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Friday, September 28, 2012

Mars Rover Opportunity Working at 'Matijevic Hill'

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov

News release: 2012-306 Sept. 28, 2012

Mars Rover Opportunity Working at 'Matijevic Hill'

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-306&cid=release_2012-306

PASADENA, Calif. -- NASA's Mars rover Opportunity, well into its ninth year on Mars, will work for the next several weeks or months at a site with some of the mission's most intriguing geological features.

The site, called "Matijevic Hill," overlooks 14-mile-wide (22-kilometer-wide) Endeavour Crater. Opportunity has begun investigating the site's concentration of small spherical objects reminiscent of, but different from, the iron-rich spheres nicknamed "blueberries" at the rover's landing site nearly 22 driving miles ago (35 kilometers).

The small spheres at Matijevic Hill have different composition and internal structure. Opportunity's science team is evaluating a range of possibilities for how they formed. The spheres are up to about an eighth of an inch (3 millimeters) in diameter.

The "blueberries" found earlier are concretions formed by the action of mineral-laden water inside rocks, but that is only one of the ways nature can make small, rounded particles. One working hypothesis, out of several, is that the new-found spherules are also concretions but with a different composition. Others include that they may be accretionary lapilli formed in volcanic ash eruptions, impact spherules formed in impact events, or devitrification spherules resulting from formation of crystals from formerly melted material. There are other possibilities, too.

"Right now we have multiple working hypotheses, and each hypothesis makes certain predictions about things like what the spherules are made of and how they are distributed," said Opportunity's principal investigator, Steve Squyres, of Cornell University, Ithaca, N.Y. "Our job as we explore Matijevic Hill in the months ahead will be to make the observations that will let us test all the hypotheses carefully, and find the one that best fits the observations."

The team chose to refer to this important site as Matijevic Hill in honor of Jacob Matijevic (1947-2012), who led the engineering team for the twin Mars Exploration Rovers Spirit and Opportunity for several years before and after their landings. He worked at NASA's Jet Propulsion Laboratory, Pasadena, Calif., from 1981 until his death last month, most recently as chief engineer for surface operations systems of NASA's third-generation Mars rover, Curiosity. In the 1990s, he led the engineering team for the first Mars rover, Sojourner.

A different Mars rover team, operating Curiosity, has also named a feature for Matijevic: a rock that Curiosity recently investigated about halfway around the planet from Matijevic Hill.

"We wouldn't have gotten to Matijevic Hill, eight-and-a-half years after Opportunity's landing, without Jake Matijevic," Squyres said.

Opportunity's project manager, John Callas, of JPL, said, "If there is one person who represents the heart and soul of all three generations of Mars rovers -- Sojourner, Spirit and Opportunity, Curiosity -- it was Jake."

JPL, a division of the California Institute of Technology in Pasadena, manages the Mars Exploration Rover Project for NASA's Science Mission Directorate in Washington. For more information about Opportunity, visit: http://www.nasa.gov/rovers and http://marsrovers.jpl.nasa.gov .

You can follow the project on Twitter and on Facebook at: http://twitter.com/MarsRovers and http://www.facebook.com/mars.rovers .

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Thursday, September 27, 2012

NASA Rover Finds Old Streambed on Martian Surface

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster / D.C. Agle 818-354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov / agle@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

News release: 2012-305 Sept. 27, 2012

NASA Rover Finds Old Streambed on Martian Surface

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-305&cid=release_2012-305

PASADENA, Calif. -- NASA's Curiosity rover mission has found evidence a stream once ran vigorously across the area on Mars where the rover is driving. There is earlier evidence for the presence of water on Mars, but this evidence -- images of rocks containing ancient streambed gravels -- is the first of its kind.

Scientists are studying the images of stones cemented into a layer of conglomerate rock. The sizes and shapes of stones offer clues to the speed and distance of a long-ago stream's flow.

"From the size of gravels it carried, we can interpret the water was moving about 3 feet per second, with a depth somewhere between ankle and hip deep," said Curiosity science co-investigator William Dietrich of the University of California, Berkeley. "Plenty of papers have been written about channels on Mars with many different hypotheses about the flows in them. This is the first time we're actually seeing water-transported gravel on Mars. This is a transition from speculation about the size of streambed material to direct observation of it."  

The finding site lies between the north rim of Gale Crater and the base of Mount Sharp, a mountain inside the crater. Earlier imaging of the region from Mars orbit allows for additional interpretation of the gravel-bearing conglomerate. The imagery shows an alluvial fan of material washed down from the rim, streaked by many apparent channels, sitting uphill of the new finds.

The rounded shape of some stones in the conglomerate indicates long-distance transport from above the rim, where a channel named Peace Vallis feeds into the alluvial fan. The abundance of channels in the fan between the rim and conglomerate suggests flows continued or repeated over a long time, not just once or for a few years.

The discovery comes from examining two outcrops, called "Hottah" and "Link," with the telephoto capability of Curiosity's mast camera during the first 40 days after landing. Those observations followed up on earlier hints from another outcrop, which was exposed by thruster exhaust as Curiosity, the Mars Science Laboratory Project's rover, touched down.

"Hottah looks like someone jack-hammered up a slab of city sidewalk, but it's really a tilted block of an ancient streambed," said Mars Science Laboratory Project Scientist John Grotzinger of the California Institute of Technology in Pasadena.

The gravels in conglomerates at both outcrops range in size from a grain of sand to a golf ball. Some are angular, but many are rounded.

"The shapes tell you they were transported and the sizes tell you they couldn't be transported by wind. They were transported by water flow," said Curiosity science co-investigator Rebecca Williams of the Planetary Science Institute in Tucson, Ariz.

The science team may use Curiosity to learn the elemental composition of the material, which holds the conglomerate together, revealing more characteristics of the wet environment that formed these deposits. The stones in the conglomerate provide a sampling from above the crater rim, so the team may also examine several of them to learn about broader regional geology.

The slope of Mount Sharp in Gale Crater remains the rover's main destination. Clay and sulfate minerals detected there from orbit can be good preservers of carbon-based organic chemicals that are potential ingredients for life.

"A long-flowing stream can be a habitable environment," said Grotzinger. "It is not our top choice as an environment for preservation of organics, though. We're still going to Mount Sharp, but this is insurance that we have already found our first potentially habitable environment."

During the two-year prime mission of the Mars Science Laboratory, researchers will use Curiosity's 10 instruments to investigate whether areas in Gale Crater have ever offered environmental conditions favorable for microbial life.

NASA's Jet Propulsion Laboratory, a division of Caltech, built Curiosity and manages the Mars Science Laboratory Project for NASA's Science Mission Directorate, Washington.

For more about Curiosity, visit: http://www.jpl.nasa.gov/msl , http://www.nasa.gov/msl and http://mars.jpl.nasa.gov/msl .

You can follow the mission on Facebook and Twitter at: http://www.facebook.com/marscuriosity and http://www.twitter.com/marscuriosity .

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Wednesday, September 26, 2012

NASA to Televise Mars Curiosity Rover Science Update Sept. 27

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

DC Agle / Guy Webster 818-354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
agle@jpl.nasa.gov / guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
Dwayne.c.brown@nasa.gov

Advisory: 2012-302 Sept. 26, 2012

NASA to Televise Mars Curiosity Rover Science Update Sept. 27

PASADENA, Calif. -- NASA will host a news conference at 11 a.m. PDT (2 p.m. EDT) Thursday, Sept. 27, to present science findings from the Curiosity rover's mission to Mars' Gale Crater. The news conference from NASA's Jet Propulsion Laboratory (JPL) in Pasadena, Calif., will be carried live on NASA Television, the agency's website and on Ustream.

Curiosity, also known as the Mars Science Laboratory, is 50 days into a two-year mission to investigate whether conditions may have been favorable for microbial life.

For NASA TV downlink information, schedules and links to streaming video, visit: http://www.nasa.gov/ntv .

To watch on Ustream, go to: http://ustream.tv/nasajpl .

For information about NASA's Curiosity mission, visit: http://www.nasa.gov/mars and http://mars.jpl.nasa.gov/msl .

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Monday, September 24, 2012

Curiosity Finishes Close Inspection of Rock Target

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster / D.C. Agle 818-354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
Guy.Webster@jpl.nasa.gov / Agle@jpl.nasa.gov

News feature: 2012-300 Sept. 24, 2012

Curiosity Finishes Close Inspection of Rock Target

Mars Science Laboratory Mission Status Report

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-300&cid=release_2012-300

PASADENA, Calif. -- NASA's rover Curiosity touched a Martian rock with its robotic arm for the first time on Sept. 22, assessing what chemical elements are in the rock called "Jake Matijevic."

