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How Archaeologists Get a Date

How Archaeologists Get a Date
A Valentine’s Day blog post 

Archaeologists like to use several dating methods to find out more about artifacts. It all depends on what the object is, where the archaeologist is located (what resources he/she has access to), and how old the artifact appears to be.

What is eligible for dating?
Not every artifact is eligible for all dating methods; for example, an artifact must be made from a carbon-based material to use radiocarbon dating (stone, for example doesn’t have carbon).  A stone artifact can be dated based on the way it looks and/or the way it was made.  Over many years of research chronologies of stone tools (and pottery) have been built, based on styles (called Seriation).

Archaeologists can also be matchmakers by using the context, which is the where, when and how an artifact is found. In the end, archaeologists often use a few different methods on an group of artifacts found together to come up with a reasonable date.

CarbonDating - How Archaeologists Get a Date


Relative Dating:  Doesn’t mean an archaeologist is dating his Aunt Betty….
Relative dating gives you the age of an artifact in relation to another object.
– Objects found deeper in the ground are older (law of superposition)
– Type dating (Seriation): types of artifacts are arranged chronologically according to style. Type dating can be done with modern cars to stone tools.
Fluorine dating: bones buried at the same time will absorb the same amount of fluorine from the soil which means they must be the same age.

Calendar dating: According to the New York Times, the best day to go on a date is Wednesday….
– Absolute dating: Only possible with objects that have dates inscribed on them (ie: coins)
Chronometric dating: Measures the time since something has elapsed.

– Radiocarbon dating: This method is based on the radioactive decay of carbon-14 isotope (14C). When a carbon-based organism dies, any 14C absorbed during its life begins radioactive decay at a rate measured by “half-life” (how long it takes half of it to decay). 14C has a half life of 5,730 years. A mass spectrometer is used to measure how much of the half life is left and calculates the time that has elapsed since it died. Problem: it has been discovered that levels of 14C in the atmosphere fluctuated in the past but has been calibrated by comparison to dendrochonological records. Archaeologists & physicists can only date organisms as old as 50,000 years with this method.

Tree-ring dating (dendrochronology): Here’s a cheesy pick up line you’re welcome to use: “You may fall from the sky, you may fall from a tree, but the best way to fall… is in love with me.”
Dating based on growth rings of a tree. Archaeologists can find the specific year a tree was cut to make a wooden object. (This requires enough wood in an artifact to see the rings.)

Potassium-argon: “Do you have a K-Ar? because you Auto be my Valentine.” (That was a bit of a stretch!)
This method measures the radioactive decay of potassium into argon gas. It has a “half life” of 1.31 billion years but the artifact needs to have the required minerals (such as mica, clay minerals, tephra, and evaporites).

Archaeomagnetism: Archaeologists are so attracting!
Iron particles in heated soil align themselves with the poles. The North Pole’s magnetic field shifts at a known rate so archaeologists can measure the magnetic alignment in the ground and compare it with today’s alignment.

– Thermoluminescence dating: This is where things get really hot! 😉
Measures the accumulated radiation dose of the time since the artifact containing crystalline mineral was heated (ceramics) or exposed to sun.

Other methods:
Lead corrosion
– Amino Acid
– Varve
– Rehydroxylation
Obsidian hydration
– Optically stimulated luminescence

White, Nancy Marie. Archaeology for Dummies. Hoboken, NJ : Wiley Publishing, Inc., 2008. Print.