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Rabu, 07 September 2011

LRO Showing Us the Moon as Never Before



NASA's Lunar Reconnaissance Orbiter (LRO) has forever changed our view of the moon, literally bringing it into sharper focus and showing us the whole globe in unprecedented detail.

This rich new portrait has been rendered by LRO's seven onboard instruments, which together have delivered more than 192 terabytes of data, images and maps -- the equivalent of nearly 41,000 typical DVDs. "This is a tremendous accomplishment," says Douglas Cooke, Associate Administrator of the Exploration Systems Mission Directorate at NASA Headquarters, Washington. "The exploration phase of the mission delivered a lot more than it originally promised, and that's been just the beginning for LRO."

The primary objective of the mission was to enable safe and effective exploration of the moon. "To do so, we needed to leverage the very best that the science community had to offer," says Michael Wargo, chief lunar scientist of the Exploration Systems Mission Directorate at NASA Headquarters, Washington. "And by doing that, we've fundamentally changed our scientific understanding of the moon."

The most precise and complete topographic maps to date of the moon's complex, heavily cratered landscape have been created from the more than 4 billion measurements -- and still counting -- taken by LRO's Lunar Orbiter Laser Altimeter (LOLA). These maps are more accurate and sample more places on the lunar surface than any available before. In fact, LOLA has taken more than 100 times more measurements than all previous lunar instruments of its kind combined, opening up a world of possibilities for future exploration and for science.

Already, researchers have used LOLA data to put together the first comprehensive set of maps of the roughness of the moon's surface. Like wrinkles on skin, the roughness of craters and other features on the moon's surface can reveal their age. By looking at where and how the roughness changes -- and by combining that information with contour maps that show where the high and low points are -- researchers can get important clues about the processes that shaped the moon.

"Before LRO, we actually knew the shape of Mars better than we knew the shape of the moon, our nearest neighbor," notes LRO's Deputy Project Scientist, John Keller of NASA's Goddard Space Flight Center in Greenbelt, Md. "But because of LRO and LOLA, we now have detailed maps of both the near side and far side of the moon."

Though less familiar than the instantly recognizable near side, the moon's far side is no less fascinating. The far side is rougher and houses more craters, including one of the biggest impact basins in the solar system, called South Pole-Aitken. This remnant of an ancient and immensely powerful impact left such a profound crater that 34 Empire State Buildings stacked on top of each other still would not reach from its depths to its rim.

"With the wealth of data from LRO freely available, everyone can get to know the far side of the moon just as well as the near side," says Wargo.



A World of Resources

LRO's search for resources has revealed that the moon is even more extreme than we thought.

In the polar regions, deep and long-shaded craters, such as Shackleton crater in the south, have been of special interest because they can act as cold storage, capable of accumulating and preserving volatile material like water ice. But it was while studying Hermite crater near the moon's north pole that the mission's Diviner Lunar Radiometer Experiment found the coldest spot in solar system, with a temperature of -415 degrees Fahrenheit (-248 degrees Celsius or 25 Kelvins).

To further explore these regions, LRO's Lyman Alpha Mapping Project (LAMP), which can "see" in the dark, is imaging the shaded areas. Already, LOLA's precise measurements have been used to map solar illumination; this work has provided new insight into the shadowed regions and also revealed areas that receive nearly continuous sun. Because sunlight itself is a resource on the moon, knowing that there are areas that get sun for approximately 243 days a year and never have a period of total darkness for more than 24 hours is extremely valuable.

Complementing those efforts are both the Lunar Exploration Neutron Detector (LEND) and the Miniature Radio Frequency (Mini-RF) advanced radar. They are searching for deposits of water ice. LEND also seeks hydrogen, a resource of interest because of its potential use as fuel. And at the same time, the Cosmic Ray Telescope for the Effects of Radiation (CRaTER) studies the lunar radiation environment, which is important for keeping our astronauts healthy and safe as they explore.

