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|    BAMA    |    Science Research Echo    |    1,586 messages    |
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|    Message 352 of 1,586    |
|    Roger Nelson to All    |
|    Curiosity Finds Old Streambed on Mars    |
|    27 Sep 12 17:24:45    |
      Hello All!              Curiosity Finds Old Streambed on Mars              Sept. 27, 2012: NASA's Curiosity rover mission has found evidence a stream       once ran vigorously across the area on Mars where the rover is driving. There       is earlier evidence for the presence of water on Mars, but this evidence --       images of rocks containing ancient streambed gravels -- is the first of its       kind.               "From the size of gravels it carried, we can interpret the water was moving       about 3 feet per second, with a depth somewhere between ankle and hip deep,"       said Curiosity science co-investigator William Dietrich of the University of       California, Berkeley. "Plenty of papers have been written about channels on       Mars with many different hypotheses about the flows in them. This is the first       time we're actually seeing water-transported gravel on Mars. This is a       transition from speculation about the size of streambed material to direct       observation of it."               http://www.youtube.com/watch?v=7sT6FOIfVOI              NASA's Curiosity rover found evidence for an ancient, flowing stream on Mars       at a few sites, including the rock outcrop pictured here, which the science       team has named "Hottah" after Hottah Lake in Canada's Northwest Territories.       Image credit: NASA/JPL-Caltech/MSSS               The finding site lies between the north rim of Gale Crater and the base of       Mount Sharp, a mountain inside the crater. Earlier imaging of the region from       Mars orbit allows for additional interpretation of the gravel-bearing       conglomerate. The imagery shows an alluvial fan of material washed down from       the rim, streaked by many apparent channels, sitting uphill of the new finds.               The rounded shape of some stones in the conglomerate indicates long-distance       transport from above the rim, where a channel named Peace Vallis feeds into       the alluvial fan. The abundance of channels in the fan between the rim and       conglomerate suggests flows continued or repeated over a long time, not just       once or for a few years.               The discovery comes from examining two outcrops, called "Hottah" and "Link,"       with the telephoto capability of Curiosity's mast camera during the first 40       days after landing. Those observations followed up on earlier hints from       another outcrop, which was exposed by thruster exhaust as Curiosity, the Mars       Science Laboratory Project's rover, touched down.               "Hottah looks like someone jack-hammered up a slab of city sidewalk, but it's       really a tilted block of an ancient streambed," said Mars Science Laboratory       Project Scientist John Grotzinger of the California Institute of Technology in       Pasadena.               The gravels in conglomerates at both outcrops range in size from a grain of       sand to a golf ball. Some are angular, but many are rounded.               "The shapes tell you they were transported and the sizes tell you they       couldn't be transported by wind. They were transported by water flow," said       Curiosity science co-investigator Rebecca Williams of the Planetary Science       Institute in Tucson, Ariz.               The science team may use Curiosity to learn the elemental composition of the       material, which holds the conglomerate together, revealing more        haracteristics of the wet environment that formed these deposits. The stones       in the conglomerate provide a sampling from above the crater rim, so the team       may also examine several of them to learn about broader regional geology.               The slope of Mount Sharp in Gale Crater remains the rover's main destination.       Clay and sulfate minerals detected there from orbit can be good preservers of       carbon-based organic chemicals that are potential ingredients for life.               "A long-flowing stream can be a habitable environment," said Grotzinger. "It       is not our top choice as an environment for preservation of organics, though.       We're still going to Mount Sharp, but this is insurance that we have already       found our first potentially habitable environment."                      Production editor: Dr. Tony Phillips | Credit: Science@NASA              More Information        During the two-year prime mission of the Mars Science Laboratory, researchers       will use Curiosity's 10 instruments to investigate whether areas in Gale       Crater have ever offered environmental conditions favorable for microbial       life.               NASA's Jet Propulsion Laboratory, a division of Caltech, built Curiosity and       manages the Mars Science Laboratory Project for NASA's Science Mission       Directorate, Washington.               For more about Curiosity, visit: http://www.nasa.gov/msl and htt       ://mars.jpl.nasa.gov/msl .               You can follow the mission on Facebook and Twitter at: http://ww       .facebook.com/marscuriosity and http://www.twitter.com/marscuriosity .                       Regards,              Roger        --- timEd/386 1.10.y2k+        * Origin: NCS BBS - Houma, LoUiSiAna - (1:3828/7)    |
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