
sedimentary
Agate (Nodule/Chert)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Gray, tan, white, and translucent with banding; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Gray, tan, white, and translucent with banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Gray, tan, white, and translucent with banding; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
Formation & geological history
Formed through the deposition of silica from groundwater in the cavities of igneous rocks or as nodules in sedimentary limestone or chalk. Many specimens date back to the Cretaceous or Tertiary periods.
Uses & applications
Used primarily for jewelry (cabochons), lapidary arts, ornamental carving, and architectural accents. Historically used for making pestles and mortars due to its hardness.
Geological facts
The name 'Agate' comes from the Achates River in Sicily. It is one of the oldest materials used in human history for adornment and tools.
Field identification & locations
Identify by its waxy appearance, translucency at the edges, and characteristic 'bubbly' or banded patterns. It is commonly found in river beds, beaches, and volcanic soil in regions like the Lake Superior area, Brazil, and India.
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