Scientists surprised by source of largest quake detected on Mars
The planet Mars is shown in this NASA Hubble Space Telescope view taken May 12, 2016. NASA/Handout via Reuters /File Photo
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On
May 4, 2022, NASA's InSight lander detected the largest quake yet recorded on
Mars, one with a 4.7 magnitude - fairly modest by Earth standards but strong
for our planetary neighbour.
Given
Mars lacks the geological process called plate tectonics that generates
earthquakes on our planet, scientists suspected a meteorite impact had caused
this marsquake.
But
a search for an impact crater came up empty, leading scientists to conclude
that this quake was caused by tectonic activity - rumbling in the planet's
interior - and giving them a deeper understanding of what makes Mars shake,
rattle and roll.
"We
concluded that the largest marsquake seen by InSight was tectonic, not an
impact. This is important as it shows the faults on Mars can host hefty
marsquakes," said planetary scientist Ben Fernando of the University of
Oxford in England, lead author of the research published this week in the
journal Geophysical Research Letters. "We really thought that this event
might be an impact."
"This
represents a significant step forward in our understanding of Martian seismic
activity and takes us one step closer to better unravelling the planet's
tectonic processes," added Imperial College London planetary scientist and
study co-author Constantinos Charalambous, co-chair of InSight's Geology
Working Group.
NASA
retired InSight in 2022 after four years of operations. In all, InSight's
seismometer instrument detected 1,319 marsquakes.
Earth's
crust - its outermost layer - is divided into immense plates that continually
shift, triggering quakes. The Martian crust is a single solid plate. But that
does not mean all is quiet on the Martian front.
"There
are still faults that are active on Mars. The planet is still slowly shrinking
and cooling, and there is still motion within the crust even though there are
no active plate tectonic processes going on anymore. These faults can trigger
quakes," Fernando said.
The
researchers determined that the 4.7 magnitude quake was centered in the
Al-Qahira Vallis region in the Martian southern hemisphere, roughly 1,200 miles
(2,000 km) southeast of InSight's location just north of the equator. They
think it originated perhaps a few dozen miles (km) below the surface.
"Most
of the marsquakes we've detected thus far have been associated with a region
called Cerberus Fossae, located eastward of InSight. Conversely, the origin of
this one left us puzzled, as no discernible surface features indicated ongoing
tectonic processes as a likely cause, particularly ones that would cause such a
powerful quake," Charalambous added.
The
energy it released surpassed the cumulative energy from all the other
marsquakes InSight recorded. The researchers initially noted similarities in
its seismic signature to two meteorite impacts detected by InSight that gouged
craters roughly 500 feet (150 meters) wide.
They
enlisted the various space agencies with spacecraft monitoring the Martian
surface - the European, U.S., Chinese, Indian and United Arab Emirates agencies
- to check for evidence of an impact on the day of the quake. No luck.
"The
absence of a crater in our image search for this large marsquake represents a
significant milestone in interpreting seismic signals on Mars,"
Charalambous said.
With
future human missions to Mars in mind, a greater understanding of Martian
seismic activity is pertinent.
"On
Earth, a quake of this size would probably break windows, shake things off
shelves, etc., but would not bring the house down," Fernando said.
Charalambous
said the location of the majority of the marsquakes detected by InSight
remained uncertain, with a poor understanding of the mechanisms that triggered
them.
"Each
seismic event detected by InSight is a valuable piece of the puzzle, but this
particular event plays a crucial role in unveiling the Red Planet's geological
history, shedding light on its interior and evolution," Charalambous said.
"Furthermore, it provides essential insights into the distribution of seismic activity on Mars, which is a vital consideration for planning future human missions to the planet."


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