
mineral
Blue Lace Agate
Silicon Dioxide (SiO2) - Variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Light blue with white or darker blue bands; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.60-2.65
- Hardness
- 6
- Color
- Light blue with white or darker blue bands
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Light blue with white or darker blue bands; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.60-2.65
Formation & geological history
Formed through the deposition of silica from groundwater in the cavities of igneous rocks, primarily volcanic lavas. Most high-quality specimens date back to the Precambrian era.
Uses & applications
Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular collector's specimen for its aesthetic banding.
Geological facts
Blue Lace Agate was first discovered in Namibia in the early 1960s by George Swanson. It is considered one of the rarest varieties of agate because the primary source in Namibia is depleting.
Field identification & locations
Identify by its distinctive delicate blue and white banding and waxy texture. It is famously found in the Ysterputs mine in southern Namibia, as well as parts of South Africa and Romania.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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