Binocular Universe: Some Lunar Lakes, Bays, and Marshes June 2012 Phil Harrington
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Petrography, Geochemistry, and Provenance
Lunar and Planetary Science XXXIV (2003) 1454.pdf THE APOLLO 16 MARE COMPONENT: PETROGRAPHY, GEOCHEMISTRY, AND PROVENANCE. R. A. Zeigler, L. A. Haskin, R. L. Korotev, B. L. Jolliff, and J. J. Gillis, Dept. of Earth and Planetary Sciences, Washington University in St. Louis, Campus Box 1169, 1 Brookings Dr., St. Louis, MO 63116 ([email protected]). Introduction: The A16 (Apollo16) site in the lunar ported may be similar to our VLT samples 65703,9-13 nearside highlands is 220 km from the nearest mare. and 62243,10-22. High-Al basalt 60053,2-9 and the Thus it is no surprise that mare basalt samples are un- high-Al basalts previously reported from A16 samples common at the site. Here, we present the petrography are similar only in being aluminous and low in TiO2. and geochemistry of 5 new mare basalt samples found at The VHT picritic glass 60603,10-16 is unlike anything the A16 site. We also discuss possible provenances of previously reported from the A16 collection. all A16 mare basalt samples using high-resolution global Transport mechanisms: We propose that the mare data for the distribution of Fe and Ti on the lunar surface basalts found at the A16 site were transported there derived from Clementine UV-VIS data [1-2]. through post-basin lateral mixing. Other potential meth- Background: The maria nearest to the A16 site are ods do not seem feasible: Pyroclastic eruption: Sinus Asperitatis (220 km) and Mare Nectaris (~400 According to theoretical models, pyroclastic eruptions km). The A16 regolith consists of basin ejecta from Nec- have an effective eruption limit of <300 km [17], less taris and Imbrium, and possibly Serenitatis, mixed with than half the distance to the nearest known pyroclastic pre-Nectarian regolith [3-4]. -
8.5 X 13.5 Doublelines.P65
Cambridge University Press 978-0-521-74128-6 - Exploring the Solar System with Binoculars: A Beginner’s Guide to the Sun, Moon, and Planets Stephen James O’Meara’s Index More information Index Adams, John Couch, 96 Carrington, Richard C., 15 degree of condensation (DC) of, Agesinax, 24 Carroll, Lewis, 60 111–112 Aionwantha (Hiawatha), 45 Ceres, 70, 99–101 estimating the brightness of, Airy, George Biddell, 50, 51, 55 discovery and history as a planet, 111–112 Alcock, George, 116 99–100 In–Out method, 111 Allen, Richard Hinckley, 136 general description of, 99, Modified–Out method, 111–112 Alphonsus VI (King of Portugal), 104 100–101 experience helps in observing, 112 Andersen, Hans Christian, 92 how to find, 101 flaring in brightness, 111 Arago, Francois, 59 Chaikin, Andrew, 54 how to locate and identify, 110 Araki, Genichi, 116 Challis, James, 50 in history, relating to, 103–108 Arend, Silvio, 115 Chambers, George F., 8, 19 King David, 103 Aristotle, 65 Cheshire Cat, 60 Melville’s Moby-Dick, 107–108 Arlt, Rainer, 132 Children of God (cult), 108 Napoleon, 106 Arrehenius, Svente, 78, 79 Chinese Catalogue (Biot’s), 131–132 Shakespeare’s Julius Caesar, 103–104 Arter, T. R., 131 Cicero (Roman emperor), 77 the broadside of the comets of Asteroid Belt, 101 City of God, The, 90 1680 and 1682, 104 brightest objects in, 101–102 Collins, Peter, 116 the death of Julius Caesar, 104 asteroids Cometographia, 103 the Middle Ages, 104 2003 EH1, 131 comets, 103–117 the Old Testament?, 103 3200 Phaeton, 142 1P (Halley), 103, 109, 114–115, the whaling ship -
Sky and Telescope
