The Spitak and Karymsky earthquakes occurred with M = 6.9 in Armenia and in
Kamchatka (Russia), respectively. As regards the Spitak earthquake, we ana
lysed the groundwater helium content data collected by three Georgian and o
ne Armenian measurement sites; as regards the Karymsky earthquake, we analy
sed the groundwater helium content data collected by two measurement sites
in Kamchatka. The first analysis has pointed out that precursory anomalies
appeared in the northern area with respect to the Spitak epicentre; on the
contrary, only co-post seismic anomalies were revealed in the southern area
. As regards the Karymsky earthquake, no pre-co-post seismic variation in t
he groundwater helium content was revealed at both the measurement sites. T
he analysis of other hydrogeochemical parameters, collected in these sites,
revealed that one site does not show any anomaly; on the contrary, at the
other measurement site clear preseimic anomalies appeared in some hydrogeoc
hemical parameters. A possible explanation of the quoted results is present
ed.