Last edited on 23 February 2021, at 21:00 Content is available under CC BY-SA 3.0 unless otherwise noted. The trachydacitic domes and associated lava flows, which were emplaced following the eruptions of rhyodacitic ignimbrites during the Pliocene, were erupted along regional ENE-WSW-trending faults. The results of a research carried out to draw up a map of the Mount Amiata vegetation to a scale of 1:25.000 are here shown. MONTE AMIATA. The Monte Amiata with its 1738 meters s.l.m. The major volcanological arguments debated on Amiata, during the last 55 years, is the occurrence of explosive eruptions and the emplacement of pyroclastic flow deposits during its activity. Italy's Volcanoes is back !!! All of this and everything else on Monte Amiata. One of the largest beech woods in Italy, unique trails immersed in greenery and nature. The largest of the domes is 1738-m-high Monte Amiata (La Vetta), a compound lava dome with a trachytic lava flow that extends to the east. Last modified on 21 November 2012. The massif is what remains of an ancient extinct volcano, whose last eruption dates back more than 700,000 years ago. Well, you will not find any new updates on volcanic activity here (for this you have to visit the web site of the Osservatorio Etneo (Catania section) of the Istituto Nazionale di Geofisica e Vulcanologia), but you will find the site very much as it was since I put it into a state of hibernation in the spring of 2005. dominates the Maremma, Val d'Orcia and Val di Chiana. A Late Pleistocene eruption occurred along a crustal fissure striking N50° (Mt Amiata Fault), which crosscuts the crustal dome. This page was last edited on 23 February 2021, at 21:00 (UTC) . Inhabited since prehistoric times the area of Mount Amiata has never been particularly populous. As a result of former volcanic activity the surrounding area is dotted with a number of thermal springs. The M. Amiata is an isolated mountain which arose in southern Tuscany from Pleistocene volcanic eruptions. For a volcano to be labeled “extinct” it must not have had any recent activity and since the The last eruption was recorded about 180,000 years ago. Hydrothermal circulation, proven by the occurrence of thermal springs and gas vents (mainly CO2 and H2S), mainly occurs along the Mt Amiata Fault both in the northeastern ans southwestern sides of the volcano. A new geochronological and geochemical study was carried out to better constrain the petrogenesis and eruptive history of Monte Amiata, a large Pleistocene trachydacitic volcano of Southern Tuscany. Monte Amiata is an extinct volcano with a peak at an altitude of 1,738 meters above sea level. The lava dome complex of Monte Amiata erupted for the last time in the late Pleistocene, 231,000 years ago. 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