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Stratovolcano 1784 m (5,853 ft)
North Sulawesi, Indonesia, 1.11°N / 124.73°ECurrent status
(2 out of 5)Soputan webcams / live data
| ReportsSoputan volcano books | ToursSoputan volcano eruptions:
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, 2016Typical eruption style:
Explosive, construction of lava domes, pyroclastic flows, strombolian activity.Last earthquakes nearby
Soputan volcano toursVolcanoes and Spices
(17 days volcano trekking tour to the Molucca Sea: N-Sulawesi, Karangetang and Halmahera)Latest satellite imagesSentinel hub
| Landsat 8
Volcano news: Soputan
Soputan volcano (North Sulawesi, Indonesia) activity update: Continuing decreasing trend of activity
Sunday Oct 14, 2018 04:08 AM | BY: MJFLEGEND
The level of activity is continuing to decline. Seismicity appears to have returned to pre-eruption pattern of low rates. A renewal of high activity remains possible at this highly active volcano, though may be a little less likely than last week.
Tuesday, Oct 09, 2018
Activity at Soputan has decreased since the strong eruptive episode on October 3. Seismicity has dropped to pre-eruption levels and only minor steaming from the summit crater has been observed. Activity could, however, increase again at any time, and the alert level remains at 3 (on a scale of 1-4).
Wednesday, Oct 03, 2018
The volcano erupted this morning at 08:47 local time. The eruption consisted of a sudden large vulcanian explosion which lasted 6 minutes and sent a vertical ash column to approx. 4 km height above the volcano and caused light to moderate ash falls in nearby areas to the W and NW. ...
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.
Source: GVP, Smithsonian Institution
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