
sedimentary
Chert (Chalcedony)
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Gray, tan, white, and translucent with waxy luster; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 7 (Mohs scale)
- Color
- Gray, tan, white, and translucent with waxy luster
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Physical properties
Hardness: 7 (Mohs scale); Color: Gray, tan, white, and translucent with waxy luster; Crystal Structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or by the chemical precipitation of silica in marine or groundwater environments. It often occurs as nodules in limestone or chalk beds.
Uses & applications
Historically used for making stone tools (arrowheads). Modern uses include gemstones (when colorful, known as jasper or agate), construction aggregate, and as a material for precision mechanical parts due to its hardness.
Geological facts
Chert has been used by humans for hundreds of thousands of years because it breaks with incredibly sharp edges. It is often referred to as 'flint' when found in chalk deposits and 'jasper' when it is pigmented red or yellow.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), waxy to dull luster, and conchoidal (shell-like) fracture patterns. Frequently found in riverbeds, glacial till, or eroding out of limestone outcrops.
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