Teacher’s Corner: Earthquakes – Wasatch Fault
Integrating Survey Notes Articles in the Classroom
By Nancy Carruthers
Is it possible to predict when or where the next large earthquake in Utah will take place? To examine this question further read the two articles in the January 2007 Survey Notes that discuss research being conducted on the Wasatch fault.
The Utah Geological Survey (UGS), in conjunction with the U.S. Geological Survey and other researchers, performs studies to determine the timing, frequency, and magnitude of large, prehistoric, surface-faulting earthquakes on the Wasatch fault and other active faults in Utah.
The Wasatch fault, comprising 10 segments that rupture independently, is the longest active normal fault in the United States. Its five central segments extend through the Wasatch Front urban corridor between Brigham City and Nephi. During the past 10,000 years at least 25 surface-faulting earthquakes have taken place on the Wasatch fault. In Utah, earthquakes that rupture the ground surface are in the magnitude range of 6.5 to 7.5. The amount of time between large surface-faulting earthquakes on the Wasatch fault averages about 300-400 years.
In the two Wasatch fault articles, learn how geologists study large prehistoric earthquakes by measuring topographic profiles and excavating trenches across fault scarps. The information obtained in these types of studies has given researchers tremendous insights into the location, timing, and magnitude of past surface-faulting earthquakes in Utah, and on the Wasatch fault in particular.
Knowledge of past earthquake behavior helps us understand the risks associated with future earthquakes, but scientists remain unable to specifically predict the timing and magnitude of future earthquakes at a given location. Residents of earthquakeprone areas such as Utah should become familiar with the earthquake risk where they live, take appropriate emergency-planning measures, and not be surprised when “the big one” happens.
For more information on earthquake hazards in Utah, visit Utah Earthquakes & Faults.
January 2007 Survey Notes articles on the Wasatch Fault:
Possible Discussion Points
- What causes earthquakes?
- How can large earthquakes change landforms?
- What are two methods discussed in these articles that provide data on large prehistoric earthquakes?
- What dating method was used to determine the timing of a large prehistoric earthquake at Santaquin?
- How does movement on a normal fault (like the Wasatch fault) differ from movement on a strike-slip fault (like the San Andreas fault in California)?
Standard 2, Objective 2 c. – Describe how volcanoes, earthquakes, and uplift change landforms.
d. – Cite examples of how technology is used to predict volcanoes and earthquakes.
8th-Grade Integrated Science
Standard 2, Objective 4 a. – Describe how energy from the Earth’s interior causes changes to Earth’s surface.
Survey Notes, v. 39 no. 1, January 2007