This specimen is a rich chunk of scheelite embedded in rock, notable for its characteristic blue-white fluorescence under ultraviolet light, marking it as an excellent piece from a historic mine. The section of quartz vein features a substantial clot of orange scheelite intersected by numerous veinlets of greasy-white quartz. This classic Timmins camp vein material is distinctively fluorescent, although seriously lacking in gold content (ie none). The mine from which this specimen originates was discovered in 1909 and operated from 1910 until 1968, contributing to its historical significance. The quartz vein and scheelite composition exemplify the mineralogical characteristics typical of the Timmins camp, renowned for its rich gold deposits.
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