
mineral
Quartz Druzy on Agate
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to white crystals with reddish-brown iron staining; Luster: Vitreous to waxy; Crystal structure: Hexagonal/trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to white crystals with reddish-brown iron staining
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to white crystals with reddish-brown iron staining; Luster: Vitreous to waxy; Crystal structure: Hexagonal/trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the deposition of silica from hydrothermal fluids in cavities or vugs of volcanic rocks. The 'druzy' refers to the tiny glittering crystals that formed on the surface of the underlying agate base during the cooling process.
Uses & applications
Used primarily in lapidary work, jewelry (pendants and rings), crystal healing collections, and as decorative display specimens.
Geological facts
The reddish-brown tint is caused by iron oxide (limonite or hematite) inclusions or coatings. Druzy crystals are highly prized for their natural sparkle which mimics the appearance of sugar or snow.
Field identification & locations
Identify by looking for a 'sugary' coating of tiny crystals over a microcrystalline base. It is common in areas with past volcanic activity like Brazil, Uruguay, and the Southwestern US. Use a streak test (white) and check for hardness to distinguish from softer calcite.
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