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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

Oxygen isotope geochemistry of the lassen volcanic center, California: Resolving crustal and mantle contributions to continental Arc magmatism Oxygen isotope geochemistry of the lassen volcanic center, California: Resolving crustal and mantle contributions to continental Arc magmatism

This study reports oxygen isotope ratios determined by laser fluorination of mineral separates (mainly plagioclase) from basaltic andesitic to rhyolitic composition volcanic rocks erupted from the Lassen Volcanic Center (LVC), northern California. Plagioclase separates from nearly all rocks have δ18O values (6·1–8·4‰) higher than expected for production of the magmas by partial melting...
Authors
T.C. Feeley, M.A. Clynne, G.S. Winer, W.C. Grice

The 8 October 2006 Md 4.5 Cowlitz chimneys earthquake in Mount Rainier National Park The 8 October 2006 Md 4.5 Cowlitz chimneys earthquake in Mount Rainier National Park

An Md 4.5 earthquake located ∼12 km east of Mount Rainier occurred on 8 October 2006 at 02:48 UTC (figure 1). Although not large enough to be damaging or of major tectonic significance, a summary description of the earthquake is warranted because of its proximity to Mount Rainier, and because earthquakes of Md ≥ 4.5 are relatively rare in this region. Previous events of Md ≥ 4.5 have...
Authors
J. Renate Hartog, Joan S. Gomberg, Seth C. Moran, Amy K. Wright, Karen L. Meagher

Eruption dynamics at Mount St. Helens imaged from broadband seismic waveforms: Interaction of the shallow magmatic and hydrothermal systems Eruption dynamics at Mount St. Helens imaged from broadband seismic waveforms: Interaction of the shallow magmatic and hydrothermal systems

The current eruption at Mount St. Helens is characterized by dome building and shallow, repetitive, long-period (LP) earthquakes. Waveform cross-correlation reveals remarkable similarity for a majority of the earthquakes over periods of several weeks. Stacked spectra of these events display multiple peaks between 0.5 and 2 Hz that are common to most stations. Lower-amplitude very-long...
Authors
G.P. Waite, B. A. Chouet, P.B. Dawson

Landslides triggered by the 8 October 2005 Kashmir earthquake Landslides triggered by the 8 October 2005 Kashmir earthquake

The 8 October 2005 Kashmir earthquake triggered several thousand landslides. These were mainly rock falls and debris falls, although translational rock and debris slides also occurred. In addition, a sturzstrom (debris avalanche) comprising ??? 80??million m3 buried four villages and blocked streams to create two lakes. Although landsliding occurred throughout the region, covering an...
Authors
L.A. Owen, U. Kamp, G.A. Khattak, E. L. Harp, D. K. Keefer, M.A. Bauer
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