Portal:Geography/Featured article/11

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Mount Tambora is an active stratovolcano on Sumbawa island, Indonesia. Sumbawa is flanked both to the north and south by oceanic crust and Tambora was formed by the active subduction zones beneath it. This process raised Mount Tambora as high as 4,300 m (14,000 ft), making it one of the tallest peaks in the Indonesian archipelago, and drained off a large magma chamber inside the mountain. In 1815, Tambora erupted with a rating of seven on the volcanic explosivity index; the largest eruption since the Lake Taupō eruption in AD 181. With an estimated ejecta volume of 160 km3 (38 cu mi), Tambora's 1815 outburst was the largest volcanic eruption in recorded history. Heavy volcanic ash falls were observed as far away as Borneo, Sulawesi, Java and Maluku islands. Most deaths from the eruption were from starvation and disease, as the eruptive fallout ruined the local agriculture. The death toll was at least 71,000 people, of whom 11,000–12,000 were killed directly by the eruption. The eruption created global climate anomalies in the following years. 1816 became known as the Year Without a Summer because of the impact on North American and European weather. During an excavation in 2004, a team of archaeologists discovered a civilization obliterated by the 1815 eruption, known as the "Pompeii of the East".