Publications
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Late eighteenth century Old Maid eruption and lahars at Mount Hood, Oregon (USA) dated with tree rings and historical observations Late eighteenth century Old Maid eruption and lahars at Mount Hood, Oregon (USA) dated with tree rings and historical observations
Tree rings of subfossil trees buried by lahars and lahar-derived sediments along the Sandy and Zigzag Rivers record the onset of a late eighteenth century eruption at Mount Hood, Oregon, USA (Figs. 1–2). Crandell (1980) described and named this eruptive activity the ‘Old Maid eruptive period’ and estimated its age at about “200–300 year” using radiocarbon ages of trees killed by lahars...
Authors
Patrick T. Pringle, Thomas C. Pierson, Kenneth A. Cameron, P.R. Sheppard
Source materials for inception stage Hawaiian magmas: Pb‐He isotope variations for early Kilauea Source materials for inception stage Hawaiian magmas: Pb‐He isotope variations for early Kilauea
New noble gas and radiogenic isotopic compositions are presented for tholeiitic, transitional, and alkalic rocks from the submarine Hilina region on the south flank of Kilauea, Hawaii. The 3He/4He ratios for undegassed glass and olivine separates (11–26 Ra) contrast with those of postshield and rejuvenated alkalic lavas, consistent with the alkalic and transitional basalts at Hilina...
Authors
Takeshi Hanyu, Jun-Ichi Kimura, Maiko Katakuse, Andrew T. Calvert, Thomas W. Sisson, Shun’ichi Nakai
Rheologic and structural controls on the deformation of Okmok volcano, Alaska: FEMs, InSAR, and ambient noise tomography Rheologic and structural controls on the deformation of Okmok volcano, Alaska: FEMs, InSAR, and ambient noise tomography
Interferometric synthetic aperture radar (InSAR) data indicate that the caldera of Okmok volcano, Alaska, subsided more than a meter during its eruption in 1997. The large deformation suggests a relatively shallow magma reservoir beneath Okmok. Seismic tomography using ambient ocean noise reveals two low‐velocity zones (LVZs). The shallow LVZ corresponds to a region of weak, fluid...
Authors
Timothy Masterlark, Matthew M. Haney, Haylee Dickinson, Cheryl Searcy, T. Fournier
Book Review: Geological fluid dynamics: Sub-surface flow and reactions Book Review: Geological fluid dynamics: Sub-surface flow and reactions
No abstract available
Authors
Steven E. Ingebritsen
Volcano-Monitoring Instrumentation in the United States, 2008 Volcano-Monitoring Instrumentation in the United States, 2008
The United States is one of the most volcanically active countries in the world. According to the global volcanism database of the Smithsonian Institution, the United States (including its Commonwealth of the Northern Mariana Islands) is home to about 170 volcanoes that are in an eruptive phase, have erupted in historical time, or have not erupted recently but are young enough (eruptions...
Authors
Marianne Guffanti, Angela K. Diefenbach, John W. Ewert, David W. Ramsey, Peter F. Cervelli, Steven P. Schilling
Subevents of long-period seismicity: implications for hydrothermal dynamics during the 2004-2008 eruption of Mount St. Helens Subevents of long-period seismicity: implications for hydrothermal dynamics during the 2004-2008 eruption of Mount St. Helens
One of the most striking aspects of seismicity during the 2004–2008 eruption of Mount St. Helens (MSH) was the precise regularity in occurrence of repetitive long-period (LP) or “drumbeat” events over sustained time periods. However, this precise regularity was not always observed, and at times the temporal occurrence of LP events became more random. In addition, accompanying the...
Authors
Robin S. Matoza, Bernard A. Chouet
Learning to recognize volcanic non-eruptions Learning to recognize volcanic non-eruptions
An important goal of volcanology is to answer the questions of when, where, and how a volcano will erupt—in other words, eruption prediction. Generally, eruption predictions are based on insights from monitoring data combined with the history of the volcano. An outstanding example is the A.D. 1980–1986 lava dome growth at Mount St. Helens, Washington (United States). Recognition of a...
Authors
Michael P. Poland
Origins of large-volume, compositionally zoned volcanic eruptions: New constraints from U-series isotopes and numerical thermal modeling for the 1912 Katmai-Novarupta eruption Origins of large-volume, compositionally zoned volcanic eruptions: New constraints from U-series isotopes and numerical thermal modeling for the 1912 Katmai-Novarupta eruption
We present the results of a combined U-series isotope and numerical modeling study of the 1912 Katmai-Novarupta eruption in Alaska. A stratigraphically constrained set of samples have compositions that range from basalt through basaltic andesite, andesite, dacite, and rhyolite. The major and trace element range can be modeled by 80–90% closed-system crystal fractionation over a...
Authors
Simon Turner, Mike Sandiford, Mark Reagan, Chris Hawkesworth, Wes Hildreth
Characterizing 6 August 2007 Crandall Canyon mine collapse from ALOS PALSAR InSAR Characterizing 6 August 2007 Crandall Canyon mine collapse from ALOS PALSAR InSAR
We used ALOS InSAR images to study land surface deformation over the Crandall Canyon mine in Utah, which collapsed on 6 August 2007 and killed six miners. The collapse was registered as a ML 3.9 seismic event. An InSAR image spanning the time of the collapse shows 25–30 cm surface subsidence over the mine. We used distributed dislocation sources to model the deformation field, and found...
Authors
Zhong Lu, Charles Wicks
Interdisciplinary studies of eruption at Chaitén volcano, Chile Interdisciplinary studies of eruption at Chaitén volcano, Chile
High-silica rhyolite magma fuels Earth's largest and most explosive eruptions. Recurrence intervals for such highly explosive eruptions are in the 100- to 100,000-year time range, and there have been few direct observations of such eruptions and their immediate impacts. Consequently, there was keen interest within the volcanology community when the first large eruption of high-silica...
Authors
John S. Pallister, Jon J. Major, Thomas C. Pierson, Richard P. Holitt, Jacob B. Lowenstern, John C. Eichelberger, Lara Luis, Hugo Moreno, Jorge Muñoz, Jonathan M. Castro, Andrés Iroumé, Andrea Andreoli, Julia Jones, Fred Swanson, Charlie Crisafulli
Eruptions of Hawaiian volcanoes—Past, present, and future Eruptions of Hawaiian volcanoes—Past, present, and future
Viewing an erupting volcano is a memorable experience, one that has inspired fear, superstition, worship, curiosity, and fascination since before the dawn of civilization. In modern times, volcanic phenomena have attracted intense scientific interest because they provide the key to understanding processes that have created and shaped more than 80 percent of the Earth’s surface. The...
Authors
Katherine M. Mulliken, Robert I. Tilling, Donald A. Swanson
Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii Infrasonic harmonic tremor and degassing bursts from Halema'uma'u Crater, Kilauea Volcano, Hawaii
The formation, evolution, collapse, and subsequent resurrection of a vent within Halema'uma'u Crater, Kilauea Volcano, produced energetic and varied degassing signals recorded by a nearby infrasound array between 2008 and early 2009. After 25 years of quiescence, a vent-clearing explosive burst on 19 March 2008 produced a clear, complex acoustic signal. Near-continuous harmonic...
Authors
David Fee, Milton Garces, Matt Patrick, Bernard Chouet, Phil Dawson, Donald A. Swanson