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Mapping the sources of the seismic wave field at Kilauea volcano, Hawaii, using data recorded on multiple seismic Antennas Mapping the sources of the seismic wave field at Kilauea volcano, Hawaii, using data recorded on multiple seismic Antennas

Seismic antennas constitute a powerful tool for the analysis of complex wave fields. Well-designed antennas can identify and separate components of a complex wave field based on their distinct propagation properties. The combination of several antennas provides the basis for a more complete understanding of volcanic wave fields, including an estimate of the location of each individual...
Authors
J. Almendros, B. Chouet, P. Dawson, Caleb G. Huber

Structure and physical characteristics of pumice from the climactic eruption of Mount Mazama (Crater Lake), Oregon Structure and physical characteristics of pumice from the climactic eruption of Mount Mazama (Crater Lake), Oregon

The vesicularity, permeability, and structure of pumice clasts provide insight into conditions of vesiculation and fragmentation during Plinian fall and pyroclastic flow-producing phases of the ~7,700 cal. year B.P. climactic eruption of Mount Mazama (Crater Lake), Oregon. We show that bulk properties (vesicularity and permeability) can be correlated with internal textures and that the...
Authors
C. Klug, K. Cashman, Charles R. Bacon

Steady subsidence of Medicine Lake volcano, northern California, revealed by repeated leveling surveys Steady subsidence of Medicine Lake volcano, northern California, revealed by repeated leveling surveys

Leveling surveys of a 193‐km circuit across Medicine Lake volcano (MLV) in 1954 and 1989 show that the summit area subsided by as much as 302 ± 30 mm (−8.6 ± 0.9 mm/yr) with respect to a datum point near Bartle, California, 40 km to the southwest. This result corrects an error in the earlier analysis of the same data by Dzurisin et al. [1991], who reported the subsidence rate as −11.1 ±...
Authors
Daniel Dzurisin, Michael P. Poland, Roland Bürgmann

Source mechanism of very-long-period signals accompanying dome growth activity at Merapi volcano, Indonesia Source mechanism of very-long-period signals accompanying dome growth activity at Merapi volcano, Indonesia

Very-long-period (VLP) pulses with period of 6–7s, displaying similar waveforms, were identified in 1998 from broadband seismographs around the summit crater. These pulses accompanied most of multiphase (MP) earthquakes, a type of long-period event locally defined at Merapi Volcano. Source mechanisms for several VLP pulses were examined by applying moment tensor inversion to the waveform...
Authors
D. Hidayat, B. Chouet, B. Voight, P. Dawson, Antonius Ratdomopurbo

Sulfur dioxide emission rates from Kīlauea Volcano, Hawai‘i, an update: 1998-2001 Sulfur dioxide emission rates from Kīlauea Volcano, Hawai‘i, an update: 1998-2001

Introduction Sulfur dioxide (SO2) emission rates from Kilauea Volcano were first measured by Stoiber and Malone (1975) and have been measured on a regular basis since 1979 (Greenland and others, 1985; Casadevall and others, 1987; Elias and others, 1998; Sutton and others, 2001). A compilation of SO2 emission-rate and wind-vector data from 1979 through 1997 is available as Open-File...
Authors
Tamar Elias, A. Jefferson Sutton

A Holocene paleosecular variation from 14C-dated volcanic rocks in western North America A Holocene paleosecular variation from 14C-dated volcanic rocks in western North America

A paleosecular variation (PSV) curve for western North America is presented on the basis of 94 virtual geomagnetic poles (VGPs) from dated volcanic rocks sampled at 446 sites. Approximately 60% of the paleomagnetic database has been previously published. A curve defined by “spherical smoothed splines” is fitted to the VGPs, ranked by the quality of the age determinations, where the data...
Authors
Jonathan T. Hagstrum, Duane E. Champion

Fault structure and kinematics of the Long Valley Caldera region, California, revealed by high-accuracy earthquake hypocenters and focal mechanism stress inversions Fault structure and kinematics of the Long Valley Caldera region, California, revealed by high-accuracy earthquake hypocenters and focal mechanism stress inversions

We have determined high-resolution hypocenters for 45,000+ earthquakes that occurred between 1980 and 2000 in the Long Valley caldera area using a double-difference earthquake location algorithm and routinely determined arrival times. The locations reveal numerous discrete fault planes in the southern caldera and adjacent Sierra Nevada block (SNB). Intracaldera faults include a series of...
Authors
Stephanie G. Prejean, William L. Ellsworth, Mark Zoback, Felix Waldhauser

Magma storage prior to the 1912 eruption at Novarupta, Alaska Magma storage prior to the 1912 eruption at Novarupta, Alaska

New analytical and experimental data constrain the storage and equilibration conditions of the magmas erupted in 1912 from Novarupta in the 20th century's largest volcanic event. Phase relations at H2O+CO2 fluid saturation were determined for an andesite (58.7 wt% SiO2) and a dacite (67.7 wt%) from the compositional extremes of intermediate magmas erupted. The phase assemblages, matrix...
Authors
J.E. Hammer, M.J. Rutherford, W. Hildreth

Preliminary volcano-hazard assessment for Kanaga Volcano, Alaska Preliminary volcano-hazard assessment for Kanaga Volcano, Alaska

Kanaga Volcano is a steep-sided, symmetrical, cone-shaped, 1307 meter high, andesitic stratovolcano on the north end of Kanaga Island (51°55’ N latitude, 177°10’ W longitude) in the western Aleutian Islands of Alaska. Kanaga Island is an elongated, low-relief (except for the volcano) island, located about 35 kilometers west of the community of Adak on Adak Island and is part of the...
Authors
Christopher F. Waythomas, Thomas P. Miller, Christopher J. Nye

Publications of the Volcano Hazards Program 2001 Publications of the Volcano Hazards Program 2001

The Volcano Hazards Program of the U.S. Geological Survey (USGS) is part of the Geologic Hazards Assessments subactivity as funded by Congressional appropriation. Investigations are carried out in the Geology and Hydrology Disciplines of the USGS and with cooperators at the Alaska Division of Geological and Geophysical Surveys, University of Alaska Fairbanks Geophysical Institute...
Authors
Manuel Nathenson

Morphology, volcanism, and mass wasting in Crater Lake, Oregon Morphology, volcanism, and mass wasting in Crater Lake, Oregon

Crater Lake was surveyed nearly to its shoreline by high-resolution multibeam echo sounding in order to define its geologic history and provide an accurate base map for research and monitoring surveys. The bathymetry and acoustic backscatter reveal the character of landforms and lead to a chronology for the concurrent filling of the lake and volcanism within the ca. 7700 calibrated yr B...
Authors
C. R. Bacon, J.V. Gardner, L. A. Mayer, M.W. Buktenica, P. Dartnell, D.W. Ramsey, J.E. Robinson
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