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When we observe the intersection in this diagram depicting these two dating techniques, we can conclude that they both have two things in common:1.Provide an idea of the sequence in which events have occurred.2.The area of intersection of both sets depicts the functions common to both.Take a look at the diagram to understand their common functions.

Relative dating is used to arrange geological events, and the rocks they leave behind, in a sequence.Relative techniques are of great help in such types of sediments.➤ It determines if an object/event is younger or older than another object/event from history.➤ Relative dating is qualitative.➤ This technique helps determine the relative age of the remains.➤ It is less specific than absolute dating.➤ Relative dating is comparatively less expensive and time-efficient.➤ It works best for sedimentary rocks having layered arrangement of sediments.The following are the major methods of relative dating.Many of these organisms have left their remains as fossils in sedimentary rocks.Geologists have studied the order in which fossils appeared and disappeared through time and rocks. Fossils can help to match rocks of the same age, even when you find those rocks a long way apart.

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