Nevada Seismological Laboratory

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The Earthquake Threat
Nevada is Earthquake Country
Confronting the Inevitable
Earthquakes in Nevada - 1850s to 1998
What are the Chances of Experiencing Strong Shaking?
What will Happen if a Disastrous Earthquake Strikes?
Earthquake Preparedness
Taking Control
Your Personal Safety
Life with Aftershocks
Home Safe Home
Eliminating Nonstructural Hazards
Avoid Earthquake Related Fires
The Anatomy of a Safe Building
Science Background
Reviewing the Basics
The Big Picture
Faults in Nevada
Measuring an Earthquake
Foreshocks, Mainshocks, and Aftershocks
What will the Shaking Feel Like
Earthquake Safety
The Road to Earthquake Safety
Earthquake Plan
Further Reading
Living with Earthquakes in Nevada: A Nevadan's guide to preparing for, surviving, and recovering from an earthquake

The Chance of Having an Earthquake in Nevada

Areas of Strong 
Shaking

Click for larger image



Over the last 150 years 24 earthquakes of magnitude 6 and larger, and about 5 earthquakes of magnitude 7 and larger have occurred in Nevada. This leads to an average time of 6 years between earthquakes with magnitudes equal to or larger than 6, but actual values have ranged from less than 5 minutes to 33 years. The largest events, those of magnitude 7 and greater, occur in Nevada on average every 30 years. These are relatively high rates of earthquake activity. The map below shows where the most intense shaking in Nevada has occurred between 1857 and 1999.


The Earthquake Hazard Perspective

We can't worry about every one of the several hundred earthquake-generating faults in Nevada every time a building is built. Nor do we need to. To prepare for earthquakes we mainly need to know the intensity of shaking we can anticipate over the expected life of the structure. Even though nobody knows for sure how long a building will last, an estimate of 50 years is commonly used. We estimate the strength of shaking that has a 1 in 50 chance of being exceeded in 50 years and design the building to be strong enough to resist damage from such a quake.

Maps like the one to the upper left are made by considering all the faults and the shaking that each might cause. Every fault needs to be identified and mapped. We study the characteristics needed to estimate the magnitude, primarily the fault length and maximum surface offset during a single earthquake. We also determine the average time between earthquakes or the average slip rate (Faults in Nevada). Finally we need to know how strong, on average, the shaking will be at every place when this fault has an earthquake. Shaking is more intense near the earthquake rupture and gradually decreases as you get farther away. Putting all this together, along with information from historical earthquakes, we make ground-motion maps like the one on the right. This map is similar to the maps that will be used in the International Building Code of 2000 (building codes give guidelines for constructing safe buildings). The map depicts peak ground shaking in percentage of the force of gravity (acceleration). The redder colors represent areas where the shaking is expected to be the strongest.

Using a measure of acceleration is common in earthquake engineering although many other measurements are needed for a complete description of ground motion; one "g" (gravity unit) is the force the Earth exerts on an object that makes it fall toward the Earth. You experience acceleration when you speed up or slow down quickly in a car. Your body is pushed back when you speed up or accelerate and is thrown forward when you slow down or deaccelerate.


Shaking Potential 
Map
Click for larger image

Engineers use computer models and model structures to see how buildings hold up to being accelerated sideways by a seismic wave. The notion of a map like this is very much like rolling the dice and calculating odds. If a rarer, but damaging, earthquake occurs in a part of Nevada that has less frequent earthquakes (yellow to blue colors), the shaking will be every bit as strong as earthquakes we anticipate in western Nevada. If we correlate this shaking potential map with possible damage, all of Nevada could experience damaging shaking. This is why Nevadans need to take messages of earthquake preparedness seriously.


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The Nevada Seismological Laboratory is a research and public service division of the University of Nevada. We are part of the Mackay School of Earth Sciences and Engineering in the College of Science.

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