
mineral
Agate (translucent slice)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored bands, milky white to translucent grey; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.60 to 2.65
- Hardness
- 6
- Color
- Multi-colored bands, milky white to translucent grey
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored bands, milky white to translucent grey; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.60 to 2.65
Formation & geological history
Formed in cavities (vesicles) of volcanic rocks (basalt or andesite) or metamorphic rocks where silica-rich groundwater deposits layers of chalcedony over time. Specimens can range from millions to hundreds of millions of years old.
Uses & applications
Commonly used in jewelry (pendants, beads), ornamental carvings, burnishing tools, and historically for precision bearings and laboratory mortars due to its hardness and chemical resistance.
Geological facts
Agate belongs to the chalcedony family. Its name comes from the Achates River in Sicily where it was first discovered by ancient Greeks. No two agates are identical because the banding depends on the mineral inclusions in the groundwater during formation.
Field identification & locations
Identify in the field by its waxy luster, translucency when held to light, and conchoidal (shell-like) fracture patterns. Frequently found in riverbeds, beaches, and weathered volcanic areas like Lake Superior (USA), Brazil, and Germany.
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