After a short drive the preceding day to get within arm's reach of the football-size rock, Curiosity put its Alpha Particle X-Ray Spectrometer (APXS) instrument in contact with the rock during the rover's 46th Martian day, or sol. The APXS is on a turret at the end of the rover's 7-foot (2.1-meter) arm. The Mars Hand Lens Imager (MAHLI), on the same turret, was used for close-up inspection of the rock. Both instruments were also used on Jake Matijevic on Sol 47 (Sept. 23).

The Chemistry and Camera (ChemCam) instrument, which shoots laser pulses at a target from the top of Curiosity's mast, also assessed what chemical elements are in the rock Jake Matijevic. Using both APXS and ChemCam on this rock provides a cross calibration of the two instruments.

With a final ChemCam laser testing of the rock on Sol 48 (Sept. 24), Curiosity finished its work on Jake Matijevic. The rover departed the same sol, with a drive of about 138 feet (42 meters), its longest yet. Sol 48, in Mars local mean solar time at Gale Crater, ended at 3:09 p.m. Sept. 24, PDT.

Curiosity landed on Mars seven weeks ago to begin a two-year mission using 10 instruments to assess whether a carefully chosen study area inside Gale Crater has ever offered environmental conditions favorable for microbial life.

JPL, a division of the California Institute of Technology, Pasadena, manages the Mars Science Laboratory Project, including Curiosity, for NASA's Science Mission Directorate, Washington. JPL designed and built the rover. The Space Division of MDA Information Systems Inc. built the robotic arm in Pasadena.

More information about Curiosity is online at http://www.nasa.gov/msl and http://mars.jpl.nasa.gov/msl/ . You can follow the mission on Facebook at: http://www.facebook.com/marscuriosity and on Twitter at: http://www.twitter.com/marscuriosity .

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Thursday, September 20, 2012

Shuttle Endeavour Flyby to Bring an Old Friend to JPL

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Alan Buis 818-354-0474
Jet Propulsion Laboratory, Pasadena, Calif.
Alan.buis@jpl.nasa.gov

News feature: 2012-299 Sept. 20, 2012

Shuttle Endeavour Flyby to Bring an Old Friend to JPL

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-299&cid=release_2012-299

It flew some of the most iconic payloads in the space shuttle program history, including "The Camera
That Saved Hubble" and "The Mission That Mapped the World," both proudly developed by NASA's
Jet Propulsion Laboratory in Pasadena, Calif. Now the spaceship dubbed "America's Best Ever, Space
Shuttle Endeavour" by the Rockwell International technicians, who lovingly assembled and tested her
in California's high desert more than two decades ago, is coming home to roost in Southern California
for a final time this week. The shuttle is set to begin a new life in retirement on permanent display at
the California Science Center in Los Angeles. But before Endeavour makes her final "wheel stop" at
Los Angeles International Airport this Friday, Sept. 21, she'll be paying an aerial house call on some
of her old friends, including JPL.

Weather and operational constraints permitting, Southern Californians will be watching the skies
beginning at 11:30 a.m PDT on Friday, as Endeavour makes low-altitude flyovers in the Los Angeles
area. In addition to JPL, Endeavour is scheduled to pass over such regional landmarks as its future
home at the California Science Center, Columbia Memorial Space Center in Downey, Disneyland,
The Getty Center, Griffith Observatory, Los Angeles City Hall, the Long Beach Aquarium of the
Pacific, Malibu Beach, the Queen Mary, Universal Studios and Venice Beach, among others.

Endeavour holds a special place in the hearts of many at JPL. After all, this is the shuttle orbiter that
JPLers have had the most interaction with over the years. The lab played key roles in several of
Endeavour's 25 space missions. Among them, JPL built the Wide Field and Planetary Camera 2
(WFPC-2) for the first Hubble Space Telescope Servicing Mission in 1993, the Spaceborne Imaging
Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) payload that flew twice in 1994, the
Inflatable Antenna Experiment (IAE) and Brilliant Eyes Ten-kelvin Sorption Cryocooler Experiment
(BETSCE) in 1996, the Shuttle Radar Topography Mission (SRTM) in 2000 and the Electronic Nose
(ENose) instrument in 2008, among other payloads.

Nicknamed "The Camera That Saved Hubble," WFPC-2 was designed to correct the spherical
aberration of the Hubble Space Telescope's main mirror, discovered after its launch in 1990. It
became the telescope's workhorse camera for nearly 16 years, obtaining 135,000 observations of the
universe.

"WFPC-2 was the instrument that corrected Hubble's vision and restored wide field imaging to the
Hubble," said John Trauger, WFPC-2 principal investigator at JPL. "It was a huge relief. We knew
this was the beginning and not an end; that Hubble's science program could now kick into high gear."

While WFPC-2 gave us new eyes to the universe, another JPL-developed payload allowed us to see
our own world in 3-D for the first time. The Shuttle Radar Topography Mission (SRTM) flew aboard
Endeavour in 2000. Its 11-day mission made the first near-global, high-resolution topographical map
of Earth, collecting data on nearly 80 percent of Earth's land surfaces. SRTM revealed for the first
time large, detailed swaths of Earth's topography previously obscured by persistent cloudiness. The
data benefit scientists, engineers, government agencies and the public alike, with applications that
range from land-use planning to virtual Earth exploration.

"SRTM was among the most significant science missions the shuttle ever performed," said Michael
Kobrick, SRTM mission project scientist at JPL. "It's probably the most significant mapping mission
of any single type ever."

SRTM used an improved version of a radar instrument that comprised the Spaceborne Imaging
Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR), which flew twice on Endeavour in 1994
as the Space Radar Laboratory-1 and -2 missions. The JPL-built SIR-C was coupled with the
German-built X-SAR to image Earth in three different wavelengths. These synthetic aperture radar
were used to study how Earth's global environment is changing, and collected data on terrestrial soil
moisture content, ocean dynamics, volcanism and tectonic activity, as well as soil erosion and
desertification.

"Both SIR-C/X-SAR flights succeeded in acquiring 100 percent of the planned science data," said
Diane Evans, SIR-C project scientist at JPL and now director of JPL's Earth Science & Technology
Directorate. "In addition, mission planners were able to redirect the radars during each flight to take
advantage of rapidly changing conditions on the ground." These included flooding, tropical cyclones
and a volcanic eruption -- in fact, SIR-C/X-SAR data provided the most detailed documentation of a
volcanic eruption ever obtained from orbit up to that time.

Another JPL-developed Endeavour payload was the Inflatable Antenna Experiment (IAE), which
flew in 1996. Built by LaGarde, Tustin, Calif., and managed by JPL, it was mounted on the Spartan-
207 satellite and was the first demonstration of inflatable reflector antenna technology in space. It
deployed a 46-foot- (14-meter) diameter, 98-foot- (30-meter) long mylar inflatable antenna from a
small container the size of a coffee table.

"Bigger than a tennis court, IAE was the largest structure ever erected in space at that time, surpassed
only by SRTM in 2000," said Steven Bard, the IAE project manager at JPL and now manager of
JPL's Earth Science Flight Projects Office. "It was so large that it was actually visible from the
ground by the naked eye as it orbited Earth. I remember how we all ran outside from Mission Control
in Houston and looked up in the sky to see the magnificent sight of the Endeavour, trailed by the IAE,
as they both flew overhead."

Also launched in 1996 on Endeavour was the JPL-developed Brilliant Eyes Ten-kelvin Sorption
Cryocooler Experiment (BETSCE). BETSCE produced small, solid-hydrogen ice cubes at 10 Kelvin
(minus 442 degrees Fahrenheit). The BETSCE cooler pioneered the use of this novel, vibration-free,
refrigeration technology in the microgravity space environment, and enabled its use on future
astrophysics and Earth observation missions. A key accomplishment of the successful BETSCE
demonstration is that it led to JPL's development of two sorption coolers that are currently cooling the
highly-sensitive infrared sensors on the European Space Agency's flagship astrophysics mission,
Planck, which is seeking answers to many fundamental questions about the early history and
evolution of our universe.

"The BETSCE was a prime example of the benefits of the shuttle program as a unique test bed for
demonstrating new technologies in space before you risk flying them on expensive missions," said
Bard, who was the principal investigator and project manager for BETSCE.

