The Multiplexed Squid Tes Array at Ninety Gigahertz (Mustang)
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March 21–25, 2016
FORTY-SEVENTH LUNAR AND PLANETARY SCIENCE CONFERENCE PROGRAM OF TECHNICAL SESSIONS MARCH 21–25, 2016 The Woodlands Waterway Marriott Hotel and Convention Center The Woodlands, Texas INSTITUTIONAL SUPPORT Universities Space Research Association Lunar and Planetary Institute National Aeronautics and Space Administration CONFERENCE CO-CHAIRS Stephen Mackwell, Lunar and Planetary Institute Eileen Stansbery, NASA Johnson Space Center PROGRAM COMMITTEE CHAIRS David Draper, NASA Johnson Space Center Walter Kiefer, Lunar and Planetary Institute PROGRAM COMMITTEE P. Doug Archer, NASA Johnson Space Center Nicolas LeCorvec, Lunar and Planetary Institute Katherine Bermingham, University of Maryland Yo Matsubara, Smithsonian Institute Janice Bishop, SETI and NASA Ames Research Center Francis McCubbin, NASA Johnson Space Center Jeremy Boyce, University of California, Los Angeles Andrew Needham, Carnegie Institution of Washington Lisa Danielson, NASA Johnson Space Center Lan-Anh Nguyen, NASA Johnson Space Center Deepak Dhingra, University of Idaho Paul Niles, NASA Johnson Space Center Stephen Elardo, Carnegie Institution of Washington Dorothy Oehler, NASA Johnson Space Center Marc Fries, NASA Johnson Space Center D. Alex Patthoff, Jet Propulsion Laboratory Cyrena Goodrich, Lunar and Planetary Institute Elizabeth Rampe, Aerodyne Industries, Jacobs JETS at John Gruener, NASA Johnson Space Center NASA Johnson Space Center Justin Hagerty, U.S. Geological Survey Carol Raymond, Jet Propulsion Laboratory Lindsay Hays, Jet Propulsion Laboratory Paul Schenk, -
Bibliographyof Space Books Andarticlesfrom Non
https://ntrs.nasa.gov/search.jsp?R=19800016707N 2020-03-11T18:02:45+00:00Zi_sB--rM-._lO&-{/£ 3 1176 00167 6031 HHR-51 NASA-TM-81068 ]9800016707 BibliographyOf Space Books And ArticlesFrom Non-AerospaceJournals 1957-1977 _'C>_.Ft_iEFERENC_ I0_,'-i p,,.,,gvi ,:,.2, , t ,£}J L,_:,._._ •..... , , .2 ,IFER History Office ...;_.o.v,. ._,.,- NASA Headquarters Washington, DC 20546 1979 i HHR-51 BIBLIOGRAPHYOF SPACEBOOKS AND ARTICLES FROM NON-AEROSPACE JOURNALS 1957-1977 John J. Looney History Office NASA Headquarters Washlngton 9 DC 20546 . 1979 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 033-000-0078t-1 Kc6o<2_o00 CONTENTS Introduction.................................................... v I. Space Activity A. General ..................................................... i B. Peaceful Uses ............................................... 9 C. Military Uses ............................................... Ii 2. Spaceflight: Earliest Times to Creation of NASA ................ 19 3. Organlzation_ Admlnlstration 9 and Management of NASA ............ 30 4. Aeronautics..................................................... 36 5. BoostersandRockets............................................ 38 6. Technology of Spaceflight....................................... 45 7. Manned Spaceflight.............................................. 77 8. Space Science A. Disciplines Other than Space Medicine ....................... 96 B. Space Medicine ..............................................119 C. -
Leag Conference on Lunar Exploration
