Eagle Mine

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Gilman, Gilman Mining District (Battle Mountain Mining District; Red Cliff Mining District), Eagle County, Colorado, USA

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Key Information

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  • The Eagle Mine is located in Gilman, Eagle County, Colorado, about one mile southeast of Minturn and eight miles southwest of Vail, in the Rocky Mountains at 8,000 feet elevation.

  • It produced significant amounts of zinc, lead, silver, copper, gold, and manganese, with notable specimens like pyrite and siderite crystals prized by collectors.

  • The mine's geological structure features sedimentary rocks with replacement deposits in dolomites and quartzite, formed through hydrothermal processes.

  • Mining began in the 1880s, peaking with zinc production, and closed in 1984 due to environmental and economic issues, leaving Gilman as a ghost town.

  • The area has a montane climate with cold winters and mild summers, and mining impacted the local ecology, notably contaminating the Eagle River.

Location and Geography

The Eagle Mine is situated in the Gilman Mining District, also known as the Battle Mountain or Red Cliff Mining District, in Eagle County, Colorado. It lies about one mile southeast of Minturn and eight miles southwest of Vail, nestled in the Rocky Mountains at an elevation of approximately 8,000 feet. The nearby town of Gilman, now a ghost town, was abandoned in 1984 due to environmental concerns and the mine's closure. For mineral enthusiasts, nearby localities within the district, such as the Iron Mask, Belden, Black Iron, and Little Chief mines, offer additional exploration opportunities.

Minerals and Geological Insights

The mine is renowned for producing zinc, lead, silver, copper, gold, and manganese, with historical production figures including 400,000 ounces of gold, 67.6 million ounces of silver, 212 million pounds of copper, 317 million pounds of lead, 1.868 billion pounds of zinc, and 200,000 tons of manganiferous iron ore. For collectors, the Eagle Mine is particularly noted for exceptional specimens like large pyrite crystal groups and freibergite-tetrahedrite-chalcopyrite combinations, considered classics from Colorado. The geological structure consists of sedimentary rocks from the Precambrian to Pennsylvanian periods, with a porphyry intrusion, featuring replacement deposits in dolomites of Mississippian and Devonian age and quartzite of Cambrian age, formed through hydrothermal processes likely related to magmatic activity.

Mining History and Cultural Context

Mining at the Eagle Mine began in the 1880s, initially for gold and silver, but later focused on zinc, lead, and copper. Owned by the New Jersey Zinc Company, a subsidiary of Gulf+Western, and later Viacom International, it was a major producer until its closure in 1984 due to environmental contamination and economic unprofitability. The town of Gilman, built as a company town, supported a peak population of 1,000 during World War II, with its own school, newspaper, and amenities. Today, it stands as a ghost town, off-limits to the public, with its dramatic cliffside location overlooking the Eagle River adding to its allure. While no famous individuals or events are directly tied to the mine, its history as a self-contained mining community is a fascinating chapter for enthusiasts.

Climate and Ecological Impact

The area has a montane climate with cold winters and mild summers, typical of the Rocky Mountains at 8,000 feet. The mining activities have significantly impacted the local ecology, particularly through contamination of the Eagle River with heavy metals like arsenic, cadmium, copper, lead, and zinc, highlighting the environmental legacy of the operations.