Volcanism of Italy
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Italy is a volcanically active country, containing the only active volcano in mainland Europe. The country''s volcanism is due chiefly to the presence, a short distance to the south, of the boundary between the Eurasian Plate and the African Plate. The magma erupted by Italy''s volcanoes is thought to result from the upward forcing of rocks melted by the subduction of one plate below another. Three main clusters of volcanism exist: a line of volcanic centres running n...
Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Italy is a volcanically active country, containing the only active volcano in mainland Europe. The country''s volcanism is due chiefly to the presence, a short distance to the south, of the boundary between the Eurasian Plate and the African Plate. The magma erupted by Italy''s volcanoes is thought to result from the upward forcing of rocks melted by the subduction of one plate below another. Three main clusters of volcanism exist: a line of volcanic centres running northwest along the central part of the Italian mainland (see Campanian volcanic arc); a cluster in the northeast of Sicily; and another cluster around the Mediterranean island of Pantelleria.
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