Definition of relative dating geology

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Dating Fossils – How Are Fossils Dated?

Determining the age of rocks, and any fossils contained within the rocks, is an interesting and ongoing aspect of geology. There are several different ways that geologists can determine the age of rocks, and each method provides information about a slightly different aspect of the rock. Relative dating is when geologists determine the age of a rock or a layer of rocks in relation to the rocks around it. Relative dating does not Become a Study.

A method of determining the age of a fossil by comparing its placement with that of fossils in other layers of rock. Relative dating is the science determining the relative order of past events, without necessarily determining their absolute age. In geology rock or superficial deposits, fossils and lithologies can be used to correlate one stratigraphic column with another.

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An absolute age is one determined usually by mass-spectrometry where an isotope is measured and then an age can be calculated a very very basic explanation. So in the end you can say this fossil is 50 thousand years old always with an associated uncertainty. We can absolute date materials but it will always have an uncertainty range, we can never know the age with infinite precision. Relative dating is like looking at a multi-layered cake. The base layer must come first, then the second and then the third.

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Definition of relative age

Relative dating is used to arrange geological events, and the rocks they leave behind, in a sequence. The method of reading the order is called stratigraphy layers of rock are called strata. Relative dating does not provide actual numerical dates for the rocks.

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