NASA's Grail Mission Solves Mystery of Moon's Surface Gravity

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May 30, 2013

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

DC Agle 
Jet Propulsion Laboratory, Pasadena, Calif. 
818-393-9011 
agle@xxxxxxxxxxxx 

Elizabeth Gardner 
Purdue University, West Lafayette, Ind. 
765/494-2081 
ekgardner@xxxxxxxxxx 

Jennifer Chu 
Massachusetts Institute of Technology, Cambridge, Mass. 
Phone: 617-715-4531 
j_chu@xxxxxxx 


RELEASE: 13-164

NASA'S GRAIL MISSION SOLVES MYSTERY OF MOON'S SURFACE GRAVITY

PASADENA, Calif. -- NASA's Gravity Recovery and Interior Laboratory 
(GRAIL) mission has uncovered the origin of massive invisible regions 
that make the moon's gravity uneven, a phenomenon that affects the 
operations of lunar-orbiting spacecraft. 

Because of GRAIL's findings, spacecraft on missions to other celestial 
bodies can navigate with greater precision in the future. 
GRAIL's twin spacecraft studied the internal structure and composition 
of the moon in unprecedented detail for nine months. They pinpointed 
the locations of large, dense regions called mass concentrations, or 
mascons, which are characterized by strong gravitational pull. 
Mascons lurk beneath the lunar surface and cannot be seen by normal 
optical cameras. 

GRAIL scientists found the mascons by combining the gravity data from 
GRAIL with sophisticated computer models of large asteroid impacts 
and known detail about the geologic evolution of the impact craters. 
The findings are published in the May 30 edition of the journal 
Science. 

"GRAIL data confirm that lunar mascons were generated when large 
asteroids or comets impacted the ancient moon, when its interior was 
much hotter than it is now," said Jay Melosh, a GRAIL co-investigator 
at Purdue University in West Lafayette, Ind., and lead author of the 
paper. "We believe the data from GRAIL show how the moon's light 
crust and dense mantle combined with the shock of a large impact to 
create the distinctive pattern of density anomalies that we recognize 
as mascons." 

The origin of lunar mascons has been a mystery in planetary science 
since their discovery in 1968 by a team at NASA's Jet Propulsion 
Laboratory (JPL) in Pasadena, Calif. Researchers generally agree 
mascons resulted from ancient impacts billions of years ago. It was 
not clear until now how much of the unseen excess mass resulted from 
lava filling the crater or iron-rich mantle upwelling to the crust. 

On a map of the moon's gravity field, a mascon appears in a target 
pattern. The bulls-eye has a gravity surplus. It is surrounded by a 
ring with a gravity deficit. A ring with a gravity surplus surrounds 
the bulls-eye and the inner ring. This pattern arises as a natural 
consequence of crater excavation, collapse and cooling following an 
impact. The increase in density and gravitational pull at a mascon's 
bulls-eye is caused by lunar material melted from the heat of a 
long-ago asteroid impact. 

"Knowing about mascons means we finally are beginning to understand 
the geologic consequences of large impacts," Melosh said. "Our planet 
suffered similar impacts in its distant past, and understanding 
mascons may teach us more about the ancient Earth, perhaps about how 
plate tectonics got started and what created the first ore deposits." 


This new understanding of lunar mascons also is expected to influence 
planetary geology well beyond that of Earth and our nearest celestial 
neighbor. 

"Mascons also have been identified in association with impact basins 
on Mars and Mercury," said GRAIL principal investigator Maria Zuber 
of the Massachusetts Institute of Technology in Cambridge. 
"Understanding them on the moon tells us how the largest impacts 
modified early planetary crusts." 

Launched as GRAIL A and GRAIL B in September 2011, the probes, renamed 
Ebb and Flow, operated in a nearly circular orbit near the poles of 
the moon at an altitude of about 34 miles (55 kilometers) until their 
mission ended in December 2012. The distance between the twin probes 
changed slightly as they flew over areas of greater and lesser 
gravity caused by visible features, such as mountains and craters, 
and by masses hidden beneath the lunar surface. 

JPL managed GRAIL for NASA's Science Mission Directorate in 
Washington. The mission was part of the Discovery Program managed at 
NASA's Marshall Space Flight Center in Huntsville, Ala. NASA's 
Goddard Space Flight Center, in Greenbelt, Md., manages the Lunar 
Reconnaissance Orbiter. Operations of the spacecraft's laser 
altimeter, which provided supporting data used in this investigation, 
is led by the Massachusetts Institute of Technology in Cambridge. 

Lockheed Martin Space Systems in Denver built GRAIL. 

For more information about GRAIL, visit: 

http://www.nasa.gov/grail 

	
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