The law of cross-cutting relationships.
One is not necessarily older than the other. It depends on the context. A fault running through any rock must be younger than that rock.
That depends! If the fault line cross cuts the igneous intrusion causing the intrusion to be displaced on either side of the fault and forming a broken mass of rock within the intrusion known as a fault breccia then the fault is younger than the intrusions, as the intrusion must have already existed for the fault to cause it's displacement. If on the other hand the igneous intrusion cross cuts the fault and is un-deformed then it is probable that it is younger than the fault.
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The Ramapo Fault runs through New York, although it is not as active as other fault lines like the San Andreas Fault in California.
A fault occurs by 2 plates sliding along each other and then breaking.
No, reverse faults typically place older rocks on top of younger rocks. This is a result of compressional stress in the Earth's crust that pushes rocks upward and over each other along the fault plane.
A strike-slip fault would create landforms through shearing stress. In a strike-slip fault, two blocks of rock slide past each other horizontally, causing a horizontal shearing stress that can result in landforms such as fault scarps or offset river channels.
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It happens by two boundaries pushing past each other which goes through California.
A compressional fault is a type of geological fault where the rock layers are squeezed together, causing them to move vertically in relation to each other. This can lead to the formation of thrust faults, where older rock layers are pushed up and over younger layers. Compressional faults are commonly associated with convergent plate boundaries where tectonic forces push rocks together.
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