Publications
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Three short videos by the Yellowstone Volcano Observatory Three short videos by the Yellowstone Volcano Observatory
This is a collection of videos of unscripted interviews with Jake Lowenstern, who is the Scientist in Charge of the Yellowstone Volcano Observatory (YVO). YVO was created as a partnership among the U.S. Geological Survey (USGS), Yellowstone National Park, and University of Utah to strengthen the long-term monitoring of volcanic and earthquake unrest in the Yellowstone National Park...
Authors
Stephen Wessells, Jake Lowenstern, Dina Venezky
Volcanic hazards to airports Volcanic hazards to airports
Volcanic activity has caused significant hazards to numerous airports worldwide, with local to far-ranging effects on travelers and commerce. Analysis of a new compilation of incidents of airports impacted by volcanic activity from 1944 through 2006 reveals that, at a minimum, 101 airports in 28 countries were affected on 171 occasions by eruptions at 46 volcanoes. Since 1980, five...
Authors
Marianne C. Guffanti, Gari C. Mayberry, Thomas J. Casadevall, Richard Wunderman
Magma degassing triggered by static decompression at Kīlauea Volcano, Hawai‘i Magma degassing triggered by static decompression at Kīlauea Volcano, Hawai‘i
During mid-June 2007, the summit of Kīlauea Volcano, Hawai‘i, deflated rapidly as magma drained from the subsurface to feed an east rift zone intrusion and eruption. Coincident with the deflation, summit SO2 emission rates rose by a factor of four before decaying to background levels over several weeks. We propose that SO2 release was triggered by static decompression caused by magma...
Authors
Michael P. Poland, Sutton A. Jeff, Terrence M. Gerlach
Objective rapid delineation of areas at risk from block-and-ash pyroclastic flows and surges Objective rapid delineation of areas at risk from block-and-ash pyroclastic flows and surges
Assessments of pyroclastic flow (PF) hazards are commonly based on mapping of PF and surge deposits and estimations of inundation limits, and/or computer models of varying degrees of sophistication. In volcanic crises a PF hazard map may be sorely needed, but limited time, exposures, or safety aspects may preclude fieldwork, and insufficient time or baseline data may be available for...
Authors
C. Widiwijayanti, B. Voight, D. Hidayat, S. P. Schilling
Discriminating assimilants and decoupling deep- vs. shallow-level crystal records at Mount Adams using 238U-230Th disequilibria and Os isotopes Discriminating assimilants and decoupling deep- vs. shallow-level crystal records at Mount Adams using 238U-230Th disequilibria and Os isotopes
A suite of 23 basaltic to dacitic lavas erupted over the last 350 kyr from the Mount Adams volcanic field has been analyzed for U–Th isotope compositions to evaluate the roles of mantle versus crustal components during magma genesis. All of the lavas have (230Th/238U) > 1 and span a large range in (230Th/232Th) ratios, and most basalts have higher (230Th/232Th) ratios than andesites and...
Authors
Brian R. Jicha, Clark M. Johnson, Wes Hildreth, Brian L. Beard, Garret L. Hart, Steven B. Shirey, Brad S. Singer
Elements of an improved model of debris-flow motion Elements of an improved model of debris-flow motion
A new depth-averaged model of debris-flow motion describes simultaneous evolution of flow velocity and depth, solid and fluid volume fractions, and pore-fluid pressure. Non-hydrostatic pore-fluid pressure is produced by dilatancy, a state-dependent property that links the depth-averaged shear rate and volumetric strain rate of the granular phase. Pore-pressure changes caused by shearing...
Authors
R.M. Iverson
Constructing constitutive relationships for seismic and aseismic fault slip Constructing constitutive relationships for seismic and aseismic fault slip
For the purpose of modeling natural fault slip, a useful result from an experimental fault mechanics study would be a physically-based constitutive relation that well characterizes all the relevant observations. This report describes an approach for constructing such equations. Where possible the construction intends to identify or, at least, attribute physical processes and contact...
Authors
N.M. Beeler
Holocene climate on the Modoc Plateau, northern California, USA: The view from Medicine Lake Holocene climate on the Modoc Plateau, northern California, USA: The view from Medicine Lake
Medicine Lake is a small (165 ha), relatively shallow (average 7.3 m), intermediate elevation (2,036 m) lake located within the summit caldera of Medicine Lake volcano, Siskiyou County, California, USA. Sediment cores and high-resolution bathymetric and seismic reflection data were collected from the lake during the fall of 1999 and 2000. Sediments were analyzed for diatoms, pollen...
Authors
Scott W. Starratt
Infrasonic ambient noise interferometry from correlations of microbaroms Infrasonic ambient noise interferometry from correlations of microbaroms
We show that microbaroms, continuous infrasound fluctuations resulting from the interaction of the ocean with the atmosphere, have long-range correlation properties that make it possible to estimate the impulse response between two microphones from passive recordings. The processing is analogous to methods employed in the emerging field of ambient noise seismology, where the random noise...
Authors
M.M. Haney
A field guide to Newberry Volcano, Oregon A field guide to Newberry Volcano, Oregon
Newberry Volcano is located in central Oregon at the intersection of the Cascade Range and the High Lava Plains. Its lavas range in age from ca. 0.5 Ma to late Holocene. Erupted products range in composition from basalt through rhyolite and cover ~3000 km2. The most recent caldera-forming eruption occurred ~80,000 years ago. This trip will highlight a revised understanding of the volcano...
Authors
Robert A. Jenson, Julie M. Donnelly-Nolan, Daniele McKay
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