History of the Cyclades and Syros tended to approach the Northeast Aegean from a cultural point of view, while the Southern Cyclades seem to have been closer to the Cretan civilisation. Ancient tradition speaks of a Minoan maritime empire, a sweeping image that demands some nuance, but it is nevertheless undeniable that Crete ended up having influence over the entire Aegean. This began to be felt more strongly beginning with the Late Cycladic, or the Late Minoan (from 1700/1600 BC), especially with regard to influence by Knossos and Cydonia. During the Late Minoan, important contacts are attested at Kea, Milos and Santorini; Minoan pottery
Minoan eruption activity and the possible generation of tsunamis. Man-made structures not buried during Minoan A were completely destroyed. The third phase was also characterized by the initiation of caldera collapse. The fourth, and last, major phase (BO/Minoan D) was marked by varied activity: lithic-rich base surge deposits, lahars, debris flows, and co-ignimbrite ash-fall deposits. This phase was characterized by the completion of caldera collapse, which produced megatsunamis. Although the fracturing process is not yet known, the altitudinal statistical analysis indicates that the caldera had formed just before the eruption. The area of the island was smaller, and the southern and eastern