Rock Identifier
Tumbled brown stone, likely jasper or fine-grained quartzite (Uncertain; probable microcrystalline quartz (SiO₂), possibly ferruginous jasper) — sedimentary or metamorphic
sedimentary or metamorphic

Tumbled brown stone, likely jasper or fine-grained quartzite

Uncertain; probable microcrystalline quartz (SiO₂), possibly ferruginous jasper

AI-generated identification · may be incorrect

Smoothly polished, opaque brown material with subtle speckling and tiny dark inclusions; likely Mohs 6.5–7, vitreous-to-dull luster, massive texture, no visible cleavage, and specific gravity around 2.6. The photograph alone cannot distinguish jasper from quartzite or another hard silicate pebble.

Identified More sedimentary or metamorphic →
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Physical properties

Smoothly polished, opaque brown material with subtle speckling and tiny dark inclusions; likely Mohs 6.5–7, vitreous-to-dull luster, massive texture, no visible cleavage, and specific gravity around 2.6. The photograph alone cannot distinguish jasper from quartzite or another hard silicate pebble.

Formation & geological history

If jasper, it formed from silica-rich fluids replacing or cementing sediment; if quartzite, it formed by metamorphism of quartz sandstone. The source rock could range from Precambrian to much younger, while tumbling is human processing.

Uses & applications

Used as a decorative tumbled stone, paperweight, craft material, or low-cost cabochon; generally not suitable for major construction because of its small size.

Geological facts

The rounded shape and uniformly polished surface indicate a commercial tumbler rather than natural weathering. Brown coloration commonly comes from iron oxides or hydroxides.

Field identification & locations

Check hardness with a steel nail or glass, streak (usually white), and acid reaction (none); a 10× loupe may reveal quartz grains or jasper-like cryptocrystalline texture. Common sources include gravel deposits and jasper/quartzite regions worldwide.