Time Frame
1 class periods of 70 minutes each
Summary
Students will learn how to find the epicenter of an earthquake using p and s waves and triangulation.
Materials
Instructional Procedures
- Students should be familiar with p and s waves. A good warm up activity is to have the students stand in a circle and create p waves by bumping the shoulder of the person next them and passing the wave. To create an s wave, hold hands and pass the wave by pulling the person next to you down and bending your knees. Describe the p wave as fast (and it will be faster) and the s wave as slower. Point out that the longer they travel the greater the time in between them (lag time)
- Read the directions with the students and do several examples with them. There are several steps to each calculation and it is easy to make a mistake.
- Allow students to work and check with you when they have an answer.
- If you have any difficulties with the formatting of the activity, email Barbara Gentry for original documents.
Assessment Plan
Scoring Guide:
Answers:
Epicenter should be located in approximately Southeast Idaho for earthquake 1 and in Missouri for earthquake 2.
Analysis:
- p-wave arrives first, s-wave second. The p-wave travels more rapidly.
- a seismograph
- The cities are different distances from the epicenter so it takes different amounts of time for the waves to arrive.
- The lag time gets larger the further you are from the epicenter.
- You could go to the place you think it happened and look for geological evidence.
Bibliography
Lesson Design by Jordan School District Teachers and Staff.
Created: 10/28/2014
Updated: 02/01/2018
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