Rock Identifier
Polished granite (likely a granite countertop or floor slab) (Granite; a coarse-grained intrusive felsic rock composed mainly of quartz, feldspar, and mica) — igneous
igneous

Polished granite (likely a granite countertop or floor slab)

Granite; a coarse-grained intrusive felsic rock composed mainly of quartz, feldspar, and mica

AI-generated identification · may be incorrect

The image shows a polished, speckled light-gray to beige surface with dark mineral grains. Granite is typically Mohs 6–7, with a granular crystalline texture and no consistent cleavage as a whole; the photographed finish obscures grain boundaries, so the exact variety cannot be confirmed.

Identified More igneous →
Explore Polished granite (likely a granite countertop or floor slab) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

The image shows a polished, speckled light-gray to beige surface with dark mineral grains. Granite is typically Mohs 6–7, with a granular crystalline texture and no consistent cleavage as a whole; the photographed finish obscures grain boundaries, so the exact variety cannot be confirmed.

Formation & geological history

Formed when silica-rich magma cooled slowly underground, allowing crystals to grow. Granite bodies occur in many ancient continental crust settings; the specimen’s age and source cannot be determined from the image.

Uses & applications

Commonly used for countertops, flooring, wall cladding, monuments, and decorative stone.

Geological facts

The light minerals are usually quartz and feldspars, while dark flecks are often biotite or amphibole. Similar-looking commercial slabs may be other granitoid rocks.

Field identification & locations

A speckled interlocking pattern and hard, polished surface suggest granite; verify by examining a fresh edge for visible crystals. The reported location in southwestern Angola is broadly compatible with regional granitoid rocks, but this appears to be installed stone, so its source is unknown.