
sedimentary
Chalcedony (Agate Pebble)
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Translucent tan to brownish-grey; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
- Hardness
- 6
- Color
- Translucent tan to brownish-grey
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Translucent tan to brownish-grey; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica-rich groundwater in cavities of igneous or sedimentary rocks. This specific specimen appears to be a water-worn river or beach pebble, likely resulting from the erosion of larger host rocks.
Uses & applications
Used for lapidary work, jewelry (beads and cabochons), and as a collector's item for rockhounds. Historically used for making stone tools due to its hardness and sharp fracture edges.
Geological facts
Chalcedony is a cryptocrystalline form of silica. Agates are a variety of chalcedony that often show banding, though small water-worn pebbles like this may only show faint patterns or solid translucent colors.
Field identification & locations
Identify in the field by its translucency (hold it up to a light source), waxy luster when dry, and inability to be scratched by a steel knife. Commonly found in riverbeds, glacial till, and coastal areas.
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