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E a R Th» »Moon Moon: Earth: Surface Area Earth » L E N Gth of Equat k k k 363 384 405 . E EARth-MOON DISTANCE (km) V A MIN. MIN. 0 200 400 600 800 km MAX. SEA OF HUMBOLDT MARE HUMBOLDTIANUM SEA OF COLD MARE FRIGORIS PLATO CE3 G. BRUNO L1 SEA OF SHOWERS MARE IMBRIUM L2 A15 L21 SEA OF SERENITY ARISTARCHUS MARE SERENITATIS JAckSON L13 A17 SEA OF MUSCOVY ENNINUS SEA OF CRISES MARE MOSCOVIENSE MARE CRISIUM L24 MONTES Ap KEPLER SEA OF TRANQUILITY L4 COPERNICUS MARE TRANQUILLITATIS L20 OCEAN OF STORMS S5 R8 OCEANUS PROCELLARUM S4/6 1° CE1 L15 1° S1 0° 0° S3 L-1° L-1° A12 0° A14 -1° A11 +1° 179° 180° SEA OF FECUNDITY -179° HERTZSPRUNG MARE FECUNDITATIS A16 KOROLEV R7 LANGRENUS GRIMALDI R9 SEA OF NECTAR MARE NECTARIS SEA OF CLOUDS SEA MARE NUBIUM OF MOISTURE EASTERN SEA MARE HUMORUM MARE ORIENTALE S7 APOLLO TYCHO SOUTH POLE–AITKEN BASIN V E R A G E + A 16 °C H » T DENSITY R LUNa–2 A g/m3 8001 : 10 000. 1 cm km. ≈ 108 SURFACE TemPERATURE E MOON EARTH ScHRÖDINGER LP Lambert Azimuthal Equal Area Projection. A AMERICAN MANNED SPACECRAFTS . V E OON R A: Apollo E E M A E A G R R TH E T F - O 18 U H AMERICAN SPACE PROBES P °C A Commission on Planetary Cartography. Published by Eötvös Loránd University, Budapest. Text © Henrik Hargitai 2014. http://childrensmaps.wordpress.com. M Editor: Henrik Hargitai. Illustration:Europlanet 2012 OutreachLászló FundingHerbszt. Scheme,Technical Paris Observatory,review: InternationalJim Zimbelman. CartographicISBN 978-963-284-423-7, ISBN 978-963-284-422-0 Illustration [PDF]. Supporters:Association © László Herbszt 2014. » S » LP: Lunar Prospector M O O N T H E E A D R S 1 3 3 BUZZ AlDRIN R: Ranger N T 3.34 g/cm 5.515 g/cm 0 MOON H U E INNER 1 SURFACE AREA S: Surveyor O 3 R R LENGTH OF ONE SOLAR DAY . SOLAR SYSTEM 2 A P TROJANS 5 2 SOVIET SPACE PROBES EARTH 29 14 44 sec : MOON MOON 38 million km N m T O L: Luna 0 b I » m b O EARTH 24 » M I T Y B S 2 S 2 :510 million km N E EARTH 7 JUPITER R N E CHINESE SPACE PROBES T MAIN ASTEROID BELT D O D O I A U T CE: Chang’e Y N R 2 A 2 I S T I 7 M MOON MOON H 3 O O F E A m/s 4 m/s Q OURS R 3 R AVITY H U T A 0 kg/m 27 7 43 sec k m G 9.81 1.62 G T TILT OF AXIS 7 5 N 0 O EARTH MOON E 0 R SOLAR DISTANCE 23 56 sec 4 EARTH L : 3 TANT 9 2 1.225 kg/m EARTH S H 1 THE MOON 0 k 150 2 EARTH T 1 million m : ICA COmmIssION ON PLANETARY CARTOGRAPHY VeNUS 1.5˚ R km A N MOON W/m 23.4 ˚ SUN MOON E O AR CON MARS MERCURY L EARTH O 1 : 10 800 000 1361 SUN EARTH MOON SUN M ATMOSPHERE: – SO GREEKS The Satellite Automobile Interkozmosz (tin toy, 1970's, Hungary, FLIM Lemezáru Gyáregység) km km THE MOON The most ancient formations of the lunar surface are the >4-billion-year-old highlands, and the areas where 3474 12742 the surface is so densely covered with craters, that a newly created one surely wipes away a few earlier craters. : The large basins and the smallest craters were all scooped out by asteroids and space debris coming from LUNOKHOD 2 the outer space and hitting the Moon. The “seas” (mare) are actually ancient lava plains, which filled up the Moon MOON EARTH: earlier large impact basins with many layers of lava. The rocks on the lunar surface have been broken up, IllUSTRATION: LÁSZLÓ HeRbsZT pulverised by “space dust” for billions of years, creating moon dust covering the entire surface. The “face” DIAMETER of the Moon has been unchanged for billions of years. It looked almost the same in the age of the dinosaurs, when the continents of the Earth had completely different shapes. The youngest formations are the light- rayed craters. There is no visible sign of water: even the meandering channels of the Moon were formed by volcanic lava..
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