Venusian Gravity Currents
Radar measurements of Venus's surface reveal the remains of many volcanic eruptions. One type of feature, known as a pancake dome, has a very flat top and steep sides; one dome, Narina Tholus, is over 140 kilometers wide. Since their discovery, scientists have been puzzling out how such domes could form. A recent study suggests that the Venusian surface's elasticity plays a role. (Image credit: NASA; research credit: M. Borelli et al.; via Gizmodo) Read the full article








