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Bookmark or Share- 14.3: Fractures, Joints, and Faults - Geosciences LibreTextsDip-Slip Faults. Dip-slip faults are so named because the dominant motion involves moving up or down the dipping (tilting) fault plane. In dip-slip faults we identify rock above the fault as the hanging wall, (or headwall) and the rock beneath as the footwall.These terms were originally used by miners to describe the rocks above and below an ore body (Figure 13.24).
- What is a fault and what are the different types?What is a fault and what are the different types? A fault is a fracture or zone of fractures between two blocks of rock. Faults allow the blocks to move relative to each other. This movement may occur rapidly, in the form of an earthquake - or may occur slowly, in the form of creep.
- FAULT | English meaning - Cambridge DictionaryFor all the faults in our education system, it is still better than that in many other countries. [ C ] (in tennis and some other games ) a mistake made by a player who is beginning a game by hitting the ball
- 3 Types of Faults: Normal, Reverse and Strike-Slip - Earth HowNormal, Reverse and Strike-Slip Faults. Faults are an important part of geology and can be categorized in various ways. This blog post offers a brief introduction to the most common type of fault. The 3 types of faults are: Normal faults; Reverse faults; Strike-slip faults
- Fault (geology) - WikipediaIn geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.
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