Step-by-step explanation:
Numerical dating and relative dating are two methods used in geology and archaeology to determine the age of rocks, fossils, and other geological or archaeological materials.
Relative dating is a method of determining the relative order of events or materials in time, without necessarily determining their absolute age. It involves comparing the ages of different rocks or materials relative to one another based on their position in the rock layers or their physical properties. The most commonly used methods of relative dating include stratigraphy, which involves studying the layers of rock and their sequence of formation, and the principle of superposition, which states that the oldest layer is at the bottom and the youngest layer is at the top.
Numerical dating, on the other hand, is a method of determining the actual age of rocks or materials in years, using various scientific techniques such as radiometric dating or dendrochronology. This method provides a more accurate and precise estimate of the age of a rock or material compared to relative dating.
In summary, relative dating provides an approximate order of events or materials in time, while numerical dating provides a more precise estimate of the actual age of rocks or materials in years