Publications
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Instrumentation in remote and dangerous settings; examples using data from GPS “spider” deployments during the 2004-2005 eruption of Mount St. Helens, Washington
Self-contained, single-frequency GPS instruments fitted
on lightweight stations suitable for helicopter-sling payloads
became a critical part of volcano monitoring during the
September 2004 unrest and subsequent eruption of Mount St.
Helens. Known as “spiders” because of their spindly frames,
the stations were slung into the crater 29 times from September 2004 to December 2005 when conditions
Authors
Richard G. LaHusen, Kelly J. Swinford, Matthew Logan, Michael Lisowski
Analysis of GPS-measured deformation associated with the 2004-2006 dome-building eruption of Mount St. Helens, Washington
Detecting far-field deformation at Mount St. Helens
since the crater-forming landslide and blast in 1980 has been
difficult despite frequent volcanic activity and improved
monitoring techniques. Between 1982 and 1991, the systematic extension of line lengths in a regional GPS trilateration network is consistent with recharge of a deep magma
chamber during that interval. The rate of extension,
Authors
Michael Lisowski, Daniel Dzurisin, Roger P. Denlinger, Eugene Y. Iwatsubo
The Pleistocene eruptive history of Mount St. Helens, Washington, from 300,000 to 12,800 years before present
We report the results of recent geologic mapping and radiometric dating that add considerable detail to our understanding of the eruptive history of Mount St. Helens before its latest, or Spirit Lake, stage. New data and reevaluation of earlier work indicate at least two eruptive periods during the earliest, or Ape Canyon, stage, possibly separated by a long hiatus: one about 300-250 ka and a seco
Authors
Michael A. Clynne, Andrew T. Calvert, Edward W. Wolfe, Russell C. Evarts, Robert J. Fleck, Marvin A. Lanphere
Book review of Avalanche Dynamics by Shiva P. Pudasaini and Kolumban Hutter. Springer: Berlin-Heidelberg, 2007. 602 pages, 225 figures, 15 tables
This highly specialized book is interesting not only because of its important subject matter but also because of its egocentric perspective. The majority of the book provides a nearly exhaustive retrospective of the authors’ many contributions to the shallow‐flow theory of granular avalanches, and it also critiques contributions by others. Indeed, some readers (including this reviewer) might be di
Authors
Richard M. Iverson
Broadband characteristics of earthquakes recorded during a dome-building eruption at Mount St. Helens, Washington, between October 2004 and May 2005
From October 2004 to May 2005, the Center for Earthquake Research and Information of the University of Memphis
operated two to six broadband seismometers within 5 to 20
km of Mount St. Helens to help monitor recent seismic and
volcanic activity. Approximately 57,000 earthquakes identified during the 7-month deployment had a normal magnitude
distribution with a mean magnitude of 1.78 and a stan
Authors
Stephen P. Horton, Robert D. Norris, Seth C. Moran
Chlorine degassing during the lava dome-building eruption of Mount St. Helens, 2004-2005
Remote measurements of volcanic gases from the
Mount St. Helens lava dome were carried out using OpenPath Fourier-Transform Infrared spectroscopy on August 31,
2005. Measurements were performed at a site ~1 km from
the lava dome, which was used as a source of IR radiation.
On average, during the period of measurement, the volcanic
gas contained 99 mol percent H2
O, 0.78 percent CO2
, 0.095
p
Authors
Marie Edmonds, Kenneth A. McGee, Michael P. Doukas
Absolute and relative locations of earthquakes at Mount St. Helens, Washington, using continuous data: Implications for magmatic processes
This study uses a combination of absolute and relative locations from earthquake multiplets to investigate the
seismicity associated with the eruptive sequence at Mount St.
Helens between September 23, 2004, and November 20, 2004.
Multiplets, a prominent feature of seismicity during this time
period, occurred as volcano-tectonic, hybrid, and low-frequency earthquakes spanning a large range of
Authors
Weston A. Thelen, Robert S. Crosson, Kenneth C. Creager
Emission rates of CO2, SO2, and H2S, scrubbing, and preeruption excess volatiles at Mount St. Helens, 2004-2005
Airborne surveillance of gas emissions began at Mount
St. Helens on September 27, 2004. Reconnaissance measurements--SO2
column abundances and CO2
, SO2
, and H2
S
concentrations--showed neither a gas plume downwind of
the volcano nor gas sources within the crater. Subsequent
measurements taken during the period of unrest before the
eruption began on October 1 and for several days after Octo
Authors
Terrence M. Gerlach, Kenneth A. McGee, Michael P. Doukas
Near-real-time information products for Mount St. Helens -- tracking the ongoing eruption
The rapid onset of energetic seismicity on September
23, 2004, at Mount St. Helens caused seismologists at the
Pacific Northwest Seismic Network and the Cascades Volcano Observatory to quickly improve and develop techniques
that summarized and displayed seismic parameters for use by
scientists and the general public. Such techniques included
webicorders (Web-based helicorder-like displays), g
Authors
Anthony I. Qamar, Stephen Malone, Seth C. Moran, William P. Steele, Weston A. Thelen
Pre- and post-eruptive investigations of gas and water samples from Mount St. Helens, Washington, 2002 to 2005
Samples of gas and water from thermal springs in
Loowit and Step canyons and creeks that drain the crater at
Mount St. Helens have been collected since October 2004
to monitor the flux of dissolved magmatic volatiles in the
hydrologic system. The changing composition of the waters
highlights a trend that began as early as 1994 and includes
decreasing SO4
and Cl concentrations and large incr
Authors
D. Bergfeld, William C. Evans, Kenneth A. McGee, Kurt R. Spicer
Seismicity associated with renewed dome building at Mount St. Helens, 2004-2005
The reawakening of Mount St. Helens after 17 years and 11 months of slumber was heralded by a swarm of shallow
(depth 2 earthquakes were
occurring at a rate of ~1 per minute. A gradual transition from
volcano-tectonic to hybrid and low-frequency events occurred
along with this intensification, a characteristic of many precursory swarms at Mount St. Helens before dome-building
eruptions in the
Authors
Seth C. Morgan, Stephen D. Malone, Anthony I. Qamar, Weston A. Thelen, Amy K. Wright, Jacqueline Caplan-Auerbach