Feature of the Month—September 2019 Gemma Frisius
Total Page:16
File Type:pdf, Size:1020Kb
Load more
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. -
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. -
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. -
Planetológiai Helyesírási Tanácsadó
Planetológiai helyesírási tanácsadó GEOLÓGIA Kőzetrétegtani egységek ridged member = gerinces tagozat Heveliusi Formáció, Hold Geokronológia (idő) imbriumi időszak kora-imbriumi kor noachi időszak Kronosztratigráfia (időrétegtani)(kőzettestek) imbriumi rendszer alsó-imbriumi sorozat noachi rendszer Az egyes egységek magyar elnevezései MERKÚR kuiperi mansuri calorisi tolsztoji pretolsztoji VÉNUSZ aureliai atlai guinevrai ruszalkai laviniai sigrúni fortunai prefortunai HOLD kopernikuszi eratoszthenészi imbriumi nektári prenektári (procellárumi: elavult) MARS amazoni heszperiai noachi prenoachi MARS - geokémiai sideriki theiiki phylloci (ejtsd: filloszi) GEOGRÁFIA Bolygófelszíni alakzatok elnevezései Köznévi taggal (az alábbiakat mindig kötőjellel kapcsoljuk, kivéve birtokos esetben: Cassini-régió, de: Válságok tengere) Megjegyzések: • Az itt felsorolt alakok: latin alak egyes szám, többes szám [latin alak latinos kiejtése], magyar megfelelő • A ¯ jel az előtte álló u-n vagy e-n lévő vonalékezet • A toldalékok a (magyar vagy latin) nevekhez általában közvetlenül kapcsolódnak, a szükséges hasonulások vagy a szóvégi magánhangzó nyúlásának a jelölésével: Caloris Montesszal, Lavinia Planitián, Ión. • A két különírt tagból álló latin elnevezésekhez az -i/-beli képzô kötôjellel kapcsolódik; az eredeti kis- és nagybetûket megtartjuk: Caloris Planitia-i, Sinus Meridiani-beli stb. (vö. AkH. 1984: 217. b) pont). A két különírt tagból álló magyar elnevezéseknél az -i képzôs forma: Halál tavabeli, Méz tengerebeli, Rothadás mocsarabeli, Szivárvány öblebeli -
SELENOLOGY the Journal of the American Lunar Society
DEVOTED TO THE STUDY OF EARTH’S MOON VOL. 26 NO. 2 SUMMER 2007 SELENOLOGY The Journal of The American Lunar Society Selenology Vol. 26 No. 2 - Summer 2007 The official journal of the American Lunar Society, an organization devoted to the observation and discovery of the earth’s moon TABLE OF CONTENTS: Cassini A and the Washbowl: As Described by Wilkins and Moore ......... 2 On Closer Examination .......................................................................... 6 Vertical Displacement of Features in the Montes Spitzbergensis Area ....... 15 COVER: Cassini Crater imaged by Wes Higgins on August, 25 2005 at 10:45 UT with a 45 cm Newtonian telescope. Selenology, Vol. 26 No. 2, Summer 2007. A publication of the American Lunar Society. President: Eric Douglass; Vice President: Steve Boint; Editor: Francis G. Graham. Web site: http://amlunsoc.org/ Layout/design by A Distant Wind (www.distantwind.com) This issue edited by Steve Boint. Copyright © 2007 by the American Lunar Society and individual authors; all rights reserved. Send manuscripts, general observations, photographs, drawings and other correspondence to: Steve Boint, VP ALS, 1807 S. Spring Ave., Sioux Falls, SD 57105 E-mail: [email protected] Send changes of address to Eric Douglass at [email protected] If you don’t have e-mail, send them to Steve Boint Page 2 SELENOLOGY Vol. 26 No. 2 Cassini A and the Washbowl: As Described by Wilkins and Moore By Raffaello Lena, Maria Teresa Bregante, Eric Douglass and Giorgio Mengoli GLR group 1. INTRODUCTION degrees. When the colongitude In this article, we report on is the same, on different several observations made by cycles, the lighting conditions the Geologic Lunar Research are similar. -
Distribution and Volumes of Lava Ponds in the Orientale Region of the Moon
