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Mars rover targets unusual rock en route to first destination | Astronomy.com
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Mars rover targets unusual rock en route to first destination

The scientists plan to touch the rock with a spectrometer to determine its elemental composition and use an arm-mounted camera to take close-up photographs.
Jake-Matijevic-rock
The drive by NASA's Mars rover Curiosity during the mission's 43rd martian day, or sol, (September 19, 2012) ended with this rock about 8 feet (2.5 meters) in front of the rover. // Image credit: NASA/JPL-Caltech
NASAò??s Mars rover Curiosity has driven up to a football-sized rock that will be the first for the roverò??s arm to examine.

Curiosity is about 8 feet (2.5 meters) from the rock. It lies about halfway from the roverò??s landing site, Bradbury Landing, to a location called Glenelg. In coming days, the team plans to touch the rock with a spectrometer to determine its elemental composition and use an arm-mounted camera to take close-up photographs.

Both the arm-mounted Alpha Particle X-Ray Spectrometer and the mast-mounted, laser-zapping Chemistry and Camera Instrument will be used for identifying elements in the rock. This will allow cross-checking of the two instruments.

The rock has been named ò??Jake Matijevic.ò?? Jacob Matijevic (mah-TEE-uh-vik) was the surface operations systems chief engineer for Mars Science Laboratory and the projectò??s Curiosity rover. He passed away August 20 at age 64. Matijevic also was a leading engineer for all of the previous NASA Mars rovers: Sojourner, Spirit, and Opportunity.

Curiosity now has driven six days in a row. Daily distances range from 72 feet to 121 feet (22m to 37m).

ò??This robot was built to rove, and the team is really getting a good rhythm of driving day after day when thatò??s the priority,ò?? said Richard Cook of NASAò??s Jet Propulsion Laboratory in Pasadena, California.

The team plans to choose a rock in the Glenelg area for the roverò??s first use of its capability to analyze powder drilled from interiors of rocks. Three types of terrain intersect in the Glenelg area ò?? one lighter-toned and another more cratered than the terrain Curiosity currently is crossing. The light-toned area is of special interest because it retains daytime heat long into the night, suggesting an unusual composition.
Phobos
As part of a multi-mission campaign, NASA's Curiosity rover is observing martian moon transits, the first of which involved the moon Phobos grazing the Sun's disk. // Image credit: NASA/JPL-Caltech/MSSS
ò??As weò??re getting closer to the light-toned area, we see thin, dark bands of unknown origin,ò?? John Grotzinger of the California Institute of Technology, Pasadena. ò??The smaller-scale diversity is becoming more evident as we get closer, providing more potential targets for investigation.ò??

Researchers are using Curiosityò??s Mast Camera (Mastcam) to find potential targets on the ground. Recent images from the roverò??s camera reveal dark streaks on rocks in the Glenelg area that have increased researchersò?? interest in the region. In addition to taking ground images, the camera also has been busy looking upward.

On two recent days, Curiosity pointed the Mastcam at the Sun and recorded images of Marsò?? two moons, Phobos and Deimos, passing in front of the Sun from the roverò??s point of view. Results of these transit observations are part of a long-term study of changes in the moonsò?? orbits. NASAò??s twin Mars Exploration Rovers, Spirit and Opportunity, which arrived at Mars in 2004, also observed solar transits by Marsò?? moons. Opportunity is doing so again this week.

ò??Phobos is in an orbit very slowly getting closer to Mars, and Deimos is in an orbit very slowly getting farther from Mars,ò?? said Mark Lemmon of Texas A&M University, College Station. ò??These observations help us reduce uncertainty in calculations of the changes.ò??

In Curiosityò??s observations of Phobos this week, the time when the edge of the moon began overlapping the disk of the Sun was predictable to within a few seconds. Uncertainty in timing is because Marsò?? interior structure isnò??t fully understood.

Phobos causes small changes to the shape of Mars in the same way Earthò??s Moon raises tides. The changes to Marsò?? shape depend on the martian interior which, in turn, cause Phobosò?? orbit to decay. Timing the orbital change more precisely provides information about Marsò?? interior structure.

During Curiosityò??s two-year prime mission, researchers will use the roverò??s 10 science instruments to assess whether the selected field site inside Gale Crater ever has offered environmental conditions favorable for microbial life.

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