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Abstract Here's a project that involves a different kind of sandbox than the ones you usually think of. This one has a moving wall inside, acting like a piston, to compress the sand. You can make layers using two different colors of sand, and then see what happens when you compress the layers with the piston. If you're handy with woodworking tools, this is a good project to give you a feel for the effects of geological forces that deform the Earth's crust.Objective The goal of this project is to investigate how layers of sand deform under lateral compression. Introduction If you've studied Earth science in school, you know that the surface of the Earth (the crust) is made up of many separate plates (Figure 1, below). These plates ride on top of the deeper, molten layer of the Earth, the mantle. You also learned that the plates are not stationary, but are slowly moving. What happens to the Earth's crust when tectonic plates collide? One result of the tremendous forces generated by movement of tectonic plates is the folding of the Earth's crust. For a quick demonstration, grasp a sheet of paper lengthwise with one hand at each end of the paper. Slowly push your hands together. The paper buckles, with the center either rising upward or extending downward as you bring the ends of the paper toward each other. Due to the tremendous pressures that can be created by plate movement, this kind of folding can occur with layers of rock. Geologists have names to describe the different types of folds. When the layers have just a slight bend, it's called a monocline. When the center of the fold rises up like an arch, the fold is called an anticline. When the center of the fold falls down in a trough, the fold is called a syncline. When the compression forces are very great, you can sometimes see multiple anticlines and synclines following one after the other. There are also more complex folds called recumbent folds ("recumbent" means "lying down"). As you might imagine, these are folds that have been "knocked over" by additional shearing forces. A reference in the Bibliography has example diagrams to illustrate each of the folding patterns described above (Pidwirny, 2007). It's a little hard to generate enough force to bend rocks with an apparatus that you can easily build in your garage, so for this project you'll be investigating layers made with different colors of sand instead of rock. For your experimental apparatus, you'll build a sandbox with a moveable piston to compress the sand (see Figure 2 in the Experimental Procedure). To do the experiment, you first carefully load up the box with layers of sand, alternating two different colors to make the layers readily visible. Then you use the piston to apply a compressive force to the layers of sand. Transparent windows in the sides of the box allow you to see the resulting layering patterns after the compressive force has been applied. You can take successive pictures, or record with a video camera, to see how the patterns develop over time as the force is applied. The surface tension of water causes the grains of sand to stick to one another, so you could investigate the effect of changing the wetness of the sand used. Or, you could investigate the effects of changing the grain size of the sand used. Or, while you're doing the experiment, your own observations may lead to another avenue of exploration. Press on and find out!
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 experiment you will need the following materials and equipment:
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| Experimental apparatus for compressing layers of sand. (Indiana School for the Deaf, date unknown) |
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| Before a sheet metal "scraper" was installed at the bottom surface of the piston a lot of sand could "leak" under the piston as it moved. (Indiana School for the Deaf, date unknown) |
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| Side view of sand compression apparatus in action (Indiana School for the Deaf, date unknown). |
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| Top view of sand compression apparatus in action (Indiana School for the Deaf, date unknown). |
Variations
Credits
Andrew Olson, Ph.D., Science Buddies
Sources
This project is based on:
Last edit date: 2007-10-05 12:00:00
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