Rock Identifier
Red porphyritic volcanic rock, likely rhyolite or andesite (Porphyritic rhyolite–andesite; predominantly quartz/feldspar with iron-oxide staining) — igneous
igneous

Red porphyritic volcanic rock, likely rhyolite or andesite

Porphyritic rhyolite–andesite; predominantly quartz/feldspar with iron-oxide staining

AI-generated identification · may be incorrect

Fine-grained volcanic matrix with scattered pale phenocrysts and strong red hematite coloration; hardness about 6–7, dull to weakly vitreous luster, no obvious cleavage. The surrounding gravel includes mixed rock fragments, so exact identification from the image is limited.

Identified More igneous →
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Physical properties

Fine-grained volcanic matrix with scattered pale phenocrysts and strong red hematite coloration; hardness about 6–7, dull to weakly vitreous luster, no obvious cleavage. The surrounding gravel includes mixed rock fragments, so exact identification from the image is limited.

Formation & geological history

Formed when silica-rich lava cooled relatively quickly at or near Earth’s surface, commonly during volcanic episodes from the Precambrian to Cenozoic. Red color typically reflects oxidation of iron-bearing minerals during weathering.

Uses & applications

Used locally as crushed aggregate, road base, landscaping stone, and occasionally decorative facing stone; generally little jewelry value.

Geological facts

Porphyritic texture records two cooling stages: crystals formed slowly underground, followed by rapid eruption and cooling. Red volcanic rocks may also be altered tuff or weathered andesite.

Field identification & locations

Look for a dense fine matrix containing larger feldspar or quartz crystals; a steel knife usually scratches poorly, while quartz-rich areas resist scratching. Common worldwide in volcanic belts.