Cambokeels Mine (Cammock Isle Mine; Cumnock Isle Mine; Cammock Eals Mine)

Mindat.org

Westgate, Stanhope, County Durham, England, UK

Loading...

Key Information

Do not enter mining areas without proper authorization.

  • Cambokeels Mine is located in Weardale, County Durham, England, UK, between Eastgate and Westgate villages, on the north banks of the River Wear.

  • It is known for producing lead and fluorspar, with fluorspar being particularly notable for its colorful varieties.

  • The mine's geology features the Slitt Vein, primarily in limestone, with minerals formed through hydrothermal processes.

  • Mining began in 1847 for lead, shifted to fluorspar in 1906, and ceased operations in 1989, with various owners over time.

  • The area has a rich mining heritage, connected to the broader Weardale mining culture, but specific local cultural ties are less documented.

  • The climate is temperate, with wet conditions potentially influencing mineral formation, though direct links are not well-established.

Location and Nearby Sites

Nestled in the scenic Weardale Valley of County Durham, England, Cambokeels Mine lies between the quaint villages of Eastgate and Westgate, on the north banks of the River Wear. This region, part of northern England, is famous for its mining history and is a short drive from the historic city of Durham, known for its cathedral. Nearby, mineral enthusiasts might explore other notable sites like the Rookhope Arch, another significant mining area in Weardale, offering a glimpse into the region's rich geological past.

Minerals and Geology

Cambokeels Mine is celebrated for its lead and fluorspar deposits, with fluorspar standing out due to its vibrant colors, making it a favorite among collectors. The mine taps into the Slitt Vein, a geological feature within limestone, where minerals formed through hydrothermal activity, as hot fluids deposited them over time. This process created unique mineral specimens, adding to the mine's allure for crystal enthusiasts.

Mining History

Mining at Cambokeels started in 1847, initially focusing on lead, but poor yields led to its early struggles. It was revitalized in 1906 for fluorspar, changing hands multiple times, including ownership by Anglo-Austral Mines Ltd in the late 1940s and later by Swiss Aluminium UK Company. Operations expanded in the 1970s with new inclines discovering high-grade fluorspar, but the mine closed in 1989, leaving behind a legacy of industrial activity.

Culture and Climate

Weardale's mining heritage is deeply woven into local culture, with Cambokeels Mine contributing to the area's identity as a mining hub. While specific local specialties or famous figures tied to the mine are less documented, the region's history is rich with mining stories. The temperate, often wet climate of northern England likely influenced the mine's environment, potentially aiding mineral formation, though direct connections are not fully clear.