central type of volcano
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Central volcanoes have a single vertical lava pipe and tend to develop a conical profile. The volcanic cone is generally built up of a succession of lavas, ignimbrites, and welded tuffs (porous rock formed by the cementation of solidified volcanic ash and dust particles).
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A central eruption is the "ejection of debris and lava flows from a centralpoint, forming a more or less symmetrical volcano" (Bates and Jackson, 1980, p. 102). The 1991 eruption of Mount Pinatubo and the 1980 explosive eruption of Mount St. Helens, after the lateral blast, are examples of central eruptions.
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