Curiosity Mars rover poised for first 'hands-on' geology

The Curiosity Mars rover, slowly creeping across the floor of Gale Crater, is ready to attempt its first hands-on "contact science," studying a pyramid-shaped rock known as "Jake."

More than half the way to its first major scientific destination, the Curiosity Mars rover will pause a few days to perform the mission's first hands-on geology, using instruments on the vehicle's robot arm to photograph and chemically assess an intriguing pyramid-shaped rock, project managers said Wednesday.

Data from the arm-mounted Alpha Particle X-ray Spectrometer, or APXS, will be compared with remote sensing data from another instrument known as Chemcam that uses a powerful laser to vaporize tiny sections of a target's surface. Debris from the laser strike is measured remotely to help determine chemical composition.

The Curiosity rover has traveled about 950 feet from its landing site and is about 650 feet from its near-term target, an area known as Glenelg where three different terrains come together. NASA

"The science team has had an interest for some time now as we're driving across the plains to find a rock that looks like it's relatively uniform in composition to do some experiments between ChemCam, which we've been acquiring a lot of data with, and APXS, which we haven't used yet on a rock," said John Grotzinger, the Mars Science Laboratory project scientist.

"Both of those instruments could make a measurement and there could be differences between the measurements because one is measuring at a small scale (ChemCam) and one is measuring at a larger scale (APXS). These rocks that we drive by on the plains here that look dark, they probably have basaltic composition. That's a familiar material to us."

A rock dubbed "Jake," named after a Mars program engineer who died shortly after Curiosity's landing in Gale Crater, will serve as the rover's first target for a robot arm-mounted camera and chemical analyzer. NASA

The rock chosen for the initial APSX measurements, and for closeup photography by the Mars Hand Lens Imager instrument, or MAHLI, has been dubbed "Jake" in honor of Jacob Matijevic, a Jet Propulsion Laboratory mathematician and engineer who died a few days after Curiosity's August 6 landing in Gale Crater.

"The hope is we can analyze this rock and then do a cross comparison between the two instruments," Grotzinger said. "Not to mention it's just a cool-looking rock there, sitting out on the plains with almost pyramidal geometry, so that's kind of fun as well."

Curiosity is expected to spend three to four days collecting data from the MAHLI, APXS, and the ChemCam instruments before resuming its slow trek to an area known as Glenelg where three different types of terrain come together. The rover has traveled about 950 feet from its landing site and has another 700 feet or so to go.

Looking toward the Glenelg site, where Curiosity will pause to carry out extensive geological observations, scientists have identified a lighter area, also visible from orbit, that may be part of an alluvial fan where water once flowed. NASA

New photographs from Curiosity show the approach to Glenelg and the steplike terrain Curiosity will need to negotiate to reach the heart of the target zone.

"We really do think it's going to be interesting," Grotzinger said. "You can see a light-toned (rock) unit, which we believe to be material that from orbit has this signature, this property, of having relatively high thermal inertia. That's the ability of a material to retain its heat. So late in the day or at night, orbiters are able to observe this rock well. We don't know what the reason for that is, but it's always been a bit of a beacon for us and we're getting closer and closer to it."

As for getting there, Grotzinger said Curiosity will have to descend several yards, passing through darker layers that may be inter-bedded with the denser, light-toned material.

"We can also see in the (orbital) data that we can detour around that and kind of contour our way down into those lower reaches where we hope to do the bulk of our investigation at that Glenelg region," he said. "We have all the tools we need to get into this exciting area."

Curiosity's long-range goal is the base of Mount Sharp, a 3-mile-high mound of layered terrain in the center of Gale Crater that is expected to provide major insights into the geologic history of Mars and whether any organic compounds might be present like those required for life as it is known on Earth. The foothills of Mount Sharp are five to seven miles away and Curiosity is not expected to get there until early next year.

In the meantime, along with studying martian geology and weather, Curiosity's cameras also are doing a bit of astronomical observing, photographing Mars' two moons Phobos and Deimos as they pass in front of the sun. Using faster cameras than those available on earlier missions, scientists are able to precisely time the events and in so doing, measure the satellites' orbits with unprecedented accuracy.

Cameras on the Curiosity rover photographed the martian moon Phobos as it recently passed in front of the sun. Precise measurements of the timing provide insights into the internal structures of both Mars and Phobos. NASA

By studying how the orbits change over time due to gravitational interactions, researchers can gain insights into the internal composition of Mars and the moons as tidal forces affect their passage. Based on earlier observations, it appears Phobos, for example, will break apart under stress from Mars' gravity some 10 million to 15 million years from now.

"Why do we take all these images of these two little moons crossing in front of the sun?" asked Mark Lemmon, a science team co-investigator at Texas A&M University. "For one thing, they have tidal forces that they exert on Mars, they change Mars' shape ever so slightly. That, in turn, changes the moon's orbit. Phobos is slowing down, Deimos is speeding up like our moon is. This is something that happens very slowly over time.

"Phobos will eventually break up and fall into Mars and with the transits, we can measure their orbits very precisely and figure out how fast they are doing this. The reason that's interesting is it constrains Mars' interior structure. We can't go inside Mars, but we can use these to tell how much Mars deforms when the moons go by."

By precisely timing the transits, "we get information on Mars' interior structure," Lemmon said. "We think the precision of these measurements...will also tell us something about Phobos' insides and whether it's uniformly dense or if there are variations."

About the author

    Bill Harwood has been covering the U.S. space program full-time since 1984, first as Cape Canaveral bureau chief for United Press International and now as a consultant for CBS News. He has covered more than 125 shuttle missions, every interplanetary flight since Voyager 2's flyby of Neptune, and scores of commercial and military launches. Based at the Kennedy Space Center in Florida, Harwood is a devoted amateur astronomer and co-author of "Comm Check: The Final Flight of Shuttle Columbia." You can follow his frequent status updates at the CBS News Space page.

     

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