Rock Identifier
Likely pink feldspar-bearing pegmatite (Quartz–feldspar pegmatite, likely containing pink potassium feldspar (KAlSi₃O₈) and quartz (SiO₂)) — igneous
igneous

Likely pink feldspar-bearing pegmatite

Quartz–feldspar pegmatite, likely containing pink potassium feldspar (KAlSi₃O₈) and quartz (SiO₂)

AI-generated identification · may be incorrect

Coarse, irregular pink-red and gray-white crystals with a glassy to pearly luster; likely feldspar hardness ~6 and quartz hardness 7 Mohs. The photo does not show enough detail to confirm mineral proportions or crystal structure.

Identified More igneous →
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Physical properties

Coarse, irregular pink-red and gray-white crystals with a glassy to pearly luster; likely feldspar hardness ~6 and quartz hardness 7 Mohs. The photo does not show enough detail to confirm mineral proportions or crystal structure.

Formation & geological history

Pegmatite forms when the final, water-rich portion of granitic magma cools slowly, producing coarse crystals; its age depends on the source intrusion and cannot be determined from the image.

Uses & applications

Pegmatite minerals are sources of feldspar, quartz, mica, and sometimes lithium or gemstones; attractive pieces are collected or used decoratively.

Geological facts

Pegmatites can contain exceptionally large crystals and economically important rare-element minerals.

Field identification & locations

Look for interlocking, coarse pink feldspar and translucent gray quartz; a hardness or fresh-surface examination would help confirm the identification. Pegmatites occur worldwide, especially in granitic regions.