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.
More Definitions
Offset Printing
A printing technique in which an inked image is impressed on a rubber cylinder or blanket through a printing plate…
Slit Weave
Also known as slit tapestry, it is a weaving technique which uses multiple weft yarns through sections of the warp,…
Twill Weave
A weave in which the weft is passed over and then under multiple warp threads in a repetitive sequence. It…
Mukaish
A variant of badla embroidery in which metallic wires are sewn onto the fabric with the help of a needle…
Double-Interlock
A technique of tapestry weaving wherein two differently coloured weft threads interlock on a single warp thread. This method allows…
Photomontage
A process of creating collages of photographs to create a composite image. It was frequently used in movements such as…
Size
A solution that is applied to warp threads before they are set on a loom for weaving, it protects the…
Inlay
An ornamentation technique in sculpture and the decorative arts, where wood, metal, stone and fabric are embedded with different materials…