| Risultati della ricerca nelle immagini - "Up" |

003-vg1_p23073.jpgDifferent colors, different elements and different speeds...60 visitenessun commento
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005-vg2_4362030.jpgThe atmosphere of Saturn60 visitenessun commento
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007-vg2_4397840.jpgThe North Pole of Saturn63 visitenessun commento
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009-vg2_p23915.jpgThe restless atmosphere of Saturn...59 visitenessun commento
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010-vg2_p23919.jpgDense clouds and "tiny" cyclons...59 visitenessun commento
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012-vg2_p23938.jpgThe "Great Red Spot" of Saturn61 visitenessun commento
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APOLLO_14_-_AS_14-64-9063.JPGAS 14-64-9063 - EVA-2 - Up-Sun (possible True Colors; credits: Lunar Explorer Italia)87 visiteSolo un commento: provate a guardare questo frame come pubblicato dalla NASA nell'Apollo Lunar Surface Journal, notate le condizioni in cui era/è e poi riguardate, attentamente, questa sua versione ripulita e colorizzata da noi. Insomma, solo per dire: grazie alla NASA, ma anche grazie a Lunexit...MareKromium
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ESP_013071_1365_RED_abrowse.jpgCentral Peak Gullies (Natural Colors; credits: Lunar Explorer Italia)82 visitenessun commentoMareKromium
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ESP_020873_1640_RED_abrowse.jpgLayered Bedrock in Central Uplift (Absolute Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)293 visitenessun commentoMareKromium
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ESP_020929_1360_RED_abrowse.jpgUplifted Bedrock (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)352 visiteCaption NASA:"Large Impact Craters expose deep Bedrock. After the transient cavity forms, the Crater Floor rebounds and creates a permanent structural Uplift, typically equivalent to about 10% of the Crater diameter.
A Crater approx. 70 Km (43,47 miles) wide like this one, can raise up and expose Bedrock that was approx. 7 Km (4,34 miles) lower in elevation prior to the Impact.
Deeper rocks are usually older, and on Mars the oldest rocks are interesting because they are more likely to have been altered by water and provide clues to ancient environments and processes. This image reveals good Bedrock exposures with diverse rock types (as indicated by colors and textures)".MareKromium
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ESP_020949_2115_RED_abrowse.jpgUnnamed Crater's Central Uplift in Amazonis Planitia (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)191 visitenessun commentoMareKromium
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ESP_022580_1560_RED_abrowse-PCF-LXTT.jpgUplifted Layered Materials (Absolute Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)181 visitenessun commentoMareKromium
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