Eruption of Thera

The eruption of the volcanic island of Thera, in the Aegean Sea, was one of the largest volcanic events of the last several thousand years, most commonly dated by geological and radiocarbon evidence to around 1600 BCE, though the exact date remains debated among archaeologists reconciling it with Egyptian historical chronology. The eruption buried the flourishing Minoan-influenced settlement of Akrotiri on Thera itself under volcanic ash, preserving multi-story buildings and vivid wall paintings in a state of preservation often compared to Pompeii, and the island's central caldera collapsed into the sea in the eruption's aftermath, creating the dramatic crescent-shaped geography visible on the island, now known as Santorini, today. The eruption's tsunami and ashfall are widely believed by archaeologists to have severely damaged Minoan coastal settlements and shipping on nearby Crete, and while it did not by itself destroy Minoan civilization, many scholars regard it as a significant contributing factor in the broader decline of Minoan power that culminated in Mycenaean Greek dominance over Crete within a few generations of the eruption.