# Venus's Rift Valleys May Explain Planet's Geological Activity New simulations suggest Venus might be more active than previously thought. - **Source:** [Nature](https://brifing.si/source/4d850c3b-dd79-4024-bc91-db2571889199) - **Published:** 2026-08-03 - **Topic:** [Business](https://brifing.si/c/business) - **Original article:** - **On Brifing:** https://brifing.si/s/98797e80-915a-42e8-8a93-891f9cdbc6ee ## Venus's Geological Mystery Computer simulations reveal that the massive rift valleys on Venus's surface formed within the last tens of millions of years and may still be active. This finding challenges the widespread belief that the planet is tectonically dead. Research supported by NASA's Jet Propulsion Laboratory and USGS shows Venus may have undergone geological evolution quite different from Earth's. ## Formation Process of Rift Valleys Venus's rift valleys are enormous depressions formed by the stretching and splitting of the planet's crust. Unlike similar formations on Earth, Venus's appear much younger. Simulations suggest these structures might still be moving and could be fed by magma activity beneath the surface. ## Evidence for Tectonic Activity Researchers detected recent active rifting on Venus by examining wide rift flank uplifts on the planet's surface. These findings indicate Venus's internal dynamics are far more complex than previously assumed, raising new questions about the planet's heat transfer mechanisms. ## Comparison with Mars Just as Marsquakes revealed the Red Planet has a solid core, Venus's rift valleys provide clues about its internal structure. These differing geological behaviors between planets are crucial for understanding terrestrial planet evolution, reopening the question of why Venus didn't develop an Earth-like tectonic system. ## Role of Deep-Sea Technologies The modeling techniques used in the research were inspired by methods developed to study tectonic movements on ocean floors. Adapting four different deep-sea technologies allowed clearer understanding of Venus's surface deformations, potentially setting a new standard for interplanetary geology studies. ## Observation of Lava Outflows Processes of seafloor spreading and lava outflows, observed for the first time on Earth, help understand similar geological formations on Venus. Venus's thick atmosphere makes surface observations challenging, making studies of terrestrial analogs more valuable for planetary geology. ## Impact on Space Exploration These new findings about Venus's geological activity could influence planning for future space missions. NASA's VERITAS and ESA's EnVision missions specifically target these rift valleys for detailed study. Understanding Venus's internal structure may explain why it evolved such a different climate from Earth. ## Significance for Planetary Science Evidence that Venus might still be geologically active forces us to rethink terrestrial planet evolution. These findings will enhance our understanding not just of Venus, but also of rocky exoplanets. For planetary scientists, Venus offers a unique laboratory to study Earth's alternative future. ## Sources covering this story - https://www.nature.com/articles/d41586-026-02372-0 — --- _Summary written by Brifing from the original reporting. Copyright in the original article belongs to its publisher; read the full piece at the link above._