Kuchinoerabu-jima

Japan - Ryukyu Islands


SUMMARY:

Type: composite
Activity: active
Last Eruption: 1980 AD
Rock Type: andesitic
Eruptive Volume: ? cu km
Location Map from Xerox PARC
Latitude: 30.43 N
Longitude: 130.22 E


Geologic Background:

A group of young stratovolcanoes forms the eastern end of Kuchinoerabu-jima island. Furu-dake, Shin-dake, and Sankakuten-yama were erupted from south to north, respectively, to form a composite cone that is parallel to the trend of the Ryukyu Islands. The youngest cone, Shin-dake, was formed after the NW side of Furu-dake was breached by an explosion. All historical eruptions have occurred from Shin-dake, although a lava flow from the south flank of Furu-dake that reached the coast has a very fresh morphology.

Historic Activity:

  • Shin-dake is the summit cone and vented the 13 known eruptions that have occurred since 1840.
  • Several villages on the 4 x 12 km island are located within a few kilometers of the active crater of Shindake and have suffered damage from historical eruptions.

Recent Activity:

  • Earthquakes began to increase in January 1996. January (32), February (40), March (77), April (91), May (86), June (75), July (25), August (62),

Data Sources:

  • Global Volcanism Network (V. 21, No. 3 to V. 24, No. 8).

ADDITIONAL INFORMATION


Last Update: 12/10/00