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2016 one-year seismic hazard forecast for the Central and Eastern United States from induced and natural earthquakes 2016 one-year seismic hazard forecast for the Central and Eastern United States from induced and natural earthquakes

The U.S. Geological Survey (USGS) has produced a 1-year seismic hazard forecast for 2016 for the Central and Eastern United States (CEUS) that includes contributions from both induced and natural earthquakes. The model assumes that earthquake rates calculated from several different time windows will remain relatively stationary and can be used to forecast earthquake hazard and damage...
Authors
Mark Petersen, Charles S. Mueller, Morgan Moschetti, Susan Hoover, Andrea Llenos, William Ellsworth, Andrew Michael, Justin Rubinstein, Arthur McGarr, Kenneth Rukstales

Illuminating wildfire erosion and deposition patterns with repeat terrestrial lidar Illuminating wildfire erosion and deposition patterns with repeat terrestrial lidar

Erosion following a wildfire is much greater than background erosion in forests because of wildfire-induced changes to soil erodibility and water infiltration. While many previous studies have documented post-wildfire erosion with point and small plot-scale measurements, the spatial distribution of post-fire erosion patterns at the watershed scale remains largely unexplored. In this...
Authors
Francis Rengers, G.E. Tucker, J. A. Moody, Brian Ebel

Uncertainty in Vs30-based site response Uncertainty in Vs30-based site response

Methods that account for site response range in complexity from simple linear categorical adjustment factors to sophisticated nonlinear constitutive models. Seismic‐hazard analysis usually relies on ground‐motion prediction equations (GMPEs); within this framework site response is modeled statistically with simplified site parameters that include the time‐averaged shear‐wave velocity to...
Authors
Eric Thompson, David Wald

High-resolution seismic reflection imaging of growth folding and shallow faults beneath the Southern Puget Lowland, Washington State High-resolution seismic reflection imaging of growth folding and shallow faults beneath the Southern Puget Lowland, Washington State

Marine seismic reflection data from southern Puget Sound, Washington, were collected to investigate the nature of shallow structures associated with the Tacoma fault zone and the Olympia structure. Growth folding and probable Holocene surface deformation were imaged within the Tacoma fault zone beneath Case and Carr Inlets. Shallow faults near potential field anomalies associated with...
Authors
Jackson K. Odum, William Stephenson, Thomas Pratt, Richard Blakely

Potential improvements in horizontal very broadband seismic data in the IRIS/USGS component of the Global Seismic Network Potential improvements in horizontal very broadband seismic data in the IRIS/USGS component of the Global Seismic Network

The Streckeisen STS‐1 has been the primary vault‐type seismometer used in the over‐150‐station Global Seismographic Network (GSN). This sensor has long been known for its outstanding vertical, very long‐period (e.g., >100  s period), and low‐noise performance, although the horizontal long‐period noise performance is less well known. The STS‐1 is a limited, important resource, because it...
Authors
Adam Ringler, J.M. Steim, T Zandt, Charles Hutt, David Wilson, Tyler Storm

Rock-avalanche dynamics revealed by large-scale field mapping and seismic signals at a highly mobile avalanche in the West Salt Creek valley, western Colorado Rock-avalanche dynamics revealed by large-scale field mapping and seismic signals at a highly mobile avalanche in the West Salt Creek valley, western Colorado

On 25 May 2014, a rain-on-snow–induced rock avalanche occurred in the West Salt Creek valley on the northern flank of Grand Mesa in western Colorado (United States). The avalanche mobilized from a preexisting rock slide in the Green River Formation and traveled 4.6 km down the confined valley, killing three people. The avalanche was rare for the contiguous United States because of its...
Authors
Jeffrey Coe, Rex Baum, Kate Allstadt, Bernard Kochevar, Robert Schmitt, Matthew Morgan, Jonathan White, Benjamin Stratton, Timothy Hayashi, Jason Kean

Weathering a Perfect Storm from Space Weathering a Perfect Storm from Space

Extreme space-weather events — intense solar and geomagnetic storms — have occurred in the past: most recently in 1859, 1921 and 1989. So scientists expect that, sooner or later, another extremely intense spaceweather event will strike Earth again. Such storms have the potential to cause widespread interference with and damage to technological systems. A National Academy of Sciences...
Authors
Jeffrey Love

A submarine landslide source for the devastating 1964 Chenega tsunami, southern Alaska A submarine landslide source for the devastating 1964 Chenega tsunami, southern Alaska

During the 1964 Great Alaska earthquake (Mw 9.2), several fjords, straits, and bays throughout southern Alaska experienced significant tsunami runup of localized, but unexplained origin. Dangerous Passage is a glacimarine fjord in western Prince William Sound, which experienced a tsunami that devastated the village of Chenega where 23 of 75 inhabitants were lost – the highest relative...
Authors
Daniel Brothers, Peter Haeussler, Lee Liberty, David Finlayson, Eric Geist, Keith A. Labay, Michael Byerly

Identifying long term empirical relationships between storm characteristics and episodic groundwater recharge Identifying long term empirical relationships between storm characteristics and episodic groundwater recharge

Shallow aquifers are an important source of water resources and provide base flow to streams; yet actual rates of groundwater recharge are difficult to estimate. While climate change is predicted to increase the frequency and magnitude of extreme precipitation events, the resulting impact on groundwater recharge remains poorly understood. We quantify empirical relations between...
Authors
Arik Tashie, Benjamin Mirus, Tamlin Pavelsky

Influence of slip-surface geometry on earth-flow deformation, Montaguto earth flow, southern Italy Influence of slip-surface geometry on earth-flow deformation, Montaguto earth flow, southern Italy

We investigated relations between slip-surface geometry and deformational structures and hydrologic features at the Montaguto earth flow in southern Italy between 1954 and 2010. We used 25 boreholes, 15 static cone-penetration tests, and 22 shallow-seismic profiles to define the geometry of basal- and lateral-slip surfaces; and 9 multitemporal maps to quantify the spatial and temporal...
Authors
L. Guerriero, Jeffrey Coe, P. Revellio, G. Grelle, F. Pinto, F. Guadagno

Earthquake ground motion Earthquake ground motion

Most of the effort in seismic design of buildings and other structures is focused on structural design. This chapter addresses another key aspect of the design process—characterization of earthquake ground motion into parameters for use in design. Section 3.1 describes the basis of the earthquake ground motion maps in the Provisions and in ASCE 7 (the Standard). Section 3.2 has examples...
Authors
Nico Luco, Charles Kircher, C. Crouse, Finley Charney, Curt Haselton, Jack Baker, Reid Zimmerman, John Hooper, William McVitty, Andy Taylor

Assessing the seismic risk potential of South America Assessing the seismic risk potential of South America

We present here a simplified approach to quantifying regional seismic risk. The seismic risk for a given region can be inferred in terms of average annual loss (AAL) that represents long-term value of earthquake losses in any one year caused from a long-term seismic hazard. The AAL are commonly measured in the form of earthquake shaking-induced deaths, direct economic impacts or indirect...
Authors
Kishor Jaiswal, Mark Petersen, Stephen Harmsen, Gregory Smoczyk
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