How big was the eruption of Mount Tambora?
The Eruption of Mount Tambora: Causes, Event, Effect. In 1815, Mount Tambora famously erupted, with the explosion being a 7 on the volcanic explosivity index, which easily made it the highest rated eruption since Lake Taupo in 1815. It is estimated that the eruption produced 160 cubic kilometres of magma.
Who was the Governor of Java during the Tambora eruption?
Accounts of the Tambora eruption were considerably rarer, yet some vivid ones do exist. An administrator of the East India Company, Sir Thomas Stamford Bingley Raffles, who was serving as governor of Java at the time, published a striking account of the disaster based on written reports he had collected from English traders and military personnel.
Why was the eruption of Krakatoa overshadowed by the Tambora eruption?
The disaster on the remote island of Sumbawa in the Indian Ocean has been overshadowed by the eruption of the volcano at Krakatoa decades later, partly because the news of Krakatoa traveled quickly via telegraph. Accounts of the Tambora eruption were considerably rarer, yet some vivid ones do exist.
How long did it take for the ash from Mount Tambora to settle?
The eruption column reached the stratosphere at an altitude of more than 43 kilometres (141,000 ft). The coarser ash particles settled out one to two weeks after the eruptions, but the finer ash particles stayed in the atmosphere from a few months to a few years at altitudes of 10–30 kilometres (33,000–98,000 ft).
Is the lava dome on Mount Tambora still active?
Mount Tambora is still active and minor lava domes and flows have been extruded on the caldera floor during the 19th and 20th centuries.
Why is Mount Tambora important to the world?
Besides the seismologists and vulcanologists who monitor the mountain’s activity, Mount Tambora is an area of interest to archaeologists and biologists. The mountain also attracts tourists for hiking and wildlife activities, though in small numbers.