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Scientific dating methods in archaeology

scientific dating methods in archaeology-33

Layers that cut across other layers are younger than the layers they cut through (principle of cross-cutting relationships).The principle of superposition builds on the principle of original horizontality.

You can also view the archaeologist categorized on the basis of country by using the link above.The age of the fossil must be determined so it can be compared to other fossil species from the same time period.Understanding the ages of related fossil species helps scientists piece together the evolutionary history of a group of organisms.Third, magnetism in rocks can be used to estimate the age of a fossil site.This method uses the orientation of the Earth's magnetic field, which has changed through time, to determine ages for fossils and rocks.A fossil can be studied to determine what kind of organism it represents, how the organism lived, and how it was preserved.

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

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

Just as when they were deposited, the strata are mostly horizontal (principle of original horizontality).

Museums enable people to explore collections for inspiration, learning and enjoyment.

They are institutions that collect, safeguard and make accessible artifacts and specimens, which they hold in trust for society.

Layers of rock are deposited horizontally at the bottom of a lake (principle of original horizontality).