The eruption triggered the sudden release of about 100,000–300,000 tons of carbon dioxide (CO2).[2][3] The gas cloud initially rose at nearly 100 kilometres per hour (62 mph; 28 m/s) and then, being heavier than air, descended onto nearby villages, suffocating people and livestock within 25 kilometres (16 mi) of the lake.[4][5]
A degassing system has since been installed at the lake, with the aim of reducing the concentration of CO2 in the waters and therefore the risk of further eruptions. Along with the Lake Monoun disaster two years earlier, it is one of only two recorded limnic eruptions in history.[6]
^Smolowe, Jill; Phillips, B. J. (8 September 1986). "Cameroon the Lake of Death". TIME. Vol. 128, no. 10. pp. 34–37. Archived from the original on 27 February 2009. Retrieved 9 December 2013.
^Ohba, Takeshi, et al. "A Depression Containing CO2-Enriched Water at the Bottom of Lake Monoun, Cameroon, and Implications for the 1984 Limnic Eruption." Frontiers in Earth Science, vol. 10, May 2022, p. 766791. DOI.org (Crossref), https://doi.org/10.3389/feart.2022.766791.