Rock Identifier
Tumbled green aventurine (likely) (Quartz, SiO₂, with possible fuchsite or other mica inclusions) — mineral
mineral

Tumbled green aventurine (likely)

Quartz, SiO₂, with possible fuchsite or other mica inclusions

AI-generated identification · may be incorrect

Smooth, rounded, pale mint-green body with a waxy to vitreous luster; quartz hardness is about 7 Mohs, no obvious cleavage, and specific gravity is approximately 2.65. The uniform appearance and lack of visible sparkle make identification uncertain from the photograph.

Identified More mineral
Explore Tumbled green aventurine (likely) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Smooth, rounded, pale mint-green body with a waxy to vitreous luster; quartz hardness is about 7 Mohs, no obvious cleavage, and specific gravity is approximately 2.65. The uniform appearance and lack of visible sparkle make identification uncertain from the photograph.

Formation & geological history

Aventurine forms when quartz crystallizes with disseminated green mica, commonly in metamorphic or hydrothermal environments; specimens may be Precambrian to younger depending on locality. The pictured piece is polished/tumbled.

Uses & applications

Used for carvings, beads, cabochons, decorative stone, and inexpensive jewelry; it has little construction use in this form.

Geological facts

Green aventurine is commonly confused with green chalcedony, jade, serpentine, and dyed quartzite. Strong aventurescence—tiny reflective sparkles—is typical but may be absent in pale material.

Field identification & locations

Common sources include India, Brazil, Russia, and Tanzania. Check hardness with care, inspect for mica sparkle under a flashlight, and use a refractometer or microscope for confirmation; color alone is not diagnostic.