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To determine relative age, geologists also study extrusions and intrusions of igneous rock, faults, gaps in the geologic record, and inclusions.
by looking at it
4 ways are folding, tilting, intrusions, and faults. Hope this helped :)
No
w0w
To determine relative age, geologists also study extrusions and intrusions of igneous rock, faults, gaps in the geologic record, and inclusions.
by looking at it
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 :)
Earthquakes
No
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
By studying how the earth's crust reacts to earthquakes, volcanoes, or underground explosions and the like.
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.
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