Publications
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Interdisciplinary studies of eruption at Chaitén volcano, Chile Interdisciplinary studies of eruption at Chaitén volcano, Chile
High-silica rhyolite magma fuels Earth's largest and most explosive eruptions. Recurrence intervals for such highly explosive eruptions are in the 100- to 100,000-year time range, and there have been few direct observations of such eruptions and their immediate impacts. Consequently, there was keen interest within the volcanology community when the first large eruption of high-silica...
Authors
John S. Pallister, Jon J. Major, Thomas C. Pierson, Richard P. Holitt, Jacob B. Lowenstern, John C. Eichelberger, Lara Luis, Hugo Moreno, Jorge Muñoz, Jonathan M. Castro, Andrés Iroumé, Andrea Andreoli, Julia Jones, Fred Swanson, Charlie Crisafulli
Characterizing 6 August 2007 Crandall Canyon mine collapse from ALOS PALSAR InSAR Characterizing 6 August 2007 Crandall Canyon mine collapse from ALOS PALSAR InSAR
We used ALOS InSAR images to study land surface deformation over the Crandall Canyon mine in Utah, which collapsed on 6 August 2007 and killed six miners. The collapse was registered as a ML 3.9 seismic event. An InSAR image spanning the time of the collapse shows 25–30 cm surface subsidence over the mine. We used distributed dislocation sources to model the deformation field, and found...
Authors
Zhong Lu, Charles Wicks
Origins of large-volume, compositionally zoned volcanic eruptions: New constraints from U-series isotopes and numerical thermal modeling for the 1912 Katmai-Novarupta eruption Origins of large-volume, compositionally zoned volcanic eruptions: New constraints from U-series isotopes and numerical thermal modeling for the 1912 Katmai-Novarupta eruption
We present the results of a combined U-series isotope and numerical modeling study of the 1912 Katmai-Novarupta eruption in Alaska. A stratigraphically constrained set of samples have compositions that range from basalt through basaltic andesite, andesite, dacite, and rhyolite. The major and trace element range can be modeled by 80–90% closed-system crystal fractionation over a...
Authors
Simon Turner, Mike Sandiford, Mark Reagan, Chris Hawkesworth, Wes Hildreth
Effects of soil aggregates on debris-flow mobilization: Results from ring-shear experiments Effects of soil aggregates on debris-flow mobilization: Results from ring-shear experiments
Rates and styles of landslide motion are sensitive to pore-water pressure changes caused by changes in soil porosity accompanying shear deformation. Soil may either contract or dilate upon shearing, depending upon whether its initial porosity is greater or less, respectively, than a critical-state porosity attained after sufficiently high strain. We observed complications in this...
Authors
Neal R. Iverson, Janet E. Mann, Richard M. Iverson
Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii
The formation, evolution, collapse, and subsequent resurrection of a vent within Halema'uma'u Crater, Kilauea Volcano, produced energetic and varied degassing signals recorded by a nearby infrasound array between 2008 and early 2009. After 25 years of quiescence, a vent-clearing explosive burst on 19 March 2008 produced a clear, complex acoustic signal. Near-continuous harmonic...
Authors
David Fee, Milton Garces, Matt Patrick, Bernard Chouet, Phil Dawson, Donald A. Swanson
Remotely triggered microearthquakes and tremor in central California following the 2010 Mw 8.8 Chile earthquake Remotely triggered microearthquakes and tremor in central California following the 2010 Mw 8.8 Chile earthquake
We examine remotely triggered microearthquakes and tectonic tremor in central California following the 2010 Mw 8.8 Chile earthquake. Several microearthquakes near the Coso Geothermal Field were apparently triggered, with the largest earthquake (Ml 3.5) occurring during the large-amplitude Love surface waves. The Chile mainshock also triggered numerous tremor bursts near the Parkfield...
Authors
Zhigang Peng, David P. Hill, David R. Shelly, Chastity Aiken
Mount St. Helens: A 30-year legacy of volcanism Mount St. Helens: A 30-year legacy of volcanism
The spectacular eruption of Mount St. Helens on 18 May 1980 electrified scientists and the public. Photodocumentation of the colossal landslide, directed blast, and ensuing eruption column—which reached as high as 25 kilometers in altitude and lasted for nearly 9 hours—made news worldwide. Reconnaissance of the devastation spurred efforts to understand the power and awe of those moments...
Authors
James W. Vallance, Cynthia A. Gardner, William E. Scott, Richard M. Iverson, Thomas C. Pierson
Röthlisberger channel theory: its origins and consequences Röthlisberger channel theory: its origins and consequences
The theory of channelized water flow through glaciers, most commonly associated with the names of Hans Röthlisberger and Ron Shreve and their 1972 papers in the Journal of Glaciology, was developed at a time when interest in glacier-bed processes was expanding, and the possible relationship between glacier sliding and water at the bed was becoming of keen interest. The R-channel theory...
Authors
Joseph S. Walder
Caldera collapse: Perspectives from comparing Galápagos volcanoes, nuclear-test sinks, sandbox models, and volcanoes on Mars Caldera collapse: Perspectives from comparing Galápagos volcanoes, nuclear-test sinks, sandbox models, and volcanoes on Mars
The 1968 trapdoor collapse (1.5 km3) of Fernandina caldera in the Galapágos Islands developed the same kinds of structures as found in small sandbox-collapse models and in concentrically zoned sinks formed in desert alluvium by fault subsidence into underground nuclear-explosion cavities. Fernandina’s collapse developed through shear failure in which the roof above the evacuating chamber...
Authors
K. A. Howard
Surface-wave potential for triggering tectonic (nonvolcanic) tremor Surface-wave potential for triggering tectonic (nonvolcanic) tremor
Source processes commonly posed to explain instances of remote dynamic triggering of tectonic (nonvolcanic) tremor by surface waves include frictional failure and various modes of fluid activation. The relative potential for Love- and Rayleigh-wave dynamic stresses to trigger tectonic tremor through failure on critically stressed thrust and vertical strike-slip faults under the Coulomb...
Authors
D.P. Hill
Time-lapse imagery of the breaching of Marmot Dam, Oregon, and subsequent erosion of sediment by the Sandy River– October 2007 to May 2008 Time-lapse imagery of the breaching of Marmot Dam, Oregon, and subsequent erosion of sediment by the Sandy River– October 2007 to May 2008
In 2007, Marmot Dam on the Sandy River, Oregon, was removed and a temporary cofferdam standing in its place was breached, allowing the river to flow freely along its entire length. Time-lapse imagery obtained from a network of digital single-lens reflex cameras placed around the lower reach of the sediment-filled reservoir behind the dam details rapid erosion of sediment by the Sandy...
Authors
Jon J. Major, Kurt R. Spicer, Rebecca A. Collins
August 2008 eruption of Kasatochi volcano, Aleutian Islands, Alaska-resetting an Island Landscape August 2008 eruption of Kasatochi volcano, Aleutian Islands, Alaska-resetting an Island Landscape
Kasatochi Island, the subaerial portion of a small volcano in the western Aleutian volcanic arc, erupted on 7-8 August 2008. Pyroclastic flows and surges swept the island repeatedly and buried most of it and the near-shore zone in decimeters to tens of meters of deposits. Several key seabird rookeries in taluses were rendered useless. The eruption lasted for about 24 hours and included...
Authors
William E. Scott, Christopher J. Nye, Christopher F. Waythomas, Christina A. Neal