Rock Identifier
Tumbled blue-gray stone, possibly chalcedony or quartzite (Likely microcrystalline quartz (SiO₂), but the image is insufficient for confident identification) — mineral
mineral

Tumbled blue-gray stone, possibly chalcedony or quartzite

Likely microcrystalline quartz (SiO₂), but the image is insufficient for confident identification

AI-generated identification · may be incorrect

Smooth, rounded, polished surface; blue-gray to tan coloration with a dull-to-waxy luster. Quartz-based material has Mohs hardness about 7, no visible cleavage, and specific gravity near 2.6; translucency and hardness testing would help distinguish it from glass or other stone.

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Physical properties

Smooth, rounded, polished surface; blue-gray to tan coloration with a dull-to-waxy luster. Quartz-based material has Mohs hardness about 7, no visible cleavage, and specific gravity near 2.6; translucency and hardness testing would help distinguish it from glass or other stone.

Formation & geological history

If chalcedony, it formed when silica-rich fluids filled cavities or fractures and precipitated as microcrystalline quartz, commonly in volcanic rocks. If quartzite, it is metamorphosed sandstone; age depends on its source locality.

Uses & applications

Typically used as a tumbled decorative stone, pocket specimen, or craft material; quality translucent examples may be used in inexpensive jewelry.

Geological facts

The blue-gray color may result from microscopic inclusions, staining, or surface treatment. A glassy appearance alone cannot reliably identify the material.

Field identification & locations

Common sources include Brazil, Madagascar, India, Uruguay, and the United States. Field tests: quartz should scratch glass and resist a steel knife; inspect for bubbles, which suggest glass, and use a specific-gravity or gemological test for confirmation.