Minoan civilization expand their influence. It is likely that the original hierarchies of the local elites were replaced by monarchies, a precondition for the palaces. At the end of the MMII period (1700 BC) there was a large disturbance on Crete—probably an earthquake, but possibly an invasion from Anatolia. The palaces at Knossos, Phaistos, Malia and Kato Zakros were destroyed. At the beginning of the neopalatial period the population increased again, the palaces were rebuilt on a larger scale and new settlements were built across the island. This period (the 17th and 16th centuries BC, MM III-Neopalatial) was the apex of Minoan
Periodisation of the Indus Valley Civilisation Periodisation of the Indus Valley Civilisation Several periodisations are employed for the periodisation of the Indus Valley Civilisation. While the Indus Valley Civilisation was divided into Early, Mature and Late Harappan by archaeologists like Mortimer Wheeler, newer periodisations include the Neolithic early farming settlements, and use a Stage-Phase model, often combining terminology from various systems. The most commonly used nomenclature classifies the Indus Valley Civilisation into Early, Mature and Late Harappan Phase. The Indus Civilisation was preceded by local agricultural villages, from where the river plains were populated when water-management became available, creating an integrated civilisation. This broader time range