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Piú votate - Mars from Orbit (from July 2009)
Channel-CoracisFossae-BosporusPlanum-20091106b.jpg
Channel-CoracisFossae-BosporusPlanum-20091106b.jpgDry Riverbed and a possible Skylight (or an EXTREMELY fresh Impact Crater) between Coracis Fossae and Bosporos Planum (EDM - credits: Lunexit)60 visiteIl rilievo ambiguo è sostanzialmente indefinibile a questa risoluzione, ma la sua colorazione "pitch black" e l'apparente assenza di rim ci fa pensare ad un Pozzo Verticale da Collasso.
Le "sbavature" scure che caratterizzano l'intero versante Nord della Surface Feature e, in parte, il lato Est-Sud/Est (senza interessamento della sua zona Ovest ed Ovest-Sud/Ovest), invece, potrebbero anche far pensare ad un impatto il quale, oltre che essere occorso assai di recente, potrebbe - se non altro parzialmente - essere ricondotto alla Classe dei "Mid-Air Impact" (ossia il bolide generatore del dettaglio si sarebbe, in questo caso, parzialmente disintegrato - esploso - in prossimità del suolo, mentre una sua parte avrebbe comunque raggiunto la superficie, così creando un cratere).

L'ipotesi del Vertical Collapse Pit, comunque, ci sembra preferibile (anche se una ragionevole spiegazione delle "sbavature" scure, in questo scenario, non siamo in grado di poterla fornire).
3 commentiMareKromium55555
(5 voti)
Dunes-AoniaTerra-20091027a.jpg
Dunes-AoniaTerra-20091027a.jpgDunefield in Aonia Terra (Natural Colors; credits: Lunar Explorer Italia)55 visitenessun commentoMareKromium55555
(5 voti)
Craters-DouglassCrater-20090930a.jpg
Craters-DouglassCrater-20090930a.jpgDunefield inside Douglass Crater - Aonia Terra (Natural Colors; credits: Lunar Explorer Italia)56 visitenessun commentoMareKromium55555
(5 voti)
Craters-Jeans_Crater-20090910a.jpg
Craters-Jeans_Crater-20090910a.jpgDunes and Layers within Jeans Crater (Natural Colors; credits: Lunexit)64 visitenessun commentoMareKromium55555
(5 voti)
Channels-Nirgal_Vallis-MO-20090721a.jpg
Channels-Nirgal_Vallis-MO-20090721a.jpgNirgal Vallis (Enhanced Natural Colors; credits: Lunar Explorer Italia)58 visitenessun commentoMareKromium55555
(5 voti)
Craters-RabeCrater-MO-20090710a.jpg
Craters-RabeCrater-MO-20090710a.jpgFeatures of Rabe Crater (IR daytime - Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)56 visiteCaption NASA:"This Daytime InfraRed image of Rabe Crater illustrates the warming effect of the Sun on sand.
The extensive sand sheet and dunes of Rabe Crater appear bright in the InfraRed indicating they are warmer than the surrounding floor and plains materials".
MareKromium55555
(5 voti)
Craters-Lipik_Crater-20090630a-PCF-LXTT.jpg
Craters-Lipik_Crater-20090630a-PCF-LXTT.jpgFeatures of Lipik Crater (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunexit Team)66 visiteCaption NASA:"This daytime InfraRed image clearly shows the multitude of channels dissecting the Rim of Lipik Crater".

Coord.: 39,9° South Lat. and 112,4° East Long.
MareKromium55555
(5 voti)
Noachis_Terra-Landforms-20090622a-PCF-LXTT.jpg
Noachis_Terra-Landforms-20090622a-PCF-LXTT.jpgOdd Rimmed Depressions in Noachis Terra (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia)56 visitenessun commentoMareKromium55555
(5 voti)
Craters-Unnamed_South_Polar_Crater-IR-MO-20090617a.jpg
Craters-Unnamed_South_Polar_Crater-IR-MO-20090617a.jpgSouthern Crater Dunes (IR - Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia)54 visiteCaption NASA:"Many craters around the South Polar Cap contain Dunefields on their Floors. This is one example of such a crater. This image was taken with the THEMIS InfraRed Camera and shows the warm daytime temperature of the dunes compared to the surrounding materials".MareKromium55555
(5 voti)
Jus_Chasma-NTV-MO-20090422a.jpg
Jus_Chasma-NTV-MO-20090422a.jpgJus Chasma at Night (False Colors; credits: Lunexit)57 visiteCaption NASA:"This is an InfraRed image of Jus Chasma taken at night. Bright surfaces are warmer than dark surfaces; the floor of the chasma is warmer than the plains at the top of the frame. Nighttime InfraRed images are extremely helpful in identifying bedrock outcrops, which stay warmer than dust covered surfaces. The landslide is also easy to identify in this image".

Coord.: 8,0° South Lat. and 280,8° East Long.
MareKromium55555
(5 voti)
Clouds-South_Polar_Regions-20090416a-PCF-LXTT-2.jpg
Clouds-South_Polar_Regions-20090416a-PCF-LXTT-2.jpgSouthern Storm (2 - Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia)81 visiteCoord.: 68,2° South Lat. and 190,6° East Long.MareKromium55555
(5 voti)
Aeolian_Features-DD_Tracks-AoniaTerra-MO-20090413a.jpg
Aeolian_Features-DD_Tracks-AoniaTerra-MO-20090413a.jpgDust Devil Tracks in Aonia Terra (Natural Colors; credits for the additional process. and color.: Dr Paolo C. Fienga - Lunar Explorer Italia)57 visitenessun commentoMareKromium55555
(5 voti)
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