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PYROCLASTIC ACTIVITY AND VENT STRUCTURES ON HAWAIIAN VOLCANOES Scott K. Rowland, University of Hawai‘i at Manoa -
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ERUPTION STYLES AND VENT FORMS
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The intersection of a dike with the Earth’s surface: a curtain of “fire” (actually lava) 1971 eruption viewed from the Hawaiian Volcano Observatory, photo by Hawai‘i Volcanoes National Park staff
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Expanding gas drives a lava fountain. The highest fountains in Hawai‘i are >500 m Technically, the base of the fountain is where the gas becomes 75% by volume, and this is usually 10s to 100s of meters below the vent rim.
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Pu‘u ‘O‘o scoria cone (in the early 1990s) - -
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Scoria cones on the lower south flank of Mauna Kea
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~2 cm Typical high-fountaining pyroclasts: reticulite, scoria, Pele’s tears, and Pele’s hair
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Crude layering in a typical high-fountaining deposit
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Pele’s hair - produced in high fountains and skylights
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Blanket of scoria downwind from Pu‘u ‘O‘o - -
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Crude bedding and large bombs in a quarried scoria cone ~2 m
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Cow dung bomb, Kilauea Iki (1959) pyroclastic deposit -
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Large spindle bomb, East Maui Volcano, SW rift zone
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low fountaining, spatter cones, and spatter ramparts (from Volcanoes in the Sea)
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Spatter is fluid when it lands ~20 cm
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~2 m-wide spatter cone, flank of Pu‘u ‘O‘o scoria cone behind - -
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photo by P. Mouginis-Mark A line of spatter cones forms a spatter rampart
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photo by P. Mouginis-Mark Satellitic shields, from eruptions with ~no pyroclastic activity
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Mauna Iki satellitic shield, Kilauea SW rift zone -
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- Kupaianaha lava pond and shield, with Pu‘u ‘O‘o scoria cone in the background - -
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Kupaianaha lava pond, Kilauea (1986-1992) - - ~20 m
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(Kapoho, 1960) HYDROMAGMATIC ERUPTIONS
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May 1924 phreatic eruption, Halema‘uma‘u view from Volcano House hotel, photo by Tai Sing Loo
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Eruption of Capelinhos, Azores, 1957. Note the “base surges” spreading laterally from the base of the column. http://volcanology.geol.ucsb.edu/surgecap.gif
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Eruption of Taal, Philippines, 1966. Note the “base surges” spreading laterally from the base of the column. http://assets.nydailynews.com/img/2009/02/03/gal_volcano_1965_taal.jpg
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Koko Rift rejuvenation-stage volcanism, Ko‘olau volcano, O‘ahu: -most of these eruptions occurred off the shoreline at the time -tuff cones, many nested and/or coalesced, resulted
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from Volcanoes in the Sea (Macdonald et al. 1983) Molokini Islet, post-shield alkalic series, E. Maui Volcano
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“surge” deposits, from lateral, turbulent deposition
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Accretionary lapilli: liquid water in the eruption cloud
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If you find footprints, do not do this ! They are fragile.
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Keanakako‘i hydromagmatic ash, SW of Kilauea caldera - - 1971 lava
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Keanakako‘i hydromagmatic ash, SW of Kilauea caldera - -
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photo by P. Mouginis-Mark Keanakako‘i tephra exposed in upper SW rift zone fractures -
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Diagram from McPhie et al. (1990) Did all this happen in a few hundred years? A few years? Painting of Keoua’s warriors, killed by an explosive eruption. - ~1500 AD ~1700 AD ~1790 AD Age dates by Don Swanson, USGS HVO
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PAU
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