Galunggung

Java


SUMMARY:

Type: composite
Activity: active
Last Eruption: 1984 AD
Rock Type: ?
Eruptive Volume: ? cu km
Location Map from Xerox PARC
Latitude: 7.25 S
Longitude: 108.05 E


GEOLOGIC HISTORY

The forested slopes of Galunggung volcano in western Java are cut by a horseshoe-shaped caldera breached to the ESE that has served to channel the products of recent eruptions to the SE. The "Ten Thousand Hills of Tasikmalaya" dotting the plain below the volcano are debris-avalanche hummocks from the collapse that formed the breached caldera about 4,200 years ago.

Historic Activity:

  • Although historical eruptions, restricted to the central vent near the caldera headwall, have been infrequent, they have caused much devastation.
  • The first historical eruption in 1822 produced pyroclastic flows and lahars that killed over 4,000 persons.

Recent Activity:

  • A vigorous explosive eruption from Galunggung began in April 1982, producing large tephra clouds and destroying the 1918 lava dome in the crater. Heavy tephra falls occurred over a wide area, and pyroclastic flows and lahars moved down flank valleys. Explosive activity stopped after extrusion of a small lava flow onto the crater floor in early January 1983.
  • A phreatic explosion on Jan. 9, 1984 produced a cloud that was mostly steam with a little ash.

Data Sources

  • Smithsonian's SEAN Bulletin (V. 7, No. 3 to V. 9, No. 2).

ADDITIONAL INFORMATION


Last Update: 2/27/00