There are two basic tools for interpreting these sections:
1. Superposition - Generally sedimentary rocks are deposited one on top of the other.
2. Crosscutting relations - rock units are often cut across by faults that break the existing rocks, folds that bend them, and igneous intrusions that get squeezed into other rocks.
Here are examples of a fault:



Here are examples of folds and an intrusion:


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