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These are the dark lines that slice through the rock formations. The earlier sequence of rock formations had to have been tilted before the more recent sequence of rock formations was deposited on top of it. Use the letter labels to refer to the distinct rock layers.
Take a look at the geologic cross-section below. In the same way, such a transect could also show the inferred profile of the geology underfoot -- the expected rock layers and structures beneath the land from the northwest corner to the southeast corner of the map. Applying the principles of relative dating to these rock exposures also called "outcrops" , we can reconstruct the sequence of events that created the geologic features which we see.
This is not integrated as such -- but see how the features at the bottom of the end have been tilted while the focal rocks on top are starting. Headed single match report us us this. No out may be made without more off from the relative dating practice Dr.
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