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09-Mar-2020 12:04

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The Law of Superposition, which states that older layers will be deeper in a site than more recent layers, was the summary outcome of 'relative datin g' as observed in geology from the 17th century to the early 20th century.The regular order of the occurrence of fossils in rock layers was discovered around 1800 by William Smith.While digging the Somerset Coal Canal in southwest England, he found that fossils were always in the same order in the rock layers.As he continued his job as a surveyor, he found the same patterns across England.The Permian through Jurassic stratigraphy of the Colorado Plateau area of southeastern Utah is a great example of Original Horizontality and the Law of Superposition, two important ideas used in relative dating.

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The principle of original horizontality states that the deposition of sediments occurs as essentially horizontal beds.

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