Raw Smoky Quartz Crystal Point Fragment

This item is a small, naturally occurring raw crystal fragment, likely smoky quartz based on its translucent to semi-opaque greyish-brown coloration. It measures approximately 1 to 1.5 centimeters in height and width, appearing as a wedge-shaped or truncated pyramidal point. The specimen exhibits a vitreous luster with internal fractures and inclusions that create various light-catching planes. Its color palette ranges from a clear, frosty white at the base to a darker, smoky grey at the upper terminal end. The surface is irregular with notable conchoidal fracturing facets, characteristic of minerals in the quartz family. There are no maker's marks or synthetic modifications, suggesting it is a geological specimen rather than a manufactured jewelry component. The condition is raw and unpolished, with jagged edges and a non-uniform apex, consistent with a mineral specimen that has been fractured from a larger geode or cluster. It lacks decorative setting or drill holes for mounting. The age is geological, spanning millions of years. This piece is representative of common mineral collecting samples often used for metaphysical purposes or as rough lapidary material.

Upon visual examination of this raw smoky quartz fragment, I find it to be a typical geological specimen of common macrocrystalline quartz. The fragment displays the characteristic conchoidal fracture and vitreous luster expected of the species, with a pleasant smoky coloration resulting from natural irradiation of trace aluminum. Measuring approximately 1 to 1.5 cm, this specimen is classified as a 'chip' or 'thumbnail' fragment rather than a high-grade cabinet specimen. The condition is raw and fractured, lacking a complete terminated crystal habit, which significantly limits its value to the decorative or metaphysical bulk market. Comparable items are typically sold by weight in 'parcel' lots rather than as individual appraised stones. The market for small, fractured quartz pieces is highly saturated, and rarity is non-existent for this specific mineral type. Factors such as the lack of clarity, small size, and absence of a pristine termination prevent it from reaching collector-grade status. My assessment is based solely on the provided image; however, photographic analysis cannot definitively distinguish between natural smoky quartz and some forms of treated glass or synthetic slag, though the internal inclusions suggest a natural origin. A full authentication would require a physical Mohs hardness test, a specific gravity measurement, and a refractometer reading to confirm internal refractive indices. Given its low market value, the cost of scientific testing would likely exceed the value of the specimen itself. This appraisal assumes the piece is natural and untreated, as is common for smaller specimens of this variety.