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Possible landing sites for future robotic craft based on Clementine data. Sites selected may allow early prospecting for water ice possibly hidden in permanently shadowed craters.Image: Courtesy Philip Stooke


Much of the area around the Moon's south pole is within the South Pole-Aitken Basin (shown at left in blue on a lunar topography image), a giant impact crater 1,550 miles (2,500 kilometers) in diameter and 7.5 miles (12 kilometers) deep at its lowest point. Many smaller craters exist on the floor of this basin. Many of those craters never see sunlight and are thought to contain water ice. Credit: NASA/National Space Science Data Center


Moon's south pole region is overseen by Malapert Mountain, now viewed as ideal spot to kickstart lunar utilization efforts. Credit: Naval Research Laboratory/U.S. Department of Defense
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Water on the Moon? Scientists Await Definitive Answer
By Rick Callahan
Associated Press
posted: 01:00 pm ET
12 November 2003

Untitled

 

INDIANAPOLIS (AP) -- The latest effort by science to answer whether there's ice on the moon has come up empty. There's no sign of a lunar skating rink in the mysterious polar craters -- or even a big slab of ice.

The results of the most detailed radar study to date of the moon's shadowy poles don't mean the moon is bone-dry. But the apparent lack of large ice tracts suggests there isn't a big supply of life-sustaining water nearby if people ever wanted to colonize the moon.

"It certainly would have been nice to find some sort of lunar skating rink, or thick layers of ice, but it looks like it's just not there," said Bruce Campbell of the Smithsonian Institution's Center for Earth and Planetary Studies.

Five years ago, NASA's Lunar Prospector orbiter found tantalizing evidence that deep, permanently shadowed craters at the moon's poles could harbor ice in their sunless depths.

Prospector found elevated levels of hydrogen -- a component of water -- around the moon's poles, with the highest readings in the perpetually shaded craters. But the evidence for ice was indirect.

Subsequent experiments that bounced radio waves off these craters revealed no sign of thick ice layers, although those tests penetrated only a few feet below the surface.

Now, Campbell and colleagues at Cornell University have used the mammoth radar dish at Puerto Rico's Arecibo Observatory to probe craters more deeply than ever before -- as far as 20 feet (6 meters) down.

And still there's no sign of thick layers of ice.

Campbell and colleagues at Cornell University say their findings support the idea that any ice in the moon's polar regions is in thin layers or widely scattered crystals mixed in with lunar soil.

The findings appear in Thursday's issue of the journal Nature.

If the moon's poles do have widely dispersed ice, Campbell said that means moon colonists would need equipment to either sort ice particles from the soil or heat up the crater floors and collect the water vapor.

Astronomers have suspected since at least the early 1960s that the moon's polar craters, miles-deep and surrounded by raised rims, could have trapped ice from comet impacts over billions of years.

Temperatures in some craters hover at about minus 280 degrees Fahrenheit (minus 173 Celsius), forming "cold traps" where water could collect even as it escaped into space over the rest of the moon.

Alan Binder, the director of the Lunar Research Institute in Tucson, Arizona, said the new results are consistent with the Lunar Prospector's findings suggesting widely scattered ice, perhaps a few hundred million metric tons of it.

But the only way to know for sure is to send a human or robot. "You've got to go down and stick your finger in it, so to speak," he said.

NASA has no lunar missions planned to address that question, but it is soliciting ideas for lunar spacecraft.

SPACE.com Editor's Note: The European Space Agency's SMART-1 spacecraft is en route to the Moon and is designed to search for firmer evidence of any possible water ice. Meanwhile, NASA recently asked for proposals for a lunar sample-return mission that would investigate the satellite's south polar region.

 

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