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Relatively, they are younger than the rock they cut through.
physical features are tilting,faults,intrusion and folding also, using superposition as long as u know which order these go by u can figure out relative age of a rock
A fault must be younger than the rock it cuts through.
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
The two types of faults that can result in mountains are reverse faults and normal faults.
by looking at it
To determine relative age, geologists also study extrusions and intrusions of igneous rock, faults, gaps in the geologic record, and inclusions.
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Relatively, they are younger than the rock they cut through.
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
4 ways are folding, tilting, intrusions, and faults. Hope this helped :)
physical features are tilting,faults,intrusion and folding also, using superposition as long as u know which order these go by u can figure out relative age of a rock
Faults are important because it can move the blocks relative to each other. And they can have a major influence on the shaping of the landscape.
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.
Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occured.
Strains in rocks near faults