Hidden below 15 miles of clouds, Venus’ stifled surface looks much different — much younger — than its nearby terrestrial brethren. While Mars and the Moon are pockmarked by thousands of craters, Venus’ features are no older than 250 million to 750 million years. Some think this is the result of an abrupt re-paving of the Venusian surface that occurred when life on Earth was just beginning to sprout fins. New research published March 25 in the Journal of Geophysical Research , however, discounts this theory, favoring instead a different explanation — perhaps that Venus’ hundreds of volcanoes are the likely culprit behind the crater-less carpet.Using numerical models to see how material in the planet’s mantle circulates, the results found that the planet couldn’t have undergone what is called mobile‐lid convection — a process where the surface rapidly sinks into the interior and is replaced by a fresh, crater-free surface. The results will help scientists understand how Venus evolved and may even help us understand how the planet’s runaway atmosphere came to be.Earth and Venus formed during the same time and they have near-identical sizes, but any similarities end there. While Earth’s atmosphere is primarily nitrogen, Venus’ is almost entirely poisonous carbon dioxide. Most of the venusian surface is a landscape of smooth volcanic plains, some of which may still be active. Astronomers have long argued how Venus’ topography arose. Was it an abrupt mobile-lid convection event, or a continual surface renewal by active volcanoes?In a mobile-lid convection event, the lithosphere — the crust — sinks to settle along the core-mantle boundary. As the mass moves inward, it falls unevenly, leaving some areas thicker than others. So if a sudden event caused Venus’ entire lithosphere to sink below the surface, then there would be geologic evidence left behind. This evidence could be seen in an offset between Venus’ center of mass and the actual center of the planet — the CM-CF offset.“It seemed to me that if material was recycled into the interior of the body, there would be significant mass anomaly, so I anticipated a CM-CF offset,” says Scott King, the paper’s author and a researcher at Virginia Tech.Observations have shown there is a slight offset. However, the models created to reconstruct such an event each found a much higher offset than the one observed on Venus.Offsets like Venus’ aren’t unusual; all the terrestrial bodies have them. On Earth it may be caused by the greater landmass in the Northern hemisphere. “On Mars, the Tharsis swell — not just the major shield volcanoes but the 5,000-kilometer-diameter region that is volcanic construct — is likely the cause of the CM-CF offset,” says King. “I don’t think there is one unique explanation for CM-CF offsets.”