Report of the SPACE RESOURCES ROUNDTABLE VII: LEAG CONFERENCE ON LUNAR EXPLORATION LPI Contribution No. 1318 REPORT OF THE SPACE RESOURCES ROUNDTABLE VII: LEAG CONFERENCE ON LUNAR EXPLORATION October 25–28, 2005 League City, Texas SPONSORED BY Lunar and Planetary Institute NASA Aeronautics and Space Administration Space Resources Roundtable, Inc. NASA Lunar Exploration Analysis Group CONVENERS G. Jeffrey Taylor, University of Hawai‘i Stephen Mackwell, Lunar and Planetary Institute James Garvin, NASA Chief Scientist Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 1318 Compiled in 2006 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Agreement No. NCC5-679 issued through the Solar System Exploration Division of the National Aeronautics and Space Administration. Any opinions, findings, and conclusions or recommendations expressed in this volume are those of the author(s) and do not necessarily reflect the views of the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113, USA Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling. ISSN No. 0161-5297 Report of the LEAG Conference iii CONTENTS Agenda ...........................................................................................................................................1 Conference Overview ..................................................................................................................13 Abstracts Unified Lunar Topographic Model B. -
GRAIL Gravity Observations of the Transition from Complex Crater to Peak-Ring Basin on the Moon: Implications for Crustal Structure and Impact Basin Formation
Icarus 292 (2017) 54–73 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus GRAIL gravity observations of the transition from complex crater to peak-ring basin on the Moon: Implications for crustal structure and impact basin formation ∗ David M.H. Baker a,b, , James W. Head a, Roger J. Phillips c, Gregory A. Neumann b, Carver J. Bierson d, David E. Smith e, Maria T. Zuber e a Department of Geological Sciences, Brown University, Providence, RI 02912, USA b NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA c Department of Earth and Planetary Sciences and McDonnell Center for the Space Sciences, Washington University, St. Louis, MO 63130, USA d Department of Earth and Planetary Sciences, University of California, Santa Cruz, CA 95064, USA e Department of Earth, Atmospheric and Planetary Sciences, MIT, Cambridge, MA 02139, USA a r t i c l e i n f o a b s t r a c t Article history: High-resolution gravity data from the Gravity Recovery and Interior Laboratory (GRAIL) mission provide Received 14 September 2016 the opportunity to analyze the detailed gravity and crustal structure of impact features in the morpho- Revised 1 March 2017 logical transition from complex craters to peak-ring basins on the Moon. We calculate average radial Accepted 21 March 2017 profiles of free-air anomalies and Bouguer anomalies for peak-ring basins, protobasins, and the largest Available online 22 March 2017 complex craters. Complex craters and protobasins have free-air anomalies that are positively correlated with surface topography, unlike the prominent lunar mascons (positive free-air anomalies in areas of low elevation) associated with large basins. -
Geological Mapping of Lunar Crater Lalande: Topographic Configuration, Morphology and Cratering Process
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W1, 2017 2017 International Symposium on Planetary Remote Sensing and Mapping, 13–16 August 2017, Hong Kong GEOLOGICAL MAPPING OF LUNAR CRATER LALANDE: TOPOGRAPHIC CONFIGURATION, MORPHOLOGY AND CRATERING PROCESS B. Li a, b*, Z.C. Ling a, J. Zhanga, J. Chen a, C.Q. Liu a, X.Y. Bi a a Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment; Institute of Space Sciences, Shandong University, Weihai, China. - [email protected] b Key Laboratory of Lunar and Deep Space Exploration, Beijing, China. Commission VI, WG VI/4 KEY WORDS: Crater Lalande, Geological mapping, Low-relief bulges, Cratering process, Elevation differences ABSTRACT: Highland crater Lalande (4.45°S, 8.63°W; D=23.4 km) is located on the PKT area of the lunar near side, southeast of Mare Insularum. It is a complex crater in Copernican era and has three distinguishing features: high silicic anomaly, highest Th abundance and special landforms on its floor. There are some low-relief bulges on the left of crater floor with regular circle