Rock Identifier
Tumbled dark stone, possibly basalt or iron-rich chert (Indeterminate; likely fine-grained basalt (plagioclase–pyroxene) or ferruginous chert) — igneous
igneous

Tumbled dark stone, possibly basalt or iron-rich chert

Indeterminate; likely fine-grained basalt (plagioclase–pyroxene) or ferruginous chert

AI-generated identification · may be incorrect

Dark brown-black, rounded and polished, with a vitreous-to-waxy luster and small lighter inclusions; hardness is approximately 5.5–7 Mohs, depending on composition. No cleavage is visible; specific gravity is roughly 2.6–3.0.

Identified More igneous
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Physical properties

Dark brown-black, rounded and polished, with a vitreous-to-waxy luster and small lighter inclusions; hardness is approximately 5.5–7 Mohs, depending on composition. No cleavage is visible; specific gravity is roughly 2.6–3.0.

Formation & geological history

If basalt, it formed from rapidly cooled mafic lava, commonly in oceanic or volcanic settings; if chert, it formed from microcrystalline silica in sedimentary environments. The specimen’s geological age cannot be determined from the photograph.

Uses & applications

Likely a tumbled lapidary or decorative stone, suitable for crafts, display, and informal collecting; it has little industrial or jewelry value without confirmed composition.

Geological facts

The smooth triangular form and glossy surface indicate mechanical tumbling or water abrasion. The pale specks may be weathered mineral grains, vesicles, or surface residue.

Field identification & locations

Test with a steel knife: basalt may scratch or be scratched near hardness 5–6, while chert should resist scratching; a streak, magnetism, and specific gravity test would help distinguish them. Common source regions include volcanic terrains and gravel deposits.