20 September 2000 10:00 AM PDT
The Federal Emergency Management Agency (FEMA) has just released a document entitled HAZUS99 Estimated Annualized Earthquake Losses for the United States. The document presents estimates, using the HAZUS computer program written for FEMA, of annualized losses due to earthquakes in all 50 states plus the District of Columbia, and in 40 metropolitan areas of the United States. The report also estimates the ratio of average annualized loss to replacement value for the states and metropolitan areas.
The Nevada Seismological Laboratory has only just received a copy of the report and has not had a chance to analyze it thoroughly. The following discussion is based on our first impression of the contents of the document. We will follow this with additional comments as appropriate.
In Nevada this document is likely to attract considerable attention for several reasons:
The following are my interpretations of the numbers in this report.
Specific comments for Nevada:
For more information about earthquakes in Nevada and how to be prepared, please contact John G. Anderson, Director, Nevada Seismological Laboratory (775-784-4265), Jonathan G. Price, Director and State Geologist, Nevada Bureau of Mines and Geology (775-784-6691 extension 126), or Frank Siracusa, Chief, Nevada Division of Emergency Management (775-687-4240) and see the Web sites of the Nevada Seismological Laboratory (www.seismo.unr.edu), the Nevada Earthquake Safety Council (www.nbmg.unr.edu/nesc/index.html), the Nevada Bureau of Mines and Geology (www.nbmg.unr.edu), and the Nevada Division of Emergency Management (www.state.nv.us/dem/index.htm). The column "Opinion: Exceeding Seismic Code Pays in the Long Run" (which is accessed from the page on "Preparedness Information from the NESC page of the Seismological Laboratory web site: http://www.seismo.unr.edu/nesc/rgj-jga980125.html) may be of particular interest.
Nevada has significant earthquake hazards and risks. On Wednesday, September 20, 2000, the Federal Emergency Management Agency (FEMA) released a report titled "HAZUS 99 Estimated Annualized Earthquake Losses for the United States." In this report FEMA estimates that the loss from earthquakes for residential and business buildings in Nevada is likely to be, on the average, approximately $55 million per year. In any given year, the actual loss is likely to be either considerably lower or higher, because earthquakes are infrequent events. One way to think of these numbers is as the result of approximately a Northridge earthquake-sized loss once every 300 years in Las Vegas, and also once every 300 years in Reno. This model includes direct damage to buildings, non-structural damage, and part of the economic loss from not being able to use many buildings immediately after an earthquake. The figure is a minimum estimate of potential loss, because it does not include damage to infrastructure (such as roads, bridges, and electrical, water, sewage, and communication systems) or building contents, and it does not consider indirect economic losses, such as effects on tourism.
Nevada has experienced many historical earthquakes. Although earthquakes dont occur at regular intervals, in historical times we have experienced a magnitude 7 or greater earthquake somewhere in the state about once every 30 years. The last major earthquake was a magnitude 7.2 in 1954 at Fairview Peak 45 miles (70 kilometers) southeast of Fallon. The largest historical earthquake in Nevada was in 1915 in Pleasant Valley 35 miles (60 kilometers) south of Winnemucca; this event has been estimated to have been a magnitude 7.3 to 7.8. In the geological past, large earthquakes have occurred near what are now urban areas. For example, within the last 3,000 years two earthquakes have occurred along the Genoa fault, which extends from south of Woodfords, California, through the town of Genoa, into Carson City. The most recent event was between 500 and 600 years ago, and the penultimate event was between 2,000 and 2,200 years ago. In each event, the fault moved as much as 18 feet (5.5 meters), and the earthquakes were probably magnitude 7.2 to 7.5.
Risk from earthquakes is a function of the geological hazard and the structures and number of people at risk. Among the states, California ranks first (with an estimated average annual loss of $3.3 billion) because it not only has a high hazard from many active faults, such as the San Andreas fault, but it also has many buildings and a large population at risk. The FEMA loss estimation computer model uses available national data sets and makes assumptions about certain parameters in the data, such as soil and rock responses to earthquakes and types of buildings at risk. At a high level of confidence, the FEMA numbers can be viewed as order-of-magnitude estimates. (That is, they could be off by a factor of ten, although calibrations with the Northridge 1994 and Loma Prieta 1989 earthquakes would suggest that the calculations may be accurate within a factor of two.) It is therefore unwise to make too much of small differences in the rankings from state to state or from city to city. Nonetheless, FEMAs calculations place Nevada fifth among the states in terms of estimated average annual loss from earthquakes.
