These eruptions are commonly phreatomagmatic eruptions, representing violent explosions caused by rising basaltic or andesitic magma coming into contact with abundant, shallow groundwater or surface water. Tuff rings, pyroclastic cones of primarily ash, are built by explosive disruption of rapidly cooled magma.
Although similar in nature to phreatomagmatic eruptions, there are several specific characteristics:
- Physical nature of magma: viscous; basaltic.
- Character of explosive activity: violent ejection of solid, warm fragments of new magma; continuous or rhythmic explosions; base surges.
- Nature of effusive activity: short, locally pillowed, lava flows; lavas may be rare.
- Nature of dominant ejecta: lithic, blocks and ash; often accretionary lapilli; spatter, fusiform bombs and lapilli absent.
- Structures built around vent: tuff rings
Examples of Surtseyan eruptions
- Bogoslof Island - Alaska, USA, 1796
- Fire Island - Alaska, USA, 1796
- Anak Krakatau - Sunda Strait, Indonesia, 1927-1930 (with smaller eruptions continuing today)
- Shōwa Iōjima - Iōjima, Kagoshima, Japan, 1934
- Capelinhos - Faial Island, Azores, 1957-1958
- Surtsey - Iceland, 1963
- Jólnir - Iceland, 1966
- Taal Volcano - Batangas, The Philippines (last erupted 1977)
- Zubair Group - Yemen, 2011-2012
- El Hierro - Canary Islands, 2011-2012 (see 2011-2012 El Hierro eruption)