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Monday, March 30, 2009

NASA Team Finds Riches in Meteorite Treasure Hunt

Feature March 30, 2009

NASA Team Finds Riches in Meteorite Treasure Hunt

Just before dawn on Oct. 7, 2008, an SUV-sized asteroid entered Earth's
atmosphere and exploded harmlessly over the Nubian Desert of northern Sudan.
Scientists expected the asteroid, called 2008 TC3, had blown to dust in the resulting
high-altitude fireball.

What happened next excited the scientific community.

Peter Jenniskens, a meteor astronomer with the SETI Institute in Mountain View, Calif.,
who works at NASA's Ames Research Center in Moffett Field, Calif., joined Muawia
Shaddad of the University of Khartoum in Sudan to search for possible extraterrestrial
remnants from the asteroid. A paper on their findings is featured in the March 26 issue
of the journal Nature.

Now, for the first time, scientists are studying recovered celestial meteorites that have a
definitive link with an asteroid from space. This presents the science community an
unprecedented opportunity to interpret asteroid data and learn more about the origins
and differentiations between asteroids and may provide better answers about the
formation of our solar system.

The asteroid was discovered by a telescope of the NASA-sponsored Catalina Sky Survey.
Astronomers and scientists around the world tracked and scanned TC3 for 20 hours prior
to its demise. This marked the first time a celestial object was located prior to entering
Earth's atmosphere. The asteroid had a velocity of 27,700 miles per hour when it entered
the atmosphere. It created a fiery trail 51 miles long before exploding 121,000 feet
from the ground.

"When Dr. Shaddad and I first arrived and started interviewing eyewitnesses,
things looked very bleak," said Jenniskens. "They all described an immense explosion
in the sky, but none had seen any material flying out of the fireball."

The location and subsequent recovery was like searching for a needle in a haystack.
Scientists used what they referred to as a treasure map to locate the meteorites.
NASA's Jet Propulsion Laboratory, or JPL, in Pasadena, Calif., produced a chart
that gave the recovery team its search grid and specific target area.

"My work usually begins and ends with trajectories of objects in space," said Steve Chesley,
a scientist at NASA's Near-Earth Object Program Office at JPL. "We had accurately
predicted when and where TC3 would enter over the Sudan. Jenniskens was asking
for a map of where any surviving fireball fragments could have landed. That was a
first for the Near-Earth Object Program Office."

Armed with the treasure map, Jenniskens, Shaddad and students and staff from the
University of Khartoum began their trek in the afternoon of Dec. 6, 2008.
After a three-day search, the team had scoured 18 miles along Chesley's asteroid path
and recovered 15 samples with a total mass 1.24 pounds. Scientists observed the
meteorites to be porous, rocky material, rounded like a pebble, with a broken face,
and very black in color.

Jenniskens and the Khartoum team visited the site on two more occasions and collected
280 meteorites with a total mass of approximately 11 pounds. Samples were sent for
analysis to Ames, NASA's Johnson Space Center in Houston, the Carnegie Institution of
Washington, and Fordham University in New York.

"We certainly found a treasure," said Michael Zolensky, a cosmic mineralogist at Johnson.
"We have never seen a meteorite on Earth exactly like this one because they are so fragile
that they explode high in the atmosphere. The samples appear to have originated from the
surface of the original asteroid, making them especially valuable to planetologists explaining
the geological history of primitive bodies and planning spacecraft missions to asteroids."
By measuring how asteroid 2008TC3 reflected sunlight in space and comparing it to how
the meteorites found on the ground reflected sunlight, the team concluded that the meteorites
came from the surface of an F-class asteroid in our solar system's asteroid belt. Furthermore,
the team determined that the meteorite was what astronomers refer to as a polymic ureilite,
in other words, a very rare and unusually fragile, dark rock.

NASA's JPL manages the Near-Earth Object Office. Johnson manages the Astromaterials
Research and Exploration Science Directorate. NASA detects and tracks asteroids and
comets passing close to Earth through a program commonly called Spaceguard.

Asteroid 2008TC3 was relatively small to most objects detected and tracked by Spaceguard.
Scientists estimate asteroids of its size enter Earth's atmosphere approximately once a year,
but meteorites rarely survive once they land because of weather and water damage as well as
human disturbance. Scientists are astounded at the good luck that not only did the meteorites
land in a part of the world with ideal conditions to preserve such cosmic artifacts, but the
observatories on the ground were able to detect and track the asteroid's entry.

For more information about NASA's Near-Earth Object office, visit:

http://neo.jpl.nasa.gov (http://neo.jpl.nasa.gov)

For more images from 2008TC4 detection and recovery effort, visit:

http://www.nasa.gov/topics/solarsystem/tc3/ (http://www.nasa.gov/topics/solarsystem/tc3/)







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NASA Continues to Advance International Polar Year Science

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

Steve Cole 202-358-0918
NASA Headquarters, Washington
Stephen.e.cole@nasa.gov

News release: 2009-059 March 30, 2009

NASA Continues to Advance International Polar Year Science

PASADENA, Calif. -- Although the International Polar Year officially came
to a close in February, NASA is continuing to push the frontiers of polar
science from space, the air and the surface of ice.

On Monday, NASA embarks on the first of two airborne field campaigns in the
Arctic to take a closer look at Greenland and Iceland ice sheets and the
region's sea ice and glaciers. From space, NASA's Ice, Cloud, and land Elevation
Satellite, known as ICESat, is completing a seasonal survey of the world's ice
sheets to gauge how and where they are changing. And later in 2009, NASA scientists
will return to Antarctica to drill into the massive Pine Island Glacier.

The two-year International Polar Year focused science and education activities on
Earth's remote polar regions and their connections to the rest of the Earth system. The
event marked the 125th anniversary of the first polar year and the 50th anniversary of
the International Geophysical Year. Scientists from more than 60 nations participated,
including researchers funded by NASA and other U.S. agencies.

The International Polar Year prompted many research projects and innovative public
outreach programs. Examples of ongoing projects NASA and its partners sponsor are:

NASA SATELLITE AND PLANE FLY IN TANDEM OVER GREELAND ICE SHEET

NASA's P-3B aircraft takes off March 30 from NASA's Wallops Flight Facility in Wallops
Island, Va., to begin a month-long Arctic research mission. Its main objective is to map
the changing thickness of the Greenland ice sheet in tandem with NASA's ICESat. Because
the ICESat mission has surpassed its expected lifetime, NASA is ensuring it can maintain
the continuity of this ice sheet data record by taking airborne measurements nearly
simultaneously with measurements from the spacecraft. NASA's William Krabill from Wallops
Flight Facility, an expert at Greenland airborne ice sheet mapping, is leading the effort,
dubbed "Operation Ice Bridge." For 2009, the P-3B is outfitted with an expanded array
of instruments.

NEW AIRBORNE RADAR TO PEER INSIDE ICE SHEETS AND GLACIERS

A team of NASA scientists begins an airborne campaign this spring to better understand
how Arctic ice is changing and assess the impacts of climate change. During the seven-week
Uninhabited Aerial Vehicle Synthetic Aperture Radar field campaign to Greenland and Iceland,
scientists will use two new ice-penetrating radars flying aboard a modified NASA Gulfstream
III aircraft. Data will provide new insights into our understanding of the flow of glaciers
and ice streams while also serving as a test bed for future satellite missions. Scott Hensley
of NASA's Jet Propulsion Laboratory, Pasadena, Calif., leads the campaign.

GLOBAL TOPOGRAPHIC SURVEY OF ICE SHEETS BEGINS SIXTH YEAR

NASA's polar-orbiting ICESat spacecraft is wrapping up its latest month-long campaign to map
Earth's changing ice sheets and polar sea ice. The new data from ICESat's laser-pulsing instrument
adds another year to a detailed record of changes in the mass of ice sheets, the thickness
of sea ice, and the speed of glacier motion at the ice sheet margins. Ron Kwok of JPL and a
team of researchers are using ICESat data to estimate how much Arctic sea ice has been lost
in recent years.

