• Opportunity Mars Rover Goes Six-Wheeling up a Ridge

    From baalke@1:2320/100 to sci.space.news on Thu Feb 25 22:35:05 2016
    From Newsgroup: sci.space.news

    http://www.jpl.nasa.gov/news/news.php?feature=5580

    Opportunity Mars Rover Goes Six-Wheeling up a Ridge
    Jet Propulsion Laboratory
    February 25, 2016

    NASA's senior Mars rover, Opportunity, is working adeptly in some of the
    most challenging terrain of the vehicle's 12 years on Mars, on a slope
    of about 30 degrees.

    Researchers are using Opportunity this month to examine rocks that may
    have been chemically altered by water billions of years ago. The mission's current targets of investigation are from ruddy-tinted swaths the researchers call "red zones," in contrast to tan bedrock around these zones.

    The targets lie on "Knudsen Ridge," atop the southern flank of "Marathon Valley," which slices through the western rim of Endeavour Crater.

    A panorama of Knudsen Ridge is online at:

    http://www.jpl.nasa.gov/spaceimages/details.php?id=PIA20319

    "We're hoping to take advantage of the steep topography that Mars provides
    us at Knudsen Ridge to get to a better example of the red zone material,"
    said Steve Squyres of Cornell University, Ithaca, New York, principal investigator for the mission.

    The red zone material crumbles easily. At locations in Marathon Valley
    where Opportunity already got a close look at it, the reddish bits are
    blended with other loose material accumulating in low locations. A purer exposure of the red zone material, such as some apparent on the ridge,
    would provide a better target for the Alpha Particle X-ray Spectrometer
    on Opportunity's arm, which reveals the chemical composition of rocks
    and soil.

    Opportunity began climbing Knudsen Ridge in late January with two drives totaling 31 feet (9.4 meters). The wheels slipped less than 20 percent
    up slopes as steep as 30 degrees, the steepest the rover has driven since
    its first year on Mars in 2004. The slip is calculated by comparing the distance the rotating wheels would have covered if there were no slippage
    to the distance actually covered in the drive, based on "visual odometry" imaging of the terrain the rover passes as it drives.

    "Opportunity showed us how sure-footed she still is," said Mars Exploration Rover Project Manager John Callas at NASA's Jet Propulsion Laboratory, Pasadena, California. "The wheel slip has been much less than we expected
    on such steep slopes."

    The rover made additional progress toward targets of red-zone material
    on Knudsen Ridge with a drive on Feb. 18.

    Knudsen Ridge forms a dramatic cap overlooking the 14-mile-wide (22-kilometer-wide)
    Endeavour Crater. Its informal naming honors the memory of Danish astrophysicist
    and planetary scientist Jens Martin Knudsen (1930-2005), a founding member
    of the science team for Opportunity and the twin rover Spirit. "This ridge
    is so spectacular, it seemed like an appropriate place to name for Jens Martin," Squyres said.

    Marathon Valley became a high-priority destination for the Opportunity
    mission when mineral-mapping observations by the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM), aboard NASA's Mars Reconnaissance Orbiter, located clay minerals (a type of phyllosilicate) in this valley.
    Clay minerals often form in the presence of water, which is why this is
    such a promising area of exploration. Opportunity found evidence of ancient water shortly after landing, but there were signs that the water would
    have been more highly acidic. The investigation in Marathon Valley could
    add understanding about the ancient environmental context for the presence
    of non-acidic water, a factor favorable for microbial life, if any has
    ever existed on Mars.

    "The locations of red zones in Marathon Valley correlate closely with
    the phyllosilicate signature we see from orbit," Squyres said. "That alone
    is not a smoking gun. We want to determine what it is about their chemistry that sets them apart and what it could have to do with water."

    To test the idea that water affected the red zone material, the experiment underway aims to compare the chemistry of that material to the chemistry
    of the surrounding tan bedrock, which could represent an unaltered baseline. Opportunity used its diamond-toothed rock abrasion tool last month to
    scrape the crust off a tan bedrock target for an examination of the chemistry inside the rock.

    The team is accomplishing productive science with Opportunity while avoiding use of the rover's flash memory, which was linked to several unplanned computer reboots last year. The only data being received from Opportunity
    is what can be transmitted each day before the solar-powered rover shuts
    down for energy-conserving overnight "sleep."

    For more information about Opportunity, visit:

    http://www.nasa.gov/rovers

    http://marsrovers.jpl.nasa.gov


    Media Contact

    Guy Webster
    Jet Propulsion Laboratory, Pasadena, Calif.
    818-354-6278
    guy.webster@jpl.nasa.gov

    Dwayne Brown / Laurie Cantillo
    NASA Headquarters, Washington
    202-358-1726 / 202-358-1077
    dwayne.c.brown@nasa.gov / laura.l.cantillo@nasa.gov

    2016-050

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