4.2 km from (1.2 miles), 2003-08-26 02:26:56 UTC 7.2 km from at 16:17 January 03, 2003 UTC, Location: Figure 2 shows the total collapse of Juarez Hospital in Mexico City, caused by the amplified ground motion during the earthquake of Sept. 19, 1985. 1980-07-12 23:59:54 UTC 3.1 magnitude, 0 km depth Central City, Kentucky, United States 3.1 magnitude earthquake 1980-07-12 23:59:54 UTC at 23:59 July 12, 1980 UTC 10.2 km from Mount Carmel Massac 9.2 km from 11.2 km from Epicenter at 37.63, -86.69 23.2 km from (7.2 miles), 1987-09-29 00:04:56 UTC Epicenter at 38.119, -86.438 at 19:41 January 29, 1990 UTC, Location: at 18:52 July 27, 1980 UTC, Location: (8.2 miles). Cloverport Wickliffe at 18:20 January 24, 1990 UTC, Location: Epicenter at 38.143, -83.878 Wilmore 8.2 km from Risk is defined by four parameters: a probability, level of severity, time period, and location. 12.2 km from (4.2 miles), 1999-07-06 09:29:00 UTC at 00:04 September 29, 1987 UTC, Location: Epicenter at 38.476, -87.847 Epicenter at 37.323, -87.259 Also, an earthquake measuring 5.2 on the Richter scale occurred in 1980 near Sharpsburg in Bath County and caused an estimated $3 million in damage; 269 homes and 37 businesses in nearby Maysville were damaged. This lack of data results in large uncertainties for the seismological parameters that are the basis for assessing seismic hazard and risk. (6.2 miles), 1987-06-10 23:48:54 UTC Many communities in Kentucky are set on soft soils, especially those along the Ohio and Mississippi River Valleys. 23.2 km from at 02:52 October 06, 2015 UTC, Location: 11.2 km from at 00:16 June 05, 1974 UTC, Location: 16.2 km from at 13:18 September 26, 1990 UTC, Location: The strongest earthquake ever felt in Kentucky was a 5.2 magnitude in 1980 in Bath County. Epicenter at 37.987, -87.78 Epicenter at 37.995, -84.922 at 22:56 January 07, 1973 UTC, Location: (14.2 miles), 2003-06-06 12:29:34 UTC (8.2 miles), 1987-06-10 23:48:54 UTC Epicenter at 38.133, -86.434 Lawrenceburg (7.2 miles), 2002-06-18 17:37:15 UTC (6.2 miles), 2020-02-27 06:05:58 UTC Lawrenceburg Kentucky is affected by several seismic zones: the New Madrid and Wabash Valley Seismic Zones the west and to the Eastern Tennessee Seismic Zone to the east (Fig. (9.2 miles), 1987-10-14 15:49:39 UTC The larger an earthquake's magnitude, the stronger the ground motion it generates. (7.2 miles), 2016-02-02 08:09:03 UTC Thus, earthquakes pose high seismic hazards and risk to the commonwealth of Kentucky. Calhoun Most damage during an earthquake is caused by ground motion (see Fig. 22.2 km from (4.2 miles), 2015-11-28 10:49:39 UTC Those communities are prone to ground-motion amplification. 1). Use this service to convert a delimited text file of coordinate values (guidelines given on the page) to a choice of 14 different coordinate values. The largest earthquake on record for Kentucky occurred on 07/27/1980, with a depth of 8.0 miles and a magnitude of … Strong ground motion can also trigger landslides —known as earthquake-induced landslides —in areas with steep slopes, such as eastern Kentucky. 8.2 km from Epicenter at 37.867, -84.74 High seismic hazard does not necessarily mean high seismic risk, and vice versa. (5.2 miles), 1980-03-23 21:38:15 UTC For example, earthquakes, hurricanes, tornadoes, and floods are natural hazards; whereas car crashes, chemical spills, train derailments, and terror attacks are manmade hazards. The geologic record suggests that the recurrence interval of earthquakes with magnitude of about 7.7 in the New Madrid Seismic Zone is about 500 years, and the historical record indicates the recurrence interval of Category 5 hurricanes is about 100 years in the Gulf Coast area. (6.2 miles), 2008-04-18 15:14:16 UTC 6.2 km from (10.2 miles), 1980-08-23 03:49:02 UTC Epicenter at 37.758, -84.663 Subscribe to ad-free EarthquakeTrack Plus for the best earthquake tracking experience plus additional features and subscriber-only perks. (8.2 miles), 1990-01-24 18:20:24 UTC The local geology and soil also play important roles in earthquake damage. Output includes the KY county and KY 1:24,000 quadrangle where the coordinate is located and links to map views. 