Rock Identifier
Chalcedony (specifically Agate or Water-worn Quartzite) (Silicon Dioxide (SiO2)) — mineral
mineral

Chalcedony (specifically Agate or Water-worn Quartzite)

Silicon Dioxide (SiO2)

Hardness: 6.5–7 on the Mohs scale. Color: Translucent tan to smoky orange. Luster: Waxy to vitreous. Crystal Structure: Hexagonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6–2.7.

Hardness
6
Color
Translucent tan to smoky orange
Luster
Waxy to vitreous
Identified More mineral

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Physical properties

Hardness: 6.5–7 on the Mohs scale. Color: Translucent tan to smoky orange. Luster: Waxy to vitreous. Crystal Structure: Hexagonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6–2.7.

Formation & geological history

Formed from the deposition of silica-rich water at low temperatures, typically in volcanic cavities or as replacement in sedimentary layers. These smooth specimens often originate as nodules that have been tumbled and rounded through fluvial (river) or marine action.

Uses & applications

Commonly used in lapidary work for making cabochons, beads, and ornamental carvings. Also used as a decorative stone for aquariums or garden landscaping.

Geological facts

Chalcedony has been used since the Bronze Age for seals and jewelry because it does not cling to wax. This specific rounded shape is the result of thousands of years of natural polishing by sand and water.

Field identification & locations

Identify by its translucency (light passes through the edges), waxy surface, and extreme hardness (it will scratch glass). Commonly found in riverbeds, gravel pits, and along beaches. Collectors should look for 'banding' which would further classify it as an Agate.