Evidence of ongoing volcanic activity on Venus revealed by Magellan radar

The surface of Venus has undergone substantial alterations due to volcanic activity throughout its geological history, and some volcanic features suggest that this activity persisted until as recently as 2.5 million years ago. Recent evidence of changes in the surface morphology of a volcanic vent has been interpreted as a potential indication of ongoing volcanic activity. To investigate more widespread alterations that have occurred over time in the planet's surface morphology, we compared radar images of the same regions observed from 1990 to 1992 with the Magellan spacecraft. We found variations in the radar backscatter from different volcanic-related flow features on the western flank of Sif Mons and in western Niobe Planitia. We suggest that these changes are most reasonably explained as evidence of new lava flows related to volcanic activities that took place during the Magellan spacecraft's mapping mission with its synthetic-aperture radar. This study provides further evidence in support of a currently geologically active Venus.Observation of new lava flows between different Magellan radar scans in regions of Sif Mons and Niobe Planitia confirms that volcanism on Venus is still ongoing. This evidence also suggests the planet's volcanic activity exceeds previous estimates.