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There are no activity reports for Kawi-Butak.
There are no Holocene eruptions known for Kawi-Butak. 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.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
The broad Kawi-Butak volcanic massif lies immediately east of Kelut volcano and south of Arjuno-Welirang volcano. The 2551-m-high Gunung Kawi was constructed to the NW of 2868-m-high Gunung Butak. No historical eruptions are known from either volcano, but both are primarily of Holocene age.