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Figure 2. How relative dating of events and radiometric (numeric) dates are combined to produce a calibrated geological time scale. In this example, the data demonstrates that "fossil B time" was somewhere between and million years ago, and that "fossil A time" is older than million years ago.

Relative Geologic Dating

4 methods of relative dating

4 methods of relative dating

General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled. They are widespread in rocks as old as 3. Coral generally grows at rates of around 1 cm per year, and these layers are easily visible. The different types of layers are summarized in Table III. Whether there's a data point on the Y-axis or not, the Y-intercept of the line doesn't change as the slope of the isochron line does as shown in Figure 5.

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4 methods of relative dating

4 methods of relative dating

General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled. They are widespread in rocks as old as 3. Coral generally grows at rates of around 1 cm per year, and these layers are easily visible. The different types of layers are summarized in Table III. Whether there's a data point on the Y-axis or not, the Y-intercept of the line doesn't change as the slope of the isochron line does as shown in Figure 5. 4 methods of relative dating

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Relative Geologic Dating