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" First, the relative age of a fossil can be determined.
The samples of both the locations will be of the same age.
Geologists have established a set of principles that can be applied to sedimentary and volcanic rocks that are exposed at the Earth's surface to determine the relative ages of geological events preserved in the rock record.
If the layers of sediments deposited is continuous then we will find all the layers of sediment throughout the basin provided the basin is geologically undisturbed.
The relative age for the respective layers will be the same.
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