Minoan civilization and courtyards between 1650 and 1600 BC. These rocks were likely quarried in Agia Pelagia on the north coast of central Crete. Palaces ("anaktora") are the best-known Minoan building types excavated on Crete. They are monumental buildings with administrative purposes, as evidenced by large archives unearthed by archaeologists. Each palace excavated to date has unique features, but they also share aspects which set them apart from other structures. Palaces are often multi-story, with interior and exterior staircases, lightwells, massive columns, storage areas and courtyards. The first palaces were constructed at the end of the Early Minoan period in the third
Minoan eruption volcano, which erupted and then collapsed in an ongoing cyclical process. Immediately before the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands with the only entrance between Thera and the tiny island of Aspronisi. This cataclysmic eruption was centered on a small island just north of the existing island of Nea Kameni in the centre of the then-existing caldera. The northern part of the caldera was refilled by the volcanic ash and lava, then collapsed again. Research by a team of international scientists in 2006 revealed that the Santorini event was much larger than