A mosaic of Mars’ Valles Marineris hemisphere, captured by 102 Viking Orbiter images, shows the vast 2,000 km-long canyon system from 2,500 km above. The image reveals the Tharsis volcanoes, ancient river channels, and cratered southern terrain. Mars, the Red Planet, has always been a bit of a mystery. Why is it so… well, red? Scientists have long known that iron oxides (aka rust) are to blame, but a new study published on February 25 in *Nature Communications* suggests there’s more to the story. Meet ferrihydrite, a water-rich iron mineral that might be the real MVP behind Mars’ iconic dusty red look. Why Ferrihydrite? Ferrihydrite forms in the presence of cool water, which is a big deal because it hints at a time when Mars was wetter and potentially more habitable. Unlike other iron minerals like hematite, ferrihydrite doesn’t need scorching temperatures to form. This means Mars might have had a cooler, wetter past before it turned into the dry, dusty desert we know...