What is relative dating geology
Most commonly, the ancient factors of the rocks or objects are examined using the method called stratigraphy.In other words, we can say that the age in the relative dating is ascertained by witnessing the layers of deposition or the rocks.
For example, rocks of the Phanerozoic eon are found on top of rocks from the Proterozoic eons therefore rocks of the Phanerozoic are younger than rocks of the Proterozoic.
Relative time places events or formations in order based on their position within the rock record relative to one another using six principles of relative dating.
Relative time can not determine the actual year a material was deposited or how long deposition lasted; it simply tell us which events came first.
In the field of Geology, dating is an important term as it is a technique through which evaluation regarding the age and period about the fossil, remains, the archaeologists do valuables and artifacts.
At first, there were not many methods of dating were available, but now with advancement in the technology, we mainly have two types of the techniques to ascertain ages of ancient belongings.
This evaluation of the rocks and fossils in the relative dating is known as the biostratigraphy.