
mineral
Blue Lace Agate (Geode/Druzy variant)
Chalcedony (SiO2) with Quartz druzy
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Pale blue, lavender-blue, or grey secondary to banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.60-2.65
- Hardness
- 6
- Color
- Pale blue, lavender-blue, or grey secondary to banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Pale blue, lavender-blue, or grey secondary to banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.60-2.65
Formation & geological history
Formed via the deposition of silica from groundwater in cavities of igneous rocks, specifically volcanic lavas. Over millions of years, layering occurs, sometimes leaving a hollow center containing 'druzy' quartz crystals. Typical geological ages range from the Cretaceous to recent periods.
Uses & applications
Primarily used in jewelry, ornamental carvings, and lapidary arts. It is highly valued by crystal collectors for its aesthetic appeal and is used in metaphysical practices for its perceived calming effects.
Geological facts
This specific specimen is carved into a heart shape and features a 'druzy window' where the inner quartz crystals are visible. Blue Lace Agate was first discovered in Namibia, which remains a primary source for high-quality blue specimens.
Field identification & locations
Identify by characteristic concentric blue and white banding and its hardness (it will scratch glass). In the field, look for nodules in volcanic regions like Namibia, Brazil, or the US Southwest. Polished pieces like this are common in rock shops.
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