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Relative dating of rocks and events Yuvutu

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The combination of these two types of geologic ages makes a complete record of earth's geologic history in terms of the order of events and in terms of how many years ago each event occurred.

As discussed before, the assumptions influence the interpretation of the data.

The most obvious feature of sedimentary rock is its layering.

This feature is produced by changes in deposition over time.

These ages have been derived from relative dating and absolute dating (radiometric dating) of rock layers and fossils.

(a) Relative Dating This technique uses principles of stratigraphy (rock strata) and the study of fossils (palaeontology) to determine the relative ages of rocks and sediments. Field geologists' rely on a number of simple techniques for dating rocks and constructing geological successions. The Law of Strata Identified by Fossils is a little bit more complex.