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modified Mercalli scale
The 28 October 2022 M w 3.8 Goesan Earthquake Sequence in Central Korea: Stress Drop, Aftershock Triggering, and Fault Interaction
Crowdsourcing Felt Reports Using the MyShake Smartphone App
New Methodology for Unbiased Ground‐Motion Intensity Conversion Equations
Macroseismic analysis and the determination of a focal mechanism of the 31 October 2019, KwaZulu-Natal earthquake in South Africa
Applications of Nonergodic Site Response Models to ShakeAlert Case Studies in the Los Angeles Area
Rupture Scenarios for the 3 June 1770 Haiti Earthquake
Education Initiatives to Support Earthquake Early Warning: A Retrospective and a Roadmap
Real‐Time Earthquake Detection and Alerting Behavior of PLUM Ground‐Motion‐Based Early Warning in the United States
The 8 April 1860 Jour de Pâques Earthquake Sequence in Southern Haiti
DeepShake: Shaking Intensity Prediction Using Deep Spatiotemporal RNNs for Earthquake Early Warning
A Methodology for Evaluating Component-Level Loss Predictions of the FEMA P-58 Seismic Performance Assessment Procedure
Seismic Performance of Ductile Steel Moment-Resisting Frames Subjected to Multiple Strong Ground Motions
Improved CENA Regression Relationships between Modified Mercalli Intensities and Ground‐Motion Parameters
Ground‐Motion Simulation for the 23 August 2011, Mineral, Virginia, Earthquake Using Physics‐Based and Stochastic Broadband Methods
Residential property damage in the epicentral area of the Mineral, Virginia, earthquake of 23 August 2011
The Mineral, Virginia (USA), earthquake of 23 August 2011 was an unusually strong seismic event in the eastern United States. It caused widespread structural damage to residential property near the epicenter. An analysis of residential property damage reports, in conjunction with visits to some damaged residences, reveals a 40 km 2 area of concentrated damage centered 11 km south of the town of Louisa. This area is west of the earthquake’s epicenter and may be in the immediate hanging wall of a northeast-striking, moderately southeast dipping causative fault suggested by seismic data. The degree of damage in this area is consistent with a maximum Modified Mercalli Intensity (MMI) of VIII. A surrounding area of ~550 km 2 reported damage that is consistent with an MMI intensity of VII. A statistical analysis of dwelling characteristics confirms that home age and condition were factors that influenced the frequency and severity of reported property damage. The median damage to homes constructed between 1900 and 1973, relative to assessed value, was approximately twice that of homes constructed after 1973 in Louisa County, and three times greater within areas of MMI intensity VI, VII, and VIII.