Publications
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Liquefaction hazard for the region of Evansville, Indiana Liquefaction hazard for the region of Evansville, Indiana
We calculated liquefaction potential index for a grid of sites in the Evansville, Indiana area for two scenario earthquakes-a magnitude 7.7 in the New Madrid seismic zone and a M6.8 in the Wabash Valley seismic zone. For the latter event, peak ground accelerations range from 0.13 gravity to 0.81 gravity, sufficiently high to be of concern for liquefaction. Recently acquired cone...
Authors
Jennifer S. Haase, Yoon S. Choi, Robert L. Nowack, Chris H. Cramer, Oliver S. Boyd, Robert A. Bauer
A reevaluation of the Munson-Nygren-Retriever submarine landslide complex, Georges bank lower slope, western north Atlantic A reevaluation of the Munson-Nygren-Retriever submarine landslide complex, Georges bank lower slope, western north Atlantic
The Munson-Nygren-Retriever (MNR) landslide complex is a series of distinct submarine landslides located between Nygren and Powell canyons on the Georges Bank lower slope. These landslides were first imaged in 1978 using widely-spaced seismic reflection profiles and were further investigated using continuous coverage GLORIA sidescan imagery collected over the landslide complex in 1987...
Authors
Jason D. Chaytor, David C. Twichell, Uri S. ten Brink
Human casualties in earthquakes: Modelling and mitigation Human casualties in earthquakes: Modelling and mitigation
Earthquake risk modelling is needed for the planning of post-event emergency operations, for the development of insurance schemes, for the planning of mitigation measures in the existing building stock, and for the development of appropriate building regulations; in all of these applications estimates of casualty numbers are essential. But there are many questions about casualty...
Authors
R.J.S. Spence, E.K.M. So
Map of debris flows caused by rainfall during 1996 in parts of the Reedsport and Deer Head Point quadrangles, Douglas County, southern Coast Range, Oregon Map of debris flows caused by rainfall during 1996 in parts of the Reedsport and Deer Head Point quadrangles, Douglas County, southern Coast Range, Oregon
This 1:12,000-scale map shows an inventory of debris flows caused by rainfall during 1996 in a 94.4 km2 area in the southern Coast Range of Oregon. This map and associated digital data are part of a larger U.S. Geological Survey study of debris flows in the southern Coast Range. Available evidence indicates that the flows were triggered by a rain storm that occurred between November 17...
Authors
Jeffrey A. Coe, John A. Michael, Marianela Mercado Burgos
Direction of unsaturated flow in a homogeneous and isotropic hillslope Direction of unsaturated flow in a homogeneous and isotropic hillslope
The distribution of soil moisture in a homogeneous and isotropic hillslope is a transient, variably saturated physical process controlled by rainfall characteristics, hillslope geometry, and the hydrological properties of the hillslope materials. The major driving mechanisms for moisture movement are gravity and gradients in matric potential. The latter is solely controlled by gradients...
Authors
Ning Lu, Basak Sener Kaya, Jonathan W. Godt
Developing seismogenic source models based on geologic fault data Developing seismogenic source models based on geologic fault data
Calculating seismic hazard usually requires input that includes seismicity associated with known faults, historical earthquake catalogs, geodesy, and models of ground shaking. This paper will address the input generally derived from geologic studies that augment the short historical catalog to predict ground shaking at time scales of tens, hundreds, or thousands of years (e.g., SSHAC...
Authors
Kathleen M. Haller, Roberto Basili
Comparison of main-shock and aftershock fragility curves developed for New Zealand and US buildings Comparison of main-shock and aftershock fragility curves developed for New Zealand and US buildings
Seismic risk assessment involves the development of fragility functions to express the relationship between ground motion intensity and damage potential. In evaluating the risk associated with the building inventory in a region, it is essential to capture 'actual' characteristics of the buildings and group them so that 'generic building types' can be generated for further analysis of...
Authors
S.R. Uma, H. Ryu, N. Luco, A.B. Liel, M. Raghunandan
Coastal subsidence in Oregon, USA during the giant Cascadia earthquake of AD 1700 Coastal subsidence in Oregon, USA during the giant Cascadia earthquake of AD 1700
Quantitative estimates of land-level change during the giant AD 1700 Cascadia earthquake along the Oregon coast are inferred from relative sea-level changes reconstructed from fossil foraminiferal assemblages preserved within the stratigraphic record. A transfer function, based upon a regional training set of modern sediment samples from Oregon estuaries, is calibrated to fossil...
Authors
A. D. Hawkes, B. P. Horton, A.R. Nelson, C. H. Vane, Y. Sawai
Improved earthquake monitoring in the central and eastern United States in support of seismic assessments for critical facilities Improved earthquake monitoring in the central and eastern United States in support of seismic assessments for critical facilities
Evaluation of seismic monitoring capabilities in the central and eastern United States for critical facilities - including nuclear powerplants - focused on specific improvements to understand better the seismic hazards in the region. The report is not an assessment of seismic safety at nuclear plants. To accomplish the evaluation and to provide suggestions for improvements using funding...
Authors
William S. Leith, Harley M. Benz, Robert B. Herrmann
Albuquerque Seismological Laboratory--50 years of global seismology Albuquerque Seismological Laboratory--50 years of global seismology
The U.S. Geological Survey Albuquerque Seismological Laboratory is about 15 miles southeast of Albuquerque on the Pueblo of Isleta, adjacent to Kirtland Air Force Base. The Albuquerque Seismological Laboratory supports the Global Seismographic Network Program and the Advanced National Seismic System through the installation, operation, and maintenance of seismic stations around the world...
Authors
C. R. Hutt, Jon Peterson, Lind Gee, John Derr, Adam Ringler, David Wilson
Earthquakes in Mississippi and vicinity 1811-2010 Earthquakes in Mississippi and vicinity 1811-2010
This map summarizes two centuries of earthquake activity in Mississippi. Work on the Mississippi map was done in collaboration with the Mississippi Department of Environmental Quality, Office of Geology. The earthquake data plotted on the map are from several sources: the Mississippi Department of Environmental Quality, the Center for Earthquake Research and Information, the National...
Authors
Richard L. Dart, Michael B. E. Bograd
Earthquakes in Arkansas and vicinity 1699-2010 Earthquakes in Arkansas and vicinity 1699-2010
This map summarizes approximately 300 years of earthquake activity in Arkansas. It is one in a series of similar State earthquake history maps. Work on the Arkansas map was done in collaboration with the Arkansas Geological Survey. The earthquake data plotted on the map are from several sources: the Arkansas Geological Survey, the Center for Earthquake Research and Information, the...
Authors
Richard L. Dart, Scott M. Ausbrooks