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Geureudong

Telong, Bur ni

성층화산 · Indonesia · 2617m

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. · 사진: Photo by Cahya Patria, 2004 (Centre of Volcanology & Geological Hazard Mitigation, Volcanological Survey of Indonesia). · Wikimedia Commons
화산 유형
성층화산
국가
Indonesia
지역
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
해발
2617m
좌표
4.769, 96.821
마지막 분화
1937년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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.

Wikipedia 요약

영어 요약

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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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1837~1847 · 2건 · 최고 VEI 21847~1857 · 1건 · 최고 VEI 21917~1927 · 2건 · 최고 VEI 21927~1937 · 1건 · 최고 VEI ?18371857188719071927

상세 타임라인

  1. 1937년VEI ?관측 기록
    1937 ~ 진행 중
  2. 1924년VEI 2지질학적 추정
    1924-12-07 ~ 진행 중
  3. 1919년VEI 2관측 기록
    1919-12 ~ 진행 중
  4. 1856년VEI 2관측 기록
    1856-04-14 ~ 진행 중
  5. 1839년VEI 2관측 기록
    1839-01-12 ~ 1839-01-13
  6. 1837년VEI 2관측 기록
    1837-09-25 ~ 진행 중

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