W Post
 
 
NASA’s lunar probes will test theory of why one side of  the moon is 
lopsided

 
 
By _Brian Vastag_ 
(http://www.washingtonpost.com/national/brian-vastag/2011/06/02/AGMEARHH_page.html)
 , Published:  January 1, 2012

 
 
< 
She hangs there nightly, a yellow or white or spookily orange disk, the  
bringer of tides, the caster of romantic shadows. She waxes and wanes and  
sometimes she turns ruddy as the shadow of the Earth crosses her face. For all  
her beauty, though, our moon hides a lumpy, unflattering secret: She’s 
lopsided.  Her backside is much thicker than her front. And no one knows why. 
It’s unseemly, really. After more than 100 robotic and human missions to 
the  moon, scientists still can’t account for why one half — the half we can’
t see —  is taller than the other.
SA _probes_ (http://www.nasa.gov/mission_pages/grail/main/index.html)  
_that  arrived_ 
(http://www.washingtonpost.com/national/health-science/new-years-countdown-twin-nasa-probes-prepare-to-slip-into-orbit-around-the-moon/2011/1
2/28/gIQAFzQtMP_story.html)  at our satellite this weekend may finally 
reveal a shocking truth:  that early on, a smaller twin moon smushed into her. 
As this intruder splatted  into its big sister, it shattered “like a 
mega-avalanche,” said _Erik Asphaug_ (http://es.ucsc.edu/personnel/Asphaug/) , 
the 
planetary  scientist at the University of California at Santa Cruz who 
_published_ 
(http://www.nature.com/nature/journal/v476/n7358/full/nature10289.html)   the 
twin-moon idea in the journal Nature in August. His co-author was 
Martin  Jutzi of the University of Bern in Switzerland.

This collision would have spread a wide hump of rock onto the back of the  
moon. There, the material cooled and hardened into a thick crust: the 
far-side  lunar highlands. 
“This is one of those ideas that all sorts of people will try to prove  
wrong,” said _Maria Zuber_ (http://www-geodyn.mit.edu/mtz.html) , the  MIT 
scientist heading up the new NASA moon mission. “But it’s extremely  testable.” 
And so GRAIL will test it. Designed to probe the moon’s interior, the two  
washing-machine-size spacecraft will reveal the thickness of the moon’s 
crust,  its topmost layer. 
If the two-moon theory is correct, the backside crust will be much thicker  
than that of the front side. The hump should taper toward the equator. 
GRAIL could also spot another hidden feature predicted by the theory. If a  
second moon did crash into the first, the collision would have occurred 
when the  big moon was young and hot. A thin layer of molten heavy elements 
including  uranium and potassium still burbled just under the crust. 
The backside impact would have squeezed this liquid, pushing it around to 
the  front side. There it would have cooled and hardened, leaving a telltale  
layer. 
The existence of both features — a thick backside crust and a thin, dense  
layer under the front’s crust — would offer strong support for the 
twin-moon  theory, Asphaug said. 
When Zuber first heard the notion, she scoffed. “This is going to be  
nonsense,” she recalled thinking. But computer simulations run by Asphaug and  
Jutzi were compelling leading Zuber to reverse course. “It’s a plausible  
scenario,” she said. 
The idea is also simple, another stroke in its favor. By contrast, other  
explanations for the moon’s front-back discrepancy tend toward the 
complicated  and unsatisfying. 
“There are all these theories out there,” Asphaug said, “that have big 
warts  on them.” 
Such as: Maybe the front side of the moon was terribly unlucky, flattened 
by  seven or eight big space rocks. The problem: Asteroids and comets arrive 
from  all directions; there’s no reason impacts should cluster. “It’s like 
flipping a  coin and getting heads eight times,” Asphaug  said.

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