Hawaiian-style eruptions are characterized by relatively gentle, non-explosive lava flows that primarily emit basaltic magma. This type of eruption often results in the formation of extensive lava fountains and broad, shield-shaped volcanoes, distinguishing them from more explosive eruption styles. The low viscosity of the basaltic lava allows it to flow easily, creating large volumes of lava that can travel great distances, contributing to the gradual build-up of volcanic landforms.
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