Dating methods in archaeology help establish chronologies of past human activity by determining the age of artifacts, structures, and environmental changes. There are two main categories:
Relative Dating – Determines the sequence of events but not the exact age.
Absolute Dating – Provides a specific age or range in years.
Based on the principle that deeper layers (strata) are older than upper layers.
Useful for sites with undisturbed soil layers like caves or riverbeds.
Typology: Comparing artifact styles (e.g., pottery, tools) to known historical examples.
Seriation: Arranging artifacts in a sequence based on changes in style or decoration over time.
Measures the amount of fluorine absorbed by bones from groundwater.
Used for comparing bones at a site but doesn’t give an exact date.
Measures carbon-14 decay in organic materials (wood, bone, charcoal).
Used widely in prehistoric archaeology but less effective for very old sites.
Uses growth rings in trees to date wooden artifacts or structures.
Very precise but requires overlapping sequences of ancient wood.
Used to date volcanic rock by measuring potassium-40 decay.
Essential for dating early human fossils in Africa.
Measures trapped electrons in heated materials (pottery, burnt stone).
Useful for dating ancient ceramics or fire pits.
Dates sand and soil by measuring the last time they were exposed to sunlight.
Used in prehistoric sites and buried landscapes.
Measures uranium decay in cave formations (stalactites, stalagmites) and bones.
Used in Neanderthal and early human sites.
Organic materials (wood, bone) → Radiocarbon dating
Volcanic rock → Potassium-Argon dating
Pottery, burned objects → Thermoluminescence
Wooden structures → Dendrochronology
Buried sand layers → Optically Stimulated Luminescence
Relative vs Absolute dating
Stratigraphic dating
Potassium Argon dating
Stratigraphy Excercise.