RESEARCHERS POISED TO RETURN TO PINE ISLAND GLACIER

Robert Bindschadler of NASA's Goddard Space Flight Center, Greenbelt, Md., and colleagues
have revised their plans to drill through Antarctica's isolated Pine Island Glacier and take
the first-ever look underneath the glacier at how the ocean and the ice interact. The researchers
were thwarted in their first attempt during the 2007-2008 field season because of concerns
about the safety of landing aircraft on the remote glacier. The new plan calls for helicopter
flights to establish a base camp later this year.

INTERNATIONAL TEAM WORKING TO CALCULATE ANTARCTIC DRAINAGE

For the first time, a group of researchers from seven countries are calculating exactly how much
ice is flowing off the Antarctic Ice Sheet and into the ocean. This fundamental measurement --
how much ice is being lost at the edges of the ice sheet -- will help researchers improve our knowledge
of the changing volume of ice on the continent. Using multiple satellite data sets, groups from seven
countries are applying a new analysis method to data from three satellites to account for all ice loss.
Robert Bindschadler of NASA's Goddard Space Flight Center is leading NASA's contribution to this international effort.

'FROZEN' OPENS ON SCIENCE ON A SPHERE THEATRES

NASA's newest production for the "Science on a Sphere" projection system debuted on March 27 at NASA's
Goddard Space Flight Center and Wallops Flight Facility. "Frozen," a 12-minute, narrated feature, explores
Earth's changing ice and snow cover. Playing on nearly 30 screens around the world, "Frozen" will be coming
soon to a museum near you.

For more information about NASA's International Polar Year projects, visit:
http://www.nasa.gov/ipy .

JPL is managed for NASA by the California Institute of Technology in Pasadena.

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Tuesday, March 24, 2009

Cassini Provides Virtual Flyover of Saturn's Moon Titan

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

Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
carolina.martinez@jpl.nasa.gov

IMAGE ADVISORY: 2009-058 March 24, 2009

Cassini Provides Virtual Flyover of Saturn's Moon Titan

PASADENA, Calif. – "Fly me to the moon"--to Saturn's moon Titan, that is. New Titan movies
and images are providing a bird's-eye view of the moon's Earth-like landscapes.

The new flyover maps show, for the first time, the 3-D topography and height of the 1,200-meter
(4,000-foot) mountain tops, the north polar lake country, the vast dunes more than 100 meters
(300 feet) high that crisscross the moon, and the thick flows that may have oozed from possible
ice volcanoes.

The topographic maps were made from stereo pairs of radar images. They are available at:
http://saturn.jpl.nasa.gov and http://www.nasa.gov/cassini .

Cassini radar team member Randy Kirk with the Astrogeology Science Center at the U.S.
Geological Survey in Flagstaff, Ariz., created the maps. He used some of the 20 or so areas
where two or more overlapping radar measurements were obtained during 19 Titan flybys. These
stereo overlaps cover close to two percent of Titan's surface. The process of making topographic
maps from them is just beginning, but the results already reveal some of the diversity of Titan's
geologic features.

"These flyovers let you take in the bird's-eye sweeping views of Titan, the next best thing to
being there," said Kirk. "We've mapped many kinds of features, and some of them remind me of
Earth. Big seas, small lakes, rivers, dry river channels, mountains and sand dunes with hills
poking out of them, lava flows."

Kirk will present these results today at the Lunar and Planetary Science Conference in The
Woodlands, Texas.

High and low features are shown in unprecedented detail at about 2.4-kilometer (1.5-mile)
resolution. The maps show some features that may be volcanic flows. These flows meander
across a shallow basin in the mountains. One area suspected to be an ice volcano, Ganesa
Macula, does not appear to be a volcanic dome. It may still have originated as a volcano, but it's
too soon to know for sure. "It could be a volcanic feature, a crater, or something else that has
just been heavily eroded," added Kirk.

The stereo coverage includes a large portion of Titan's north polar lakes of liquid ethane and
methane. Based on these topographical models, scientists are better able to determine the depth
of lakes. The highest areas surrounding the lakes are some 1,200 meters (about 4,000 feet) above
the shoreline. By comparing terrain around Earth to the Titan lakes, scientists estimate their
depth is likely about 100 meters (300 feet) or less.

More 3-D mapping of these lakes will help refine these depth estimates and determine the
volume of liquid hydrocarbons that exist on Titan. This information is important because these
liquids evaporate and create Titan's atmosphere. Understanding this methane cycle can provide
clues to Titan's weather and climate.

Launched in 1997, Cassini completed its primary four-year mission in 2008 and is now in
extended mission operations, which run through September 2010. Over the course of the
mission, Cassini plans to map more than three percent of Titan's surface in 3-D. About 38
percent of Titan's surface has been mapped with radar so far. On March 27, Cassini will
complete its 52nd targeted flyby of Titan.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and
the Italian Space Agency. JPL manages the Cassini-Huygens mission for NASA's Science
Mission Directorate. The Cassini orbiter was designed, developed and assembled at JPL. The
radar instrument was built by JPL and the Italian Space Agency, working with team members
from the United States and several European countries.

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Monday, March 23, 2009

Watching Space Rocks: Live Chat With NASA's Asteroid Trackers

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

INTERNET ADVISORY: 2009-057 March 23, 2009

Watching Space Rocks: Live Chat With NASA's Asteroid Trackers

A live videocast and chat from NASA's Jet Propulsion Laboratory, Pasadena, Calif., offers a
unique opportunity for viewers to ask questions of scientists with NASA's Near-Earth Object
Program Office about how NASA discovers and tracks asteroids.

The live event will air on the "NASAJPL" channel available on Ustream TV at:
http://www.ustream.tv/channel/nasajpl on March 25 at 4:30 p.m. PDT (7:30 p.m. EDT and 23:30
UTC).

NASA detects and tracks asteroids and comets passing close to Earth. The Near-Earth Object
Observation Program, commonly called "Spaceguard," discovers, characterizes and computes
trajectories for these objects to determine if any could be potentially hazardous to our planet.

Participants include:
* Don Yeomans, manager, NASA's Near-Earth Object Office at JPL
* Steve Chesley, scientist, NASA's Near-Earth Object Office at JPL
* Paul Chodas, scientist, NASA's Near-Earth Object Office at JPL

If you are unable to take part in the live chat, you can submit questions in advance to
chatquestion@jpl.nasa.gov and watch the archived video at a later time.

More information about NASA's Near-Earth Object Program Office is available at:
http://neo.jpl.nasa.gov/

NASA's Jet Propulsion Laboratory, managed by the California Institute of Technology,
Pasadena, manages the Near-Earth Object Program Office for NASA's Science Mission
Directorate, Washington.

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Thursday, March 19, 2009

Online Poll for NASA's Mars Rover Naming Contest Opens March 23

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

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

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

NEWS RELEASE: 2009-055 March 19, 2009

Online Poll for NASA's Mars Rover Naming Contest Opens March 23

PASADENA, Calif. -- NASA will post online nine names that are finalists for the agency's Mars
Science Laboratory mission and invite the public to vote for its favorite. The non-binding poll to
help NASA select a name opens online Monday, March 23, and will accept votes through March
29.

More than 9,000 students in kindergarten through 12th grades submitted essays proposing names
for the rover in a nationwide contest that ended Jan. 25. Entries came from all 50 states, Puerto
Rico and the families of American service personnel overseas. NASA will select the winning
name, based on a student's essay and the public poll, and announce the name in April.

"The names that students proposed range from heroes to animals and bugs," said Michelle Viotti,
manager of the Mars Public Engagement program at NASA's Jet Propulsion Laboratory,
Pasadena, Calif. "No matter what name is finally chosen, this is a mission for everyone, and we
can't wait to start calling this rover by name."

The student who submitted the winning name will be invited to JPL to sign the rover.
Additionally, all 30 student semifinalists in the naming contest will have an opportunity to place
an individually-tailored message on a microchip that will be carried on the car-sized robotic
explorer.

For worldwide participation beyond the contest, the public also has a chance to participate in
"Send Your Name to Mars." The agency will collect names to be recorded on the microchip.
Names will be collected via the contest Web link beginning Monday, March 23.

The naming contest is part of a Space Act Agreement between NASA and Disney. Walt Disney
Studios Motion Pictures is the prize provider for the contest. This collaboration made it possible
for WALL-E, the animated robotic hero from the 2008 movie of the same name, to appear in the
online content inviting students to participate.

