AL – Lunar II Observation David M. Douglass 2017-12-07 Tempe, Arizona

Total Page:16

File Type:pdf, Size:1020Kb

AL – Lunar II Observation David M. Douglass 2017-12-07 Tempe, Arizona AL – Lunar II Observation David M. Douglass 2017-12-07 Tempe, Arizona #038 Mersenius (Crater and Rimae) #043 Montes Cordillera #045 Montes Rock https://en.wikipedia.org/wiki/Mersenius_(crater) Mersenius is a lunar crater that is located to the west of the Mare Humorum, in the southwestern part of the Moon. To the southwest is the crater Cavendish, and to the south-southeast lies Liebig. Mersenius is 84 kilometers in diameter and 2.3 kilometers deep. It is from the Nectarian period, 3.92 to 3.85 billion years ago.[1] The rim of Mersenius is heavily worn, especially in the low northern section. The crater Mersenius N lies across the southwestern rim. The interior has been flooded by basaltic lava, which bulges upwards forming a convex domed shape with an estimated height of 450 metres relative to the floor edges. This was most likely formed by lava upwelling beneath the surface. There are several tiny craterlets across the floor surface, but little in the way of a central peak. At least two faint rilles lie along the surface of the floor.[2][3] To the east of the crater on the surface and edges of the Mare Humorum is a rille system designated Rimae Mersenius. These rilles are generally parallel and run to the north-northeast for a length of about 230 kilometers.[2] https://en.wikipedia.org/wiki/Montes_Cordillera Montes Cordillera is a mountain range on the Moon. This feature forms the outer wall of peaks that surround the Mare Orientale impact basin, the inner ring being formed by the Montes Rook.[1] The center of the range is located at selenographic coordinates 17.5° S, 81.6° W, and the diameter is 574 km (357 mi). https://en.wikipedia.org/wiki/Montes_Rook Montes Rook is a ring-shaped mountain range that lies along the western limb of the Moon, crossing over to the far side. It completely encircles the Mare Orientale, and forms part of a massive impact basin feature. This range in turn is encircled by the larger Montes Cordillera, which is separated from the Montes Rook by a rugged, ring-shaped plain. .
Recommended publications
  • 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.
    [Show full text]
  • Lroc and Other Remote Sensing Studies of Pyroclastic Deposits in the Mare Humorum Region
    41st Lunar and Planetary Science Conference (2010) 1583.pdf LROC AND OTHER REMOTE SENSING STUDIES OF PYROCLASTIC DEPOSITS IN THE MARE HUMORUM REGION. B.R. Hawke 1, T.A. Giguere 1,2 , S.J. Lawrence 3, B.A. Campbell 4, L.R. Gaddis 5, J. O. Gustafson 6, J.J. Hagerty 5, C.A. Peterson 1, M.S. Robinson 3 and the LROC Team, 1Hawaii Institute of Geophysics and Planetology, Univ. of Hawaii, Honolulu, HI 96822, 2Intergraph Corporation, P.O. Box 75330, Kapolei, HI 96707, 3School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85281, 4Center for Earth and Planetary Studies, National Air and Space Museum, Washing- ton, D.C. 20560, 5U.S. Geological Survey, Astrogeology Science Center, 2255 N. Gemini Drive, Flags- taff, AZ 86001, 6Dept. of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14853. Introduction: In recent years, interest in image cube served as the basis for the produc- lunar dark mantle deposits of pyroclastic origin tion of a number of data products, including opt- has greatly increased. This interest is due partly ical maturity (OMAT) images and FeO and TiO 2 to the results of intensive studies of lunar pyroc- maps [8, 9]. In addition, Earth-based telescopic lastic glasses [e.g., 1, 2], as well as remote sens- near-IR reflectance spectra obtained for various ing investigations of both localized and regional units in the Humorum region were utilized in pyroclastic deposits [3, 4]. Laboratory analyses this investigation. The depolarized 12.6-cm and of pyroclastic spheres from several regional de- 70-cm radar images recently obtained by Camp- posits show that this volcanic debris had a bell et al .
