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Robinson Mine

The Robinson Mine is a porphyry copper deposit located at Ruth, White Pine County, Nevada, in the Egan Range, 4 miles (6.4 km) west of Ely. The mine comprises three large open pits: Liberty, Tripp-Veteran and Ruth. The ore is extracted using conventional surface methods, and is then processed into a copper-gold concentrate, and a molybdenum concentrate in a concentrating plant. Since 2012 the mine has been owned and operated by Polish copper miner KGHM Polska Miedź

History and current operations
Around 1868, prospector Thomas Robinson discovered gold and silver, along with widespread, low-grade copper, in what became the Robinson Mining District. From around 1892 to 1907, several gold mines were opened, but none were successful. Around 1907, interest turned towards copper. Under Daniel C. Jackling, in 1905 Nevada Consolidated Copper Corporation (Nevada Con) began copper mining in the Veteran Mine. "The resulting mine was an impressive open-pit and satellite cave." During World War I and until the Great Depression, Nevada Con employed some 1000 - 1200 men in their mines. Mining ended around 1949. Future production would come from open-pit mining. In 1932, Nevada Con became a wholly owned subsidiary of Kennecott Copper, another Guggenheim-controlled company. In September 1978, Kennecott closed its Nevada mines, and in 1983 the McGill smelter was also closed. and cuprite in a high-grade copper ore specimen from the Robinson Mining District. Magma Copper bought Robinson in 1991 and began work on reopening the mine in 1994. In 1996, BHP acquired Magma, and operated Robinson from 1996 to 1999. Magma/BHP invested around $480 million in the mine and plant. The mine was closed in 1999 due to low copper prices. Quadra Mining bought Robinson in 2004, and reopened the mine later that year. Since 2005, production has averaged about 125 million pounds of copper per year. In 2012, Quadra was acquired by KGHM Polska Miedź, a large Polish copper producer. As of December 2017, the Robinson Mine had 605 employees. ==Geology==
Geology
Paleozoic limestones, shales and sandstones were intruded in the Cretaceous by a quartz monzonite porphyry. This intrusion metamorphosed the surrounding sediments creating a tactite zone in the altered limestone up to 150 meters away, producing porphyry ores with traces of gold. Chalcopyrite is the primary ore mineral, which may be altered to chalcocite. File:Ely Mine Locations.PNG|Geology map of the Ruth area showing alteration zone, copper and gold mineralized areas, and the Veteran, Trapp, Liberty and Ruth open pits (l-r) File:Ely Mine Locations 3.PNG|Key: Alteration and mineralization areas File:Ely Geology Part 1.PNG|Solid geology map of the Ruth area File:Ely Geology Part 3.PNG|Key: Solid geology map File:Ruth Cross Section.PNG|Ruth pit cross section File:Ruth Cross Section Index.PNG|Key: Ruth pit cross section ==References==
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