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As clarification, the name Tianchi is used to refer to the ~ 5 km diameter summit caldera vent of the volcanic complex, and the name Changbaishan is used to refer to the complex in general.

The latter name has many synonyms, including Baegdu, Baekdoosan, Baitoushan, Chang-pai-shan, Hakuto, and P'aektu-san.

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A histogram of the annual number of earthquakes from 2002 through 2005 shows a peak in 2003.

Focusing on Changbaishan volcano and its summit caldera called Tianchi, Tianchi Volcano Observatory (TVO) released data collected since it formed in 1999.

This report will summarize both the TVO's monitoring network and their findings from 1999 to 2010, focusing on the seismic crisis during mid-2002 to mid-2005.

From fluid geochemistry measurements, Liu and others (2011) reported that H China National Report on Volcanology and Chemistry of the Earth's Interior, for the 25th General Assembly of IUGG, Melbourne, Australia, 28 June-7 July 2011 (prepared by the Chinese National Committee for the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI)), pgs. Liu, G., Yang, J., Wang, L., and Sun, J., 2011, The active level analysis of Changbaishan volcano, China National Report on Volcanology and Chemistry of the Earth's Interior, for the 25th General Assembly of IUGG, Melbourne, Australia, 28 June - 7 July 2011 (prepared by the Chinese National Committee for the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI)), pgs. Machida, H., and Arai, F., 1983, Extensive ash falls in and around the Sea of Japan from large late Quaternary eruptions, Journal of Volcanology and Geothermal Research, v. The official Xinhua News Agency quoted Ruoxin Liu from the State Seismological Bureau, but we have received no direct confirmation.

Charles Dunlap, Susanne Horn, and Hans Schmincke worked on and around the summit with Chinese geologist Tang Deping during 21-25 July 1993, but saw no emissions.

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