Publications
Filter Total Items: 3006
The 2009 eruption of Redoubt Volcano, Alaska The 2009 eruption of Redoubt Volcano, Alaska
Redoubt Volcano, an ice-covered stratovolcano on the west side of Cook Inlet, erupted in March 2009 after several months of escalating unrest. The 2009 eruption of Redoubt Volcano shares many similarities with eruptions documented most recently at Redoubt in 1966–68 and 1989–90. In each case, the eruptive phase lasted several months, consisted of multiple ashproducing explosions...
Authors
Katharine F. Bull, Cheryl Cameron, Michelle L. Coombs, Angie Diefenbach, Taryn Lopez, Steve McNutt, Christina A. Neal, Allison Payne, John A. Power, David J. Schneider, William E. Scott, Seth Snedigar, Glenn Thompson, Kristi L. Wallace, Christopher F. Waythomas, Peter Webley, Cynthia A. Werner
The 2010 explosive eruption of Java's Merapi volcano—A ‘100-year’ event The 2010 explosive eruption of Java's Merapi volcano—A ‘100-year’ event
Merapi volcano (Indonesia) is one of the most active and hazardous volcanoes in the world. It is known for frequent small to moderate eruptions, pyroclastic flows produced by lava dome collapse, and the large population settled on and around the flanks of the volcano that is at risk. Its usual behavior for the last decades abruptly changed in late October and early November 2010, when...
Authors
Surono, Philippe Jousset, John S. Pallister, Marie Boichu, M. Fabrizia Buongiorno, Agus Budisantoso, Fidel Costa, Supriyati Andreastuti, Fred Prata, David J. Schneider, Lieven Clarisse, Hanik Humaida, Sri Sumarti, Christian Bignami, Julia P. Griswold, Simon A. Carn, Clive Oppenheimer, Franck Lavigne
Mechanics of debris flows and rock avalanches: Chapter 43 Mechanics of debris flows and rock avalanches: Chapter 43
Debris flows are geophysical phenomena intermediate in character between rock avalanches and flash floods. They commonly originate as water-laden landslides on steep slopes and transform into liquefied masses of fragmented rock, muddy water, and entrained organic matter that disgorge from canyons onto valley floors. Typically including 50%–70% solid grains by volume, attaining speeds >10...
Authors
Richard M. Iverson
El Niño-Southern oscillation variability from the late cretaceous marca shale of California El Niño-Southern oscillation variability from the late cretaceous marca shale of California
Changes in the possible behavior of El Niño–Southern Oscillation (ENSO) with global warming have provoked interest in records of ENSO from past “greenhouse” climate states. The latest Cretaceous laminated Marca Shale of California permits a seasonal-scale reconstruction of water column flux events and hence interannual paleoclimate variability. The annual flux cycle resembles that of the...
Authors
Andrew Davies, Alan E.S. Kemp, Graham P. Weedon, John A. Barron
Generation and evolution of hydrothermal fluids at Yellowstone: Insights from the Heart Lake Geyser Basin Generation and evolution of hydrothermal fluids at Yellowstone: Insights from the Heart Lake Geyser Basin
We sampled fumaroles and hot springs from the Heart Lake Geyser Basin (HLGB), measured water and gas discharge, and estimated heat and mass flux from this geothermal area in 2009. The combined data set reveals that diverse fluids share an origin by mixing of deep solute-rich parent water with dilute heated meteoric water, accompanied by subsequent boiling. A variety of chemical and...
Authors
J. B. Lowenstern, D. Bergfeld, William C. Evans, S. Hurwitz
Earthquake studies reveal the magmatic plumbing system of the Katmai volcanoes Earthquake studies reveal the magmatic plumbing system of the Katmai volcanoes
The 1912 eruption of Novarupta was the largest of the 1900s (Fierstein and Hildreth 2001, Hildreth et al. 2003). A century later, fundamental questions remain regarding the source of the magma for that eruption. A previous seismic study of the Katmai area (Jolly et al. 2007) identified a single large area of anomalous structure in the subsurface centered beneath Katmai Pass (Figure 2)...
