Rock Identifier
Iron-stained quartz-rich rock (Likely quartz-feldspar rock (granite or pegmatite) with iron-oxide staining) — igneous
igneous

Iron-stained quartz-rich rock

Likely quartz-feldspar rock (granite or pegmatite) with iron-oxide staining

AI-generated identification · may be incorrect

Rough, irregular specimen with pink-brown and gray translucent grains and rusty patches. Quartz is Mohs 7 with vitreous luster and no cleavage; feldspar is softer (about 6) and commonly shows cleavage.

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Physical properties

Rough, irregular specimen with pink-brown and gray translucent grains and rusty patches. Quartz is Mohs 7 with vitreous luster and no cleavage; feldspar is softer (about 6) and commonly shows cleavage.

Formation & geological history

Likely crystallized from silica-rich magma as granite or pegmatite; iron-bearing minerals later oxidized, producing the rusty coloration. The image does not allow a precise age or rock identification.

Uses & applications

Common examples are used as aggregate or building stone; attractive pieces may be collected, but this specimen appears unpolished and modest in value.

Geological facts

Rust-colored coatings commonly form when iron minerals weather to hematite or goethite.

Field identification & locations

A quartz-rich, feldspar-bearing texture and hard glassy grains would support this identification; field confirmation requires a closer look at grain boundaries and mineral hardness. Similar rocks occur widely in continental crust.