Answer :
The purpose of relative age dating is to establish the chronological sequence of previous occurrences on Earth. The ideas of superposition and cross-cutting connections are two of the most significant of the few straightforward principles used by geologists in relative age dating.
Without necessarily determining their absolute ages, relative age dating is the science of figuring out the relative sequence of historical events (i.e., the age of an object in comparison to another) (i.e., estimated age). In geology, one stratigraphic column can be correlated with another using rock or surface deposits, fossils, and lithologies. Prior to the early 20th century discovery of radiometric dating, which offered an absolute dating method, archaeologists and geologists utilized relative dating to ascertain the ages of materials. Relative dating is nevertheless a helpful technique even though it can only tell you the order in which a set of events happened, not when they did. In certain ways, relative dating via biostratigraphy is more accurate and is the method of choice in paleontology. The main result of "relative dating" as observed in geology from the 17th century to the early 20th century was the Law of Superposition, which asserts that older strata would be deeper in a site than more recent layers.
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