Split bracelet made of Malachite from Congo formerly Zaire

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"Always fits" bracelet made of gemstone chips. Beautiful, thick 5 to 10 mm chips. All beautifully cut and polished. A very attractive, matching bracelet.

Article number: 2724 Categories: ,

Description

Malachite is a mineral used as a gemstone. It is a copper carbonate with the chemical formula Cu2CO3(OH)2. It is often found in nature together with the related azurite (Cu3(CO3)2(OH)2). The crystal structure is monoclinic and usually botryoidal. The mineral's name comes from Greek and refers to the color of the mallow plant. Malachite was used as a gemstone from early times. In Egypt, cameos, amulets, and ornaments were made from it. The Greeks and Romans also knew malachite. The pulverized mineral was used as makeup and as a dye. It was said that malachite could protect children from sorcery and witchcraft. In antiquity, it was believed to cure eye ailments. In the 16th century, it was used in Central Europe to promote growth in children and to relieve pain. Malachite is found worldwide. In Asia, significant quantities are found in China, India, and the Urals in Russia, as well as in Australia. On the American continent, the main deposits are located in the southwestern United States, primarily in Arizona (a 4.5-ton block was found near Bisbee). Malachites in Mexico, Chile, and Cuba are of gemstone quality. However, the most important and historically well-known malachite reserves are in Africa. Here, malachite has been mined since ancient times in the Copperbelt in the Democratic Republic of the Congo and Zambia. The malachite zone extends from Katanga Province (Democratic Republic of the Congo) to Zambia. These malachites are considered the finest and best in the world. Beautiful malachite crystals are found in Namibia (Tsumeb), Morocco, Zimbabwe, and Angola. Europe has only small, insignificant deposits in Germany, Slovakia, Hungary, Romania, England, and France. In Belgium, malachite is found in the Salm Valley and in limestone at Visé. Malachite is formed in oxidation zones of copper deposits.