The underlying physics begins in the kiln. When a clay vessel is fired at high temperature, the magnetic particles embedded in the clay are heated beyond their ability to hold any prior magnetic record. As the pot cools, these particles align themselves with the Earth’s magnetic field prevailing at that moment, and once cooled below a critical temperature, the alignment becomes permanently fixed. This permanent record is known as thermal remanent magnetism. For a pot made today, that record points toward today’s magnetic north pole; for a rock that cooled 800,000 years ago, when the Earth’s field was reversed, the tiny magnetic crystals point toward the south pole. In principle, this imprint offers a timestamp of the original firing.

In practice, however, the direction of a magnetic signal alone cannot reveal a sample’s age, because the recorded direction depends entirely on how the object happened to be oriented as it cooled. Hold a sherd one way and its signal appears to point north; rotate it and the same signal seems to point south or in any number of other directions. Archaeologists have long used magnetic direction and intensity to date in-place features such as hearths and walls, where orientation is known, but a loose pot on a dealer’s table offers no such reference frame. Forgers, meanwhile, have grown increasingly sophisticated, and museums have lacked a reliable laboratory test that works on an object of unknown orientation and uncertain provenance.

The Scripps team’s breakthrough came from separating two distinct kinds of magnetism that coexist in fired clay. The first, thermal remanent magnetism, is carried by the larger magnetic particles, whose signals settle permanently into the direction of the field at the time of firing and remain trapped there essentially forever. The second, called viscous remanent magnetism, is carried by the smallest particles, whose magnetic moments never fully stabilize. Instead, these tiny grains continually re-equilibrate with the ambient geomagnetic field, so their magnetism drifts and fluctuates over time in response to the field’s slow changes. Crucially, this viscous component is the part that accumulates after manufacture, and it is the part that can be erased and reset by reheating.

That erasability is the key to the new test. When pottery is reheated in the laboratory, the viscous remanent magnetization can be wiped away, and the temperature required to erase it depends on how long the material has been sitting in the Earth’s field. The newer the pottery, the lower the temperature needed to reset its viscous signal. The researchers exploited this relationship by heating a variety of pottery objects at progressively higher temperatures, starting at 50 degrees Celsius and increasing in increments of 10 degrees. Their sample set included vessels known to be thousands of years old, souvenir pottery purchased in shops around Jerusalem, and objects already known to be fakes.

The results revealed a clear and statistically significant divide between modern and ancient material. Samples older than roughly 1,000 years retained their viscous magnetization until temperatures rose above 112 degrees Celsius, whereas modern samples lost their viscous signal at lower temperatures. In other words, the viscous component of an ancient pot carries a distinct thermal threshold, a kind of magnetic timestamp that a recently fired forgery simply cannot reproduce. A forger who bakes clay today, no matter how carefully the vessel is styled or artificially aged, produces a viscous magnetization profile characteristic of the present day, and the new method detects that discrepancy directly.

Establishing the 112-degree threshold required more than laboratory heating experiments. The team supplemented their measurements with micromagnetic models that simulated the baking of hypothetical samples over varying spans of time, tracking how the viscous signal builds and decays in ensembles of magnetic grains. Such simulations are computationally demanding, and the authors note that computing power had long been insufficient to run them at the necessary resolution. Advances in processing capability finally made it possible to model the behavior of the smallest magnetic particles realistically, allowing the researchers to connect the laboratory observations to a quantitative criterion that can be applied to artifacts of unknown age.

The practical implications extend across several communities. Vaknin expressed hope that the method will serve museum curators who wish to display only authentic artifacts, archaeologists and historians studying the societies that created ancient objects, and law enforcement authorities working to eliminate the illicit antiquities trade, which involves both the looting of archaeological sites and outright forgery. The authors point out that a recent prosecution in Israel involving the sale of fake artifacts had failed because of a lack of conclusive evidence, underscoring how badly courts need an objective, physically grounded test. Because the method yields a measurable temperature threshold rather than a subjective judgment of style or surface patina, it has the potential to stand up as proof in forgery trials.

Co-author Lisa Tauxe, a geoscientist at Scripps, said the team’s technique could be a boon to museums and governments that need to stay one step ahead of forgers. Fakes, she noted, have been an enduring problem in Israel, China, Mexico, and almost every region of the world where archaeological dig sites are found, particularly in places where treachery abounds. The antiquities market is vast and often opaque, and objects can acquire convincing provenances through forged documentation alone. A laboratory test that interrogates the physical fabric of the artifact itself, independent of paperwork or stylistic opinion, offers a fundamentally different kind of evidence, one rooted in the immutable physics of magnetic grains and the slow drift of the geomagnetic field.

With the method now established, the researchers intend to apply it to artifacts of debated authenticity in museums around the world. The work, authored by Vaknin, Tauxe, former Scripps doctoral student Brendan Cych, and geoscientist Jeff Gee, was supported by funding from the U.S.-Israel Binational Science Foundation and the National Science Foundation. For a field that has long relied on connoisseurship, provenance records, and stylistic analysis to separate genuine antiquities from clever imitations, the ability to read a magnetic timestamp directly from fired clay marks a meaningful shift. Every ancient pot, it turns out, carries within its smallest grains a quiet record of the centuries it has spent in the Earth’s magnetic field, and for the first time, that record can be interrogated with enough precision to unmask a forgery.

Subject of Research: A magnetic dating method for authenticating ancient fired-clay artifacts

Article Title: Researchers develop method to tell authentic artifacts from fakes

Article References: Researchers develop method to tell authentic artifacts from fakes. (n.d.). Original publication

Image Credits: AI Generated

DOI: Not provided

Keywords: archaeology, pottery, forgery detection, magnetism, viscous remanent magnetization, thermal remanent magnetism, geomagnetic field, Scripps Institution of Oceanography, PNAS, antiquities trade, museum authentication, micromagnetic modeling