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Fe sites in day minerals

Fig. 8.34 Lefty, outcrop rocks found at the crater wall of Eagle Crater, where the rover Opportunity landed on 24 January 2004. Clearly, the sedimentary structure is seen. Right) in the spectrum, taken on sol 33 (sol = Martian day) of the mission, the mineral Jarosite, an Fe -sulfate, could be identified at the Meridiani Planum landing site. It forms only under aqueous conditions at low pH (< 3 ) and is therefore clear mineralogical evidence for aqueous processes on Mars... Fig. 8.34 Lefty, outcrop rocks found at the crater wall of Eagle Crater, where the rover Opportunity landed on 24 January 2004. Clearly, the sedimentary structure is seen. Right) in the spectrum, taken on sol 33 (sol = Martian day) of the mission, the mineral Jarosite, an Fe -sulfate, could be identified at the Meridiani Planum landing site. It forms only under aqueous conditions at low pH (< 3 ) and is therefore clear mineralogical evidence for aqueous processes on Mars...

See other pages where Fe sites in day minerals is mentioned: [Pg.289]    [Pg.291]    [Pg.299]    [Pg.303]    [Pg.307]    [Pg.289]    [Pg.291]    [Pg.299]    [Pg.303]    [Pg.307]    [Pg.81]    [Pg.610]    [Pg.547]    [Pg.651]    [Pg.28]    [Pg.289]    [Pg.61]   


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