Abstract
If you live in an area where earthquakes happen, you might be especially interested in this science project. You'll learn how to build your own seismograph and how to use it to detect ground motion.Objective
The goal of this science project is to build and test your own seismograph.
Introduction
A seismograph is an instrument that detects and records ground motion. Ground motion can be caused by something man-made, such as a mine blast or a nuclear explosion; or by natural events, such as landslides, volcanic activity, or most often, earthquakes. Whenever any of these events occur, seismic waves are created, and it is these waves that a seismograph picks up.
There are two main types of seismic waves: body waves, which can travel through the inner layers of the earth, and surface waves, which can only travel on the surface. Body waves are the fastest and have the highest frequency. The first type of body wave is called the primary or P-wave. It pushes and pulls the solid rock or liquid matter that it is moving through, and people feel it as back-and-forth or side-to-side motion. The second type of body wave that you feel in an earthquake is called the secondary or S-wave. S-waves cannot move through liquids, only through solid rock. They move rock particles perpendicular to the direction the wave is traveling in. Don’t miss the exciting wave animations in the bibliography where you can see body waves and surface waves in action on rock particles!
![]() Click here to watch a video of this earthquake investigation, produced by DragonflyTV and presented by pbskidsgo.org. |
Did you know you can see evidence of the power of seismic waves all around the San Francisco Bay area? Watch the DragonflyTV video and follow Claire and Nisha as they discover signs of earthquakes in the roads, buildings, and ground all around their neighborhood.
So how does a seismograph measure seismic waves? Imagine trying to draw a straight line on a piece of paper while someone is holding your elbow and jiggling it back and forth. It would be hard to get the line straight, wouldn't it? A simple seismograph is kind of like your arm holding a pen. A horizontal beam (like your arm) holds the pen. The "elbow" end of the rod (the stand) is connected firmly to a sturdy vertical post (see the diagram below). To keep the beam from moving from small vibrations, a heavy weight is attached to the beam. The pen writes on paper mounted on a roll, which is turned at a constant speed (either by hand, or with a motor). Shaking of the ground causes the vertical stand to move up and down. This, in turn, causes the horizontal beam to jiggle back and forth. So instead of a straight line on the paper, the pen makes back-and-forth motions to draw squiggly lines. The greater the vibration, the greater the height of the squiggles, meaning the greater the intensity of the seismic waves.
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| This is a diagram of a homemade seismograph. (UC Regents, 1995.) |
The lines drawn by the seismograph result in what is called a seismogram. In this science project, you will build your own seismograph and see how well it can record ground vibrations.
Terms, Concepts and Questions to Start Background Research
To do this project, you should do research that enables you to understand the following terms and concepts:
Questions
Bibliography
Materials and Equipment
To do this science project you will need the following materials and equipment:
Experimental Procedure
Building the Seismograph
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| This is a diagram of a homemade seismograph. (UC Regents, 1995.) |
Testing the Seismograph
Here are some ideas for testing the seismograph. You can probably think of other ideas on your own.
Variations
Credits
Sources
This project is from:
Edited by Andrew Olson, PhD, Science Buddies
Last edit date: 2008-06-18 12:00:00
If you like this project, you might enjoy exploring careers in Geology.
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