mineral

Pale green tumbled stone, possibly green aventurine

Likely quartz-rich aventurine (SiO₂ with fuchsite inclusions); exact identification is uncertain from the image

AI-generated identification · may be incorrect

Opaque, pale green, smooth and rounded with a subdued luster. If aventurine, hardness is about 6.5–7 Mohs and its crystal structure is trigonal; no clear cleavage, with uneven fracture and specific gravity near 2.6.

Identified October 15, 2026More mineral →

Explore Pale green tumbled stone, possibly green aventurine in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Formation & geological history

Aventurine forms when quartz crystallizes with reflective mica or other mineral inclusions, commonly during metamorphic or hydrothermal processes; its age depends on the deposit.

Uses & applications

Tumbled aventurine is used for jewelry, carvings, and decorative collections; quartz is also widely used in glass and electronics.

Geological facts

Green aventurine’s characteristic sparkle, called aventurescence, comes from platy mineral inclusions; it is not apparent in this image.

Field identification & locations

The smooth shape suggests a tumbled specimen, but color alone cannot confirm aventurine. Check for glittering inclusions and a hardness near 7; green calcite or other stones may look similar.