Name: Acanthite on Electrum (G-038)
Brand: Weinrich Minerals
Price: 1200 USD
Availability: InStock

Acanthite on Electrum (G-038)

Free shipping
Seller offers an extended return window of up to 14 days
Ships from USA

A cluster of electrum wires, these hosting micro sparkling metallic crystals of acanthite. Superb miniature for the locality, in great condition. The Fresnillo mining district, located in the central portion of the State of Zacatecas, Mexico, is an immensely productive, world-class underground operation primarily extracted for silver alongside significant lead, zinc, and gold. Geologically, the deposit is a major epithermal vein and stockwork system hosted within a complex sequence of Cretaceous sedimentary and volcanic rocks, including the Proano Group limestones and greywackes, which were heavily fractured and intruded by Tertiary felsic dikes. Hydrothermal fluids migrating through these fault networks deposited rich bands of base and precious metal sulfides, notably argentite, acanthite, galena, and sphalerite, making it one of the largest continuous silver accumulations on Earth. Discovered by Spanish explorers in 1554, small-scale silver extraction began almost immediately, but modern corporate industrialization took off in 1831 with the founding of the Zacateco-Mexicana company. The district experienced various operational phases, including a major revival by the Mexican Corporation in 1919 and subsequent long-term development by the Fresnillo Company, which transitioned the site into a massive, highly mechanized underground complex that continues continuous commercial production through recent years under Fresnillo plc. Electrum is a naturally occurring alloy of gold and silver, typically containing variable amounts of copper and other trace metals, that has been utilized since antiquity for coinage and jewelry. Geologically, it forms in low-temperature epithermal vein environments and orogenic gold deposits where hydrothermal fluids deposit the alloy within quartz veins alongside pyrite, chalcopyrite, and sphalerite. To be classified mineralogically as electrum rather than silver-bearing gold, the silver content generally ranges between twenty and fifty percent, a composition that directly dictates its physical properties by lowering its melting point and imparting a distinctive pale yellow to yellowish-white metallic luster. Historically, the ancient Greeks referred to it as white gold, and its first major economic use occurred in Asia Minor around 600 BC, when the Kingdom of Lydia minted the western world's first standardized coins using electrum nuggets washed down from the Pactolus River.