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The Global Volcanism Program has no activity reports for Telomoyo.
The Global Volcanism Program has no Weekly Reports available for Telomoyo.
The Global Volcanism Program has no Bulletin Reports available for Telomoyo.
Telomoyo volcano, also spelled Telemojo, was constructed over the southern flank of the eroded Pleistocene Soropati volcano and is in part of Holocene age (van Bemmelen 1941). It lies along a NNW-SSE-trending line of volcanoes extending from Ungaran in the north to Merapi in the south. The eastern flank of Soropati volcano collapsed during the Pleistocene, leaving a U-shaped depression. Telomoyo subsequently filled much of the southern side of this depression and grew to a height of 600 m above its rim.
The Global Volcanism Program is not aware of any Holocene eruptions from Telomoyo. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Telomoyo page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Telomojo | Telemojo|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Kendil, Gunung||Cone||1273 m|
|The two small peaks at the left are part of the Telomoyo volcanic complex, which was constructed along a NNW-SSE-trending line of volcanoes extending from Ungaran in the north to Merapi in the south. Telomoyo filled much of the southern side of a depression formed by collapse of the Pleistocene Soropati volcano and grew to a height of 600 m above its rim. The two towering conical peaks in the background are Sumbing (L) and Sundoro (R); Slamet volcano is on the far right horizon.
Photo by Hideko and Minoru Kusakabe, 2000 (Okayama University).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
van Bemmelen R W, 1941. Bulletin of the East Indian Volcanology Survey for the year 1941. East Indian Volc Surv Bull, 95-98: 1-110.