Yellow Fluorite Specimen, Beijing Region
This raw fluorite mineral specimen features a beautiful cluster of transparent to pale yellow cubic crystals with excellent luster and clarity. Sourced from Beijing, China, this piece displays tightly intergrown fluorite cubes with sharp edges, delicate zoning, and an elegant shimmer under natural light. The pale coloration and near-translucent quality give it a graceful, understated aesthetic prized by mineral collectors.
Specimen details
| Mineral | Fluorite |
|---|---|
| Locality | — |
| Crystal system | Isometric |
| Dimensions | 4.8 cm × 2.5 cm × 2.5 cm |
| Weight | 45 g |
| Color | Yellow |
| Size | Miniature (up to 2 inches / up to 5 cm) |
| Species | Fluorite |
| Condition | No damage on display faces |
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About this specimen
This exceptional Yellow Fluorite Crystal Cluster is a stunning natural specimen. The cluster features multiple well-formed crystals displaying excellent natural formation that makes it a standout addition to any mineral collection.
Fluorite (CaF₂) crystallizes in the cubic (isometric) crystal system with a Mohs hardness of 4. This mineral is known for exceptional fluorescence under ultraviolet light, perfect octahedral cleavage, and a wide range of colors including purple, green, blue, yellow, and colorless. This specimen demonstrates the characteristic features that make Fluorite a favorite among mineral enthusiasts.
This specimen weighs 1.587 oz (45.0 g) and measures approximately 1.9 × 1 × 1 inches. Each specimen is carefully hand-selected to ensure excellent crystal development, natural aesthetics, and display-worthy presentation. Photographs represent the actual specimen you will receive.
Whether you are a seasoned mineral collector, a geology enthusiast, or searching for a distinctive natural display piece, this Fluorite specimen offers exceptional quality and visual appeal. It makes an impressive addition to a specimen cabinet, educational display, or curated mineral collection — Fluorite is prized by collectors for its vivid color zoning and phantom growth patterns, and industrially important as a flux in steelmaking and in the production of hydrofluoric acid.




