Rock Identifier
Dark igneous rock with white feldspar/quartz patches (Likely porphyritic basalt or andesite; white patches may be plagioclase feldspar or quartz) — igneous
igneous

Dark igneous rock with white feldspar/quartz patches

Likely porphyritic basalt or andesite; white patches may be plagioclase feldspar or quartz

AI-generated identification · may be incorrect

Dark gray to black, fine-grained groundmass with conspicuous pale crystals or mineral aggregates; likely Mohs hardness 5–7 and vitreous to dull luster. Exact composition and crystal structure cannot be confirmed from the image alone.

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Physical properties

Dark gray to black, fine-grained groundmass with conspicuous pale crystals or mineral aggregates; likely Mohs hardness 5–7 and vitreous to dull luster. Exact composition and crystal structure cannot be confirmed from the image alone.

Formation & geological history

Probably formed as lava cooled, with larger crystals growing before the remaining melt solidified; its geological age and precise setting cannot be determined visually.

Uses & applications

Commonly used crushed for aggregate and road base; this small specimen is mainly of educational or collecting interest.

Geological facts

The pale inclusions contrast with the finer dark matrix, suggesting a porphyritic texture, though some may be mineral-filled cavities or attached material.

Field identification & locations

Look for a fine dark matrix containing larger, lighter crystals; a fresh broken surface and hardness tests can help distinguish feldspar from quartz. Similar volcanic rocks occur in many volcanic regions worldwide.