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Relative dating is the science of determining the relative order of past events i. In geology, rock or superficial deposits , fossils and lithologies can be used to correlate one stratigraphic column with another. Prior to the discovery of radiometric dating in the early 20th century, which provided a means of absolute dating , archaeologists and geologists used relative dating to determine ages of materials. Though relative dating can only determine the sequential order in which a series of events occurred, not when they occurred, it remains a useful technique. Relative dating by biostratigraphy is the preferred method in paleontology and is, in some respects, more accurate. The regular order of the occurrence of fossils in rock layers was discovered around by William Smith.
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5 of The Best Geology Books For Beginners

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Geology | HISTORY Channel

William 'Strata' Smith 23 March — 28 August was an English geologist , credited with creating the first detailed, nationwide geological map of any country. Financially ruined, Smith spent time in debtors' prison. It was only late in his life that Smith received recognition for his accomplishments, and became known as the "Father of English Geology ". In , he met and found work as an assistant for Edward Webb of Stow-on-the-Wold , Gloucestershire , a surveyor. He was quick to learn, and soon became proficient at the trade. In , he travelled to Somerset to make a valuation survey of the Sutton Court estate, and building on earlier work in the same area by John Strachey.
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Geological formation

Stratigraphic cycles refer to the transgressive and regressive sequences bounded by unconformities in the stratagraphic record on the cratons. These cycles represent a large scale eustasy cycle since the Cambrian period with further sub-divisions of those units. The division of these sequences were originally constructed in the Appalachian Basin and Cordilleran Basin of North America.
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In terms of origin, oceans and continents have certain differences. Generally, the materials which constitute the ocean bottom are harder and heavier than those which constitute the continents. Though the interior of the earth is still in a hot and molten state, it is still undergoing contraction.
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