Emeralds in antiquity were mined in
Ancient Egypt at locations on Mount Smaragdus since 1500 BC, and India and Austria since at least the 14th century AD. The Egyptian mines were exploited on an industrial scale by the Roman and Byzantine Empires, and later by Islamic conquerors. Mining in Egypt ceased with the discovery of the Colombian deposits. Today, only ruins remain in Egypt. Colombia is historically the world's largest producer of emeralds, with the quantity varying depending on the year, source, and grade. · For the decade leading up to 2005, Colombia accounted for 47 percent of global emerald output, but has declined due to several factors ranging from a lack of new discoveries to outdated mining technologies to global oversupply The three main emerald mining areas in Colombia are
Muzo, Coscuez, and
Chivor. Rare
"trapiche" emeralds are found in Colombia, distinguished by ray-like spokes of dark impurities.
Zambia is the world's second biggest producer, with its
Kafubu River area deposits (Kagem Mines) about southwest of Kitwe responsible for 20% of the world's production of gem-quality stones in 2004. · Kagem Mining Limited was the single largest producer of emerald in the country, producing 1,880 kg (9.4 million carats) of emerald and beryl in 2020. Zambian emeralds fall within the bluish green to green range, superior transparency, and fewer inclusions compared to the heavily fractured Colombian varieties, which are prized mainly for their intense hue. Emeralds are found all over the world in countries such as Afghanistan, Australia, Austria, Brazil, Bulgaria, Cambodia, Canada, China, Egypt, Ethiopia, France, Germany, India, Kazakhstan, Madagascar, Mozambique, Namibia, Nigeria, Norway, Pakistan, Russia, Somalia, South Africa, Spain, Switzerland, Tanzania, the United States, Zambia, and Zimbabwe. In the US, emeralds have been found in
Connecticut,
Montana,
Nevada,
North Carolina, and
South Carolina.
Origin determinations Since the onset of concerns regarding diamond origins, research has been conducted to determine if the mining location could be determined for an emerald already in circulation. Traditional research used qualitative guidelines such as an emerald's color, style and quality of cutting, type of fracture filling, and the anthropological origins of the artifacts bearing the mineral to determine the emerald's mine location. More recent studies using
energy-dispersive X-ray spectroscopy methods have uncovered trace chemical element differences between emeralds, including ones mined in close proximity to one another. American gemologist David Cronin and his colleagues have extensively examined the chemical signatures of emeralds resulting from fluid dynamics and subtle precipitation mechanisms, and their research demonstrated the chemical homogeneity of emeralds from the same mining location and the statistical differences that exist between emeralds from different mining locations, including those between the three locations: Muzo, Coscuez, and Chivor, in Colombia, South America. == Synthetic emerald ==