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Ischia volcano

stratovolcano, lava domes, cinder cone 790 m
Italy, 40.73°N / 13.9°E
Current status: dormant (1 out of 5) | Reports
Ischia volcano books | Tours
Typical eruption style: Explosive
Ischia volcano eruptions: 1302 AD
TimeMag. / DepthDistanceLocation
Thu, 14 Jun
Thu, 14 Jun 21:57 UTCM 1.5 / 3.1 km6 km2 km SW Pozzuoli (NA)
Wed, 13 Jun
Wed, 13 Jun 09:43 UTCM 1.9 / 7.5 km35 kmTirreno Meridionale (MARE)
The Ischia volcanic complex forms a rectangular, 6 x 9 km island immediately SW of the Campi Flegrei area at the western side of the Bay of Naples.

Background:

The eruption of the trachytic Green Tuff ignimbrite about 55,000 years ago was followed by caldera formation. The high point on the island, 789-m-high Monte Epemeo, is a volcanic horst composed of the Green Tuff ignimbrite deposit that was submerged after its eruption and then uplifted. Volcanism on the island has been significantly affected by tectonism that formed a series of horsts and grabens; at least 800 m of uplift has formed as a result of resurgent doming during past 33,000 years. Many small monogenetic volcanoes were formed around the uplifted block. Volcanism during the Holocene produced a series of pumiceous tephras, tuff rings, lava domes, and lava flows. The latest eruption of Ischia, in 1302 AD, produced a spatter cone and the Arso lava flow, which reached the NE coast. Source: Smithsonian GVP

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