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Mount Pangrango

Gede-Pangrango

Stratovulcano · Indonesia · 3026 m

The summit crater (right) of Gede is at the broad summit of the volcano. Gunung Gede is one of the most prominent volcanoes in western Java, immediately adjacent to Pangrango volcano to the NW. Many lava flows are visible on the flanks of the younger Gede. Activity recorded since the 16th century has typically consisted of small explosive eruptions of short duration.
The summit crater (right) of Gede is at the broad summit of the volcano. Gunung Gede is one of the most prominent volcanoes in western Java, immediately adjacent to Pangrango volcano to the NW. Many lava flows are visible on the flanks of the younger Gede. Activity recorded since the 16th century has typically consisted of small explosive eruptions of short duration. · Foto: Photo by Cahya Patria, 2004 (Centre of Volcanology & Geological Hazard Mitigation, Volcanological Survey of Indonesia). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Indonesia
Regione
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitudine
3026 m
Coordinate
-6.786, 106.983
Ultima eruzione
1957
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The two peaks of the Gede-Pangrango volcanic complex overlook the major cities of Cianjur, Sukabumi, and Bogor, situated to the E, S, and NW, respectively. The summit of Gunung Pangrango, constructed over the NE rim of a 3 x 5 km caldera, forms the high point. Many lava flows are visible on the flanks of the younger Gunung Gede to the SE of Pangrango. The steep-walled summit crater has migrated about 1 km NNW over time. Two large debris-avalanche deposits are present on its flanks, one of which underlies the city of Cianjur. Activity recorded since the 16th century has typically consisted of small short explosive eruptions.

Sintesi da Wikipedia

Riassunto in inglese

Mount Pangrango is a dormant stratovolcano located in the Sunda Arc of West Java, Indonesia. The mountain is formed by a subduction zone on the southern coast of Java as part of the Sunda Plate facing the Australian Plate which contains the Indian Ocean. It is located about 80 kilometres (50 mi) south of Jakarta, the capital of Indonesia.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1747~1768 · 2 eruzioni · VEI max. 31831~1852 · 7 eruzioni · VEI max. 31852~1873 · 4 eruzioni · VEI max. 31873~1894 · 6 eruzioni · VEI max. 21894~1915 · 2 eruzioni · VEI max. 21936~1957 · 5 eruzioni · VEI max. 217471789185218941936

Cronologia dettagliata

  1. 1957VEI 2Osservata
    1957-03-13 – 1957-03-13
  2. 1956VEI 2Osservata
    1956-04-28 – 1956-04-28
  3. 1955VEI 1Stima geologica
    1955-07-21 – 1955-08-02
  4. 1948VEI 2Osservata
    1948-11-15 – 1949-02-05
    Kawah Leutik (Kawah Ratu)
  5. 1947VEI 2Osservata
    1947-09-02 – 1948-01-28
    Kawah Ratu?, Kawah Lanang
  6. 1909VEI 1Osservata
    1909-05-02 – 1909-05-02
  7. 1899VEI 2Osservata
    1899-05-01 – 1899-05-14
  8. 1891VEI 2Osservata
    1891 – In corso
  9. 1889VEI 1Stima geologica
    1889-05-08 – In corso
  10. 1888VEI 2Osservata
    1888 – In corso
  11. 1887VEI 2Osservata
    1887-10-22 – 1887-10-22
  12. 1886VEI 2Osservata
    1886-06-10 – 1886-08-16
  13. 1885VEI 2Stima geologica
    1885-01 – 1885-02
  14. 1870VEI 2Osservata
    1870-08 – 1870-10-03
  15. 1866VEI 2Osservata
    1866-09-18 – In corso
  16. 1853VEI 3Osservata
    1853-03-14 – 1853-03-14
  17. 1852VEI 2Osservata
    1852-05-28 – 1852-05-28
  18. 1848VEI 2Osservata
    1848-05-08 – In corso
  19. 1847VEI 2Osservata
    1847-10-17 – 1847-10-18
  20. 1845VEI 2Osservata
    1845-01-23 – 1845-03-05
  21. 1843VEI 2Osservata
    1843-07-28 – In corso
  22. 1840VEI 3Osservata
    1840-11-12 – 1840-12-11
  23. 1839VEI ?Stima geologica
    1839 – In corso
  24. 1832VEI 3Osservata
    1832-08-29 – 1832-08-29
  25. 1761VEI 2Osservata
    1761 – In corso
  26. 1747VEI 3Osservata
    1747 – 1748

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