36°25′12″ North and 25°25′54″ East
There was no eruption at Santorini in 1883. The last activity there. The island of Karkatoa famously destroyed itself in a cataclysmic volcanic eruption in 1883. This eruption was similar to the one that occurred at Santorini around 1600 BC.
This was caused by the Minoan eruption of Thera or the Santorini eruption between 1642 and 1540 BC
Yes, Santorini is a volcanic island known for its geological formations created by past volcanic activity. The island's main feature is the caldera, a large submerged volcanic crater, which was formed by a massive volcanic eruption in the Bronze Age.
In 1628 BC, the volcanic eruption of Thera (Santorini) occurred. This cataclysmic event led to the collapse of the Minoan civilization on the island of Crete, causing widespread destruction and tsunamis in the Aegean Sea. The eruption is believed to have significantly impacted the ancient world and may have inspired the legend of Atlantis.
Catastrophic eruption Volcanic Explosivity Index (VEI) = 6 - 7 Dense-rock equivalent (DRE) = 60 km3
The caldera of Santorini is the gulf surrounded by the roughly crescent-shaped island. This caldera formed when the island underwent a cataclysmic volcanic eruption between 1500 and 1700 BC. The eruption drained so much magma from the chamber beneath Santorini that most of the island collapsed into the space left behind and disappeared beneath the sea.
The volcanic eruption that formed the caldera of Santorini is believed to have occurred around 1600 BCE during the Minoan civilization. It is known as one of the largest volcanic events in recorded history.
The Santorini caldera is a collapsed volcanic cone.
The eruption of the Santorini volcano, known as the Minoan eruption, occurred around 1600 BC. It was one of the largest volcanic events in recorded history, causing significant destruction to the island of Santorini and impacting civilizations in the surrounding area. The eruption is believed to have contributed to the decline of the Minoan civilization on the island of Crete.
It is currently not possible to predict exactly when Santorini will erupt next, as volcanic activity is unpredictable. Scientists continue to monitor the volcano for any signs of unrest to provide early warnings if an eruption is imminent.
Santorini volcano was formed by the conversion of the African plate and the Aegean Sea Plate. As subduction occurred, some magma burned to the surface and create volcanic islands called island arcs. Santorini is one of those volcanic islands.
There are no serious volcanoes located in Southwest Asia. The last major volcanic eruption in the area was the Greek island of Santorini over 2500 years ago.