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|    sci.space.science    |    Space and planetary science and related    |    1,217 messages    |
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|    Message 907 of 1,217    |
|    David Stinson to Jeffrey Cornish    |
|    Re: Mars "Blueberries"    |
|    03 May 05 07:59:54    |
      From: arc5@ix.netcom.com              Jeffrey Cornish wrote:              > As metorite impacts are random events, and the debris from such impacts       > would likely be randomly sized, please explain the uniform size and       > distribution of the blueberries.              Uniform distribution:       We cannot really say this; the rovers have covered       a vanishingly small fraction of the surface.       Even if we do see blueberries over a wide area-       the Martian atmosphere is not as dynamic as the Earth's and       would have a similar effect on wet, fine-grained matter       over a larger area.       Given the consistent texture of the fine-grained component       of impact ejecta on the Martian surface,       consistent upper atmosphere dynamics over a large part of the planet       and also given a surface covered either with a shallow brine sea       or with saturated mud flats (the current model), the ejecta       from large impacts would behave in a consistent manner.              The blueberries we see are uniform in size for several reasons:       The wet, pulverized particles ejected into the upper atmosphere would       be "sorted" (larger particles falling out at lower altitudes), sending       very fine-grain and water saturated material into the cold, windy       Martian "stratosphere." As with Earthly hailstones, the energy of       the fine-grain mud's motion, transferred into rotation as the particles       froze and accumulated, acquire a rounded shape as their "spin"       precludes further accumulation, the size of the spheres being       dependent on many factors but mostly on these atmospheric effects,       which we already know to be more uniform over a larger area than in       an Earthly "thunderstorm." Earth storms generate hailstones       of uniform size in this manner,       their sphericial size dependent on the storm's dynamics over       the area it covers. Since Martian atmospheric dynamics are       still energetic but simpler, the similar-sized "mud hail" result       would cover a much wider area with a consistent hailstone size.       Lower gravity, lower atmospheric pressure, etc.- all contribute       to a more uniform process over a larger area.              And it's still just "one man's opinion;"       I'm not smart enough to deal in hypothesis ;-).       What would disprove it?       Several things could-       the first being general disuniformity in       the internal structures or large-particle inclusions       ( in the few we've seen "ground open,"       the structure has been fine and uniform, such as you would expect       from the process I've posited).       A closer study of the fine grain that supported slow accumulation       as in the current "concretion" hypothesis would disprove it.       Frankly, I think the lack of large inclusions stands against       the "concretion" answer, along with other questions.       I'm sure there are others- I guess we'll have to wait       until someone actually has some blueberries to study.       Don't hold your breath ;-).              Kindly,       David S.              --- SoupGate-Win32 v1.05        * Origin: you cannot sedate... all the things you hate (1:229/2)    |
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