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Principle of cross-cutting relationships The principle of cross-cutting relationships states that a rock unit or other geological feature, such as a fault that is cut by another rock unit or feature must be older than the rock unit or feature that does the cutting. Imagine cutting a slice of bread from a whole loaf. When investigating rocks in the field, geologists commonly observe features such as igneous intrusions or faults that cut through other rocks. Because these features are the ones doing the cutting, we know that they are younger than the rocks that they cut into. Have a look at the photographs below, which show the curb of a road in a neighborhood in Hollister, California.
You can see that the curb is offset: As it turns out, the famous San Andreas fault runs below the curb at this location, which has caused the curb to be broken and displaced. We know that the curb was originally straight when it was first constructed. The fault cut the curb and is thus younger than the curb itself. A curb in Hollister, California that is offset by the San Andreas fault. The cartoon below shows an imaginary sequence of rocks and geological events labeled A-I. Using the principles of superposition and cross-cutting relationships, can you reconstruct the geological history of this place, at least based upon the information you have available?
An imaginary cross-section, showing a series of rock layers and geological events A-I. A is a fault. B-F are sedimentary rock layers. G and H are both igneous intrusions. Finally, I is an erosional surface. Based on the principles of superposition and cross-cutting relationships, what are the relative ages of these rocks and events?