Explore the Moon—Binocular
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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. -
July 2020 in This Issue Online Readers, ALPO Conference November 6-7, 2020 2 Lunar Calendar July 2020 3 Click on Images an Invitation to Join ALPO 3 for Hyperlinks
A publication of the Lunar Section of ALPO Edited by David Teske: [email protected] 2162 Enon Road, Louisville, Mississippi, USA Recent back issues: http://moon.scopesandscapes.com/tlo_back.html July 2020 In This Issue Online readers, ALPO Conference November 6-7, 2020 2 Lunar Calendar July 2020 3 click on images An Invitation to Join ALPO 3 for hyperlinks. Observations Received 4 By the Numbers 7 Submission Through the ALPO Image Achieve 4 When Submitting Observations to the ALPO Lunar Section 9 Call For Observations Focus-On 9 Focus-On Announcement 10 2020 ALPO The Walter H. Haas Observer’s Award 11 Sirsalis T, R. Hays, Jr. 12 Long Crack, R. Hill 13 Musings on Theophilus, H. Eskildsen 14 Almost Full, R. Hill 16 Northern Moon, H. Eskildsen 17 Northwest Moon and Horrebow, H. Eskildsen 18 A Bit of Thebit, R. Hill 19 Euclides D in the Landscape of the Mare Cognitum (and Two Kipukas?), A. Anunziato 20 On the South Shore, R. Hill 22 Focus On: The Lunar 100, Features 11-20, J. Hubbell 23 Recent Topographic Studies 43 Lunar Geologic Change Detection Program T. Cook 120 Key to Images in this Issue 134 These are the modern Golden Days of lunar studies in a way, with so many new resources available to lu- nar observers. Recently, we have mentioned Robert Garfinkle’s opus Luna Cognita and the new lunar map by the USGS. This month brings us the updated, 7th edition of the Virtual Moon Atlas. These are all wonderful resources for your lunar studies. -
Guide User Manual (PDF)
CONTENTS 1: 2 Installing Guide 2: 2 Getting Help 3: 3 What Guide is showing you 4: 4 Panning and zooming 5: 5 Finding objects 5a: 8 Finding stars 5b: 10 Finding galaxies 5c: 12 Finding nebulae 5d: 12 Entering coordinates 6: 13 Getting information about objects 6a: 15 Measuring angular distances on the screen 6b: 15 Quick info 7: 16 The Display menu 7a: 17 The Star Display menu 7b: 19 The Data Shown menu 7c: 21 Planet display 7d: 23 The Camera Frame menu 7e: 24 The Legend Menu 7f: 26 Measurement markings (grids, ticks, etc.) 7g: 28 Backgrounds dialog 8: 29 Changing settings 8a: 34 Location dialog 8b: 35 Inversion dialog 9: 36 Overlays menu 10: 38 User Object menu 11: 39 Telescope control 12: 42 DOS Printer setup and printing 13: 43 PostScript charts 14: 44 The time dialog 15: 46 Planetary animation and ephemeris generation 16: 50 Tables menu 17: 52 Extras menu 17a: 54 DSS/RealSky Images 17b: 56 Downloading star data from the Internet 17c: 58 Installing to the hard drive 17d: 59 Asteroid options 18: 62 Eclipses, occultations, transits 19: 63 Saving and going to marks 20: 64 User-added (.TDF) datasets 21: 65 Adding your own notes for objects 22: 66 About Guide's data 23: 67 Accessing Guide's data from your own programs 24: 68 Acknowledgments Appendices: A: 70 RA and Declination Explained B: 70 Precession and Epochs Explained C: 71 Altitude and Azimuth (Alt/Az) Explained D: 72 Troubleshooting Positions 1 E: 73 Notes on Accuracy F: 73 Adding New Comets G: 75 Astronomical Magnitudes H: 75 Copyright and Liability Notices I: 77 List of Program-Wide Hotkeys Index 79 Questions and bug reports should be sent to: Project Pluto 168 Ridge Road Bowdoinham ME 04008 Fax (207) 666 3149 Tel (207) 666 5750 Tel (800) 777 5886 E-mail: [email protected] WWW: http://www.projectpluto.com 1: HOW TO INSTALL GUIDE To install Guide, put the Guide DVD into the DVD drive. -
Explore the Moon with Binoculars
