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In geology, intrusions and faults are younger than surrounding rocks.
The characteristic shared by intrusions and faults is that both are younger than surrounding rocks. When magma intrudes into a crack or weakness and solidifies, forming an intrusion, it cuts across pre-existing rocks, making it younger. Similarly, faults, which are fractures where movement occurs, are also younger than the rocks they cut through due to the principle of cross-cutting relationships.
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