1- 4). Owingsville 14.2 km from All files associated with this page are copyrighted © 1997 –, Induced Seismic Events in Kentucky Factsheet, More seismology-related publications at KGS, 504 Rose Street, 228 Mining and Mineral Resources Building, University of Kentucky, Lexington, KY 40506-0107. at 15:49 October 14, 1987 UTC, Location: (4.2 miles), 2012-04-18 06:16:35 UTC (6.2 miles), 2018-01-21 04:37:24 UTC 11.2 km from If the occurrences of earthquakes and hurricanes both follow a Poisson distribution, the risk posed by earthquakes in the New Madrid Seismic Zone can be estimated to be about a 10 percent probability of exceedance in 50 years for a magnitude 7.7 earthquake, a specific level of ground motion or MMI at a site, or total losses (life and money); the risk posed by Hurricane Katrina in the Gulf Coast area can be estimated to be about a 39 percent probability of exceedance in 50 years for a Category 5 hurricane, a specific level of flood or wind speed at a site, or total losses (life and money). 10.2 km from Epicenter at 38.476, -87.847 at 17:00 September 12, 2015 UTC, Location: Central City 2008-04-18 09:36:59 UTC (7.2 miles), 1980-07-27 18:52:21 UTC Lawrenceburg 10.2 km from Sumner The fundamental difference between PSHA and DSHA is in how the uncertainties are treated: either implicitly (PSHA) or explicitly (DSHA). at 09:29 July 06, 1999 UTC, Location: There are 77 earthquake incidents in Kentucky on record since 1931. 7.2 km from A commonly measured ground motion is peak ground acceleration (PGA), which is expressed as a percentage of the acceleration of gravity (g). Bardwell 6.2 km from An example might be a fatal car crash (severity) in every month (frequency) at a specific intersection. Epicenter at 37.63, -86.69 Bath County has the record for the largest and second-largest earthquakes in Kentucky history, according to Zhenming Wang, Ph.D., head of the geologic hazards section for the Kentucky Geological Survey at the University of Kentucky. The state averages 1 earthquakes per year. at 17:37 June 18, 2002 UTC, Location: Epicenter at 37.097, -88.724 Seismic risk depends not only on seismic hazard and exposure, but also on the models used to describe the occurrence of earthquakes. at 03:49 August 23, 1980 UTC, Location: Epicenter at 37.165, -89.577 Output is the same text file with the converted values and the KY county and KY 1:24,000 quadrangle where a coordinate is located. (6.2 miles). Original Story Monday afternoon a 3.6 magnitude earthquake hit near the Kentucky … (5.2 miles), 1990-01-29 19:41:47 UTC Massac Epicenter at 37.265, -86.988 Shelbyville Assessing seismic hazard and risk is difficult because of insufficient data, especially in the central and eastern United States, where the data on large earthquakes are very limited. Mount Vernon Mount Vernon 24.2 km from In general, hazard is a phenomenon that has potential to cause harm. at 01:40 November 24, 2017 UTC, Location: 11.2 km from Seismic hazard is commonly assessed either by probabilistic seismic hazard analysis or deterministic seismic hazard analysis. On the other hand, seismic risk could be high in some areas, such as Pakistan and Iran, because of high exposure, even though the hazard may be moderate. 12.2 km from Epicenter at 37.049, -88.793 Epicenter at 38.028, -84.819 Epicenter at 37.995, -84.841 Epicenter at 38.147, -85.071 12.2 km from Epicenter at 38.42, -84.412 at 02:45 August 20, 2015 UTC, Location: Owensboro at 06:05 February 27, 2020 UTC, Location: Paris Epicenter at 38.452, -87.886 Ground-motion amplification contributed to the heavy damage in Mexico City during the 1985 earthquake (see Fig. Sumner Subscribe to ad-free EarthquakeTrack Plus for the best earthquake tracking experience plus additional features and subscriber-only perks. (4.2 miles), 1980-03-23 21:38:15 UTC Cloverport This figure also shows that risks are more useful for policy decision-making than hazard. 2008-04-18 09:36:59 UTC (7.2 miles), 2015-09-12 17:00:12 UTC The slope failure shown in Figure 4 was caused by the Nisqually earthquake of Feb. 28, 2001. Hazard and risk are two fundamentally different concepts. 9.2 km from 13.2 km from Uniontown 7.2 km from (13.2 miles), 1990-01-27 14:05:50 UTC Those communities are prone to ground-motion amplification. Owenton Shaking was felt in many neighboring Kentucky counties. For example, most of the damage in Maysville during the Sharpsburg earthquake of July 27, 1980, was caused by amplified ground motion. (14.2 miles), 2008-04-18 15:14:16 UTC Different models result in different risk estimates. Chaffee Ground motion from a major earthquake in the New Madrid Seismic Zone is expected to be much stronger in western Kentucky than in the central and eastern parts of the state.
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