mineral

Small polished or naturally worn stone, possibly quartz-bearing rock

Indeterminate from the blurred image; likely quartz (SiO₂) or a pale feldspar-rich fragment

AI-generated identification · may be incorrect

The specimen appears gray-green, translucent to opaque, and irregular with a slight vitreous or waxy luster. Quartz has Mohs hardness 7, no cleavage, and conchoidal fracture; feldspar is Mohs 6–6.5 with two cleavage directions.

Identified August 17, 2026More mineral →

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At a glance

Common name: Small polished or naturally worn stone, possibly quartz-bearing rock
Scientific name: Indeterminate from the blurred image; likely quartz (SiO₂) or a pale feldspar-rich fragment
Category: mineral
Identified: August 17, 2026
Method: Standard

AI Estimated Value

Typically $0–$5 as an unidentified small specimen; potentially $5–$25 if it proves to be an attractive collectible mineral.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

Likely a naturally weathered fragment from an igneous or metamorphic rock; exact formation age and host rock cannot be determined visually. Quartz commonly crystallizes from cooling magma or hydrothermal fluids.

Uses & applications

Quartz-bearing stones are used as aggregate, abrasives, glass and ceramics; attractive pieces may be collected or used decoratively. This small fragment has little commercial value unless diagnostic minerals or gem quality are confirmed.

Geological facts

The image is too low-resolution and the specimen is too small for confident species identification. A scratch test, streak test, magnification, and clearer close-up would distinguish quartz from feldspar or another pale mineral.

Field identification & locations

Look for crystal faces, cleavage, translucency, and hardness; quartz should not be scratched by a steel knife, while feldspar may be. Common sources include stream gravel, weathered granite, pegmatites, and metamorphic veins.