[FPSPACE] Lunar Topsy-Turviness
Jens Kieffer-Olsen
dstdba at post4.tele.dk
Mon May 4 20:35:31 EDT 2009
It's common knowledge that the Moon is tidally locked
to the Earth making its far side an enigma to mankind,
until Russian scientists almost 50 years ago published
photos taken by Luna 3 that revealed new craters, such
as the one aptly named Циолковский in honour of the
visionary space age pioneer.
However, a recent study points to the lunar farside
having actually faced Earth a long time ago. But then
a sudden switch-around occurred as a result of a hit
from an asteroid.
From Cosmos Online, January 2009
http://www.cosmosmagazine.com/news/2493/moons-backside-may-once-have-faced-e
arth
we learn:
[ ... ] new study, detailed this month in the journal
Icarus, Wieczorek and Le Feuvre scoured images of the
Moon's cratering patterns.
Recent work has suggested that as the Moon orbits Earth,
its leading side - the western hemisphere - is 30 per cent
more likely to get hit by asteroids that the other. "It's
really like a car moving through the rain, there'd be more
rain falling on the front windscreen than the back,"
explained Wieczorek.
The researchers compared the ages of craters across the
surface. As expected, that the younger asteroid impacts
were on the western side. But to their surprise, the oldest
craters were on the eastern side - the back windscreen -
suggesting that the Moon's orientation may once have been
reversed.
The age of the craters was estimated by measured by looking
at layers of debris thrown out from multiple impacts, and
also by the number of craters superimposed on top of one
another.
But where's the evidence for a massive Moon-flipping
asteroid impact? Wieczorek claims there are six giant
basins that could mark the site of the blow.
The current favourite is the Smythii basin that lies on
the Moon's equator "so it would have more ability to
spin up the Moon than, say, if it was on the north pole."
The experts estimates the direct hit at over 3.9 billion
years ago.
--
Jens Kieffer-Olsen
Slagelse, Denmark
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