Teaching radiometric dating

For example, in the rocks exposed in the walls of the Grand Canyon (Figure 1) there are many horizontal layers, which are called strata.

The study of strata is called stratigraphy, and using a few basic principles, it is possible to work out the relative ages of rocks.

In the Grand Canyon, the layers of strata are nearly horizontal.

Most sediment is either laid down horizontally in bodies of water like the oceans, or on land on the margins of streams and rivers.

There are three general approaches that allow scientists to date geological materials and answer the question: "How old is this fossil?

" First, the relative age of a fossil can be determined.

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.

Mountains have been built and eroded, continents and oceans have moved great distances, and the Earth has fluctuated from being extremely cold and almost completely covered with ice to being very warm and ice-free.

These changes typically occur so slowly that they are barely detectable over the span of a human life, yet even at this instant, the Earth's surface is moving and changing.

However, by itself a fossil has little meaning unless it is placed within some context.

The age of the fossil must be determined so it can be compared to other fossil species from the same time period.

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