A recent study funded by NASA has provided new insights into the reason behind Mars’ distinctive red color, identifying the iron mineral ferrihydrite as a key contributor. This research suggests that the Martian environment may have been more conducive to life in its past, potentially supporting the existence of liquid water and possibly habitable conditions.

Researchers involved in the study meticulously analyzed data collected from various Mars missions, specifically examining the mineral composition of Martian dust and rock formations. They also conducted laboratory experiments to replicate Martian conditions and to better understand the minerals present on the planet’s surface.

The findings challenge long-standing theories that attributed Mars’ red hue to hematite, a type of iron oxide that typically forms in warmer conditions. In contrast, the study indicates that ferrihydrite is the more likely culprit for the planet’s reddish appearance. Ferrihydrite, which is associated with cooler and wetter conditions, is found extensively in Martian dust and rock samples, according to the researchers.