Artwork depicting Mars during its Hesperian Period, roughly 3700-3000 million years ago. The period
is characterised by extreme volcanism which led to catastrophic flooding. These latter helped carve
the extensive outflow channels seen on Mars - wide, long surface features resembling huge rivers and
deltas. The canyon Valles Marineris (centre right) was formed during this period, as were the famous
Tharsis volcanoes such as Olympus Mons (upper left in this image). This was also a transitional
period for Mars, during which it lost much of its atmosphere and surface water, and became colder
and dryer than during the previous Noachian Period.