WASHINGTON:
Mars' largest moon, Phobos, is slowly falling towards the planet and is
likely to be shredded into pieces that will be strewn about the red
planet in a ring like those encircling Saturn and Jupiter, scientists,
including one of Indian-origin, say.
The demise of Phobos will
probably happen in 20 to 40 million years, leaving a ring that will
persist for anywhere from one million to 100 million years. Postdoctoral
fellow Benjamin Black and graduate student Tushar Mittal estimate the
cohesiveness of Phobos and conclude that it is insufficient to resist
the tidal forces that will pull it apart when it gets closer to Mars.
Just as Earth's moon pulls on our planet in different directions,
raising tides in the oceans, Mars too tugs differently on different
parts of Phobos. As Phobos gets closer to the planet, the tugs are
enough to actually pull the moon apart, the scientists say. This is
because Phobos is highly fractured, with lots of pores and rubble.
While the largest chunks would eventually spiral into the planet and
collide at a grazing angle to produce eggshaped craters, the majority of
the debris would circle the planet for millions of years until these
pieces, too, drop onto the planet in `moon' showers, like meteor
showers.Only Mars' other moon, Deimos, would remain.
"While our
moon is moving away from Earth at a few centimetres per year, Phobos is
moving towards Mars at a few centimetres per year, so it is almost
inevitable that it will either crash into Mars or break apart," Black
said. PTI
UV rays wiped out carbon from Red planet
Scientists have found that UV rays from Sun caused Mars to lose its
atmospheric carbon dioxide. Mars is blanketed by a carbon dioxide
atmosphere that is too thin to keep water from freezing or quickly
evaporating. However, scientists have concluded that ancient Mars was
once a warmer, wetter place than today.
But scientists have
been puzzled by why they have not found more carbon -in the form of
carbonate -in Martian rocks.Scientists suggest that 3.8 billion years
ago, Mars might have had a moderately dense atmosphere. Such an
atmosphere could have evolved into the thin one, not only minus the
"missing" carbon problem, but also consistent with the observed ratio of
carbon-13 to carbon-12, which differ by number of neutrons in the
nucleus.
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