SkyandTelescope.com The Lunar 100 By Charles A. Wood Just about every telescope user is familiar with French comet hunter Charles Messier's catalog of fuzzy objects. Messier's 18th-century listing of 109 galaxies, clusters, and nebulae contains some of the largest, brightest, and most visually interesting deep-sky treasures visible from the Northern Hemisphere. Little wonder that observing all the M objects is regarded as a virtual rite of passage for amateur astronomers. But the night sky offers an object that is larger, brighter, and more visually captivating than anything on Messier's list: the Moon. Yet many backyard astronomers never go beyond the astro-tourist stage to acquire the knowledge and understanding necessary to really appreciate what they're looking at, and how magnificent and amazing it truly is. Perhaps this is because after they identify a few of the Moon's most conspicuous features, many amateurs don't know where Many Lunar 100 selections are plainly visible in this image of the full Moon, while others require to look next. a more detailed view, different illumination, or favorable libration. North is up. S&T: Gary The Lunar 100 list is an attempt to provide Moon lovers with Seronik something akin to what deep-sky observers enjoy with the Messier catalog: a selection of telescopic sights to ignite interest and enhance understanding. Presented here is a selection of the Moon's 100 most interesting regions, craters, basins, mountains, rilles, and domes. I challenge observers to find and observe them all and, more important, to consider what each feature tells us about lunar and Earth history. -
For Immediate Release: TWO GOOGLE LUNAR XPRIZE
Media Contact: Kyoko Yonezawa [email protected] For Immediate Release: TWO GOOGLE LUNAR XPRIZE TEAMS ANNOUNCE RIDESHARE PARTNERSHIP FOR MISSION TO THE MOON IN 2016 Team HAKUTO (Japan) and Team Astrobotic (U.S.) Plan Cooperative Launch in Pursuit of $30 Million Prize to Land a Private Spacecraft on the Lunar Surface TOKYO, Japan (February 24, 2015) – HAKUTO, the only Japanese team competing for the $30 million Google Lunar XPRIZE, has announced a contract with fellow competitor, Astrobotic, based in Pittsburgh, Pa., to carry a pair of rovers to the moon. Astrobotic plans to launch its Google Lunar XPRIZE mission on a SpaceX Falcon 9 rocket from Cape Canaveral, Fla., during the second half of 2016. HAKUTO’s twin rovers, Moonraker and Tetris, will piggyback on Astrobotic's Griffin lander to reach the lunar surface. Upon touchdown, the rovers will be released simultaneously with Astrobotic’s Andy rover, developed by Carnegie Mellon University, travel 500 meters on the moon’s surface and send high-definition images and video back to Earth, all in pursuit of the $20M Google Lunar XPRIZE Grand Prize. Last month, both teams were awarded Google Lunar XPRIZE Milestone Prizes: HAKUTO won $500,000 for technological advancements in the Mobility category, while Astrobotic, in partnership with Carnegie Mellon University, won a total of $1.75M for innovations in all three focus areas—Landing, Mobility and Imaging. Throughout the judging process, all three rovers, Moonraker, Tetris and Andy, demonstrated the ability to move 500 meters across the lunar surface and withstand the high radiation environment and extreme temperatures on the moon. -
October 2006
