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Well, there are a variety of ways to "date" rocks and fossils. The easiest way is to examine samples above and below the sample in question, and come up with an age relative to those. For example, rock layers a, b, and c are in order with a at the top and c at the bottom. As long as the layers are relatively undisturbed, rock layer c, and therefore the fossils within it, are older than the ones in layer b, which in turn are older than the ones in layer a. This is called the "Principle of Superposition," and it holds true as long as there has been minimal folding, tilting, or faulting of rock layers, which is a form of unconformity. Beyond that, you can use what's called "radiocarbon dating," which utilizes the ratio between isotopes of a certain element within the rock sample which have gradually changed over time. This is a complicated procedure which must be carried out with carefully calibrated and computerized scientific equipment, but the results can be quite accurate relative to the great age of the sample.

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Q: How do geologists make their jobs easier when it comes to dating fossils and rocks?
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There are a number of ways to tell the age of a rock. Some rocks contain radioactive elements, such as thorium or uranium, which have known half lives (a half life being the amount of time that it takes for half of a given sample to decay) and by analyzing relative quantities of the various isotopes present in the rock, it is possible to figure out how long it took them to reach their present state. There is also stratigraphic analysis, which determines in which layer the rock appears, when there are means of dating the various layers by means of processes that happen at a known speed (erosion, deposition of microscopic shells, etc.).


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