THE ROYAL ASTRONOMICAL SOCIETY OF CANADA presents: Explore the Moon with binoculars photo by Ian Corbett, Liverpool, Nova Scotia an RASC observing program with certificate for beginning observers © Royal Astronomical Society of Canada 2016 Explore the Moon (binocular version) Table of Contents Preface...............................................................................................2 Introduction: Why Observe the Moon?.............................................3 Suggested Resources .........................................................................3 Planning and Observing ....................................................................3 Recording Observations and Applying for your Certificate .............5 Maps ..................................................................................................6 Feature Index Table.........................................................................10 Preface The idea behind Explore the Moon (EtM) surfaced in 2011–12 during casual conversations between RASC members Dave Chapman (Halifax Centre), Patrice Scattolin (Centre francophone de Montréal), and Kevin Dunphy (New Brunswick Centre). We were looking for a more elementary introduction to lunar observing than the more daunting RASC Isabel Williamson Lunar Observing Program (directed at intermediate-to-advanced observers. We also identified a general need for a beginner’s observing program one step up from the novice-level Explore the Universe. Such a program would provide an opportunity for observers to gain -
Sources of Extraterrestrial Rare Earth Elements: to the Moon and Beyond
resources Article Sources of Extraterrestrial Rare Earth Elements: To the Moon and Beyond Claire L. McLeod 1,* and Mark. P. S. Krekeler 2 1 Department of Geology and Environmental Earth Sciences, 203 Shideler Hall, Miami University, Oxford, OH 45056, USA 2 Department of Geology and Environmental Earth Science, Miami University-Hamilton, Hamilton, OH 45011, USA; [email protected] * Correspondence: [email protected]; Tel.: 513-529-9662; Fax: 513-529-1542 Received: 10 June 2017; Accepted: 18 August 2017; Published: 23 August 2017 Abstract: The resource budget of Earth is limited. Rare-earth elements (REEs) are used across the world by society on a daily basis yet several of these elements have <2500 years of reserves left, based on current demand, mining operations, and technologies. With an increasing population, exploration of potential extraterrestrial REE resources is inevitable, with the Earth’s Moon being a logical first target. Following lunar differentiation at ~4.50–4.45 Ga, a late-stage (after ~99% solidification) residual liquid enriched in Potassium (K), Rare-earth elements (REE), and Phosphorus (P), (or “KREEP”) formed. Today, the KREEP-rich region underlies the Oceanus Procellarum and Imbrium Basin region on the lunar near-side (the Procellarum KREEP Terrain, PKT) and has been tentatively estimated at preserving 2.2 × 108 km3 of KREEP-rich lithologies. The majority of lunar samples (Apollo, Luna, or meteoritic samples) contain REE-bearing minerals as trace phases, e.g., apatite and/or merrillite, with merrillite potentially contributing up to 3% of the PKT. Other lunar REE-bearing lunar phases include monazite, yittrobetafite (up to 94,500 ppm yttrium), and tranquillityite (up to 4.6 wt % yttrium, up to 0.25 wt % neodymium), however, lunar sample REE abundances are low compared to terrestrial ores. -
January 2021 Click on Images in This Issue for Hyperlinks
A publication of the Lunar Section of ALPO Edited by David Teske: [email protected] 2162 Enon Road, Louisville, Mississippi, USA Back issues: http://www.alpo-astronomy.org/ Online readers, January 2021 click on images In This Issue for hyperlinks Announcements 2 Lunar Calendar October 2020 3 An Invitation to Join ALPO 3 Observations Received 4 By the Numbers 6 Submission Through the ALPO Image Achieve 7 When Submitting Observations to the ALPO Lunar Section 8 page 83 Call For Observations Focus-On 8 Focus-On Announcement 9 Schickard Sunrise Patch, S. Berté 10 Another Dome Home, R. Hill 11 Some Wonders on the Shores of Mare Crisium, A. Anunziato 12 Lunar Topographic Studies Program: Banded Craters 14 A Fleet Vision of Posidonius Y on Dorsa Smirnov, A. Anunziato 20 Aristarchus Plateau Region, H. Eskildsen 21 Focus On: The Lunar 100, Features 41-50, J. Hubbell 22 Lunar 41-50, a Personal View, A. Anunziato 25 Wargentin, R. Hays, Jr. 37 Recent Topographic Studies 79 Lunar Geologic Change Detection Program, T. Cook 119 page 84 Key to Images in this Issue 131 A very Happy New Year to all. We look forward to a good year ahead. Thank you contributors for your many contributions to this issue of The Lunar Observer. Your excellent submissions is what makes this newsletter possible. If you are reading this issue, welcome aboard! Perhaps you would like to contribute your own lunar observations to us. You can contribute observations if you are not a member of ALPO, but we sure would like you to consider becoming a member (yearly rates start at only $18.00, a great deal!). -
