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The plane along which motion occurs is called the fault plane. If it is visible at the surface, it is called a fault scarp Figure Figure 13 Click on link : Hanging wall, footwall, and scarp of a normal fault. There are three main types of faults: normal faults , reverse faults , and transform or strike-slip faults. In normal faults , the hanging wall moves downward relative to the footwall Figure 13 and Figure
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1. Relative age dating

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Adapted by Joyce M. First Edition. View Source. Last edited: 14 July Relative time is an important tool for geologist to quickly construct a model for a series of geologic events, especially in the field. In the following section, apply what you have learned regarding relative time to the questions below.
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Nicolaus Steno introduced basic principles of stratigraphy, the study of layered rocks, in [ 1 ]. William Smith , working with the strata of English coal mines, noticed that strata and their sequence were consistent throughout the region. The figure of this geologic time scale shows the names of the units and subunits. Using this time scale, geologists can place all events of Earth history in order without ever knowing their numerical ages. The specific events within Earth history are discussed in Chapter 8.
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This learning module discusses the geologic history of the Earth, the principles scientists use to define the Earth's geologic history, and relative dating techniques. Make sure students have a basic understanding of lithologies in addition to the method of crater counting for dating and interpreting the ages of Martian terrain. Your Account.
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