Rock Identifier
Rounded porphyritic volcanic pebble (Likely andesite porphyry (identification from the photo is approximate)) — igneous
igneous

Rounded porphyritic volcanic pebble

Likely andesite porphyry (identification from the photo is approximate)

AI-generated identification · may be incorrect

Fine-grained, olive-gray matrix with scattered pale feldspar-like crystals and dark mineral grains; rounded by transport. Likely hardness about 6 on Mohs scale, with no obvious cleavage; specific gravity roughly 2.5–2.8.

Identified More igneous →
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Physical properties

Fine-grained, olive-gray matrix with scattered pale feldspar-like crystals and dark mineral grains; rounded by transport. Likely hardness about 6 on Mohs scale, with no obvious cleavage; specific gravity roughly 2.5–2.8.

Formation & geological history

Probably cooled from volcanic lava, then weathered and rounded in a stream or on a beach. Andesitic rocks are common in the active volcanic belt of central Chile; the pebble’s age cannot be determined from the image.

Uses & applications

As a small pebble it has little industrial value; similar andesite is used as crushed aggregate and building stone. This specimen is mainly of interest to collectors.

Geological facts

Its speckled appearance may reflect larger crystals embedded in a finer volcanic groundmass, a texture called porphyritic.

Field identification & locations

A hand lens can reveal crystals, and a fresh broken surface would help distinguish andesite from other volcanic rocks. The reported central-Chile location is geologically plausible; a rounded pebble could have been transported from its source.