DISTRIBUTION AND VOLUMES OF LAVA PONDS IN THE ORIENTALE REGION OF THE MOON. Lisa R. Gaddis and James W. Head, Dept, of Geological Sciences, Brown University, Providence, R. I, 02912 Stratigraphic and volumetric studies of mare deposits on the Moon have generally been restricted to areas which display several stages of mare fil- ling (1-3). With the notable exception of the Imbrium flows (4), little work has been done on the volumes and extent of individual flows and small volcanic deposits isolated by nap-mare units. Informati on cn these small mare deposits or lava ponds could lead to a better understanding of minimum eruption volumes, the relati onship between these volumes and associated vent characteristics , and their eruption conditions. In addition, the distribution and mode of occurrence of small lava ponds may be useful in determining the nature of the early stages of volcanism in the highland crust. One approach to this problem is LO examine individual lava ponds in high- land areas adjacent to the major lunar maria. The purpose of this study is to present an analysis of such an area, between Mare Orientale and southwestern Oceanus Procell arum, in order to further characterize erupti on vol umes and the relation of volcanism to the lunar crustal environment. Distribution of Lava Ponds - Lava ponds chosen for this study are con- centrated in an arc between Mare Orientale and southwestern Oceanus Procellarum (Figure 1). Of the thirty-three ponds analyzed, eleven are located within the mu1 ti-ringed basin of Orientale (nos. 1 - ll), ten occur predominantly in crater floors (nos. -
FEATURE of the MONTH – AUGUST 2016 W Bond B
A PUBLICATION OF THE LUNAR SECTION OF THE A.L.P.O. EDITED BY: Wayne Bailey [email protected] 17 Autumn Lane, Sewell, NJ 08080 RECENT BACK ISSUES: http://moon.scopesandscapes.com/tlo_back.html FEATURE OF THE MONTH – AUGUST 2016 W Bond B Sketch and text by Robert H. Hays, Jr. - Worth, Illinois, USA March 18, 2016 01:50-02:30 UT, 15 cm refl, 170x, seeing 8/10, transparency 6/6 I drew this crater and vicinity on the evening of March 17/18, 2016 before the moon hid 1 Cancri. This crater is the most conspicuous feature within the large ruined ring W. Bond, north of Mare Frigoris. This is a very crisp crater with much interior shadow and slight exterior shadow at this time. The smaller crater W. Bond C is north of B, and is a miniature version of its neighbor. A wide, slightly curved ridge with dark shadowing is southeast of W. Bond B. It tapers almost to a point at its southern end, and a small peak is just off this tip. A large, blocky peak, also with dark shadowing, is north of this ridge, and a small peak with much lighter shadowing is between this block and W. Bond C. Another ridge is just east of the wide ridge and block. This ridge has two branches, and has relatively light shadowing except at the elbow formed by one of its branches. A low peak is just off this ridge's north end. The crater just east of this ridge is probably Archytas U. -
Rimae Sirsalis
RIMAE SIRSALIS Nieves del Río, José Castillo, Eduardo Adarve, Jorge Arranz y Alberto Martos del Grupo de Estudios Lunares “Enrique Silva”. [Página dejada intencionadamente en blanco] - 2 - INTRODUCCIÓN Rimae Sirsalis es un sistema de grietas que comprende dos estructuras de esta clase, Rima Sirsalis y Rima Sirsalis I, siendo la primera mucho más larga y mucho más perceptible que la segunda. Pertenecen a la clase de grietas rectas, cuyo aspecto es diferente del aspecto de las grietas circulares que bordean las cuencas de las grandes estructuras de impacto. Lo que tiene de particular este sistema, para que haya merecido figurar como objetivo 1 en el apartado “Call for Observations 2”, del boletín TLO 3 de ALPO 4, son sus dos características principales: siendo Rima Sirsalis la grieta más larga existente