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Thermoluminescence dating is very useful for determining the age of pottery. Electrons from quartz and other minerals in the pottery clay are bumped out of their normal positions ground state when the clay is exposed to radiation. This radiation may come from radioactive substances such as uraniumpresent in the clay or burial medium, or from cosmic radiation. The longer the exposure to the radiation, the more electrons that are bumped into an excited state, and the more dating light that is emitted upon heating.

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Thermoluminescence can be used to date materials containing crystalline minerals to a specific heating event.

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This is useful for ceramics, as it determines the date of firing, as well as for dating light, or even sediments that were exposed to substantial sunlight. These crystalline solids are constantly subjected to ionizing radiation from their environment, which causes some energized electrons to become trapped in defects in the molecular crystal structure.

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An input of energy, such as heat, is required to free these trapped electrons. When a specimen is reheated, the trapped energy is released in the form of light thermoluminescence as the electrons escape.

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The amount of light produced is a specific and measurable phenomenon. Because this accumulation of trapped electrons begins with the formation of the crystal structure, thermoluminescence can date crystalline materials to their date of formation; for ceramics, this is the moment they are fired.

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The major source of error in establishing dates from thermoluminescence is a consequence of inaccurate measurements of the radiation acting on a specimen. The complex history of radioactive force on a sample can be difficult to estimate. However, dating light proven acceptable in providing approximate dates in the absence of more exact measures.

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Thermoluminescence Dating Thermoluminescence can be used to date materials containing crystalline minerals to a specific heating event. Michels, Joseph.

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