F
fangsheath
Guest
I am truly stunned to see how different Wishstone is chemically from the rocks of West Spur, less than a quarter of a mile away. Not only is it remarkably rich in potassium and phosphorus, it is stunningly poor in chromium. Chlorine and sulfur are higher than is typical of the basaltic rocks of the plain, but lower than those of the West Spur rocks. Even after I saw that Wishstone was distinctly different in morphology (and another nearby rock seems to have similar appearance), I did not suspect that it would be so dramatically different in chemistry. The phosphorus level, to my knowledge, is well above that of every other Martian rock thus far examined. Of course phosphorus is an important element in living organisms on this planet.<br /><br />In petrological terms I still don't know what we're looking at here, perhaps a volcanic breccia of some sort. But what this says is that the Columbia Hills are complex and diverse, and it's virtually all bets off as to what lies ahead. We will need to try to hit as many areas as possible. I hope our little robot friend is up to it. I believe if we can just get another 60 m eastward we will be able to see for miles to the northeast.