Authors
Clifford Thurber, Rachel Murphy, Stephanie G. Prejean, Matthew M. Haney, Ninfa Bennington, Lee Powell, John F. Paskievitch
Modeling the formation of porphyry-copper ores Modeling the formation of porphyry-copper ores
Porphyry-copper ore systems, the source of much of the world's copper and molybdenum, form when metal-bearing fluids are expelled from shallow, degassing magmas. On page 1613 of this issue, Weis et al. (1) demonstrate that self-organizing processes focus metal deposition. Specifically, their simulation studies indicate that ores develop as consequences of dynamic variations in rock...
Authors
Steven E. Ingebritsen
Seawater capacitance – a promising proxy for mapping and characterizing drifting hydrocarbon plumes in the deep ocean Seawater capacitance – a promising proxy for mapping and characterizing drifting hydrocarbon plumes in the deep ocean
Hydrocarbons released into the deep ocean are an inevitable consequence of natural seep, seafloor drilling, and leaking wellhead-to-collection-point pipelines. The Macondo 252 (Deepwater Horizon) well blowout of 2010 was even larger than the Ixtoc event in the Gulf of Campeche in 1979. History suggests it will not be the last accidental release, as deepwater drilling expands to meet an...
Authors
Jeff Wynn, John A. Fleming
Rootless shield and perched lava pond collapses at Kīlauea Volcano, Hawai'i Rootless shield and perched lava pond collapses at Kīlauea Volcano, Hawai'i
Effusion rate is a primary measurement used to judge the expected advance rate, length, and hazard potential of lava flows. At basaltic volcanoes, the rapid draining of lava stored in rootless shields and perched ponds can produce lava flows with much higher local effusion rates and advance velocities than would be expected based on the effusion rate at the vent. For several months in...
Authors
Matthew R. Patrick, Tim R. Orr
Keanakākoʻi Tephra produced by 300 years of explosive eruptions following collapse of Kīlauea's caldera in about 1500 CE Keanakākoʻi Tephra produced by 300 years of explosive eruptions following collapse of Kīlauea's caldera in about 1500 CE
The Keanakākoʻi Tephra at Kīlauea Volcano has previously been interpreted by some as the product of a caldera-forming eruption in 1790 CE. Our study, however, finds stratigraphic and 14C evidence that the tephra instead results from numerous eruptions throughout a 300-year period between about 1500 and 1800. The stratigraphic evidence includes: (1) as many as six pure lithic ash beds...
Authors
Donald A. Swanson, Timothy R. Rose, Richard S. Fiske, John P. McGeehin
Mapping ground surface deformation using temporarily coherent point SAR interferometry: Application to Los Angeles Basin Mapping ground surface deformation using temporarily coherent point SAR interferometry: Application to Los Angeles Basin
Multi-temporal interferometric synthetic aperture radar (InSAR) is an effective tool to detect long-term seismotectonic motions by reducing the atmospheric artifacts, thereby providing more precise deformation signal. The commonly used approaches such as persistent scatterer InSAR (PSInSAR) and small baseline subset (SBAS) algorithms need to resolve the phase ambiguities in interferogram...
Authors
L. Zhang, Zhong Lu, X. Ding, H.-S. Jung, G. Feng, C.-W. Lee
Water and heat transport in boreal soils: Implications for soil response to climate change Water and heat transport in boreal soils: Implications for soil response to climate change
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. However, the movement of liquid water, which plays an important role in the heat transport of temperate soils, has been under-represented in boreal studies. Two different heat transport models with and without convective heat transport were compared to measurements of soil temperatures in...
Authors
Zhaosheng Fan, Jennifer W. Harden, G.C. Winston, Jonathan A. O’Donnell, Jason C. Neff, Tingjun Zhang, Hugo Veldhuis, C.I. Czimczik