The JPL-developed Electronic Nose (ENose), which flew aboard Endeavour in 2008, was an air
quality and event monitor designed to assess the breathing air in a crewed space habitat for dangerous
chemicals that could harm astronaut health. It was installed on the International Space Station. The
ENose can provide early identification and quantification of changes in the atmosphere caused by
leaks or spills of analytes (chemical substances that are the subject of chemical analyses), including
mercury, ammonia, sulfur dioxide, ethanol and benzene.

"The JPL ENose operated continually as a technology demonstration on the International Space
Station for seven months," said JPL senior engineer Margie Homer, the ENose co-investigator.
"While on board, the ENose detected several events of interest, including perfluoropropane and
ethanol. After a successful demonstration, the ENose returned to Earth on space shuttle Discovery."

In addition to the JPL-developed payloads Endeavour took to space, two astronauts who had formerly
worked at JPL flew aboard Endeavour: Jay Apt and Andrew Thomas. Many other JPL employees had
worked on Endeavour in some capacity over the years before coming to JPL.

The Los Angeles-area flyovers mark the final leg of Endeavour's cross-country ferry flight from
NASA's Kennedy Space Center in Florida to Los Angeles International Airport. Endeavour departed
Kennedy on Wed., Sept. 19, mounted atop NASA's modified Shuttle Carrier Aircraft. Following low-
level flyovers of several locations, Endeavour arrived at Ellington Field in Houston, near NASA's
Johnson Space Center, where it spent the night. After departing Houston on Thursday, Sept. 20,
Endeavour made a refueling stop at Biggs Army Airfield in El Paso, Texas, then traveled to NASA's
Dryden Flight Research Center on Edwards Air Force Base, Calif., Thursday afternoon for an
overnight stay.

The final leg of the ferry flight from NASA Dryden on Friday morning, Sept. 21 will include low-
level flyovers of the Lancaster-Palmdale area and several Northern California locations before
concluding with the Los Angeles-area flyovers, including JPL, and a landing at Los Angeles
International Airport around 12:45 p.m. PDT.

After arrival at LAX, Endeavour will be removed from the Shuttle Carrier Aircraft and spend a few
weeks at a United Airlines hangar undergoing preparations for transport and display. Endeavour then
will travel through Inglewood and Los Angeles city streets on a 12-mile journey from the airport to
its new permanent home, the California Science Center in Los Angeles, where it is scheduled to
arrive the evening of Oct. 13.

Beginning Oct. 30, the shuttle will be on display in the science center's Samuel Oschin Space Shuttle
Endeavour Display Pavilion, embarking on its new mission to commemorate past achievements in
space and educate and inspire future generations of explorers.

Endeavour was the final space shuttle built, and was constructed from orbiter vehicle structural spare
parts as a replacement for space shuttle Challenger. It completed 25 missions between 1992 and 2011,
spending 299 days in orbit and orbiting Earth 4,671 times while traveling 122,883,151 miles. It was
named after the British sailing ship HMS Endeavour, which Captain James Cook sailed on his first
voyage of discovery.

Social media users are encouraged to share their Endeavour sightings using the hashtags
#spottheshuttle and #OV105, Endeavour's orbiter vehicle designation.

In addition to Endeavour, a number of other prominent JPL missions flew on other space shuttle
orbiters. These included the Shuttle Imaging Radar-A aboard space shuttle Columbia in 1981 and
Shuttle Imaging Radar-B aboard space shuttle Challenger in 1984; Galileo orbital mission to Jupiter,
launched from space shuttle Atlantis in 1989; Magellan orbital mission to Venus, launched from
space shuttle Atlantis in 1989; Ulysses mission to study the sun, launched from space shuttle
Discovery in 1990; the Hubble Space Telescope's Wide Field and Planetary Camera 1, launched
aboard space shuttle Discovery in 1990; ACRIM2 instrument on the Upper Atmosphere Research
Satellite, launched aboard space shuttle Discovery in 1991; Drop Dynamics Module, launched by
space shuttle Challenger in 1985; Lambda Point Experiment, launched aboard space shuttle Columbia
in 1992; and numerous additional shuttle payloads that flew aboard various space shuttles between
1981 and 1998. Other shuttle astronauts who previously worked for JPL include Stanley Love, John
Olivas, Engene Trinh, Taylor Wang and Stephanie Wilson.

For more on WFPC-2, visit: http://www.jpl.nasa.gov/missions/details.php?id=5931 and
http://www.jpl.nasa.gov/news/news.php?feature=2144 . For more on SRTM, visit:
http://www2.jpl.nasa.gov/srtm/ . For more on SIR-C/X-SAR, visit:
http://www.jpl.nasa.gov/missions/details.php?id=5975 . For more on BETSCE, visit:
http://www2.jpl.nasa.gov/adv_tech/thermal/ThrSysEng.htm . For more on ENose, visit:
http://enose.jpl.nasa.gov/ .

The California Institute of Technology in Pasadena manages JPL for NASA.

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Dawn Sees Hydrated Minerals on Giant Asteroid

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Jia-Rui C. Cook 818-354-0850
Jet Propulsion Laboratory, Pasadena, Calif.
jccook@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

News release: 2012-297 Sept. 20, 2012

Dawn Sees Hydrated Minerals on Giant Asteroid

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-297&cid=release_2012-297

PASADENA, Calif. – NASA's Dawn spacecraft has revealed that the giant asteroid Vesta has its own
version of ring around the collar. Two new papers based on observations from the low-altitude
mapping orbit of the Dawn mission show that volatile, or easily evaporated materials, have colored
Vesta's surface in a broad swath around its equator.

Pothole-like features mark some of the asteroid's surface where the volatiles, likely water, released
from hydrated minerals boiled off. While Dawn did not find actual water ice at Vesta, there are signs
of hydrated minerals delivered by meteorites and dust evident in the giant asteroid's chemistry and
geology. The findings appear today in the journal Science.

One paper, led by Thomas Prettyman, the lead scientist for Dawn's gamma ray and neutron detector (GRaND) at the Planetary Science Institute in Tucson, Ariz., describes how the instrument found signatures of hydrogen, likely in the form of hydroxyl or water bound to minerals in Vesta's surface.

"The source of the hydrogen within Vesta's surface appears to be hydrated minerals delivered by
carbon-rich space rocks that collided with Vesta at speeds slow enough to preserve their volatile
content," said Prettyman.

A complementary paper, led by Brett Denevi, a Dawn participating scientist based at the Johns
Hopkins University Applied Physics Laboratory in Laurel, Md., describes the presence of pitted
terrain created by the release of the volatiles.

Vesta is the second most massive member of the main asteroid belt. The orbit at which these data
were obtained averaged about 130 miles (210 kilometers) above the surface. Dawn left Vesta earlier
this month, on Sept. 4 PDT (Sept. 5 EDT), and is now on its way to its second target, the dwarf planet
Ceres.

Scientists thought it might be possible for water ice to survive near the surface around the giant
asteroid's poles. Unlike Earth's moon, however, Vesta has no permanently shadowed polar regions
where ice might survive. The strongest signature for hydrogen in the latest data came from regions
near the equator, where water ice is not stable.

In some cases, other space rocks crashed into these deposits later at high speed. The heat from the
collisions converted the hydrogen bound to the minerals into water, which evaporated. The holes that
were left as the water escaped stretch as much as 0.6 miles (1 kilometer) across and go down as deep
as 700 feet (200 meters). Seen in images from Dawn's framing camera, this pitted terrain is best
preserved in sections of Marcia crater.

"The pits look just like features seen on Mars, but while water was common on Mars, it was totally
unexpected on Vesta in these high abundances," said Denevi. "These results provide evidence that not
only were hydrated materials present, but they played an important role in shaping the asteroid's
geology and the surface we see today."

GRaND's data are the first direct measurements describing the elemental composition of Vesta's
surface. Dawn's elemental investigation by the instrument determined the ratios of iron to oxygen and
iron to silicon in the surface materials. The new findings solidly confirm the connection between
Vesta and a class of meteorites found on Earth called the Howardite, Eucrite and Diogenite
meteorites, which have the same ratios for these elements. In addition, more volatile-rich fragments
of other objects have been identified in these meteorites, which supports the idea that the volatile-rich
material was deposited on Vesta.

