Plinian and Pelean eruptions are characterized by their distinct features and behaviors. Plinian eruptions are marked by their explosive nature, releasing large volumes of volcanic ash and gas high into the atmosphere, creating tall eruption columns. In contrast, Pelean eruptions are characterized by the formation of pyroclastic flows, which are fast-moving currents of hot gas and volcanic materials that flow down the volcano's slopes. Both types of eruptions pose significant hazards due to their explosive nature and the potential for widespread devastation.
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