Hulubelu

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Hulubelu
Indonesia relief location map.jpg
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Hulubelu
Location on the Indonesian island of Sumatra
Highest point
Elevation 1,040 m (3,410 ft) [1]
Listing List of volcanoes in Indonesia
Coordinates 5°21′S104°36′E / 5.350°S 104.600°E / -5.350; 104.600 [1]
Geography
Location Sumatra, Indonesia
Geology
Mountain type Caldera
Last eruption Unknown [1]

Hulubelu is an elliptical, 4-km-long caldera the floor of which is about 700 m above sea level and is surrounded by steep walls in South-Eastern Sumatra. Post-caldera volcanism formed central cones and basaltic and andesitic flank volcanoes. Solfataric areas, mud volcanoes, and hot springs occur at several locations but it is not known for sure when the volcano last erupted, possibly in the Holocene epoch . Thermal areas are aligned North East of and parallel to the Great Sumatran fault, which runs the entire length of the island of Sumatra.

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A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface. Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018.

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References

  1. 1 2 3 "Hulubelu". Global Volcanism Program . Smithsonian Institution . Retrieved 2006-12-26.