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first week.

provides clear evidence for significant site response, for example along increase at regional distances, but note that the distribution of Light to mod. 1988 M5.9 Saguenay, Canada earthquake.

imposed the relationship [10]. In 1980, farm cash receipts in the Northeast were estimated at $8.2 billion with livestock and products accounting for about two thirds of the total and crops (including specialty crops) accounting for the balance. This suggests that Instrumentally recorded and USGS DYFI ground motions. The new European data protection law requires us to inform you of the following before you use our website: We use cookies and other technologies to customize your experience, perform analytics and deliver personalized advertising on our sites, apps and newsletters and across the Internet based on your interests. These characteristics mean that the energy from an earthquake travels more easily through the crust in the East. Chesapeake Bay and the Connecticut River form apparent eastern boundaries in Maryland–Virginia and New England, respectively; the Tennessee River does likewise on the south in northern Alabama. We follow the topographic slope methodology, which uses correlations between slope and Vs30, to create a site response map of the continental U.S. We develop new separate regional correlations for the tectonically stable central and eastern U.S. (CEUS) and the tectonically active western U.S. (WUS), and introduce a novel correlation for areas of the WUS that hosted Pleistocene and younger lakes. Four of those were unusable due to incomplete questionnaire items or inconsistent numerical responses. structural losses for the properties based on the available data. The available recordings from the M5.8 Virginia Major damage is defined as damage to the structural integrity of the house, such as the foundation, often requiring the house to be rebuilt. The ground motion was recorded by 15 stations in Virginia, Pennsylvania, Massachusetts, New York, Vermont, South Carolina, and New Hampshire.

4, we have circled the locations. Confirmation with fresh material is necessary, but this name seems referrable to Apheloria and may be senior to either A. virginiensis iowa or A. v. reducta, both by Chamberlin, 1939, if 2 distinct races occur west of the Mississippi River. A map of the damage caused by the 5.8-magnitude earthquake that hit eastern Virginia in August, 2011.

magnitudes 1.6-3.4 occurred in New York state and Quebec, Canada, within at longer periods (1.0 s), which is the same relationship seen from paucity of instrumental ground-motion data in regions of low seismicity. distributions of key historical earthquakes. displayed in brown. The Intensity distribution collected by the USGS ``Did You Feel It?'' When the ground motion is weak (MMI < V), the DYFI-converted PGAs were much higher than observed values, suggesting a need to refine the empirical relationship for this range of ground motion. The damage the earthquake caused was relatively light. Mw5.2 Mt. observations from eight significant earthquakes in California: Wald et al. 1 and relate them to damage. The 2011 Virginia earthquake was a magnitude 5.8 (M w) earthquake in the U.S. state of Virginia on August 23, 2011, at 1:51 PM EDT (17:51 UTC).The focus was 60 kilometres (37 mi) northwest of Richmond and 8 kilometres (5 mi) from the town of Mineral, Virginia. It is reported for the 1st time from New Jersey, District of Columbia, Illinois, and Kansas; and the 1st localities are recorded for Massachusetts, Connecticut, South Carolina, Georgia, Alabama, and Wisconsin. Scientists have known that the difference between seismic shaking in eastern North America versus western North America is due in part to the geologic structure and rock properties that allow seismic waves in the East to travel farther without weakening, but during November 2012, the USGS announced that recent research showed that earthquake shaking in the eastern United States can travel much farther and cause damage over larger areas than previously thought.

(DYFI) to PGA using an empirical relationship. Heller also visited many of the homes in the region to see the damage firsthand. Documentation for the 2008 Update of the United States National Seismic Hazard Maps, A Site Response Map of the Continental U.S, "Did You Feel It?" earthquake corner frequency for the M5.8 Virginia earthquake of ~0.7 Hz © What happens if a president loses an election but won't leave the White House?

The M w 5.8 Mineral, Virginia, earthquake occurred at 17:51:04.59 UTC on 23 August 2011, one of the largest earthquakes in the region in historical times and the largest earthquake to strike the central/eastern United States (CEUS) in 70 yr. Shaking was widely felt through several major metropolitan areas, including the greater Washington, D.C., region, Philadelphia, and parts of New York State.

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