4 types of absolute dating

Suppose a dinosaur fossil has been found in the beds of an ancient delta (the mouth of a river leading to the sea).

The sediment of this area was laid down after ammonite A appeared 199 million years ago, and before ammonite B became extinct 195 million years ago.

The simplest and most intuitive way of dating geological features is to look at the relationships between them.

There are a few simple rules for doing this, some of which we’ve already looked at in Chapter 6.

All rocks and minerals contain long-lived radioactive elements that were incorporated into Earth when the Solar System formed.

These radioactive elements constitute independent clocks that allow geologists to determine the age of the rocks in which they occur.

This is because new sediments are always laid down on top of sediments that have already been deposited.As radioactive Parent atoms decay to stable daughter atoms (as uranium decays to lead) each disintegration results in one more atom of the daughter than was initially present and one less atom of the parent.The probability of a parent atom decaying in a fixed period of time is always the same for all atoms of that type regardless of temperature, pressure, or chemical conditions. The time required for one-half of any original number of parent atoms to decay is the half-life, which is related to the decay constant by a simple mathematical formula.This narrows the date of the delta beds to the four million years between these dates.There are some radioactive elements in rock that decay by giving off energy and turning into different, more stable elements.

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