QUOTE (PaulH51 @ Jul 19 2018, 09:39 AM)
Is it probably just my wishful thinking, but the cuttings appear to bunched together and aligned by size at the rim of the hole. I was reminded of iron filings on a sheet of paper held above the pole of a magnet. Could this be an indication that the hematite-rich minerals at this hot spot are slightly magnetic?
If there would be a significant overall magnetic field, and the grains would consist partially of magnetite, the particles would probably line up parallel to magnetic field lines. I don't perceive such an effect here. But slightly magnetic particles might clot together in a more random fashion.
Here, I'm inclined to presume, that the pattern the tailings are forming after the LIBS shots are just a result of the wind pressure decreasing with distance from the LIBS hits, maybe combined with the slope of the abraded area, and surface roughness, but without obvious evidence of magentism being involved.
Compositionally, this would suggest absence of magnetite that might have been magnetized by friction. But the color, of course, suggests presence of hematite.
And the hardness of the rock could explain why there is a ridge.
It would be interesting to know, whether the hematite itself is the cause of the hardness, or if it just plays the role of a pigment, and the hardness is caused by another mineral, like e.g. quartz. But APXS should be able to provide constraints, even if the drill powder isn't accessible for CheMin.