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The Minoan eruption was a catastrophic volcanic eruption that devastated the Aegean island of Thera (also called Santorini) circa 1600 BCE. [2] [3] It destroyed the Minoan settlement at Akrotiri, as well as communities and agricultural areas on nearby islands and the coast of Crete with subsequent earthquakes and paleotsunamis. [4]
A view of the mountaintop ruins of Ancient Thera from Mt. Elias. The theater is built into the slope below the city. Ancient Thera (Greek: Αρχαία Θήρα) is the name of an archaeological site [1] from classical antiquity [2] on the island of Santorini, which sits on the top of a limestone hill called Mesa Vouno.
Santorini caldera is a large, mostly submerged caldera, located in the southern Aegean Sea, 120 kilometers north of Crete in Greece.Visible above water is the circular Santorini island group, consisting of Santorini (classic Greek Thera), the main island, Therasia and Aspronisi at the periphery, and the Kameni islands at the center.
Taken on 16 May 2001, 4 years before the 23 September 2005 roof collapse. [1] Layout map of Akrotiri in the Bronze Age. Pumice, here: northern shelving coast. Eruption of 165 ka buried it all. Akrotiri (Greek: Ακρωτήρι, pronounced Greek:) is the site of a Cycladic Bronze Age settlement on the volcanic Greek island of Santorini (Thera).
The remains of the Thera volcano's caldera. The timing of natural disasters is of importance to high and low chronologies, which can use the resulting geological evidence to date co-located artifacts. The eruption of the Thera volcano on what is now the island of Santorini is of particular significance to the chronology of Minoan history.
A notable event from this era was the eruption of the Thera volcano, which occurred around 1600 BC towards the end of the LM IA subperiod. [28] One of the largest volcanic explosions in recorded history, it ejected about 60 to 100 cubic kilometres (14 to 24 cu mi) of material and was measured at 7 on the Volcanic Explosivity Index .
The geologic time scale, proportionally represented as a log-spiral with some major events in Earth's history. A megaannus (Ma) represents one million (10 6) years.. The geologic time scale or geological time scale (GTS) is a representation of time based on the rock record of Earth.
The first eon in Earth's history, the Hadean, begins with the Earth's formation and is followed by the Archean eon at 3.8 Ga. [2]: 145 The oldest rocks found on Earth date to about 4.0 Ga, and the oldest detrital zircon crystals in rocks to about 4.4 Ga, [34] [35] [36] soon after the formation of the Earth's crust and the Earth itself.