ChemCam Follows the ‘Yellowknife Road’ to Martian Wet Area

Researchers have tracked a trail of minerals that point to the prior presence of water at the Curiosity rover site on Mars.

Written byLos Alamos National Laboratory
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Researchers have tracked a trail of minerals that point to the prior presence of water at the Curiosity rover site on Mars.

LOS ALAMOS, N.M., January 15, 2013—Researchers from Los Alamos National Laboratory and the French Space Agency have tracked a trail of minerals that point to the prior presence of water at the Curiosity rover site on Mars.

Researchers from the Mars Science Laboratory’s ChemCam team today described how the laser instrument aboard the Curiosity Rover—an SUV-sized vehicle studying the surface of the Red Planet—has detected veins of gypsum running through an area known as Yellowknife Bay, located some 700 meters away from where the Curiosity Rover landed five months ago.

“These veins are composed mainly of hydrated calcium sulfate, such as bassinite or gypsum,” said ChemCam team member Nicolas Mangold, of the Laboratoire de Planétologie et Géodynamique de Nantes, in Nantes, France. “On Earth, forming veins like these requires water circulating in fractures.”

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