The 1000 x 2000 km area region of Tyrrhena Terra (outlined by the
white box in the inset) sits between two regions of low altitude – Hellas
Planitia and Isidis Planitia – in Mars’ southern hemisphere, as shown in this
global topography map. Hydrated minerals were found in 175 locations
associated with impact craters in Tyrrhena Terra, such as inside the walls of
craters, along crater rims, or in material excavated by the impact. Analysis
suggests that these minerals were formed in the presence of water that
persisted at depth for an extended period of time.