Publications
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Unified facilities criteria 3-301-01: structural engineering Unified facilities criteria 3-301-01: structural engineering
This Unified Facility Criteria (UFC) provides requirements for structures designed and constructed for the Department of Defense (DoD). These technical requirements are based on the 2012 International Building Code (IBC 2012), as modified by UFC 1-200- 01. This information shall be used by structural engineers to develop design calculations, specifications, plans, and design-build...
Authors
Sean M. McGowan, Sanaz Rezaeian, Nicolas Luco
Geodesy- and geology-based slip-rate models for the Western United States (excluding California) national seismic hazard maps Geodesy- and geology-based slip-rate models for the Western United States (excluding California) national seismic hazard maps
The 2014 National Seismic Hazard Maps for the conterminous United States incorporate additional uncertainty in fault slip-rate parameter that controls the earthquake-activity rates than was applied in previous versions of the hazard maps. This additional uncertainty is accounted for by new geodesy- and geology-based slip-rate models for the Western United States. Models that were...
Authors
Mark D. Petersen, Yuehua Zeng, Kathleen M. Haller, Robert McCaffrey, William C. Hammond, Peter Bird, Morgan Moschetti, Zhengkang Shen, Jayne Bormann, Wayne Thatcher
Evaluating a slope-stability model for shallow rain-induced landslides using gage and satellite data Evaluating a slope-stability model for shallow rain-induced landslides using gage and satellite data
Improving prediction of landslide early warning systems requires accurate estimation of the conditions that trigger slope failures. This study tested a slope-stability model for shallow rainfall-induced landslides by utilizing rainfall information from gauge and satellite records. We used the TRIGRS model (Transient Rainfall Infiltration and Grid-based Regional Slope-stability analysis)...
Authors
S. Yatheendradas, D. Kirschbaum, Rex L. Baum, Jonathan W. Godt
Characterizing the primary material sources and dominant erosional processes for post-fire debris-flow initiation in a headwater basin using multi-temporal terrestrial laser scanning data Characterizing the primary material sources and dominant erosional processes for post-fire debris-flow initiation in a headwater basin using multi-temporal terrestrial laser scanning data
Wildfire dramatically alters the hydrologic response of a watershed such that even modest rainstorms can produce hazardous debris flows. Relative to shallow landslides, the primary sources of material and dominant erosional processes that contribute to post-fire debris-flow initiation are poorly constrained. Improving our understanding of how and where material is eroded from a watershed...
Authors
Dennis M. Staley, Thad A. Waslewicz, Jason W. Kean
Time causal operational estimation of electric fields induced in the Earth's lithosphere during magnetic storms Time causal operational estimation of electric fields induced in the Earth's lithosphere during magnetic storms
In support of projects for monitoring geomagnetic hazards for electric power grids, we develop a simple mathematical formalism, consistent with the time causality of deterministic physics, for estimating electric fields that are induced in the Earth's lithosphere during magnetic storms. For an idealized model of the lithosphere, an infinite half‐space having uniform electrical...
Authors
Jeffrey J. Love, Andrei Swidinsky
Variability in wood-frame building damage using broad-band synthetic ground motions: a comparative numerical study with recorded motions Variability in wood-frame building damage using broad-band synthetic ground motions: a comparative numerical study with recorded motions
Earthquake damage to light-frame wood buildings is a major concern for North America because of the volume of this construction type. In order to estimate wood building damage using synthetic ground motions, we need to verify the ability of synthetically generated ground motions to simulate realistic damage for this structure type. Through a calibrated damage potential indicator, four...
Authors
Shiling Pei, John W. van de Lindt, Stephen H. Hartzell, Nicolas Luco
A brief test of the Hewlett-Packard MEMS seismic accelerometer A brief test of the Hewlett-Packard MEMS seismic accelerometer
Testing was performed on a prototype of Hewlett-Packard (HP) Micro-Electro-Mechanical Systems (MEMS) seismic accelerometer at the U.S. Geological Survey’s Albuquerque Seismological Laboratory. This prototype was built using discrete electronic components. The self-noise level was measured during low seismic background conditions and found to be 9.8 ng/√Hz at periods below 0.2 s...
