This photograph shows the law crosscutting. What is the law of crosscutting? * 1 point A fault or intrusion of rock younger than the rock it cuts through. In undisturbed rock layers, the older rocks are on the bottom and the younger rocks are on the top.
The law of crosscutting is a principle in geology that states that any feature that cuts across another feature is younger than the feature it cuts through. It applies to faults, dikes, and intrusions, where the rock or geological feature cutting through another rock layer is considered younger than the rock it intersects. In undisturbed rock layers, the older rocks are indeed typically found at the bottom, with younger rocks on top, as described by the principle of superposition.
