Publications
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High precision relocation of earthquakes at Iliamna Volcano, Alaska High precision relocation of earthquakes at Iliamna Volcano, Alaska
In August 1996, a period of elevated seismicity commenced beneath Iliamna Volcano, Alaska. This activity lasted until early 1997, consisted of over 3000 earthquakes, and was accompanied by elevated emissions of volcanic gases. No eruption occurred and seismicity returned to background levels where it has remained since. We use waveform alignment with bispectrum-verified cross-correlation...
Authors
P. Statz-Boyer, C. Thurber, J.D. Pesicek, S. Prejean
Halogen degassing during ascent and eruption of water-poor basaltic magma Halogen degassing during ascent and eruption of water-poor basaltic magma
A study of volcanic gas composition and matrix glass volatile concentrations has allowed a model for halogen degassing to be formulated for K??lauea Volcano, Hawai'i. Volcanic gases emitted during 2004-2005 were characterised by a molar SO2/HCl of 10-64, with a mean of 33; and a molar HF/HCl of 0-5, with a mean of 1.0 (from approximately 2500 measurements). The HF/HCl ratio was more...
Authors
M. Edmonds, T.M. Gerlach, Richard A. Herd
Variations in population exposure and sensitivity to lahar hazards from Mount Rainier, Washington Variations in population exposure and sensitivity to lahar hazards from Mount Rainier, Washington
Although much has been done to understand, quantify, and delineate volcanic hazards, there are fewer efforts to assess societal vulnerability to these hazards, particularly demographic differences in exposed populations or spatial variations in exposure to regional hazards. To better understand population diversity in volcanic hazard zones, we assess the number and types of people in a...
Authors
N. Wood, C. Soulard
Isotopic and trace element constraints on the petrogenesis of lavas from the Mount Adams volcanic field, Washington Isotopic and trace element constraints on the petrogenesis of lavas from the Mount Adams volcanic field, Washington
Strontium, Nd, Pb, Hf, Os, and O isotope compositions for 30 Quaternary lava flows from the Mount Adams stratovolcano and its basaltic periphery in the Cascade arc, southern Washington, USA indicate a major component from intraplate mantle sources, a relatively small subduction component, and interaction with young mafic crust at depth. Major- and trace-element patterns for Mount Adams...
Authors
B.R. Jicha, G.L. Hart, C.M. Johnson, Wes Hildreth, B.L. Beard, S.B. Shirey, J.W. Valley
Long-term changes in quiescent degassing at Mount Baker Volcano, Washington, USA; Evidence for a stalled intrusion in 1975 and connection to a deep magma source Long-term changes in quiescent degassing at Mount Baker Volcano, Washington, USA; Evidence for a stalled intrusion in 1975 and connection to a deep magma source
Long-term changes have occurred in the chemistry, isotopic ratios, and emission rates of gas at Mount Baker volcano following a major thermal perturbation in 1975. In mid-1975 a large pulse in sulfur and carbon dioxide output was observed both in emission rates and in fumarole samples. Emission rates of CO2 and H2S were ∼ 950 and 112 t/d, respectively, in 1975; these decreased to ∼ 150...
Authors
Cynthia A. Werner, William C. Evans, Michael P. Poland, Michael P. Doukas, D.S. Tucker
Modeling hazardous mass flows Geoflows09: Mathematical and computational aspects of modeling hazardous geophysical mass flows; Seattle, Washington, 9–11 March 2009 Modeling hazardous mass flows Geoflows09: Mathematical and computational aspects of modeling hazardous geophysical mass flows; Seattle, Washington, 9–11 March 2009
A recent workshop at the University of Washington focused on mathematical and computational aspects of modeling the dynamics of dense, gravity-driven mass movements such as rock avalanches and debris flows. About 30 participants came from seven countries and brought diverse backgrounds in geophysics; geology; physics; applied and computational mathematics; and civil, mechanical, and...