OCTOBER 2 0 0 6 �������������� http://www.universetoday.com �������������� TAMMY PLOTNER WITH JEFF BARBOUR 283 SUNDAY, OCTOBER 1 In 1897, the world’s largest refractor (40”) debuted at the University of Chica- go’s Yerkes Observatory. Also today in 1958, NASA was established by an act of Congress. More? In 1962, the 300-foot radio telescope of the National Ra- dio Astronomy Observatory (NRAO) went live at Green Bank, West Virginia. It held place as the world’s second largest radio scope until it collapsed in 1988. Tonight let’s visit with an old lunar favorite. Easily seen in binoculars, the hexagonal walled plain of Albategnius ap- pears near the terminator about one-third the way north of the south limb. Look north of Albategnius for even larger and more ancient Hipparchus giving an almost “figure 8” view in binoculars. Between Hipparchus and Albategnius to the east are mid-sized craters Halley and Hind. Note the curious ALBATEGNIUS AND HIPPARCHUS ON THE relationship between impact crater Klein on Albategnius’ southwestern wall and TERMINATOR CREDIT: ROGER WARNER that of crater Horrocks on the northeastern wall of Hipparchus. Now let’s power up and “crater hop”... Just northwest of Hipparchus’ wall are the beginnings of the Sinus Medii area. Look for the deep imprint of Seeliger - named for a Dutch astronomer. Due north of Hipparchus is Rhaeticus, and here’s where things really get interesting. If the terminator has progressed far enough, you might spot tiny Blagg and Bruce to its west, the rough location of the Surveyor 4 and Surveyor 6 landing area. -
List of Targets for the Lunar II Observing Program (PDF File)
Task or Task Description or Target Name Wood's Rükl Target LUNAR # 100 Atlas Catalog (chart) Create a sketch/map of the visible lunar surface: 1 Observe a Full Moon and sketch a large-scale (prominent features) L-1 map depicting the nearside; disk of visible surface should be drawn 2 at L-1 3 least 5-inches in diameter. Sketch itself should be created only by L-1 observing the Moon, but maps or guidebooks may be used when labeling sketched features. Label all maria, prominent craters, and major rays by the crater name they originated from. (Counts as 3 observations (OBSV): #1, #2 & #3) Observe these targets; provide brief descriptions: 4 Alpetragius 55 5 Arago 35 6 Arago Alpha & Arago Beta L-32 35 7 Aristarchus Plateau L-18 18 8 Baco L-55 74 9 Bailly L-37 71 10 Beer, Beer Catena & Feuillée 21 11 Bullialdus, Bullialdus A & Bullialdus B 53 12 Cassini, Cassini A & Cassini B 12 13 Cauchy, Cauchy Omega & Cauchy Tau L-48 36 14 Censorinus 47 15 Crüger 50 16 Dorsae Lister & Smirnov (A.K.A. Serpentine Ridge) L-33 24 17 Grimaldi Basin outer and inner rings L-36 39, etc. 18 Hainzel, Hainzel A & Hainzel C 63 19 Hercules, Hercules G, Hercules E 14 20 Hesiodus A L-81 54, 64 21 Hortensius dome field L-65 30 22 Julius Caesar 34 23 Kies 53 24 Kies Pi L-60 53 25 Lacus Mortis 14 26 Linne 23 27 Lamont L-53 35 28 Mairan 9 29 Mare Australe L-56 76 30 Mare Cognitum 42, etc. -
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. -
3D Printered Structure of Lacus Mortis Pit Crater with Assumption of a Cave Underneath
2nd International Planetary Caves Conference (2015) 9015.pdf 3D PRINTERED STRUCTURE OF LACUS MORTIS PIT CRATER WITH ASSUMPTION OF A CAVE UNDERNEATH. Ik-Seon Hong1, Eunjin Cho1, Yu Yi1, Jaehyung Yu1, Junichi Haruyama2, 1Department of Astron- omy, Space Science and Geology, Chungnam National University, Daejeon 34134, South Korea; [email protected], 2Department of Solar System Sciences, Institute of Space and Aeronautical Science, Japan Aerospace Exploration Agency, Sagamihara, Kanagawa 252-5210, Japan. Introduction: Several places presumed to be the en- until the actual exploration on foot and the small shad- trances of caves were discovered in the Moon and ow in the northern side also indicates that there is a Mars [1][2][3][4][5][6]. Besides, about 200 pit-looking ramp alongside the wall of the pit, it is considered that places, which are known as pit craters (abbreviated to this ramp could be an entrance to the inside of the pit. pits), have been discovered and these can be candidates Also, since the collapsed ceiling materials covered the of caves. The pits are found in the regions of the lunar floor of the pit, it is assumed that the entrance of the mare and in places that experienced melting due to cave was buried or the size of the entrance is much meteorite impact [7][8]. Other study showed that those smaller compared to the thickness of ceiling. Thus, the pits could be entrances of caves through comparing entrance is set to have a small size. Moreover, the big those pits to the actual cave entrance of the Earth [9]. -
