Publications
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Seismic hazard assessment for Guam and the Northern Mariana Islands Seismic hazard assessment for Guam and the Northern Mariana Islands
We present the results of a new probabilistic seismic hazard assessment for Guam and the Northern Mariana Islands. The Mariana island arc has formed in response to northwestward subduction of the Pacific plate beneath the Philippine Sea plate, and this process controls seismic activity in the region. Historical seismicity, the Mariana megathrust, and two crustal faults on Guam were...
Authors
Charles S. Mueller, Kathleen M. Haller, Nicholas Luco, Mark D. Petersen, Arthur D. Frankel
Stability of infinite slopes under transient partially saturated seepage conditions Stability of infinite slopes under transient partially saturated seepage conditions
Prediction of the location and timing of rainfall‐induced shallow landslides is desired by organizations responsible for hazard management and warnings. However, hydrologic and mechanical processes in the vadose zone complicate such predictions. Infiltrating rainfall must typically pass through an unsaturated layer before reaching the irregular and usually discontinuous shallow water...
Authors
Jonathan W. Godt, Başak Şener-Kaya, Ning Lu, Rex L. Baum
On the reported ionospheric precursor of the 1999 Hector Mine, California earthquake On the reported ionospheric precursor of the 1999 Hector Mine, California earthquake
Using Global Positioning System (GPS) data from sites near the 16 Oct. 1999 Hector Mine, California earthquake, Pulinets et al. (2007) identified anomalous changes in the ionospheric total electron content (TEC) starting one week prior to the earthquake. Pulinets (2007) suggested that precursory phenomena of this type could be useful for predicting earthquakes. On the other hand, and in...
Authors
Jeremy N. Thomas, Jeffrey J. Love, Attila Komjathy, Olga P. Verkhoglyadova, Mark Butala, Nicholas Rivera
GEM Basic Building Taxonomy (Version 1.0) GEM Basic Building Taxonomy (Version 1.0)
This report documents the development of Global Earthquake Model (GEM) Basic Building Taxonomy and it also provides version 1.0 of this Taxonomy for its immediate application within GEM Physical Risk projects. Criteria for development of the GEM Building Taxonomy required that the Taxonomy be relevant to seismic performance of different construction types; be comprehensive yet simple; be
Authors
S. Brzev, C. Scawthorn, A.W. Charleson, K. Jaiswal
Real-time monitoring of landslides Real-time monitoring of landslides
Landslides cause fatalities and property damage throughout the Nation. To reduce the impact from hazardous landslides, the U.S. Geological Survey develops and uses real-time and near-real-time landslide monitoring systems. Monitoring can detect when hillslopes are primed for sliding and can provide early indications of rapid, catastrophic movement. Continuous information from up-to-the...
Authors
Mark E. Reid, Richard G. LaHusen, Rex L. Baum, Jason W. Kean, William H. Schulz, Lynn M. Highland
Modified Mercalli Intensity for scenario earthquakes in Evansville, Indiana Modified Mercalli Intensity for scenario earthquakes in Evansville, Indiana
Evansville, Indiana, has experienced minor damage from earthquakes several times in the past 200 years. Because of this history and the fact that Evansville is close to the Wabash Valley and New Madrid seismic zones, there is concern about the hazards from earthquakes. Earthquakes currently cannot be predicted, but scientists can estimate how strongly the ground is likely to shake as a...
Authors
Chris Cramer, Jennifer Haase, Oliver Boyd
Understanding earthquake hazards in urban areas - Evansville Area Earthquake Hazards Mapping Project Understanding earthquake hazards in urban areas - Evansville Area Earthquake Hazards Mapping Project
The region surrounding Evansville, Indiana, has experienced minor damage from earthquakes several times in the past 200 years. Because of this history and the proximity of Evansville to the Wabash Valley and New Madrid seismic zones, there is concern among nearby communities about hazards from earthquakes. Earthquakes currently cannot be predicted, but scientists can estimate how...
Authors
Oliver S. Boyd
Spatial distribution of landslides triggered from the 2007 Niigata Chuetsu–Oki Japan Earthquake Spatial distribution of landslides triggered from the 2007 Niigata Chuetsu–Oki Japan Earthquake
Understanding the spatial distribution of earthquake-induced landslides from specific earthquakes provides an opportunity to recognize what to expect from future events. The July 16, 2007 Mw 6.6 (MJMA 6.8) Niigata Chuetsu–Oki Japan earthquake triggered hundreds of landslides in the area surrounding the coastal city of Kashiwazaki and provides one such opportunity to evaluate the impacts...
Authors
Brian D. Collins, Robert E. Kayen, Yasuo Tanaka
By
Geology, Energy, and Minerals Mission Area, Natural Hazards Mission Area, Energy Resources 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
Post-wildfire wind erosion in and around the Idaho National Laboratory Site Post-wildfire wind erosion in and around the Idaho National Laboratory Site
Wind erosion following large wildfires on and around the INL Site is a recurrent threat to human health and safety, DOE operations and trafficability, and ecological and hydrological condition of the INL Site and down-wind landscapes. Causes and consequences of wind erosion are mainly known from warm deserts (e.g., Southwest U.S.), dunefields, and croplands, and some but not all findings...
Authors
Matthew J. Germino
Post-earthquake building safety assessments for the Canterbury Earthquakes Post-earthquake building safety assessments for the Canterbury Earthquakes
This paper explores the post-earthquake building assessment program that was utilized in Christchurch, New Zealand following the Canterbury Sequence of earthquakes beginning with the Magnitude (Mw.) 7.1 Darfield event in September 2010. The aftershocks or triggered events, two of which exceeded Mw 6.0, continued with events in February and June 2011 causing the greatest amount of damage...
Authors
J. Marshall, J. Barnes, N. Gould, K. Jaiswal, B. Lizundia, David A. Swanson, F. Turner
Magnitude Estimates of M7.3-7.8 for the 1811-1812 New Madrid and M7.0 for the 1886 Charleston Earthquakes from a Monte Carlo Analysis of Mean MMIs Magnitude Estimates of M7.3-7.8 for the 1811-1812 New Madrid and M7.0 for the 1886 Charleston Earthquakes from a Monte Carlo Analysis of Mean MMIs
No abstract available
Authors
Chris H. Cramer, Oliver S. Boyd
Measuring the orthogonality error of coil systems Measuring the orthogonality error of coil systems
Recently, a simple method was proposed for the determination of pitch angle between two coil axes by means of a total field magnetometer. The method is applicable when the homogeneous volume in the centre of the coil system is large enough to accommodate the total field sensor. Orthogonality of calibration coil systems used for calibrating vector magnetometers can be attained by this...
Authors
B. Heilig, A. Csontos, K. Pajunpaa, Tim White, B. St. Louis, D. Calp