Publications
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Converting HAZUS capacity curves to seismic hazard-compatible building fragility functions: effect of hysteretic models Converting HAZUS capacity curves to seismic hazard-compatible building fragility functions: effect of hysteretic models
A methodology was recently proposed for the development of hazard-compatible building fragility models using parameters of capacity curves and damage state thresholds from HAZUS (Karaca and Luco, 2008). In the methodology, HAZUS curvilinear capacity curves were used to define nonlinear dynamic SDOF models that were subjected to the nonlinear time history analysis instead of the capacity...
Authors
Hyeuk Ryu, Nicolas Luco, Jack W. Baker, Erdem Karaca
Rapid Assessment of earthquake-induced landsliding Rapid Assessment of earthquake-induced landsliding
The Pacific Northwest in the United States including Seattle, Washington, experienced unusually heavy rainfall in the winters of 1995/1996 and 1996/1997, which caused numerous landslides. Following these two winters, the City of Seattle resolved to reduce future landslide losses within its jurisdiction. By coincidence, in 1997 the U.S. Geological Survey (USGS) began a five-year project...
Authors
J. W. Godt, B. Sener, K.L. Verdin, D.J. Wald, P.S. Earle, E. L. Harp, R.W. Jibson
High resolution imaging science experiment (HiRISE) images of volcanic terrains from the first 6 months of the Mars reconnaissance orbiter primary science phase High resolution imaging science experiment (HiRISE) images of volcanic terrains from the first 6 months of the Mars reconnaissance orbiter primary science phase
In the first 6 months of the Mars Reconnaissance Orbiter's Primary Science Phase, the High Resolution Imaging Science Experiment (HiRISE) camera has returned images sampling the diversity of volcanic terrains on Mars. While many of these features were noted in earlier imaging, they are now seen with unprecedented clarity. We find that some volcanic vents produced predominantly effusive...
Authors
Laszlo P. Keszthelyi, Windy L. Jaeger, Alfred S. McEwen, Livio L. Tornabene, Ross A. Beyer, Colin M. Dundas, Moses P. Milazzo
Pre-1991 sulfur transfer between mafic injections and dacite magma in the Mt. Pinatubo reservoir Pre-1991 sulfur transfer between mafic injections and dacite magma in the Mt. Pinatubo reservoir
Before the 1991–1992 activity, a large andesite lava dome belonging to the penultimate Pinatubo eruptive period (Buag ∼ 500 BP) formed the volcano summit. Buag porphyritic andesite contains abundant amphibole-bearing microgranular enclaves of basaltic–andesite composition. Buag enclaves have lower K2O and incompatible trace element (LREE, U, Th) contents than mafic pulses injected in the...
Authors
Muro A. Di, John S. Pallister, B. Villemant, Chris Newhall, M. Semet, M. Martinez, C. Mariet
A volcano rekindled: The renewed eruption of Mount St. Helens, 2004-2006 A volcano rekindled: The renewed eruption of Mount St. Helens, 2004-2006
Mount St. Helens began a dome-building eruption in September 2004 after nearly two decades of quiescence. Dome growth was initially robust, became more sluggish with time, and ceased completely in late January 2008. The volcano has been quiet again since January 2008. Professional Paper 1750 describes the first 1 1/2 years of this eruptive activity, chiefly from September 2004 until...
Authors
David R. Sherrod, William E. Scott, Peter H. Stauffer
EAARL topography - Vicksburg National Military Park 2008: Bare earth EAARL topography - Vicksburg National Military Park 2008: Bare earth
These remotely sensed, geographically referenced elevation measurements of Lidar-derived bare earth (BE) topography were produced as a collaborative effort between the U.S. Geological Survey (USGS), Florida Integrated Science Center (FISC), St. Petersburg, FL; the National Park Service (NPS), Gulf Coast Network, Lafayette, LA; and the National Aeronautics and Space Administration (NASA)...
