Here at www.travel-to-santorini.com you can find information on formation of the volcano, all the eruptions, date considerations, Santorini's geology and … Thirty million cubic meters of magma in the form of pumice and ash were blown to a height of up to 36 kilometers above the island. It is actually a Caldera (crater), an ancient rim of a still active volcano.The beautiful white houses are scattered along the cliffside. That is why Santorini has the weirdest beaches with black, red or white volcanic sand and the caldera which was mainly formed by solidified lava — a… was one of the largest in the last 10,000 years.About 7 cubic miles (30 cubic km) of rhyodacite magma was erupted. is a non-profit organisation, founded in the summer of 1995, whose primary aim is to continue to maintain the operation of the Volcano Observatory and the monitoring networks, which were established under a research program funded by the E.U. Santorini Volcano: Formation of Palea and Nea Kameni. The volcano showed no more activity until 726 AD, when the new eruption produced material that united Iera and Thia and formed … Now the center of the crater-like caldera is … Although dormant, Santorini is an active volcano.

In 197 BC, a new eruption created a small island named Iera and in 46 AD, the island of Thia emerged beside it. The last huge eruption of the volcano dates back 3,600 years (17th century B.C. Santorini is probably the most extraordinary island in the Aegean Sea. Location: Nea Kameni Santorini Volcano: Santorini is gifted with a unique natural beauty and a wild scenery created by the volcanic eruptions.As it is extremely famous for the beautiful caldera, the island is also known for the two small islands of black lava positioned at the center of the basin of Santorini which is, geographically, the youngest islets in the Eastern Mediterranean. The Institute for the Study and Monitoring of the Santorini Volcano (I.S.M.O.SA.V.) Photo: Konstantina Sidiropoulou. Palea Kameni and Nea Kameni were formed as a result of multiple, initially submarine eruptions at the center of the caldera. The current caldera was formed about 3600 years ago during the Minoan eruption. Santorini, Greece Location: 36.4N, 25.4E Elevation: 1,850 feet (564 m) The eruption of Santorini in Greece in 1,650 B.C. In 1646 BC a massive volcanic eruption, perhaps one of the largest ever witnessed by mankind, took place at Thera (present day Santorini), an island in the Aegean not far from Crete. The plinian column during the initial phase of the eruption was about 23 miles (36 km) high. ), to the late bronze age. Santorini Volcano is one of the most significant volcanoes in the world history because it is considered responsible for the destruction of the Minoan Crete . The Geology of Santorini: The island of Santorini, popularly referred to as Thera, is located at the extreme southernmost part of Cyclades islands, Greece.Santorini is a unique island in the Mediterranean Sea, as it is the place of several remarkable volcanic explosions that have erupted here over the past thousands of years. The Greek islands of Santorini form the perimeter of a volcano whose last major explosion happened about 3,400 years ago. Intrested into Santorini Volcano? Santorini eruption: new theory says ‘pyroclastic flows’ caused devastating Bronze Age tsunamis November 8, 2016 11.29am EST Matthew Pound , Northumbria University, Newcastle

In fact, the five islands that make up Santorini were formed over 2 million years of volcanic eruptions.

Santorini volcano facts If you are a reader of this blog then you already know that the whole island of Santorini was formed because of a volcanic eruption.