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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]
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.
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.
Akrotiri (Greek: Ακρωτήρι, pronounced Greek:) is the site of a Cycladic Bronze Age settlement on the volcanic Greek island of Santorini (Thera). The name comes from the nearby village of Akrotiri.
Thera is built upon a small non-volcanic basement that represents the former non-volcanic island, which was approximately 9 by 6 km (5.6 by 3.7 mi). The basement rock is primarily composed of metamorphosed limestone and schist , which date from the Alpine Orogeny.
Therasia, also known as Thirasía (Greek: Θηρασία), is an island in the volcanic island group of Santorini in the Greek Cyclades.It lies north-west of Nea Kameni, a small island formed in recent centuries by volcanic activity and thus marking the centre of the island group.
Bismarck volcanic arc, the Rabaul Caldera includes the sub-vent of Tavurvur and the sub-vent of Vulcan. Bismarck volcanic arc, Pago volcano, New Britain, Papua New Guinea, is a young post-caldera cone within the Witori Caldera. The Buru Caldera cuts the SW flank of the Witori volcano.
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. [6] 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.