Chalcedony sits at 7 on the Mohs scale —
harder than glass; scratches steel.
Colors:
Streak White
Crystal system Trigonal (microcrystalline)
Oxides & HydroxidesOxides (Silica Group)
TL;DR · 1 min read
Chalcedony is the cryptocrystalline form of quartz — submicroscopic interlocked quartz fibers producing a tough, waxy-lustered material. Many named varieties are Chalcedony: agate (banded), carnelian (red-orange), chrysoprase (apple-green Ni), bloodstone (green with red jasper), and onyx (parallel-banded).
Chalcedony is the cryptocrystalline form of quartz — submicroscopic interlocked quartz fibers producing a tough, waxy-lustered material. Many named varieties are Chalcedony: agate (banded), carnelian (red-orange), chrysoprase (apple-green Ni), bloodstone (green with red jasper), and onyx (parallel-banded). Chalcedony forms in basalt cavities and silica-replacement environments.
Nickel-bearing apple-green chalcedony variety; the rarest chalcedony color.
Bloodstone (Heliotrope)(u8840u77f3)
green with red spots
Dark-green chalcedony with red iron-oxide spots resembling blood drops.
About Chalcedony
Chalcedony is a tectosilicate mineral in the quartz group and has the chemical formula SiO2. It crystallizes in the trigonal system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Chalcedony typically forms microcrystalline to cryptocrystalline masses; nodules, botryoidal coatings, stalactitic; no visible crystals. Its color range is broad, including white, gray, blue, pale blue (classic), and also many other colors. The luster is waxy to dull, the streak is white, and specimens are typically translucent. The fracture is conchoidal, which is one of its key identifying features.
Collector context
How it forms
Chalcedony forms in low-temperature hydrothermal; volcanic vesicles; replacement of limestone; weathering; diagenetic in sediments. It is commonly found in association with quartz, calcite, zeolites, opal.
Classic Chinese localities
Documented Chinese occurrences are recorded at Shangbao Mine, Jiama Cu-polymetallic deposit and Jinduicheng Mine, among others.
Why collectors care
Collectors pursue Chalcedony for its patterns, color depth, and polish response rather than for pattern character. Good material has a surface that polishes cleanly, a visual character that holds up in direct light, and enough size to anchor a display on its own. Chinese sources, where present, supply much of the material currently cut and sold as decorative pieces.
What affects value
Value in Chalcedony is assessed, in typical order of weight, against: (1) source locality; (2) size; (3) pattern and visual character; (4) color depth and distribution; (5) polish response and surface finish; (6) piece integrity (absence of major cracks or chips). Uniqueness of pattern and verified source region add significantly to decorative pieces.
Naming history
The name Chalcedony has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
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