Scheduled to launch in 2011 and land on Mars in 2012, the rover will use a set of advanced
science instruments to check whether the environment in a selected landing region ever has been
favorable for supporting microbial life and preserving evidence of such life. The rover also will
search for minerals that formed in the presence of water and look for chemical building blocks of
life.

JPL, a division of the California Institute of Technology, manages the Mars Science Laboratory
mission for NASA's Science Mission Directorate in Washington.

To view the nine finalist names and cast your vote, visit: http://marsrovername.jpl.nasa.gov .

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Wednesday, March 18, 2009

NASA Celebrates Sun-Earth Day With Illuminating Webcast

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

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

Dewayne Washington 301-286-0040
Goddard Space Flight Center, Greenbelt, Md.
dewayne.a.washington@nasa.gov

NEWS RELEASE: 2008-054 March 18, 2009

NASA Celebrates Sun-Earth Day With Illuminating Webcast

PASADENA, Calif. – NASA scientists will reveal new information and images about our sun and its
influence on Earth and the solar system for Sun-Earth Day, recognized each year in conjunction with
the spring equinox. The highlight of this year's celebration is a webcast for students and teachers
around the world, beginning at 10 a.m. PDT (1 p.m. EDT), Friday, March 20.

This year's theme, "Our Sun, Yours to Discover," celebrates the International Year of Astronomy and
emphasizes daytime astronomy. During the live, interactive event, participants from around the world
and NASA scientists will share new discoveries and visualizations about our sun. Participating
students will have the opportunity to demonstrate personally designed sundials, while others will be
monitoring the sun and preparing their own space weather forecast.

"Tremendous strides have been made with satellite and ground-based observations of the sun, which
have enabled us to monitor the sun to gain a better understanding of the processes that govern its
influence on our solar system," said Eric Christian, a scientist at NASA's Goddard Space Flight
Center in Greenbelt, Md.

Sun-Earth Day is a celebration of the sun and how it affects life on our planet and the space around
Earth, known as geospace. For the past nine years, NASA has sponsored and coordinated education
and public outreach events for Sun-Earth Day that highlight NASA heliophysics research and
discoveries. NASA's goal is to use celestial events to engage the public and students in kindergarten
through 12th grade via webcasts, podcasts, space science activities, demonstrations and interactions
with space scientists.

"These events also support the spirit of international collaboration," said Lou Mayo, project manager
at Goddard for Sun-Earth Day 2009. "We are excited about sharing the latest discoveries about our
sun and encourage others to join our quest for a greater understanding of our closest star."

Goddard is producing the Sun-Earth Day webcast. NASA's Jet Propulsion Laboratory in Pasadena,
Calif., and the Adler Planetarium in Chicago also are participating in the broadcast. NASA Television
and the agency's Web site will broadcast the event live.

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

For more information about Sun-Earth Day, visit: http://sunearthday.nasa.gov/2009/index.php .

For more information about NASA's Education programs, visit: http://www.nasa.gov/education .

JPL is managed for NASA by the California Institute of Technology in Pasadena.

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One Mars Rover Sees a Distant Goal; The Other Takes a New Route

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIFORNIA 91109. TELEPHONE 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: 2009-053 March 18, 2009

One Mars Rover Sees a Distant Goal; The Other Takes a New Route

PASADENA, Calif. -- On a plain that stretches for miles in every direction, the panoramic
camera on NASA's Mars rover Opportunity has caught a first glimpse on the horizon of the
uplifted rim of the big crater that has been Opportunity's long-term destination for six months.

Opportunity's twin, Spirit, also has a challenging destination, and last week switched to a
different route for making progress.

Endeavour Crater, 22 kilometers (14 miles) in diameter, is still 12 kilometers (7 miles) away from
Opportunity as the crow flies, and at least 30 percent farther away on routes mapped for evading
hazards on the plain. Opportunity has already driven about 3.2 kilometers (2 miles) since it
climbed out of Victoria Crater last August after two years of studying Victoria, which is less
than one-twentieth the size of Endeavour.

"It's exciting to see our destination, even if we can't be certain whether we'll ever get all the way
there," said John Callas of NASA's Jet Propulsion Laboratory, Pasadena, Calif., project manager
for the twin Mars rovers, Opportunity and Spirit. "At the pace we've made since leaving Victoria,
the rest of the trek will take more than a Martian year." A Martian year lasts about 23 months.

The image with portions of Endeavour's rim faintly visible can be seen online at
http://www.nasa.gov/mission_pages/mer/images/mer20090318.html .

Steve Squyres of Cornell University, Ithaca, N.Y., principal investigator for the rovers' science
instruments, said, "We can now see our landfall on the horizon. It's far away, but we can
anticipate seeing it gradually look larger and larger as we get closer to Endeavour. We had a
similar experience during the early months of the mission watching the Columbia Hills get bigger
in the images from Spirit as Spirit drove toward them."

Both rovers landed on Mars in January 2004 to begin missions designed to last for three months.
Both are still active after more than five years.

For the next several days, the rover team plans to have Opportunity use the tools on its robotic
arm to examine soil and rock at an outcrop along the route the rover is taking toward Endeavour.

"We're stopping to taste the terrain at intervals along our route so that we can watch for trends in
the composition of the soil and bedrock," Squyres said. "It's part of systematic exploration."

The pause for using the tools on the arm also provides two other benefits. Opportunity's right-
front wheel has been drawing more electric current than usual, an indication of friction within the
wheel. Resting the wheel for a few days is one strategy that has in the past helped reduce the
amount of current drawn by the motor. Also, on March 7, the rover did not complete the
backwards-driving portion of its commanded drive due to unanticipated interaction between the
day's driving commands and onboard testing of capabilities for a future drive. The team is
analyzing that interaction before it will resume use of Opportunity's autonomous-driving
capabilities.

Meanwhile, on March 10, the rover team decided to end efforts to drive Spirit around the
northeastern corner of a low plateau called "Home Plate" in the inner basin of the Columbia Hills,
on the other side of Mars from Opportunity. Spirit has had the use of only five wheels since its
right-front wheel stopped working in 2006. Consequently, it usually drives backwards, dragging
that wheel, so it can no longer climb steep slopes.

Callas said, "After several attempts to drive up-slope in loose material to get around the northeast
corner of Home Plate, the team judged that route to be impassable."

The new route to get toward science targets south of Home Plate is to go around the west side of
the plateau.

Squyres said, "The western route is by no means a slam dunk. It is unexplored territory. There are
no rover tracks on that side of Home Plate like there are on the eastern side. But that also makes
it an appealing place to explore. Every time we've gone someplace new with Spirit since we got
into the hills, we've found surprises."

JPL, a division of the California Institute of Technology, Pasadena, manages the Mars
Exploration Rovers for the NASA Science Mission Directorate, Washington. More information
about the rovers is at http://www.nasa.gov/rovers .

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Tuesday, March 17, 2009

Quadruple Saturn Moon Transit Snapped by Hubble

Media RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIFORNIA 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

Ray Villard 410-338-4514
Space Telescope Science Institute, Baltimore, Md.
villard@stsci.edu

IMAGE ADVISORY: 2009-051 March 17, 2009

Quadruple Saturn Moon Transit Snapped by Hubble

PASADENA, Calif. -- On Feb. 24, 2009, NASA's Hubble Space Telescope took a photo
of four moons of Saturn passing in front of their parent planet. The pictures were taken by
the Wide Field and Planetary Camera 2, developed and built by NASA's Jet Propulsion
Laboratory, Pasadena, Calif.

In the new view, the giant orange moon Titan casts a large shadow onto Saturn's north
polar hood. Below Titan, near the ring plane and to the left, is the moon Mimas, casting a
much smaller shadow onto Saturn's equatorial cloud tops. Farther to the left, and off
Saturn's disk, are the bright moons Dione and the fainter Enceladus.

These rare moon transits only happen when the tilt of Saturn's ring plane is nearly "edge
on" as seen from Earth. Saturn's rings will be perfectly edge on to our line of sight on
Aug. 10, 2009, and Sept. 4, 2009. Unfortunately, Saturn will be too close to the sun to be
seen by viewers on Earth at that time. This "ring plane crossing" occurs every 14 to 15
years. In 1995 to 1996, Hubble witnessed the ring plane crossing event as well as many
moon transits, and even helped discover several new moons of Saturn.

