Rock Identifier
Likely pink feldspar-rich granite or pegmatite fragment (Uncertain from the image; possibly potassium feldspar (orthoclase/microcline) with quartz) — igneous
igneous

Likely pink feldspar-rich granite or pegmatite fragment

Uncertain from the image; possibly potassium feldspar (orthoclase/microcline) with quartz

AI-generated identification · may be incorrect

Pale peach to cream, opaque, unevenly fractured, with a dull to slightly vitreous luster. Individual crystals and cleavage are not clear enough to confirm; feldspar hardness is about 6 Mohs.

Identified More igneous →
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Physical properties

Pale peach to cream, opaque, unevenly fractured, with a dull to slightly vitreous luster. Individual crystals and cleavage are not clear enough to confirm; feldspar hardness is about 6 Mohs.

Formation & geological history

If feldspar-rich igneous rock, it crystallized slowly from silica-rich magma, commonly in granite or pegmatite. The specimen’s age and exact formation cannot be determined visually.

Uses & applications

Granite is used as construction and decorative stone; feldspar is used in ceramics and glass. This small, unidentified fragment has little commercial value.

Geological facts

The image does not show enough texture or scale to distinguish a feldspar crystal from a weathered rock fragment or other pale mineral.

Field identification & locations

A fresh feldspar surface commonly shows two near-right-angle cleavage planes and can scratch glass; granite should show multiple interlocking minerals. Common in continental crust and pegmatites worldwide.