    [Show full text]
  • Thumbnail Index
    Thumbnail Index The following five pages depict each plate in the book and provide the following information about it: • Longitude and latitude of the main feature shown. • Sun’s angle (SE), ranging from 1°, with grazing illumination and long shadows, up to 72° for nearly full Moon conditions with the Sun almost overhead. • The elevation or height (H) in kilometers of the spacecraft above the surface when the image was acquired, from 21 to 116 km. • The time of acquisition in this sequence: year, month, day, hour, and minute in Universal Time. 1. Gauss 2. Cleomedes 3. Yerkes 4. Proclus 5. Mare Marginis 79°E, 36°N SE=30° H=65km 2009.05.29. 05:15 56°E, 24°N SE=28° H=100km 2008.12.03. 09:02 52°E, 15°N SE=34° H=72km 2009.05.31. 06:07 48°E, 17°N SE=59° H=45km 2009.05.04. 06:40 87°E, 14°N SE=7° H=60km 2009.01.10. 22:29 6. Mare Smythii 7. Taruntius 8. Mare Fecunditatis 9. Langrenus 10. Petavius 86°E, 3°S SE=19° H=58km 2009.01.11. 00:28 47°E, 6°N SE=33° H=72km 2009.05.31. 15:27 50°E, 7°S SE=10° H=64km 2009.01.13. 19:40 60°E, 11°S SE=24° H=95km 2008.06.08. 08:10 61°E, 23°S SE=9° H=65km 2009.01.12. 22:42 11.Humboldt 12. Furnerius 13. Stevinus 14. Rheita Valley 15. Kaguya impact point 80°E, 27°S SE=42° H=105km 2008.05.10.
    [Show full text]
  • The Isabel Williamson Lunar Observing Program
    The Isabel Williamson Lunar Observing Program by The RASC Observing Committee Revised Third Edition September 2015 © Copyright The Royal Astronomical Society of Canada. All Rights Reserved. TABLE OF CONTENTS FOR The Isabel Williamson Lunar Observing Program Foreword by David H. Levy vii Certificate Guidelines 1 Goals 1 Requirements 1 Program Organization 2 Equipment 2 Lunar Maps & Atlases 2 Resources 2 A Lunar Geographical Primer 3 Lunar History 3 Pre-Nectarian Era 3 Nectarian Era 3 Lower Imbrian Era 3 Upper Imbrian Era 3 Eratosthenian Era 3 Copernican Era 3 Inner Structure of the Moon 4 Crust 4 Lithosphere / Upper Mantle 4 Asthenosphere / Lower Mantle 4 Core 4 Lunar Surface Features 4 1. Impact Craters 4 Simple Craters 4 Intermediate Craters 4 Complex Craters 4 Basins 5 Secondary Craters 5 2. Main Crater Features 5 Rays 5 Ejecta Blankets 5 Central Peaks 5 Terraced Walls 5 ii Table of Contents 3. Volcanic Features 5 Domes 5 Rilles 5 Dark Mantling Materials 6 Caldera 6 4. Tectonic Features 6 Wrinkle Ridges 6 Faults or Rifts 6 Arcuate Rilles 6 Erosion & Destruction 6 Lunar Geographical Feature Names 7 Key to a Few Abbreviations Used 8 Libration 8 Observing Tips 8 Acknowledgements 9 Part One – Introducing the Moon 10 A – Lunar Phases and Orbital Motion 10 B – Major Basins (Maria) & Pickering Unaided Eye Scale 10 C – Ray System Extent 11 D – Crescent Moon Less than 24 Hours from New 11 E – Binocular & Unaided Eye Libration 11 Part Two – Main Observing List 12 1 – Mare Crisium – The “Sea of Cries” – 17.0 N, 70-50 E;
    [Show full text]
  • Physics of the Moon
    NASA TECHNICAL NOTE -cNASA TN D-2944 e. / PHYSICS OF THE MOON SELECTED TOPICS CONCERNING LUNAR EXPLORATION Edited by George C. ‘Bucker and Henry E. Siern George C. Marsball Space Flight Center Hzmtsville, A Za: NATIONAL AERONAUTICSAND SPACEADMINISTRATION - WASHINGTON;D. C. TECH LIBRARY KAFB. NM llL5475b NASA TN D-2944 PHYSICS OF THE MOON SELECTED TOPICS CONCERNING LUNAR EXPLORATION Edited by George C. Bucher and Henry E. Stern George C. Marshall Space Flight Center Huntsville, Ala. NATIONAL AERONAUTICS AND SPACE ADMINISTRATION For sole by the Clearinghouse for Federal Scientific and Technical information Springfield, Virginia 22151 - Price 56.00 I - TABLE OF CONTENTS Page SUMMA=. 1 INTRODUCTION. i SECTION I. CHARACTERISTICS OF THE MOON. i . 3 Chapter 1. The Moon’s .History, by Ernst Stuhlinger. 5 Chapter 2. Physical Characteristics of the Lunar Surface, by John Bensko . 39 Chapter 3. The’ Lunar Atmosphere, by Spencer G. Frary . , 55 Chapter 4. Energetic Radiation Environment of the Moon, by Martin 0. Burrell . 65 Chapter 5. The Lunar Thermal Environment , . 9i The Thermal Model of the Moon, by Gerhard B. Heller . 91 p Thermal Properties of the Moon as a Conductor of Heat,byBillyP. Jones.. 121 Infrared Methods of Measuring the Moon’s Temperature, by Charles D. Cochran. 135 SECTION II. EXPLORATION OF THE MOON . .I59 Chapter I. A Lunar Scientific Mission, by Daniel Payne Hale. 161 Chapter 2. Some Suggested Landing Sites for Exploration of the Moon, by Daniel Payne Hale. 177 Chapter 3. Environmental Control for Early Lunar Missions, by ‘Herman P. Gierow and James A. Downey, III . , . .2i I Chapter 4.