The banded structure in Saturn's atmosphere is similar to Jupiter's.

Early 2009 was a favorable time for viewers with small telescopes to watch moon and
shadow transits crossing the face of Saturn. Titan, Saturn's largest moon, crossed Saturn
on four separate occasions: January 24, February 9, February 24, and March 12, although
not all events were visible from all locations on Earth.

These pictures were taken with the Wide Field and Planetary Camera 2 on Feb. 24, 2009,
when Saturn was roughly 1.25 billion kilometers (775 million miles) from Earth. Hubble
can see details as small as 300 kilometers (190 miles) across on Saturn. The dark band
running across the face of the planet slightly above the rings is the shadow of the rings
cast on the planet.

For images, video, and more information, visit http://hubblesite.org/news/2009/12 and
http://heritage.stsci.edu/2009/12 .

The California Institute of Technology manages JPL for NASA.

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Monday, March 16, 2009

Hearts of Galaxies Close in for Cosmic Train Wreck

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

NEWS RELEASE: 2009-050 March 16, 2009

Hearts of Galaxies Close in for Cosmic Train Wreck

PASADENA, Calif. -- A new image from NASA's Spitzer Space Telescope offers a rare view of
an imminent collision between the cores of two merging galaxies, each powered by a black hole
with millions of times the mass of the sun.

The galactic cores are in a single, tangled galaxy called NGC 6240, located 400-million light
years away in the constellation Ophiuchus. Millions of years ago, each core was the dense center
of its own galaxy before the two galaxies collided and ripped each other apart. Now, these cores
are approaching each other at tremendous speeds and preparing for the final cataclysmic collision.
They will crash into each other in a few million years, a relatively short period on a galactic
timescale.

The spectacular image is online at:
http://www.nasa.gov/mission_pages/spitzer/multimedia/spitzer-20090316.html . It combines
visible light from NASA's Hubble Space Telescope and infrared light from Spitzer. It catches the
two galaxies during a rare, short-lived phase of their evolution, when both cores of the interacting
galaxies are still visible but closing in on each other fast.

"One of the most exciting things about the image is that this object is unique," said Stephanie
Bush of the Harvard-Smithsonian Center for Astrophysics, Cambridge, Mass., lead author of a
new paper describing the observation in an upcoming issue of the Astrophysical Journal.
"Merging is a quick process, especially when you get to the train wreck that is happening. There
just aren't many galactic mergers at this stage in the nearby universe."

NGC 6240 is already putting out huge amounts of infrared light, an indication that a burst of star
formation is underway. The extra infrared radiation is common in interacting galaxies; as the two
galaxies interact, dust and gas swept up by the collision form a burst of new stars that give off
infrared light. Such galaxies are called luminous infrared galaxies. Spitzer's infrared array
camera can image the extra heat from newly formed stars, even though their visible light is
obscured by thick dust clouds around them.

The blob-like shape of the galaxy is due to the sustained violence of the collision. Streams of
millions of stars are being ripped off the galaxy, forming wispy "tidal tails" that lead off NGC
6240 in several directions. But things are about to get even more violent as the main event
approaches and the two galactic cores meld into one.

In the center of NGC 6240, the two black holes in the cores will whip up a frenzy of radiation as
they careen towards one another head-on, likely transforming the galaxy into a monster known as
an ultra-luminous infrared galaxy, thousands of times as bright in infrared as our Milky Way.

Another fascinating aspect of this rare object is that no two galactic mergers are the same. "Not
only are there few objects at this stage, but each object is unique because it came from different
progenitor galaxies," said Bush. "These observations give us another layer of information about
this galaxy, and galactic mergers in general."

Infrared light taken by Spitzer's infrared array camera at 3.6 and 8.8 microns (red) shows cold
dust and radiation from star formation; visible light from Hubble (green and blue) shows hot gas
and stars.
Other authors of this paper include Zhong Wang, Margarita Karovska and Giovanni Fazio, all of
the Harvard-Smithsonian Center for Astrophysics.
NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages the Spitzer Space Telescope
mission for NASA's Science Mission Directorate, Washington. Science operations are conducted
at the Spitzer Science Center at the California Institute of Technology, also in Pasadena. Caltech
manages JPL for NASA.

More information about Spitzer is at http://www.spitzer.caltech.edu/spitzer and
http://www.nasa.gov/spitzer .

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Thursday, March 12, 2009

NASA Launches 'Eyes on the Earth 3-D'

MEDIA RELATIONS OFFICE
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http://www.jpl.nasa.gov

Alan Buis 818-354-0474/354-5011
Jet Propulsion Laboratory, Pasadena, Calif.
Alan.D.Buis@jpl.nasa.gov

INTERNET ADVISORY: 2009-048 March 12, 2008

NASA Launches 'Eyes on the Earth 3-D'

New interactive features on NASA's Global Climate Change Web site give the public the
opportunity to "fly along" with NASA's fleet of Earth science missions and observe Earth
from a global perspective in an immersive, 3-D environment.

Developed using a state-of-the-art, browser-based visualization technology, "Eyes on the
Earth 3-D" displays the location of all of NASA's 15 currently operating Earth-observing
missions in real time. These missions constantly monitor our planet's vital signs, such as
sea level height, concentration of carbon dioxide in our atmosphere, global temperatures
and extent of sea ice in the Arctic, to name a few.

The new "Eyes on the Earth 3-D" features are online at: http://climate.jpl.nasa.gov .

Visitors to "Eyes on the Earth 3-D" can:

- Ride along with a spacecraft, observing Earth as it sweeps below in accelerated time.
- View authentic data maps of ozone, sea level or carbon dioxide distribution, mapped
onto the surface of the globe.
- Compare the size of each satellite to a car or a scientist.
- Blast through a global carbon dioxide map to uncover some of the world's most
populous cities in the new interactive game, "Metropolis."

"This innovative new Web application gives the public an unprecedented perspective on
our changing planet, as only NASA can," said Michael Greene, manager for public
engagement strategy at NASA's Jet Propulsion Laboratory, Pasadena, Calif.

NASA's Global Climate Change Web site is devoted to educating the public about
Earth's changing climate, providing easy-to-understand information about the causes and
effects of climate change and how NASA studies it. For more on NASA's Earth Science
Program, visit: http://www.nasa.gov. JPL is a division of the California Institute of
Technology in Pasadena.

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Galactic Dust Bunnies Found to Contain Carbon After All

Feature March 12, 2009


Galactic Dust Bunnies Found to Contain Carbon After All

Using NASA's Spitzer Space Telescope, researchers have found evidence suggesting that stars
rich in carbon complex molecules may form at the center of our Milky Way galaxy.

This discovery is significant because it adds to our knowledge of how stars form heavy elements
-- like oxygen, carbon and iron -- and then blow them out across the universe, making it possible
for life to develop.

Astronomers have long been baffled by a strange phenomenon: Why have their telescopes never
detected carbon-rich stars at the center of our galaxy even though they have found these stars in
other places? Now, by using Spitzer's powerful infrared detectors, a research team has found the
elusive carbon stars in the galactic center.

"The dust surrounding the stars emits very strongly at infrared wavelengths," says Pedro García-
Lario, a research team member who is on the faculty of the European Space Astronomy Center,
the European Space Agency's center for space science. He co-authored a paper on this subject in
the February 2009 issue of the journal Astronomy & Astrophysics.

"With the help of Spitzer spectra, we can easily determine whether the material returned by the
stars to the interstellar medium is oxygen-rich or carbon-rich."

The team of scientists analyzed the light emitted from 40 planetary nebulae – blobs of dust and
gas surrounding stars -- using Spitzer's infrared spectrograph. They analyzed 26 nebulae toward
the center of the Milky Way -- a region called the "Galactic Bulge" -- and 14 nebulae in other
parts of the galaxy. The scientists found a large amount of crystalline silicates and polycyclic
aromatic hydrocarbons, two substances that indicate the presence of oxygen and carbon.

This combination is unusual. In the Milky Way, dust that combines both oxygen and carbon is
rare and is usually only found surrounding a binary system of stars. The research team, however,
found that the presence of the carbon-oxygen dust in the Galactic Bulge seems to be suggestive
of a recent change of chemistry experienced by the star.

