Rock Identifier
Polished pietersite cabochon (Pietersite (brecciated fibrous quartz/chalcedony, commonly with riebeckite or crocidolite remnants)) — metamorphic
metamorphic

Polished pietersite cabochon

Pietersite (brecciated fibrous quartz/chalcedony, commonly with riebeckite or crocidolite remnants)

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; brown, orange, gray, and blue chatoyant patches with vitreous to waxy luster. Microcrystalline quartz has no visible cleavage and commonly shows tiger’s-eye-like chatoyancy; this specimen is polished and labeled.

Identified More metamorphic
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Physical properties

Hardness about 6.5–7 Mohs; brown, orange, gray, and blue chatoyant patches with vitreous to waxy luster. Microcrystalline quartz has no visible cleavage and commonly shows tiger’s-eye-like chatoyancy; this specimen is polished and labeled.

Formation & geological history

Forms when fibrous quartz-rich material is brecciated and recemented by silica, preserving aligned amphibole fibers that create chatoyancy. Commercial material mainly comes from Namibia and China, generally formed in Precambrian host rocks.

Uses & applications

Used for cabochons, pendants, beads, and collectible lapidary pieces; it is not a major construction or industrial stone.

Geological facts

Its strongest identifying feature is shifting, silky reflection as the stone moves under light. Pietersite is sometimes marketed as “tempest stone” and may be confused with tiger’s eye or hawk’s eye.

Field identification & locations

Look for irregular breccia-like brown-gold or blue-gray color zones and directional chatoyancy, rather than tiger’s eye’s uniform parallel bands. Common sources are Namibia and China; verify with a loupe and hardness testing before any scratch test.