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Demonstrating P and S Waves with a Slinky
Pier Bartow
, Klamath Community College
Initial Publication Date: December 2, 2008 Summary
P and S seismic waves can be demonstrated with a slinky. P waves have energy traveling parallel to the direction the wave is moving. S waves have energy traveling perpendicular to the direction the wave is moving.
Topics
Seismology
Grade Level
College Introductory
Follow the link above to find activities from Teach the Earth on a specific topic.
Share your modifications and improvements to this activity through the Community Contribution Tool »Context
Audience
Introductory level seismology in a physical geology course.
Skills and concepts that students must have mastered
Hopefully they will have read the chapter.
How the activity is situated in the course
This is the hands-on part of a lecture on seismic waves. I have found this to be an eye opener for students. Also, any time you bring a slinky to class the students want to play with it. So, it's fun! Goals
Content/concepts goals for this activity
The students can see that I am putting energy into the slinky in two different ways. A quick push down the length of the stretched out slinky demonstrates a pressure wave and a quick flip of the wrist will send a shear wave down the slinky.
Higher order thinking skills goals for this activity
This is a simple analog model of P and S seismic waves. The demonstrations allows the students to answer questions about why P waves travel faster than S waves. Also, they can see why P waves can travel through a liquid while S waves cannot. Other skills goals for this activity
This is a great exercise to get a group of students working together.
Description of the activity/assignment
The students can see that I am putting energy into the slinky in two different ways. A quick push down the length of the stretched out slinky demonstrates a pressure wave and a quick flip of the wrist will send a shear wave down the slinky. This allows the students to answer questions about why P waves travel faster than S waves. Also, they can see why P waves can travel through a liquid while S waves cannot.
I first do the demonstration as described above then they break up into groups to experiment for themselves. I provide one slinky for every 4 students. We then talk about the liquid outer core of the Earth and how this would effect seismograph readings around the globe. Then I give a quiz to help them focus on what they have learned. Determining whether students have met the goals
A short quiz asks the students to explain the differences between P and S waves, and their unique attributes. More information about assessment tools and techniques.Teaching materials and tips
Share your modifications and improvements to this activity through the Community Contribution Tool »
Other Materials
- This activity has supplemental information submitted as part of the InTeGrate Teaching the Methods of Geoscience workshop in June 2012.
Related Links
Related Links
Demonstrating P and S Waves with a Slinky
Pier Bartow
, Klamath Community College
Initial Publication Date: December 2, 2008
Summary
P and S seismic waves can be demonstrated with a slinky. P waves have energy traveling parallel to the direction the wave is moving. S waves have energy traveling perpendicular to the direction the wave is moving.
Topics
SeismologyGrade Level
College Introductory Follow the link above to find activities from Teach the Earth on a specific topic.
Context
Audience
Introductory level seismology in a physical geology course.
Skills and concepts that students must have mastered
Hopefully they will have read the chapter.
How the activity is situated in the course
This is the hands-on part of a lecture on seismic waves. I have found this to be an eye opener for students. Also, any time you bring a slinky to class the students want to play with it. So, it's fun!
Goals
Content/concepts goals for this activity
The students can see that I am putting energy into the slinky in two different ways. A quick push down the length of the stretched out slinky demonstrates a pressure wave and a quick flip of the wrist will send a shear wave down the slinky.
Higher order thinking skills goals for this activity
This is a simple analog model of P and S seismic waves. The demonstrations allows the students to answer questions about why P waves travel faster than S waves. Also, they can see why P waves can travel through a liquid while S waves cannot.
Other skills goals for this activity
This is a great exercise to get a group of students working together.
Description of the activity/assignment
The students can see that I am putting energy into the slinky in two different ways. A quick push down the length of the stretched out slinky demonstrates a pressure wave and a quick flip of the wrist will send a shear wave down the slinky. This allows the students to answer questions about why P waves travel faster than S waves. Also, they can see why P waves can travel through a liquid while S waves cannot.
I first do the demonstration as described above then they break up into groups to experiment for themselves. I provide one slinky for every 4 students. We then talk about the liquid outer core of the Earth and how this would effect seismograph readings around the globe. Then I give a quiz to help them focus on what they have learned.
I first do the demonstration as described above then they break up into groups to experiment for themselves. I provide one slinky for every 4 students. We then talk about the liquid outer core of the Earth and how this would effect seismograph readings around the globe. Then I give a quiz to help them focus on what they have learned.
Determining whether students have met the goals
A short quiz asks the students to explain the differences between P and S waves, and their unique attributes.
More information about assessment tools and techniques.Teaching materials and tips
Share your modifications and improvements to this activity through the Community Contribution Tool »
Other Materials
- This activity has supplemental information submitted as part of the InTeGrate Teaching the Methods of Geoscience workshop in June 2012.