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 Sequence of rocks deposited in layers, the youngest layers on top and the oldest on bottom, each layer being younger than the one beneath it and older than the one above it.

One of the geological precepts that scientists use to assess the relative ages of rock strata, or layers, is the law of superposition.

What are the examples of law of superposition?

The oldest pancake is on the bottom, and the newest is on top.

This is an example of the Law of Superposition, in which rock layers form over time, with the ancient layer forming first (at the bottom), and each layer forming on top of the previous one.

Thus, the law of superposition is to assess rock strata relative age.

For more details regarding law of superposition, visit:

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