Curiosity rover celebrates 2,000 sols on Mars as it prepares to examine ancient clays

Mosaic image of the current view towards Mount Sharp. The region rich in clay minerals cuts across the center of the image. Photo Credit: NASA/JPL-Caltech/MSSS

Time goes by quickly when you are exploring Mars. It may not seem like it, but NASA’s Curiosity rover has now passed the 2,000-sol marksince its landing way back in August 2012. In those 5+ years, the rover has discovered evidence that Gale crater used to be home to a large non-acidic lake or series of lakes, with conditions suitable for life to have existed. It is still not known whether any Martian critters, most likely microscopic, ever did live there or elsewhere on the planet, but thanks to Curiosity and other robotic explorers, we now know that they certainly could have.

A sol is a Martian day, just a bit longer than an Earth day. Going beyond 2,000 sols is a major milestone for Curiosity, although not too surprising, since the rover was designed to last at least several years thanks to being nuclear powered, which can easily outlast the solar power lifetimes of previous rovers. It should be noted however that the Opportunity rover, which landed in 2004, is also still going strong after about 14 years! Curiosity has traveled a total of 18.7 kilometres (11.6 miles) so far during that time, racking up many different discoveries.

The current view (sol 2003) from the top of Vera Rubin Ridge, looking toward the mountainous rim of Gale crater. Photo Credit: NASA/JPL-Caltech

As mentioned on the NASA website, Curiosity is currently exploring the lower slopes of Mount Sharp, a huge mountain in the middle of Gale crater, which can provide more clues about the habitability of this region a few billion years ago. Right now it is still on Vera Rubin Ridge, which contains large amounts of hematite. The rover’s next target for study just up ahead is a region rich in clay minerals. These kinds of minerals tend to form in the presence of water, so they are important in determining what conditions were like when the lake(s) existed.

“The formation of clay minerals requires water. Scientists have already determined that the lower layers of Mount Sharp formed within lakes that once spanned Gale Crater’s floor. The area ahead could offer additional insight into the presence of water, how long it may have persisted, and whether the ancient environment may have been suitable for life.”

A new test drill hole from Feb. 26, 2018, the first since the drill became inoperable in December 2016. Photo Credit: NASA/JPL-Caltech/MSSS

Curiosity reached the base of Mount Sharp in 2014 and has examined 600 vertical feet of rock which contains evidence of the ancient lakes as well as groundwater.

Another significant accomplishment is that the rover team has started testing the use of the drill again, on a rock target called Lake Orcadie – the first time since December 2016, after problems with the drill mechanism caused it to be inoperable.

“The development work and testing here at JPL has been promising,” said Deputy Project Manager Steve Lee, of NASA’s Jet Propulsion Laboratory in Pasadena, California. “The next step is to assess the force/torque sensor on Mars. We’ve made tremendous progress in developing feed-extended drilling, using the rover’s versatile capabilities beyond the original design concepts. While there are still uncertainties that may complicate attempts to drill on Mars again, we are optimistic.”

Martian riverbed gravel, which show that shallow rivers once flowed into the lake(s) in Gale crater. The inset is a close-up view. Image Credit: NASA/JPL-Caltech/MSSS
Ancient mud cracks in Gale crater; red marks are where the rock was hit with the rover’s laser for analysis. Image Credit: NASA/JPL-Caltech/LANL/CNES/IRAP/LPGNANTES/CNRS/IAS

Curiosity also recently examined some unusual stick-like rock formations and found that the methane in the Martian atmosphere appears to be seasonal, a finding which may relate to the possibility of current microscopic life. As Pascal Lee, a planetary scientist at NASA Ames, Mars Institute and SETI Institute, previously mentioned:

“The Curiosity pic really piques our curiosity. From this picture alone, it’s hard to tell what the wiggly sticks are, and a strictly mineral origin is of course the most plausible. But as a field geologist, when I first saw the pic, the immediate thought that came to my mind is bioturbation. Bioturbation is the process through which organisms living in sediments can disturb the very structure of these sediments. A common example of bioturbation is the formation of worm burrows. The burrows, once refilled with sediments, fossilized, and then exposed by erosion, can end up looking like wiggly sticks.”

MAHLI view of the unusual “sticks” seen by the Curiosity rover on sol 1922. Their origin is currently being debated. Photo Credit: NASA/JPL-Caltech/MSSS

Regarding the methane, “The thing that’s so shocking here is this large variation,” said Chris Webster, who leads the methane-sensing instrument on NASA’s Curiosity rover. “We’re left trying to imagine how we can create this seasonal variation,” said Webster, who is at the Jet Propulsion Laboratory in Pasadena, California.

Now that the 2,000-sol milestone has been achieved, we can look forward, hopefully, to the 3,000th sol of Curiosity’s exploration of the Red Planet. What else is waiting to be discovered?

More information about Curiosity is available on the mission website.

This article was first published on AmericaSpace.

 

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