Rock Identifier
Iron-stained quartz-rich rock, possibly weathered granite or pegmatite (Quartz–feldspar-rich rock with iron-oxide staining; exact rock type cannot be determined from the image) — igneous
igneous

Iron-stained quartz-rich rock, possibly weathered granite or pegmatite

Quartz–feldspar-rich rock with iron-oxide staining; exact rock type cannot be determined from the image

AI-generated identification · may be incorrect

Coarse, irregular texture with cream, rusty-brown, and dark patches; likely quartz and feldspar with iron oxides and dark accessory minerals. Hardness and cleavage cannot be confirmed visually; quartz is Mohs 7, while feldspars are about 6.

Identified More igneous →
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Physical properties

Coarse, irregular texture with cream, rusty-brown, and dark patches; likely quartz and feldspar with iron oxides and dark accessory minerals. Hardness and cleavage cannot be confirmed visually; quartz is Mohs 7, while feldspars are about 6.

Formation & geological history

Likely formed by cooling of silica-rich magma, then fractured and weathered, with iron oxides staining the surface. No geological age or precise formation environment can be established from the photograph.

Uses & applications

Quartz- and feldspar-rich rocks may be used as construction aggregate or decorative stone; this specimen appears mainly suitable for collecting or display.

Geological facts

The rusty coloration commonly results when iron-bearing minerals oxidize during weathering.

Field identification & locations

Look for interlocking light-colored grains, glassy quartz, and feldspar cleavage; a fresh broken surface would help distinguish granite from pegmatite or another rock. Such rocks are widespread in continental crust, but the image gives no locality.