    [Show full text]
  • The Mare Humorum Region of the Moon: New Optical, Compositional, and Geological Inferences from Clementine
    Lunar and Planetary Science XXVIII 1621.PDF THE MARE HUMORUM REGION OF THE MOON: NEW OPTICAL, COMPOSITIONAL, AND GEOLOGICAL INFERENCES FROM CLEMENTINE. P.D. Martin, P.C. Pinet, and S.D. Chevrel; UMR5562/CNRS, Observatoire Midi-Pyrénées, 14 Avenue E. Belin, F-31400 Toulouse, FRANCE. Introduction. The present paper deals with a surface unit in the northwestern highlands. This detailed assessment of the surface properties in unit, located in the close vicinity of Mersenius P the Mare Humorum region of the Moon. Spec- and S, is interpreted to be composed of pure tral investigations have been made by means of anorthosite on the basis of its very low Fe the processing and analysis of Clementine abundance (<3%). This conclusion corroborates UV/VIS multispectral data, at 340m spatial those derived from analyses of spot spectra resolution, in order to provide new insights into conducted by (2, 3) in the mare-bounding ring both optical/compositional heterogeneities and region, with the additional information of ex- emplacement of the geological units within the tension of this unit. Concerning variations in basin interior and vicinity. The spatial coverage fractional abundances of the highland units sur- of our image-cube (more than 2.6 million spec- rounding Humorum, they are proposed to be the tra) maps the western part of the basin, up to result of varied proportions of anorthosite. the longitude of Vitello E. An extended highland area is also mapped west of the basin, including Evidence for pyroclastic deposits. Among the the western portion of the mare-bounding ring. three major spectral units representative of the Spatially coherent spectral units have been highland materials, the area located northwest identified with the application of a new meth- of Mersenius toward Herigonius and Letronne odology, consisting in a coupled approach of a regions, which is low in topography, corre- principal component analysis and an iterative sponds to intermediate-albedo terrains and ex- linear mixing modeling.
    [Show full text]
  • Appendix a Luna and Telescopes
    Appendix A Luna and Telescopes Exploring Luna’s surface is one of the easiest things to do in this book. You have a few options when you do this. It has the advan- tage of being the only moon visible to the naked eyes. (You might be able to just see the Galilean moons, but you would hardly be able to do anything beyond just see them.) So the next step is to consider an instrument. Be aware, this is not a general purpose guide. If you want one, look at the local library or bookseller for a copy of “NightWatch” as the book is excellent, has a sturdy plastic spiral for easy hands- free use and will serve you in more ways than just binoculars for many years to come. That being said all my recommendations in this chapter are for viewing ONLY OUR MOON. Most other moons will be pinpricks, so if you can see them at all you did the best you could. If you also wish to view nebula, galaxies, birds, be rude to your neighbors, and so forth, do your homework. Binoculars The first option is to go with binoculars. These come in a variety of sizes, which is listed as two numbers. The first is magnification and the second is aperture size (in mm). Common sizes include 7 × 35, 7 × 42, 8 × 40, 9 × 50 or even 10 × 50. For dim object you will want the bigger sizes, but the moon is not a dim object. Even a 7 × 35 will produce some pretty spectacular views.
