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It's called the Principle of Original Horizontality, and it just means what it sounds like: that all rock layers were originally horizontal.As you can imagine, regular sediments, like sand, silt, and clay, tend to accumulate over a wide area with a generally consistent thickness.We follow this same idea, with a few variations, when we talk about cross-cutting relationships in rock.Let's say, in this set of rock strata, that we found a single intrusion of igneous rock punching through the sedimentary layers.It's a fun and interactive dating event for singles.Their goal is to enrich your life with: Connection Companionship Fulfillment.Relative dating requires an extensive knowledge of stratigraphic succession, a fancy term for the way rock strata are built up and changed by geologic processes.

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