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Report on Lokon-Empung (Indonesia) — March 1986


Lokon-Empung

Scientific Event Alert Network Bulletin, vol. 11, no. 3 (March 1986)
Managing Editor: Lindsay McClelland.

Lokon-Empung (Indonesia) Explosions empty crater lake; mud flows

Please cite this report as:

Global Volcanism Program, 1986. Report on Lokon-Empung (Indonesia) (McClelland, L., ed.). Scientific Event Alert Network Bulletin, 11:3. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198603-266100



Lokon-Empung

Indonesia

1.358°N, 124.792°E; summit elev. 1580 m

All times are local (unless otherwise noted)


"Activity began 22 March at 0336 with a small phreatic eruption from the Tompaluan Crater . . . . A small (700,000 m3) crater lake within Tompaluan crater was ~60% evacuated during the 22 March eruption. A larger, phreatomagmatic eruption occurred on 24 March at 0343, emptying the remainder of the lake and throwing out incandescent ballistic blocks to heights of 800-1,000 m. Mudflows were produced during both eruptions. No casualties or damage have been reported. Small explosions occurred on 29 March at 1547 to 250 m height, at 1806 to 300 m, and at 1817 to 200 m. The VSI observation post is located at Kakaskasen, ~5 km SE of the volcano. The observatory has one vertical component seismometer, located at Lokon."

Geological Summary. The Lokong-Empung volcanic complex, rising above the plain of Tondano in North Sulawesi, includes four peaks and an active crater. Lokon, the highest peak, has a flat craterless top. The morphologically younger Empung cone 2 km NE has a 400-m-wide, 150-m-deep crater that erupted last in the 18th century. A ridge extending 3 km WNW from Lokon includes the Tatawiran and Tetempangan peaks. All eruptions since 1829 have originated from Tompaluan, a 150 x 250 m crater in the saddle between Lokon and Empung. These eruptions have primarily produced small-to-moderate ash plumes that sometimes damaged croplands and houses, but lava-dome growth and pyroclastic flows have also occurred.

Information Contacts: Suratman, A. Sudradjat and T. Casadevall, VSI.