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Mt. Amiata (Southern Tuscany, Central Italy) is an extinct Quaternary volcano located in an area still marked by high heat-flow that is caused by deep seated (6-10 km) hot masses related to Pliocene magmatic activity. The anomalous geothermal gradient giv
Mt. Amiata (Southern Tuscany, Central Italy) is an extinct Quaternary volcano located in an area still marked by high heat-flow that was caused by deep seated (6-10 km) hot masses related to Pliocene magmatic activity. The anomalous geothermal gradient giv