Furthermore, the interpretation of the age and stratigraphy of sediments blanketing the bottom of the Cyprus Basin from sea bottom cores containing Pleistocene and older marine sediments and thousands of kilometers of seismic lines from the Cyprus and adjacent basins clearly demonstrates that the Mediterranean Sea last dried up during the Messinian Salinity Crisis between 5.59 and 5.33 million years ago. For example, research conducted south of Cyprus as part of Leg 160 of the Ocean Drilling Project recovered from Sites 963, 965, and 966 cores of sediments underlying the bottom of the Mediterranean Sea at depths as shallow as 470, 1506, and 1044 meters (1540, 4940, and 3420 ft) below sea level. Thus, these cores came from parts of sea bottom of the eastern Mediterranean Sea that either lie above or at the depth of Sarmast's Atlantis, which lies at depths between 1470 and 1510 meters (4820 and 4950 ft) below mean sea level. These cores provide 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 kilometer of water.