| Piú viste - Mars from Orbit (from July 2009) |

Channels-Mesa_Vallis-PIA15312-PCF-LXTT.jpgMesa Vallis (Absolute Natural Colors; credits for the additonal process. and color.: Dr Paolo C. Fienga - Lunexit Team)93 visiteOrbit Number: 44529
Latitude: 13,254° North
Longitude: 326,951° East
Instrument: VIS
Captured: December, 28th, 2011
Mars Local Solar Time: 19:14 (Early Evening Hours)MareKromium
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Fissures-Cerberus_Fossae-PIA13138-exp2.jpgFissure in Cerberus Fossae (possible Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)92 visitenessun commentoMareKromium
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DustDevilStreaks-Arcadia_Planitia-PIA13361.jpgDust Devils' Tracks in Arcadia Planitia (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)92 visitenessun commentoMareKromium
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Ridges-Reull_Vallis-PCF-LXTT.jpgRidges in Reull Vallis (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)92 visitenessun commentoMareKromium
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North_Polar_Regions-Olympia_Undae-PIA16320-PCF-LXTT-IPF.jpgFeatures of Olympia Undae (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga/Lunar Explorer Italia/Italian Planetary Foundation)92 visiteThis NASA - Mars Odyssey Orbiter "VIS" image shows a portion of Olympia Undae, the largest Dunefield near the North Polar Cap. In this Region, the Dunes are spaced far enough apart so to allow us to see the details of the Surface that they are moving across.
Orbit Number: 47095
Latitude: 79,6934° North
Longitude: 149,575° East
Instrument: VIS
Captured: July, 26, 2012MareKromium
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Dunes-Ganges_Chasma-2005_07.jpgThe Dark Dunes of Ganges Chasma (Eastern Valles Marineris - Saturated Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia)91 visitenessun commentoMareKromium
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Craters-Unnamed_Craters-20080314a.jpgThe "Three Kings" of Arabia Terra (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)91 visitenessun commentoMareKromium
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Volcanoes-Olympus_Mons-20071004a-PCF-LXTT.jpgLava Flows on the Eastern Flank of Olympus Mons (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team) 91 visitenessun commentoMareKromium
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Volcanic_Features-Collapse_Pits-Elysium_Mons-PCF-LXTT-01.jpgCollapse Pit-Chain on Elysium Mons (Absolute Natural Colors; credits for the additional process. and color: Dr Paolo C. Fienga - Lunexit Team)91 visitenessun commentoMareKromium
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Aeolian_Features-Windstreaks-PIA15306-PCF-LXTT.jpgWindstreaks in Chrise Planitia (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)91 visiteOrbit Number: 44467
Latitude: 28,205° North
Longitude: 316,709° East
Instrument: VIS
Captured: December, 23rd, 2011
Mars Local Solar Time: 16:41 (Middle Afternoon)MareKromium
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Chaotic_Terrain-Cerberus_Fossae.jpgChaotic Terrain in Cerberus Fossae (Original NASA/JPL/ASU b/w Frame)90 visiteNella Regione Marziana conosciuta con il tenebroso nome di "Cerberus Fossae" possiamo vedere, grazie a questa splendida 'veduta orbitale' ottenuta dalla Sonda NASA "2001 - Mars Odyssey", un terreno ricco di intriganti e variegati rilievi.
Qualche cratere relativamente recente (che reca segni di wind-streaks scuri) e qualcuno più antico e semi-sepolto; delle colline che sembrano poggiare sopra un "basamento" e poi - forse una delle caratteristiche più inquietanti di questo scorcio di Marte - dei profondi e scoscesi crepacci frastagliati.
Questo tipo di zona viene definito "chaos" e si tratta di un'area che è stata - letteralmente - privata di sostegno sotterraneo e che quindi è "crollata su sè stessa" (---> "Chaos" is typically interpreted to be a collapse terrain; it is the blocky landscape after the transport and removal of subsurface support).
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Utopia_Planitia-PIA13350.jpgUtopian Landscape (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)90 visitenessun commentoMareKromium
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