Rock Identifier
Blue Lace Agate (Silicon Dioxide (SiO₂)) — Mineral (Variety of Chalcedony/Quartz)
Mineral (Variety of Chalcedony/Quartz)

Blue Lace Agate

Silicon Dioxide (SiO₂)

Hardness: 6.5-7 on Mohs scale. Color: Light blue with white or darker blue banding. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.

Hardness
6
Color
Light blue with white or darker blue banding
Luster
Vitreous to waxy

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Physical properties

Hardness: 6.5-7 on Mohs scale. Color: Light blue with white or darker blue banding. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.

Formation & geological history

Formed in volcanic rock cavities (vugs) through the deposition of silica from groundwater. The blue color is often attributed to the scattering of light by microscopic inclusions. Most significant deposits are associated with Precambrian formations, though the agate itself forms much later in volcanic vents.

Uses & applications

Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for crystal collecting and metaphysical practices.

Geological facts

First discovered in Namibia in the early 1960s by George Swanson. It is considered a rare variety of agate because original high-quality deposits in Namibia are becoming depleted.

Field identification & locations

Identify by its distinct concentric or wavy banding of sky blue and white. It is commonly found in Namibia, South Africa, and occasionally Brazil. Collectors should look for translucency and the absence of 'dye' lines, which are common in fakes.