Rock Identifier
Weathered copper-bearing rock, possibly chrysocolla-bearing quartz or host rock (Indeterminate from the photo; possible chrysocolla (hydrated copper silicate) with quartz or other host minerals) — mineral
mineral

Weathered copper-bearing rock, possibly chrysocolla-bearing quartz or host rock

Indeterminate from the photo; possible chrysocolla (hydrated copper silicate) with quartz or other host minerals

AI-generated identification · may be incorrect

Small rounded specimen with pale blue-green and cream patches; likely opaque and earthy to dull in luster. Hardness and crystal structure cannot be reliably determined visually; chrysocolla is typically Mohs 2–4, while quartz is 7.

Identified More mineral →
Explore Weathered copper-bearing rock, possibly chrysocolla-bearing quartz or host rock in the encyclopedia →

Identify your own rocks.

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

Physical properties

Small rounded specimen with pale blue-green and cream patches; likely opaque and earthy to dull in luster. Hardness and crystal structure cannot be reliably determined visually; chrysocolla is typically Mohs 2–4, while quartz is 7.

Formation & geological history

The blue-green coloration may result from copper minerals forming during near-surface oxidation of copper deposits. Geological age and exact formation cannot be determined from the image.

Uses & applications

Copper-bearing rocks may be collected as mineral specimens; richer ores can be sources of copper. This small, unverified piece has no evident commercial use.

Geological facts

Blue-green color is common in secondary copper minerals, but color alone cannot confirm chrysocolla or distinguish it from other copper minerals.

Field identification & locations

A field identification would require tests such as hardness, streak, and examination of fresh surfaces; avoid relying on color alone. Copper minerals occur in oxidized zones of copper deposits worldwide.