Rock Identifier
Tumbled prehnite (probable) (Prehnite — Ca₂Al(AlSi₃O₁₀)(OH)₂) — mineral
mineral

Tumbled prehnite (probable)

Prehnite — Ca₂Al(AlSi₃O₁₀)(OH)₂

AI-generated identification · may be incorrect

Pale green, translucent, waxy-to-vitreous luster with cloudy inclusions; hardness 6–6.5 Mohs, orthorhombic crystal structure, poor cleavage, and specific gravity about 2.8–2.95. The rounded shape indicates tumbling or natural abrasion.

Identified More mineral
Explore Tumbled prehnite (probable) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Pale green, translucent, waxy-to-vitreous luster with cloudy inclusions; hardness 6–6.5 Mohs, orthorhombic crystal structure, poor cleavage, and specific gravity about 2.8–2.95. The rounded shape indicates tumbling or natural abrasion.

Formation & geological history

Forms in cavities and fractures of basalt and other volcanic rocks through low-temperature hydrothermal alteration, commonly alongside zeolites; deposits range from relatively young volcanic terrains to ancient metamorphosed systems.

Uses & applications

Used mainly as a semiprecious collector gemstone and ornamental stone; rarely used industrially because attractive material is limited.

Geological facts

Prehnite is often recognized by its soft apple-green color and pearly or waxy appearance, though epidote, serpentine, jade, or green chalcedony can look similar.

Field identification & locations

Common localities include South Africa, Australia, India, China, Canada, and the United States. Look for rounded pale-green nodules with translucent edges and curved fracture; laboratory testing is needed for certainty.