Opportunity Mars Rover Goes Six-Wheeling adult a Ridge

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This stage from NASA’s Mars Exploration Rover Opportunity looks ceiling during “Knudsen Ridge” from a hollow below. Enhanced tone creates “red zone” element on a shallow easier to recognize.
Credits: NASA/JPL-Caltech/Cornell Univ./Arizona State Univ.

NASA’s comparison Mars rover, Opportunity, is operative adeptly in some of a many severe turf of a vehicle’s 12 years on Mars, on a slope of about 30 degrees.

Researchers are regulating Opportunity this month to inspect rocks that might have been chemically altered by H2O billions of years ago. The mission’s stream targets of review are from ruddy-tinted swaths a researchers call “red zones,” in contrariety to tan bedrock around these zones.

The targets distortion on “Knudsen Ridge,” atop a southern side of “Marathon Valley,” that slices by a western edge of Endeavour Crater.

This stereo perspective from NASA’s Mars Exploration Rover Opportunity looks ceiling during “Knudsen Ridge” from a hollow below. The stage appears 3 dimensional when noticed by blue-red eyeglasses with a red lens on a left. It was performed with a breathtaking camera on Opportunity’s mast.
Credits: NASA/JPL-Caltech/Cornell Univ./Arizona State Univ.

A scenery of Knudsen Ridge is online at:

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

“We’re anticipating to take advantage of a high topography that Mars provides us during Knudsen Ridge to get to a improved instance of a red section material,” pronounced Steve Squyres of Cornell University, Ithaca, New York, principal questioner for a mission.

The red section element crumbles easily. At locations in Marathon Valley where Opportunity already got a tighten demeanour during it, a reddish pieces are blended with other lax element accumulating in low locations. A purer bearing of a red section material, such as some apparent on a ridge, would yield a improved aim for a Alpha Particle X-ray Spectrometer on Opportunity’s arm, that reveals a chemical combination of rocks and soil.

Opportunity began climbing Knudsen Ridge in late Jan with dual drives totaling 31 feet (9.4 meters). The wheels slipped reduction than 20 percent adult slopes as high as 30 degrees, a steepest a corsair has driven given a initial year on Mars in 2004. The trip is distributed by comparing a stretch a rotating wheels would have lonesome if there were no slippage to a stretch indeed lonesome in a drive, formed on “visual odometry” imaging of a turf a corsair passes as it drives.

“Opportunity showed us how sure-footed she still is,” pronounced Mars Exploration Rover Project Manager John Callas during NASA’s Jet Propulsion Laboratory, Pasadena, California. “The circle trip has been most reduction than we approaching on such high slopes.”

This stage from NASA’s Mars Exploration Rover Opportunity looks ceiling during “Knudsen Ridge” from a hollow below.
Credits: NASA/JPL-Caltech/Cornell Univ./Arizona State Univ.

The corsair done additional swell toward targets of red-zone element on Knudsen Ridge with a expostulate on Feb. 18.

Knudsen Ridge forms a thespian top unaware a 14-mile-wide (22-kilometer-wide) Endeavour Crater. Its spontaneous fixing honors a memory of Danish astrophysicist and heavenly scientist Jens Martin Knudsen (1930-2005), a first member of a scholarship group for Opportunity and a twin corsair Spirit. “This shallow is so spectacular, it seemed like an suitable place to name for Jens Martin,” Squyres said.

Marathon Valley became a high-priority end for a Opportunity goal when mineral-mapping observations by a Compact Reconnaissance Imaging Spectrometer for Mars (CRISM), aboard NASA’s Mars Reconnaissance Orbiter, located clay minerals (a form of phyllosilicate) in this valley. Clay minerals mostly form in a participation of water, that is because this is such a earnest area of exploration. Opportunity found justification of ancient H2O shortly after landing, though there were signs that a H2O would have been some-more rarely acidic. The review in Marathon Valley could supplement bargain about a ancient environmental context for a participation of non-acidic water, a cause auspicious for microbial life, if any has ever existed on Mars.

“The locations of red zones in Marathon Valley relate closely with a phyllosilicate signature we see from orbit,” Squyres said. “That alone is not a smoking gun. We wish to establish what it is about their chemistry that sets them detached and what it could have to do with water.”

To exam a thought that H2O influenced a red section material, a hearing underway aims to review a chemistry of that element to a chemistry of a surrounding tan bedrock, that could paint an unaltered baseline. Opportunity used a diamond-toothed stone erosion apparatus final month to scratch a membrane off a tan bedrock aim for an hearing of a chemistry inside a rock.

The group is accomplishing prolific scholarship with Opportunity while avoiding use of a rover’s peep memory, that was related to several random mechanism reboots final year. The usually information being perceived from Opportunity is what can be transmitted any day before a solar-powered corsair shuts down for energy-conserving overnight “sleep.”

Source: NASA