Constraining the Evolutionary History of the Moon and the Inner Solar System: a Case for New Returned Lunar Samples
Constraining the Evolutionary History of the Moon and the Inner Solar System: A Case for New Returned Lunar Samples The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Tartèse, Romain, et al. "Constraining the Evolutionary History of the Moon and the Inner Solar System: A Case for New Returned Lunar Samples." Space Science Reviews, 215 (December 2019): 54. © 2019, The Author(s). As Published http://dx.doi.org/10.1007/s11214-019-0622-x Publisher Springer Science and Business Media LLC Version Final published version Citable link https://hdl.handle.net/1721.1/125329 Terms of Use Creative Commons Attribution 4.0 International license Detailed Terms https://creativecommons.org/licenses/by/4.0/ Space Sci Rev (2019) 215:54 https://doi.org/10.1007/s11214-019-0622-x Constraining the Evolutionary History of the Moon and the Inner Solar System: A Case for New Returned Lunar Samples Romain Tartèse1 · Mahesh Anand2,3 · Jérôme Gattacceca4 · Katherine H. Joy1 · James I. Mortimer2 · John F. Pernet-Fisher1 · Sara Russell3 · Joshua F. Snape5 · Benjamin P. Weiss6 Received: 23 August 2019 / Accepted: 25 November 2019 / Published online: 2 December 2019 © The Author(s) 2019 Abstract The Moon is the only planetary body other than the Earth for which samples have been collected in situ by humans and robotic missions and returned to Earth. Scien- tific investigations of the first lunar samples returned by the Apollo 11 astronauts 50 years ago transformed the way we think most planetary bodies form and evolve. Identification of anorthositic clasts in Apollo 11 samples led to the formulation of the magma ocean concept, and by extension the idea that the Moon experienced large-scale melting and differentiation. -
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. -
June 2019 the Monthly Newsletter of the Bays Mountain Astronomy Club
June 2019 The Monthly Newsletter of the Bays Mountain Astronomy Club More on Edited by Adam Thanz this image. See FN1 Chapter 1 Cosmic Reflections William Troxel - BMAC Chair More on this image. See FN2 William Troxel More on Cosmic Reflections this image. See FN3 Greetings BMACer’s. I wanted to recap the events of May. Those have not attended in the past I invite you to consider coming out of you that were able to attend got to see and hear very in 2020! wonderful science fair presentations from the young men and This month I want to introduce 3 more terms for your working women from Sullivan South High School who are our future astronomy vocabulary. scientists and astronomers! Each presentation was well planned and presented. Each young person shared their goal, method Aurora - (noun) - An aurora is formed when charged particles and results. After each presentation, the students welcomed emitted from the Sun during a solar flare penetrate the Earth’s comments and questions from those present. I want to thank magnetic shield and collide with atoms and molecules in the Tom Rutherford for bringing his students, it is always a wonderful atmosphere. These collisions results in countless little bursts of meeting. Every May we invite Tom's young men and women to light called photons. present their projects. It is one meeting that many of you have told me that you enjoy each year. I agree with you. Eclipse - (noun) - the total or partial obscuring of one celestial body by another. Sentence use: The solar eclipse was viewed by The second event this month was the annual Astronomy Day. -
Hls-Ug-001 Human Landing System Lunar Thermal Analysis Guidebook
