Smoky Quartz Crystal Point
This specimen is a natural smoky quartz crystal point, characterized by its translucent to transparent earthy brown and golden-bronze coloration. The crystal displays a classic hexagonal prism structure at its base, tapering toward a termination point. Physically, it exhibits a vitreous luster with various internal fractures and veining that create interesting light refraction and depths of color. The specimen shows significant natural ruggedness; the termination tip appears weathered or slightly chipped, indicating a raw, unpolished state typical of crystals extracted directly from geode or pocket environments without extensive lapidary treatment. Its construction is geological rather than manufactured, with visible conchoidal fractures along the sides that are signature to the quartz family. The color variation suggests a presence of natural irradiation and aluminum impurities within the silicon dioxide structure. Notably, there are no artificial signatures or stamps, emphasizing its origin as a mineral specimen. The condition includes some surface abrasions and internal inclusions that are considered natural 'growth marks' rather than damage. Such pieces are typically valued based on their clarity, richness of the 'smoky' hue, and the integrity of the crystal facets.
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Estimated Value
$65–$95
Basic Information
Category
Minerals and Gemstones
Appraised On
April 27, 2026
Estimated Value
$65–$95
Item Description
This specimen is a natural smoky quartz crystal point, characterized by its translucent to transparent earthy brown and golden-bronze coloration. The crystal displays a classic hexagonal prism structure at its base, tapering toward a termination point. Physically, it exhibits a vitreous luster with various internal fractures and veining that create interesting light refraction and depths of color. The specimen shows significant natural ruggedness; the termination tip appears weathered or slightly chipped, indicating a raw, unpolished state typical of crystals extracted directly from geode or pocket environments without extensive lapidary treatment. Its construction is geological rather than manufactured, with visible conchoidal fractures along the sides that are signature to the quartz family. The color variation suggests a presence of natural irradiation and aluminum impurities within the silicon dioxide structure. Notably, there are no artificial signatures or stamps, emphasizing its origin as a mineral specimen. The condition includes some surface abrasions and internal inclusions that are considered natural 'growth marks' rather than damage. Such pieces are typically valued based on their clarity, richness of the 'smoky' hue, and the integrity of the crystal facets.
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