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Mars Reconnaissance Orbiter a detectat prezenta carbonatului mineral in rocile din regiunea Nili Fossae, o zona formata din vai sapate adanc in crusta. Mineralul, care se formeaza in prezenta apei, a fost detectat si anterior in mici mostre de sol si praf martian, insa prezenta sa in roci indica faptul ca apa nu era foarte acida, prin urmare putea sustine viata.
Urmatoarea misiune pe Marte este fixata pentru anul 2011, iar unul dintre locurile posibile in care va amartiza sonda Mars Science Laboratory este chiar valea Nili Fossae.
Sursa: The Independent
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