These craters were formed by a Sept. 5,
2021, meteoroid impact on Mars, the first to be detected by NASA’s InSight.
Taken by NASA’s Mars Reconnaissance Orbiter, this enhanced-color image
highlights the dust and soil disturbed by the impact in blue in order to make
details more visible to the human eye. Credits: NASA/JPL-Caltech/University
of Arizona
The Mars lander’s seismometer has picked
up vibrations from four separate impacts in the past two years.
NASA’s InSight lander has detected seismic
waves from four space rocks that crashed on Mars in 2020 and 2021. Not only do
these represent the first impacts detected by the spacecraft’s seismometer
since InSight touched down on the Red Planet in 2018, it also marks the first
time seismic and acoustic waves from an impact have been detected on Mars.
A new paper published Monday in Nature Geoscience details the impacts, which ranged
between 53 and 180 miles (85 and 290 kilometers) from InSight’s location, a
region of Mars called Elysium Planitia.
The first of the four confirmed meteoroids
– the term used for space rocks before they hit the ground – made the most
dramatic entrance: It entered Mars’ atmosphere on Sept. 5, 2021, exploding into
at least three shards that each left a crater behind.
Learn more about the first meteoroid impact NASA’s InSight lander detected on Mars in this video. Credits: NASA/JPL-Caltech
Then, NASA’s Mars Reconnaissance Orbiter flew over the estimated impact site
to confirm the location. The orbiter used its black-and-white Context Camera to
reveal three darkened spots on the surface. After locating these spots, the
orbiter’s team used the High-Resolution Imaging Science Experiment camera,
or HiRISE, to get a color close-up of the craters
(the meteoroid could have left additional craters in the surface, but they
would be too small to see in HiRISE’s images).
“After three years of InSight waiting to detect an impact, those craters looked beautiful,” said Ingrid Daubar of Brown University, a co-author of the paper and a specialist in Mars impacts.
This collage shows three other meteoroid
impacts that were detected by the seismometer on NASA’s InSight lander and
captured by the agency’s Mars Reconnaissance Orbiter using its HiRISE camera. Credits:
NASA/JPL-Caltech/University of Arizona
After combing through earlier data,
scientists confirmed three other impacts had occurred on May 27, 2020; Feb. 18,
2021; and Aug. 31, 2021.
Researchers have puzzled over why they
haven’t detected more meteoroid impacts on Mars. The Red Planet is next to the
solar system’s main asteroid belt, which provides an ample supply of space
rocks to scar the planet’s surface. Because Mars’ atmosphere is just 1% as
thick as Earth’s, more meteoroids pass through it without disintegrating.
InSight’s seismometer has detected over 1,300 marsquakes.
Provided by France’s space agency, the Centre National d’Études Spatiales, the
instrument is so sensitive that it can detect seismic waves from thousands of
miles away. But the Sept. 5, 2021, event marks the first time an impact was
confirmed as the cause of such waves.
InSight’s team suspects that other impacts
may have been obscured by noise from wind or by seasonal changes in the
atmosphere. But now that the distinctive seismic signature of an impact on Mars
has been discovered, scientists expect to find more hiding within InSight’s
nearly four years of data.
The sound of a meteoroid striking Mars – created from data recorded by NASA’s InSight lander – is like a “bloop” due to a peculiar atmospheric effect. In this audio clip, the sound can be heard three times: when the meteoroid enters the Martian atmosphere, explodes into pieces, and impacts the surface. Credit: NASA/JPL-Caltech/CNES/IPGP
Science
Behind the Strikes
Seismic data offer various clues that will
help researchers better understand the Red Planet. Most marsquakes are caused
by subsurface rocks cracking from heat and pressure. Studying how the resulting
seismic waves change as they move through different material provides
scientists a way to study Mars’ crust,
mantle, and core.
The four meteoroid impacts confirmed so
far produced small quakes with a magnitude of no more than 2.0. Those smaller
quakes provide scientists with only a glimpse into the Martian crust, while
seismic signals from larger quakes, like the magnitude 5
event that occurred in May 2022,
can also reveal details about the planet’s mantle and core.
But the impacts will be critical to
refining Mars’ timeline. “Impacts are the clocks of the solar system,” said the
paper’s lead author, Raphael Garcia of Institut Supérieur de l’Aéronautique et
de l’Espace in Toulouse, France. “We need to know the impact rate today to
estimate the age of different surfaces.”
Read postcards people have sent to
InSight
Scientists can
approximate the age of a planet’s surface by counting its impact craters: The
more they see, the older the surface. By calibrating their statistical models
based on how often they see impacts occurring now, scientists can then estimate
how many more impacts happened earlier in the solar system’s history.
InSight’s data, in combination with
orbital images, can be used to rebuild a meteoroid’s trajectory and the size of
its shock wave. Every meteoroid creates a shock wave as it hits the atmosphere
and an explosion as it hits the ground. These events send sound waves through
the atmosphere. The bigger the explosion, the more this sound wave tilts the
ground when it reaches InSight. The lander’s seismometer is sensitive enough to
measure how much the ground tilts from such an event and in what direction.
“We’re learning more about the impact
process itself,” Garcia said. “We can match different sizes of craters to
specific seismic and acoustic waves now.”
The lander still has time to study Mars. Dust buildup on the lander’s solar panels is reducing its power and will eventually lead to the spacecraft
shutting down. Predicting precisely when is difficult, but based on the latest
power readings, engineers now believe the lander could shut down between
October of this year and January 2023.
More
About the Mission
NASA’s Jet Propulsion Laboratory, a
division of Caltech in Pasadena, California, manages InSight for the agency’s
Science Mission Directorate in Washington. InSight is part of NASA’s Discovery
Program, managed by the agency’s Marshall Space Flight Center in Huntsville,
Alabama. Lockheed Martin Space in Denver built the InSight spacecraft,
including its cruise stage and lander, and supports spacecraft operations for
the mission.
A number of European partners, including France’s Centre National d’Études Spatiales (CNES) and the German Aerospace Center (DLR), are supporting the InSight mission. CNES provided the Seismic Experiment for Interior Structure (SEIS) instrument to NASA, with the principal investigator at IPGP (Institut de Physique du Globe de Paris). Significant contributions for SEIS came from IPGP; the Max Planck Institute for Solar System Research (MPS) in Germany; the Swiss Federal Institute of Technology (ETH Zurich) in Switzerland; Imperial College London and Oxford University in the United Kingdom; and JPL. DLR provided the Heat Flow and Physical Properties Package (HP3) instrument, with significant contributions from the Space Research Center (CBK) of the Polish Academy of Sciences and Astronika in Poland. Spain’s Centro de Astrobiología (CAB) supplied the temperature and wind sensors.
Source: NASA’s
InSight ‘Hears’ Its First Meteoroid Impacts on Mars | NASA
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