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Earthquakes occur as a result of motions on faults. In this lesson we examine how geologists characterize and classify faults. We have two learning objectives; To introduce key terms geologists use to classify faults; and, to illustrate examples the major faults so that you can learn how to draw and label a sketch of each type the fault. We use the term dip to indicate the slope or inclination of any geological surface measured relative to horizontal. The steeper the slope the larger the dip angle. A second characteristic of inclined surfaces is the strike. A strike line is any horizontal line drawn or inscribed on a sloping surface. It is the water line in a sink or bathtub, or the line your coffee makes as it rests in your cup. Dip and strike are perpendicular or 90 degrees from each other. We can see examples of the dip and strike on various surfaces we encounter in our daily lives. The mortar between these bricks is parallel to the strike and dip as the corners of the bricks are a