or ellipse shapes. They are ~250 to 680 m wide and ~30 to 91 m high with maximum flank slopes >20°. There are two possible scenarios for the formation of these low-relief bulges which are impact melt products or young silicic volcanic eruptions. According to the absolute model ages of ejecta, melt ponds and hummocky floor, the ratio of diameter and depth, similar bugle features within other Copernican-aged craters and lack of volcanic source vents, we hypothesized that these low-relief bulges were most consistent with an origin of impact melts during the crater formation instead of small and young volcanic activities occurring on the crater floor. -
O Lunar and Planetary Institute Provided by the NASA Astrophysics Data System 414 LPS XXVII
LPS XXVII THE COMPOSITION AND GEOLOGIC SETTING OF LUNAR FAR SIDE MARIA. Jeffrey J. illi is', & Paul D. ~~udis"', 1. Dept. of Geology and Geophysics, Rice University, Houston TX, 77005 2. Lunar and Planetary Institute, Houston Texas 77058. The dichotomy in the distribution of maria between the Earth facing side and the far side of the Moon has evoked many questions concerning the emplacement mechanisms, compositional variation, and source regions of lunar basalts. The near side maria have been well analyzed using a variety of Earth based, and lunar surface and satellite information. The Clementine mission has provided the first global mineralogical and chemical maps for the Moon. These data will allow us to gain knowledge of many lunar far side basalt deposits for the first time. Although the far side maria (Figure 1) represents only about 1% of the surface of the Moon [I], these deposits provide insight into the crustal evolution, thermal history, and the interior of the Moon. Information on the composition, age, and volume of mare deposits will further our understanding of these questions. We are now studying several data sets, including multi-spectral images, crater statistics, and altimetry, to reconstruct and understand lunar volcanic evolution. Ultravioletlvisible (UVVIS) image data provide information of the composition of mare deposits. Ratios 4151750 provide information of titanium content [2,4] and the 9501750 absorptions is correlated with the concentration of ~e~+and mafic minerals [2, 31. Crater statistics provide relative age determination, which can be used to estimate absolute ages. Knowing the range in ages of all the mare units on the far side will allow us to determine the duration of magmatism on the far side. -
The Lassell Massif-A Silicic Lunar Volcano
Icarus 273 (2016) 248–261 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus The Lassell massif—A silicic lunar volcano ∗ J.W. Ashley a, b , , M.S. Robinson a, J.D. Stopar a, T.D. Glotch c, B. Ray Hawke d, C.H. van der Bogert e, H. Hiesinger e, S.J. Lawrence a, B.L. Jollifff, B.T. Greenhagen g, T.A. Giguere d, D.A. Paige h a School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85281, USA b Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA c Department of Geosciences, Stony Brook University, Stony Brook, NY 11794, USA d Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI 96822, USA e Institut für Planetologie, Westfälische Wilhelms-Universität, Münster, Germany f Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63105, USA g Johns Hopkins University – Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA h Department of Earth and Space Sciences, University of California Los Angeles, Los Angeles, CA 90095, USA a r t i c l e i n f o a b s t r a c t Article history: Lunar surface volcanic processes are dominated by mare-producing basaltic extrusions. However, spec- Received 24 June 2014 tral anomalies, landform morphology, and granitic or rhyolitic components found in the Apollo sample Revised 20 November 2015 suites indicate limited occurrences of non-mare, geochemically evolved (Si-enriched) volcanic deposits. Accepted 14 December 2015 Recent thermal infrared spectroscopy, high-resolution imagery, and topographic data from the Lunar Re- Available online 30 December 2015 connaissance Orbiter (LRO) show that most of the historic “red spots” and other, less well-known loca- Keywords: tions on the Moon, are indeed silica rich (relative to basalt). -
