Saturday, February 17, 2007

New Mars Pictures Show Signs of Watery "Aquifers"

Richard A. Lovett in San Francisco, California
for National Geographic News
February 16, 2007

Stunning color pictures from Mars offer new evidence that plentiful groundwater once percolated through Martian bedrock.

The new images, taken by NASA's Mars Reconnaissance Orbiter, reveal a terrain of banded rocks similar to that found in the southwestern U.S., said Chris Okubo, a postdoctoral researcher at the University of Arizona's Lunar and Planetary Laboratory.

The new pictures show that Martian rocks in this sandy landscape are riddled with small cracks.

These cracks bear telltale signs that fluid—probably water—seeped through them hundreds of millions of years ago.

Prominent riblike structures along the cracks, for instance, suggest that running water dissolved minerals in the Martian soil, forming a kind of cement.

The water also dissolved dark minerals out of the rocks, leaving light-colored "halos" around the cracks.

These findings are exciting, because they suggest that similar water-filled fractures might still exist beneath the Martian surface, scientists said.

"What we see at the surface today are glimpses of what used to be underground," Okubo said.

Okubo presented the new images at a press conference today in San Francisco, California. His team's findings will appear in tomorrow's issue of the journal Science.

Search for Life May Shift

Water is a key component of life as we know it, so the new discovery will be useful in helping scientists hone the search for possible life on Mars, researchers at the conference said.

There is already abundant evidence that early Mars was once water rich, said Stephen Clifford, a Mars hydrologist from the Lunar and Planetary Institute in Houston, Texas.

But the water has since retreated, presumably underground, and appears to have occasionally reached the surface in large floods.

(Read related story: "Mars's Water Could Be Below Surface, Experts Say" [January 25, 2007].)

Now that it is widely agreed that water once flowed along extensive networks of cracks, a new clue falls into place in a lingering mystery.

"One of the problems [was] how, if the water is underground, you get so much of it to the surface at once," Clifford said.

Other Ingredients of Life

Water appears to have been very common at various times on Mars's surface. So in the search for life it's now time to do more than seek out places where the red planet was once wet, said Tori Hoehler, an astrobiologist with NASA's Ames Research Center in Moffett Field, California.

Instead, scientists need to start thinking about other possible requirements for life, such as energy, Hoehler said.

For example, he said, microorganisms might be able to harness chemical energy from Martian rocks, as some earthly bacteria appear to do.

"This is the next thing we should be looking for on Mars," he said.

But expanding the search for life requires studying the geology in more detail, the scientists said.

NASA's Opportunity rover is currently on the rim of Victoria Crater, where scientists have observed outcrops of rock similar to that seen in Okubo's photos. (Related photos: Mars rovers).

"If we can get to [those outcrops]," Hoehler said, "it would be a great to visit them."

But, Okubo added, "right now, they're on the far side of the craters, so it may take a while for Opportunity to get there."

reposted from: NatGeorgraphic

my highlights / emphasis / comments




Stunning new images from a satellite orbiting Mars reveal that water once snuck along fractures in Mars's layered rocks.

The fractures are clearly visible in this view of Becquerel Crater, shooting through both the light- and dark-colored layers that make up the canyon's walls. The blue areas are vast sand dunes, not water.

Shot by the HiRISE (High Resolution Imaging Science Experiment) camera on the Mars Reconnaissance Orbiter, the image also reveals light-colored features, which scientists are calling halos, that cut across the dark bands. The researchers say these are areas where water flowing through the fractures has altered the appearance of rock.

Image courtesy Science

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