 Messier Catalogue 30 5.1 M1, Tau, SN Rem........................................ 30 5.2 M2, Aqr, Glob CL....................................... -
Articles and Also and Instrumental Development
Atmos. Chem. Phys., 19, 12631–12686, 2019 https://doi.org/10.5194/acp-19-12631-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. A review of experimental techniques for aerosol hygroscopicity studies Mingjin Tang1, Chak K. Chan2, Yong Jie Li3, Hang Su4,5, Qingxin Ma6, Zhijun Wu7, Guohua Zhang1, Zhe Wang8, Maofa Ge9, Min Hu7, Hong He6,10,11, and Xinming Wang1,10,11 1State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 2School of Energy and Environment, City University of Hong Kong, Kowloon, Hong Kong, China 3Department of Civil and Environmental Engineering, Faculty of Science and Technology, University of Macau, Avenida da Universidade, Taipa, Macau, China 4Center for Air Pollution and Climate Change Research, Institute for Environmental and Climate Research, Jinan University, Guangzhou 511443, China 5Department of Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz 55118, Germany 6State Key Joint Laboratory of Environment Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China 7State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China 8Department of Civil and Environmental Engineering, Hong Kong Polytechnic University, Hong Kong, China 9State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, China 10University of Chinese Academy of Sciences, Beijing 100049, China 11Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China Correspondence: Mingjin Tang ([email protected]) and Chak K. -
10Great Features for Moon Watchers
Sinus Aestuum is a lava pond hemming the Imbrium debris. Mare Orientale is another of the Moon’s large impact basins, Beginning observing On its eastern edge, dark volcanic material erupted explosively and possibly the youngest. Lunar scientists think it formed 170 along a rille. Although this region at first appears featureless, million years after Mare Imbrium. And although “Mare Orien- observe it at several different lunar phases and you’ll see the tale” translates to “Eastern Sea,” in 1961, the International dark area grow more apparent as the Sun climbs higher. Astronomical Union changed the way astronomers denote great features for Occupying a region below and a bit left of the Moon’s dead lunar directions. The result is that Mare Orientale now sits on center, Mare Nubium lies far from many lunar showpiece sites. the Moon’s western limb. From Earth we never see most of it. Look for it as the dark region above magnificent Tycho Crater. When you observe the Cauchy Domes, you’ll be looking at Yet this small region, where lava plains meet highlands, con- shield volcanoes that erupted from lunar vents. The lava cooled Moon watchers tains a variety of interesting geologic features — impact craters, slowly, so it had a chance to spread and form gentle slopes. 10Our natural satellite offers plenty of targets you can spot through any size telescope. lava-flooded plains, tectonic faulting, and debris from distant In a geologic sense, our Moon is now quiet. The only events by Michael E. Bakich impacts — that are great for telescopic exploring. -
Relative Ages
CONTENTS Page Introduction ...................................................... 123 Stratigraphic nomenclature ........................................ 123 Superpositions ................................................... 125 Mare-crater relations .......................................... 125 Crater-crater relations .......................................... 127 Basin-crater relations .......................................... 127 Mapping conventions .......................................... 127 Crater dating .................................................... 129 General principles ............................................. 129 Size-frequency relations ........................................ 129 Morphology of large craters .................................... 129 Morphology of small craters, by Newell J. Fask .................. 131 D, method .................................................... 133 Summary ........................................................ 133 table 7.1). The first three of these sequences, which are older than INTRODUCTION the visible mare materials, are also dominated internally by the The goals of both terrestrial and lunar stratigraphy are to inte- deposits of basins. The fourth (youngest) sequence consists of mare grate geologic units into a stratigraphic column applicable over the and crater materials. This chapter explains the general methods of whole planet and to calibrate this column with absolute ages. The stratigraphic analysis that are employed in the next six chapters first step in reconstructing -
