New research based on NASA's Magellan mission data suggests that tectonic activity may be deforming Venus' surface, indicating ongoing tectonics on the planet.
Coronae, vast quasi-circular features on Venus, are believed to be shaped by tectonic processes caused by molten material from the planet's mantle.
A recent study published in Science Advances reveals new evidence of tectonic activity beneath Venus' coronae.
Researchers studied coronae, which are thought to be locations where plumes of hot material rise from the mantle, influencing the planet's lithosphere.
The study, led by Gael Cascioli, suggests that coronae on Venus could provide insights into Earth's past and present subsurface processes.
NASA's upcoming VERITAS mission aims to provide high-resolution gravity data to further understand Venus' geological processes.
Coronae formation on Venus involves various tectonic processes like subduction and lithospheric dripping, different from Earth's tectonic activities.
The VERITAS mission will use advanced instruments to map Venus' surface, measure its gravitational field, and study its interior structure.
Future data from VERITAS could revolutionize our understanding of Venus' geology, drawing parallels to early Earth's geological evolution.
The Magellan mission, managed by NASA's Jet Propulsion Laboratory, made significant contributions to understanding Venus' geological features.