
mineral
Agate with Quartz Druzy
Silicon Dioxide (SiO2) - Microcrystalline and Macrocrystalline varieties
Hardness: 6.5-7 on Mohs scale. Color: Waxy grey-blue chalcedony base with reddish-brown rinds and translucent crystalline druzy. Luster: Vitreous to waxy. Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.65.
- Hardness
- 6
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Waxy grey-blue chalcedony base with reddish-brown rinds and translucent crystalline druzy. Luster: Vitreous to waxy. Structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.65.
Formation & geological history
Formed through the deposition of silica from groundwater into cavities (vugs) within volcanic host rocks or limestone. The reddish-brown crust suggests a high iron oxide presence during the formation of the outer layers. These are typically millions of years old, often dating from the Cenozoic era.
Uses & applications
Commonly used for lapidary work (cabbing and polishing), jewelry, spiritual/metaphysical collecting, and as decorative display specimens.
Geological facts
Agate is a variety of chalcedony characterized by its fineness of grain and brightness of color. The internal cavity seen in this specimen is a 'vug' where quartz crystals had space to grow, creating the 'druzy' sparkle.
Field identification & locations
Identify in the field by checking for a translucent waxy texture and conchoidal fractures. Look for it in riverbeds or agricultural fields near volcanic regions. To collectors, the presence of internal crystal structures within a weathered rind is a key indicator.
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