Santorini, also known as Thira, is a Greek island in the southern Aegean Sea about 200 kilometers southeast of the mainland, the largest landmass in a circular group of islands formed by the Santorini caldera. It sits above the Hellenic volcanic arc and was built through repeated cycles of shield-volcano growth followed by caldera collapse, resting on a basement of metamorphosed limestone and schist. About 3,600 years ago the island was the site of the Minoan eruption, one of the most powerful volcanic events in recorded history, which expelled roughly 61 cubic kilometers of magma and rock and buried the Minoan settlement at Akrotiri in ash. Santorini remains the most active volcanic center in the South Aegean Volcanic Arc, and today draws about two million visitors a year while its volcanic soils still support traditional viticulture.
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Source Santorini (Wikipedia)
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Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Santorini
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Source Wikidata: Santorini
Sources
1. UNEP-WCMC and IUCN, World Database on Protected Areas: World Database on Protected Areas record: SANTORINI: NEA KAI PALIA KAMENI - PROFITIS ILIAS
UNEP-WCMC and IUCN, World Database on Protected AreasWDPA record, field desig_engQuote, WDPA record, field desig_eng
"desig_eng": "Special Areas of Conservation (Habitats Directive)"
View the Source Wikidata: Santorini
Wikidata Q129296, class allow-list match (w-wdresolver-0926)View the Source Protected Planet (UNEP-WCMC and IUCN): SANTORINI: NEA KAI PALIA KAMENI - PROFITIS ILIAS
Protected Planet (UNEP-WCMC and IUCN)Protected area profileQuote, Protected area profile
Protected Area Profile for SANTORINI: NEA KAI PALIA KAMENI - PROFITIS ILIAS from the World Database on Protected Areas
View the Source Santorini (Wikipedia)
Caused By: Volcanism, Lead section (caused-by Volcanism)Quote, Caused By: Volcanism, Lead section (caused-by Volcanism)
It is the largest island of a small, circular archipelago formed by the Santorini caldera.
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