The scientists hypothesize that as the central star of a planetary nebula ages and dies, its heavier
elements do not make their way to the star's outer layers, as they do in other stars. Only in the
last moments of the central star's life, when it expands and then violently expels almost all of its
remaining outer gasses, does the carbon become detectable. That's when astronomers see it in the
nebula surrounding the star.

"The carbon produced through these recurrent 'thermal pulses' is very inefficiently dredged up to
the surface of the star, contrary to what is observed in low-metallicity, galactic disk stars," said
García-Lario. "It only becomes visible when the star is about to die."

This study supports a hypothesis about why the carbon in some stars does not make its way to
the stars' surfaces. Scientists believe that small stars -- those with masses up to one-and-a-half
times that of our sun -- that contain lots of metal do not bring carbon to their surfaces as they
age. Stars in the Galactic Bulge tend to have more metals than other stars, so the Spitzer data
support this commonly held hypothesis. Before the Spitzer study, this hypothesis had never been
supported by observation.

This aging and expelling process is typical of all stars. As stars age and die, they burn
progressively heavier and heavier elements, beginning with hydrogen and ending with iron.
Towards the end of their lives, some stars become what are called "red giants." These dying stars
swell so large that if one of them were placed in our solar system, where the sun is now, its
outermost border would touch Earth's orbit. As these stars pulsate – losing mass in the process –
and then contract, they spew out almost all of their heavier elements. These elements are the
building blocks of all planets, including our own Earth (as well as of human beings and any other
life forms that may exist in the universe).

The paper is co-authored by José Vicente Perea-Calderón of the European Space Astronomy
Center in Villanueva de la Cañada, Spain; Domingo Anibal García-Hernández of the Instituto de
Astrofísica de Canarias, on Spain's Tenerife island; Ryszard Szczerba of the Nicolaus Copernicus
Astronomical Center in Torun, Poland; and Matt Bobrowsky of the University of Maryland,
College Park.

NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages the Spitzer Space Telescope
mission for NASA's Science Mission Directorate, Washington. Science operations are conducted
at the Spitzer Science Center at the California Institute of Technology, also in Pasadena. Caltech
manages JPL for NASA.

For more information about Spitzer, visit http://www.spitzer.caltech.edu/spitzer and
http://www.nasa.gov/spitzer .

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Cassini-Huygens Mission Status Report

MEDIA RELATIONS OFFICE
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Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
carolina.martinez@jpl.nasa.gov

STATUS REPORT: 2009-047 March 12, 2009

Cassini-Huygens Mission Status Report

Cassini Swaps Thrusters

PASADENA, Calif. – Early this morning the Cassini spacecraft relayed information that it had
successfully swapped to a backup set of propulsion thrusters late Wednesday.

The swap was performed because of degradation in the performance of the primary thrusters,
which had been in use since Cassini's launch in 1997. This is only the second time in Cassini's 11
years of flight that the engineering teams have gone to a backup system.

The thrusters are used for making small corrections to the spacecraft's course, for some attitude
control functions, and for making angular momentum adjustments in the reaction wheels, which
also are used for attitude control. The redundant set is an identical set of eight thrusters. Almost
all Cassini engineering subsystems have redundant backup capability.

Cassini has successfully completed its original four-year planned tour of Saturn and is now in
extended mission operations.

More information on the mission is available at: http://saturn.jpl.nasa.gov and
http://www.nasa.gov/cassini .

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and
the Italian Space Agency. JPL, a division of the California Institute of Technology in Pasadena,
manages the Cassini mission for NASA's Science Mission Directorate, Washington, D.C. The
Cassini orbiter was designed, developed and assembled at JPL.

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Wednesday, March 11, 2009

Mars Odyssey Mission Status Report

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
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http://www.jpl.nasa.gov

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif. March 11, 2009
guy.webster@jpl.nasa.gov

Mars Odyssey Mission Status Report
Spacecraft Reboots Successfully

PASADENA, Calif. -- NASA's Mars Odyssey orbiter properly followed commands today to shut
down and restart, a strategy by its engineers to clear any memory flaws accumulated in more than five
years since Odyssey's last reboot.

The procedure also restored Odyssey's onboard set of backup systems, called the spacecraft's "B side,"
allowing its use in the future when necessary.

"For nearly two years, we have not known for certain whether the backup systems would be usable, so
this successful reboot has allowed us to ascertain their health and availability for future use," said
Odyssey Project Manager Philip Varghese of NASA's Jet Propulsion Laboratory, Pasadena, Calif.

Odyssey has been orbiting Mars since 2001 and has never switched from its primary set of
components, the "A side," to the backup set, which includes an identical computer processor,
navigation sensors, relay radio and other components. In March 2006, the B-side spare of a component
for managing the distribution of power became inoperable. Analysis by engineers identified a
possibility that rebooting Odyssey might restore that component, which proved to be a side benefit of
today's procedure to refresh onboard memory.

The Odyssey team began a series of steps after the reboot to carefully return the spacecraft to full
functioning over the next few days. Following that path, the science instruments will be back to
studying Mars by next week.

An unexpected rise in temperature of the star camera in Odyssey's navigation system on March 9 had
prompted a postponement of the rebooting originally scheduled for the next day. Engineers identified
the cause as a heater circuit that was temporarily stuck "on." The circuit was turned off before today's
reboot.

JPL, a division of the California Institute of Technology, Pasadena, manages Mars Odyssey for the
NASA Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, is the
prime contractor for the project and built the spacecraft. Additional information about Odyssey is at
http://www.nasa.gov/mission_pages/odyssey .

#2009-046

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Friday, March 6, 2009

NASA's Kepler Mission Rockets to Space in Search of Other Earths

MEDIA RELATIONS OFFICE
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Whitney Clavin 818-354-4673/818-458-9008
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

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

Michael Mewhinney 650-604-3937
Ames Research Center, Moffett Field,Calif.
michael.s.mewhinney@nasa.gov

George Diller 321-861-7643
Kennedy Space Center, Fla.
george.h.diller@nasa.gov

NEWS RELEASE: 2009-043 March 6, 2009

NASA's Kepler Mission Rockets to Space in Search of Other Earths

CAPE CANAVERAL, Fla. -- NASA's Kepler mission successfully launched into space from Cape
Canaveral Air Force Station, Fla., aboard a United Launch Alliance Delta II at 10:49 p.m. EST (7:49 p.m.
PST), Friday, March 6. Kepler is designed to find the first Earth-size planets orbiting stars at distances
where water could pool on the planet's surface. Liquid water is believed to be essential for the formation of
life.

"It was a stunning launch," said Kepler Project Manager James Fanson of NASA's Jet Propulsion
Laboratory in Pasadena, Calif. "Our team is thrilled to be a part of something so meaningful to the human
race -- Kepler will help us understand if our Earth is unique or if others like it are out there."

Engineers acquired a signal from Kepler at 12:11 a.m. Saturday EST (9:11 p.m. Friday PST), after it
separated from its spent third-stage rocket and entered its final sun-centered orbit, trailing about 1,529
kilometers (950 miles) behind Earth. The spacecraft is generating its own power from its solar panels.

"Kepler now has the perfect place to watch more than 100,000 stars for signs of planets," said William
Borucki, the mission's science principal investigator at NASA's Ames Research Center at Moffett Field,
Calif. Borucki has worked on the mission for 17 years. "Everyone is very excited as our dream becomes a
reality. We are on the verge of learning if other Earths are ubiquitous in the galaxy."

Engineers have begun to check Kepler to ensure it is working properly, a process called "commissioning"
that will take about 60 days. In about a month or less, NASA will send up commands for Kepler to eject its
dust cover and make its first measurements. After another month of calibrating Kepler's single instrument, a
wide-field charge-couple device camera, the telescope will begin to search for planets.

The first planets to roll out on the Kepler "assembly line" are expected to be the portly "hot Jupiters" -- gas
giants that circle close and fast around their stars. NASA's Hubble and Spitzer space telescopes will be able
to follow up with these planets and learn more about their atmospheres. Neptune-size planets will most
likely be found next, followed by rocky ones as small as Earth. The true Earth analogs -- Earth-sized planets
orbiting stars like our sun at distances where surface water, and possibly life, could exist -- would take at
least three years to discover and confirm. Ground-based telescopes also will contribute to the mission by
verifying some of the finds.