    [Show full text]
  • Astrogeolog1c Studies
    i ASTROGEOLOG1C STUDIES PART A LUNAR AND PLANETARY INVESTIGATIONS DEPARTMENT OF THE INTERIOR b UNITED STATES GEOLOGICAL SURVEY I ASTROGEOLOGIC STUDIES Alq_AL PROGRESS P,EPOKT August 25, 1962 to July I, 1963 PART A: LIYblAR AND PLANETARY INVESTIGATIONS May 1964 This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature. It should not be quoted without permission. This report concerns work done on behalf of the /J National Aeronautics and Space Administration. _/ DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CONTENTS Page PART A--LUNARAND PLANETARY INVESTIGATIONS Introduction I. Stratigraphy and structure of the Montes Apenninus Quadrangle of the Moon, by R. J. Hackman Introduction 1 Stratigraphy I Structure and structural history- 6 References-- 8 2. The geology of the Timocharis Quadrangle, by M. H. Cart ...... Introduction .................................. 9/ Summary of stratigraphy ..... 10 Rays as an index of age ....................... 12 Structures of large craters 17 Secondary craters 21 t References ...................................... 22 3. Progress in mapping the Taruntius Quadrangle, by D. E. J Wilhelm ................ 24 _" Introduction ......................... 24 i Stratigraphy ..... 24 Pre-lmbrian System ........................... 26 Imbrian or pre-lmbrian System 26 Regional material .................................... 26 Palus Somni material ................................. 27 CONTENTS--Continued Page Imbrian System- 27 Mare material
    [Show full text]
  • Brief Description of the Various Crater Types Complex Craters
    Brief Description of the various crater types Complex craters: are according to the standard model normal impact craters with a diameter larger than 20 km. They have terraced walls, a central peak or central mountains, partial landslides and outside the main crater a region with melted material that was ejected out of the crater as well as secondary craters. Floor Fractured craters: FF craters are normal impact craters that have a distinct fissure / rille system on the crater floor. They usually have a diameter greater than 40 km and are almost exclusively on the outskirts of the large Moon Mare. Their origin can be briefly described as follows: while the lava flows flooded the impact basins there was also some magma pressed through cracks in the lunar mantle under these FF craters. Under the immense pressure of the magma, the crater floors were raised and bended. When the stress in the slow moving or already solidified lava inside the crater was too big, the fissures in the crater floor formed - usually concentrically in the rim of the crater. A prototype of this is the crater Pitatus in the southern region of Mare Nubium. Occasionally some lava was extruded through these fissures then, or as in the case of Alphonsus, there were some regions with pyroclastic volcanism and ash deposits. In principle, the FF craters are formed due to a combination of intrusive and effusive / pyroclastic volcanism. Later - but nevertheless while the impact basins were flooded - the Mare shields in the center of the basin subsided under the immense weight of up to 5 km thick lava.
    [Show full text]
  • Hard Copy (HC) Microfiche
    GPO PRICE $ CFSTI PRICE(S) $ Hard copy (HC) Microfiche (MF) ff 653 ,July 85 Communications of the LUNAR AND PLANETARY LABORATORY Volume 3 Number 50 THE UNIVERSITY OF ARIZONA !965 at 4k Communications of the Lunar and Planetary Laboratory These Communications contain the shorter publications and reports by the staff of the Lunar and Planetary Laboratory. They may be either original contributions, reprints of articles published in professional journals, preliminary reports, or announcements. Tabular material too bulky or specialized for regular journals is included if future use of such material appears to warrant it. The Communications are issued as separate numbers, but they are paged and indexed by volumes. The Communications are mailed to observatories and to laboratories known to be engaged in planetary, interplanetary or geophysical research in exchange for their reports and publica- tions. The University of Arizona Press can supply at cost copies to other libraries and interested persons. The University of Arizona GE_RD P. KUIPER, Director Tucson, Arizona Lunar and Planetary Laboratory Published with the support of the National Aeronautics and Space Administration Library of Congress Catalog Number 62-63619 NO. 50 THE SYSTEM OF LUNAR CRATERS, QUADRANT III by D. W. G. ARTHUR, ALICE P. AGNIERAY, RUTH H. PELLICORI, C. A. WOOD, AND T. WELLER February 25, 1965 ABSTRACT The designation, diameter, position, central peak information, and state of completeness are listed for each discernible crater with a diameter exceeding 3.5 km in the third lunar quadrant. The catalog contains about 5200 items and is illustrated by a map in I1 sections. his Communication is the third part of The Sys- on the averted lunar hemisphere, and therefore, these tem oJ Lunar Craters, which is a catalog in four are not listed in the catalog.
