Strombolian eruptions are similar to Hawaiian eruptions, but there are differences.
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Hawaiian eruptions are responsible for several unique volcanological objects.
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Hawaiian eruptions are a type of volcanic eruption, named after the gaseous content.
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They are commonly associated with Hawaiian eruptions.
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The volume of ejected material from Hawaiian eruptions is less than half of that found in other eruptive types.
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This volcanic activity has produced numerous Hawaiian eruptions, which created lava fountains, small cinder cones and lava flows.
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Hawaiian eruptions are often extremely long lived; Pu?u ?L?M, a cinder cone of Kilauea, has been erupting continuously since 1983.
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The key factors in generating a Hawaiian eruption are basaltic magma and a low percentage of dissolved water ( less than one percent ).
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Hawaiian eruptions such as those at K + lauea can eject clots of magma suspended into gas; this is called a " fire fountain ".
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On the one extreme there are effusive Hawaiian eruptions, which are characterized by lava fountains and lava flows, which are typically not very dangerous.
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