This specimen features a sharp, complete black octahedral spinel crystal, accompanied by forsterite and set within a calcite matrix. The spinel exhibits well-defined faces with successive, stacked layers of parallel crystal growth, a characteristic feature of this mineral. 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.
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