
Mineral
Agate (specifically Carnelian or Honey Agate)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale. Color: Translucent orange to honey-yellow. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Translucent orange to honey-yellow
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Translucent orange to honey-yellow. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
Formation & geological history
Formed as a result of silica-rich groundwater filling cavities or vesicles in volcanic rocks (igneous host). The layers are deposited inward toward the center, often spanning millions of years. This specimen likely originates from the Cenozoic era.
Uses & applications
Extensively used in lapidary work for jewelry, cabochons, and beads. Historically used for cylinder seals and amulets. Today, it is popular among rockhounds for polishing and display specimens.
Geological facts
Agate is a variety of chalcedony characterized by its translucency and fine grain. Because of its hardness and resistance to chemical weathering, it is frequently found as 'river stones' or on beaches long after the parent rock has eroded away.
Field identification & locations
Identification: Look for a waxy texture, conchoidal (shell-like) fractures, and translucency when held to light. Found globally, but prolific in areas with ancient volcanic activity like Brazil, India, and the Pacific Northwest, USA. Collectors should look for unique internal banding or inclusions.
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