Nabukelevu

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 19.12°S
  • 177.98°E

  • 805 m
    2640 ft

  • 245030
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Nabukelevu.



 Available Weekly Reports

There are no Weekly Reports available for Nabukelevu.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1660 ± 30 years Unknown Confirmed   Radiocarbon (corrected) Dome NW of summit
0340 (?) Unknown Confirmed   Radiocarbon (corrected) West side of summit dome complex
0580 BCE ± 300 years Unknown Confirmed   Radiocarbon (corrected) Summit lava dome

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Cronin S J, Ferland M A, Terry J P, 2004. Nabukelevu volcano (Mt. Washington), Kadavu - a source of hitherto unknown volcanic hazard in Fiji. J Volc Geotherm Res, 131: 371-396.

The andesitic-to-dacitic Nabukelevu lava-dome complex occupies the SW end of Kadavu Island at the southern end of the Fiji archipelago. The high point of the Nabukelevu complex is 805 m Mt. Washington, an andesitic lava dome. Flat-lying dacitic lava flows are found at Cape Washington along the west coast and at Talaulia Bay on the NE coast. NNE-trending faults cut the complex in several locations and define its eastern boundary. The dome complex is cut by several collapse scarps that were the source of debris avalanches that have incorporated human artifacts and remains. Debris avalanches have entered the sea on the both the northern and southern sides of the volcano. Onshore and offshore deposits as well as native legends indicate that several eruptions have occurred at Nabukelevu during the Holocene. Block-and-ash flows related to dome growth have occurred within the past few hundred years.