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Mamma
Etna's countless children |
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Located
in a densely populated area low on the southeast flank of Mount Etna,
Monte Serra is a youthful, horseshoe-shaped pyroclastic cone that is now
a public park of the nearby town of Viagrande. The height of the cone
above its base ranges from about 60 m on the west side to more than 130
m on the southeast side; it has a crater about 250 m in diameter and open
to the northeast. Some sources attribute the formation of this cone to
an eruption in 122 B.C. but the eruption of that year is now known to
have been a Plinian (i.e. highly explosive) summit eruption. The exact
date of the formation of Monte Serra is thus not constrained, but it is
plausible that it occurred in Roman time, about 2000 years ago. On the
southeast base of Monte Serra lies the village of Viagrande, and little
more than 1 km to the west lies the village of Trecastagni, both with
picturesque historical centers and nice churches in baroque architecture.
No lava flow has been clearly associated with the alleged Monte Serra
eruption in 122 B.C. on the 1979 Geological Map of Etna, but several lava
flows extend from that cone to the southeast, passing close to the town
of Acireale. |
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Copyright © Boris Behncke, "Italy's Volcanoes: The Cradle of Volcanology" |
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Page set up on 29 February 2004, last modified on 11 March 2004 |