Volcanic gases also rely on the composition of magma in the chamber of the volcano and gas separation processes before the point of eruption.
[3] This type of eruption is episodic, non-damaging to its source vent, and one of the slowest forms of activity, with the ability to sustain itself for thousands of years.
[5] Gas slugs help volcanologists monitor Strombolian eruptions with the help of overpressure stimulation, which occurs when too much pressure grows from the uprising of magmatic material.
Seismic and infrasonic signals also contribute to the monitoring of these specific eruptions around the world with the help of gas slugs.
These currents from the flows are very dense due to their solid and gaseous properties, allowing them to seep into the environment, harming agriculture and any other living aspects.