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Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.

Dwayne Brown 202-358-1726
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Peter Golkin 202-633-2374
National Air and Space Museum, Washington, D.C.                 

NEWS RELEASE: 2006-149                                   December 13, 2006

Geologists Finding a Different Mars Underneath

Mars is showing scientists its older, craggier face buried beneath the surface, 
thanks to a 
pioneering sounding radar co-sponsored by NASA aboard the European Space 
Agency's 
Mars Express orbiter.

Observations by the first project to explore a planet by sounding radar 
strongly suggest that 
ancient impact craters lie buried beneath the smooth, low plains of Mars' 
northern 
hemisphere. The technique uses echoes of waves that have penetrated below the 
surface. 

"It's almost like having X-ray vision," said Dr. Thomas R. Watters of the 
National Air and 
Space Museum's Center for Earth and Planetary Studies, Washington. "Besides 
finding 
previously unknown impact basins, we've also confirmed that some of the subtle 
topographic depressions mapped previously in the lowlands are related to impact 
features."

Studies of how Mars evolved aid understanding of early Earth. Some signs of the 
forces at 
work a few billion years ago are more evident on Mars because, on Earth, many 
of them 
have been obliterated during Earth's more active resurfacing by tectonic 
activity.

Watters and nine co-authors report the findings in the Dec. 14, 2006 issue of 
the journal 
Nature. 

The researchers used the orbiter's Mars Advanced Radar for Subsurface and 
Ionospheric 
Sounding, which was provided to the European Mars mission by NASA and the 
Italian 
Space Agency. The instrument transmits radio waves that pass through the 
Martian surface 
and bounce off features in the subsurface with electrical properties that 
contrast with those 
of materials that buried them. 

The findings bring planetary scientists closer to understanding one of the most 
enduring 
mysteries about the geologic evolution of the planet. In contrast to Earth, 
Mars shows a 
striking difference between its northern and southern hemispheres. Almost the 
entire 
southern hemisphere has rough, heavily cratered highlands, while most of the 
northern 
hemisphere is smoother and lower in elevation.

Since the impacts that cause craters can happen anywhere on a planet, the areas 
with fewer 
craters are generally interpreted as younger surfaces where geological 
processes have 
erased the impact scars. The abundance of buried craters that the radar has 
detected 
beneath Mars' smooth northern plains means the underlying crust of the northern 
hemisphere is extremely old, "perhaps as ancient as the heavily cratered 
highland crust in 
the southern hemisphere."  

Learning about the ancient lowland crust has been challenging because that 
crust was 
buried first by vast amounts of volcanic lava and then by sediments carried by 
episodic 
flood waters and wind.

Co-authors are Carl J. Leuschen, Johns Hopkins University Applied Physics 
Laboratory, 
Laurel, Md.; Jeffrey J. Plaut, Ali Safaeinili and Anton B. Ivanov of NASA's Jet 
Propulsion 
Laboratory, Pasadena, Calif.; Giovanni Picardi, "La Sapienza" University of 
Rome, Italy; 
Stephen M. Clifford, Lunar and Planetary Institute, Houston; William M. 
Farrell, NASA's 
Goddard Space Flight Center, Greenbelt, Md.; Roger J. Phillips, Washington 
State 
University, St. Louis; and Ellen R. Stofan, Proxemy Research, Laytonsville, Md.

Additional information about the Mars Advanced Radar for Subsurface and 
Ionospheric 
Sounding is available at http://www.marsis.com .  JPL, a division of the 
California Institute 
of Technology, Pasadena, manages NASA's roles in Mars Express for the NASA 
Science 
Mission Directorate, Washington. 

The Center for Earth and Planetary Studies is the scientific research unit 
within the 
Collections and Research Department of the Smithsonian Institution's National 
Air and 
Space Museum. The Center's scientists perform original research and outreach 
activities on 
topics covering planetary science, terrestrial geophysics and the remote 
sensing of 
environmental change.

-end-




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