Minoan pottery moved into the palace of Knossos. They were well-established by 1400, if the Linear B tablets can be dated to then. The resulting LM II culture is not a break with the Minoan past. Minoan traditions continue under a new administration. However, the vase forms and designs became more and more Mycenaean in character with a large variety of decoration. Style names have multiplied and depend to some degree on the author. The names below are only a few of the most common. Some authors just use the name "Mycenaean Koine"; that is, the Late Minoan pottery of Crete was
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