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Syneruptive features and sedimentary processes associated with pyroclastic currents entering the sea: the AD 79 eruption of Vesuvius, Bay of Naples, Italy
- Article from:
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Journal of the Geological Society
- Article date:
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July 1, 2008
- Author:
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Copyright informationCopyright Geological Society Publishing House Jul 2008. Provided by ProQuest LLC. (Hide copyright information)
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Abstract:
The AD 79 Plinian eruption of Vesuvius that buried Pompeii and Herculaneum began with pumice falls deposited towards the SE of the volcano followed by pyroclastic currents directed towards the SW. These currents reached Herculaneum and rapidly entered the sea, forming a fan. The interpretation of seismic reflection profiles and gravity cores collected off Herculaneum documents a submarine fan-shaped pyroclastic body at 10-140 m water depth that we interpret as the submarine counterpart of the onshore pyroclastic current deposits. This fan, c. 0.3 km^sup 3^ in volume, displays a chaotic seismic facies that changes seaward to parallel reflectors and then to wavy reflectors. Gravity ...
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