Baluan

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 2.57°S
  • 147.28°E

  • 254 m
    833 ft

  • 250020
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Baluan.



 Available Weekly Reports

There are no Weekly Reports available for Baluan.

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

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
[ 1931 ] [ Unknown ] Uncertain 0  

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.

Johnson R W, 1990. . (pers. comm.).

Johnson R W, Davies R A, 1972. Volcanic geology of the St. Andrew Strait Islands, Bismarck Sea, Papua New Guinea. Geol Surv Papua New Guinea, Note on Invest, 72-002: 1-29.

Katsui Y (ed), 1971. List of the World Active Volcanoes. Volc Soc Japan draft ms, (limited circulation), 160 p.

Reynolds M A, Best J G, Johnson R W, 1980. 1953-57 eruption of Tuluman volcano: rhyolitic volcanic activity in the northern Bismarck Sea. Geol Surv Papua New Guinea Mem, 7: 1-44.

The circular, 5.5-km-wide island of Baluan in the Admiralty Islands is formed by a Pleistocene stratovolcano with a large summit crater and several flank vents. Some of these might be of Holocene age (Johnson 1990, pers. comm.). In contrast to its neighboring islands to the north, Baluan has erupted basaltic rather than rhyolitic rocks. Sabroma, the elliptical summit crater, has a maximum width of about 1 km. The arcuate rim of the Batapona Mountain pyroclastic cone is prominent at the north edge of the island. Several small islands consisting of cone remnants are located within a kilometer of the north coast. Warm springs occur along the coast. The only historical activity is an uncertain report of a submarine eruption near the island in 1931.