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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): occasional minor ash emissions
Tuesday May 05, 2020 07:04 AM | BY: MARTIN
Plume rising from Soputan volcano on 4 May (image: PVMBG)
Volcanic Ash Advisory Center (VAAC) Darwin recorded on 2 May at 00:07 local time
new emissions of steam and ash that rose 1,148 ft (350 m)
above the summit.
PVMBG recorded 51 volcano-tectonic earthquakes.
The warning bulletin states that ballistic impacts of volcanic bombs, pyroclastic flows and lava flows could affect an area of about 1.5 km distance from the main crater and 2.5 km zone away on the SW side.
Monday, Mar 23, 2020
Volcanic Ash Advisory Center (VAAC) Darwin recorded an explosive activity from the active crater with ash emissions that reached 14,000 ft (4,267 m)
Wednesday, Dec 19, 2018
Following the recent vigorous eruptive phase, activity is gradually declining, though at a slower rate than after the previous phase in early October. Another phase of strong eruption could begin quickly again in the volcano's current and somewhat-temperamental state.
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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