en la cara cislunar (la visible), está situada en una región cuyo suelo es geológicamente distinto de la naturaleza de suelos por los que discurren en general las grietas lunares. En efecto, las grietas lunares (llamadas en latín rimae ) son siempre estructuras volcánicas, generalmente túneles de lava cuyo techo se ha desplomado, o surcos por los cuales fluyó la lava en su día, en favor de la pendiente del suelo. Por esta razón, se las encuentra siempre sobre terrenos magmáticos, como los maria (plural de mare ), los sini (plural de sinus ), los laci (plural de lacus ), o los paludes (plural de palus ), o sea sobre los “mares”, las “bahías”, los “lagos” o las “marismas” lunares. Como ejemplos de esta condición se puede citar a Rimae Hypatia, situada en el Mare Tranquillitatis, a Rima Oppolzer, en Sinus Medii, a Rimae Bürg y Rimae Daniell, en Lacus Mortis y Lacus Somniorum, respectivamente y Rima Hesiodus en Palus Epidemiarum. -
Hungarian Localization of the International Planetary Nomenclature System
3rd INTERNATIONAL CONFERENCE ON CARTOGRAPHY AND GIS 15-20 June, 2010, Nessebar, Bulgaria HUNGARIAN LOCALIZATION OF THE INTERNATIONAL PLANETARY NOMENCLATURE SYSTEM Henrik Hargitai Author: Henrik Hargitai Eötvös Loránd University, Institute of Geography and Earth Sciences, Planetary Science Research Group 1117 Budapest, Pázmány P st 1/1 hhargitai[at]gmail.com Abstract: The paper describes the Hungarian localization of the official IAU nomenclature system of planetary body surface features and planetary body names. The localized forms are recommended for use in texts published in popular science journals and newspapers and books for the general public. Keywords: planetary cartography, Mars, Moon, planetary nomenclature, placenames, toponymy INTRODUCTION The Planetary Nomenclature System is maintained by the Working Group for Planetary System Nomenclature (WGPSN) of the International Astronomical Union, and is published as the Gazetteer of Planetary Nomenclature which is distributed by the U.S. Geological Survey (USGS). Planetary surface feature Place Names consist of two elements: a specific term and a descriptor term. Crater, bright albedo and some other names have no descriptor term. Descriptor terms are in Latin language; for specifics, the original form is retained if the original is using Latin alphabet; if not, a transformation to Latin alphabet is applied. The origin of this system goes back to the 17th century, when the first Lunar maps, especially the Grimaldi-Riccioli map used Latin terms which was a conventional custom of cartographers -
Unit Five Lītus Mareque
Rërum Nätüra Unit Five 114 Unit Five Lïtus Mareque Part I: Cëtï · Verbs plus infinitive · Possum, volö and ferö · Seasons · Reading: Balaenae Part II: Nävigätio Römäna · Imperfect tense · Adverbs · Reading: Nävigätio Römäna Part III: Delphïnï · Ablative Meanings · Dative Meanings · Reading Notes · Reading: Delphïnï Part IV: Chapter Vocabulary · Chapter Vocabulary · Luna redux Lïtus Mareque Shore and sea A map of Italy shows why the sea was so important in the economy and imagination of the Roman Empire: the Mediterranean sea, mare Mediterraneum, surrounds Italy and is a central thoroughfare and meeting place for all of the different peoples and cultures that made up the Empire. (The Romans referred to the Mediterranean as mare nostrum, our sea: noster, nostra, nostrum =our.) The most common word for ocean is mare, maris n, from which we derive words like marine and maritime. (Our word ocean derives from a Greek word, also adopted into poetic Latin, öceanus, -ïï m). The word for wave is unda, -ae f (from which we get our word undulate), and the ocean could be referred to as undae, the waves, especially if you referred to bestiae sub undis, creatures beneath the waves, or travelling super undäs, above the waves. Rërum Nätüra Unit Five 115 Sometimes the sea was referred to poetically as the deep, or altum, -ïï n. This word comes from the adjective altus, -a, -um, which means both high (as in mons altus, a high mountain) and deep (as in mare altum, the deep sea). To us, these meanings are opposite; to the Romans, altus just reflects a vertical expanse, whether up or down. -
