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Volcanism in Italy : ウィキペディア英語版
Volcanology of Italy

File:Italy_volcano_map.png|right
rect 209 240 265 255 Stromboli
rect 134 306 183 323 Pantelleria
rect 121 281 184 306 Ferdinandea
rect 199 272 222 291 Etna
rect 172 245 209 259 Lipari
rect 158 258 209 268 Vulcanello
rect 208 256 254 268 Vulcano
rect 158 190 196 207 Ischia
rect 194 181 244 194 Vesuvius
rect 165 166 230 180 Monte Nuovo
rect 130 126 164 145 Vulcini
rect 117 101 163 123 Larderello
desc bottom-left

Italy is a volcanically active country, containing the only active volcanoes 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.
==Active volcanoes==
Three of Italy's volcanoes have erupted in the last hundred years:
* Mount Etna, on Sicily (continuous activity)
* Stromboli, one of the Aeolian Islands (continuous activity)
* Mount Vesuvius, near Naples (last erupted in 1944); the only active volcano in mainland Europe.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Volcanology of Italy」の詳細全文を読む



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