Among the metropolitan areas that FEMA evaluated in its loss estimation model, Las Vegas and Reno ranked high on the list (at $28 million and approximately $18 million per year, respectively) in terms of estimated loss. Although the hazard is higher in Reno than in Las Vegas (that is, the geological and seismic evidence suggest to us that there is a higher probability of having a major earthquake in the Reno-Sparks-Carson City area than in the Las Vegas area), the calculated loss is higher in Las Vegas because the greater size of Las Vegas more than offsets the greater number of earthquakes in the vicinity of Reno.
The FEMA report illustrates earthquake risk in two ways average annual dollar loss and the ratio of dollar loss to the value of the building stock. The latter way of portraying the numbers closely reflects the earthquake hazards as presented in the probabilistic seismic hazard maps of the U.S. Geological Survey, which provide some of the input for FEMA's computer model. In comparing estimated earthquake losses for metropolitan areas, Reno ranks higher than Las Vegas in terms of the ratio of dollar loss to the value of the building stock. That is, there is a higher percentage of the building stock at risk from earthquakes in Reno than in Las Vegas. By any measure, the Reno-Sparks-Carson City and Las Vegas metropolitan areas have high earthquake risks.
There is a good chance that you will experience a major earthquake if you live in western Nevada. There are approximately 30 faults that are likely to cause damage in the Reno-Carson City urban corridor. The probability of at least one magnitude 6 or greater event in the next fifty years is between 34 and 98%. The probability of at least one magnitude 7 or greater event in the next fifty years is between 4 and 50%. Hazards include intense ground shaking, ruptures of the ground, liquefaction, landslides, and ancillary problems, such as fires and hazardous waste spills.
An urban earthquake today could cause billions of dollars in damage. FEMA's analysis uses a nationally consistent approach that looks at long-term probabilities rather than worst-case or likely scenarios. Although the numbers are reasonable estimates of average annual loss, the actual loss may be considerably higher in any given event.
We dont know everything that needs to be known. More research can accomplish two things: it can reduce the uncertainties in the estimates of the seismic risk, and it can lead to a more precise description of the hazard for planning, earthquake-resistant construction, and hazard mitigation. For instance, only 15% of the state is adequately mapped geologically, and much more needs to be learned about the geological history of faults. Seismometers adequately cover only small portions of the state, and only a few strong-motion instruments have been installed. The effects of soils on ground shaking have not been adequately determined anyplace in Nevada. There are not enough continuous global positioning system (GPS) sites recording strain in Nevada.
We cant predict when earthquakes will occur, but we can be better prepared. Earthquake risks can be reduced through non-structural mitigation; structural hardening or rehabilitation of buildings and infrastructure; better understanding and mapping of the hazards; zoning restrictions where appropriate; strengthening and enforcing building codes; insurance and related incentives for mitigation; engineering, seismological, and geological research; and education of the public.
For more information about earthquakes in Nevada and how to be prepared, please contact John G. Anderson, Director, Nevada Seismological Laboratory (775-784-4265), Jonathan G. Price, Director and State Geologist, Nevada Bureau of Mines and Geology (775-784-6691 extension 126), or Frank Siracusa, Chief, Nevada Division of Emergency Management (775-687-4240) and see the Web sites of the Nevada Earthquake Safety Council (www.nbmg.unr.edu/nesc/index.html), the Nevada Bureau of Mines and Geology (www.nbmg.unr.edu), the Nevada Seismological Laboratory (www.seismo.unr.edu), and the Nevada Division of Emergency Management (www.state.nv.us/dem/index.htm).
References:
dePolo, C.M., Jones, L.M., dePolo, D.M., and Tingley, S., 2000, Living with earthquakes in Nevada: Nevada Bureau of Mines and Geology Special Publication 27, 36 p. (free on the Web at www.nbmg.unr.edu/dox.htm).
dePolo, C.M., Ramelli, A.R., and dePolo, D.M., Earthquakes in Nevada and how to survive them: Nevada Bureau of Mines and Geology Educational Series Publication E-16 (8-page brochure, free on the Web, Spanish translation is Educational Series Publication E-27).
dePolo, C.M., Anderson, J.G., dePolo, D.M., and Price, J.G., 1997, Earthquake occurrence in the Reno-Carson City urban corridor: Seismological Research Letters, v. 68, No. 3, p. 401-412.
dePolo, D.M., and dePolo, C.M., 1999, Earthquakes in Nevada, 1852-1998 (1:1,000,000-scale, full-color, shaded relief map with epicenters): Nevada Bureau of Mines and Geology Map 119.
Ramelli, A.R., Bell, J.W., dePolo, C.M., and Yount, J.C., 1999, Large-magnitude, late Holocene earthquakes on the Genoa fault, west-central Nevada and eastern California: Bulletin of the Seismological Society of America, v. 89, p. 1458-1472.