O Personenregister
O Personenregister A alle Zeichnungen von Sylvia Gerlach Abbe, Ernst (1840 – 1904) 100, 109 Ahnert, Paul Oswald (1897 – 1989) 624, 808 Airy, George Biddell (1801 – 1892) 1587 Aitken, Robert Grant (1864 – 1951) 1245, 1578 Alfvén, Hannes Olof Gösta (1908 – 1995) 716 Allen, James Alfred Van (1914 – 2006) 69, 714 Altenhoff, Wilhelm J. 421 Anderson, G. 1578 Antoniadi, Eugène Michel (1870 – 1944) 62 Antoniadis, John 1118 Aravamudan, S. 1578 Arend, Sylvain Julien Victor (1902 – 1992) 887 Argelander, Friedrich Wilhelm August (1799 – 1875) 1534, 1575 Aristarch von Samos (um −310 bis −230) 627, 951, 1536 Aristoteles (−383 bis −321) 1536 Augustus, Kaiser (−62 bis 14) 667 Abbildung O.1 Austin, Rodney R. D. 907 Friedrich W. Argelander B Baade, Wilhelm Heinrich Walter (1893 – 1960) 632, 994, 1001, 1535 Babcock, Horace Welcome (1912 – 2003) 395 Bahtinov, Pavel 186 Baier, G. 408 Baillaud, René (1885 – 1977) 1578 Ballauer, Jay R. (*1968) 1613 Ball, Sir Robert Stawell (1840 – 1913) 1578 Balmer, Johann Jokob (1825 – 1898) 701 Abbildung O.2 Bappu, Manali Kallat Vainu (1927 – 1982) 635 Aristoteles Barlow, Peter (1776 – 1862) 112, 114, 1538 Bartels, Julius (1899 – 1964) 715 Bath, KarlLudwig 104 Bayer, Johann (1572 – 1625) 1575 Becker, Wilhelm (1907 – 1996) 606 Bekenstein, Jacob David (*1947) 679, 1421 Belopolski, Aristarch Apollonowitsch (1854 – 1934) 1534 Benzenberg, Johann Friedrich (1777 – 1846) 910, 1536 Bergh, Sidney van den (*1929) 1166, 1576, 1578 Bertone, Gianfranco 1423 Bessel, Friedrich Wilhelm (1784 – 1846) 628, 630, 1534 Bethe, Hans Albrecht (1906 – 2005) 994, 1010, 1535 Binnewies, Stefan (*1960) 1613 Blandford, Roger David (*1949) 723, 727 Blazhko, Sergei Nikolajewitsch (1870 – 1956) 1293 Blome, HansJoachim 1523 Bobrovnikoff, Nicholas T. -
Volume of Abstracts
Volume of Abstracts Indian Planetary Science Conference-2021 25-26 February 2021 Physical Research Laboratory ORAL Presentations No Details Speaker Page No The Impact of Stealth CMEs on Martian Topside 1 Smitha Thampi, SPL 1 Ionosphere Spatio-temporal characteristics of the He bulge in the 2 Neha Gupta, NARL 2 Martian Upper Atmosphere 3 Recurrent Space Weather Events at Mars C Krishnaprasad, SPL 3 How do we understand dust in the Martian 4 Varun Sheel, PRL 4 atmosphere? Response of the Martian ionospheric peak to the 5 Vrinda Mukundan, NCESS 5 Planet Encircling Dust Event of June 2018 MOM and MAVEN Observations of the Effects of Venkateswara Rao Narukull, 6 the 2018 Planet‐Encircling Dust Event on the Martian 6 NARL Thermospheric Densities Water ice clouds observations over Olympus Mons 7 using the Mars Color Camera and Mars Climate Jagabandhu Panda, NIT, Rourkela 7 Sounder Variation of composition of Martian atmosphere Nagaraja Kamsali, Bangalore 8 8 during solar quiet and disturbed periods University A study on the characteristic features of the V1 layer 9 of the Venus ionosphere using Akatsuki Ambili K M, SPL 9 measurements. Dinesh Kumar V. R., BITS Pilani, 10 Current Status of Venus Lightning Research 10 Hyderabad Analogue research in Astrobiology: Implications for 11 Sudha Rajamani, IISER Pune 11 delineating prebiotically relevant processes 12 Graphene in Titan Rahul Kumar Kushwaha, PRL 12 Isita, SRM Institute of Science & 13 Violacein: a Bio-pigment Exploited in Mars 13 Technology, Tamil Nadu Complex structures in the ejecta of