Atlantis basin [SEP] located on astronomical body
Atlantis basin
Atlantis basin is an eroded impact crater in the southern hemisphere of Mars, in the Phaethontis quadrangle, Sirenum Terrae region, centered at 177° West, 35° South. It was formed during the early Noachian period.
Atlantis basin contains Atlantis Chaos, a region of chaos terrain. It also contains an ancient dry lakebed (possibly part of Eridania Lake), as well as structures that appear to be volcanic dikes and recently formed gullies, which suggests the possibility of long-term hydrothermal activity.
a detailed and continuous record of sea level that demonstrates that for millions of years at least during the entire Pliocene, Pleistocene, and Holocene epochs that the feature that Sarmast interprets to be Atlantis and its adjacent sea bottom were always submerged below sea level. Therefore, the entire Cyprus Basin, including the ridge where Sarmast claims that Atlantis is located, has been submerged beneath the Mediterranean Sea for millions of years. Since its formation, the sea bottom feature identified by Sarmast as "Atlantis" has always been submerged beneath over a