Raoul Island

Kermadec Islands


SUMMARY

Type: compound
Activity: active
Last Eruption: 1964
Rock Type: dacite
Eruptive Volume: ?
Location Map from Xerox PARC
Latitude: 29.27 S
Longitude: 177.92 E


Geologic Background:

Anvil-shaped Raoul Island, the largest and northernmost of the Kermadec Islands, has been the source of vigorous eruptive activity during the past several thousand years that was dominated by dacitic explosive eruptions. Two small Holocene calderas are found on the island, one at Denham Bay on its west side. The Denham Bay caldera was created during the largest Holocene eruption, a little more than 2100 years before present.

Historic Activity:

  • Historical eruptions during the 19th and 20th centuries have occurred simultaneously from both calderas, and have consisted of small-to-moderate phreatic eruptions, some of which formed ephemeral islands in Denham Bay.
  • Major hydrothermal eruption occurred on Nov. 20, 1964. The 1964 eruption was primarily phreatic and formed 12 small craters in Raoul Caldera. A submarine eruption in Denham Bay is believed to have occurred at about the same time.

Recent Activity:

  • The srongest earthquake swarm since the 1964 eruption occured on March 9, 1993.

Data Sources:

  • Global Volcanism Network (V. 15, No. 3 and V. 18, No. 3).

ADDITIONAL INFORMATION


Last Update: 12/13/00