In the end, Kepler will give us our first look at the frequency of Earth-size planets in our Milky Way galaxy,
as well as the frequency of Earth-size planets that could theoretically be habitable.

"Even if we find no planets like Earth, that by itself would be profound. It would indicate that we are
probably alone in the galaxy," said Borucki.

As the mission progresses, Kepler will drift farther and farther behind Earth in its orbit around the sun.
NASA's Spitzer Space Telescope, which was launched into the same orbit more than five years ago, is now
more than about 100 million kilometers (62 million miles) behind Earth.

Kepler is a NASA Discovery mission. Ames is the home organization of the science principal investigator
and is responsible for the ground system development, mission operations and science data analysis. JPL
manages the Kepler mission development. Ball Aerospace & Technologies Corp. of Boulder, Colo., is
responsible for developing the Kepler flight system and supporting mission operations. NASA's Launch
Services Program at NASA's Kennedy Space Center, Fla., managed the launch service including payload
integration and certifying the Delta II launch vehicle for NASA's use.

For more information about the Kepler mission, visit http://www.nasa.gov/kepler .

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Thursday, March 5, 2009

Five Things About the Kepler Mission

Feature March 5, 2009



Five Things About the Kepler Mission

Some quick facts about the Kepler mission, scheduled to launch March 6, 2009:

• Kepler is the world's first mission with the ability to find true Earth analogs -- planets that orbit stars like our sun in the "habitable zone." The habitable zone is the region around a star where the temperature is just right for water -- an essential ingredient for life as we know it -- to pool on a planet's surface.

• By the end of Kepler's three-and-one-half-year mission, it will give us a good idea of how common or rare other Earths are in our Milky Way galaxy. This will be an important step in answering the age-old question: Are we alone?

• Kepler detects planets by looking for periodic dips in the brightness of stars. Some planets pass in front of their stars as seen from our point of view on Earth; when they do, they cause their stars to dim slightly, an event Kepler can see.

• Kepler has the largest camera ever launched into space, a 95-megapixel array of charge-coupled devices, or CCDs, like those in everyday digital cameras.

• Kepler's telescope is so powerful that, from its view up in space, it could detect one person in a small town turning off a porch light at night.

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NASA's Mars Rover Spirit Faces Circuitous Route

MEDIA RELATIONS OFFICE
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http://www.jpl.nasa.gov

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

NEWS RELEASE: 2009-041 March 5, 2009

NASA's Mars Rover Spirit Faces Circuitous Route

PASADENA, Calif. -- Loose soil piled against the northern edge of a low plateau called "Home Plate"
has blocked NASA's Mars Exploration Rover Spirit from taking the shortest route toward its southward
destinations for the upcoming Martian summer and following winter.

The rover has begun a trek skirting at least partway around the plateau instead of directly over it.

However, Spirit has also gotten a jump start on its summer science plans, examining a silica-rich outcrop
that adds information about a long-gone environment that had hot water or steam. And even a circuitous
route to the destinations chosen for Spirit would be much shorter than the overland expedition Spirit's
twin, Opportunity, is making on the opposite side of Mars.

Both rovers landed on Mars in 2004 for what were originally planned as three-month missions there.

Spirit spent 2008 on the northern edge of Home Plate, a flat-topped deposit about the size of a baseball
field, composed of hardened ash and rising about 1.5 meters (5 feet) above the ground around it. There,
the north-facing tilt positioned Spirit's solar arrays to catch enough sunshine for the rover to survive the
six-month-long Martian winter.

The scientists and engineers who operate the rovers chose as 2009 destinations a steep mound called
"Von Braun" and an irregular, 45-meter-wide (150-foot-wide) bowl called "Goddard." These side-by-
side features offer a promising area to examine while energy is adequate during the Martian summer and
also to provide the next north-facing winter haven beginning in late 2009. Von Braun and Goddard
intrigue scientists as sites where Spirit may find more evidence about an explosive mix of water and
volcanism in the area's distant past. They are side-by-side, about 200 meters, or yards, south of where
Spirit is now.

It's mid-spring now in the southern hemisphere of Mars. The sun has climbed higher in the sky over
Spirit in recent weeks.

The rover team tried to drive Spirit onto Home Plate, heading south toward Von Braun and Goddard.
They tried this first from partway up the slope where the rover had spent the winter. Only five of the six
wheels on Spirit have been able to rotate since the right-front wheel stopped working in 2006. With five-
wheel drive, Spirit couldn't climb the slope. In January and February, Spirit descended from Home Plate
and drove eastward about 15 meters (about 50 feet) toward a less steep on-ramp. Spinning wheels in
loose soil led the rover team to choose another of its options.

"Spirit could not make progress in the last two attempts to get up onto Home Plate," said John Callas of
NASA's Jet Propulsion Laboratory, Pasadena, Calif., project manager for both rovers. "Alternatively, we
are driving Spirit around Home Plate to the east. Spirit will have to go around a couple of small ridges
that extend to the northeast, and then see whether a route east of Home Plate looks traversable. If that
route proves not to be traversable, a route around the west side of Home Plate is still an option."

During the drive eastward just north of Home Plate in January, Spirit stopped to use tools on its robotic
arm to examine a nodular, heavily eroded outcrop dubbed "Stapledon," which had caught the eye of
rover-team scientist Steve Ruff when he looked at images and infrared spectra Spirit took from its
winter position.

"It looked like the material east of Home Plate that we found to be rich in silica," said Ruff, of Arizona
State University, Tempe. "The silica story around Home Plate is the most important finding of the Spirit
mission so far with regard to habitability. Silica this concentrated forms around hot springs or steam
vents, and both of those are favorable environments for life on Earth."

Sure enough, Spirit's alpha particle X-ray spectrometer found Stapledon to be rich in silica, too.

"Now we have found silica on a second side of Home Plate, expanding the size of the environment we
know was affected by hot springs or steam vents," Ruff said. "The bigger this system, the more water
was involved, the more habitable this system may have been."

The contact measurement with the X-ray spectrometer also gave the team confidence in its ability to
identify silica-rich outcrops from a distance with the rover's thermal emission spectrometer, despite some
dust that has accumulated on a periscope mirror of that instrument. Researchers plan to use Spirit's
thermal emission spectrometer and panoramic camera to check for more silica-rich outcrops on the route
to Von Braun and Goddard. However, the team has set a priority to make good progress toward those
destinations. Winds cleaned some dust off Spirit's solar panels on Feb. 6 and Feb. 14, resulting in a
combined increase of about 20 percent in the amount of power available to the rover.

Opportunity, meanwhile, shows signs of increased friction in its right-front wheel. The team is driving
the rover backwards for a few sols, a technique that has helped in similar situations in the past,
apparently by redistributing lubricant in the wheel. Opportunity's major destination is Endeavour Crater,
about 22 kilometers (14 miles) in diameter and still about 12 kilometers (7 miles) away to the southeast.
Opportunity has been driving south instead of directly toward Endurance, to swing around an area
where loose soil appears deep enough to potentially entrap the rover.

JPL, a division of the California Institute of Technology, Pasadena, manages the Mars Exploration
Rovers for the NASA Science Mission Directorate, Washington. More information about the rovers is at
http://www.nasa.gov/rovers .

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NASA's Kepler Mission Set For Launch

MEDIA RELATIONS OFFICE
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Whitney Clavin 818-354-4673/818-458-9008
Jet Propulsion Laboratory, Pasadena, Calif.
whitney.clavin@jpl.nasa.gov

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

Michael Mewhinney 650-604-3937
Ames Research Center, Moffett Field, Calif.
michael.s.mewhinney@nasa.gov

NEWS RELEASE: 2009-040

NASA's Kepler Mission Set For Launch March 5, 2009

PASADENA, Calif. -- NASA's Kepler mission to seek other Earth-like planets is undergoing final
preparations for liftoff Friday, March 6, from Pad 17-B at Cape Canaveral Air Force Station in
Florida. The spacecraft launch aboard a Delta II rocket has two windows of opportunity Friday,
from 7:49 to 7:52 p.m. PST (10:49 to 10:52 p.m. EST) and 8:13 to 8:16 p.m. PST (11:13 to 11:16
p.m. EST).

