The Science of Sustainability

A Most Earthly Mineral on Mars

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This solid vein of white mineral near Endeavour crater, up to 2 centimeters thick, has every appearance of the well-known mineral gypsum. NASA/JPL-Caltech/Cornell/ASU image.

We have been studying Mars with spacecraft for almost 40 years now, starting with fly-bys and progressing to landers and then rovers. Each of these scientific missions has been more ambitious than the one before, and each has found more and more Earth-like features on Mars. The latest example was announced last month in San Francisco at the annual AGU meeting: Mars has veins of gypsum. I've seen gypsum veins myself, right here in California. And you can too.

The currently operating Mars rover is named Opportunity, and it has managed to roll across the pristine Martian ground for more than 33 kilometers since it landed in 2004. Nosing around the rampart of the crater Endeavour in a monotonous area of basalt rock, Opportunity came upon the vein of solid bone-white mineral shown above. It approached closer and turned its alpha particle X-ray spectrometer on the stuff, along with its close-up camera. The spectrometer indicated sulfur and calcium in the right proportions, and the camera images reminded NASA scientists of nothing but gypsum, hydrated calcium sulfate or CaSO4·2H2O.

Close-up of the Martian gypsum vein. NASA/JPL-Caltech/Cornell/ASU image.

All right, so what? Well, gypsum points directly and unmistakably to liquid water, something that we've been looking for on Mars but never quite proving. There is gypsum-like dust blowing around parts of Mars, like it does at White Sands in New Mexico, but no sign of its origin. The mission's chief scientist, Steve Squyres, said at the AGU press conference, "This stuff was formed right here. There was a fracture in the rock, water flowed through it, gypsum was precipitated from the water. End of story. Okay, there is no ambiguity about this. This is what makes it so cool. . . . Here the chemistry and mineralogy of it just scream of water."

On Earth, gypsum is found in two main settings: wherever seawater begins to dry up, gypsum comes out of solution first and can accumulate in thick beds. And wherever hot-spring type fluids concentrate dissolved matter, gypsum is a likely mineral. The Martian vein appears to be of the latter, hydrothermal type. California's Central Valley, for much of recent geologic time, has been the former type of setting—a shallow sea basin or brackish lake.

Gypsum is especially abundant in the Kettleman Hills, an area of former Central Valley seabed that has been gently lifted by recent tectonic activity. If you have an extra hour next time you're on Interstate 5 going to Los Angeles, turn off at 25th Avenue, south of Kettleman City, and pull over once you enter the hills. Gypsum litters the ground there, and farther south near Lost Hills gypsum is being mined to make drywall, soil additives and plaster of Paris.

Gypsum of the Kettleman Hills. Photo by Andrew Alden.

If you're there in nice weather, enjoy the scene and think of Mars. Maybe you'll share the tantalizing feeling that the discovery of Martian gypsum arouses in geologists despite their best mental effort.

Kettleman Hills, 26 May 2010. Photo by Andrew Alden.

Endeavour crater, Mars, 6 August 2011. NASA/JPL-Caltech/Cornell/ASU image.

Like one of those 1950s-vintage Cuban taxis, Opportunity has hung on far longer than people originally planned. Planetary space missions have a fairly short "prime mission" of a few months or maybe a year, but everyone knows without admitting it that the rugged, overdesigned machinery will last a lot longer. NASA makes a big deal out of extending the mission, a year or so at a time, and we all feel good about getting our money's worth. In the case of Opportunity, its prime mission began eight years ago and the solar-powered contraption is still plugging along. Imagine what its successor, the rover Curiosity, might do once it lands in Gale crater in August of this year.

Read more about the discovery from NASA.

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Category: Astronomy, Geology

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Andrew Alden

About the Author ()

Andrew Alden earned his geology degree at the University of New Hampshire and moved back to the Bay Area to work at the U.S. Geological Survey for six years. He has written on geology for About.com since its founding in 1997. In 2007, he started the Oakland Geology blog, which won recognition as "Best of the East Bay" from the East Bay Express in 2010. In writing about geology in the Bay Area and surroundings, he hopes to share some of the useful and pleasurable insights that geologists give us—not just facts about the deep past, but an attitude that might be called the deep present. Read his previous contributions to QUEST, a project dedicated to exploring the Science of Sustainability.
  • Torbjörn Larsson

    Yes, it is inspiring. But Curiosity can't do much more time, if that. Its nuclear MMRTG has a maximum lifetime of 14 years since assembly, and it has aged 2 years due to the launch delay. (Unfortunately the isotope core was assembled according to the old launch schedule.)

    Remove another year for transit and we can expect 9 years life.

    When I checked on this earlier for a comment on another blog though, I uncovered that the launch preparations had protocoled undue aging risks because the MMRTG is a new construction. The landing shocks can worsen the package output to 5 years lifetime if we are unlucky. To play it safe they have scaled down on the nominal mission requirements even. :-/

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