Authors
Amar Nayegandhi, John Brock, C. Wayne Wright, Martha Segura, Xan Yates
Hydrocarbon lakes on Titan: Distribution and interaction with a porous regolith Hydrocarbon lakes on Titan: Distribution and interaction with a porous regolith
Synthetic Aperture Radar (SAR) images of Titan's north polar region reveal quasi‐circular to complex features which are interpreted to be liquid hydrocarbon lakes. We investigate methane transport in Titan's hydrologic cycle using the global distribution of lake features. As of May 2007, the SAR data set covers ∼22% of the surface and indicates multiple lake morphologies which are...
Authors
A. Hayes, O. Aharonson, P. Callahan, C. Elachi, Y. Gim, Randolph L. Kirk, K. Lewis, R. Lopes, R. Lorenz, J. Lunine, Ken Mitchell, Giuseppe Mitri, E. Stofan, S. Wall
Meteorites on Mars observed with Mars Exploration Rovers Meteorites on Mars observed with Mars Exploration Rovers
Reduced weathering rates due to the lack of liquid water and significantly greater typical surface ages should result in a higher density of meteorites on the surface of Mars compared to Earth. Several meteorites were identified among the rocks investigated during Opportunity's traverse across the sandy Meridiani plains. Heat Shield Rock is a IAB iron meteorite and has been officially...
Authors
C. Schroder, D.S. Rodionov, T.J. McCoy, B.L. Jolliff, Ralf Gellert, L.R. Nittler, W. H. Farrand, J. R. Johnson, S. W. Ruff, James W. Ashley, D. W. Mittlefehldt, Kenneth E. Herkenhoff, I. Fleischer, A. F. C. Haldemann, G. Klingelhofer, D. W. Ming, R.V. Morris, P.A. de Souza, S. W. Squyres, C. Weitz, A. S. Yen, J. Zipfel, T. Economou
Landslide hazard mitigation in North America Landslide hazard mitigation in North America
Active landslides throughout the states and territories of the United States result in extensive property loss and 25-50 deaths per year. The U.S. Geological Survey (USGS) has a long history of detailed examination of landslides since the work of Howe (1909) in the San Juan Mountains of Colorado. In the last four decades, landslide inventory maps and landslide hazard maps have depicted...
Authors
G. F. Wieczorek, P.P. Leahy
Iron isotope fractionation during magmatic differentiation in Kilauea Iki lava lake Iron isotope fractionation during magmatic differentiation in Kilauea Iki lava lake
Magmatic differentiation helps produce the chemical and petrographic diversity of terrestrial rocks. The extent to which magmatic differentiation fractionates nonradiogenic isotopes is uncertain for some elements. We report analyses of iron isotopes in basalts from Kilauea Iki lava lake, Hawaii. The iron isotopic compositions (56Fe/54Fe) of late-stagemeltveins are 0.2 permil (per...
Authors
F.-Z. Teng, N. Dauphas, Rosalind Tuthill Helz
4th EGU Alexander von Humboldt conference - the Andes: challenge for geosciences 4th EGU Alexander von Humboldt conference - the Andes: challenge for geosciences
No abstract available.
Authors
P. Fabian, R. Garreau, Christoph Schneider, Robert I. Tilling
Using amphibole phenocrysts to track vapor transfer during magma crystallization and transport: An example from Mount St. Helens, Washington Using amphibole phenocrysts to track vapor transfer during magma crystallization and transport: An example from Mount St. Helens, Washington
In order to evaluate and further constrain models for volatile movement and vapor enrichment of magma stored at shallow levels, amphibole phenocrysts from 2004–2005 Mount St. Helens dacite were analyzed for major and selected trace elements (Li, Cu, Zn, Mn, and REE) and Li isotopes. Several recent studies have examined fluid-mobile trace element abundances in phencryst phases and melt...
Authors
M.C. Rowe, A.J.R. Kent, C.R. Thornber