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Geureudong

Telong, Bur ni

Estratovolcán · Indonesia · 2617 m

Historically active Bur ni Telong volcano, seen here from the SE, was constructed on the southern flank of Bur ni Geureudong volcano, part of which is visible in the background. The two summits of the complex are 4.5 km apart and are similar in elevation. The summit crater has migrated to the ESE, leaving arcuate crater rims. Lava flows are exposed on the southern flank. Explosive eruptions were recorded during the 19th and 20th centuries.
Historically active Bur ni Telong volcano, seen here from the SE, was constructed on the southern flank of Bur ni Geureudong volcano, part of which is visible in the background. The two summits of the complex are 4.5 km apart and are similar in elevation. The summit crater has migrated to the ESE, leaving arcuate crater rims. Lava flows are exposed on the southern flank. Explosive eruptions were recorded during the 19th and 20th centuries. · Foto: Photo by Cahya Patria, 2004 (Centre of Volcanology & Geological Hazard Mitigation, Volcanological Survey of Indonesia). · Wikimedia Commons
Tipo
Estratovolcán
País
Indonesia
Región
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitud
2617 m
Coordenadas
4.769, 96.821
Última erupción
1937
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The conical Bur ni Telong volcano was constructed at the southern base of the massive Bur ni Geureudong volcanic complex, one of the largest in northern Sumatra. The historically active volcano lies 4.5 km from the summit of Geureudong,and its summit crater has migrated to the ESE, leaving arcuate crater rims. Lava flows are exposed on the southern flank. Explosive eruptions were recorded during the 19th and 20th centuries.

Resumen de Wikipedia

Resumen en inglés

Geureudong or Bur ni Geureudong or Bur ni Telong is a stratovolcanic complex in northern Sumatra, Indonesia. The official name of the whole complex is confusing between the two adjacent volcanoes: Bur ni Geureudong and Bur ni Telong. Two other volcanic cones are Salah Nama and Pepanji, and there are small sediment hills. Bur ni Geureudong has been eroded since the Pleistocene age, but has solfatara and hot springs on its flanks. Bur ni Telong is located in the south of Bur ni Geureudong. Bur ni Telong has active crater that lava flows are exposed in the southern flank.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1837~1847 · 2 erupciones · VEI máx. 21847~1857 · 1 erupciones · VEI máx. 21917~1927 · 2 erupciones · VEI máx. 21927~1937 · 1 erupciones · VEI máx. ?18371857188719071927

Línea de tiempo detallada

  1. 1937VEI ?Observado
    1937 – En curso
  2. 1924VEI 2Estimación geológica
    1924-12-07 – En curso
  3. 1919VEI 2Observado
    1919-12 – En curso
  4. 1856VEI 2Observado
    1856-04-14 – En curso
  5. 1839VEI 2Observado
    1839-01-12 – 1839-01-13
  6. 1837VEI 2Observado
    1837-09-25 – En curso

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.