The Dawn mission is managed by the Jet Propulsion Laboratory for NASA's Science Mission
Directorate, Washington. It is a project of the Discovery Program managed by NASA's Marshall
Space Flight Center, Huntsville, Ala. UCLA is responsible for overall mission science. Orbital
Sciences Corporation of Dulles, Va., designed and built the Dawn spacecraft.

The framing cameras were developed and built under the leadership of the Max Planck Institute for
Solar System Research, Katlenburg-Lindau, Germany, with contributions by the German Aerospace
Center (DLR) Institute of Planetary Research, Berlin, and in coordination with the Institute of
Computer and Communication Network Engineering, Braunschweig. The framing camera project is
funded by the Max Planck Society, DLR and NASA. The gamma ray and neutron detector instrument
was built by Los Alamos National Laboratory, N.M., and is operated by the Planetary Science
Institute, Tucson, Ariz.

JPL is a division of the California Institute of Technology, Pasadena.

To view new images and for more information about Dawn, visit: http://www.nasa.gov/dawn and
http://dawn.jpl.nasa.gov .

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Quakesim and NASA Mobile App Win NASA Software Award

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Alan Buis 818-354-0474
Jet Propulsion Laboratory, Pasadena, Calif.
Alan.buis@jpl.nasa.gov

Rachel Hoover 650-604-4789
NASA Ames Research Center, Moffett Field, Calif.
rachel.hoover@nasa.gov

Sonja Alexander 202-358-1761
NASA Headquarters, Washington
sonja.r.alexander@nasa.gov

News release: 2012-296 Sept. 20, 2012

QuakeSim and NASA Mobile App Win NASA Software Award

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-296&cid=release_2012-296

PASADENA, Calif. – NASA software that models the behavior of earthquake faults to improve
earthquake forecasting and our understanding of earthquake processes, and NASA's first mobile
application are co-winners of NASA's 2012 Software of the Year Award. The award recognizes
innovative software technologies that significantly improve the agency's exploration of space and
maximize scientific discovery on Earth.

QuakeSim, developed at NASA's Jet Propulsion Laboratory in Pasadena, Calif., is a comprehensive,
state-of-the-art software tool for simulating and understanding earthquake fault processes and
improving earthquake forecasting. Initiated in 2002, QuakeSim uses NASA remote sensing and other
earthquake-related data to simulate and model the behavior of faults in 3-D both individually and as
part of complex, interacting systems. This provides long-term histories of fault behavior that can be
used for statistical evaluation. QuakeSim also is used to identify regions of increased earthquake
probabilities called hotspots.

Studies have shown QuakeSim to be the most accurate tool of its kind for intermediate earthquake
forecasting and detecting the subtle, transient deformation in Earth's crust that precedes and follows
earthquakes. Its varied applications include scientific studies, developing earthquake hazard maps
that can be used for targeted retrofitting of earthquake-vulnerable structures, providing input for
damage and loss estimates after earthquakes, guiding disaster response efforts, and studying fluid
changes in reservoirs, among others.

QuakeSim provides model and analysis tools, computational infrastructure, access to data and an
interface for understanding the complete cycle of earthquakes. The software assimilates data of
crustal deformation that leads to and follows earthquakes, together with seismicity data of
earthquakes and geologic data. QuakeSim's integrated, map-based interfaces and applications make
an unprecedented amount of complex geophysical data from the ground, air and space available and
accessible to a broad range of scientists and end users, including emergency responders, commercial
disaster companies, the insurance industry and civil engineers. The software allows them to explore
and analyze observations, model earthquake processes and analyze patterns to focus attention and
identify significant and/or subtle features in the data.

QuakeSim has had a number of notable accomplishments to date. It produced the first readily
accessible set of digital fault models of California. It was used to identify regions in extreme southern
California at risk for earthquakes, guiding the collection of data by NASA's Uninhabited Aerial
Vehicle Synthetic Aperture Radar (UAVSAR) prior to a magnitude 7.2 earthquake in Baja, Mexico
in 2010, which led to the first-ever airborne radar images of deformation in Earth's surface caused by
a major earthquake. It helped define NASA's planned synthetic aperture radar satellite mission. It was
used to rule out tectonic deformation of Earth's surface as a factor when a spate of water pipe breaks
afflicted Los Angeles in 2009. The software also was used in several recent government earthquake
response exercises, including the 2008 California ShakeOut, 2011 National Level Exercise and the 2012 Golden Guardian Exercise. QuakeSim approaches are being adopted by numerous organizations, including the Southern California Earthquake Center, United States Geological Survey
and the California Geological Survey.

The multidisciplinary QuakeSim team includes principal investigator Andrea Donnellan, Jay Parker,
Robert Granat, Charles Norton and Greg Lyzenga of JPL; Geoffrey Fox and Marlon Pierce of Indiana
University, Bloomington; John Rundle of the University of California, Davis; Dennis McLeod of the
University of Southern California, Los Angeles; and Lisa Grant Ludwig of the University of
California, Irvine.

Software engineers at NASA's Ames Research Center in Moffett Field, Calif., developed the NASA
App for mobile platforms including the iPhone, iPod touch, iPad and Android phones and tablets. The NASA App currently has more than 9.6 million user installations and receives more than three million hits per day on average.

The NASA App gathers the agency's online content, breaking news, image and video collections,
news and image feeds, social media accounts, and more in one easy-to-use location that aids public
access to science, technology and engineering discoveries. The app's creators are program manager
Jerry Colen, software engineer John Freitas and new media specialist Charles Du. A NASA software advisory panel reviews Software of the Year entries and recommends winners to NASA's Inventions and Contributions Board for confirmation. Both Ames and JPL have won
individually or shared the award several times since it was initiated in 1994.

For more information about QuakeSim, visit: http://www.quakesim.org . For more information about
NASA's Inventions and Contributions Board, visit: http://icb.nasa.gov . For more information about
NASA and agency programs, visit: http://www.nasa.gov .

The California Institute of Technology in Pasadena manages JPL for NASA.

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Help NASA Document the Historical Last Journey of the Space Shuttle Endeavor

September 20, 2012


This is a feature from the NASA/JPL Education Office.


Help NASA Document the Historical Last Journey of the Space Shuttle Endeavor

The end of the active flight missions of the Space Shuttle Program is being celebrated with the transfer of the
space shuttles to various museums for permanent display in an effort to further educate the public about the
successful program. Endeavour will be the last shuttle to be transferred via the shuttle carrier aircraft thus making
it the last time a shuttle will fly, a very historic moment in NASA's history. This last ferry flight will originate from
Kennedy Space Center prior to embarking on the historic last leg of the flight throughout the state of California
into Los Angeles International Airport. We are extremely fortunate to have this rare opportunity to view
Endeavour as she arrives in California.

Goal
To engage the public, specifically the students, in a fun way to document this historical event of the Endeavor
Flyover, while also promoting NASA STEAM (Science, Technology, Engineering, Arts, Math).

Overview
By reaching out to California School districts, the challenge is for students to take a photograph of the shuttle
flyover and/or during the transport from LAX to the California Science Center.

These pictures can then be uploaded (by teachers) and then a panel of judges will select "winning
photos". Winning photos may be posted on NASA websites, and exhibited for NASA visitor centers and other
education venues, or used for other NASA purposes. There will be an option of having a NASA day at the winning
school sites.

How to Submit Images
* Teachers select the four best photos from their students and upload them to:
http://www.flickr.com/groups/spaceshuttleendeavour/

* Submitted Photos: Reference Name & Location of School and Teacher
* Submission Deadline: 9 NOV 2012

Educator Resources

The public webcast will be held on NASA's DLinfo Channel on September 20, 2012 from 1:30 pm
– 2:30 pm PST. This exciting opportunity will allow unprecedented engagement for students to
learn about the Shuttle and its significance in American History and the future of space
exploration. For those who wish to join the webcast, please visit:

http://www.nasa.gov/offices/education/programs/national/dln/webcast/webcast.html

NASA's Digital Learning Network provides science, technology, engineering, and mathematics
or STEM content featuring NASA missions and research. Registration is free. To register and for
a list of other interactive events listed in our catalog or watch our webcasts visit:

http://www.nasa.gov/offices/education/programs/national/dln/index.html

For Education Resources on the Shuttle Program visit:

http://www.nasa.gov/audience/foreducators/rocketry/home/shuttle-commem-index.html

Follow Endeavor:
Twitter: @NASA
Hashtags: #spottheshuttle or #OV105
Facebook: NASA
Google+: NASA

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Wednesday, September 19, 2012

NASA Mars Rover Targets Unusual Rock Enroute to First Destination

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster / D.C. Agle 818-354-5011
Jet Propulsion Laboratory, Pasadena,Calif.
guy.webster@jpl.nasa.gov / agle@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

News release: 2012-295 Sept. 19, 2012

NASA Mars Rover Targets Unusual Rock Enroute to First Destination

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.cfm?release=2012-295&cid=release_2012-295

PASADENA, Calif. -- NASA's Mars rover Curiosity has driven up to a football-size rock that will be the first for the rover's arm to examine.

