
sedimentary
Chert (Carnelian/Jasper variety)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7.0 (Mohs scale); Color: Orangey-brown to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Orangey-brown to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7.0 (Mohs scale); Color: Orangey-brown to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed primarily through the precipitation of silica from groundwater or the accumulation of silica-rich organic remains in sedimentary basins. The color is typically derived from iron oxide impurities.
Uses & applications
Used historically for stone tools and weapons due to its conchoidal fracture. In modern times, it is used for lapidary work, jewelry (cabs), and as a decorative landscaping stone.
Geological facts
This specimen displays classic conchoidal (shell-like) fracturing, which was a vital property for prehistoric humans to create sharp edges on arrowheads and knives.
Field identification & locations
Identify in the field by its waxy appearance, extreme hardness (scratches glass), and distinctive curved, glass-like fracture surfaces. Frequently found in stream beds or within limestone/chalk deposits.
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