Publications
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Overview of the 2004 to 2006, and continuing, eruption of Mount St. Helens, Washington Overview of the 2004 to 2006, and continuing, eruption of Mount St. Helens, Washington
Rapid onset of unrest at Mount St. Helens on September 23, 2004, initiated an uninterrupted lava-dome-building eruption that continues to the time of writing this overview (spring 2006) for a volume of papers focused on this eruption. About three weeks of intense seismic unrest and localized surface uplift, punctuated by four brief explosions, constituted a ventclearing phase, during...
Authors
William E. Scott, David R. Sherrod, Cynthia A. Gardner
Paleoseismicity and neotectonics of the Aleutian subduction zone — An overview Paleoseismicity and neotectonics of the Aleutian subduction zone — An overview
The Aleutian subduction zone is one of the most seismically active plate boundaries and the source of several of the world’s largest historic earthquakes. The structural architecture of the subduction zone varies considerably along its length. At the eastern end is a tectonically complex collision zone where the allochthonous Yakutat terrane is moving northwest into mainland Alaska. West...
Authors
Gary A. Carver, George Plafker
Managing public and media response to a reawakening volcano: lessons from the 2004 eruptive activity of Mount St. Helens Managing public and media response to a reawakening volcano: lessons from the 2004 eruptive activity of Mount St. Helens
Volcanic eruptions and other infrequent, large-scale natural disturbances pose challenges and opportunities for public-land managers. In the days and weeks preceding an eruption, there can be considerable uncertainty surrounding the magnitude and areal extent of eruptive effects. At the same time, public and media interest in viewing developing events is high and concern for public...
Authors
Peter M. Frenzen, Michael T. Matarrese
Toward a time-dependent probabilistic seismic hazard analysis for Alaska Toward a time-dependent probabilistic seismic hazard analysis for Alaska
We report on a time-dependent seismic hazard analysis for Alaska and the Aleutians to complement our recently completed time-independent map. Whereas the time-independent map treats all sources as statistically independent, the time-dependent analysis is based on calculations of the conditional probability of occurrence for the next 50 years by using a Brownian Passage Time model for the...
Authors
Oliver S. Boyd, Yuehua Zeng, Charles G. Bufe, Robert L. Wesson, Frederick Pollitz, Jeanne L. Hardebeck
Does a boundary of the Wrangell Block extend through southern Cook Inlet and Shelikof Strait, Alaska? Does a boundary of the Wrangell Block extend through southern Cook Inlet and Shelikof Strait, Alaska?
In southcentral Alaska, the boundaries of two different tectonic blocks extend southwestward from the Denali Fault toward Cook Inlet and Shelikof Strait. We use offshore multichannel seismic reflection data and oil-well stratigraphy to evaluate whether local geologic structures are compatible with boundaries of either tectonic block and with the relative motion expected across the block...
Authors
Michael A. Fisher, Ray W. Sliter, Florence L. Wong
Note from the Hubbert Quorum Note from the Hubbert Quorum
No abstract available.
Authors
Steven E. Ingebritsen, Shaul Hurwitz, E. E. Brodsky
Numerical modeling of rainfall thresholds for shallow landsliding in the Seattle, Washington, area Numerical modeling of rainfall thresholds for shallow landsliding in the Seattle, Washington, area
The temporal forecasting of landslide hazard has typically relied on empirical relations between rainfall characteristics and landslide occurrence to identify conditions that may cause shallow landslides. Here, we describe an alternate, deterministic approach to define rainfall thresholds for landslide occurrence in the Seattle, Washington, area. This approach combines an infinite slope...
Authors
Jonathan W. Godt, Jonathan P. McKenna
The critical role of volcano monitoring in risk reduction The critical role of volcano monitoring in risk reduction
Data from volcano-monitoring studies constitute the only scientifically valid basis for short-term forecasts of a future eruption, or of possible changes during an ongoing eruption. Thus, in any effective hazards-mitigation program, a basic strategy in reducing volcano risk is the initiation or augmentation of volcano monitoring at historically active volcanoes and also at geologically...
Authors
R.I. Tilling
Rainfall-triggered landslides, anthropogenic hazards, and mitigation strategies Rainfall-triggered landslides, anthropogenic hazards, and mitigation strategies
Rainfall-triggered landslides are part of a natural process of hillslope erosion that can result in catastrophic loss of life and extensive property damage in mountainous, densely populated areas. As global population expansion on or near steep hillslopes continues, the human and economic costs associated with landslides will increase. Landslide hazard mitigation strategies generally...
Authors
M. C. Larsen
Observations of the north polar water ice annulus on Mars using THEMIS and TES Observations of the north polar water ice annulus on Mars using THEMIS and TES
The Martian seasonal CO2 ice caps advance and retreat each year. In the spring, as the CO2 cap gradually retreats, it leaves behind an extensive defrosting zone from the solid CO2 cap to the location where all CO2 frost has sublimated. We have been studying this phenomenon in the north polar region using data from the THermal EMission Imaging System (THEMIS), a visible and infra-red (IR)...
Authors
Kiri L. Wagstaff, Timothy N. Titus, Anton B. Ivanov, Rebecca Castano, Joshua L. Bandfield
Dunes on Titan observed by Cassini Radar Dunes on Titan observed by Cassini Radar
Thousands of longitudinal dunes have recently been discovered by the Titan Radar Mapper on the surface of Titan. These are found mainly within ±30° of the equator in optically-, near-infrared-, and radar-dark regions, indicating a strong proportion of organics, and cover well over 5% of Titan's surface. Their longitudinal duneform, interactions with topography, and correlation with other...
Authors
J. Radebaugh, R. D. Lorenz, J. I. Lunine, S. D. Wall, G. Boubin, E. Reffet, Randolph L. Kirk, R.M. Lopes, E. R. Stofan, Laurence A. Soderblom, M. Allison, M. Janssen, P. Paillou, P. Callahan, Carl Spencer
Three-dimensional P-wave velocity structure and precise earthquake relocation at Great Sitkin Volcano, Alaska Three-dimensional P-wave velocity structure and precise earthquake relocation at Great Sitkin Volcano, Alaska
Waveform cross-correlation with bispectrum verification is combined with double-difference tomography to increase the precision of earthquake locations and constrain regional 3D P-wave velocity heterogeneity at Great Sitkin volcano, Alaska. From 1999 through 2005, the Alaska Volcano Observatory (AVO) recorded ∼1700 earthquakes in the vicinity of Great Sitkin, including two ML 4.3...
Authors
Jeremy Pesicek, Clifford H. Thurber, Heather R. DeShon, Stephanie G. Prejean, Haijiang Zhang