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Hawaiian Volcano Observatory 1974 Annual Administrative Report Hawaiian Volcano Observatory 1974 Annual Administrative Report

INTRODUCTORY NOTE The Hawaiian Volcano Observatory Summaries have been published in the current format since 1956. The Quarterly Summaries (1956 through 1973) and the Annual Summaries (1974 through 1985) were originally published as Administrative Reports. These reports have been compiled and published as U.S. Geological Survey Open-File Reports. The quarterly reports have been combined...
Authors
Jennifer S. Nakata

Hazards from hydrothermally sealed volcanic conduits Hazards from hydrothermally sealed volcanic conduits

The 17 March 2006 eruption from Raoul Island (Kermadec arc, north of New Zealand) is interpreted as a magmatic‐hydrothermal event triggered by shaking associated with a swarm of local earthquakes. The eruption, which tragically claimed the life of New Zealand Department of Conservation Ranger Mark Kearney, occurred without significant volcanic seismicity or any of the precursory...
Authors
B.W. Christenson, Cynthia A. Werner, A.G. Reyes, S. Sherburn, B.J. Scott, C. Miller, M.J. Rosenburg, A.W. Hurst, K.A. Britten

40Ar/39Ar ages of the AD 79 eruption of Vesuvius, Italy 40Ar/39Ar ages of the AD 79 eruption of Vesuvius, Italy

The Italian volcano, Vesuvius, erupted explosively in AD 79. Sanidine from pumice collected at Casti Amanti in Pompeii and Villa Poppea in Oplontis yielded a weighted-mean 40Ar/39Ar age of 1925±66 years in 2004 (1σ uncertainty) from incremental-heating experiments of eight aliquants of sanidine. This is the calendar age of the eruption. Our results together with the work of Renne et al....
Authors
Marvin A. Lanphere, Duane E. Champion, Leone Melluso, Vincenzo Morra, Annamaria Perrotta, Claudio Scarpati, Dario Tedesco, Andrew T. Calvert

Mount St. Helens Petrology Workshop Mount St. Helens Petrology Workshop

Following seismic activity in late September 2004, the current eruption of Mount St. Helens began with an explosive steam and ash emission on 1 October 2004, with hot dacite emerging from the crater floor on 11 October 2004. Nearly two years later, with more than 80 million cubic meters of erupted dacite, accompanied by rare explosions and predominantly shallow seismicity questions still...
Authors
Michael C. Rowe, John S. Pallister, Anita L. Grunder

Drag-out effect of piezomagnetic signals due to a borehole: The Mogi source as an example Drag-out effect of piezomagnetic signals due to a borehole: The Mogi source as an example

We show that using borehole measurements in tectonomagnetic experiments allows enhancement of the observed signals. New magnetic dipoles, which vary with stress changes from mechanical sources, are produced on the walls of the borehole. We evaluate such an effect quantitatively. First we formulate a general expression for the borehole effect due to any arbitrary source models. This is...
Authors
Y. Sasai, M.J.S. Johnston, Y. Tanaka, R. Mueller, T. Hashimoto, M. Utsugi, S. Sakanaka, M. Uyeshima, J. Zlotnicki, P. Yvetot

Hydrothermal circulation at Mount St. Helens determined by self-potential measurements Hydrothermal circulation at Mount St. Helens determined by self-potential measurements

The distribution of hydrothermal circulation within active volcanoes is of importance in identifying regions of hydrothermal alteration which may in turn control explosivity, slope stability and sector collapse. Self-potential measurements, indicative of fluid circulation, were made within the crater of Mount St. Helens in 2000 and 2001. A strong dipolar anomaly in the self-potential...
Authors
Paul A. Bedrosian, Martyn J. Unsworth, Malcolm J. S. Johnston

Annual modulation of seismicity along the San Andreas Fault near Parkfield, CA Annual modulation of seismicity along the San Andreas Fault near Parkfield, CA

We analyze seismic data from the San Andreas Fault (SAF) near Parkfield, California, to test for annual modulation in seismicity rates. We use statistical analyses to show that seismicity is modulated with an annual period in the creeping section of the fault and a semiannual period in the locked section of the fault. Although the exact mechanism for seasonal triggering is undetermined...
Authors
L.B. Christiansen, Shaul Hurwitz, Steven E. Ingebritsen

Vapor transfer prior to the October 2004 eruption of Mount St. Helens, Washington Vapor transfer prior to the October 2004 eruption of Mount St. Helens, Washington

Dome lavas from the 2004 eruption of Mount St. Helens show elevated Li contents in plagioclase phenocrysts at the onset of dome growth in October 2004. These cannot be explained by variations in plagioclase-melt partitioning, but require elevated Li contents in coexisting melt, a fact confirmed by measurements of Li contents as high as 207 µg/g in coexisting melt inclusions. Similar Li...
Authors
A.J.R. Kent, J. Blundy, K. V. Cashman, K.M. Copper, C. Donnelly, John S. Pallister, M. Reagan, M.C. Rowe, Carl Thornber

Understanding Merapi-type volcanoes Understanding Merapi-type volcanoes

"We have to understand volcano science to know what to monitor.” That simple statement by Antonius Ratdomopurbo, director of the Indonesian Center for Volcano Technology [Balai Penyelidikan dan Pengembangan‐Teknologi (BPPTK)],captured the spirit and content of a recent workshop about Merapi and Merapi‐type volcanoes. Merapi still is experiencing low levels of unrest, following a peak in...
Authors
M.A. Purbawinata, Antonius Ratdomopurbo, John S. Pallister, B. Luehr, Chris Newhall

Tsunami warnings: Understanding in Hawai'i Tsunami warnings: Understanding in Hawai'i

The devastating southeast Asian tsunami of December 26, 2004 has brought home the destructive consequences of coastal hazards in an absence of effective warning systems. Since the 1946 tsunami that destroyed much of Hilo, Hawai‘i, a network of pole mounted sirens has been used to provide an early public alert of future tsunamis. However, studies in the 1960s showed that understanding of...
Authors
Chris E. Gregg, Bruce F. Houghton, Douglas Paton, David M. Johnston, David A. Swanson, B.S. Yanagi

Three-dimensional P-wave velocity structure derived from local earthquakes at the Katmai group of volcanoes, Alaska Three-dimensional P-wave velocity structure derived from local earthquakes at the Katmai group of volcanoes, Alaska

The three-dimensional P-wave velocity structure beneath the Katmai group of volcanoes is determined by inversion of more than 10,000 rays from over 1000 earthquakes recorded on a local 18 station short-period network between September 1996 and May 2001. The inversion is well constrained from sea level to about 6 km below sea level and encompasses all of the Katmai volcanoes; Martin...
Authors
A.D. Jolly, S.C. Moran, S.R. McNutt, D.B. Stone

Accelerated uplift and magmatic intrusion of the Yellowstone caldera, 2004 to 2006 Accelerated uplift and magmatic intrusion of the Yellowstone caldera, 2004 to 2006

The Yellowstone caldera began a rapid episode of ground uplift in mid-2004, revealed by Global Positioning System and interferometric synthetic aperture radar measurements, at rates up to 7 centimeters per year, which is over three times faster than previously observed inflation rates. Source modeling of the deformation data suggests an expanding volcanic sill of ???1200 square...
Authors
Wu-Lung Chang, Robert B. Smith, Charles Wicks, J.M. Farrell, C.M. Puskas
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