    [Show full text]
  • Lunar 1000 Challenge List
    LUNAR 1000 CHALLENGE A B C D E F G H I LUNAR PROGRAM BOOKLET LOG 1 LUNAR OBJECT LAT LONG OBJECTIVE RUKL DATE VIEWED BOOK PAGE NOTES 2 Abbot 5.6 54.8 37 3 Abel -34.6 85.8 69, IV Libration object 4 Abenezra -21.0 11.9 55 56 5 Abetti 19.9 27.7 24 6 Abulfeda -13.8 13.9 54 45 7 Acosta -5.6 60.1 49 8 Adams -31.9 68.2 69 9 Aepinus 88.0 -109.7 Libration object 10 Agatharchides -19.8 -30.9 113 52 11 Agrippa 4.1 10.5 61 34 12 Airy -18.1 5.7 63 55, 56 13 Al-Bakri 14.3 20.2 35 14 Albategnius -11.2 4.1 66 44, 45 15 Al-Biruni 17.9 92.5 III Libration object 16 Aldrin 1.4 22.1 44 35 17 Alexander 40.3 13.5 13 18 Alfraganus -5.4 19.0 46 19 Alhazen 15.9 71.8 27 20 Aliacensis -30.6 5.2 67 55, 65 21 Almanon -16.8 15.2 55 56 22 Al-Marrakushi -10.4 55.8 48 23 Alpetragius -16.0 -4.5 74 55 24 Alphonsus -13.4 -2.8 75 44, 55 25 Ameghino 3.3 57.0 38 26 Ammonius -8.5 -0.8 75 44 27 Amontons -5.3 46.8 48 28 Amundsen -84.5 82.8 73, 74, V Libration object 29 Anaxagoras 73.4 -10.1 76 4 30 Anaximander 66.9 -51.3 2 31 Anaximenes 72.5 -44.5 3 32 Andel -10.4 12.4 45 33 Andersson -49.7 -95.3 VI Libration object 34 Angstrom 29.9 -41.6 19 35 Ansgarius -12.7 79.7 49, IV Libration object 36 Anuchin -49.0 101.3 V Libration object 37 Anville 1.9 49.5 37 38 Apianus -26.9 7.9 55 56 39 Apollonius 4.5 61.1 2 38 40 Arago 6.2 21.4 44 35 41 Aratus 23.6 4.5 22 42 Archimedes 29.7 -4.0 78 22, 12 43 Archytas 58.7 5.0 76 4 44 Argelander -16.5 5.8 63 56 45 Ariadaeus 4.6 17.3 35 46 Aristarchus 23.7 -47.4 122 18 47 Aristillus 33.9 1.2 69 12 48 Aristoteles 50.2 17.4 48 5 49 Armstrong 1.4 25.0 44
    [Show full text]
  • Lunar and Planetary Science XXIX 1547.Pdf
    Lunar and Planetary Science XXIX 1547.pdf HIGHLAND CRUST DIVERSITY AND MARE-HIGHLAND MIXING RELATIONSHIPS IN THE MARE HUMORUM REGION OF THE MOON: A CLOSER LOOK WITH UV/VIS CLEMENTINE MULTISPECTRAL IMAGES: P. D. Martin1, P. C. Pinet2, S. D. Chevrel2, and Y. H. Daydou2 (1Planetary Geosciences Division, HIGP/SOEST, Univ. of Hawaii, Honolulu, Hawaii 96822; [email protected];2UMR 5562/CNRS, Observatoire Midi-Pyrénées, 14 Av. E. Belin, F-31400 Toulouse, France). Introduction: Following the results issued from contributions (2), might indicate the presence of crypto- Clementine UV/VIS multispectral analyses at 340m per maria, in consistency with the conclusions of (6), or materi- pixel spatial resolution (1,2), we present in Figure 1 three als partially covered by crater ejecta or basaltic flows, such schematic cross sections through mare-highland boundaries, as exposed remnants of regional deposits. Measurements which give insights into the stratigraphic properties within acquired in the infrared would allow to bring answer ele- the Humorum basin area. Regions of particular interest are ments for confirming the presence of such undefined depos- the mare-highland western boundaries, the northwestern its. The low radar returns obtained in this area might indicate highlands, and the low-albedo unit in the highlands west of a deficit of fragments of size 1 to 50-cm on or near the sur- the basin. Spatially coherent spectral units have been identi- face, or the presence of materials having a dielectric constant fied, characterized, and mapped according to combined spe- different from those of typical highland materials (4,7). cific spectral characteristics such as iron and titanium con- The cross-section in Figure 1b indicates the pres- tent, soil maturity, and fractional abundance with respect to ence of potential cryptomare (e.g., 8) materials located be- selected spectral end-members (1).
    [Show full text]