When combined with the related principle of faunal succession, the law of superposition provides a very powerful tool for dating rocks and strata.
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Thrust faults were unknown to Steno and his contemporaries and were not described until the late 19th Century and early 20th century by Peach and Horne at Knockan Crag, Scotland, on the Moine Thrust Fault.
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Members low in the stratigraphic sequence are older than those lying above, in accordance with Steno's law of superposition.