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Relative Dating - Admission/Application Essay Example

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Relative dating is the scientific process of the determination of the relative sequence of past occurrences without mainly determining their actual age.Lithologies, superficial deposits, geological rocks and fossils can all be utilized to relate one statigraphic column to…
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Relative Dating
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Relative Dating

Download file to see previous pages... relative dating is only used to find out the occurrence of events sequentially, and not the time they occur, it still remains a very valuable method especially when studying materials which do not have radioactive isotopes. The most preferred style of relative dating in paleontology is by biostratigraphy and in most aspects more accurate. A summarized result of relative dating as found in geological period from seventeenth century to the early twentieth century resulted into a law called Superposition. In 1800, a gentleman by the name of Smith William discovered an organized order of occurrence of fossils in layers of rock. This is while he was excavating, the Somerset Coal Canal in the southwest part of England. He discovered that fossils were found in a particular order in layers of rock. The more he excavated and surveyed, the more he discovered that similar patterns across England. He further discovered that particular animals were found in only particular layers and that they remained in similar layers all over England. Due to this realization, William was able to find out the order in which the rocks were formed. He later published a map showing the geology of England (sixteen years later), which showed all the rocks of various geologic time zones.
This principle is all about crosscutting intrusions. The following are examples of various types of intrusions; dikes, batholiths, laccoliths, sills and also stocks. In the study of earth if an igneous intrusion penetrates through a layer of sedimentary formation, then it can always be determined that the sedimentary rock is older than the igneous ...Download file to see next pagesRead More
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