National Aeronautics and Space Administration

Summary

National Aeronautics and Space Administration MER press briefing, February 9…

You can see the layers, inherently very, very fine-grained sitting there for millions of years being sandblasted. This stuff sits there, the wind blows, these grains are striking and eroding the softer portions developing this intricate texture telling you how well indurated the rock is. Then embedded in the stuff are the little spherules. Those seem to be pretty tough. So what happens is that the rock erodes away as it gets sandblasted and the little blueberries drop out and roll down the slope where we take pictures of them. There's one in the process of being eroded out.
Source: Wikisource

National Aeronautics and Space Administration MER press briefing, February 9…

Everything we're seeing so far is either the outcrop itself and some of the stuff that's fallen down. Some that's fallen has fallen from the outcrop and some maybe from above. We can't tell with the granules in the crater in front of us, their pedigree is unknown. That's the nice thing about the spherules in the outcrop. You know where they come from. The evidence suggests that the highest concentration of hematite comes from up above the outcrop layer that we're not gonna see until we start to climb out of this crater.
Source: Wikisource

National Aeronautics and Space Administration MER press briefing, February 9…

I think the idea that they're lapilli would only work with the matrix being volcanic ash. Those two are tied together. With respect to concretions, if you have fluid, water with dissolved stuff in it flowing through a sediment, it can precipitate minerals, stuff that's dissolved in the water, and commonly will nucleate in a spot and this concretion will grow and grow in a spherical fashion. These are found in a variety of settings on the earth. By making observations about how these round things are related to the layers, we can test distinguish between the various hypothesis.
Source: Wikisource

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