The discovery was made by an international team of geoscientists and volcanologists, led by researchers at the University of Geneva (UNIGE) in Switzerland, as well as Italy’s Institute of Geosciences and Earth Resources, and the Italian National Institute of Geophysics and Volcanology.<\/p>\n “We knew that this region, which extends from north to south across Tuscany, is geothermally active, but we did not realize it contained such a large volume of magma, comparable to that of supervolcanic systems such as Yellowstone,” explains<\/a> lead author and geoscientist Matteo Lupi from UNIGE.<\/p>\n The size of the magma reservoir beneath Tuscany was measured using a network of seismometers, which can probe the subsurface sort of like an X-ray<\/a> for the Earth. Using the resulting data, Lupi and his colleagues modeled the upper 15 kilometers of continental crust in Tuscany.<\/p>\n “These results are important both for fundamental research and for practical applications, such as locating geothermal reservoirs or deposits rich in lithium<\/a> and rare earth elements<\/a>, which are used, for example, in electric vehicle batteries,” explains<\/a> Lupi.<\/p>\n “In addition to their great scientific interest, these studies show that tomography, by exploring the subsoil quickly and at low cost, can be a useful tool for the energy transition.”<\/p>\n The team’s interpretation of their data is that the middle crust of the Tuscany region is home to a large magmatic reservoir.<\/p>\n The sheer volume of the network, the authors write<\/a>, is on par with “those of some of the largest eruptive systems worldwide, such as Taup\u014d<\/a>, Long Valley<\/a>, and Yellowstone. All these volcanic systems featured super-eruptions.”<\/p>\n In Tuscany, however, there is no recognized eruption associated with this geothermal system.<\/p>\n With nowhere to go, scientists predict that in the shallow subsurface, supercritical fluids could exceed temperatures of 500 \u00b0C (932 \u00b0F).<\/p>\n Related: One of Earth’s Most Explosive Volcanoes Is Quietly Refilling With Magma<\/a><\/p>\n “The reason why this large amount of melt never gave rise to eruptions is enigmatic and debated,” the authors conclude<\/a>.<\/p>\n “Such partial melts may help understand the long-term evolutionary processes taking place at volcanic systems that featured super-eruptions and in regional-scale high-enthalpy systems that have not (yet?) erupted.”<\/p>\n![\"Tuscany](\"https:\/\/www.newsbeep.com\/us\/wp-content\/uploads\/2026\/04\/TuscanyMagma-642x230.png\")
Conceptual model of the Tuscan Magmatic Province. (Lupi et al., Communications Earth & Environment<\/a>, 2026)<\/p>\n![\"Subscribe](\"https:\/\/www.newsbeep.com\/us\/wp-content\/uploads\/2026\/03\/Generic-Health-Promo-Final-642x273.jpg\")
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