Episode 49 of the Pu'u 'O'o-Kupaianaha eruption of Kilauea volcano-breakdown of a steady-state eruptive era |
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Authors: | M. T. Mangan C. C. Heliker T. N. Mattox J. P. Kauahikaua R. T. Helz |
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Affiliation: | (1) Hawaiian Volcano Observatory, USGS, Hawaii National Park, 96718, HI, USA;(2) MS 959 National Center, USGS, 22092 Reston, VA, USA |
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Abstract: | The Pu'u 'O'o-Kupaianaha eruption (1983-present) is the longest lived rift eruption of either Kilauea or neighboring Mauna Loa in recorded history. The initial fissure opening in January 1983 was followed by three years of episodic fire fountaining at the Pu'u 'O'o vent on Kilauea's east rift zone 19km from the summit (episodes 4–47). These spectacular events gave way in July 1986 to five and a half years of nearcontinuous, low-level effusion from the Kupaianaha vent, 3km to the cast (episode 48). A 49th episode began in November 1991 with the opening of a new fissure between Pu'u 'O'o and Kupaianaha. this three week long outburst heralded an era of more erratic eruptive behavior characterized by the shut down of Kupaianaha in February 1992 and subsequent intermittent eruption from vents on the west flank of Pu'u 'O'o (episodes 50 and 51). The events occurring over this period are due to progressive shrinkage of the rift-zone reservoir beneath the eruption site, and had limited impact on eruption temperatures and lava composition. |
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Keywords: | Kilauea Pu'u 'O'o-Kupaianaha basaltic eruption volcanic plumbing lava flows geochemistry |
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