L’hémisphère Cerberus est une partie de la géographie de la planète Mars approximativement de latitude 20° Sud à 55° Nord et de longitude 150° à 230°.
Parmi les points notables de cette zone se trouvent Amazonis Planitia, Cerberus, Mangala Valles et Utopia Planitia.
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Cerberus Hemisphere — Mosaic of the Cerberus hemisphere of Mars Cerberus Hemisphere is a part of Mars geography and refers to the area approximately of Latitude: 20° South to 55° North and Longitude: 150° to 230°. Prominent features of the Cerberus Hemisphere include … Wikipedia
Hémisphère Cerberus — Dans la cadre de la géographie de la planète Mars, l’hémisphère de Cerberus désigne de façon informelle l hémisphère visible depuis l espace quand Cerberus se trouve au centre du disque de Mars … Wikipédia en Français
Crotalus oreganus cerberus — Scientific classification Kingdom: Animalia Phylum … Wikipedia
Geology of Mars — Mars Mars as seen by the Hubble Space Telescope Designations … Wikipedia
Mars — This article is about the planet. For other uses, see Mars (disambiguation) … Wikipedia
Volcanism on Mars — Mariner 9 image of Olympus Mons[1]. This is one of the first images to show that Mars has large volcanoes. Volcanic activity, or volcanism, has played a significant role in the geologic evolution of Mars.[ … Wikipedia
Outflow channels — Kasei Valles, seen in MOLA elevation data. Flow was from bottom left to right. North is up. Image is approx. 1600 km across. The channel system extends another 1200 km south of this image to Hebes Chasma. Outflow channels is the term used to… … Wikipedia
Astronomy on Mars — Mosaic of two different Mars Global Surveyor Mars Orbiter Camera (MOC) exposures of Earth, the Moon, and Jupiter from 2003 … Wikipedia
Geography of Mars — Topographic map of Mars, courtesy NASA Goddard Space Flight Center, from Mars Global Surveyor laser altimeter research led by Maria Zuber and David Smith. North is at the top. Notable features include the Tharsis volcanoes in the west (including… … Wikipedia
Martian dichotomy — The most conspicuous feature of Martian surface geology is a sharp contrast, known as the Martian dichotomy, between the rugged southern highlands and the relatively smooth northern basins. The two hemispheres differ in elevation by 1 to… … Wikipedia
