Home >> Santorini >> Santorini Volcán
Santorini Volcano
The volcanic destructive Thira eruption has become most famous in the Aegean Sea before the fall of Weight troy. The eruption probably would have caused a change of considerable climate for the Mediterranean region of East. This was one of the eruptions hugest volcanic on the Earth in the slightly last one [...]
The volcanic destructive Thira eruption has become most famous in the Aegean Sea before the fall of Weight troy. The eruption probably would have caused a change of considerable climate for the Mediterranean region of East. This was one of the eruptions hugest volcanic on the Earth in the slightly last thousand of years. When the volcano exploded, approximately 1650 aC, it is said to have produced giant waves superior to 200 meters that were sent striking the coast of the north of Crete, causing a violent devastation. The earthquakes were activated and the ash and the ruins obstructed the skies. The civilization Minoan is not great after this, once the chiefs of the seas, it disappeared.
After the eruption, quite what remained of Santorini was the horseshoe the formed island that we know today. The island was covered in a layer of volcanic ash of 30 or 40 meters of depth. The eruptions persisted in the IIIrd century aC when the island of Therasia was cut of Santorini, and in the IInd century aC when the volcanic islet Palaia Kameni began to appear in the bay. In 1707, the eruptions caused the appearance of Nea Kameni. Soft vibrations often are felt to the island, but in 1950 a severe earthquake produced devestation considerably in Fira and It heard, and many of the houses along the rocks were destroyed.
New archaeological discoveries for a team of international scientists in 2006 it showed that the event Santorini was much more massive than earlier the sucediera. This expelled 61 cubic kilometers of magma and the rock in the ambience of the Earth contrasted to the previous estimations of only 39 cubic kilometers in 1991. Only the Assembly Bass drum the volcanic eruption of 1815 (and possibly the eruption in the Lake Taupo of 181 CE) liberated more material in the ambience in last 5,000 years in approximately 100 cubic kilometers.
You can still see tests of this today, but in many places added to the labyrinth of interesting architecture that you preserve to the rock face. The dry amazing climate and the light of the sun keeps on creating images the year about perfect conditions for the look, photos and videos under an extraordinary variety of natural lights and colors that give to the visitor the exceptional advantage of reaching the interior of the volcano in ship.