The Geologic Context of Major Lunar Mare Pits. L
3rd International Planetary Caves 2020 (LPI Contrib. No. 2197) 1048.pdf THE GEOLOGIC CONTEXT OF MAJOR LUNAR MARE PITS. L. Kerber1 L. M. Jozwiak2, J. Whitten3, R.V. Wagner4, B.W. Denevi2, , The Moon Diver Team. 1Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., Pasadena, CA, 91109 ([email protected]). 2Johns Hopkins Applied Physics Laboratory, Laurel, MD, 20723, 3Tulane University, New Orleans, LA, 70118, 4Arizona State Univeristy, Tempe, AZ, 85287. Introduction: In 2009, the Kaguya spacecraft dis- surface void [3]. The pit is located a few kilometers to covered several large pits in the lunar surface [1]. Later the west of the Rimae Burg graben, and could be relat- Lunar Reconaissance Orbiter Camera (LROC) images ed [7]. Compositionally, the pit is located in a deposit captured these pits in greater detail, revealing that of low- to very low-Ti and high Al2O3 lavas that extend some of them expose tens of meters of in-situ lava bed- from Lacus Mortis across the larger Mare Frigoris re- rock cross-sections in their walls [2,3]. Such exposures gion [8]. The Lacus Mortis region itself is a small, offer tantalizing natural drill-holes through the regolith semi-circular mare deposit to the south of Mare Frigor- and into the lunar maria. In particular, the pits provide is, and appears to be composed of a single basaltic unit the opportunity to examine maria deposits from the top [8]. The Lacus Mortis pit would provide access to 5-6 of the regolith, through the regolith/bedrock interface, layers of undersampled Al-rich lavas [8]. -
Basalts in Mare Serenitatis, Lacus Somniorum, Lacus Mortis and Part of Mare Tranquillitatis
Lunar and Planetary Science XXXVI (2005) 1654.pdf BASALTS IN MARE SERENITATIS, LACUS SOMNIORUM, LACUS MORTIS AND PART OF MARE TRANQUILLITATIS. Terence Hackwill1, John Guest2 and Paul Spudis3. 1, 2 Deptartment of Earth Sciences, University College London, Gower Street, London. WC1E 6BT [email protected] [email protected] 3 Applied Phys- ics Laboratory, Johns Hopkins University, Laurel, MD 20723-6099 [email protected] Introduction. We have identified a number of discreet basaltic units in the area being studied. An assessment of their ages, their extent, trends in their chemistry and an indication of the volume of basalt within the basin may provide new informa- tion about the geological history of the area. A number of previous studies have tried to deter- mine the existence and boundaries of basaltic units within the area we examined. For example, [1] described a few units using Earth-based tele- Fig. 1. FeO plotted against TiO wt% for the 54 scopic spectral reflectance techniques while [2] 2 units. identified more units, and in greater detail using images from the Galileo spacecraft. We have used The units have been colour-coded and are dis- the higher resolution Clementine ultraviolet- played in Fig. 2. visible data (down to 200m/pixel [3]) to try and determine the boundaries of units within the re- gion. Additionally we have used Clementine FeO and TiO2 wt% data using the method described in [4] to see if they can suggest variations in the thickness of basalts in the region. We have also used crater depths to suggest the volume of basalt within Mare Serenitatis. -