Byzantium and France: the Twelfth Century Renaissance and the Birth of the Medieval Romance
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 12-1992 Byzantium and France: the Twelfth Century Renaissance and the Birth of the Medieval Romance Leon Stratikis University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Modern Languages Commons Recommended Citation Stratikis, Leon, "Byzantium and France: the Twelfth Century Renaissance and the Birth of the Medieval Romance. " PhD diss., University of Tennessee, 1992. https://trace.tennessee.edu/utk_graddiss/2521 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Leon Stratikis entitled "Byzantium and France: the Twelfth Century Renaissance and the Birth of the Medieval Romance." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Modern Foreign Languages. Paul Barrette, Major Professor We have read this dissertation and recommend its acceptance: James E. Shelton, Patrick Brady, Bryant Creel, Thomas Heffernan Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council: I am submitting herewith a dissertation by Leon Stratikis entitled Byzantium and France: the Twelfth Century Renaissance and the Birth of the Medieval Romance. -
Moon Viewing Guide
MMoooonn MMaapp What lunar features can you find? Use this Moon Map & Viewing Guide to explore different areas of the Moon - no binoculars needed! MMoooonn VViieewwiinngg GGuuiiddee A quick look at the Moon in the night sky – even without binoculars - shows light areas and dark areas that reveal lunar history. Can you find these features? Use the Moon Map (above) to help. Sea of Tranquility (Mare Tanquilitatus) – Formed when a giant t! nd I asteroid hit the Moon almost 4 billion years ago, this 500-mile wide Fou dark, smooth, circular basin is the site of the Apollo 11 landing in 1969. Sea of Rains (Mare Imbrium) – Imbrium Basin is the largest t! nd I basin on the Moon that was formed by a giant asteroid almost 4 Fou billion years ago. Sea of Serenity (Mare Serenitatis) – Apollo 17 astronauts t! sampled some of the oldest rocks on the Moon from edges of nd I Fou the Sea of Serenity. These ancient rocks formed in the Moon’s magma ocean. Lunar Highlands – The lighter areas on the Moon are the lunar t! highlands. These are the oldest regions on the Moon; they formed nd I Fou from the magma ocean. Because they are so old, they have been hit by impact craters many times, making the highlands very rough. Want an extra challenge? If you have a telescope or pair of binoculars, try finding these features: Appenine Mountains (Montes Apenninus) – Did you know there are mountain ranges on the Moon? The rims of the craters and t! nd I basins rise high above the Moon’s surface. -
Glossary of Lunar Terminology
Glossary of Lunar Terminology albedo A measure of the reflectivity of the Moon's gabbro A coarse crystalline rock, often found in the visible surface. The Moon's albedo averages 0.07, which lunar highlands, containing plagioclase and pyroxene. means that its surface reflects, on average, 7% of the Anorthositic gabbros contain 65-78% calcium feldspar. light falling on it. gardening The process by which the Moon's surface is anorthosite A coarse-grained rock, largely composed of mixed with deeper layers, mainly as a result of meteor calcium feldspar, common on the Moon. itic bombardment. basalt A type of fine-grained volcanic rock containing ghost crater (ruined crater) The faint outline that remains the minerals pyroxene and plagioclase (calcium of a lunar crater that has been largely erased by some feldspar). Mare basalts are rich in iron and titanium, later action, usually lava flooding. while highland basalts are high in aluminum. glacis A gently sloping bank; an old term for the outer breccia A rock composed of a matrix oflarger, angular slope of a crater's walls. stony fragments and a finer, binding component. graben A sunken area between faults. caldera A type of volcanic crater formed primarily by a highlands The Moon's lighter-colored regions, which sinking of its floor rather than by the ejection of lava. are higher than their surroundings and thus not central peak A mountainous landform at or near the covered by dark lavas. Most highland features are the center of certain lunar craters, possibly formed by an rims or central peaks of impact sites. -
Apollo 15 Mission
