A strong quake in the last year of the NASA Mars InSight mission, enabled researchers at ETH Zurich to determine the global thickness and density of the planet’s crust. On average, the Martian crust much thicker than the Earth’s or the Moon’s crust and the planet’s main source of heat is radioactive.
In May 2022, the Marsquake Service at ETH Zurich recorded the largest quake ever observed on another planet. This event, with an estimated magnitude of 4.6 was recorded on the surface of Mars by the seismometer deployed as part of the NASA Mars InSight mission. "This marsquake sent out strong seismic waves that traveled along the surface of Mars," says Doyeon Kim, a seismologist at the Institute of Geophysics at ETH Zurich.
Surface waves offer a global perspectiveAfter more than three years of daily monitoring and with the power levels decreasing on InSight’s seismometer, researchers were rewarded with data from a sizeable marsquake. The surface waves observed from this large marsquake not only travelled from the quake’s source to the measuring station, they also continued to travel around the entire planet several times. This data not only provided information about specific areas of Mars, but also enabled a global view of the planet.
"From this quake, the largest quake recorded during the entire InSight mission, we observed surface waves that circled Mars up to three times," says the seismologist and lead author of a study just published in the journal, Geophysical Research Letters. In order to gain information about the structure that the waves passed through, the researchers measured how fast these waves propagate at different frequencies.
These seismic velocities provide insights into the interior structure at different depths. Previously, observed surface waves from the two large meteorite impacts also allowed regional findings along their specific propagation paths. "Now, we have seismic observations that represent the global structure," says Kim.
Comparing data from Mars with that of the Earth and MoonCombining their newly obtained results with existing data on the gravity and topography of Mars, the researchers were able to determine the thickness of the Martian crust. It averages 42 to 56 kilometres (26 - 35 miles). On average, the crust is thinnest at the Isidis impact basin at ~10 km (6 miles), and thickest at Tharsis province at ~90 km (56 miles). To put this into perspective, seismic data indicates that the Earth’s crust has an average thickness of 21 to 27 kilometres (13 - 17 miles), while the lunar crust, as determined by the Apollo mission seismometers is between 34 and 43 kilometre (21 - 27 miles) thick.
"This means that the Martian crust is much thicker than that of the Earth or the Moon," says Kim. Generally, smaller planetary bodies in our solar system have a thicker crust than the larger bodies. Kim explains, "We were fortunate to observe this quake. On Earth, we would have difficulty determining the thickness of the Earth’s crust using the same magnitude of quake that occurred on Mars. While Mars is smaller than the Earth, it transports seismic energy more efficiently."
One of the most important results of this research concerns the difference between the northern and southern hemispheres of Mars. This contrast has been observed for as long as there have been telescopes; it is particularly visible in images from Mars satellites. The northern hemisphere on Mars consists of flat lowlands, while there are high mountains in the south. The division between northern lowlands and southern highlands is called a Martian dichotomy.
Similar crust density and radioactive heat"One might think that this difference could be explained by two different rock compositions," says Kim: "One rock would be denser than the other." While the composition may be the same in the north and south, the thickness of the crust varies. If the crust is thicker in the south, there would be less dense Martian mantle material underneath it, whereas a thinner crust in the north would have more of this dense, heavier material.
Precisely what have the researchers have been able to prove? "Based on the seismic observations and the gravity data, we show that the density of the crust in the northern lowlands and the southern highlands is similar," they write. In contrast, the crust in the southern hemisphere extends to a greater depth than in the northern hemisphere. "This finding is exciting, although not very surprising," says Kim. After all, analysis of meteorite impacts on Mars last year already provided evidence that the crusts in the north and south are made of the same material.
Further conclusions can also be drawn from the thick Martian crust. "Our study provides how the planet generates its heat and explains Mars’ thermal history," says Kim. As a single-plate planet, the main source of heat produced in the interior of Mars today is a result of the decay of radioactive elements such as thorium, uranium, and potassium. The study found that 50 to 70 percent of these heat-producing elements are found in the Martian crust. This high accumulation could explain why there are local regions underneath where melting processes may still be taking place today.
More about the NASA Mars InSight MissionThe Jet Propulsion Laboratory (JPL) managed InSight for NASA’s Science Mission Directorate. InSight is part of NASA’s Discovery Program, managed by the agency’s Marshall Space Flight Center. Lockheed Martin Space built the InSight spacecraft, including its cruise stage and lander, and supported 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. The Marsquake Service is headed by ETH Zurich, with significant contributions from IPGP; the University of Bristol; Imperial College; ISAE (Institut Supérieur de l’Aéronautique et de l’Espace); MPS; 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.
NASA Mars InSight: external page https://mars.nasa.gov/insight/ call_made
Details of ETH Zurich’s contributions to Mars InSight: https://www.insight.ethz.ch/en/home/