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A multidisciplinary effort to assign realistic source parameters to models of volcanic ash-cloud transport and dispersion during eruptions A multidisciplinary effort to assign realistic source parameters to models of volcanic ash-cloud transport and dispersion during eruptions

During volcanic eruptions, volcanic ash transport and dispersion models (VATDs) are used to forecast the location and movement of ash clouds over hours to days in order to define hazards to aircraft and to communities downwind. Those models use input parameters, called “eruption source parameters”, such as plume height H, mass eruption rate Ṁ, duration D, and the mass fraction m63 of...
Authors
Larry G. Mastin, Marianne C. Guffanti, R. Servranckx, P. Webley, S. Barsotti, K. Dean, A. Durant, John W. Ewert, A. Neri, W.I. Rose, David J. Schneider, Lee Siebert, B. Stunder, G. Swanson, A. Tupper, A. Volentik, Christopher F. Waythomas

Features of lava lake filling and draining and their implications for eruption dynamics Features of lava lake filling and draining and their implications for eruption dynamics

Lava lakes experience filling, circulation, and often drainage depending upon the style of activity and location of the vent. Features formed by these processes have proved difficult to document due to dangerous conditions during the eruption, inaccessibility, and destruction of features during lake drainage. Kilauea Iki lava lake, Kilauea, Hawai'i, preserves many such features, because...
Authors
W.K. Stovall, Bruce F. Houghton, A.J.L. Harris, D. A. Swanson

SBAS-InSAR analysis of surface deformation at Mauna Loa and Kilauea volcanoes in Hawaii SBAS-InSAR analysis of surface deformation at Mauna Loa and Kilauea volcanoes in Hawaii

We investigate the deformation of Mauna Loa and Kllauea volcanoes, Hawai'i, by exploiting the advanced differential Synthetic Aperture Radar Interferometry (InSAR) technique referred to as the Small BAseline Subset (SBAS) algorithm. In particular, we present time series of line-of-sight (LOS) displacements derived from SAR data acquired by the ASAR instrument, on board the ENVISAT...
Authors
F. Casu, Riccardo Lanari, E. Sansosti, G. Solaro, Pietro Tizzani, Michael Poland, Asta Mikijus

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

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
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