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Not all publications have extents, not all extents are completely accurate
Volcanic geology and eruption frequency, lower east rift zone of Kilauea volcano, Hawaii
R. B. Moore
1992, Bulletin of Volcanology (54) 475-483
Detailed geologic mapping and radiocarbon dating of tholeiitic basalts covering about 275 km2 on the lower east rift zone (LERZ) and adjoining flanks of Kilauea volcano, Hawaii, show that at least 112 separate eruptions have occurred during the past 2360 years. Eruptive products include spatter ramparts and cones, a shield,...
Volcano growth and evolution of the island of Hawaii
James G. Moore, David A. Clague
1992, Geological Society of America Bulletin (104) 1471-1484
The seven volcanoes comprising the island of Hawaii and its submarine base are, in order of growth, Mahukona, Kohala, Mauna Kea, Hualalai, Mauna Loa, Kilauea, and Loihi. The first four have completed their shield-building stage, and the timing of this event can be determined from the depth of the slope...
Multispectral thermal infrared mapping of the 1 October 1988 Kupaianaha flow field, Kilauea volcano, Hawaii
V.J. Realmuto, K. Hon, A.B. Kahle, E.A. Abbott, D.C. Pieri
1992, Bulletin of Volcanology (55) 33-44
Multispectral thermal infrared radiance measurements of the Kupaianaha flow field were acquired with the NASA airborne Thermal Infrared Multispectral Scanner (TIMS) on the morning of 1 October 1988. The TIMS data were used to map both the temperature and emissivity of the surface of the flow field. The temperature map...
Ages, rare-earth element enrichment, and petrogenesis of tholeiitic and alkalic basalts from Kahoolawe Island, Hawaii
R.V. Fodor, F.A. Frey, G.R. Bauer, D.A. Clague
1992, Contributions to Mineralogy and Petrology (110) 442-462
Kahoolawe Island, Hawaii (18×11 km), is a basaltic shield volcano with caldera-filling lavas, seven identified postshield vents, and at least two occurrences of apparent rejuvenated-stage eruptive. We examined 42 samples that represent all stages of Kahoolawe volcano stratigraphy for their petrography, whole-rock major-and trace-element contents, mineral...
Mechanism of explosive eruptions of Kilauea Volcano, Hawaii
J.J. Dvorak
1992, Bulletin of Volcanology (54) 638-645
A small explosive eruption of Kilauea Volcano, Hawaii, occurred in May 1924. The eruption was preceded by rapid draining of a lava lake and transfer of a large volume of magma from the summit reservoir to the east rift zone. This lowered the magma column, which reduced hydrostatic pressure beneath...
Surface chemistry associated with the cooling and subaerial weathering of recent basalt flows
A. F. White, M.F. Hochella Jr.
1992, Geochimica et Cosmochimica Acta (56) 3711-3721
The surface chemistry of fresh and weathered historical basalt flows was characterized using surface-sensitive X-ray photoelectron spectroscopy (XPS). Surfaces of unweathered 1987–1990 flows from the Kilauea Volcano, Hawaii, exhibited variable enrichment in Al, Mg, Ca, and F due to the formation of refractory fluoride compounds and pronounced depletion in Si...
The ten-year eruption of Kilauea Volcano
D.A. Clague, C. Heliker
1992, Earthquakes & Volcanoes (USGS) (23) 244-254
The Pu'u 'O' o-Kupaianaha eruption now ranks as the longest-lived historic eruption on the East Rift Zone and the most destructive in Kilauea's recent history. About 1 km3 of lava erupted during the first 0 years of the eruption. Lava flows have destroyed 181 houses and severed the coastal highway along...
Tracking the movement of Hawaiian volcanoes; Global Positioning System (GPS) measurement
J.J. Dvorak
1992, Earthquakes & Volcanoes (USGS) (23) 255-267
Most, if not all, volcanic eruptions are preceded by surface movements near the volcano. These ground movements are the response of the shallow crust to the accumulation of the magma or the buildup of magma pressure within a subterranean reservoir beneath the volcano. As the magma reservoir expands, the summit...
The Pu'u ‘O’o‐Kupaianaha eruption of Kilauea
Christina C. Heliker, Thomas L. Wright
1991, Eos, Transactions, American Geophysical Union (72) 521-526
Kilauea is nearing the 10th year of its most voluminous rift zone eruption in the last 2 centuries. Lava flows have covered 75 km2 to depths as great as 25 m and have added almost 1.2 km2 of new land to the island. These flows have devastated downslope communities and have provided...
Picritic glasses from Hawaii
D.A. Clague, W. S. Weber, J.E. Dixon
1991, Nature (353) 553-556
Estimates of the MgO content of primary Hawaiian tholeiitic melts range from 8wt% to as high as 25wt% (refs 1, 2). In general, these estimates are derived from analysis of the whole-rock composition of lavas, coupled with the compositions of the most magnesian olivine phenocrysts observed. But the best estimate...
