An example of relative dating is observed where a rock outcrop shows three and flat-lying layers of rock when the lowest layer is the oldest while the top layer is the youngest.
In geological event, this refers to the method used to arrange geological events and the rocks they leave behind in a sequence.
This methods is one that helps to estimate whether an object is younger or older than other things found at the site such as the determination of if an artifact, fossil or stratigraphic layer is older than another.
This scientific method of reading the order is known as stratigraphy because the layers of rock are called strata, however, the relative dating does not provide actual numerical dates for the rocks.
Hence, the example of relative dating is observed where a rock outcrop shows three and flat-lying layers of rock when the lowest layer is the oldest while the top layer is the youngest.
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