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Visualizing Global Earthquakes Where and Why do Earthquakes Occur?
Cara Harwood, University of California-Davis
In this activity students visualize the distribution and magnitude of earthquakes at and below the surface of Earth and how their distribution is related to plate boundaries. Earthquakes are visualized on a 3D ...

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Subduction Zone Earthquakes
David Steer, University of Akron Main Campus;
While working in groups to facilitate peer tutoring, students manipulate a hands-on, physical model to better comprehend several characteristics of subduction zone earthquakes. -

Introduction to Earthquake Seismology Methods
Bruce Rueger, Colby College
This lab introduces students of aspects of earthquake seismology methods. These include analysis of p-wave amplitude, location of an earthquake epicenter and determining the time of occurrence of an earthquake. ...

Downloading Earthquake Data from the USGS Earthquake Hazards Site for Anywhere in the World and Studying it Using ArcGIS
Barb Tewksbury, Hamilton College
Students download earthquake data from the USGS Earthquake Hazards website and plot and anlyze the earthquakes using ArcMap and ArcScene.

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Earthquake Demonstration
This demonstration uses an "earthquake machine" constructed from bricks, sand paper, and a winch, to simulate the buildup of elastic strain energy prior to a seismic event and the release of that energy ...

Earthquake! A Term Paper and Presentation Assignment
Laura Wetzel, Eckerd College
In this writing and oral presentaion assignment, students are challenged to assess a building site for a fictitious organization, the Society for Earthquake Enthusiasts. Each student must choose a historically ...

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Determining Earthquake Recurrence Intervals from Trench Logs
Patricia Cashman, University of Nevada-Reno
Trench logs of the San Andreas Fault at Pallett Creek, CA are the data base for a lab or homework assignment that teaches about relative dating, radiometric dating, fault recurrence intervals and the reasons for uncertainty in predicting geologic phenomena. Students are given a trench log that includes several fault strands and dated stratigraphic horizons. They estimate the times of faulting based on bracketing ages of faulted and unfaulted strata. They compile a table with the faulting events from the trench log and additional events recognized in nearby trenches, then calculate maximum, minimum and average earthquake recurrence intervals for the San Andreas Fault in this area. They conclude by making their own prediction for the timing of the next earthquake.

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A Kinesthetic Demonstration for Locating Earthquake Epicenters
John Keyantash, California State University-Dominguez Hills
A kinesthetic activity for students to understand the technique for locating the epicenter of an earthquake. It is performed indoors and outdoors in three lessons.

Cascadia Great Earthquake and Tsunami Suite
Michael Mayhew, National Science Foundation;
Michael Mayhew and Michelle Hall, Science Education Solutions Summary The Cascadia Earthquakes and Tsunami Suite contains five case studies organized around understanding the potential for large earthquakes and ...

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Is the New Madrid Seismic Zone at risk for a large earthquake?
Eliza Richardson, Penn State
In this lesson we discuss the controversy regarding the extent of seismic risk in the central United States today. We learn how to estimate earthquake recurrence interval using a variety of methods. This lesson ...

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