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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Amli
Also known as amlikar, it is a needle-embroidered Kashmiri shawl dating to the nineteenth century. While it is likely to…
Calotype
An early photographic technique invented by William Henry Fox Talbot, who patented it in 1841. Also known as talbotype, the…
Weft
It refers to yarn or threads that pass horizontally over and under the fixed longitudinal warp to weave cloth and…
Collagraph
A printmaking technique in which colour is applied to a printing surface covered with different materials and texture, then transferred…
Kani
A term referring to both the weaving technique and the final textile created by this method. It may also refer…
High Relief
Also known as alto-relievo, it is a technique of relief sculpting where the image projects significantly from the ground. The…
Slit Weave
Also known as slit tapestry, it is a weaving technique which uses multiple weft yarns through sections of the warp,…
Linocut
A printmaking process in which a design is carved in relief on a sheet of linoleum, then inked. The sheet…