Karangetang
Indonesia's Relentless Island Volcano
1,797 m
2023
Stratovolcano
Indonesia
Location
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Volcanic Hazards & Risk Assessment
Primary Hazards
- Pyroclastic flows
- Lava flows
- Volcanic bombs and ballistics
- Lahars and mudflows
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 3 years ago | Very Recent | Currently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Authority Sources
Interesting Facts
Karangetang has erupted more than 60 times since 1675, making it one of the most frequently active volcanoes in all of Indonesia.
The volcano's alternative name, Api Siau, translates to 'Fire of Siau' in the local Sangirese language.
Siau Island, entirely dominated by the Karangetang edifice, measures only 17 km by 8 km yet supports roughly 22,000 residents.
Five summit craters are aligned on a north–south axis across the peak — an unusual configuration reflecting deep structural controls.
Pyroclastic flows from the summit can reach the coast in under ten minutes due to the volcano's steep flanks and short run-out distance of approximately 5 km.
Siau Island is one of Indonesia's largest producers of cloves, cultivated on the fertile lower slopes of the volcano.
The volcano sits on the Sangihe Volcanic Arc, formed by the rare double subduction of the Molucca Sea Plate beneath both the Sangihe and Halmahera arcs.
Karangetang was active in every single decade of the 20th century, with 37 recorded eruptions between 1900 and 1999.
The submarine base of the Karangetang edifice rises approximately 3,000 m from the seafloor, making the total structure far larger than the visible island.
Evacuation from Siau Island must occur by sea, as the island has no airport — a major constraint on emergency response planning.