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News / Life / Science & Technology

Study: Streaks on Mars are sand, not water

A new study suggests that dark streaks on Mars are signs of flowing sand, not water

By MARCIA DUNN, Associated Press
Published: November 21, 2017, 6:00am

CAPE CANAVERAL, Fla. — A new study suggests that dark streaks on Mars represent flowing sand — not water.

Monday’s news throws cold water on 2015 research that indicated that lines on some Martian slopes were signs of water currently on the planet. Instead, Arizona scientists report in Nature Geoscience that these lines appear more like dry, steep flows of sand, rather than water trickling downhill, at or near the surface.

If water is present, they said, it’s likely a small amount — and not conducive to life.

NASA, though, said the jury is still out.

The lead scientist for NASA’s Mars exploration program, Michael Meyer, points out that the latest study does not rule out the presence of water. But he acknowledges, “It just may not be as exciting as the idea of rivers going down the sides of cliffs.”

NASA’s Mars Reconnaissance Orbiter provided the images of these so-called recurring slope lineae, or RSL. Thousands have been spotted on Mars, from the equator midway to each pole.

The team led by the U.S. Geological Survey’s Colin Dundas in Flagstaff, Ariz., measured 151 of these dark lines at 10 sites. Most of them end with slopes between 28 degrees and 35 degrees, a match for active sand dunes on both Mars and Earth, according to the researchers. A thin layer of dust on top that shifts and sometimes brightens the surface might help explain why these streaks seem to occur in the Martian summertime and then disappear, only to reappear the next year.

If these lines are dry, “this suggests that recent Mars has not had considerable volumes of liquid water,” the researchers write.

That’s key because water in liquid form would be essential to microbial life.

Dundas and his colleagues stress that many questions remain, demanding further study.

To Meyer, this is what makes Mars so fun.

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