THE APOLLO 15 MISSION On July 30, 1971, the Apollo 15 lunar module Falcon, descending over the 4,000 meter Apennine Mountain front, landed at one of the most geologically diverse sites selected in the Apollo program, the Hadley-Apennine region. Astronauts Dave Scott and Jim Irwin brought the spacecraft onto a mare plain just inside the most prominent mountain ring structure of the Imbrium basin, the Montes Apennines chain which marks its southeastern topographic rim, and close to the sinuous Hadley Rille (Fig. 1). The main objectives of the mission were to investigate and sample materials of the Apennine Front itself (expected to be Imbrium ejecta and pre-Imbrium materials), of Hadley Rille, and of the mare lavas of Palus Putredinis (Fig. 2). A package of seven surface experiments, including heat flow and passive seismic, was also set up and 1152 surface photographs were taken. A television camera, data acquisition (sequence) camera, and orbital photography and chemical data provided more information. The Apollo 15 mission was the first devoted almost entirely to science, and the first to use a Rover vehicle which considerably extended the length of the traverses, from a total of 3.5 km on Apollo 14 to 25.3 km during three separate traverses on Apollo 15 (Fig. 3). The collected sample mass was almost doubled, from 43 kg on Apollo 14 to 78 kg on Apollo 15. A reduction in the planned traverse length was made necessary, in part by unexpected and time-consuming difficulties in the collection of the deep core sample (at the experiments package area). -
VV D C-A- R 78-03 National Space Science Data Center/ World Data Center a for Rockets and Satellites
VV D C-A- R 78-03 National Space Science Data Center/ World Data Center A For Rockets and Satellites {NASA-TM-79399) LHNAS TRANSI]_INT PHENOMENA N78-301 _7 CATAI_CG (NASA) 109 p HC AO6/MF A01 CSCl 22_ Unc.las G3 5 29842 NSSDC/WDC-A-R&S 78-03 Lunar Transient Phenomena Catalog Winifred Sawtell Cameron July 1978 National Space Science Data Center (NSSDC)/ World Data Center A for Rockets and Satellites (WDC-A-R&S) National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt) Maryland 20771 CONTENTS Page INTRODUCTION ................................................... 1 SOURCES AND REFERENCES ......................................... 7 APPENDIX REFERENCES ............................................ 9 LUNAR TRANSIENT PHENOMENA .. .................................... 21 iii INTRODUCTION This catalog, which has been in preparation for publishing for many years is being offered as a preliminary one. It was intended to be automated and printed out but this form was going to be delayed for a year or more so the catalog part has been typed instead. Lunar transient phenomena have been observed for almost 1 1/2 millenia, both by the naked eye and telescopic aid. The author has been collecting these reports from the literature and personal communications for the past 17 years. It has resulted in a listing of 1468 reports representing only slight searching of the literature and probably only a fraction of the number of anomalies actually seen. The phenomena are unusual instances of temporary changes seen by observers that they reported in journals, books, and other literature. Therefore, although it seems we may be able to suggest possible aberrations as the causes of some or many of the phenomena it is presumptuous of us to think that these observers, long time students of the moon, were not aware of most of them. -
Ancient Lamps in the J. Paul Getty Museum
ANCIENT LAMPS THE J. PAUL GETTY MUSEUM Ancient Lamps in the J. Paul Getty Museum presents over six hundred lamps made in production centers that were active across the ancient Mediterranean world between 800 B.C. and A.D. 800. Notable for their marvelous variety—from simple clay saucers GETTYIN THE PAUL J. MUSEUM that held just oil and a wick to elaborate figural lighting fixtures in bronze and precious metals— the Getty lamps display a number of unprecedented shapes and decors. Most were made in Roman workshops, which met the ubiquitous need for portable illumination in residences, public spaces, religious sanctuaries, and graves. The omnipresent oil lamp is a font of popular imagery, illustrating myths, nature, and the activities and entertainments of daily life in antiquity. Presenting a largely unpublished collection, this extensive catalogue is ` an invaluable resource for specialists in lychnology, art history, and archaeology. Front cover: Detail of cat. 86 BUSSIÈRE AND LINDROS WOHL Back cover: Cat. 155 Jean Bussière was an associate researcher with UPR 217 CNRS, Antiquités africaines and was also from getty publications associated with UMR 140-390 CNRS Lattes, Ancient Terracottas from South Italy and Sicily University of Montpellier. His publications include in the J. Paul Getty Museum Lampes antiques d'Algérie and Lampes antiques de Maria Lucia Ferruzza Roman Mosaics in the J. Paul Getty Museum Méditerranée: La collection Rivel, in collaboration Alexis Belis with Jean-Claude Rivel. Birgitta Lindros Wohl is professor emeritus of Art History and Classics at California State University, Northridge. Her excavations include sites in her native Sweden as well as Italy and Greece, the latter at Isthmia, where she is still active.