What's Hot on the Moon Tonight?: the Ultimate Guide to Lunar Observing
What’s Hot on the Moon Tonight: The Ultimate Guide to Lunar Observing Copyright © 2015 Andrew Planck All rights reserved. No part of this book may be reproduced in any written, electronic, recording, or photocopying without written permission of the publisher or author. The exception would be in the case of brief quotations embodied in the critical articles or reviews and pages where permission is specifically granted by the publisher or author. Although every precaution has been taken to verify the accuracy of the information contained herein, the publisher and author assume no responsibility for any errors or omissions. No liability is assumed for damages that may result from the use of information contained within. Books may be purchased by contacting the publisher or author through the website below: AndrewPlanck.com Cover and Interior Design: Nick Zelinger (NZ Graphics) Publisher: MoonScape Publishing, LLC Editor: John Maling (Editing By John) Manuscript Consultant: Judith Briles (The Book Shepherd) ISBN: 978-0-9908769-0-8 Library of Congress Catalog Number: 2014918951 1) Science 2) Astronomy 3) Moon Dedicated to my wife, Susan and to my two daughters, Sarah and Stefanie Contents Foreword Acknowledgments How to Use this Guide Map of Major Seas Nightly Guide to Lunar Features DAYS 1 & 2 (T=79°-68° E) DAY 3 (T=59° E) Day 4 (T=45° E) Day 5 (T=24° E.) Day 6 (T=10° E) Day 7 (T=0°) Day 8 (T=12° W) Day 9 (T=21° W) Day 10 (T= 28° W) Day 11 (T=39° W) Day 12 (T=54° W) Day 13 (T=67° W) Day 14 (T=81° W) Day 15 and beyond Day 16 (T=72°) Day 17 (T=60°) FINAL THOUGHTS GLOSSARY Appendix A: Historical Notes Appendix B: Pronunciation Guide About the Author Foreword Andrew Planck first came to my attention when he submitted to Lunar Photo of the Day an image of the lunar crater Pitatus and a photo of a pie he had made. -
Detect Lunar Ice Explore Lava Tubes Explore Lunar Swirls Taurus-Littrow
Lunar Surface Gravimetry Science Opportunities Kieran A. Carroll1, David Hatch2, Rebecca Ghent3, Sabine Stanley4, Natasha Urbancic5, Marie-Claude Williamson6, W. Brent Garry7, Manik Talwani8 , Harrison H. Schmitt9 , Jennifer Elliott2 1: Gedex Systems Inc., [email protected], 2: Gedex Systems Inc., 3: University of Toronto, 4: Johns Hopkins University, 5: University of British Columbia, 6: Geological Survey of Canada, 7: NASA GSFC, 8: Rice University, 9: University of Wisconsin-Madison Introduction Past Lunar Surface Gravimetry VEGA Instrument December 1972: Lunar Traverse Gravimeter Experiment on Apollo 17 • Gedex has developed a low cost compact space gravimeter instrument , VEGA (Vector Gravimeter/Accelerometer) • This instrument could be used in various lunar surface science investigations VEGA Space Gravimeter Information • Measures absolute gravity vector, with no bias • Accuracy: 0.1-1 microG on the Moon VEGA mechanical breadboard • Bandwidth: 1-10 mHz • Size: 9.5 x 9.5 x 18.5 cm • Power consumption: 4-12.5 W (depending on spacecraft temperature) • Gravimeter sensor is a Bosch • Current Technology Status: TRL 4 ARMA D4E Vibrating String Accelerometer (VSA) • Adapted [following Wing] by MIT’s CSDL • Scalar gravimeter • This was the first surface gravimetry • Survey conducted by Harrison Schmitt and Eugene Cernan, funded by NASA • Target performance: 1 mGal (1 survey ever done off-Earth, and the • An intriguing gravity low was found at Station 5… microG) only one done to date. • Science team: Manik Talwani (P.I.), George Thomson, Brian Dent, Hans-Gert Kahle, Sheldon • Achieved performance: 1.8 mGal • Site: Taurus-Littrow Valley, Mare Buck RMS noise, 5 mGal accuracy Serenitatis • The survey “did geophysics,” with the P.I.