Curiosity is about 8 feet (2.5 meters) from the rock. It lies about halfway from the rover's landing site, Bradbury Landing, to a location called Glenelg. In coming days, the team plans to touch the rock with a spectrometer to determine its elemental composition and use an arm-mounted camera to take close-up photographs.

Both the arm-mounted Alpha Particle X-Ray Spectrometer and the mast-mounted, laser-zapping Chemistry and Camera Instrument will be used for identifying elements in the rock. This will allow cross-checking of the two instruments.

The rock has been named "Jake Matijevic." Jacob Matijevic (mah-TEE-uh-vik) was the surface operations systems chief engineer for Mars Science Laboratory and the project's Curiosity rover. He passed away Aug. 20, at age 64. Matijevic also was a leading engineer for all of the previous NASA Mars rovers: Sojourner, Spirit and Opportunity.

Curiosity now has driven six days in a row. Daily distances range from 72 feet to 121 feet (22 meters to 37 meters).

"This robot was built to rove, and the team is really getting a good rhythm of driving day after day when that's the priority," said Mars Science Laboratory Project Manager Richard Cook of NASA's Jet Propulsion Laboratory in Pasadena, Calif.

The team plans to choose a rock in the Glenelg area for the rover's first use of its capability to analyze powder drilled from interiors of rocks. Three types of terrain intersect in the Glenelg area -- one lighter-toned and another more cratered than the terrain Curiosity currently is crossing. The light-toned area is of special interest because it retains daytime heat long into the night, suggesting an unusual composition.

"As we're getting closer to the light-toned area, we see thin, dark bands of unknown origin," said Mars Science Laboratory Project Scientist John Grotzinger of the California Institute of Technology, Pasadena. "The smaller-scale diversity is becoming more evident as we get closer, providing more potential targets for investigation."

Researchers are using Curiosity's Mast Camera (Mastcam) to find potential targets on the ground. Recent new images from the rover's camera reveal dark streaks on rocks in the Glenelg area that have increased researchers' interest in the area. In addition to taking ground images, the camera also has been busy looking upward.

On two recent days, Curiosity pointed the Mastcam at the sun and recorded images of Mars' two moons, Phobos and Deimos, passing in front of the sun from the rover's point of view. Results of these transit observations are part of a long-term study of changes in the moons' orbits. NASA's twin Mars Exploration Rovers, Spirit and Opportunity, which arrived at Mars in 2004, also have observed solar transits by Mars' moons. Opportunity is doing so again this week.

"Phobos is in an orbit very slowly getting closer to Mars, and Deimos is in an orbit very slowly getting farther from Mars," said Curiosity's science team co-investigator Mark Lemmon of Texas A&M University, College Station. "These observations help us reduce uncertainty in calculations of the changes."

In Curiosity's observations of Phobos this week, the time when the edge of the moon began overlapping the disc of the sun was predictable to within a few seconds. Uncertainty in timing is because Mars' interior structure isn't fully understood.

Phobos causes small changes to the shape of Mars in the same way Earth's moon raises tides. The changes to Mars' shape depend on the Martian interior which, in turn, cause Phobos' orbit to decay. Timing the orbital change more precisely provides information about Mars' interior structure.

During Curiosity's two-year prime mission, researchers will use the rover's 10 science instruments to assess whether the selected field site inside Gale Crater ever has offered environmental conditions favorable for microbial life.

For more about Curiosity, visit: http://www.nasa.gov/msl and http://mars.jpl.nasa.gov/msl . You can follow the mission on Facebook and Twitter at: http://www.facebook.com/marscuriosity and http://www.twitter.com/marscuriosity .


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NASA Telescopes Spy Ultra-Distant Galaxy

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Whitney Clavin 818-354-4673
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

J.D. Harrington 202-358-5241
NASA Headquarters, Washington
j.d.harrington@nasa.gov

News release: 2012-294 Sept. 19, 2012

NASA Telescopes Spy Ultra-Distant Galaxy

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-294&cid=release_2012-294

PASADENA, Calif. -- With the combined power of NASA's Spitzer and Hubble space
telescopes, as well as a cosmic magnification effect, astronomers have spotted what could be the
most distant galaxy ever seen. Light from the young galaxy captured by the orbiting
observatories first shone when our 13.7-billion-year-old universe was just 500 million years old.

The far-off galaxy existed within an important era when the universe began to transit from the
so-called cosmic dark ages. During this period, the universe went from a dark, starless expanse to
a recognizable cosmos full of galaxies. The discovery of the faint, small galaxy opens a window
onto the deepest, most remote epochs of cosmic history.

"This galaxy is the most distant object we have ever observed with high confidence," said Wei
Zheng, a principal research scientist in the department of physics and astronomy at Johns
Hopkins University in Baltimore who is lead author of a new paper appearing in Nature. "Future
work involving this galaxy, as well as others like it that we hope to find, will allow us to study
the universe's earliest objects and how the dark ages ended."

Light from the primordial galaxy traveled approximately 13.2 billion light-years before reaching
NASA's telescopes. In other words, the starlight snagged by Hubble and Spitzer left the galaxy
when the universe was just 3.6 percent of its present age. Technically speaking, the galaxy has a
redshift, or "z," of 9.6. The term redshift refers to how much an object's light has shifted into
longer wavelengths as a result of the expansion of the universe. Astronomers use redshift to
describe cosmic distances.

Unlike previous detections of galaxy candidates in this age range, which were only glimpsed in a
single color, or waveband, this newfound galaxy has been seen in five different wavebands. As
part of the Cluster Lensing And Supernova Survey with Hubble Program, the Hubble Space
Telescope registered the newly described, far-flung galaxy in four visible and infrared
wavelength bands. Spitzer measured it in a fifth, longer-wavelength infrared band, placing the
discovery on firmer ground.

Objects at these extreme distances are mostly beyond the detection sensitivity of today's largest
telescopes. To catch sight of these early, distant galaxies, astronomers rely on gravitational
lensing. In this phenomenon, predicted by Albert Einstein a century ago, the gravity of
foreground objects warps and magnifies the light from background objects. A massive galaxy
cluster situated between our galaxy and the newfound galaxy magnified the newfound galaxy's
light, brightening the remote object some 15 times and bringing it into view.

Based on the Hubble and Spitzer observations, astronomers think the distant galaxy was less than
200 million years old when it was viewed. It also is small and compact, containing only about 1
percent of the Milky Way's mass. According to leading cosmological theories, the first galaxies
indeed should have started out tiny. They then progressively merged, eventually accumulating
into the sizable galaxies of the more modern universe.

These first galaxies likely played the dominant role in the epoch of reionization, the event that
signaled the demise of the universe's dark ages. This epoch began about 400,000 years after the
Big Bang when neutral hydrogen gas formed from cooling particles. The first luminous stars and
their host galaxies emerged a few hundred million years later. The energy released by these
earliest galaxies is thought to have caused the neutral hydrogen strewn throughout the universe to
ionize, or lose an electron, a state that the gas has remained in since that time.

"In essence, during the epoch of reionization, the lights came on in the universe," said paper co-
author Leonidas Moustakas, a research scientist at NASA's Jet Propulsion Laboratory, a division
of the California Institute of Technology in Pasadena, Calif.

Astronomers plan to study the rise of the first stars and galaxies and the epoch of reionization
with the successor to both Hubble and Spitzer, NASA's James Webb Telescope, which is
scheduled for launch in 2018. The newly described distant galaxy will likely be a prime target.

For more information about Spitzer, visit http://www.nasa.gov/spitzer . For more information
about Hubble, visit: http://www.nasa.gov/hubble .

