Analysis of Marsquakes

NASA’s InSight lander has revealed the depth of Mars’s crust and the size of its central core by using data from dozens of marsquakes captured since the probe landed in 2018.

The Seismic Experiment for Interior Structure, otherwise known as the SEIS, is a dome-shaped instrument that sits on the surface of Mars on a mission to detect seismic events hundreds or even thousands of miles away. Since its deployment, the instrument has been busy recording over 700 marsquakes.

NASA's analysis shows that the Martian crust is between 12 and 23 miles (20-37km) thick. Below this is the mantle, which extends about 970 miles down to the Martian core, which has been revealed to have a radius of 1,137 miles.

Earth’s crust is also about 22 miles thick but our planet is 1.8 times larger than Mars. In terms of percentages, the Martian mantle and core are similar to the Earth’s at around 45 percent and 54 percent of the planet’s radius respectively.

Mars is only the third celestial object, after Earth and the moon, to have these measurements made. A key finding is that the Martian core is still molten; most scientists had assumed it would be solid.