HLS-UG-001 BASELINE RELEASE National Aeronautics and EFFECTIVE DATE: JANUARY 04, 2021 Space Administration HUMAN LANDING SYSTEM LUNAR THERMAL ANALYSIS GUIDEBOOK Publicly Available: Release to Public Websites Requires Approval of Chief, Office of Primary Responsibility, and approval via the Scientific and Technical Information (STI) process, if applicable The electronic version is the official approved document. Verify this is the correct version before use. Human Landing System Lunar Thermal Analysis Guidebook January 2021 Revision: Baseline Release Document No: HLS-UG-01 Effective Date: January 04, 2021 Page: 1 of 147 Title: Human Landing System Lunar Thermal Analysis Guidebook REVISION AND HISTORY PAGE Revision Change Effective Description No. No. Date - HLS- Baseline Release (Reference HCB.07.01.2020) 01/04/2021 C0064 The electronic version is the official approved document. Verify this is the correct version before use. Human Landing System Lunar Thermal Analysis Guidebook January 2021 Revision: Baseline Release Document No: HLS-UG-01 Effective Date: January 04, 2021 Page: 2 of 147 Title: Human Landing System Lunar Thermal Analysis Guidebook TABLE OF CONTENTS SECTION PAGE 1.0 INTRODUCTION ................................................................................................. 10 PURPOSE ........................................................................................................... 10 SCOPE ................................................................................................................ 10 CHANGE -
Science Concept 3: Key Planetary Processes Are Manifested in the Diversity of Lunar Crustal Rocks
Science Concept 3: Key Planetary Processes are Manifested in the Diversity of Lunar Crustal Rocks Science Concept 3: Key planetary processes are manifested in the diversity of crustal rocks Science Goals: a. Determine the extent and composition of the primary feldspathic crust, KREEP layer, and other products of differentiation. b. Inventory the variety, age, distribution, and origin of lunar rock types. c. Determine the composition of the lower crust and bulk Moon. d. Quantify the local and regional complexity of the current lunar crust. e. Determine the vertical extent and structure of the megaregolith. INTRODUCTION Formation and Evolution of the Moon The Moon is a unique environment, preserving crucial information about the early history and later evolution of the solar system. The lack of major surficial tectonic processes within the past few billion years or so, as well as the lack of significant quantities of surface water, have allowed for excellent preservation of the lithologies and geomorphological features that formed during the major planetary formation events. Fundamental discoveries during the Apollo program showed that the Moon is made up of a variety of volcanic and impact rock types that exhibit a particular range of chemical and mineralogical compositions. The key planetary processes conveyed by this diversity include planetary differentiation, volcanism, and impact cratering. Analysis of Apollo, Luna, and lunar meteoritic samples, as well as orbital data from a series of lunar exploration missions, generated geophysical models that strove to tell the story of the Moon. However, such models are restricted in the sense that they are based on information gathered from the samples that have so far been acquired. -
Farouk El-Baz Papers, 1927-2012
Farouk El-Baz Papers, 1927-2012 Finding aid prepared by Smithsonian Institution Archives Smithsonian Institution Archives Washington, D.C. Contact us at [email protected] Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Descriptive Entry.............................................................................................................. 1 Names and Subjects ...................................................................................................... 2 Container Listing ............................................................................................................. 4 Farouk El-Baz Papers https://siarchives.si.edu/collections/siris_arc_390696 Collection Overview Repository: Smithsonian Institution Archives, Washington, D.C., [email protected] Title: Farouk El-Baz Papers Identifier: Accession 17-262 Date: 1927-2012 Extent: 88.891 cu. ft. (80 record storage boxes) (14 tall document boxes) (1 16x20 box) Creator:: El-Baz, Farouk Language: Language of Materials: English Administrative Information Prefered Citation Smithsonian Institution Archives, Accession 17-262, Farouk El-Baz Papers Use Restriction Restricted for duration of Farouk El-Baz's lifetime without written permission from Donor. Transferring office; 2/27/1983 Agreement of Transfer; Contact reference staff for details. Descriptive Entry Farouk