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Ischia volcano

stratovolcano, lava domes, cinder cone 790 m
Italy, 40.73°N / 13.9°E
Current status: normal or dormant (1 out of 5) | Reports
Ischia volcano books | Tours
Typical eruption style: Explosive
Ischia volcano eruptions: 1302 AD
TimeMag. / DepthDistanceLocation
Fri, 12 Oct
Fri, 12 Oct 07:43 UTCM 2.0 / 1.8 km2 km5 km E Pozzuoli (NA)
Mon, 8 Oct
Mon, 8 Oct 01:34 UTCM 1.5 / 2.6 km0 km4 km SE Pozzuoli (NA)
Fri, 28 Sep
Fri, 28 Sep 06:59 UTCM 1.7 / 2.9 km0 km4 km E Pozzuoli (NA)
Tue, 18 Sep
Tue, 18 Sep 21:36 UTCM 1.6 / 10 km9 km- 4km SSE of Bacoli, Italy
Tue, 18 Sep 21:36 UTCM 2.5 / 2.3 km1 km5 km E Pozzuoli (NA)
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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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