Relative and chronometric dating methods shanghai expat online dating
In relative dating, the temporal order of a sequence of events is determined, allowing the investigator to surmise whether a particular object or event is older or younger than, or occurred before or after, another object or event.
In absolute or chronometric dating, the investigator establishes the age of an object or event in calendar years.
Studying the layers of rock or strata can also be useful. If a layer of rock containing the fossil is higher up in the sequence that another layer, you know that layer must be younger in age. This can often be complicated by the fact that geological forces can cause faulting and tilting of rocks.
Absolute dating is used to determine a precise age of a rock or fossil through radiometric dating methods.
While people are most familiar with carbon dating, carbon dating is rarely applicable to fossils.
However, as the basic principles of relative dating progressed during the course of the 19th cent., investigators were able to correctly determine the relative age of many archaeological and geological materials.
Stratigraphic dating is accomplished by interpreting the significance of geological or archaeological strata, or layers.
The method begins with the careful drawing and description of strata (the geological or archaeological profile).
The profile from one location is then compared with profiles from surrounding sites.
Scientists can use certain types of fossils referred to as index fossils to assist in relative dating via correlation.