Seriation stratigraphy and index fossils the backbone of archaeological dating

Historical Continuity, Heritable Continuity, and the Study of Artifacts.

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It is difficult for today's students of archaeology to imagine an era when chronometric dating methods were unavailable.

However, even a casual perusal of the large body of literature that arose during the first half of the twentieth century reveals a battery of clever methods used to determine the relative ages of archaeological phenomena, often with considerable precision.

Stratigraphy is the study of layered materials (strata ) that were deposited over time—their lateral and vertical relations, as well as their composition.

The basic law of stratigraphy, the law of superposition, states that lower layers are older than upper layers, unless the sequence has been disturbed.

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Seriation I: Historical Continuity, Heritable Continuity, and Phyletic Seriation.

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