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Fotos al azar
Lokon volcano
Lokon volcano
Latest news from Lokon volcano
Earthquake swarm at Lokon volcano on 8 Mar 2016 (VSI)
Wednesday, Mar 09, 2016
Una advertencia fue emitida por el volcán y su nivel de alerta elevado a 3 ("siaga" - alerta, en una escala de 1-4) el lunes pasado después de que se detectó un enjambre sísmico que se produzca bajo el edificio. ... [Leer más]
Seismic activity at Lokon volcano 1-12 Jan 2016 (VSI)
Wednesday, Jan 13, 2016
El volcán permanece en disturbios importantes y moderados a grandes explosiones pueden ocurrir en cualquier momento, el último informe de evaluación de los Estados de Observatorio del volcán y alerta nivel 3 ("siaga") se mantiene en una escala de 1-4. ... [Leer más]
 

Lokon-Empung volcano

Stratovolcano 1580 m / 5,184 ft
North Sulawesi, Indonesia, 1.36°N / 124.79°E
Current status: restless (2 out of 5)
Lokon-Empung webcams / datos en tiempo real | Reports
Lokon-Empung volcano books | Tours
Last update: 9 Mar 2016 (seismic unrest, eruption warning)
Typical eruption style: Small-moderate explosive eruptions.
Erupciones del volcán Lokon-Empung: 1375, 1775, 1829, 1893-94, 1930, 1942, 1948, 1951-53, 1958-59, 1961, 1962, 1963-64, 1965, 1966, 1969-70, 1971, 1973-74, 1975-80, 1984(?), 1986-87, 1988, 1991-92, 2000-01, 2002, 2002-03, 2011, 2011-12, 2012-13, 2015
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Sun, 7 Jul 2019
Sun, 7 Jul 21:10 UTCM 3.6 / 10 km11 kmNorthern Molucca Sea (Indonesia)
The twin volcanoes Lokon and Empung, rising about 800 m above the plain of Tondano, are among the most active volcanoes of Sulawesi.
Lokon, the higher of the two peaks (whose summits are only 2.2 km apart), has a flat, craterless top. The younger Empung volcano has a 400-m-wide, 150-m-deep crater that erupted last in the 18th century, but all subsequent eruptions have originated from Tompaluan, a 150 x 250 m wide double crater situated in the saddle between the two peaks.
Historical eruptions have primarily produced small-to-moderate ash plumes that have occasionally damaged croplands and houses, but lava-dome growth and pyroclastic flows have also occurred.

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