
sedimentary
Chert
Silicon Dioxide (Microcrystalline Quartz)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Varies from white, grey, beige, to brown; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.60 - 2.65
- Hardness
- 7 on Mohs scale
- Color
- Varies from white, grey, beige, to brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Varies from white, grey, beige, to brown; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.60 - 2.65
Formation & geological history
Formed by the chemical precipitation of silica from aqueous solutions or the accumulation of siliceous skeletal remains of microscopic organisms like radiolarians and diatoms, typically within limestone or chalk formations over millions of years.
Uses & applications
Historically used for making stone tools, arrowheads, and blades due to its sharp conchoidal fracture; occasionally used in landscaping or decorative gravel.
Geological facts
Chert has been utilized by humans for stone tool manufacture since the Paleolithic era because it flakes in predictable, razor-sharp pieces.
Field identification & locations
Easily identified by its hard conchoidal fracture, waxy luster, and ability to scratch glass. Commonly found weathering out of limestone or chalk cliffs and riverbeds worldwide.
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