Possible solar noble-gas component in Hawaiian basalts
M. Honda, I. McDougall, D.B. Patterson, A. Doulgeris, D.A. Clague
1991, Nature (349) 149-151
The noble-gas elemental and isotopic composition in the Earth is significantly different from that of the present atmosphere, and provides an important clue to the origin and history of the Earth and its atmosphere. Possible candidates for the noble-gas composition of the primordial Earth include a solar-like component, a planetary-like...
Tritium concentrations in the active Pu'u O'o crater, Kilauea volcano, Hawaii: implications for cold fusion in the Earth's interior
J. E. Quick, T. K. Hinkley, G.M. Reimer, C. E. Hedge
1991, Physics of the Earth and Planetary Interiors (69) 132-137
The assertion that deuterium-deuterium fusion may occur at low temperature suggests a potential new source of geothermal heat. If a cold-fusion-like process occurs within the Earth, then a test for its existence would be a search for anomalous tritium in volcanic emissions. The Pu'u O'o crater is the first point...
Underwater observations of active lava flows from Kilauea volcano, Hawaii
G.W. Tribble
1991, Geology (19) 633-636
Underwater observation of active submarine lava flows from Kilauea volcano, Hawaii, in March-June 1989 revealed both pillow lava and highly channelized lava streams flowing down a steep and unconsolidated lava delta. The channelized streams were 0.7-1.5 m across and moved at rates of...
Reequilibration of chromite within Kilauea Iki lava lake, Hawaii
P.A.H. Scowen, P.L. Roeder, Rosalind Tuthill Helz
1991, Contributions to Mineralogy and Petrology (107) 8-20
Chromite mainly occurs as tiny inclusions within or at the edges of olivine phenocrysts in the 1959 Kilauea Iki lava lake. Liquilus chromite compositions are only preserved in scoria that was rapidly quenched from eruption temperatures. Analyses of drill core taken from the lava lake in 1960, 1961, 1975, 1979,...
Distribution of metals between particulate and gaseous forms in a volcanic plume
T. K. Hinkley
1991, Bulletin of Volcanology (53) 395-400
In order to gain information on the distribution of metals between particles and gaseous forms in the plume of Kilauea volcano, a filter designed to collect metals associated with particles was followed in series by two other collectors intended to trap metals present in gaseous (atomic, molecular, or complexed) form:...
Fractal properties of tremor and gas piston events observed at Kilauea Volcano, Hawaii
B. Chouet, H. R. Shaw
1990, Journal of Geophysical Research (96) 10177-10189
Studies the fractal properties of shallow volcanic tremor and gas piston events associated with magma degassing at Kilauea Volcano, Hawaii, using data from two dense short-baseline arrays of seismographs deployed near the active crater of Puu Oo on the east rift of the volcano. The existence of a categorically stable...
Deep magma body beneath the summit and rift zones of Kilauea Volcano, Hawaii
Paul T. Delaney, R.S. Fiske, Asta Miklius, Arnold T. Okamura, Maurice K. Sako
1990, Science (247) 1311-1316
A magnitude 7.2 earthquake in 1975 caused the south flank of Kilauea Volcano, Hawaii, to move seaward in response to slippage along a deep fault. Since then, a large part of the volcano's edifice has been adjusting to this perturbation. The summit of Kilauea extended at a rate of 0.26...
Horizontal ground deformation patterns and magma storage during the Puu Oo eruption of Kilauea volcano, Hawaii: episodes 22-42
J.P. Hoffmann, G. E. Ulrich, M.O. Garcia
1990, Bulletin of Volcanology (52) 522-531
Horizontal ground deformation measurements were made repeatedly with an electronic distance meter near the Puu Oo eruption site approximately perpendicular to Kilauea's east rift zone (ERZ) before and after eruptive episodes 22-42. Line lengths gradually extended during repose periods and rapidly contracted about the same amount following eruptions. The repeated...
Cooling rate and thermal structure determined from progressive magnetization of the dacite dome at Mount St. Helens, Washington
D. Dzurisin, R.P. Denlinger, J. G. Rosenbaum
1990, Journal of Geophysical Research Solid Earth (95) 2763-2780
Our study of a magnetic anomaly associated with the recently active dacite dome at Mount St. Helens suggests that the dome consists of a hot, nonmagnetized core surrounded by a cool, magnetized carapace and flanking talus. The talus does not contribute to the anomaly because...
Phreatomagmatic and phreatic fall and surge deposits from explosions at Kilauea volcano, Hawaii, 1790 a.d.: Keanakakoi Ash Member
J. McPhie, G.P.L. Walker, R.L. Christiansen
1990, Bulletin of Volcanology (52) 334-354
In or around 1790 a.d. an explosive eruption took place in the summit caldera of Kilauea shield volcano. A group of Hawaiian warriors close to the caldera at the time were killed by the effects of the explosions. The stratigraphy of pyroclastic deposits surrounding Kilauea (i.e., the Keanakakoi Ash Member)...