Antiparos Volcano
Updated: 17 mai 2024 00:46 GMT -
Pyroclastic cone(s) 282 m / 925 ft
Aegean Sea, Greece, 37°N / 25.05°E
Condition actuelle: (probablement) éteint (0 sur 5)
Aegean Sea, Greece, 37°N / 25.05°E
Condition actuelle: (probablement) éteint (0 sur 5)
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Eruptions du volcan Antiparos: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)
Derniers séismes proches
Heure | Mag. / Profondeur | Distance / Lieu |
Introduction
Antiparos Island, positioned within the back-arc region of the South Aegean Volcanic Arc, contains a group of rhyolitic lava domes and pyroclastic cones with associated lava flows that are of Miocene to early Quaternary age (Pe-Piper and Piper, 2007; IAVCEI; Keller, 1982; Clapsopoulos, 1998). The domes are surrounded by tuffs containing obsidian particles and pumice, which are believed to be the result of subaqueous pyroclastic flows. The volcanic products are distributed over a total area of about 4.5 km2 (Clapsopoulos, 1998). K-Ar dates listed in Fytikas et al. (1984) range from 5.4 to 4.0 Ma.---
Smithsonian / GVP volcano information
Antiparos Volcano Photos
De gauche à droite, les îles Despotiko, Antiparos et Paros (maintenant inhabitées) dans le centre des Cyclades (Grèce), vues du ciel (Photo: Tom Pfeiffer)