A Picnic on the Moon

Stunning details of the moon's surface have been revealed by the Lunar Reconnaissance Orbiter Camera (LROC), which imaged nearly 5.7 million square kilometers of the moon's surface during the exploration phase of the mission. That is roughly the same amount of land as all contiguous states west of the Mississippi River.

Though earlier missions also imaged the moon, what sets LROC apart is its ability to image with surface pixels that are only 1.5 feet in size, small enough to distinguish details never before possible.

"With this resolution, LRO could easily spot a picnic table on the moon," says LRO's Project Scientist, Richard Vondrak of NASA Goddard.

And thanks to some operational efficiencies, the dual Narrow Angle Cameras that are part of LROC have delivered 50 percent more images than initially expected.

LRO was charged with surveying specific sites but with the added goal of making measurements globally across the moon. "LRO is designed to look down all the time, and most of the instruments are collecting data all the time," Wargo explains. "This, along with LRO's performance and reliability, has given us a more comprehensive view of the moon than ever before."

And there's plenty more to come from LRO. "Not only did we accomplish all of this during the exploration phase of the mission," says Vondrak, "but two more years of wonderful science are already under way."

LRO launched aboard an Atlas V rocket from Cape Canaveral, Fla., on June 18, 2009. LRO was built and is managed by NASA's Goddard Space Flight Center, Greenbelt, Md. The exploration phase was funded by NASA's Exploration Systems Missions Directorate in Washington, D.C. LRO operates under NASA's Science Mission Directorate. Elizabeth Zubritzky
NASA's Goddard Space Flight Center, Greenbelt, Md.

Sabtu, 30 Juli 2011

Rare Volcanoes Discovered on 'Dark Side' of the Moon !!!









Shielded from Earth-bound eyes, the far side of the moon is home to a rare set of dormant volcanoes that changed the face of the lunar surface, a new study finds.
Data and photos from NASA's Lunar Reconnaissance Orbiter (LRO) reveal the presence of now-dead silicate volcanoes, not the more common basaltic volcanoes that litter the moon's surface, researchers said.
"Most of the volcanic activity on the moon was basaltic," primary author Brad Jolliff of Washington University told SPACE.com in an email. "Finding other volcanic types is interesting as it shows the geologic complexity and range of processes that operate on the moon, and how the moon's volcanism changed with time." [Photos of the dormant far side moon volcanoes]
Searching the far side
Because the moon's rotation has been affected by tidal forces between the Earth and the moon, only one side of the moon is visible from the Earth. The far side of the moon — sometimes referred to inaccurately as the "dark side" — was hidden from view until 1959, when Soviet Union's Luna 3 spacecraft took the first photos of the region.
When NASA's Lunar Prospector probe circled the moon in 1998, it revealed a highly reflective plain lying between two ancient impact craters. Known as the Compton-Belkovich region, this part of the moon contains thorium and other silicate rocks, suggesting a more involved type of volcanic activity than that which created the moon's well-known dark plains of basaltic plains known as "maria," or "seas."
But it wasn't until the LRO captured higher-resolution images for the region could this volcanic activity be confirmed. The spacecraft found a number of domelike features with steeply sloping sides — telltale signs of lunar volcanoes.
Jolliff said that the domes likely formed by lava probably came from deep within the moon. It flowed upward through cracks to pool just beneath the surface, where it pressed out to form large domes.
Lava continued to work its way to the surface throughout the area, building other, smaller volcanic domes. Some areas then collapsed, creating the irregular depressions observed by LRO's camera, researchers said.
The research is detailed in the July 24 edition of the journal Nature Geoscience.
Rare volcanoes on the moon
Most volcanoes, on Earth and off, are near other volcanoes. But the grouping in the Compton-Belkovich region is isolated.
"This small volcanic complex occurs far away from the part of the moon where most of the volcanic activity was concentrated, and where other silicic volcanism occurred," Jolliff said. "That's a puzzle." [10 Coolest Moon Discoveries]


Read more: http://www.foxnews.com/scitech/2011/07/26/rare-volcanoes-discovered-on-far-side-moon/#ixzz1TdTRhzS8