Move Over, I'm Coming Through! |
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| When you look closely at various rock formations, you often find that they seem to not always follow the order of oldest on the bottom and youngest on the top (like you learned on the previous Sci-ber text page.) This page is designed to help you see ways that Earth's changes can alter the order that rocks are found in. If you have some clay or want to make some salt dough, you can model these examples on your own.
There are three kinds of faults that can occur when an earthquake happens. Each of these is the result of Earth's movement along the fault line.
A difference between the normal and reverse fault is that the force deforming the crust in a normal fault pulls apart while the force deforming the crust in a reverse fault pushes together. Another difference is that in a normal fault the half of the fault that lies above is called the hanging wall. The half of the fault that lies below is called the footwall. The rock forming the hanging wall of a reverse fault slides up and over the footwall. A fault is a break in Earths crust where slabs of rock slip past each other. In this activity, you will make a model of the movements along faults.
Materials:
Procedure:
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Analysis:
Extensions: Draw a river on the surface of your clay model. Modify your data chart to show the effects the three faults have on the river. Enrichment: On Earths surface, individual faults do not exist all by themselves. With one or more of your classmates, combine your models to show how faults combine to form mountains. |
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