NASA’s InSight lander
Solok Why in news? InSight detected seismic and acoustic waves from the impact of four meteorites and calculated the location of the craters they left.
- 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 neighbours.
- Scientists are now gaining a fuller understanding of this Martian trait, with help from NASA’s robotic InSight lander.
- Researchers 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.
- 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.
How is this detection useful?
- 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.
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.
- 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.