Corrigendum to “Chemical variability in volcanic gas plumes and fumaroles along the East African Rift System: New insights from the Western Branch” [Chemical Geology 596 (2022) 120811] (Chemical Geology (2022) 596, (S000925412200105X), (10.1016/j.chemgeo.2022.120811))

The authors regret that data from literature about the composition of the gas plume of the Nyamulagira volcano (green coloured field for 2014 measurements; Bobrowski et al., 2017b) was incorrectly plotted in Fig. 2a. This mistake is linked to a shift in reporting a data column for formatting the figure. Consequently, we also modify induced corresponding lines in the “Results” section (changes are underlined):. At Nyamulagira, CO2/SO2 values are higher than those obtained in the volcanic gas plume in 2014 with the same instrument but with a higher H2O/CO2 ratio, on average (CO2/SO2 = 3.8 ± 0.2; H2O/CO2 = 4.5 ± 0.2; Bobrowski et al., 2017b). Current and previous data show that the range of CO2/SO2 values at Nyamulagira (3.6–21.1) is similar to the range of values measured at Nyiragongo (5.0–29.1). Meanwhile, the range of H2O/CO2 values is clearly higher at Nyamulagira (4.3–19.6) than at Nyiragongo (1.1–3.2). On the other hand, this in no way alters the rest of the manuscript. The authors would like to apologise for any inconvenience caused.[Figure presented] Fig. 2 References Bobrowski, N., Giuffrida, G. B., Arellano, S., Yalire, M., Liotta, M., Brusca, L., Calabrese, S., Scaglione, S., Rüdiger, J., Castro, J. M., Galle, B., & Tedesco, D. (2017b). Plume composition and volatile flux of Nyamulagira volcano, Democratic Republic of Congo, during birth and evolution of the lava lake, 2014–2015. Bulletin of Volcanology, 79(12), 1-12.