NASA's InSight lander detects space rocks as they slam into Mars
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[September 20, 2022]
By Will Dunham
WASHINGTON (Reuters) - Mars, by virtue of
its tenuous atmosphere and proximity to our solar system's asteroid
belt, is far more vulnerable than Earth to being struck by space rocks -
one of the many differences between the two planetary neighbors.
Scientists are now gaining a fuller understanding of this Martian trait,
with help from NASA's robotic InSight lander. Researchers on Monday
described how InSight detected seismic and acoustic waves from the
impact of four meteorites and then calculated the location of the
craters they left - the first such measurements anywhere other than
Earth.
The researchers used observations from NASA's Mars Reconnaissance
Orbiter in space to confirm the crater locations.
"These seismic measurements give us a completely new tool for
investigating Mars, or any other planet we can land a seismometer on,"
said planetary geophysicist Bruce Banerdt of NASA's Jet Propulsion
Laboratory, the InSight mission's principal investigator.
The space rocks InSight tracked - one landing in 2020 and the other
three in 2021 - were relatively modest in size, estimated to weigh up to
about 440 pounds (200 kg), with diameters of up to about 20 inches (50
cm) and leaving craters of up to about 24 feet (7.2 meters) wide. They
landed between 53 miles (85 km) and 180 miles (290 km) from InSight's
location. One exploded into at least three pieces that each gouged their
own craters.
"We can connect a known source type, location and size to what the
seismic signal looks like. We can apply this information to better
understand InSight's entire catalog of seismic events, and use the
results on other planets and moons, too," said Brown University
planetary scientist Ingrid Daubar, a co-author of the study published in
the journal Nature Geoscience.
The researchers believe that now the seismic signature of such impacts
has been discovered they expect to find more contained in InSight's
data, going back to 2018.
The three-legged InSight - its name is short for Interior Exploration
Using Seismic Investigations, Geodesy and Heat Transport - landed in
2018 in a vast and relatively flat plain just north of the Martian
equator called Elysium Planitia.
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Craters formed by a September 5, 2021,
meteoroid impact on Mars, the first to be detected by NASA?s InSight,
are seen in an image taken by NASA?s Mars Reconnaissance Orbiter.
NASA/JPL-Caltech/University of Arizona/Handout via REUTERS. THIS
IMAGE HAS BEEN SUPPLIED BY A THIRD PARTY.
"The moon is also a target for future meteor impact detection," said
planetary scientist and study lead author Raphael Garcia of the
University of Toulouse's ISAE-SUPAERO institute of aeronautics and
space.
"And it may be the same sensors will do it, because the spare
sensors of InSight are currently integrated in the Farside Seismic
Suite instrument for a flight to the moon in 2025," Garcia added,
referring to an instrument due to be placed near the lunar south
pole on the side of the moon permanently facing away from Earth.
Mars is about twice as likely as Earth to have its atmosphere hit by
a meteoroid - the name for a space rock before it strikes the
surface. However, Earth has a much thicker atmosphere that protects
the planet.
"So meteoroids usually break up and disintegrate in the Earth's
atmosphere, forming fireballs that only rarely reach the surface to
form a crater. In comparison on Mars, hundreds of impact craters are
forming somewhere on the planet's surface every year," Daubar said.
The Martian atmosphere is only about 1% as thick as Earth's. The
asteroid belt, an abundant source of space rocks, is located between
Mars and Jupiter.
The scientific goals set for InSight ahead of the mission were to
investigate the internal structure and processes of Mars, as well as
studying seismic activity and meteorite impacts.
InSight's seismometer instrument established that Mars is
seismically active, detecting more than 1,300 marsquakes. In
research published last year, seismic waves detected by InSight
helped decipher the internal structure of Mars, including the first
estimates of the size of its large liquid metal core, thickness of
its crust, and nature of its mantle.
(Reporting by Will Dunham, Editing by Rosalba O'Brien)
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