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The Carnegie Institution for Science reports "a much higher water content in the Moon’s interior than previous studies." For decades, the moon's water content was estimated at less than 1 part per billion; the new estimates range from 64 ppb to 5 parts per million. A scientist at Washington University said, "We can now finally begin to consider the implications—and the origin—of water in the interior of the Moon.”
There's more at
NASA and the
BBC, and the full paper is available at
PNAS (PDF).
posted by Stan Carey
on Jun 15, 2010 -
21 comments
On October 9th, NASA spacecraft will run into the moon, and on purpose. The
Lunar Crater Observation and Sensing Satellite (
LCROSS) and its rocket's
Centaur upper stage will impact the moon, with the goal of sending some of the (possibly present) ice above the lunar surface. Once out of the eternal shade of the moon's south pole, sunlight will break the ice up into H+ and OH- molecules, which can be detected by the
Lunar Reconnaissance Orbiter (
LRO). The
initial impact site was the crater Cabeus A, but the target was
later changed to Cabeus (proper), selected for highest hydrogen concentrations with the greatest level of certainty, and for the high-contrast back drop to detect ejecta and vapor measurements. NASA has provided
guides for amateur observations of the impact,
a facebook group, and
a Twitter feed so you don't miss the moment.
posted by filthy light thief
on Oct 8, 2009 -
53 comments
Future Moon Base Sited
the key points:
Shackleton crater (
best image)
a resource of hydrogen, likely in the form of water ice, ammonia, and other materials
at the Moon’s south pole and is some 30 kilometers in size
peak of external light - more or less continual Sun. solar energy becomes usable all the time. in the permanently shadowed areas in that region, various astronomical instruments could be operated with telescopic optics kept cold and stable
posted by Sean Meade
on Apr 11, 2001 -
15 comments
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