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They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins.
Hanging wall and footwall normal fault. The hanging wall on the right slides down relative to the footwall. Where the fault plane is sloping as with normal and reverse faults the upper side is the hanging wall and the lower side is the footwall. Reverse faults occur in areas undergoing compression squishing. What is a reverse fault.
An upthrown block between two normal faults dipping away from each other is a horst. A normal fault occurs when the hanging wall moves relative to the footwall. With compressional forces the hanging wall moves upward relative to the footwall. A downthrown block between two normal faults dipping towards each other is a graben.
Its strike and its dip. The hanging wall slides down relative to the footwall. Which fault will see the hanging wall move down relative to the footwall. A n fault forms when the hanging wall moves down relative to the footwall a.
If the hanging wall rises relative to the footwall you have a reverse fault. In a normal fault the hanging wall moves downward relative to the footwall. If the hanging wall drops relative to the footwall you have a normal fault. Are exactly the opposite of normal faults.
When the fault plane is vertical there is no hanging wall or footwall. Two parallel normal faults form. If you imagine undoing the motion of a normal fault you will undo the stretching and thus shorten the horizontal distance between two points on either side of the fault. Normal faults occur in areas undergoing extension stretching.
A type of fault in which the hanging wall moves down relative to the footwall and the fault surface dips steeply commonly from 50 o to 90 o groups of normal faults can produce horst and graben topography or a series of relatively high and low standing fault blocks as seen in areas where the crust is rifting or being pulled apart by plate tectonic activity. Normal dip slip faults are produced by vertical compression as earth s crust lengthens. Low angle normal faults with regional tectonic significance may be designated detachment faults. Other articles where normal fault is discussed.
Normal fractures in rock with no offset where there has been no motion are called. Normal faults are common. The hanging wall on the left slides down relative to the footwall.
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