The Law of Superposition and Determining the Relative Ages of Undisturbed Sedimentary Rocks. List the chronologic order of formation (oldest to youngest) and explain what happened and use the stratigraphic principles. Strat #1 H E D C Dike K Fault L Intrusion J 1. Chronologic order of formation (oldest to youngest) A-K Oldest — Youngest 2. Explain what happened (Use stratigraphic principles)


The Law of Superposition and Determining the Relative Ages of Undisturbed Sedimentary Rocks

The Law of Superposition is an important principle in geology that states that in an undisturbed sequence of sedimentary rocks, the oldest layers will be at the bottom and the youngest layers will be at the top. This principle can be used to determine the relative ages of the undisturbed sequence of sedimentary rocks (James, 2017). To determine the relative ages of the undisturbed sequence of sedimentary rocks, geologists use the law of superposition, which states that in an undisturbed sequence of sedimentary rocks, the oldest layers will be at the bottom and the youngest layers will be at the top. This principle can be seen in outcrops, where the oldest rocks are exposed at the bottom and the youngest rocks are exposed at the top. Geologists can also use other relative datings methods such as cross-cutting relationships, inclusions, and fossil correlation to determine the relative age of the rocks. To apply the law of superposition to determine the relative ages of the undisturbed sequence of sedimentary rocks, geologists need to identify the oldest rock layer at the bottom and the youngest rock layer at the top (James, 2017). Cont…

 

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