The InSight mission was sent to Mars in 2018 with a very specific objective: to probe the interior of the Red Planet. And as surprising as it may seem, it involves, among other things, an analysis of the vibrations induced by the blowing of the winds. Researchers are now offering us, based on these data, a rather detailed map of the Martian subsoil.
. It intrigues researchers. It makes amateurs dream. And in recent years, a large number of scientific missions have gone out to meet him. They flew over it. Have put themselves in orbit around it. Or have landed on its ground. Returning to Earth a quantity of information on the or the surface of Mars. But the , which landed on the side ofElysium Planitia, a volcanic area located on the of the planet, is the first to take a specific interest in its subsoil.
Thanks to hison-board, the Seis instrument for Seismic Experiment for Interior Structure, InSight has already given scientists an idea of the size and composition of the Red Planet’s core. But also of the nature of its and the thickness of its . Today, (Switzerland) show how, by tracing the reverberations of the sound of the wind on the layers of soil and rocks, they are able to specify what the first two hundred meters of the Martian crust are made of.
The technique they used was developed for quite earthly purposes. In order to study the underground structures of the regions at risk of seismic activity. On our good old, indeed, the oceans, but also the , keep the ground shaking. And those weak jerks that can measure thanks to their most sensitive instruments constitute like imprints of what goes on in the basement.
On Mars, no oceans. A very tenuous atmosphere. With little wind, then. And a single measuring station, the. Yet the lander records have just revealed some astonishing details of the Martian subsoil, with a one meter near the surface and a few tens of meters deeper.
The mapping established by the researchers reveals an unexpected layer of 30 to 40 meters of. Their origin remains to be determined. This layer is surrounded by thick deposits of solidified. All covered with a layer of about three meters sandy. And suggesting that the story ofElysium Planitia could have been more disturbed than the did not think so until then.
Already, thanks to previous studies on nearby craters, researchers have determined that the layers of lava date from around 1.7 billion – in the middle of a rather calm, cold and dry period on Mars – and 3.6 billion in ‘years – during a period of strong. Above the youngest lava layer, just below the surface regolith, is also a rock layer about 15 meters thick. It was probably lifted from the Martian surface by a meteorite impact.
Now, the researchers hope they can apply their technique to explore the subsoil of Mars more deeply. Until the first kilometers of the Martian crust.