Kepler is designed to find the first Earth-size planets orbiting stars in habitable zones -- regions
where water could pool on the surface of the planets. Liquid water is believed to be essential for the
formation of life.

"This mission attempts to answer a question that is as old as time itself -- are other planets like ours
out there?" said Ed Weiler, associate administrator for NASA's Science Mission Directorate at
NASA Headquarters in Washington. "It's not just a science question -- it's a basic human question."

After the clock ticks down to liftoff, the Delta II's first-stage main engine and six strap-on solid
rocket boosters will ignite. Three remaining boosters will ignite 65.5 seconds later, and the first-stage
main engine will continue to burn for 4.5 minutes. The second stage will then ignite, carrying Kepler
into a circular orbit about 185 kilometers (115 miles) above Earth less than 10 minutes after launch.
After coasting for 43 minutes, the second-stage engine will fire again, followed by second-stage
shutdown and separation. The third stage will then burn for five minutes.

Sixty-two minutes after launch, Kepler will have separated entirely from its rocket and will be in its
final Earth-trailing orbit around the sun, an orbit similar to that of NASA's Spitzer Space Telescope.
"We are very excited to see this magnificent spacecraft come to life when it reaches space," said
James Fanson, Kepler project manager at NASA's Jet Propulsion Laboratory, Pasadena, Calif.

After a commissioning period lasting about two months, Kepler will begin its job of staring at more
than 100,000 stars for three-and-one-half years, looking for planets. Its isolated perch behind Earth
will give the telescope an unobstructed view of a single, very large patch of sky near the Cygnus and
Lyra constellations.

"We will monitor a wide range of stars; from small cool ones, where planets must circle closely to
stay warm, to stars bigger and hotter than the sun, where planets must stay well clear to avoid being
roasted," said William Borucki, science principal investigator for the mission at NASA's Ames
Research Center at Moffett Field, Calif. Borucki has been working on the mission for 17 years.
"Everything about the mission is optimized to find Earth-size planets with the potential for life, to
help us answer the question -- are Earths bountiful or is our planet unique?"

Kepler will find planets by looking for periodic dips in starlight. Planets that happen to pass directly
in front of their stars from Earth's point of view cause the stars to dim by almost imperceptible
amounts. Kepler's powerful camera, the largest ever flown in space, can see the faintest of these
"winks."

"Trying to detect Jupiter-size planets crossing in front of their stars is like trying to measure the effect
of a mosquito flying by a car's headlight," said Fanson. "Finding Earth-sized planets is like trying to
detect a very tiny flea in that same headlight."

If the mission does find Earth-size planets in the habitable zones of stars, it should find them first
around stars that are smaller than our sun. This is because the habitable zone is closer for small stars;
planets circling in this region would take less time to complete one lap and, theoretically, less time for
Kepler to find them and for other ground-telescopes to confirm their existence. Any Earth-size
planets orbiting in the habitable zones of stars like our sun -- the true Earth analogs -- would take at
least three years to be confirmed.

Kepler is a NASA Discovery mission. The NASA Ames Research Center, Moffett Field, Calif., is
the home organization of the science principal investigator and is responsible for the ground system
development, mission operations and science data analysis. Kepler mission development is managed
by NASA's Jet Propulsion Laboratory, Pasadena, Calif. Ball Aerospace & Technologies Corporation
of Boulder, Colo., is responsible for developing the Kepler flight system and supporting mission
operations.

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

For more information about the Kepler mission, visit: http://www.nasa.gov/kepler .

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Wednesday, March 4, 2009

Scientists Expose 'Buried' Fault That Caused Deadly 2003 Quake

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

Iqbal Pittalwala 951-827-6050
University of California, Riverside
iqbal@ucr.edu

Robert Sanders 510-643-6998
University of California, Berkeley
rsanders@berkeley.edu

NEWS RELEASE: 2009-039 March 4, 2009

Scientists Expose 'Buried' Fault That Caused Deadly 2003 Quake

PASADENA, Calif. – Using satellite radar data, NASA-funded scientists have observed, for the
first time, the healing of subtle, natural surface scars from an earthquake that occurred on a "buried"
fault several miles below the surface--a fault whose fractures are not easily observed at Earth's
surface.

Reporting in the March 5 issue of Nature, geophysicist Eric Fielding of NASA's Jet Propulsion
Laboratory in Pasadena, Calif., describes how so-called "buried" faults are not so hidden after all.
Using the magnitude 6.6 earthquake that devastated Bam, Iran, in 2003 as a case study, Fielding and
his university colleagues analyzed radar images from the European Space Agency's Envisat satellite
to study the land surface above a fault that is buried about 1 kilometer (half a mile) under Earth's
surface. They discovered a shallow, narrow surface depression that formed and evolved after the
quake, which killed more than 30,000 people.

The results have implications for assessing the risk of future earthquakes associated with known
buried faults, which can be found around the world but are often missed by geologists or assumed
not to be active. Buried faults are thought to be responsible for the major 1992 Landers and 1999
Hector Mine earthquakes in Southern California.

Previous seismic and satellite studies showed that the fault under Bam had slipped by about 2 to 3
meters (6.6 to 9.8 feet) at the time of the earthquake. But when scientists from Iran went out in the
field after the earthquake, the cracks they found at the surface only showed 25 centimeters (9.8
inches) of slip or less. If indeed there had been 2 to 3 meters of slip at depth, the surface must have
somehow absorbed that slip.

Fielding and colleagues suspected the fault zone below could reveal itself in a slight deformation of
Earth's surface because the pressure and stress during an earthquake causes rocks in the fault zone to
expand and become more porous. After the quake, the ground will "heal" over a period of years,
settling and forming a depression.

To investigate the extent and rate of surface deformation after the 2003 earthquake, the researchers
turned to the Advanced Synthetic Aperture Radar instrument on Envisat. Researchers use images
from that instrument to precisely measure elevation by bouncing a beam of microwave radiation off
Earth's surface and observing the reflection back to the satellite. Fielding and colleagues then
compared images from the 3.5 years following the Bam quake to see how the surface elevation
changed, using a technique known as interferometric synthetic aperture radar, or InSAR.

"The advantage of InSAR is that you get a map of the pattern," said Fielding, "whereas a single
surveying station on the ground would just reveal that something funny was going on at one place."

Indeed, InSAR revealed a shallow, ditch-like depression on the surface -- measuring between 200 to
400 meters (219 to 437 yards) wide and about 3 centimeters (1.2 inches) deep -- directly above the
ruptured fault. "Using InSAR, we know that the deformation and the earthquake are associated," he
said. "The depression deepened for at least 3.5 years after the earthquake."

The team also modeled the sinking throughout the fault zone, using a model that is normally used to
study crustal compaction and expansion around volcanoes. By analyzing an array of points along the
fault to estimate how compaction produced the features at the surface, the researchers concluded
that the 2 to 3 meters of slip at depth was absorbed by a "damage zone," close to Earth's surface.
This means that the earthquake slip was spread over a wide volume of rock in the surface layers
instead of a single fault.

"There's a big, crushed-up mass of the rock that absorbs this slip that occurred at depth, and it is only
visible at the surface as a subtle deformation after the earthquake," Fielding said.

The study is helping the researchers anticipate the future behavior of the fault. Initially, they were
concerned that if stress at depth was not relieved at the surface, then a subsequent earthquake could
result. Because the rupture's stress was absorbed in the damage zone, the researchers believe the fault
that shook Bam in 2003 is no longer a risk.

"There's always the chance that a nearby, related fault could rupture, as eastern Iran is full of faults
that are active at some scale," Fielding said. "But this one beneath Bam is the type that ruptures
every 2,000 years or longer, and the stress on it seems to have been relieved."

Other researchers on the study include Paul Lundgren of JPL; Roland Bürgmann of the University
of California, Berkeley; and Gareth Funning of the University of California, Riverside.

NASA is studying designs for a future Earth observation mission called Deformation, Ecosystem
Structure and Dynamics of Ice. A key objective of the mission would be to enable InSAR
measurements of deformation on fault zones around the world to better understand the processes
that cause earthquakes.

JPL is managed for NASA by the California Institute of Technology in Pasadena.