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Tuesday, September 18, 2012

JPL to Stream Mars Curiosity Telecon

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

DC Agle / Guy Webster 818-393-9011/818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
agle@jpl.nasa.gov / guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
Dwayne.c.brown@nasa.gov

Advisory: 2012-292b September 18, 2012

JPL to Stream Mars Curiosity Telecon

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-292b&cid=release_2012-292b

PASADENA, Calif. -- NASA will host a media teleconference at 11 a.m. PDT (2 p.m. EDT)
tomorrow (Wednesday, Sept. 19), to provide a status update on the Curiosity rover's mission to Mars'
Gale Crater.

Curiosity, the Mars Science Laboratory, is 43 days into a two-year mission to investigate whether
conditions may have been favorable for microbial life.

Audio and visuals from the telecon will be streamed live to one of JPL's Ustream.tv channels, at
www.ustream.tv/nasajpl .

Visuals only will be available at the start of the telecon at: http://go.nasa.gov/curiositytelecon .

For more information about NASA's Curiosity mission, visit: http://www.nasa.gov/msl and
http://mars.jpl.nasa.gov/msl .

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Researchers Brew Up Organics on Ice

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

Whitney Clavin 818-354-4673
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

News feature: 2012-293 Sept. 18, 2012

Researchers Brew Up Organics on Ice

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-293&cid=release_2012-293

Would you like icy organics with that? Maybe not in your coffee, but researchers at
NASA's Jet Propulsion Laboratory in Pasadena, Calif., are creating concoctions of
organics, or carbon-bearing molecules, on ice in the lab, then zapping them with lasers.
Their goal: to better understand how life arose on Earth.

In a new study published in the Astrophysical Journal Letters, the research team provides
the first direct look at the organic chemistry that takes place on icy particles in the frigid
reaches of our solar system, and in the even chillier places between stars. Scientists think
that the basic ingredients of life, including water and organics, began their journey to
Earth on these lonesome ice particles. The ice and organics would have found their way
into comets and asteroids, which then fell to Earth, delivering "prebiotic" ingredients that
could have jump-started life.

The various steps needed to go from icy organics to slime molds are not clear, but the
new findings help explain how the process works. The lab experiments show that organic
material can begin the processing it needs to become prebiotic -- while still frozen in ice.

"The very basic steps needed for the evolution of life may have started in the coldest
regions of our universe," said Murthy Gudipati, lead author of the new study at JPL. "We
were surprised to see organic chemistry brewing up on ice, at these very cold
temperatures in our lab."

The organics looked at in the study are called polycyclic aromatic hydrocarbons, or PAHs
for short. These carbon-rich molecules can be found on Earth as combustion products: for
example, in barbecue pits, candle soot and even streaming out of the tail pipe of your car. They have also been spotted throughout space in comets, asteroids and more distant objects. NASA's Spitzer Space Telescope has detected PAHs in the swirling planet-forming disks around stars, in the spaces between stars and in remote galaxies.

Murthy and his colleague Rui Yang of JPL used their lab setup to mimic the environment
of icy PAH molecules in the quiet cold of space, at temperatures as low as 5 Kelvin
(minus 450 degrees Fahrenheit, or minus 268 degrees Celsius). First, they bombarded the
particles with ultraviolet radiation similar to that from stars. Then, to determine the
products of the chemical reaction, they used a type of laser system known as MALDI (for
Matrix Assisted Laser Desorption and Ionization), which involves zapping the ice with
both infrared and ultraviolet lasers.

The results revealed that the PAHs had transformed: they had incorporated hydrogen
atoms into their structure and lost their circular, aromatic bonds, becoming more complex
organics. According to Gudipati, this is the type of change that would need to occur if the
material were to eventually become amino acids and nucleotides -- bits and pieces of
protein and DNA, respectively.

"PAHs are strong, stubborn molecules, so we were surprised to see them undergoing
these chemical changes at such freezing-cold temperatures," said Gudipati.

Another bonus for the research is that it might explain the mystery of why PAHs have not
yet been identified on ice grains in space. While the hardy organics are pervasive in the
cosmos as gases and hot dust, researchers have remained puzzled that their signatures do
not show up on ice. The new findings show that PAHs, once they stick to the ice surface,
are chemically transformed into other complex organics, explaining why they might not
be seen.

While the new results teach us that life's journey could have already begun in the very
cold regions of the universe, another question remains: Did it arise elsewhere beyond our
sun, too? Researchers don't know, but studies like this one help the ongoing search for
life beyond Earth.

The journal article is online at http://iopscience.iop.org/2041-8205/756/1/L24 .

The California Institute of Technology in Pasadena manages JPL for NASA.

-end-













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Friday, September 14, 2012

NASA Mars Rover Opportunity Reveals Geological Mystery

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

DC Agle 818-393-9011
Jet Propulsion Laboratory, Pasadena, Calif.
agle@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.brown@nasa.gov

News release: 2012-290 September 14, 2012

NASA Mars Rover Opportunity Reveals Geological Mystery

PASADENA, Calif. -- NASA's long-lived rover Opportunity has returned an image of the Martian
surface that is puzzling researchers.

Spherical objects concentrated at an outcrop Opportunity reached last week differ in several ways
from iron-rich spherules nicknamed "blueberries" the rover found at its landing site in early 2004 and
at many other locations to date.

Opportunity is investigating an outcrop called Kirkwood in the Cape York segment of the western
rim of Endeavour Crater. The spheres measure as much as one-eighth of an inch (3 millimeters) in
diameter. The analysis is still preliminary, but it indicates that these spheres do not have the high iron
content of Martian blueberries.

"This is one of the most extraordinary pictures from the whole mission," said Opportunity's principal
investigator, Steve Squyres of Cornell University in Ithaca, N.Y. "Kirkwood is chock full of a dense
accumulation of these small spherical objects. Of course, we immediately thought of the blueberries,
but this is something different. We never have seen such a dense accumulation of spherules in a rock
outcrop on Mars."

The Martian blueberries found elsewhere by Opportunity are concretions formed by action of
mineral-laden water inside rocks, evidence of a wet environment on early Mars. Concretions result
when minerals precipitate out of water to become hard masses inside sedimentary rocks. Many of the
Kirkwood spheres are broken and eroded by the wind. Where wind has partially etched them away, a
concentric structure is evident.

Opportunity used the microscopic imager on its arm to look closely at Kirkwood. Researchers
checked the spheres' composition by using an instrument called the Alpha Particle X-Ray
Spectrometer on Opportunity's arm.

"They seem to be crunchy on the outside, and softer in the middle," Squyres said. "They are different
in concentration. They are different in structure. They are different in composition. They are different
in distribution. So, we have a wonderful geological puzzle in front of us. We have multiple working
hypotheses, and we have no favorite hypothesis at this time. It's going to take a while to work this
out, so the thing to do now is keep an open mind and let the rocks do the talking."

Just past Kirkwood lies another science target area for Opportunity. The location is an extensive pale-
toned outcrop in an area of Cape York where observations from orbit have detected signs of clay
minerals. That may be the rover's next study site after Kirkwood. Four years ago, Opportunity
departed Victoria Crater, which it had investigated for two years, to reach different types of
geological evidence at the rim of the much larger Endeavour Crater.

The rover's energy levels are favorable for the investigations. Spring equinox comes this month to
Mars' southern hemisphere, so the amount of sunshine for solar power will continue increasing for
months.

"The rover is in very good health considering its 8-1/2 years of hard work on the surface of Mars," said Mars Exploration Rover Project Manager John Callas of NASA's Jet Propulsion Laboratory in Pasadena, Calif. "Energy production levels are comparable to what they were a full Martian year ago, and we are looking forward to productive spring and summer seasons of exploration."

NASA launched the Mars rovers Spirit and Opportunity in the summer of 2003, and both completed
their three-month prime missions in April 2004. They continued bonus, extended missions for years. Spirit finished communicating with Earth in March 2010. The rovers have made important discoveries about wet environments on ancient Mars that may have been favorable for supporting microbial life.

JPL manages the Mars Exploration Rover Project for NASA's Science Mission Directorate in
Washington.

To view the image of the area, visit: http://www.nasa.gov/mission_pages/mer/multimedia/pia16139.html

For more information about Opportunity, visit: http://www.nasa.gov/rovers and
http://marsrovers.jpl.nasa.gov .

You can follow the project on Twitter and on Facebook at: http://twitter.com/MarsRovers and
http://www.facebook.com/mars.rovers .

