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Ultimi commenti - Mars Reconnaissance Orbiter (MRO)
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 21:53MareKromium: Caro Gianluca,

non importa il fatto che non pu...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 20:31Gianluca1989: Grazie Marco.. Poco fa ho inviato una mail al Dr.A...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 17:36titanio44: un saluto ed un benvenuto a Gianluca.
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 12:03MareKromium: In immagini scattate da grandi distanze (e dall...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 07:10Anakin: domanda: quello che appare celeste (cos? li vedo i...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/22/10 at 04:162di7: Ciao Gianluca! : ) Benvenuto! Bene, un altro appas...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/21/10 at 22:18Gianluca1989: Grazie mille... Quoto: come dici te "I colori...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/21/10 at 21:59MareKromium: Buonasera e benvenuto Gianluca. Tutti i colori che...
ESP_016136_1525_RED_abrowse-01.jpg
ESP_016136_1525_RED_abrowse-01.jpgColourful Streaks (EDM - possible True Colors; credits: NASA/JPL/Univ. of Arizona and Dr Paolo C. Fienga - Lunexit Team)81 visiteIn this enhanced True Color EDM, we see colorful Streaks, where the bedrock is eroding, moving downhill a bit, then getting swept by the wind.14 commentiMareKromium01/21/10 at 21:37Gianluca1989: Immagini davvero meravigliose,la stessa foto ma co...
ESP_016087_2595_RED_abrowse.jpg
ESP_016087_2595_RED_abrowse.jpgFrost-covered Dunes (Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)58 visiteDunes are often found on Crater Floors. In the Winter time, at high Northern Latitudes, the Terrain is covered by Carbon Dioxide Ice (Dry Ice - CO2 Ice). In the Spring, as this seasonal ice evaporates or sublimates, many unusual features - certainly unique to Mars - become visible.

On the Floor of this Crater, where there are no Dunes, the ice forms an uninterrupted layer. On the Dunes, however, Dark Streaks form as surface material from below the ice is mobilized and deposited on top of the ice. In some cases this mobile material probably slides down the steep face of the Dunes, while in other cases it may be literally blown out in a process of gas release similar to the one that we could obtain by removing a cork from a champagne bottle.

Nota Lunexit: ma i commenti NASA ai frames (non tutti, ma certamente alcuni, tipo questo) li fanno scrivere ai bambini ed alle bambine di Scuole Medie e/o Licei, per caso? Lo avevamo già stigmatizzato in passato ma, a volte, repetita juvant: alcuni commenti non solo sono, in sè, piuttosto naif (diciamo "ingenui", valà...) ed alquanto banali ma - e questa è la cosa più grave - essi contengono degli strafalcioni grammaticali (frequenti) e sintattici (meno di frequente) che fanno rabbrividire noi, poveri "ignoranti Italiani".
Bah...
4 commentiMareKromium01/17/10 at 12:41MareKromium: Si Matt, hai ragione. E sono totalmente d'acco...
ESP_016087_2595_RED_abrowse.jpg
ESP_016087_2595_RED_abrowse.jpgFrost-covered Dunes (Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)58 visiteDunes are often found on Crater Floors. In the Winter time, at high Northern Latitudes, the Terrain is covered by Carbon Dioxide Ice (Dry Ice - CO2 Ice). In the Spring, as this seasonal ice evaporates or sublimates, many unusual features - certainly unique to Mars - become visible.

On the Floor of this Crater, where there are no Dunes, the ice forms an uninterrupted layer. On the Dunes, however, Dark Streaks form as surface material from below the ice is mobilized and deposited on top of the ice. In some cases this mobile material probably slides down the steep face of the Dunes, while in other cases it may be literally blown out in a process of gas release similar to the one that we could obtain by removing a cork from a champagne bottle.

Nota Lunexit: ma i commenti NASA ai frames (non tutti, ma certamente alcuni, tipo questo) li fanno scrivere ai bambini ed alle bambine di Scuole Medie e/o Licei, per caso? Lo avevamo già stigmatizzato in passato ma, a volte, repetita juvant: alcuni commenti non solo sono, in sè, piuttosto naif (diciamo "ingenui", valà...) ed alquanto banali ma - e questa è la cosa più grave - essi contengono degli strafalcioni grammaticali (frequenti) e sintattici (meno di frequente) che fanno rabbrividire noi, poveri "ignoranti Italiani".
Bah...
4 commentiMareKromium01/17/10 at 12:33John Koenig: Ciao vecchio mio! Ah... attento che ci avviciniamo...
ESP_016087_2595_RED_abrowse.jpg
ESP_016087_2595_RED_abrowse.jpgFrost-covered Dunes (Natural Colors; credits: Dr Paolo C. Fienga - Lunexit Team)58 visiteDunes are often found on Crater Floors. In the Winter time, at high Northern Latitudes, the Terrain is covered by Carbon Dioxide Ice (Dry Ice - CO2 Ice). In the Spring, as this seasonal ice evaporates or sublimates, many unusual features - certainly unique to Mars - become visible.

On the Floor of this Crater, where there are no Dunes, the ice forms an uninterrupted layer. On the Dunes, however, Dark Streaks form as surface material from below the ice is mobilized and deposited on top of the ice. In some cases this mobile material probably slides down the steep face of the Dunes, while in other cases it may be literally blown out in a process of gas release similar to the one that we could obtain by removing a cork from a champagne bottle.

Nota Lunexit: ma i commenti NASA ai frames (non tutti, ma certamente alcuni, tipo questo) li fanno scrivere ai bambini ed alle bambine di Scuole Medie e/o Licei, per caso? Lo avevamo già stigmatizzato in passato ma, a volte, repetita juvant: alcuni commenti non solo sono, in sè, piuttosto naif (diciamo "ingenui", valà...) ed alquanto banali ma - e questa è la cosa più grave - essi contengono degli strafalcioni grammaticali (frequenti) e sintattici (meno di frequente) che fanno rabbrividire noi, poveri "ignoranti Italiani".
Bah...
4 commentiMareKromium01/17/10 at 11:04MareKromium: Carissimo John/Matteo, Buon Anno, innanzitutto!

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