Color-coded topographic view shows the relative heights of features in Cerberus Fossae: reds and whites are relatively higher than blues and purples. The image is based on a digital terrain model of the region, from which the topography of the landscape can be derived. Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO
Until now, Mars has generally been considered a geologically dead planet. An international team of scientists now reports that seismic signals indicate vulcanism still plays an active role in shaping the Martian surface.
Ever since the NASA InSight Mission deployed the SEIS seismometer on the surface of Mars in 2018, seismologists and geophysicists at ETH Zurich have been listening to the seismic pings of more than 1,300 marsquakes.
Ever since the NASA InSight Mission deployed the SEIS seismometer on the surface of Mars in 2018, seismologists and geophysicists at ETH Zurich have been listening to the seismic pings of more than 1,300 marsquakes.
Again and again, the researchers registered smaller and larger Mars quakes. A detailed analysis of the quakes’ location and spectral character eventually brought a surprise. With epicenters originating in the vicinity of the Cerberus Fossae — a region consisting of a series of rifts or graben — these quakes tell a new story.
A story that suggests an active role is still played by vulcanism in shaping the Martian surface.
Mars shows signs of geological life
Led by ETH Zurich, an international team of researchers analyzed a cluster of more than 20 recent marsquakes that originated in the Cerberus Fossae graben system. From the seismic data, scientists concluded that the low-frequency quakes indicate a potentially warm source that could be explained by present-day molten lava, i.e., magma at that depth, and volcanic activity on Mars. Specifically, they found that the quakes are located mostly in the innermost part of Cerberus Fossae. READ MORE...
Mars shows signs of geological life
Led by ETH Zurich, an international team of researchers analyzed a cluster of more than 20 recent marsquakes that originated in the Cerberus Fossae graben system. From the seismic data, scientists concluded that the low-frequency quakes indicate a potentially warm source that could be explained by present-day molten lava, i.e., magma at that depth, and volcanic activity on Mars. Specifically, they found that the quakes are located mostly in the innermost part of Cerberus Fossae. READ MORE...
