Relative dating methods estimate whether an object is younger or older than other things found at the site. Relative dating does not offer specific dates, it simply allows to determine if one artifact, fossil, or stratigraphic layer is older than another.
Relative dating is used to arrange geological events, and the rocks they leave behind, in a sequence. Next time you find a cliff or road cutting with lots of rock strata, try working out the age order using some simple principles: Sedimentary rocks are normally laid down in order, one on top of another.
What is relative dating and how can it be determined?
Relative dating is the process of determining if one rock or geologic event is older or younger than another, without knowing their specific ages—i.e., how many years ago the object was formed.
What are the pros of relative dating?
Dating rocks using relative dating allows a geologist to reconstruct a series of events cheaply, often very quickly, and can be used out in the field on a rocky outcrop. Relative dating also can be used on many different types of rocks, where absolute dating is restricted to certain minerals or materials.