Mineral within Sedimentary Rock
Chalcedony in Limestone Host Rock
Silicon Dioxide (SiO2) within Calcium Carbonate (CaCO3)
Hardness: 7 (inner crystal), 3 (outer rock). Color: Grey to translucent white. Luster: Waxy or dull. Structure: Microcrystalline (Quartz) and Massive. Cleavage: None/Conchoidal.
- Hardness
- 7 (inner crystal), 3 (outer rock)
- Color
- Grey to translucent white
- Luster
- Waxy or dull
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Physical properties
Hardness: 7 (inner crystal), 3 (outer rock). Color: Grey to translucent white. Luster: Waxy or dull. Structure: Microcrystalline (Quartz) and Massive. Cleavage: None/Conchoidal.
Formation & geological history
Formed through secondary mineralization where silica-rich fluids precipitate into cavities or vugs within sedimentary limestone formations, often during the Paleozoic era.
Uses & applications
Used primarily for decorative geological specimens, historical flint-knapping for tools, or as a source of high-purity silica in industrial abrasive applications.
Geological facts
This specimen appears to be a small 'vug' or geode-like cavity. Chalcedony is technically a fibrous form of cryptocrystalline quartz that is too small to see with the naked eye.
Field identification & locations
Identify in the field by checking for the hardness difference; the inner grey crystals will scratch glass, while the outer grey rock will not. Commonly found in riverbeds or limestone quarries.
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