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A Hawaiian eruption is a type of volcanic eruption characterized by effusive lava flows. These eruptions are similar to Icelandic eruptions but occur from a volcano's summit and radial fissures, forming large, gently sloping shield volcanoes. The lava is typically basaltic and has low viscosity and gas content, allowing it to flow easily. Examples include eruptions from Kilauea and Mauna Loa in Hawaii. These flows can be classified as pahoehoe (smooth, ropy surface) or aa (rough, clinkery surface).123

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