gemstone

Tumbled carnelian agate with dark mineral inclusions

Carnelian, an orange variety of microcrystalline quartz (chalcedony), SiO₂; dark inclusions are likely iron oxides/hydroxides, possibly hematite, goethite, or a basaltic/matrix fragment

AI-generated identification · may be incorrect

Identified July 31, 2026More gemstone →

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At a glance

Common name: Tumbled carnelian agate with dark mineral inclusions
Scientific name: Carnelian, an orange variety of microcrystalline quartz (chalcedony), SiO₂; dark inclusions are likely iron oxides/hydroxides, possibly hematite, goethite, or a basaltic/matrix fragment
Category: gemstone
Identified: July 31, 2026
Method: Standard

AI Estimated Value

Approximately $3–$15 USD for a common tumbled piece of this size; about $15–$50 if the color, translucency, inclusions, or provenance are particularly attractive. It is unlikely to have high gem value without exceptional color, pattern, or documented origin.

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

The specimen is a polished/tumbled, orange-red, translucent to opaque chalcedony. It has a waxy to vitreous luster, conchoidal fracture, no obvious cleavage, and approximate Mohs hardness of 6.5–7. Carnelian commonly owes its orange color to finely dispersed iron oxides. The irregular dark gray-black patch and spots appear to be natural mineral or rock inclusions. Specific gravity is typically about 2.58–2.65. Exact identification is uncertain from the photograph alone; orange jasper or iron-stained agate are possible alternatives.

Formation & geological history

Carnelian forms when silica-rich fluids fill cavities and fractures in volcanic rocks, depositing microscopic quartz fibers and chalcedony. Iron-bearing impurities produce the orange to red coloration, often through oxidation. Agates and related chalcedony commonly formed in volcanic cavities during the Paleozoic through Cenozoic eras, although the age of this individual specimen cannot be determined visually.

Uses & applications

Used for beads, cabochons, carvings, ornaments, polished stones, and lapidary specimens. Historically it has been used in seals, signet rings, and decorative objects. Common tumbled pieces have modest commercial and collecting value.

Geological facts

Carnelian is closely related to sard, with the boundary between the two based mainly on color intensity and translucency. Heating can deepen or redden the color by oxidizing iron. The dark material is not diagnostic of carnelian and may represent hematite, goethite, manganese minerals, or host-rock residue.

Field identification & locations

In the field, carnelian is recognized by its orange-red color, translucency at thin edges, hardness sufficient to scratch ordinary glass, conchoidal fracture, and waxy polish. It commonly occurs as rounded nodules or cavity fillings with agate banding. Important sources include India, Brazil, Uruguay, Madagascar, Botswana, Germany, and parts of the western United States. A close inspection with a loupe, streak testing of the dark inclusion, hardness testing, specific gravity, and ideally Raman or X-ray analysis would be needed to confirm the exact material.