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Flight Team to Check Status of Backup System

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

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif. March 4, 2009
guy.webster@jpl.nasa.gov

Flight Team to Check Status of Backup System

Mars Odyssey Mission Status Report

PASADENA, Calif. -- The team operating NASA's Mars Odyssey orbiter plans a procedure
next week to address a long-known, potential vulnerability of accumulated memory
corruption.

The procedure requires rebooting the spacecraft's computer. This is not a risk-free event, but
the Odyssey team and NASA have carefully weighed the risks of performing a cold reboot
compared with the risk of doing nothing, and determined that the proper course of action is to
proceed with the reboot.

The chief concern about the potential memory vulnerability stems from the length of time that
the spacecraft has been exposed to the accumulated effects of the space radiation environment
since the last reboot, which occurred on Oct. 31, 2003.

As an additional benefit, the cold-reboot procedure will demonstrate whether Odyssey's
onboard backup systems will be available should they ever be required.

"We have lost no functionality, but there would be advantages to knowing whether the B side
is available," said Odyssey Mission Manager Gaylon McSmith of NASA's Jet Propulsion
Laboratory, Pasadena, Calif. "We have developed a careful plan for attempting to determine
that."

In all the years since its April 7, 2001, launch, Odyssey has not needed to use its set of spare
components. The spares are called the spacecraft's "B side," which includes an identical set of
a computer processor, navigation sensors, relay radio and other subsystems. To use any of
them, Odyssey would have to shift to all of them at once from its primary set of components,
called the "A side."

On March 21, 2007, the B-side spare of an electronic component for managing the distribution
of power, called the high-efficiency power supply, became inoperable. If it is permanently
disabled, then none of the B side is available for use. Engineers have investigated the
inoperability of the B-side high-efficiency power supply. They concluded that the component
can probably be made to work properly again by rebooting the orbiter's computer, although the
memory-vulnerability issue that is the current concern is not directly related to the March 2007
event that affected the power supply.

Odyssey is in the third two-year extension of its mission at Mars. Some A-side components,
such as the UHF radio used for communications with spacecraft on the surface of Mars, have
worked as long as they were designed to last.

In addition to its own major scientific discoveries and continuing studies of the planet, the
Odyssey mission has played important roles in supporting the missions of the Mars rovers
Spirit and Opportunity and the Phoenix Mars Lander.

JPL, a division of the California Institute of Technology, Pasadena, manages Mars Odyssey
for the NASA Science Mission Directorate, Washington. Lockheed Martin Space Systems,
Denver, is the prime contractor for the project and built the spacecraft. Additional information
about Odyssey is at http://www.nasa.gov/mission_pages/odyssey .

#2009-038
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Tuesday, March 3, 2009

NASA Announces Mishap Board Members for Oco Investigation

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIFORNIA 91109. TELEPHONE 818-354-5011

Katherine Trinidad 202-358-1100
NASA Headquarters, Washington
katherine.trinidad@nasa.gov

RELEASE: 2009-036 March 3, 2009

NASA Announces Mishap Board Members for OCO Investigation

PASADENA, Calif. - NASA has selected the members of the board that will investigate the
unsuccessful launch of the Orbiting Carbon Observatory on Feb. 24. Rick Obenschain, deputy
director at NASA's Goddard Space Flight Center in Greenbelt, Md., will lead the mishap
investigation board.

The board consists of four other voting members:
-- Jose Caraballo, safety manager at NASA's Langley Research Center in Hampton, Va.
-- Patricia Jones, acting chief of the Human Systems Integration Division in the Exploration
Technology Directorate at NASA's Ames Research Center at Moffett Field, Calif.
-- Richard Lynch, Aerospace Systems Engineering, Goddard Space Flight Center
-- Dave Sollberger, deputy chief engineer of the NASA Launch Services Program at NASA's
Kennedy Space Center in Florida.

The ex officio member is Ruth Jones, Safety and Mission Assurance manager at NASA's Marshall
Space Flight Center in Huntsville, Ala. The ex officio member assures board activity conforms to
NASA procedural requirements.

The board began its investigation March 3. The members will gather information, analyze the facts
and identify the failure's cause or causes and contributing factors. The board will make
recommendations for actions to prevent a similar incident.

The Orbiting Carbon Observatory satellite failed to reach orbit after its 1:55 a.m. PST liftoff Feb. 24
from California's Vandenberg Air Force Base.

For information about the Orbiting Carbon Observatory failed launch and investigation, visit:
http://www.nasa.gov/oco .

NASA's Jet Propulsion Laboratory, Pasadena, Calif., has managed the Orbiting Carbon Observatory
mission for NASA's Science Mission Directorate, Washington. JPL is managed for NASA by the
California Institute of Technology in Pasadena.

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Newfound Moon May Be Source of Outer Saturn Ring

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
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NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
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Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
carolina.martinez@jpl.nasa.gov

Joe Mason 720-974-5859
Space Science Institute, Boulder, Colo.
media@ciclops.org

NEWS RELEASE: 2009-035 March 3, 2009

Newfound Moon May Be Source of Outer Saturn Ring

NASA's Cassini spacecraft has found within Saturn's G ring an embedded moonlet that
appears as a faint, moving pinprick of light. Scientists believe it is a main source of the G
ring and its single ring arc.

Cassini imaging scientists analyzing images acquired over the course of about 600 days
found the tiny moonlet, half a kilometer (about a third of a mile) across, embedded within
a partial ring, or ring arc, previously found by Cassini in Saturn's tenuous G ring.

The finding is being announced today in an International Astronomical Union circular.
Images can be found at http://www.nasa.gov/cassini, http://saturn.jpl.nasa.gov and
http://ciclops.org .

"Before Cassini, the G ring was the only dusty ring that was not clearly associated with a
known moon, which made it odd," said Matthew Hedman, a Cassini imaging team
associate at Cornell University in Ithaca, N.Y. "The discovery of this moonlet, together
with other Cassini data, should help us make sense of this previously mysterious ring."

Saturn's rings were named in the order they were discovered. Working outward they are:
D, C, B, A, F, G and E. The G ring is one of the outer diffuse rings. Within the faint G
ring there is a relatively bright and narrow, 250-kilometer-wide (150-miles) arc of ring
material, which extends 150,000 kilometers (90,000 miles), or one-sixth of the way
around the ring's circumference. The moonlet moves within this ring arc. Previous Cassini
plasma and dust measurements indicated that this partial ring may be produced from
relatively large, icy particles embedded within the arc, such as this moonlet.

Scientists imaged the moonlet on Aug. 15, 2008, and then they confirmed its presence by
finding it in two earlier images. They have since seen the moonlet on multiple occasions,
most recently on Feb. 20, 2009. The moonlet is too small to be resolved by Cassini's
cameras, so its size cannot be measured directly. However, Cassini scientists estimated
the moonlet's size by comparing its brightness to another small Saturnian moon, Pallene.

Hedman and his collaborators also have found that the moonlet's orbit is being disturbed
by the larger, nearby moon Mimas, which is responsible for keeping the ring arc together.

This brings the number of Saturnian ring arcs with embedded moonlets found by Cassini
to three. The new moonlet may not be alone in the G ring arc. Previous measurements
with other Cassini instruments implied the existence of a population of particles, possibly
ranging in size from 1 to 100 meters (about three to several hundred feet) across.
"Meteoroid impacts into, and collisions among, these bodies and the moonlet could
liberate dust to form the arc," said Hedman.

Carl Murray, a Cassini imaging team member and professor at Queen Mary, University of
London, said, "The moon's discovery and the disturbance of its trajectory by the
neighboring moon Mimas highlight the close association between moons and rings that
we see throughout the Saturn system. Hopefully, we will learn in the future more about
how such arcs form and interact with their parent bodies."

Early next year, Cassini's camera will take a closer look at the arc and the moonlet. The
Cassini Equinox mission, an extension of the original four-year mission, is expected to
continue until fall of 2010.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space
Agency and the Italian Space Agency. The Jet Propulsion Laboratory (JPL), a division of
the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission
for NASA's Science Mission Directorate, Washington. The Cassini orbiter and its two
onboard cameras were designed, developed and assembled at JPL. The imaging team is
based at the Space Science Institute, Boulder, Colo.

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