Civil War Bounties 1861-1865
Chester County Civil War Bounties 1861-1865 Last Name First Name Middle Name Residence/To Age Rank Company Regiment/Unit Year Folder See/Page Record Cable John 21st PA Cavalry 1863‐1864 OS #5 5 Bounty List Cable John 21st PA Cavalry 1865 71 Bounty Volume Cabreza Miguel Willistown 19 1864 3 Receipts Cahill James East 27 45th 1864 26 Cahill, James Receipts Nottingham Cahill James East 1864 165 Bounty Nottingham Volume Cain George East 1864 165 Bounty Nottingham Volume Cain George East 22 5th PA Cavalry 1864 3 Receipts Nottingham Cain Samuel G 55th 1865 79 Bounty Volume Cain William Willistown 28 17 Bounty List Cain William U.S.C.T. 1864 125 Bounty Volume Cain William Willistown 1864 28 47 Bounty List Cain William Willistown 1864 190 Bounty Volume Cairnes William Honey Brook 1862 OS #3 4 1st Draft List Cake William J.B 1st PA Reserve 1863‐1864 OS #4 1 Bounty List Cake William J.1st Sergt. 1st Infantry P.R.C. 1863‐1864 OS #5 4 Bounty List Chester County Archives and Record Services, West Chester, PA 19380 Last Name First Name Middle Name Residence/To Age Rank Company Regiment/Unit Year Folder See/Page Record Cake William J.A 1st PA Reserves 1864 102 Bounty Volume Calahan John New Garden 28 29 Bounty List Calahan John New Garden 1864 162 Bounty Volume Calaman Charles W. U.S.C.T. 1864 125 Bounty Volume Calderwood John Private D 53rd 1863‐1864 OS #5 4 Bounty List Calderwood John D 53rd 1863‐1864 OS #4 4 Bounty List Calderwood John D 53rd 1865 84 Bounty Volume Caldwell John Drummer H 53rd 1863‐1864 OS #5 4 Bounty List Caldwell John C.H 53rd 1863‐1864 -
Suited for Spacewalking
Suited for Spacewalking A Teacher's Guide with Activities for Technology Education, Mathematics, and Science National Aeronautics and Space Administration Office of Human Resources and Education Education Division Washington, DC Education Working Group NASA Johnson Space Center Houston, Texas This publication is in the Public Domain and is not protected by copyright. Permission is not required for duplication. EG- 1998-03- I 12-HQ Deborah A. Shearer Acknowledgments Science Teacher Zue S. Baales Intermediate School This publication was developed for the National Friendswood, Texas Aeronautics and Space Administration by: Sandy Peck Writer/Illustrator: Clear Creek Independent School District Gregory L. V0gt, Ed.D. League City, Texas Crew Educational Affairs Liaison Teaching From Space Program Marilyn L. Fowler, Ph.D. NASA Johnson Space Center Science Project Specialist Houston, TX Charles A. Dana Center University of Texas at Austin Editor: Jane A. George Jeanne Gasiorowski Educational Materials Specialist Manager, NASA Educator Resource Center Teaching From Space Program Classroom of the Future NASA Headquarters Wheeling Jesuit University Washington, DC Wheeling, West Virginia Reviewers: Dr, PeggyHouse Linda Godwin Director, The Glenn T Seaborg NASA Astronaut Center for Teaching and Learning NASA Johnson Space Center Science and Mathematics Northern Michigan University Joseph J. Kosmo Senior Project Engineer Doris K. Grigsby, Ed.D. EVA and Spacesuit Systems Branch AESP Management and Performance NASA Johnson Space Center Specialist for Training Oklahoma State University Philip R. West Project Manager, EVA Tools Flint Wild for the International Space Station Technology Specialist NASA Johnson Space Center Teaching From Space Program Oklahoma State University Cathy A. Gardner Teacher Intern, Teaching From Space Patterson A. -
