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Relatively, they are younger than the rock they cut through.
They are used to determine the relative ages of rocks by stating that younger rocks lie above older rocks, and that rocks that cut through a layer are younger than the existing layer.
Normal faults are caused by tension in the movement of rocks
Crystal
Neither cracks nor faults cause earthquakes by themselves. It is the motion of the Earth's plates.
Relatively, they are younger than the rock they cut through.
Because the rocks have to be there first, all faults are younger than the rocks they end up cutting across. In regard to sedimentary rock layers, each layer is younger than the one below it.
Faults are always younger than the rocks they cut. They cannot be older that the rocks they are cutting, because the rocks would not be there.
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
They are used to determine the relative ages of rocks by stating that younger rocks lie above older rocks, and that rocks that cut through a layer are younger than the existing layer.
A joint is a crack in rock; a fault is a crack in rock along which the rocks have been displaced.
Strike-slip faults indicate rocks are sliding past each other horizontally, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.
Before 1965, geologists were unable to explain the abrupt disappearance of transcurrent faults in crustal rocks. Wilson explained the phenomenon with his suggestion that the vanishing faults could be explained by the presence of zones of contraction and expansion in the crustal bedrock. He named these "disappearing" faults transform faults.
Faults
Normal faults are caused by tension in the movement of rocks
Rocks moving apart can cause normal faults to form, as opposed to reverse and strike-slip faults.
relative dating.Relative dating is used to determine the relative age of rocks.