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First Planets Found Around Sun-Like Stars in a Cluster

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. PHONE 818-354-5011
http://www.jpl.nasa.gov

Whitney Clavin 818-354-4673
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

J.D. Harrington 202-358-5241
Headquarters, Washington
j.d.harrington@nasa.gov

News release: 2012-289 Sept. 14, 2012

First Planets Found Around Sun-Like Stars in a Cluster

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-289&cid=release_2012-289

PASADENA, Calif. -- NASA-funded astronomers have, for the first time, spotted planets
orbiting sun-like stars in a crowded cluster of stars. The findings offer the best evidence yet that
planets can sprout up in dense stellar environments. Although the newfound planets are not
habitable, their skies would be starrier than what we see from Earth.

The starry-skied planets are two so-called hot Jupiters, which are massive, gaseous orbs that are
boiling hot because they orbit tightly around their parent stars. Each hot Jupiter circles a different
sun-like star in the Beehive Cluster, also called the Praesepe, a collection of roughly 1,000 stars
that appear to be swarming around a common center.

The Beehive is an open cluster, or a grouping of stars born at about the same time and out of the
same giant cloud of material. The stars therefore share a similar chemical composition. Unlike
the majority of stars, which spread out shortly after birth, these young stars remain loosely bound
together by mutual gravitational attraction.

"We are detecting more and more planets that can thrive in diverse and extreme environments
like these nearby clusters," said Mario R. Perez, the NASA astrophysics program scientist in the
Origins of Solar Systems Program. "Our galaxy contains more than 1,000 of these open clusters,
which potentially can present the physical conditions for harboring many more of these giant
planets."

The two new Beehive planets are called Pr0201b and Pr0211b. The star's name followed by a "b" is the standard naming
convention for planets.

"These are the first 'b's' in the Beehive," said Sam Quinn, a graduate student in astronomy at
Georgia State University in Atlanta and the lead author of the paper describing the results, which
was published in the Astrophysical Journal Letters.

Quinn and his team, in collaboration with David Latham at the Harvard-Smithsonian Center for
Astrophysics, discovered the planets by using the 1.5-meter Tillinghast telescope at the
Smithsonian Astrophysical Observatory's Fred Lawrence Whipple Observatory near Amado,
Arizona to measure the slight gravitational wobble the orbiting planets induce upon their host
stars. Previous searches of clusters had turned up two planets around massive stars but none had
been found around stars like our sun until now.

"This has been a big puzzle for planet hunters," Quinn said. "We know that most stars form in
clustered environments like the Orion nebula, so unless this dense environment inhibits planet
formation, at least some sun-like stars in open clusters should have planets. Now, we finally
know they are indeed there."

The results also are of interest to theorists who are trying to understand how hot Jupiters wind up
so close to their stars. Most theories contend these blistering worlds start out much cooler and
farther from their stars before migrating inward.

"The relatively young age of the Beehive cluster makes these planets among the youngest
known," said Russel White, the principal investigator on the NASA Origins of Solar Systems
grant that funded this study. "And that's important because it sets a constraint on how quickly
giant planets migrate inward -- and knowing how quickly they migrate is the first step to figuring
out how they migrate."

The research team suspects planets were turned up in the Beehive cluster because it is rich in
metals. Stars in the Beehive have more heavy elements such as iron than the sun has.

According to White, "Searches for planets around nearby stars suggest that these metals act like
a 'planet fertilizer,' leading to an abundant crop of gas giant planets. Our results suggest this may
be true in clusters as well."

NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages NASA's Exoplanet Exploration
Program office. More information about exoplanets and NASA's planet-finding program is
available at: http://planetquest.jpl.nasa.gov .

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Wednesday, September 12, 2012

Mars Rover Curiosity Arm Tests Nearly Complete

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster / D.C. Agle 818-354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov / agle@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwane.c.brown@nasa.gov

News release: 2012-288 September 12, 2012

Mars Rover Curiosity Arm Tests Nearly Complete

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-288&cid=release_2012-288

PASADENA, Calif. -- NASA's Mars Curiosity team has almost finished robotic arm tests in
preparation for the rover to touch and examine its first Martian rock.

Tests with the 7-foot (2.1-meter) arm have allowed the mission team to gain confidence in the
arm's precise maneuvering in Martian temperature and gravity conditions. During these
activities, Curiosity has remained at a site it reached by its most recent drive on Sept. 5. The
team will resume driving the rover this week and use its cameras to seek the first rock to touch
with instruments on the arm.

"We're about to drive some more and try to find the right rock to begin doing contact science
with the arm," said Jennifer Trosper, Curiosity mission manager at NASA's Jet Propulsion
Laboratory in Pasadena, Calif.

Two science instruments -- a camera called Mars Hand Lens Imager (MAHLI) that can take
close-up, color images and a tool called Alpha Particle X-Ray Spectrometer (APXS) that
determines the elemental composition of a target rock -- have passed preparatory tests at the
rover's current location. The instruments are mounted on a turret at the end of the arm and can be
placed in contact with target rocks.

Curiosity's Canadian-made APXS had taken atmospheric readings earlier, but its first use on a
solid target on Mars was this week on a calibration target brought from Earth. X-ray detectors
work best cold, but even the daytime APXS tests produced clean data for identifying elements in
the target.

"The spectrum peaks are so narrow, we're getting excellent resolution, just as good as we saw in
tests on Earth under ideal conditions," said APXS principal investigator Ralf Gellert of the
University of Guelph, in Ontario, Canada. "The good news is that we can now make high-
resolution measurements even at high noon to support quick decisions about whether a sample is
worthwhile for further investigations."

The adjustable-focus MAHLI camera this week has produced sharp images of objects near and
far.

"Honestly, seeing those images with Curiosity's wheels in the foreground and Mount Sharp in
the background simply makes me cry," said MAHLI principal investigator Ken Edgett of Malin
Space Science Systems in San Diego. "I know we're just getting started, but it's already been an
incredible journey."

MAHLI is also aiding evaluation of the arm's ability to position its tools and instruments.
Curiosity moved the arm to predetermined "teach points" on Sept. 11, including points above
each of three inlet ports where it will later drop samples of soil and powdered rock into analytical
instruments inside the rover. Images from the MAHLI camera confirmed the placements. Photos
taken before and after opening the inlet cover for the chemistry and mineralogy (CheMin)
analytical instrument also confirmed good operation of the cover.

"Seeing that inlet cover open heightens our anticipation of getting the first solid sample into
CheMin in the coming weeks," said CheMin principal investigator David Blake of NASA's
Ames Research Center in Moffett Field, Calif.

A test last week that checked X-rays passing through an empty sample cell in CheMin worked
well. It confirmed the instrument beneath the inlet opening is ready to start analyzing soil and
rock samples.

Curiosity is five weeks into a 2-year prime mission on Mars. It will use 10 science instruments to
assess whether the selected field site inside Gale Crater has ever offered environmental
conditions favorable for microbial life.

For more about Curiosity, visit: http://www.nasa.gov/msl and http://mars.jpl.nasa.gov/msl . You
can follow the mission on Facebook and Twitter at: http://www.facebook.com/marscuriosity and
http://www.twitter.com/marscuriosity .

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Tuesday, September 11, 2012

JPL to Stream Mars Curiosity Telecon and Lecture

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

DC Agle / Guy Webster 818-393-9011/818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
agle@jpl.nasa.gov / guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
Dwayne.c.brown@nasa.gov

Advisory: 2012-287b September 11, 2012

JPL to Stream Mars Curiosity Telecon and Lecture

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-287&cid=release_2012-287

PASADENA, Calif. -- NASA will host a media teleconference at 11 a.m. PDT (2 p.m. EDT)
tomorrow (Wednesday, Sept. 12), to provide a status update on the Curiosity rover's mission to Mars' Gale Crater.

The Mars Science Laboratory spacecraft is more than one month into a two-year mission to
investigate whether conditions have been favorable for microbial life and preserving clues in the
rocks about possible past life.

Audio and visuals from the telecon will be streamed live to one of JPL's Ustream.tv channels, at
www.ustream.tv/nasajpl .

Visuals only will be available at the start of the telecon at: http://go.nasa.gov/curiositytelecon .
Also this week, Mars Science Laboratory Project Manager Richard Cook will speak Thursday, Sept. 13 in JPL's von Karman Auditorium.
The lecture, which begins at 7 p.m. PDT (10 p.m. EDT), is open
to the public and will be broadcast live with moderated chat, on JPL's Ustream channel.

