The Utilisation of Volcanic Steam in Italy

Appropriateness of hospital utilisation

Appropriateness of hospital utilisation in Italy

✍ IF Angelillo; G Ricciardi; N Nante; A Boccia; A Bianco; G La Torre; V Vinci; M D 📂 Article 📅 2000 🏛 Elsevier Science 🌐 English ⚖ 74 KB

Volcanic steam output directly measured

Volcanic steam output directly measured in fumaroles: the observed variations at Vulcano Island, Italy, between 1983 and 1987

✍ F Italiano; P M Nuccio 📂 Article 📅 1992 🏛 Springer-Verlag 🌐 English ⚖ 710 KB

Economy in the generation and utilisatio

Economy in the generation and utilisation of steam. Part I

✍ Wade, Chas. F. 📂 Article 📅 1924 🏛 Wiley (John Wiley & Sons) ⚖ 399 KB

Wlien wc talk nbout " coal," i t is not suficicntly rcaliscd that this is n gcncrnl namc for a class of mntcriol rathcr than a substnncc of tlefinitc composition nnd chnrnctcristics. Con1 may rangc from thc almost pure carbon known as antliracitc to tlic scmilignite with no uncombincd cnrbon in its

Volcanic hazard mapping in the Aeolian I

Volcanic hazard mapping in the Aeolian Islands (Italy)

📂 Article 📅 2010 🏛 John Wiley and Sons 🌐 English ⚖ 217 KB

Plio-Quaternary Volcanism in Italy || Th

Plio-Quaternary Volcanism in Italy || The Tuscany Province

✍ , 📂 Article 📅 2005 🏛 Springer-Verlag 🌐 German ⚖ 936 KB

Central-Southern Italy and the Tyrrhenian Sea are the sites of extensive Plio-Quaternary magmatic activity. The rock compositions include crustal anatectic granites and rhyolites, tholeiitic, calc-alkaline, shoshonitic volcanics, and potassic to ultrapotassic and Na-alkaline volcanics. This very wid

Plio-Quaternary Volcanism in Italy || Th

Plio-Quaternary Volcanism in Italy || The Ernici-Roccamonfina Province

✍ , 📂 Article 📅 2005 🏛 Springer-Verlag 🌐 German ⚖ 646 KB

Central-Southern Italy and the Tyrrhenian Sea are the sites of extensive Plio-Quaternary magmatic activity. The rock compositions include crustal anatectic granites and rhyolites, tholeiitic, calc-alkaline, shoshonitic volcanics, and potassic to ultrapotassic and Na-alkaline volcanics. This very wid