The submarine eruption of the Bombarda volcano, Milos Island, Cyclades, Greece

The Milos volcanic field includes a well-exposed volcaniclastic succession which records a long history of submarine explosive volcanism. The Bombarda volcano, a rhyolitic monogenetic center, erupted ∼1.7 Ma at a depth

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Bibliographic Details
Published in:Bulletin of volcanology 2003-05, Vol.65 (4), p.282-293
Main Authors: RINALDI, M, CAMPOS VENUTI, M
Format: Article
Language:English
Subjects:
Breccia
Carapace
Crystalline rocks
Earth sciences
Earth, ocean, space
Exact sciences and technology
Explosions
Geology
Igneous and metamorphic rocks petrology, volcanic processes, magmas
Juveniles
Lava
Lava domes
Lithic
Obsidian
Pumice
Sea level
Seismic activity
Volcanic eruptions
Volcanic fields
Volcanism
Volcanoes
Volcanology
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Description
Summary:The Milos volcanic field includes a well-exposed volcaniclastic succession which records a long history of submarine explosive volcanism. The Bombarda volcano, a rhyolitic monogenetic center, erupted ∼1.7 Ma at a depth
ISSN:0258-8900
1432-0819
DOI:10.1007/s00445-002-0260-z