The Day the Earth Shook

This program presents information about some architectural features that work and those that don’t during an earthquake. To give the students some hands-on experience in structural design, conduct this activity.

EARTHQUAKES LESSON

Objective:
By completing this lesson, students will learn about earthquakes, and in the process demonstrate their reading comprehension skills, including reading strategies, inference, literal meaning, and critical analysis.

Earthquake Teaching Box

The goal of this Teaching Box is to teach students about how and why earthquakes cause damage. Living in Earthquake Country explores seismic waves, the ability of scientists to predict the likelihood and severity of earthquakes at specific locations, the difference between magnitude and intensity, the occurrence of earthquakes along patches of planar faults, and the potential damage caused by earthquakes such as landslides, liquefaction, or structural failure.

A Model of Three Faults

One of the most frightening and destructive phenomena of nature is a severe earthquake and its terrible aftereffects. An earthquake is a sudden movement of the Earth, caused by the abrupt release of strain that has accumulated over a long time. For hundreds of millions of years, the forces of plate tectonics have shaped the Earth as the huge plates that form the Earth’s surface slowly move over, under and past each other. Sometimes the movement is gradual. At other times, the plates are locked together, unable to release the accumulating energy. When the accumulated energy grows strong enough, the plates break free. If the earthquake occurs in a populated area, it may cause many deaths and injuries and extensive property damage.

Locating an earthquake with recent seismic data

Objective

By the end of this activity, the student will be able to:
1. Identify P and S waves on seismograms,
2. Determine the distance of an epicenter from a seismic station using travel time curves,
3. Locate the epicenter of an earthquake by triangulation, and
4. Calculate the time of origin of an earthquake based on seismic data