As part of constructing a new global map of Mars minerals, the Oxia Planum region was discovered to be rich in clays. These clays included the iron- and magnesium-rich minerals of smectite and vermiculite, and locally kaolin, which is known on Earth as china clay. Hydrated silica is also mapped over an ancient delta in Oxia. The close-up data were obtained from a global map of minerals produced by ESA’s Mars Express and NASA’s Mars Reconnaissance Orbiter.
Because clays are formed in water-rich environments it makes these site excellent locations to study for clues as to whether life once began on Mars. Oxia Planum was selected as the landing site for ESA’s Rosalind Franklin rover.