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

Piú viste - Mars through the Viking Orbiters
vo1_mg01n104[1]-PCF-LXTT-00.jpg
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)195 visitenessun commentoMareKromium
vo1_003a07[1]-PCF-LXTT.jpg
vo1_003a07[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 003a07 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)194 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)193 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)192 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)189 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)189 visitenessun commentoMareKromium
vo1_010a56[1]-PCF-LXTT.jpg
vo1_010a56[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 010a56 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)188 visitenessun commentoMareKromium
vo1_759a73[1]-PCF-LXTT.jpg
vo1_759a73[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 759a73 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)185 visitenessun commentoMareKromium
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)179 visitenessun commentoMareKromium
vo1_224a13[1]-PCF-LXTT.jpg
vo1_224a13[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 224a13 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)171 visitenessun commentoMareKromium
vo1_020a62[1]-PCF-LXTT.jpg
vo1_020a62[1]-PCF-LXTT.jpgFrame Viking Orbiter 1 n. 020a62 (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)169 visitenessun commentoMareKromium
vo1_mg01n104[1]-PCF-LXTT-01.jpg
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)163 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
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