A method of determining the objective age of carbon-based materials by measuring the amount of carbon-14, formed when the nitrogen of radiocarbon decays, against an internationally used standard reference. William F Libby is credited with developing the method in 1946. It is used widely in disciplines such as archaeology and other natural sciences to determine the age of biological specimens and artefacts.
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Gilt
An object that is covered with a thin layer of gold, often used in jewellery, ornamentation and textile. From the…
Hand Stencil
The technique of imprinting human hands on rock surfaces, found in Prehistoric cave paintings. The process involves placing one hand,…
Japanese Ink Wash Technique
Known as sumi-e (black ink painting) in Japanese, it is a painting technique that uses black ink in water in…
Tapestry Weave
A weft-facing technique of weaving, wherein coloured weft yarns are interlaced with plain-coloured warp. The design is created using the…
Weft
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Screen-Printing
Also known as serigraphy and silk-screen printing, it is a stencil-based technique of printing on a substrate such as paper…
Fluting
Decorative ridges or grooves that are carved along the shaft of a column or pilaster to make it appear rounder…
Somak Weaving
A flat-weave tapestry weaving technique where weft yarns are wrapped over four warp threads before being twisted back under the…