
mineral
Tumbled banded agate (likely blue lace agate)
Microcrystalline quartz, SiO₂ (chalcedony variety)
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; translucent pale blue, white, and gray banding; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The smooth shape indicates tumbling and polishing.
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Physical properties
Hardness 6.5–7 Mohs; translucent pale blue, white, and gray banding; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The smooth shape indicates tumbling and polishing.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rocks, depositing successive chalcedony layers; banding commonly developed over millions of years, often in Cenozoic volcanic terrains.
Uses & applications
Used for cabochons, beads, carvings, ornamental objects, and lapidary collections; generally modest commercial value unless strongly colored, naturally patterned, or exceptionally transparent.
Geological facts
Blue lace agate is prized for delicate lace-like blue-and-white bands, though many commercial pieces are simply pale banded agate. Color may be enhanced by dyeing, but this specimen’s subdued appearance is consistent with natural material.
Field identification & locations
Identify by curved parallel bands, translucency, glassy/waxy surface, and inability to scratch it with a steel knife; it should scratch ordinary glass. Common sources include Namibia, Botswana, Brazil, Uruguay, and Mexico.
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