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From field data to volumes: Constraining uncertainties in pyroclastic eruption parameters From field data to volumes: Constraining uncertainties in pyroclastic eruption parameters

In this study, we aim to understand the variability in eruption volume estimates derived from field studies of pyroclastic deposits. We distributed paper maps of the 1959 Kīlauea Iki tephra to 101 volcanologists worldwide, who produced hand-drawn isopachs. Across the returned maps, uncertainty in isopach areas is 7 % across the well-sampled deposit but increases to over 30 % for isopachs...
Authors
Malin Klawonn, Bruce F. Houghton, Don Swanson, Sarah A. Fagents, Paul Wessel, Cecily J. Wolfe

The earthquake cycle in the San Francisco Bay region: A.D. 1600–2012 The earthquake cycle in the San Francisco Bay region: A.D. 1600–2012

Stress changes produced by the 1906 San Francisco earthquake had a profound effect on the seismicity of the San Francisco Bay region (SFBR), dramatically reducing it in the twentieth century. Whether the SFBR is still within or has emerged from this seismic quiescence is an issue of debate with implications for earthquake mechanics and seismic hazards. Historically, the SFBR has not...
Authors
David P. Schwartz, James J. Lienkaemper, Suzanne Hecker, Keith I. Kelson, Thomas E. Fumal, John N. Baldwin, Gordon G. Seitz, Tina Niemi

Analysis of induced seismicity in geothermal reservoirs – An overview Analysis of induced seismicity in geothermal reservoirs – An overview

In this overview we report results of analysing induced seismicity in geothermal reservoirs in various tectonic settings within the framework of the European Geothermal Engineering Integrating Mitigation of Induced Seismicity in Reservoirs (GEISER) project. In the reconnaissance phase of a field, the subsurface fault mapping, in situ stress and the seismic network are of primary interest...
Authors
Arno Zang, Volker Oye, Philippe Jousset, Nicholas Deichmann, Roland Gritto, Arthur F. McGarr, Ernest Majer, David Bruhn

Aftershock risks such as those demonstrated by the recent events in New Zealand and Japan Aftershock risks such as those demonstrated by the recent events in New Zealand and Japan

Recent earthquakes in New Zealand and Japan show that it is important to consider the spatial and temporal distribution of aftershocks following large magnitude events since the probability of high intensity ground motions from aftershocks, which are capable of causing significant societal impact, can be considerable. This is due to the fact that a mainshock will have many aftershocks...
Authors
Nilesh Shome, Nico Luco, Matt Gerstenberger, Oliver S. Boyd, Edward H. Field, Abbie Liel, John W. van de Lindt

Rethinking turbidite paleoseismology along the Cascadia subduction zone Rethinking turbidite paleoseismology along the Cascadia subduction zone

A stratigraphic synthesis of dozens of deep-sea cores, most of them overlooked in recent decades, provides new insights into deep-sea turbidites as guides to earthquake and tsunami hazards along the Cascadia subduction zone, which extends 1100 km along the Pacific coast of North America. The synthesis shows greater variability in Holocene stratigraphy and facies off the Washington coast...
Authors
Brian F. Atwater, Bobb Carson, Gary B. Griggs, H. Paul Johnson, Marie Salmi

Modified expression for bulb-tracer depletion—Effect on argon dating standards Modified expression for bulb-tracer depletion—Effect on argon dating standards

40Ar/39Ar geochronology depends critically on well-calibrated standards, often traceable to first-principles K-Ar age calibrations using bulb-tracer systems. Tracer systems also provide precise standards for noble-gas studies and interlaboratory calibration. The exponential expression long used for calculating isotope tracer concentrations in K-Ar age dating and calibration of 40Ar/39Ar...
Authors
Robert J. Fleck, Andrew T. Calvert

Frequency-dependent seismic attenuation in the eastern United States as observed from the 2011 central Virginia earthquake and aftershock sequence Frequency-dependent seismic attenuation in the eastern United States as observed from the 2011 central Virginia earthquake and aftershock sequence

Ground shaking due to earthquakes in the eastern United States (EUS) is felt at significantly greater distances than in the western United States (WUS) and for some earthquakes it has been shown to display a strong preferential direction. Shaking intensity variation can be due to propagation path effects, source directivity, and/or site amplification. In this paper, we use S and Lg waves...
Authors
Daniel E. McNamara, Lind Gee, Harley M. Benz, Martin Chapman

Relationship between the Cascadia fore-arc mantle wedge, nonvolcanic tremor, and the downdip limit of seismogenic rupture Relationship between the Cascadia fore-arc mantle wedge, nonvolcanic tremor, and the downdip limit of seismogenic rupture

Great earthquakes anticipated on the Cascadia subduction fault can potentially rupture beyond the geodetically and thermally inferred locked zone to the depths of episodic tremor and slip (ETS) or to the even deeper fore-arc mantle corner (FMC). To evaluate these extreme rupture limits, we map the FMC from southern Vancouver Island to central Oregon by combining published seismic...
Authors
Patricia A. McCrory, Roy D. Hyndman, J. Luke Blair

Strong ground motions generated by earthquakes on creeping faults Strong ground motions generated by earthquakes on creeping faults

A tenet of earthquake science is that faults are locked in position until they abruptly slip during the sudden strain-relieving events that are earthquakes. Whereas it is expected that locked faults when they finally do slip will produce noticeable ground shaking, what is uncertain is how the ground shakes during earthquakes on creeping faults. Creeping faults are rare throughout much of...
Authors
Ruth A. Harris, Norman A. Abrahamson

Finite-fault slip model of the 2011 Mw 5.6 Prague, Oklahoma earthquake from regional waveforms Finite-fault slip model of the 2011 Mw 5.6 Prague, Oklahoma earthquake from regional waveforms

The slip model for the 2011 Mw 5.6 Prague, Oklahoma, earthquake is inferred using a linear least squares methodology. Waveforms of six aftershocks recorded at 21 regional stations are used as empirical Green's functions (EGFs). The solution indicates two large slip patches: one located around the hypocenter with a depth range of 3–5.5 km; the other located to the southwest of the...
Authors
Xiaodan Sun, Stephen H. Hartzell

The UCERF3 grand inversion: Solving for the long‐term rate of ruptures in a fault system The UCERF3 grand inversion: Solving for the long‐term rate of ruptures in a fault system

We present implementation details, testing, and results from a new inversion‐based methodology, known colloquially as the “grand inversion,” developed for the Uniform California Earthquake Rupture Forecast (UCERF3). We employ a parallel simulated annealing algorithm to solve for the long‐term rate of all ruptures that extend through the seismogenic thickness on major mapped faults in...
Authors
Morgan T. Page, Edward H. Field, Kevin Milner, Peter M. Powers

2010 Volcanic activity in Alaska, Kamchatka, and the Kurile Islands: Summary of events and response of the Alaska Volcano Observatory 2010 Volcanic activity in Alaska, Kamchatka, and the Kurile Islands: Summary of events and response of the Alaska Volcano Observatory

The Alaska Volcano Observatory (AVO) responded to eruptions, possible eruptions, volcanic unrest or suspected unrest at 12 volcanic centers in Alaska during 2010. The most notable volcanic activity consisted of intermittent ash emissions from long-active Cleveland volcano in the Aleutian Islands. AVO staff also participated in hazard communication regarding eruptions or unrest at seven...
Authors
Christina A. Neal, Julie Herrick, O.A. Girina, Marina Chibisova, Alexander Rybin, Robert G. McGimsey, Jim Dixon
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