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Page 12, results 276 - 300

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Stabilization of volcanic flanks by dike intrusion: An example from Kilauea
P.T. Delaney, R.P. Denlinger
1999, Bulletin of Volcanology (61) 356-362
Dike propagation and dilation increases the compression of adjacent rocks. On volcanoes, especially oceanic shields, dikes are accordingly thought to be structurally destabilizing. As compression is incremented, volcanic flanks are driven outward or downslope and thus increase their susceptibility to destructive earthquakes and giant landslides. We show, however, that the...
The absence of lithium isotope fractionation during basalt differentiation: New measurements by multicollector sector ICP-MS
P.B. Tomascak, F. Tera, Rosalind Tuthill Helz, R.J. Walker
1999, Geochimica et Cosmochimica Acta (63) 907-910
We report measurements of the isotopic composition of lithium in basalts using a multicollector magnetic sector plasma-source mass spectrometer (MC-ICP-MS). This is the first application of this analytical technique to Li isotope determination. External precision of multiple replicate and duplicate measurements for a variety of sample types averages ±1.1‰ (2σ...
Metal emissions from Kilauea, and a suggested revision of the estimated worldwide metal output by quiescent degassing of volcanoes
T. K. Hinkley, P. J. Lamothe, S. A. Wilson, David L. Finnegan, T.M. Gerlach
1999, Earth and Planetary Science Letters (170) 315-325
Measurements of a large suite of metals (Pb, Cd, Cu, Zn and several others) and sulfur at Kilauea volcano over an extended period of time has yielded a detailed record of the atmospheric injection of ordinarily-rare metals from this quiescently degassing volcano, representative of an important type. We have combined...
Sulfur dioxide emission rates of Kilauea Volcano, Hawaii, 1979-1997
Tamar Elias, A. J. Sutton, J. B. Stokes, T. J. Casadevall
1998, Open-File Report 98-462
Sulfur dioxide (SO2) emission rates from Kilauea Volcano were first measured by Stoiber and Malone (1975) and have been measured on a regular basis since 1979 (Casadevall and others, 1987; Greenland and others, 1985; Elias and others, 1993; Elias and Sutton, 1996). The purpose of this report is to present...
Trace element abundances of high-MgO glasses from Kilauea, Mauna Loa and Haleakala volcanoes, Hawaii
T.P. Wagner, David A. Clague, E.H. Hauri, T.L. Grove
1998, Contributions to Mineralogy and Petrology (131) 13-21
We performed an ion-microprobe study of eleven high-MgO (6.7-14.8 wt%) tholeiite glasses from the Hawaiian volcanoes Kilauea, Mauna Loa and Haleakala. We determined the rare earth (RE), high field strength, and other selected trace element abundances of these glasses, and used the data to establish their relationship to typical Hawaiian...
Rates of volcanic CO2 degassing from airborne determinations of SO2 Emission rates and plume CO2SO2: test study at Pu′u ′O′o Cone, Kilauea Volcano, Hawaii
Terrence M. Gerlach, Kenneth A. McGee, A. Jefferson Sutton, Tamar Elias
1998, Geophysical Research Letters (25) 2675-2678
We present an airborne method that eliminates or minimizes several disadvantages of the customary plume cross-section sampling method for determining volcanic CO2 emission rates. A LI-COR CO2analyzer system (LICOR), a Fourier transform infrared spectrometer system (FTIR), and a correlation spectrometer (COSPEC) were used to constrain the plume CO2/SO2 and the...
Observations on basaltic lava streams in tubes from Kilauea Volcano, island of Hawai'i
J. Kauahikaua, K. V. Cashman, T. N. Mattox, C. Christina Heliker, K.A. Hon, M. T. Mangan, C.R. Thornber
1998, Journal of Geophysical Research B: Solid Earth (103) 27303-27323
From 1986 to 1997, the Pu'u 'O'o-Kupaianaha eruption of Kilauea produced a vast pahoehoe flow field fed by lava tubes that extended 10–12 km from vents on the volcano's east rift zone to the ocean. Within a kilometer of the vent, tubes were as much as 20 m high and...
Waveform inversion of very long period impulsive signals associated with magmatic injection beneath Kilauea Volcano, Hawaii
T. Ohminato, B. A. Chouet, P. Dawson, S. Kedar
1998, Journal of Geophysical Research B: Solid Earth (103) 23839-23862
We use data from broadband seismometers deployed around the summit of Kilauea Volcano to quantify the mechanism associated with a transient in the flow of magma feeding the east rift eruption of the volcano. The transient is marked by rapid inflation of the Kilauea summit peaking at 22 μrad 4.5...
Shallow velocity structure of Stromboli Volcano, Italy, derived from small-aperture array measurements of Strombolian tremor
B. Chouet, G. De Luca, G. Milana, P. Dawson, M. Martini, R. Scarpa
1998, Bulletin of the Seismological Society of America (88) 653-666
The properties of the tremor wave field at Stromboli are analyzed using data from small-aperture arrays of short-period seismometers deployed on the north flank of the volcano. The seismometers are configured in two semi-circular arrays with radii of 60 and 150 m and...
