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The least powerful of them all is the Hawaiian eruption which is mainly produced by shield volcanoes that have low gas levels within the lava. Without the high gas levels the explosiveness of the event is relatively quiet with the lava flowing quickly through lava channels and tunnels from the crater to lower points around the base. Occasionally the eruptions do produce pyroclastic discharges but they are not violent in nature.
Fissure eruptions are similar to Hawaiian eruptions in that they produce low explosive events and lava flows that travel along the sides of the volcano.
Strombolian eruptions are a little more violent and produce more frequent eruption discharges than do Hawaiian eruptions...
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