Spinel, Forsterite

This specimen features several jet-black octahedral spinel crystals on a well formed forsterite and set within a matrix made up almost entirely of forsterite and a bit of calcite. The specimen originates from the Parker Mine, a well-known locality in Quebec, Canada. Initially opened in the early 1900s for mica mining, the Parker Mine is renowned for producing exceptionally large and well-formed crystals, particularly within its carbonate vein-dyke systems. The area, composed of regionally metamorphosed Precambrian sediments, has yielded notable specimens, including euhedral forsterite crystals up to 30 cm and ferroan spinel crystals up to 6 cm. This specimen is an excellent example of the fine mineralogical diversity found within the Parker Mine’s unique geological environment.