*This is for college purposes only.
The most dramatic of all the Greek islands, Santorini is best known for the cliff-top towns of Fira and Oia, which lie on the west coast, overlooking the deep, blue sea-filled caldera. Made up of typical Cycladic whitewashed cubic buildings, many of which have been converted into boutique hotels with infinity pools, both Fira and Oia are considered romantic destinations, popular for weddings and honeymoons. Things to do include sunbathing and swimming at the black volcanic sand beaches on the south and east coasts and visiting the archaeological site of Akrotiri, an Ancient Minoan settlement buried below lava following the volcanic eruption that created the caldera, some 3,600 years ago. The island has an airport and is served by ferries and catamarans from Athens’ port, Piraeus.
The whole complex of Santorini islands is still an active volcano (the same as Méthana, Mílos and Nísiros) and probably the only volcano in the world whose crater is in the sea? The islands that form Santorini came into existence as a result of intensive volcanic activity; twelve huge eruptions occurred, one every 20,000 years approximately, and each violent eruption caused the collapse of the volcano’s central part creating a large crater (caldera). The volcano, however, managed to recreate itself over and over again.
The last big eruption occurred 3,600 years ago (during the Minoan Age), when igneous material (mainly ash, pumice and lava stones) covered the three islands (Thíra, Thirassiá and Asproníssi). The eruption destroyed the thriving local prehistoric civilization, evidence of which was found during the excavations of a settlement at Akrotíri. The solid material and gases emerging from the volcano’s interior created a huge “vacuum” underneath, causing the collapse of the central part and the creation of an enormous “pot” –today’s Caldera– with a size of 8×4 km and a depth of up to 400m below sea level.