They call it "Bonanza King."
It is not at the "Pahrump Hills" site the team anticipated the rover might reach by mid-August. Unexpected challenges while driving in sand prompted the mission to reverse course last week after entering a valley where ripples of sand fill the floor and extend onto sloping margins. However, the new target outcrop's brightness and its position within the area's geological layers resemble the Pahrump Hills outcrop.
"Geologically speaking, we can tie the Bonanza King rocks to those at Pahrump Hills. Studying them here will give us a head start in understanding how they fit into the bigger picture of Gale Crater and Mount Sharp," said Curiosity Deputy Project Scientist Ashwin Vasavada of NASA's Jet Propulsion Laboratory in Pasadena, California.
Mount Sharp is the mission's long-term science destination, offering a stack of layers holding evidence about environmental changes on ancient Mars. The mountain rises from inside Gale Crater, where Curiosity landed in August 2012. All three rocks the rover has drilled so far have been geologically associated with the crater floor, rather than the mountain. Sample material pulled from the first two and delivered to Curiosity's onboard analytical laboratories in 2013 provided evidence for ancient environmental conditions favorable for microbial life. A drilled sample from Bonanza King may add understanding about how environments varied and evolved.
It lies in one of several patches of similar-looking slabs, up to about the size of dinner plates, on the ramp at the northeastern end of sandy-floored "Hidden Valley." Curiosity passed over them early last week when it entered the valley, headed toward Pahrump Hills and, beyond that, toward the planned entry point to Mount Sharp's slopes.
The rover's wheels slipped more in Hidden Valley's sand than the team had expected based on experience with one of the mission's test rovers driven on sand dunes in California. The valley is about the length of a football field and does not offer any navigable exits other than at the northeastern and southwestern ends.
"We need to gain a better understanding of the interaction between the wheels and Martian sand ripples, and Hidden Valley is not a good location for experimenting," said Curiosity Project Manager Jim Erickson of JPL.
Terrain with sharp rocks that Curiosity has previously navigated tore holes in the rover's wheels. Sandy terrain could still be part of the rover's route to Mount Sharp. Compared to sharp-rock terrain, sandy ground could reduce the pace of wheel damage. In some sandy areas, ripples don't cover the ground deeply wall-to-wall, as they do in Hidden Valley.
Curiosity reversed course and drove out of Hidden Valley northeastward. On the way toward gaining a good viewpoint to assess a possible alternative route north of the valley, it passed over the pale paving stones on the ramp again. Where a rover wheel cracked one of the rocks, it exposed bright interior material, possibly from mineral veins.
"We considered postponing the first condensed drilling, and we considered other possible drilling targets, but this outcrop on the ramp is too appealing to pass up," Vasavada said.
One step in assessing whether Bonanza King can be drilled will be to check whether the individual plates of the outcrop are loose. During the drilling campaign, the team will also be analyzing possible routes to Mount Sharp and planning how to better understand how the rover's wheels interact with Martian sand ripples.
JPL, a division of Caltech, built Curiosity and manages Mars rover projects for NASA's Science Mission Directorate in Washington.
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Jet Propulsion Laboratory, Pasadena, Calif.