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Kawah Ijen

Ijen

Stratovulcano · Indonesia · 2769 m

Active fumaroles on the SE crater wall of the highly acidic Kawah Ijen crater lake, within one of the cones that formed in the 20-km-wide Ijen caldera. The 1-km-wide turquoise-colored crater lake is near the eastern rim of Ijen caldera and has been the site of phreatic eruptions in historical time and is noted for its sulfur deposits.
Active fumaroles on the SE crater wall of the highly acidic Kawah Ijen crater lake, within one of the cones that formed in the 20-km-wide Ijen caldera. The 1-km-wide turquoise-colored crater lake is near the eastern rim of Ijen caldera and has been the site of phreatic eruptions in historical time and is noted for its sulfur deposits. · Foto: Photo by Tom Casadevall, 1987 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Indonesia
Regione
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
Altitudine
2769 m
Coordinate
-8.058, 114.242
Ultima eruzione
1999
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The Ijen volcano complex at the eastern end of Java consists of a group of small stratovolcanoes constructed within the 20-km-wide Ijen (Kendeng) caldera. The north caldera wall forms a prominent arcuate ridge, but elsewhere the rim was buried by post-caldera volcanoes, including Gunung Merapi, which forms the high point of the complex. Immediately west of the Gunung Merapi stratovolcano is the historically active Kawah Ijen crater, which contains a nearly 1-km-wide, turquoise-colored, acid lake. Kawah Ijen is the site of a labor-intensive mining operation in which baskets of sulfur are hand-carried from the crater floor. Many other post-caldera cones and craters are located within the caldera or along its rim. The largest concentration of cones forms an E-W zone across the southern side of the caldera. Coffee plantations cover much of the caldera floor; nearby waterfalls and hot springs are tourist destinations.

Sintesi da Wikipedia

Il complesso vulcanico di Kawah Ijen è un gruppo di stratovulcani nella Reggenza di Banyuwangi, in Indonesia, nella parte orientale di Giava. È all'interno della grande caldera Ijen, larga circa 20 chilometri. Lo stratovulcano Gunung Merapi è il punto più alto del complesso. Il nome "Merapi" significa "montagna di fuoco" in lingua indonesiana; Monte Merapi, nel centro di Giava, e Marapi, a Sumatra, hanno la stessa etimologia.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
640 BCE~451 BCE · 1 eruzioni · VEI max. ?1625~1813 · 1 eruzioni · VEI max. 21813~2002 · 9 eruzioni · VEI max. 2640 BCE74 BCE68112471813

Cronologia dettagliata

  1. 2002VEI 1Stima geologica
    2002-07-29 – 2002-08-15
    Kawah Ijen
  2. 2000VEI 1Stima geologica
    2000-09-01 – 2000-09-10
    Kawah Ijen
  3. 1999VEI 1Osservata
    1999-06-28 – 1999-06-28
    Kawah Ijen
  4. 1994VEI 1Osservata
    1994-02-03 – 1994-02-03
    Kawah Ijen
  5. 1993VEI 1Osservata
    1993-07-03 – 1993-08-01
    Kawah Ijen
  6. 1952VEI 1Osservata
    1952-04-22 – 1952-04-24
    Kawah Ijen
  7. 1936VEI 2Osservata
    1936-11-05 – 1936-11-25
    Kawah Ijen
  8. 1917VEI 1Osservata
    1917-02-25 – 1917-03-14
    Kawah Ijen
  9. 1817VEI 2Osservata
    1817-01-15 – 1817-02-18
    Kawah Ijen
  10. 1796VEI 2Osservata
    1796 – In corso
    Kawah Ijen
  11. 640 a.C. (±50 anni)VEI ?Stima geologica
    BCE 640 – In corso
    Kawah Ijen

Link esterni

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