Earthquake Hazards
Utah has experienced 17 earthquakes greater than magnitude (M) 5.5 since pioneer settlement in 1847, and geologic investigations of our region’s faults indicate a long history of repeated large earthquakes of M 6.5 and greater prior to settlement. Seismic activity can often trigger a succession of additional potentially destructive hazards. The seismic-related hazards listed below all possess their own potential for destruction. Some areas of the state are more susceptible than others when it comes to being at risk.
Learn About Utah Earthquakes
While Utah is not on a boundary between tectonic plates where most of the world’s earthquakes occur, it is in the tectonically extending western part of the North American plate. Thus, earthquakes in Utah are related to interactions with the Pacific plate along the plate margin on the west coast of the United States. Also, many small earthquakes in east-central Utah are induced by underground coal mining.
Earthquake-Related Geologic Hazards:
Utah Earthquakes Virtual Field Trip from the Natural History Museum of Utah.
Utah Earthquakes (1850 to 2016) and Quaternary Faults Map
This map shows earthquakes known to have occurred within and surrounding Utah from 1850 through December 2016 and mapped Quaternary faults considered to be earthquake sources. The faults shown on the map have been sources of large earthquakes (about magnitude 6.5 or greater) during the Quaternary Period (past 2.6 million years) and are the most likely sources of large earthquakes in the future. Most small to moderate size earthquakes plotted on the map are “background” earthquakes not readily associated with known faults and of a size generally below the threshold of surface faulting (about magnitude 6.5). Buried or unmapped secondary faults are likely sources of much of the background seismicity.
Costs of Earthquake Hazards
Although only two fatalities (ground shaking-related) from earthquakes have occurred in Utah since 1847, scenario modeling predicts 2000 to 2500 fatalities, 7400 to 9300 life-threatening injuries, 55,400 buildings completely damaged, 21 million tons of debris, and $33.2 billion in estimated short-term, direct economic losses from a major M 7.0 earthquake on the Salt Lake City segment of the Wasatch fault zone. Short-term financial losses and long-term economic costs include damages, cleanup, closed businesses, lower productivity and economic output, and other costs. It is projected that 61% of the total number of buildings in the 12 county area in northern Utah will be moderately damaged or totally destroyed. Such an event will likely take decades to recover from and will be the single most costly geologic hazard event to affect Utah.
Related Information:
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Public Interest Articles
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