OPTICALLY STIMULATED LUMINESCENCE. A method of dating soil sediments and can be used to date deposits up to 200 000 years old. All soils contain traces of minerals, including uranium, thorium and potassium. These slowly decay over time and the ionising radiation they produce is absorbed by quartz and feldspar. Stimulating samples using infrared light causes luminescence, the intensity of which varies depending on the amount of radiation absorbed. Exposure to sunlight resets the luminescent signature and so the time period since the soil was buried by later sediments can be calculated. Wind blown, rainwashed and soil creep deposits are particularly suitable for OSL dating, and unlike radiocarbon dating, the technique does not require organic samples. It is more reliable and can be used on older deposits than radiocarbon dating and therefore is most suitable for use by archaeologist on prehistoric sites.