mineral

Blue-gray tumbled stone, possibly carnelian mislabeled

Unidentified; carnelian is orange-red chalcedony (microcrystalline SiO₂), so the pictured blue-gray stone is unlikely to be carnelian.

AI-generated identification · may be incorrect

Opaque to slightly translucent, smooth rounded polish, blue-gray with pale mottling and a subdued waxy luster. If chalcedony, Mohs hardness is about 6.5–7; the photograph does not establish its mineral identity or crystal structure.

Identified October 3, 2026More mineral →

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At a glance

Common name: Blue-gray tumbled stone, possibly carnelian mislabeled
Scientific name: Unidentified; carnelian is orange-red chalcedony (microcrystalline SiO₂), so the pictured blue-gray stone is unlikely to be carnelian.
Category: mineral
Identified: October 3, 2026
Method: Standard

AI Estimated Value

About $1–$5 as a small common tumbled stone; more only if a valuable identity is verified.

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

A tumbled, human-shaped specimen; its original formation and age cannot be determined from the image. Carnelian typically forms when silica fills cavities or fractures, but this color does not match typical carnelian.

Uses & applications

Tumbled stones are commonly sold for collecting, decoration, and jewelry; value depends on confirmed identity, size, and quality.

Geological facts

The label reads “carnelian,” but carnelian is characteristically orange to reddish-brown. Blue-gray appearance may instead indicate another mineral or dyed material.

Field identification & locations

The specimen’s identity cannot be confirmed visually. The reported location in southeast Texas is dominated by sedimentary deposits, but a transported or purchased tumbled stone need not be locally sourced; confirm with hardness, translucence, and mineral testing.