Kana Keoki

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 8.75°S
  • 157.03°E

  • -700 m
    -2296 ft

  • 255052
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Kana Keoki.



 Available Weekly Reports

There are no Weekly Reports available for Kana Keoki.

There are no Holocene eruptions known for Kana Keoki. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

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.

Exon N F, Johnson R W, 1986. The elusive Cook volcano and other submarine forearc volcanoes in the Solomon Islands. Aust Bur Min Resour Geol Geophys J, 10: 77-83.

Taylor B, 1987. A geophysical survey of the Woodlark-Solomons region. In: Taylor B and Exon N F (eds) {Marine Geology, Geophysics, and Geochemistry of the Woodlark Basin, Solomon Islands}, Circum-Pacific Council Energy Min Resour Earth Sci Ser, 7: 25-48.

Tiffin D L, Taylor B, Crook K A W, Sinton J, Frankel E, 1986. Surveys in the Solomon Islands and Papua New Guinea using SEAMARC II--A Cruise Report of the R/V Moana Wave, November 29, 1985 - January 9, 1986. CCOP/SOPAC Cruise Rpt 117 (unpublished).

Bathymetry and petrologic evidence indicated the presence of an active dacitic submarine volcano SW of Rendova Island (Taylor, 1987). Kana Keoki Seamount, located along the Ghizo Ridge south of the convergent margin between the Indo-Australian and Pacific plates, rises to within about 700 m of the surface from a depth of 3700 m and is surrounded by a volcaniclastic apron.