29/9/1538: è la data dell'ultima eruzione avvenuta ai Campi Flegrei, che diede forma al M. Nuovo. In questo articolo ripercorriamo la storia dei precursori dell'eruzione e poi gli eventi dell'eruzione vera e propria, sulla base di numerose fonti storiche.
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Il 29 settembre di 25 anni fa nasceva il nostro Istituto, l'INGV!
A partire da oggi, inizia una lunga sequenza di eventi su tutto il territorio nazionale. Nell'articolo qui sotto, tutte le info ed anche un portale in continuo aggiornamento: stay tuned!
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September 29, 1538, the last historic eruption in the Campi Flegrei, the famous supervolcano near Naples, starts. In the following 5 months volcanic material build up a 133 meters high cone called Monte Nuovo - the New Mountain (red spot in this 1892 geological map)
September 27, 2014, 63 people are killed when Mount Ontake (Japan) unexpectedly erupts with a phreatic eruption.
A phreatic eruption occurs when water touches magma beneath the earth's surface, leading to the rapid conversion of water into steam
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Fantastic Rhodochrosite with Fluorite, Tetrahedrite, Chalcopyrite on Quartz from Steve’s Pocket, Sweet Home Mine, Colorado.
Photo: Thomas Spann
Credit: Mineral Masterpiece
This is a common misconception. Diamonds and coal are both formed deep within the Earth's crust, but under vastly different conditions:
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Ferruginous Quartz, also known as red quartz, is a variety of quartz that is colored red by the presence of iron oxide. The iron oxide can be in the form
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September 10, 1509, estimated 1000 to 10,000 people died in Constantinople (modern Istanbul) due to an Mw 7+ #earthquake so strong, it was named “the Lesser Judgement Day.” The quake was followed by a tsunami on the Black Sea
September 11, 1522, birthday of Italian naturalist Ulisse Aldrovandi. He studied & classified rocks🪨& minerals💎 recognizing the organic origin of some fossils🐚
Also used the word "la giologia" #geology ⚒️ as #science of unearthed things for the 1st time
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After an eruption destroyed the city of St. Pierre (Martinique) & killed 30.000 people, a 300 meters high pinnacle made from the cooling, high-viscosity lava was pushed upwards from the volcanic vent of La Pelée. It collapsed in September 1903
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