As you may have heard, the Mount Nyiragongo volcano in the Democratic Republic of Congo has roared to life again, already claiming 32 lives as lava flowed into the city of Goma1 2. The volcano sits on the western branch of the East African Rift system (Figure 1), and has recently been active off and on since 19773. The current eruption is from multiple fissures on the sound flank of the volcano4.
Although the lava flows are devastating, the current concern is that the fissure eruptions will extend south to Lake Kive and Goma. In that case, there could be a rare lake “limnic eruption,” which could expel an extensive CO2 gas cloud into the air, potentially killing thousands. This kind of event is not unprecedented. In a tectonically unrelated setting over 1000 miles to the northwest, a landslide into the caldera Lake Nyos in 1986 in Cameroon triggered the release of CO2 gas, resulting in the deaths of over 1700 people and thousands of animals. The source of the CO2 was escaping gases from the magma body beneath Lake Nyos. The CO2 dissolved into the cold lake water and was stored there for years. When the landslide occurred, it triggered the release of the CO2, much like opening a shaken Coke can. The CO2 is denser than air and flowed down the mountain side, suffocating the people and animals in its path. A similar tragedy is feared for Goma if a limnic eruption occurs. It is unlikely that lava from the current fissures will reach the lake and trigger a limnic eruption3.
For more information see:
3 https://phys.org/news/2021-05-limnic-eruption-dr-congo-volcano.html
—– Dr. Mark Evans