Rock Identifier
Quartz-rich pegmatite (Granitic pegmatite, composed mainly of quartz and feldspar with dark mica or other accessory minerals) — igneous
igneous

Quartz-rich pegmatite

Granitic pegmatite, composed mainly of quartz and feldspar with dark mica or other accessory minerals

AI-generated identification · may be incorrect

Coarse, irregularly intergrown white to tan crystals with scattered dark minerals; quartz hardness 7 and feldspar about 6 Mohs, typically vitreous to dull. The image suggests a coarse crystalline texture, but mineral identification and composition cannot be confirmed from appearance alone.

Identified More igneous →
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Physical properties

Coarse, irregularly intergrown white to tan crystals with scattered dark minerals; quartz hardness 7 and feldspar about 6 Mohs, typically vitreous to dull. The image suggests a coarse crystalline texture, but mineral identification and composition cannot be confirmed from appearance alone.

Formation & geological history

Pegmatite crystallizes from late-stage, silica-rich magma, often in veins cutting older igneous or metamorphic rocks. Its age depends on the local geology and cannot be determined from the image.

Uses & applications

Quartz and feldspar pegmatites are sources of industrial minerals; attractive crystals may be collected or used decoratively. This specimen appears too weathered and massive for gem use.

Geological facts

Pegmatites can contain exceptionally large crystals and sometimes rare minerals such as tourmaline, beryl, or lithium-bearing minerals.

Field identification & locations

Look for very coarse interlocking crystals, commonly quartz, feldspar, and mica; field identification is best confirmed by testing individual minerals. Found worldwide in association with granites; location is unknown here.