
Chalcedony
Silicon dioxide (SiO2), microcrystalline quartz
A waxy, translucent microcrystalline form of quartz that serves as the parent group for agate, jasper, carnelian, and onyx.
- Mohs hardness
- 6.5-7
- Color
- White, gray, blue, pink, and many pastel hues; often translucent
- Type
- mineral
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Overview
Chalcedony is the broad family name for microcrystalline (cryptocrystalline) quartz, composed of submicroscopic intergrown quartz and moganite fibers. In the strictest gem trade sense, "chalcedony" refers to the solid, evenly colored, translucent material, often pale blue, gray, or white.
Many familiar stones are varieties of chalcedony, including agate (banded), carnelian (red-orange), chrysoprase (green), onyx (black), and jasper (opaque and impure). Its smooth, waxy texture made it a favored carving material in the ancient world.
It is abundant, durable, and takes a high polish, which is why it appears across countless cultures and time periods.
Formation & geology
Chalcedony forms from silica-rich aqueous solutions at low temperatures, precipitating in cavities, fractures, and voids in volcanic and sedimentary rocks. The silica deposits as tiny fibrous quartz crystals rather than large single crystals.
It commonly lines or fills vesicles in basalt, forms in the weathering zones of silica-rich rocks, and replaces other materials such as wood and fossils. Slow, rhythmic deposition produces banded varieties like agate, while uniform deposition gives solid chalcedony.
Major sources are worldwide, including Brazil, India, Namibia, Turkey (famous blue chalcedony), Indonesia, and the United States.
How to identify it
Chalcedony is translucent to semi-translucent with a waxy to slightly greasy or vitreous luster and a smooth conchoidal fracture. It has a hardness of 6.5-7 and a white streak.
Colors are typically soft and even in pure chalcedony. It scratches glass easily and resists a steel knife, which separates it from softer look-alikes like calcite (Mohs 3) and opal (softer, often with play-of-color).
Opal is distinguished by lower hardness and amorphous structure; glass imitations lack the natural waxy translucency and may show bubbles. Dyed chalcedony shows unnatural, concentrated color.
Uses & significance
Chalcedony has been carved into seals, cameos, intaglios, beads, and bowls since antiquity and is still widely used for cabochons and jewelry today. Blue chalcedony from Turkey and Namibia is especially prized.
Industrially, its fine grain and durability once made it useful for instrument bearings and as a tough utility stone. As the parent of agate, jasper, and carnelian, it underpins a huge segment of the lapidary trade.
Metaphysically, chalcedony is linked to calm, balance, and communication. Value depends on color, translucency, and freedom from fractures.
Frequently asked questions
Is chalcedony the same as quartz?
Chalcedony is a microcrystalline form of quartz, made of microscopic quartz fibers rather than visible crystals, so it shares quartz's chemistry and hardness but has a waxy, massive appearance.
What stones are types of chalcedony?
Agate, carnelian, chrysoprase, onyx, sard, bloodstone, and jasper are all varieties of chalcedony.
How can I tell natural blue chalcedony from dyed stone?
Natural blue chalcedony has soft, slightly uneven color; dyed material often shows overly vivid or uniform color and dye concentrated in tiny cracks.
Is chalcedony durable enough for rings?
Yes. At 6.5-7 Mohs it is suitable for everyday jewelry, though it can chip if struck hard against a surface.
Chalcedony guides
In-depth guides for identifying, valuing, and understanding Chalcedony.











