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Inizio > THE LUNAR EXPLORER ARCHIVES > Mars through the Viking Orbiters

Mars through the Viking Orbiters

vo1_840a16[1]-PCF-LXTT.jpg
vo1_840a16[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 840a16 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)93 visitenessun commentoMareKromium
vo1_890a68[1]-PCF-LXTT.jpg
vo1_890a68[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 890a68 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)185 visitenessun commentoMareKromium
vo1_mf31s343.jpg
vo1_mf31s343.jpgMars: according to Viking 1 Orbiter55 visite
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vo1_mg01n104[1]-PCF-LXTT-00.jpgFrame Viking Orbiter 1 n. mg01n104 (Enhanced Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)185 visitenessun commentoMareKromium
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vo1_mg01n104[1]-PCF-LXTT-01.jpgThe "Tharsis' Montes" (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)153 visiteThe alignment of the 3 Shield Volcanoes that make up the Tharsis Montes is clearly evident in this view. The 3 Volcanoes are named Ascraeus Mons, Pavonis Mons and Arsia Mons, going from North to South. The 3 Volcanoes are each somewhat smaller than Olympus Mons, varying from about 350 to 450 Km (approx. 210 to 270 mi) in horizontal extent and each rising about 15 Km (approx. 9 miles) above the surrounding Plains.
The Tharsis Montes are located on the crest of a broad uplift of the Martian Crust so that their Summits are at about the same elevation as the Summit of Olympus Mons.

The "Fractures" to the South/East of Pavonis Mons, are known as "Noctis Labyrinthus"; this Region merges with the enormous Valles Marineris Canyon System to the East. The white patches around the lower Flanks of the Volcanoes are thin Clouds that commonly occur near them.
MareKromium
vo1_mg12n190.jpg
vo1_mg12n190.jpgMars: according to Viking 1 Orbiter54 visite
vo2_007b94[1]-PCF-LXTT.jpg
vo2_007b94[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 007b94 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)173 visitenessun commentoMareKromium
vo2_039b59[1]-PCF-LXTT.jpg
vo2_039b59[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 039b59 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)184 visitenessun commentoMareKromium
vo2_043b20[1]-PCF-LXTT.jpg
vo2_043b20[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 043b20 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)187 visitenessun commentoMareKromium
vo2_044b50[1]-PCF-LXTT.jpg
vo2_044b50[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 044b50 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)184 visitenessun commentoMareKromium
vo2_065b74[1]-PCF-LXTT.jpg
vo2_065b74[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 065b74 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)329 visitenessun commentoMareKromium
vo2_248b57[1]-PCF-LXTT.jpg
vo2_248b57[1]-PCF-LXTT.jpgFrame Viking Orbiter 2 n. 248b57 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)206 visitenessun commentoMareKromium
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