Magmatic Volatiles (H, C, N, F, S, Cl) in the Lunar Mantle, Crust, and Regolith: Abundances, Distributions, Processes, and Reservoirs†K
American Mineralogist, Volume 100, pages 1668–1707, 2015 THE SECOND CONFERENCE ON THE LUNAR HIGHLANDS CRUST AND NEW DIRECTIONS REVIEW Magmatic volatiles (H, C, N, F, S, Cl) in the lunar mantle, crust, and regolith: Abundances, distributions, processes, and reservoirs†k FRANCIS M. MCCUBBIN1,2,*, KATHLEEN E. VANDER KAADEN1,2, ROMAIN TARTÈSE3, RACHEL L. KLIMA4, YANG LIU5, JAMES MORTIMER3, JESSICA J. BARNES3,6, CHARLES K. SHEARER1,2, ALLAN H. TREIMAN7, DAVID J. LAWRENCE3, STEPHEN M. ELARDO1,2,8, DANA M. HURLEY3, JEREMY W. BOYCE9 AND MAHESH ANAND3,6 1Institute of Meteoritics, University of New Mexico, 200 Yale Blvd SE, Albuquerque, New Mexico 87131, U.S.A. 2Department of Earth and Planetary Sciences, University of New Mexico, 200 Yale Blvd SE, Albuquerque, New Mexico 87131, U.S.A. 3Planetary and Space Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6AA, U.K. 4Planetary Exploration Group, Space Department, Johns Hopkins University Applied Physics Lab, Laurel, Maryland 20723, U.S.A. 5Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109, U.S.A. 6Department of Earth Sciences, The Natural History Museum, Cromwell Road, London, SW7 5BD, U.K. 7Lunar and Planetary Institute, USRA, 3600 Bay Area Boulevard, Houston, Texas 77058, U.S.A. 8Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 9Department of Earth and Space Sciences, University of California, Los Angeles, California 90095-1567, U.S.A. ABSTRACT Many studies exist on magmatic volatiles (H, C, N, F, S, Cl) in and on the Moon, within the last several years, that have cast into question the post-Apollo view of lunar formation, the distribution and sources of volatiles in the Earth-Moon system, and the thermal and magmatic evolution of the Moon. -
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 ........................................................... -
Understanding the Lunar Surface and Space-Moon Interactions Paul Lucey1, Randy L
Reviews in Mineralogy & Geochemistry Vol. 60, pp. 83-219, 2006 2 Copyright © Mineralogical Society of America Understanding the Lunar Surface and Space-Moon Interactions Paul Lucey1, Randy L. Korotev2, Jeffrey J. Gillis1, Larry A. Taylor3, David Lawrence4, Bruce A. Campbell5, Rick Elphic4, Bill Feldman4, Lon L. Hood6, Donald Hunten7, Michael Mendillo8, Sarah Noble9, James J. Papike10, Robert C. Reedy10, Stefanie Lawson11, Tom Prettyman4, Olivier Gasnault12, Sylvestre Maurice12 1University of Hawaii at Manoa, Honolulu, Hawaii, U.S.A. 2Washington University, St. Louis, Missouri, U.S.A. 3University of Tennessee, Knoxville, Tennessee, U.S.A. 4Los Alamos National Laboratory, Los Alamos, New Mexico, U.S.A. 5Smithsonian Institution, Washington D.C., U.S.A. 6Lunar and Planetary Laboratory, Univ. of Arizona, Tucson, Arizona, U.S.A. 7University of Arizona, Tucson, Arizona, U.S.A. 8Boston University, Cambridge, Massachusetts, U.S.A. 9Brown University, Providence, Rhode Island, U.S.A. 10University of New Mexico, Albuquerque, New Mexico, U.S.A. 11 Northrop Grumman, Van Nuys, California, U.S.A. 12Centre d’Etude Spatiale des Rayonnements, Toulouse, France Corresponding authors e-mail: Paul Lucey <[email protected]> Randy Korotev <[email protected]> 1. INTRODUCTION The surface of the Moon is a critical boundary that shapes our understanding of the Moon as a whole. All geologic mapping and remote sensing techniques utilize only the outermost portion of the Moon. Before leaving the Moon for study in our laboratories, all lunar samples that have been studied existed at or very near the surface. With the exception of the deeply probing geophysical techniques, our understanding of the interior of the Moon is derived from surficial, but not superficial, information, coupled with geologic reasoning.