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Strombolian eruption

In volcanology, a Strombolian eruption is a type of volcanic eruption with relatively mild blasts, typically having a Volcanic Explosivity Index of 1 or 2. Strombolian eruptions consist of ejection of incandescent scoria which can range from small lapilli, to larger volcanic bombs, to altitudes of tens to a few hundreds of metres. The eruptions are small to medium in volume, with sporadic violence. This type of eruption is named for the Italian volcano Stromboli.

Violent Strombolian
The most energetic Strombolian eruptions are sometimes termed "violent Strombolian" by volcanologists. in 2013 Violent Strombolian eruptions are more explosive in nature than their regular counterparts (up to VEI 3), and may produce sustained lava fountains, eruption columns several kilometres in height, Rarely, Violent Strombolian eruptions may transition into Subplinian eruptions. Examples of violent Strombolian activity include the paroxysms of Mt. Etna, the 1943-1952 eruption of Parícutin, ==See also==
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