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National Earthquake Information Center systems overview and integration National Earthquake Information Center systems overview and integration

Overview The primary mission of the U.S. Geological Survey (USGS) National Earthquake Information Center (NEIC) is comprehensive global earthquake monitoring (M4.5 or larger) and complete seismic monitoring of the United States for all significant earthquakes (M3.0 or larger or felt). In recent years, the NEIC has assumed a more prominent role in local and regional seismic monitoring...
Authors
Michelle R. Guy, John Patton, Jeremy Fee, Mike Hearne, Eric Martinez, D. Ketchum, Charles Worden, Vince Quitoriano, Edward Hunter, Gregory Smoczyk, Stan Schwarz

The Boulder magnetic observatory The Boulder magnetic observatory

The Boulder magnetic observatory has, since 1963, been operated by the Geomagnetism Program of the U.S. Geological Survey in accordance with Bureau and national priorities. Data from the observatory are used for a wide variety of scientific purposes, both pure and applied. The observatory also supports developmental projects within the Geomagnetism Program and collaborative projects with...
Authors
Jeffrey Love, Carol Finn, Kolby L. Pedrie, Cletus Blum

Earthquake shaking hazard estimates and exposure changes in the conterminous United States Earthquake shaking hazard estimates and exposure changes in the conterminous United States

A large portion of the population of the United States lives in areas vulnerable to earthquake hazards. This investigation aims to quantify population and infrastructure exposure within the conterminous U.S. that are subjected to varying levels of earthquake ground motions by systematically analyzing the last four cycles of the U.S. Geological Survey's (USGS) National Seismic Hazard...
Authors
Kishor S. Jaiswal, Mark Petersen, Kenneth Rukstales, William Leith

Earthquake forewarning in the Cascadia region Earthquake forewarning in the Cascadia region

This report, prepared for the National Earthquake Prediction Evaluation Council (NEPEC), is intended as a step toward improving communications about earthquake hazards between information providers and users who coordinate emergency-response activities in the Cascadia region of the Pacific Northwest. NEPEC charged a subcommittee of scientists with writing this report about forewarnings...
Authors
Joan Gomberg, Brian Atwater, Nicholas Beeler, Paul Bodin, Earl Davis, Arthur Frankel, Gavin Hayes, Laura McConnell, Tim Melbourne, David Oppenheimer, John Parrish, Evelyn Roeloffs, Gary Rogers, Brian Sherrod, John Vidale, Timothy J. Walsh, Craig Weaver, Paul Whitmore

Estimating rates of debris flow entrainment from ground vibrations Estimating rates of debris flow entrainment from ground vibrations

Debris flows generate seismic waves as they travel downslope and can become more dangerous as they entrain sediment along their path. We present field observations that show a systematic relation between the magnitude of seismic waves and the amount of erodible sediment beneath the flow. Specifically, we observe that a debris flow traveling along a channel filled initially with sediment...
Authors
Jason Kean, Jeffrey Coe, V. Coviello, Joel Smith, S.W. McCoy, M. Arattano

Stratigraphy and structural development of the southwest Isla Tiburón marine basin: Implications for latest Miocene tectonic opening and flooding of the northern Gulf of California Stratigraphy and structural development of the southwest Isla Tiburón marine basin: Implications for latest Miocene tectonic opening and flooding of the northern Gulf of California

Accurate information on the timing of earliest marine incursion into the Gulf of California (northwestern México) is critical for paleogeographic models and for understanding the spatial and temporal evolution of strain accommodation across the obliquely divergent Pacific-North America plate boundary. Marine strata exposed on southwest Isla Tiburón (SWIT) have been cited as evidence for...
Authors
Scott Bennett, Michael Oskin, Rebecca Dorsey, Alexander Iriondo, Michael Kunk

Crustal deformation in the New Madrid seismic zone and the role of postseismic processes Crustal deformation in the New Madrid seismic zone and the role of postseismic processes

Global Navigation Satellite System data across the New Madrid seismic zone (NMSZ) in the central United States over the period from 2000 through 2014 are analyzed and modeled with several deformation mechanisms including the following: (1) creep on subsurface dislocations, (2) postseismic frictional afterslip and viscoelastic relaxation from the 1811–1812 and 1450 earthquakes in the NMSZ...
Authors
Oliver Boyd, Jr Robert Smalley, Yuehua Zeng

Evaluating the importance of characterizing soil structure and horizons in parameterizing a hydrologic process model Evaluating the importance of characterizing soil structure and horizons in parameterizing a hydrologic process model

Incorporating the influence of soil structure and horizons into parameterizations of distributed surface water/groundwater models remains a challenge. Often, only a single soil unit is employed, and soil-hydraulic properties are assigned based on textural classification, without evaluating the potential impact of these simplifications. This study uses a distributed physics-based model to...
Authors
Benjamin Mirus

Assessment of existing and potential landslide hazards resulting from the April 25, 2015 Gorkha, Nepal earthquake sequence Assessment of existing and potential landslide hazards resulting from the April 25, 2015 Gorkha, Nepal earthquake sequence

Introduction On April 25, 2015, a large (M7.8) earthquake shook much of central Nepal and was followed by a series of M>6 aftershocks, including a M7.3 event on May 12, 2015. This earthquake and aftershocks, referred to as the “Gorkha earthquake sequence,” caused thousands of fatalities, damaged and destroyed entire villages, and displaced millions of residents. The earthquakes also...
Authors
Brian D. Collins, Randall Jibson

On the lognormality of historical magnetic-storm intensity statistics: Implications for extreme-event probabilities On the lognormality of historical magnetic-storm intensity statistics: Implications for extreme-event probabilities

An examination is made of the hypothesis that the statistics of magnetic storm maximum intensities are the realization of a lognormal stochastic process. Weighted least squares and maximum likelihood methods are used to fit lognormal functions to −Dst storm time maxima for years 1957–2012; bootstrap analysis is used to established confidence limits on forecasts. Both methods provide fits...
Authors
Jeffrey Love, E. Rigler, Antti Pulkkinen, Pete Riley

Hundreds of earthquakes per day: The 2014 Guthrie, Oklahoma, Earthquake Sequence Hundreds of earthquakes per day: The 2014 Guthrie, Oklahoma, Earthquake Sequence

A remarkable increase in seismic activity in Oklahoma since 2009 has been shown to correlate closely with enhanced hydrocarbon extraction and associated wastewater disposal; 99% of this recent Oklahoma earthquake activity has occurred within 15 km of a call II injection well (Ellsworth, 2013). In response to this increase in seismic activity, the U.S. Geological Survey (USGS) partnered...
Authors
Harley Benz, Nicole McMahon, R Aster, Daniel McNamara, David Harris

Aftershock collapse vulnerability assessment of reinforced concrete frame structures Aftershock collapse vulnerability assessment of reinforced concrete frame structures

In a seismically active region, structures may be subjected to multiple earthquakes, due to mainshock–aftershock phenomena or other sequences, leaving no time for repair or retrofit between the events. This study quantifies the aftershock vulnerability of four modern ductile reinforced concrete (RC) framed buildings in California by conducting incremental dynamic analysis of nonlinear...
Authors
Meera Raghunandan, Abbie Liel, Nico Luco
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