For additional options to view live streaming video of Thursday's talk please visit:
http://www.jpl.nasa.gov/events/lectures_archive.cfm?year=2012&month=9#NASA . For more
information about NASA's Curiosity mission, visit: http://www.nasa.gov/msl and
http://mars.jpl.nasa.gov/msl .
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NASA Orbiter Observations Point to 'Dry Ice' Snowfall on Mars

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 PHONE 818-354-5011
http://www.jpl.nasa.gov

Guy Webster 818-354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webster@jpl.nasa.gov

Dwayne Brown 202-358-1726
Headquarters, Washington
dwayne.c.brown@nasa.gov

News release: 2012-286 September 11, 2012

NASA Orbiter Observations Point to 'Dry Ice' Snowfall on Mars

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-286&cid=release_2012-286

PASADENA, Calif. -- NASA's Mars Reconnaissance Orbiter data have given scientists the clearest
evidence yet of carbon-dioxide snowfalls on Mars. This reveals the only known example of carbon-
dioxide snow falling anywhere in our solar system.

Frozen carbon dioxide, better known as "dry ice," requires temperatures of about minus 193 degrees
Fahrenheit (minus 125 Celsius), which is much colder than needed for freezing water. Carbon-
dioxide snow reminds scientists that although some parts of Mars may look quite Earth-like, the Red
Planet is very different. The report is being published in the Journal of Geophysical Research.

"These are the first definitive detections of carbon-dioxide snow clouds," said the report's lead author,
Paul Hayne of NASA's Jet Propulsion Laboratory in Pasadena, Calif. "We firmly establish the clouds
are composed of carbon dioxide -- flakes of Martian air -- and they are thick enough to result in
snowfall accumulation at the surface."

The snowfalls occurred from clouds around the Red Planet's south pole in winter. The presence of
carbon-dioxide ice in Mars' seasonal and residual southern polar caps has been known for decades.
Also, NASA's Phoenix Lander mission in 2008 observed falling water-ice snow on northern Mars.

Hayne and six co-authors analyzed data gained by looking at clouds straight overhead and sideways
with the Mars Climate Sounder, one of six instruments on the Mars Reconnaissance Orbiter. This
instrument records brightness in nine wavebands of visible and infrared light as a way to examine
particles and gases in the Martian atmosphere. The analysis was conducted while Hayne was a post-
doctoral fellow at the California Institute of Technology in Pasadena.

The data provide information about temperatures, particle sizes and their concentrations. The new
analysis is based on data from observations in the south polar region during southern Mars winter in
2006-2007, identifying a tall carbon-dioxide cloud about 300 miles (500 kilometers) in diameter
persisting over the pole and smaller, shorter-lived, lower-altitude carbon dioxide ice clouds at
latitudes from 70 to 80 degrees south.

"One line of evidence for snow is that the carbon-dioxide ice particles in the clouds are large enough
to fall to the ground during the lifespan of the clouds," co-author David Kass of JPL said. "Another
comes from observations when the instrument is pointed toward the horizon, instead of down at the
surface. The infrared spectra signature of the clouds viewed from this angle is clearly carbon-dioxide
ice particles and they extend to the surface. By observing this way, the Mars Climate Sounder is able
to distinguish the particles in the atmosphere from the dry ice on the surface."

Mars' south polar residual ice cap is the only place on the Red Planet where frozen carbon dioxide
persists on the surface year-round. Just how the carbon dioxide from Mars' atmosphere gets deposited
has been in question. It is unclear whether it occurs as snow or by freezing out at ground level as
frost. These results show snowfall is especially vigorous on top of the residual cap.

"The finding of snowfall could mean that the type of deposition -- snow or frost -- is somehow linked
to the year-to-year preservation of the residual cap," Hayne said.

JPL, a division of the California Institute of Technology in Pasadena, provided the Mars Climate
Sounder instrument and manages the Mars Reconnaissance Orbiter Project for NASA's Science
Mission Directorate in Washington.

For more information about the Mars Reconnaissance Orbiter, visit: http://www.nasa.gov/mro and
http://mars.jpl.nasa.gov/mro .

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Extreme Life Forms Might be Able to Survive on Eccentric Exoplanets

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE 818-354-5011
http://www.jpl.nasa.gov

Written by Josh Rodriquez
Media contact:
Whitney Clavin (818) 354-4673
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

News feature: 2012-285 Sept. 11, 2012

Extreme Life Forms Might Be Able to Survive on Eccentric Exoplanets

The full version of this story with accompanying images is at:
http://www.jpl.nasa.gov/news/news.php?release=2012-285&cid=release_2012-285

Astronomers have discovered a veritable rogues' gallery of odd exoplanets -- from
scorching hot worlds with molten surfaces to frigid ice balls.

And while the hunt continues for the elusive "blue dot" -- a planet with roughly the same
characteristics as Earth -- new research reveals that life might actually be able to survive
on some of the many exoplanetary oddballs that exist.

"When we're talking about a habitable planet, we're talking about a world where liquid
water can exist," said Stephen Kane, a scientist with the NASA Exoplanet Science
Institute at the California Institute of Technology in Pasadena. "A planet needs to be the
right distance from its star -- not too hot and not too cold." Determined by the size and
heat of the star, this temperature range is commonly referred to as the "habitable zone"
around a star.

Kane and fellow Exoplanet Science Institute scientist Dawn Gelino have created a
resource called the "Habitable Zone Gallery." It calculates the size and distance of the
habitable zone for each exoplanetary system that has been discovered and shows which
exoplanets orbit in this so-called "goldilocks" zone. The Habitable Zone Gallery can be
found at www.hzgallery.org . The study describing the research appears in the
Astrobiology journal and is available at http://arxiv.org/abs/1205.2429 .

But not all exoplanets have Earth-like orbits that remain at a fairly constant distance from
their stars. One of the unexpected revelations of planet hunting has been that many
planets travel in very oblong, eccentric orbits that vary greatly in distance from their
stars.

"Planets like these may spend some, but not all of their time in the habitable zone," Kane
said. "You might have a world that heats up for brief periods in between long, cold
winters, or you might have brief spikes of very hot conditions."

Though planets like these would be very different from Earth, this might not preclude
them from being able to support alien life. "Scientists have found microscopic life forms
on Earth that can survive all kinds of extreme conditions," Kane said. "Some organisms
can basically drop their metabolism to zero to survive very long-lasting, cold conditions.
We know that others can withstand very extreme heat conditions if they have a protective
layer of rock or water. There have even been studies performed on Earth-based spores,
bacteria and lichens, which show they can survive in both harsh environments on Earth
and the extreme conditions of space."

Kane and Gelino's research suggests that habitable zone around stars might be larger than
once thought, and that planets that might be hostile to human life might be the perfect
place for extremophiles, like lichens and bacteria, to survive. "Life evolved on Earth at a
very early stage in the planet's development, under conditions much harsher than they are
today," Kane said.

Kane explained that many life-harboring worlds might not be planets at all, but rather
moons of larger, gas-giant planets like Jupiter in our own solar system. "There are lots of
giant planets out there, and all of them may have moons, if they are like the giant planets
in the solar system," Kane says. "A moon of a planet that is in or spends time in a
habitable zone can be habitable itself."

As an example, Kane mentioned Titan, the largest moon of Saturn, which, despite its
thick atmosphere, is far too distant from the sun and too cold for life as we know it to
exist on its surface. "If you moved Titan closer in to the sun, it would have lots of water
vapor and very favorable conditions for life."

Kane is quick to point out that there are limits to what scientists can presently determine
about habitability on already-discovered exoplanets. "It's difficult to really know about a
planet when you don't have any knowledge about its atmosphere," he said. For example,
both Earth and Venus experience an atmospheric "greenhouse effect" -- but the runaway
effect on Venus makes it the hottest place in the solar system. "Without analogues in our
own solar system, it's difficult to know precisely what a habitable moon or eccentric
planet orbit would look like."

Still, the research suggests that habitability might exist in many forms in the galaxy -- not
just on planets that look like our own. Kane and Gelino are hard at work determining
which already-discovered exoplanets might be candidates for extremophile life or
habitable moons. "There are lots of eccentric and gas giant planet discoveries," Kane
says. "We may find some surprises out there as we start to determine exactly what we
consider habitable."

NASA's Exoplanet Science Institute at Caltech manages time allocation on the Keck
Telescope for NASA. NASA's Jet Propulsion Laboratory in Pasadena, Calif., manages
NASA's Exoplanet Exploration program office. Caltech manages JPL for NASA. More
information about exoplanets and NASA's planet-finding program is at
http://planetquest.jpl.nasa.gov .

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