Authors
Brian D. Homeijer, Donald J. Milligan, Charles R. Hutt
Uplift and subsidence reveal a nonpersistent megathrust rupture boundary (Sitkinak Island, Alaska) Uplift and subsidence reveal a nonpersistent megathrust rupture boundary (Sitkinak Island, Alaska)
We report stratigraphic evidence of land-level change and tsunami inundation along the Alaska-Aleutian megathrust during prehistoric and historical earthquakes west of Kodiak Island. On Sitkinak Island, cores and tidal outcrops fringing a lagoon reveal five sharp lithologic contacts that record coseismic land-level change. Radiocarbon dates, 137Cs profiles, CT scans, and microfossil...
Authors
Richard W. Briggs, Simon E. Engelhart, Alan R. Nelson, Tina Dura, Andrew C. Kemp, Peter J. Haeussler, D. Reide Corbett, Stephen J. Angster, Lee-Ann Bradley
Preliminary interpretation of pre-2014 landslide deposits in the vicinity of Oso, Washington Preliminary interpretation of pre-2014 landslide deposits in the vicinity of Oso, Washington
High-resolution topographic surveys allow fairly precise mapping of landslide deposits and their relative ages. Relative ages are determined by cross-cutting relations and the amount of smoothing—more smoothed slide deposits are older—of these deposits. The Tulalip Tribes, in partnership with the Puget Sound Lidar Consortium, acquired a high-resolution lidar (light detection and ranging)...
Authors
Ralph A. Haugerud
By
Geology, Energy, and Minerals Mission Area, Natural Hazards Mission Area, Energy Resources Program, Groundwater and Streamflow Information Program, Landslide Hazards Program, Mineral Resources Program, National Laboratories Program, Science and Decisions Center, Geologic Hazards Science Center, Geology, Minerals, Energy, and Geophysics Science Center
Comparison of smoothing methods for the development of a smoothed seismicity model for Alaska and the implications for seismic hazard Comparison of smoothing methods for the development of a smoothed seismicity model for Alaska and the implications for seismic hazard
In anticipation of the update of the Alaska seismic hazard maps (ASHMs) by the U. S. Geological Survey, we report progress on the comparison of smoothed seismicity models developed using fixed and adaptive smoothing algorithms, and investigate the sensitivity of seismic hazard to the models. While fault-based sources, such as those for great earthquakes in the Alaska-Aleutian subduction...
Authors
Morgan P. Moschetti, Charles S. Mueller, Oliver S. Boyd, Mark D. Petersen
Seismological analyses of the 2010 March 11, Pichilemu, Chile Mw 7.0 and Mw 6.9 coastal intraplate earthquakes Seismological analyses of the 2010 March 11, Pichilemu, Chile Mw 7.0 and Mw 6.9 coastal intraplate earthquakes
On 2010 March 11, a sequence of large, shallow continental crust earthquakes shook central Chile. Two normal faulting events with magnitudes around Mw 7.0 and Mw 6.9 occurred just 15 min apart, located near the town of Pichilemu. These kinds of large intraplate, inland crustal earthquakes are rare above the Chilean subduction zone, and it is important to better understand their...
Authors
Javier A. Ruiz, Gavin P. Hayes, Daniel Carrizo, Hiroo Kanamori, Anne Socquet, Diana Comte
Breaking the oceanic lithosphere of a subducting slab: the 2013 Khash, Iran earthquake Breaking the oceanic lithosphere of a subducting slab: the 2013 Khash, Iran earthquake
[1] Large intermediate depth, intraslab normal faulting earthquakes are a common, dangerous, but poorly understood phenomenon in subduction zones owing to a paucity of near field geophysical observations. Seismological and high quality geodetic observations of the 2013 Mw7.7 Khash, Iran earthquake reveal that at least half of the oceanic lithosphere, including the mantle and entire crust...
Authors
William D. Barnhart, Gavin P. Hayes, S. Samsonov, E. Fielding, L. Seidman