Rock Identifier
Pink-and-gray feldspar-rich rock, likely granite or pegmatite fragment (Granite/pegmatite; chiefly quartz and feldspar, possibly mica) — igneous
igneous

Pink-and-gray feldspar-rich rock, likely granite or pegmatite fragment

Granite/pegmatite; chiefly quartz and feldspar, possibly mica

AI-generated identification · may be incorrect

Small, coarse-looking pink, white, and gray grains with a vitreous-to-dull luster. Likely hardness 6–7, with no obvious cleavage visible at this scale; exact identification needs a closer view.

Identified More igneous →
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Physical properties

Small, coarse-looking pink, white, and gray grains with a vitreous-to-dull luster. Likely hardness 6–7, with no obvious cleavage visible at this scale; exact identification needs a closer view.

Formation & geological history

If granite or pegmatite, it crystallized slowly from silica-rich magma underground; such rocks formed in many geological periods and occur in continental crust.

Uses & applications

Granite is widely used as building and dimension stone; pegmatite is valued as a source of feldspar, quartz, mica, and collectible crystals.

Geological facts

Pink coloration commonly comes from potassium feldspar, while gray translucent patches may be quartz.

Field identification & locations

Look for interlocking grains and distinguishable quartz and feldspar; the image is too close and small to confirm the rock type. Granite and pegmatite are widespread, especially in ancient continental terrains.