
mineral
Polished agate (likely fortification or plume agate)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide inclusions
AI-generated identification · may be incorrectCream, tan, and honey-brown translucent banding with fine curved layers and a gray included zone; waxy to glassy luster. Mohs hardness about 6.5–7, no cleavage, conchoidal fracture, trigonal quartz structure; specific gravity about 2.6.
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Physical properties
Cream, tan, and honey-brown translucent banding with fine curved layers and a gray included zone; waxy to glassy luster. Mohs hardness about 6.5–7, no cleavage, conchoidal fracture, trigonal quartz structure; specific gravity about 2.6.
Formation & geological history
Agate forms when silica-rich groundwater fills cavities in volcanic rock, depositing successive chalcedony layers. The pictured piece is cut and polished; its exact geological age and source cannot be determined from the image.
Uses & applications
Used for cabochons, carvings, ornaments, lapidary pieces, and collector specimens; durable but relatively common material.
Geological facts
The curved “fortification” bands record repeated changes in fluid chemistry during cavity filling. Gray areas may be included host material or contrasting chalcedony rather than a separate mineral.
Field identification & locations
Identify by hardness, translucent edges, waxy luster, and persistent curved bands; it should scratch glass but not be scratched by a steel knife. Agate is common worldwide, including volcanic terrains of coastal California, though this exact variety cannot be localized visually.
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