| Risultati della ricerca nelle immagini - "Marte" |
Channels-Marte_Vallis-PCF-LXTT.jpgUnnamed Channel in Marte Vallis (Natural Colors/Tri-Chromatic Version; credits: Dr Paolo C. Fienga - Lunexit Team)167 visitenessun commentoMareKromium
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Channels-Marte_Vallis-Streamlined_Islands-PIA16507-PCF-LXTT-IPF.jpgStreamlined Island in Marte Vallis (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia/Italian Planetary Foundation)58 visiteToday's APOD is a frame taken by the NASA - Mars Odyssey Orbiter which shows us a so-called "Streamlined Island" that formed in the Northern Channel known as Marte Vallis. This Martian Channel is about 185 Km long and it has been identified as an Outflow Channel, carved in a quite distant geological past by the action of catastrophic releases of Water from Aquifers existing beneath the Martian Surface.
Orbit Number: 47605
Latitude: 12,4105° North
Longitude: 182,426° East
Instrument: VIS
Captured: September, 6th, 2012
This frame (which is an Original Mars Odyssey Orbiter b/w frame published on the NASA - Planetary Photojournal with the ID n. PIA 16507) has been additionally processed and then colorized in Absolute Natural Colors (such as the colors that a human eye would actually perceive if someone were onboard the NASA - Mars Odyssey Orbiter and then looked down, towards the Surface of Mars), by using an original technique created - and, in time, dramatically improved - by the Lunar Explorer Italia Team.MareKromium
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Marte_Vallis-MGS-PCF-LXTT.jpgThe alleged "Frozen Ocean" of Marte Vallis (Natural Colors; credits for the additonal process. and color.: Dr Paolo C. Fienga - Lunexit Team)96 visitenessun commentoMareKromium
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Marte_Vallis-PIA13249.jpgMarte Vallis (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)54 visitenessun commentoMareKromium
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PSP_003570_1915_RED_abrowse-PCF-LXTT.jpgColourful Slope-Streaks in Marte Vallis (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)71 visiteThis image of a large Hill in Marte Vallis has numerous dark- and light-toned Streaks along its Slopes, showing a variety of characteristics observed in other areas with these features.
For example, several dark Streaks have formed "fingers" at their Termini (such as the point where where the Streaks end).
Their formation may be due to the material "feeling" the roughness of the ground as it reaches shallower slopes near the base of the Hill. The dark Streaks also appear to travel over many obstacles along their paths, such as impact craters, small boulders, and rock outcrops. This indicates that the Slope Streaks have sufficient "momentum" and energy early in their descent downslope that they are not affected by such features or the ground.
The Slope Streaks also do not start at a common elevation along the sides of the Hill, suggesting that they are not related to any particular layer(s) of material.
Dark Slope Streaks are thought to fade over time by deposition of a new bright Dust Layer over the old streaked Surface. The presence of light-toned Streaks relative to their surrounding darker-toned surface is particularly interesting.
Scientists have wondered: if dark Streaks fade over time by deposits of new Dust, then how can there be light-toned streaks? Does this mean light-toned Streaks are formed differently? Are the materials of a light-toned Streak different from dark-toned Streaks?
Slope Streaks have been discovered and studied since the early Mariner and Viking Missions to Mars in the '60s and '70s. Scientists are hoping to resolve some of these questions using HiRISE images with its high spatial resolution compared to these previous Mars datasets.MareKromium
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Streamlined_Islands-Marte_Vallis-PCF-LXTT.jpgStreamlined Islands in Marte Vallis (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team:)74 visitenessun commentoMareKromium
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T-TRA_000853_1900_RED_MarteValles_01.jpgSeepage in Marte Vallis (Natural Colors; credits: Lunar Explorer Italia)54 visitenessun commentoMareKromium
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