Although these rocks may ultimately be classed as metamorphic (and I am by no means certain of that at this point), I have something much more specific in mind when I say theme. Even assuming they are metamorphic, have they metamorphosed from sedimentary or igneous rock? The implication from Squyres seems to be that they are modified basalts. I don't think so. Basaltic minerals such as olivine and pyroxene are hard. If you take a basalt and soak it in water, you might get a rind of hematite, which is hard, or sulfate, which is soft. What you will not get is a rock with a hard rind and a soft interior, or one that is completely soft, the interior having plenty of chlorides and bromides. Sounds like a sedimentary rock to me, or a metamorphic rock derived from one.<br /><br />To be fair, Squyres is usually careful to use equivocal language, such as "I think" or "We believe at this time." I believe at this time that these hills are loaded with sedimentary rocks that have been heavily modified by the action of water. What Meridiani Planum is telling us is that Mars must have had a much thicker atmosphere at one time. Liquid water was stable on the surface. As Squyres has said, "This was a very different Mars." Not just a very different Meridian Planum. A very different Mars. Rain. Liquid water, on the surface, for substantial periods. Streams, lakes. I see no way around it. The basalt plain we came off of is recent history. The Columbia Hills are telling us a much older, much more watery story.