Bertram boltwood radiometric dating

At the turn of the nineteenth century, William Smith (1769-1839), an English canal engineer, observed that certain types of rocks, along with certain groups of fossils, always occurred in a predictable order in relation to each other.

In 1815, he published a map of England and Wales geology, establishing a practical system of stratigraphy, or the study of geologic history layer-by-layer.

In most cases, a boundary is drawn to represent a time when a major catastrophe or evolutionary change in animals or plants (including the evolution of specific species) occurred.

Natural erosion clearly reveals the layers of Earths crust, such as seen here in Badlands National Park in South Dakota.

The eon represents the longest geologic unit on the scale; an era is a division of time smaller than the eon, and is normally subdivided into two or more periods.

This unambiguously showed that the age of the earth had to be at least 2 billion years, to the considerable relief of evolutionary biologists and most geologists. The uranium mineral boltwoodite was named in his honor in 1956.It is based on the location of a rock layer in comparison to the location of other rock layers; that is, it is only relative, not absolute, time.In many cases, rock layers are laid down in order, the older layers being below the younger layers.Smiths work, combined with the first discoveries of dinosaur fossils in the early 1800s, led to a framework that scientists still use today to divide Earths long history into the geologic time scale, with its various, arbitrary divisions of time including eras, periods, and epochs.Established between 18, the time divisions are a relative means of dating; that is, rocks and fossils are dated relative to each other as to which are older and younger.

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It was not until radiometric dating was invented in the 1920s that absolute dates were applied to rocks and fossils and to the geologic time scale.

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