This paper reports on new data concerning the chemical and isotopic composition of volcanic gases, the emission of volcanic SO2 and of soil CO2 at the active Ebeko Volcano. The volcano erupted in 2009, 2010, 2011, from October 2016 to November 2021. The composition of volcanic gases for 2003-2016, 2021 was obtained by straightforward sampling of the fumaroles. The high-temperature gas (420-529 degrees C) has a composition that is typical of Kuril magmatic gases with an atomic ratio C/S <1 and the concentration of HCl 5-7 mmol/mol; the isotopic composition of the condensates: delta D similar to -24, delta O-18 = 2.6-4.9. We have identified geochemical precursors of the eruption: increasing concentrations of CO2, H-2, SO2, H2S, and HCl; decreasing C/S ratio down to values below 1, which is characteristic for magmatic gases at the Kurils; increasing temperature; heavier isotopes of delta D and delta O-18 in condensates of volcanic vapor; increasing gas flux. The accumulation chamber technique was used to measure a high soil flux of CO2 in two thermal fields (reaching 10442 g/m(2)/day), which exceeds the visible fumarolic output (similar to 50 t/day as against similar to 40 t/day). The flux of SO2 from the active crater was measured using a DOAS scanning HC spectrometer in 2020 and in 2021, and was 99 +/- 28 and 9 +/- 2.7 t/day in gas plumes, and 747 +/- 220 and 450 +/- 130 t/day in ash plumes, respectively. The decreasing emission of SO2 in August 2021 is here related to degassing of the magma before the termination of the eruption.
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