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Fotos al azar
Soputan volcano
Stratovolcano 1784 m (5,853 ft)
North Sulawesi, Indonesia, 1.11°N / 124.73°E
Current status: restless (2 out of 5)
Soputan webcams / datos en tiempo real | Reports
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Erupciones del volcán Soputan:
1785, 1819, 1833(?), 1845, 1890, 1901, 1906, 1907, 1908-09, 1910, 1911-12, 1913, 1915, 1917, 1923-24, 1947, 1953, 1966-67, 1968, 1970, 1971, 1973, 1982, 1984, 1985, 1989, 1991-96, 2000-03, 2004, 2005, 2006, 2007, 2008, 2011, 2012, 2013, 2015, 2016
Typical eruption style:
Explosive, construction of lava domes, pyroclastic flows, strombolian activity.
Últimos terremotos cercanos
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Volcano news: Soputan

más reciente (2018) ... | 2008 | 2007 | | 2006 | 2005
sáb, 23 dic 2006, 04:18

According to the Volcanological Survey of Indonesia,  seismic signals from rockfalls increased at Soputan during 11-13 December. On 14 December, ash clouds rose to an altitude of 2 km (6,600 ft) a.s.l. and ash fell within a 15 km radius of the peak. The emissions were accompanied by thunderous noises that were heard 8 km from the peak. On 15 December the Alert Level was raised from 2 to 3 (on a scale of 1-4) due to this increase in activity.

jue, 1 jun 2006, 15:10

As our correspondant Donald Tapehe from Manado reports, Soputan is getting restless: "Also Mt. Soputan has been showing activity. The local government has determined to raise alert status for all people who live near Mt. Soputan. One week ago my friend (a climber) told me that he saw yellow/brown smoke on the peak of Mt. Soputan from the caldera. Now, it's difficult to take breathe at the campsite, because of the poisonous gasses which blow up from the old crater." 

más reciente (2018) ... | 2008 | 2007 | | 2006 | 2005

Background:

The small Soputan stratovolcano on the southern rim of the Quaternary Tondano caldera on the northern arm of Sulawesi Island is one of Sulawesi's most active volcanoes.  The youthful, largely unvegetated volcano rises to 1784 m and is located SW of Sempu volcano.  It was constructed at the southern end of a SSW-NNE trending line of vents.  During historical time the locus of eruptions has included both the summit crater and Aeseput, a prominent NE-flank vent that formed in 1906 and was the source of intermittent major lava flows until 1924.


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Source: GVP, Smithsonian Institution


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