
sedimentary
Chert (and Agate/Quartz in Geode-like Nodule)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Brown, gray, white, and translucent; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Brown, gray, white, and translucent
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Brown, gray, white, and translucent; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the precipitation of silica from groundwater or hydrothermal fluids within a host rock (likely limestone or volcanic ash). This specimen shows a nodular structure where silica has replaced original material or filled a cavity.
Uses & applications
Historically used for stone tools (flintknapping); currently used as a decorative garden stone, for lapidary work (polishing), and as a collector's specimen.
Geological facts
Chert is remarkably durable and resistant to chemical weathering. When it contains translucent, banded layers, it is often referred to as agate. This specific piece looks like a silica-filled nodule or a 'thunder egg' fragment.
Field identification & locations
Identify in the field by its waxy luster on broken surfaces and its ability to scratch glass. It often breaks with sharp, shell-like (conchoidal) edges. Found worldwide in sedimentary basins and volcanic deposits.
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