Authors
Richard M. Iverson, Randall J. LeVeque
The morphology and distribution of submerged reefs in the Maui-Nui Complex, Hawaii: New insights into their evolution since the Early Pleistocene The morphology and distribution of submerged reefs in the Maui-Nui Complex, Hawaii: New insights into their evolution since the Early Pleistocene
Reef drowning and backstepping have long been recognised as reef responses to sea-level rise on subsiding margins. During the Late Pleistocene (~500–14 ka) Hawaiian reefs grew in response to rapid subsidence and 120 m 100 kyr sea-level cycles, with recent work on the submerged drowned reefs around the big island of Hawaii, and in other locations from the last deglacial, providing insight...
Authors
Iain D.E. Faichney, James M. Webster, David A. Clague, Chris Kelley, Bruce Applegate, James G. Moore
Laguna del Maule volcanic field: Eruptive history of a Quaternary basalt-to-rhyolite distributed volcanic field on the Andean rangecrest in central Chile Laguna del Maule volcanic field: Eruptive history of a Quaternary basalt-to-rhyolite distributed volcanic field on the Andean rangecrest in central Chile
The Laguna del Maule (LdM) volcanic field, which surrounds the 54-km2 lake of that name, covers ~500 km2 of rugged glaciated terrain with Quaternary lavas and tuffs that extend for 40 km westward from the Argentine frontier and 30 km north-south from the Rio Campanario to Laguna Fea. The distributed rear-arc volcanic field is contiguous with the Tatara-San Pedro stratovolcano complex on...
Authors
Wes Hildreth, Estanislao Godoy, Judy Fierstein, Brad Singer
Observation and modeling of source effects in coda wave interferometry at Pavlof volcano Observation and modeling of source effects in coda wave interferometry at Pavlof volcano
Sorting out source and path effects for seismic waves at volcanoes is critical for the proper interpretation of underlying volcanic processes. Source or path effects imply that seismic waves interact strongly with the volcanic subsurface, either through partial resonance in a conduit (Garces et al., 2000; Sturton and Neuberg, 2006) or by random scattering in the heterogeneous volcanic...
Authors
Matthew M. Haney, Wijik K. van, L.A. Preston, D.F. Aldridge
The source of infrasound associated with long-period events at mount St. Helens The source of infrasound associated with long-period events at mount St. Helens
During the early stages of the 2004-2008 Mount St. Helens eruption, the source process that produced a sustained sequence of repetitive long-period (LP) seismic events also produced impulsive broadband infrasonic signals in the atmosphere. To assess whether the signals could be generated simply by seismic-acoustic coupling from the shallow LP events, we perform finite difference...
Authors
R.S. Matoza, M.A. Garces, B. A. Chouet, L. D’Auria, M.A.H. Hedlin, C. De Groot-Hedlin, G.P. Waite
The unexpected awakening of Chaitén Volcano, Chile The unexpected awakening of Chaitén Volcano, Chile
On 2 May 2008, a large eruption began unexpectedly at the inconspicuous Chaitén volcano in Chile's southern volcanic zone. Ash columns abruptly jetted from the volcano into the stratosphere, followed by lava dome effusion and continuous low-altitude ash plumes [Lara, 2009]. Apocalyptic photographs of eruption plumes suffused with lightning were circulated globally. Effects of the...
Authors
Simon A. Carn, John S. Zogorski, Luis Lara, John W. Ewert, Sebastian Watt, Alfred J. Prata, Ronald J. Thomas, Gustavo Villarosa
Multiple dendrochronological responses to the eruption of Cinder Cone, Lassen Volcanic National Park, California Multiple dendrochronological responses to the eruption of Cinder Cone, Lassen Volcanic National Park, California
Two dendrochronological properties – ring width and ring chemistry – were investigated in trees near Cinder Cone in Lassen Volcanic National Park, northeastern California, for the purpose of re-evaluating the date of its eruption. Cinder Cone is thought to have erupted in AD 1666 based on ring-width evidence, but interpreting ring-width changes alone is not straightforward because many...
Authors
P.R. Sheppard, M.H. Ort, K.C. Anderson, M.A. Clynne, E.M. May