Lower Chindwin

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 22.28°N
  • 95.1°E

  • 385 m
    1263 ft

  • 275090
  • Latitude
  • Longitude

  • Summit

  • Volcano

There are no activity reports for Lower Chindwin.

 Available Weekly Reports

There are no Weekly Reports available for Lower Chindwin.

There are no Holocene eruptions known for Lower Chindwin. 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..

Whitford-Stark J L, 1987. A survey of Cenozoic volcanism on mainland Asia. Geol Soc Amer Spec Pap, 213: 1-74.

The Lower Chindwin area contains seven or eight late-Pliocene and Pleistocene explosion craters. Scattered outcrops of basaltic lava flows are found in this area, including an undated, but very recent basalt that forms a plateau north of Thayet-Pingan. A lake-filled crater located at Songyuang is surrounded by olivine basaltic lava flows and pyroclastic material. This region along the lower Chindwin River also contains rhyolitic, dacitic, and andesitic rocks.