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Luminescence dating is a technique used to date Quaternary sediments and for determining when ancient materials such as pottery, ceramics, bricks or tiles were last heated.

The technique can be applied to material from about 100 to several hundred thousand years old.

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The laboratory is set up in dark rooms with extremely subdued orange illumination.

One room serves as preparation laboratory, where all incoming samples are unpacked and chemically treated to purify the sample and extract the desired minerals in the right grain size.

Identify a suitable sediment outcrop – ideally a sandy/silty consistency2.

Cut back the surface of the outcrop by about 20 cm to expose fresh material3. Slip Rate on the Wellington Fault, New Zealand, during the Late Quaternary: Evidence for Variable Slip during the Holocene.

We are also involved in research projects requiring gammaspectrometry.

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