New evidence suggests Venus is not geologically dead, with signs of hot material rising from its interior indicating ongoing crustal activities.
Research published in Science Advances reveals coronae features on Venus' surface are likely formed by rising hot rock plumes reshaping the crust.
Venus, despite lacking plate tectonics like Earth, may share internal dynamics indicating active processes reshaping its surface.
Of the 75 coronae studied, 52 appear to be above buoyant mantle plumes, potentially driving ongoing geological processes on Venus.
Scientists believe Venus' thin crust, coupled with extreme conditions, leads to crustal shedding or melting that aids in regulating surface structure.
The shedding process could recycle water and materials back into Venus' interior, fueling volcanic activity and influencing its atmosphere.
Upcoming missions like NASA's VERITAS and DAVINCI, as well as ESA's EnVision, aim to provide detailed data on Venus' geology and surface activities.
Direct observations from these missions may revolutionize our understanding of Venus's geology and its correlation to early Earth.
The discoveries challenge the traditional view of Venus as a dormant planet, highlighting potential ongoing geological processes beneath its surface.
The new findings offer insights into Venus' geological evolution and its role in comparison to Earth's history, raising intriguing questions in planetary science.