Publications
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Volcanic versus anthropogenic carbon dioxide Volcanic versus anthropogenic carbon dioxide
Which emits more carbon dioxide (CO2): Earth's volcanoes or human activities? Research findings indicate unequivocally that the answer to this frequently asked question is human activities. However, most people, including some Earth scientists working in fields outside volcanology, are surprised by this answer. The climate change debate has revived and reinforced the belief, widespread...
Authors
T. Gerlach
Migrating swarms of brittle-failure earthquakes in the lower crust beneath Mammoth Mountain, California Migrating swarms of brittle-failure earthquakes in the lower crust beneath Mammoth Mountain, California
Brittle-failure earthquakes in the lower crust, where high pressures and temperatures would typically promote ductile deformation, are relatively rare but occasionally observed beneath active volcanic centers. Where they occur, these earthquakes provide a rare opportunity to observe volcanic processes in the lower crust, such as fluid injection and migration, which may induce brittle...
Authors
D.R. Shelly, D.P. Hill
Pigeonholing pyroclasts: Insights from the 19 March 2008 explosive eruption of Kīlauea volcano Pigeonholing pyroclasts: Insights from the 19 March 2008 explosive eruption of Kīlauea volcano
We think, conventionally, of volcanic explosive eruptions as being triggered in one of two ways: by release and expansion of volatiles dissolved in the ejected magma (magmatic explosions) or by transfer of heat from magma into an external source of water (phreatic or phreatomagmatic explosions). We document here an event where neither magma nor an external water source was involved in...
Authors
Bruce F. Houghton, Don Swanson, R.J. Carey, J. Rausch, Andrew Sutton
Origin of a rhyolite that intruded a geothermal well while drilling at the Krafla volcano, Iceland Origin of a rhyolite that intruded a geothermal well while drilling at the Krafla volcano, Iceland
Magma flowed into an exploratory geothermal well at 2.1 km depth being drilled in the Krafla central volcano in Iceland, creating a unique opportunity to study rhyolite magma in situ in a basaltic environment. The quenched magma is a partly vesicular, sparsely phyric, glass containing ∼1.8% of dissolved volatiles. Based on calculated H2O-CO2 saturation pressures, it degassed at a...
Authors
W.A. Elders, G.O. Fridleifsson, R.A. Zierenberg, E.C. Pope, A.K. Mortensen, A. Gudmundsson, Jacob B. Lowenstern, N.E. Marks, L. Owens, D.K. Bird, M. Reed, N.J. Olsen, Peter Schiffmant
Variations in eruption style during the 1931 A.D. eruption of Aniakchak volcano, Alaska Variations in eruption style during the 1931 A.D. eruption of Aniakchak volcano, Alaska
The 1931 A.D. eruption of Aniakchak volcano, Alaska, progressed from subplinian to effusive eruptive style and from trachydacite to basaltic andesite composition from multiple vent locations. Eyewitness accounts and new studies of deposit stratigraphy provide a combined narrative of eruptive events. Additional field, compositional, grain size, componentry, density, and grain morphology...
Authors
Robert S. Nicholson, James E. Gardner, Christina A. Neal
Database for potential hazards from future volcanic eruptions in California Database for potential hazards from future volcanic eruptions in California
More than 500 volcanic vents have been identified in the State of California. At least 76 of these vents have erupted, some repeatedly, during the past 10,000 yr. Past volcanic activity has ranged in scale and type from small rhyolitic and basaltic eruptions through large catastrophic rhyolitic eruptions. Sooner or later, volcanoes in California will erupt again, and they could have...
Authors
Melissa N. White, David W. Ramsey, C. Dan Miller
Infrasound from the 2007 fissure eruptions of Kīlauea Volcano, Hawai'i Infrasound from the 2007 fissure eruptions of Kīlauea Volcano, Hawai'i
Varied acoustic signals were recorded at Kīlauea Volcano in mid-2007, coincident with dramatic changes in the volcano's activity. Prior to this time period, Pu'u 'Ō'ō crater produced near-continuous infrasonic tremor and was the primary source of degassing and lava effusion at Kīlauea. Collapse and draining of Pu'u 'Ō'ō crater in mid-June produced impulsive infrasonic signals and...
Authors
D. Fee, M. Garces, Tim R. Orr, Michael P. Poland
Segregating gas from melt: an experimental study of the Ostwald ripening of vapor bubbles in magmas Segregating gas from melt: an experimental study of the Ostwald ripening of vapor bubbles in magmas
Diffusive coarsening (Ostwald ripening) of H2O and H2O-CO2 bubbles in rhyolite and basaltic andesite melts was studied with elevated temperature–pressure experiments to investigate the rates and time spans over which vapor bubbles may enlarge and attain sufficient buoyancy to segregate in magmatic systems. Bubble growth and segregation are also considered in terms of classical steady...
Authors
Nicole C. Lautze, Thomas W. Sisson, Margaret T. Mangan, Timothy L. Grove
Multiplets: Their behavior and utility at dacitic and andesitic volcanic centers Multiplets: Their behavior and utility at dacitic and andesitic volcanic centers
Multiplets, or groups of earthquakes with similar waveforms, are commonly observed at volcanoes, particularly those exhibiting unrest. Using triggered seismic data from the 1980-1986 Mount St. Helens (MSH) eruption, we have constructed a catalog of multiplet occurrence. Our analysis reveals that the occurrence of multiplets is related, at least in part, to the viscosity of the magma. We...
Authors
W. Thelen, S. Malone, M. West
Ancient Saltworks of the Sierra Nevada Ancient Saltworks of the Sierra Nevada
No abstract available.
Authors
James G. Moore, Michael F. Diggles
High-resolution receiver function imaging reveals Colorado Plateau lithospheric architecture and mantle-supported topography High-resolution receiver function imaging reveals Colorado Plateau lithospheric architecture and mantle-supported topography
After maintaining elevations near sea level for over 500 million years, the Colorado Plateau (CP) has a present average elevation of 2 km. We compute new receiver function images from the first dense seismic transect to cross the plateau that reveal a central CP crustal thickness of 42–50 km thinning to 30–35 km at the CP margins. Isostatic calculations show that only approximately 20%...
Authors
Dorothy L. Domingo, R. Aster, S. Grand, J Ni, W.S. Baldridge, David C. Wilson USGS
Digital topographic map showing the extents of glacial ice and perennial snowfields at Mount Rainier, Washington, based on the LiDAR survey of September 2007 to October 2008 Digital topographic map showing the extents of glacial ice and perennial snowfields at Mount Rainier, Washington, based on the LiDAR survey of September 2007 to October 2008
In response to severe flooding in November 2006, the National Park Service contracted for a high-resolution aerial Light Detection and Ranging (LiDAR) topographic survey of Mount Rainier National Park, Washington. Due to inclement weather, this survey was performed in two stages: early September 2007 and September-October 2008. The total surveyed area of 241,585 acres includes an...
Authors
Joel E. Robinson, Thomas W. Sisson, Darin D. Swinney