Update: NASA today announced the destination for its next Mars rover, due for launch in 2020. The agency said it would send the rover to the 50-kilometer-wide Jezero crater, which billions of years ago harbored a lake that half filled the 500-meter-deep basin. The crater also contains within its rim a fossilized river delta, the sediments from a river that spilled into the crater—a promising place to search for evidence of past life. “Getting samples from this unique area will revolutionize how we think about Mars and its ability to harbor life,” Thomas Zurbuchen, NASA’s associate administrator for science in Washington, D.C., said in a press conference.
Mars scientists also wanted to visit a nearby site, called Northeast Syrtis, which contains rocks formed in the presence of mineral springs. So NASA dangled the possibility of a two-for-one special—that after visiting Jezero, the rover might climb out of the crater and travel 25 kilometers to Midway, a site that contains many of the same rocks as Northeast Syrtis. Zurbuchen said the possibility of an extended mission to Midway is not ruled out, but he wants the team to focus on Jezero crater for now. “Come the time, we want to talk about it,” he said. “But at this moment we’re focusing on the prime mission.”
The 2020 rover will be tasked with gathering and caching rock and soil samples for eventual return to Earth by subsequent missions. At a workshop attended by hundreds of Mars scientists a month ago, Jezero was one of the leading landing sites. Here is our previous story from 10 October:
Sometimes, a problem really can be solved by meeting halfway. For the past 4 years, planetary scientists have wrestled over where to send NASA's next Mars rover, a $2.5 billion machine to be launched in 2020 that will collect rock samples for eventual return to Earth. Next week, nearly 200 Mars scientists will gather for a final landing site workshop in Glendale, California, where they will debate the merits of the three candidate sites that rose to the top of previous discussions. Two, Jezero and Northeast Syrtis, hold evidence of a fossilized river delta and mineral springs, both promising environments for ancient life. Scientists yearn to visit both, but they are 37 kilometers apart—much farther than any martian rover has traveled except Opportunity.
Now, the Mars 2020 science team is injecting a compromise site, called Midway, into the mix. John Grant, a planetary scientist at the Smithsonian Institution's Center for Earth and Planetary Studies at the National Air and Space Museum in Washington, D.C., who co-leads the landing site workshops, says the team wanted to know whether a rover might be able to study the terrains found at Jezero and Northeast Syrtis by landing somewhere in the middle.
So far, the answer appears to be yes. The Mars 2020 rover borrows much from the design of the Curiosity rover that has been exploring another Mars site for 6 years. But it includes advances such as a belly-mounted camera that will help it avoid landing hazards during its harrowing descent to the surface. This capability allowed scientists to consider Midway, just 25 kilometers from Jezero and close enough to drive there. At the same time, Midway's rocks resemble those of Northeast Syrtis, says Bethany Ehlmann, a planetary scientist at the California Institute of Technology (Caltech) in Pasadena and member of the Mars 2020 science team.
Midway and Northeast Syrtis both hail from a time, some 4 billion years ago, when Mars was warmer and wetter. Surveys from orbit suggest the sites harbor rocks that formed underground in the presence of water and iron, a potential food for microbes. The rocks, exposed on the flanks of mesas, include a layer of carbonate deposits that many scientists believe were formed by underground mineral springs. Sheltered from a harsh surface environment, these springs would have been hospitable to life, Ehlmann says. "We should go where the action was."
Nearby Jezero crater has its own allure, etched on the surface: a fossilized river delta. Nearly 4 billion years ago, water spilled into the crater, creating the delta. "It's right there," says Ray Arvidson, a planetary geologist at Washington University in St. Louis, Missouri. "It's beautiful." Geologists know deltas concentrate and preserve the remnants of life; they can see that on Earth in offshore deposits of oil—itself preserved organic matter—fed by deltas like the Mississippi's. New work to be presented at the workshop by Briony Horgan, a planetary scientist at Purdue University in West Lafayette, Indiana, will show that Jezero crater has a bathtub ring of carbonate—a strong sign that it once contained a lake. On Earth, such layers are often home to stromatolites, cauliflowerlike minerals created by ancient microbial life.
Right now, the Mars 2020 team favors landing at Jezero and driving uphill to Midway, says Matt Golombek, a planetary scientist at NASA's Jet Propulsion Lab (JPL) in Pasadena, and the other workshop co-leader. For the past year, the team has scoured potential routes between the two. "We haven't identified any deal-breakers," says Ken Farley, the mission's project scientist and a Caltech geologist. The rover's advanced autonomous driving should allow it to cover more ground than Curiosity, which often stops to plan routes. Even so, the path from Jezero to Midway would take nearly 2 years, Farley says. That means the rover could explore only one site during its primary 2-year mission, when it must drill and store 20 rock cores, to be picked up by future sample return missions. Exploration of the second site would have to come during an extended mission, after the rover's warranty expires. "The further away you land from your gold mine, the higher the risk you might not get there," Arvidson says.
Left out of those plans is the last leading candidate site: Columbia Hills. "I have a sense there's a hill to climb," says the site's chief advocate, Steven Ruff, a planetary scientist at Arizona State University in Tempe. "I'll go in with a lot of questions of whether they can make that drive between Midway and Jezero." Columbia Hills sits within the large Gusev crater that the Spirit rover explored from 2004 to 2010. Driving backward while dragging a bad front wheel, Spirit gouged a trench that revealed opaline silica, a mineral that on Earth is a sure sign of life-supporting hot springs. Ruff has even proposed that the martian silica deposits are stromatolites.
The engineers building Mars 2020 will be glad to settle on a destination, says Matt Wallace, the rover's deputy project manager at JPL. The lab's clean room is starting to fill up. The "sky crane" that will lower the rover to the surface is done. The spacecraft that will shepherd the rover to Mars is nearly complete—it just needs a heat shield, which is being rebuilt after testing revealed a crack. Several weeks ago, the chassis of the rover arrived and is now being filled with computers, batteries, and other electronics. Assembly of its complex drilling and sample storage system is underway, with other scientific instruments due by the end of February. "This is the mad scramble," Farley adds. "It is full bore get it done, get it done now."
At the workshop's end, scientists will vote on the candidates, followed by a closed-door meeting of the rover team to make a final choice. Engineers have deemed the sites safe for landing, Golombek adds, so it will come down to the science. The team's recommendation won't be the final word—the choice is ultimately up to NASA science chief Thomas Zurbuchen. But expect a decision within the next few months, if not sooner.
*Correction, 12 October, 11:20 a.m.: An earlier version of this story incorrectly stated that no rover has traveled more than 37 kilometers or visited 4-billion-year-old martian terrain. The Opportunity rover has done both.