Contents of halide ions (F-, Cl-, Br- and I-) of twelve hot spring wat
ers in the Kusatsu-Shirane volcano area were determined using ion chro
matography. High correlations were observed among those ions, which in
dicated that they were of the same origin, that is, they were all deri
ved by the volcanic activity of Mt. Kusatsu-Shirane. Secular changes i
n F-, Cl- and Br- contents of Kusatsu-Yubatake and Bandaiko hot spring
waters and Yugama lake water since around 1970 were presented. Increa
ses in most of those contents are observed in recent years.