
mineral
Agate
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale). Color: Multicolored banding in translucent tan, white, and orange. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Multicolored banding in translucent tan, white, and orange
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale). Color: Multicolored banding in translucent tan, white, and orange. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
Formation & geological history
Formed as a secondary mineral in volcanic rock cavities (vugs) or ancient sedimentary rocks. Silica-rich groundwater precipitates layers of microscopic quartz crystals over time, often filling gas bubbles in cooling lava.
Uses & applications
Used primarily in lapidary arts for jewelry, figurines, and beads. Also used in industry for mortar and pestles due to its hardness, and highly valued as a collectible mineral specimen.
Geological facts
The word Agate comes from the Achates River in Sicily, where agates were first discovered. Unlike most minerals, its unique banding pattern makes every single specimen one-of-a-kind.
Field identification & locations
Identify in the field by its characteristic concentric or planar banding visible on weathered surfaces and its ability to scratch glass. Commonly found in areas with past volcanic activity or in riverbeds. Collectors should look for 'fortification' patterns.
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Arenite (SiO2 based)
sedimentary
Schist
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Metamorphic
Epidote
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metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral