Rock Identifier
Polished basalt with chalcedony/agate vein (Basalt (fine-grained mafic volcanic rock) with microcrystalline quartz, SiO₂) — igneous
igneous

Polished basalt with chalcedony/agate vein

Basalt (fine-grained mafic volcanic rock) with microcrystalline quartz, SiO₂

AI-generated identification · may be incorrect

Dark gray-black, fine-grained and granular with a glossy polish; the translucent brown-gray band is likely chalcedony or agate. Basalt hardness is about 6–7 Mohs, quartz-rich vein about 7; no obvious cleavage, with generally high specific gravity around 2.8–3.1.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained and granular with a glossy polish; the translucent brown-gray band is likely chalcedony or agate. Basalt hardness is about 6–7 Mohs, quartz-rich vein about 7; no obvious cleavage, with generally high specific gravity around 2.8–3.1.

Formation & geological history

Basalt formed from rapidly cooled mafic lava, commonly in volcanic flows, while silica-rich fluids later filled a cavity or fracture to produce chalcedony/agate. The specimen’s exact geological age and locality cannot be determined from the image.

Uses & applications

Used mainly as a decorative, polished, or lapidary specimen; basalt is also used for aggregate, paving, and construction stone. The vein adds modest ornamental and collecting interest.

Geological facts

The granular dark matrix may also be a related mafic volcanic rock such as diabase, but the image favors basalt. Translucent chalcedony commonly displays waxy luster and curved internal banding.

Field identification & locations

Identify it by its heavy dark matrix, tiny interlocking crystals, and contrasting translucent quartz vein; a glassy streak or bubbles would suggest artificial glass instead. Common settings include volcanic provinces worldwide, especially flood-basalt regions and ancient lava flows.