Airborne volcanic plume measurements using a FTIR spectrometer, Kilauea volcano, Hawaii
K.A. McGee, T.M. Gerlach
1998, Geophysical Research Letters (25) 615-618
A prototype closed-path Fourier transform infrared spectrometer system (FTIR), operating from battery power and with a Stirling engine microcooler for detector cooling, was successfully used for airborne measurements of sulfur dioxide at Kilauea volcano. Airborne profiles of the volcanic plume emanating from the erupting Pu′u′O′o vent...
Volcanic Air Pollution - A Hazard in Hawai'i
Jeff Sutton, Tamar Elias, James W. Hendley II, Peter H. Stauffer
1997, Fact Sheet 169-97
Noxious sulfur dioxide gas and other pollutants emitted from Kilauea Volcano on the Island of Hawai'i react with oxygen and atmospheric moisture to produce volcanic smog (vog) and acid rain. Vog poses a health hazard by aggravating preexisting respiratory ailments, and acid rain damages crops and can leach lead into...
Volcano geodesy: The search for magma reservoirs and the formation of eruptive vents
J.J. Dvorak, D. Dzurisin
1997, Reviews of Geophysics (35) 343-384
Routine geodetic measurements are made at only a few dozen of the world's 600 or so active volcanoes, even though these measurements have proven to be a reliable precursor of eruptions. The pattern and rate of surface displacement reveal the depth and rate of pressure increase within shallow magma reservoirs....
Multispectral thermal infrared mapping of sulfur dioxide plumes: A case study from the East Rift Zone of Kilauea Volcano, Hawaii
V.J. Realmuto, A. J. Sutton, T. Elias
1997, Journal of Geophysical Research B: Solid Earth (102) 15057-15072
The synoptic perspective and rapid mode of data acquisition provided by remote sensing are well suited for the study of volcanic SO2 plumes. In this paper we describe a plume-mapping procedure that is based on image data acquired with NASA's airborne thermal infrared multispectral scanner (TIMS) and apply the procedure to...
Littoral hydrovolcanic explosions: A case study of lava-seawater interaction at Kilauea Volcano
T. N. Mattox, M. T. Mangan
1997, Journal of Volcanology and Geothermal Research (75) 1-17
A variety of hydrovolcanic explosions may occur as basaltic lava flows into the ocean. Observations and measurements were made during a two-year span of unusually explosive littoral activity as tube-fed pahoehoe from Kilauea Volcano inundated the southeast coastline of the island of Hawai'i. Our observations suggest that explosive interactions require...
Imaging the crustal magma sources beneath Mauna Loa and Kilauea volcanoes, Hawaii
Paul G. Okubo, Harley M. Benz, Bernard A. Chouet
1997, Geology (25) 867-870
Three-dimensional seismic P-wave traveltime tomography is used to image the magma sources beneath Mauna Loa and Kilauea volcanoes, Hawaii. High-velocity bodies (>6.4 km/s) in the upper 9 km of the crust beneath the summits and rift zones of the volcanoes correlate with zones of high magnetic intensities and are interpreted...
Chronology of the episode 54 eruption at Kilauea Volcano, Hawaii, from GOES-9 satellite data
A.J.L. Harris, L. Keszthelyi, L.P. Flynn, P. J. Mouginis-Mark, C. Thornber, J. Kauahikaua, D. Sherrod, F. Trusdell, M.W. Sawyer, P. Flament
1997, Geophysical Research Letters (24) 3281-3284
The free availability of GOES satellite data every 15 minutes makes these data an attractive tool for studying short-term changes on cloud-free volcanoes in the Pacific basin. We use cloud-free GOES-9 data to investigate the chronology of the January 1997, episode 54 eruption of Kilauea Volcano, Hawaii. Seventy-six images for...
A dynamic balance between magma supply and eruption rate at Kilauea volcano, Hawaii
R.P. Denlinger
1997, Journal of Geophysical Research B: Solid Earth (102) 18091-18100
The dynamic balance between magma supply and vent output at Kilauea volcano is used to estimate both the volume of magma stored within Kilauea volcano and its magma supply rate. Throughout most of 1991 a linear decline in volume flux from the Kupaianaha vent on Kilauea's east rift zone was...
Evidence for water influx from a caldera lake during the explosive hydromagmatic eruption of 1790, Kilauea volcano, Hawaii
L.G. Mastin
1997, Journal of Geophysical Research B: Solid Earth (102) 20093-20109
In 1790 a major hydromagmatic eruption at the summit of Kilauea volcano, Hawaii, deposited up to 10 m of pyroclastic fall and surge deposits and killed several dozen Hawaiian natives who were crossing the island. Previous studies have hypothesized that the explosivity of this eruption was due to the influx...
A preliminary survey of the broadband seismic wavefield at Puu Oo, the active vent of Kilauea volcano, Hawaii
D. Seidl, M. Hellweg, P. Okubo, H. Rademacher
1996, Annali di Geofisica (39) 283-297
The seismic wavefield near an active volcanic vent consists of superimposed signals in a wide range of frequency bands from sources inside and outside the volcano. To characterize the broadband wavefield near Puu Oo, we deployed a profile of three three-component broadband sensors in a 200 m long line about...