
igneous
Weathered granite fragment
Granite, chiefly quartz–feldspar–mica aggregate
AI-generated identification · may be incorrectCoarse-grained, pale pink-gray rock with visible quartz and feldspar plus dark mica; vitreous to earthy luster, uneven fracture, hardness about 6–7 Mohs, and typical specific gravity 2.6–2.7.
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Physical properties
Coarse-grained, pale pink-gray rock with visible quartz and feldspar plus dark mica; vitreous to earthy luster, uneven fracture, hardness about 6–7 Mohs, and typical specific gravity 2.6–2.7.
Formation & geological history
An intrusive igneous rock formed by slow cooling of silica-rich magma deep in the crust, commonly during Precambrian to Phanerozoic mountain-building events; the fragment appears naturally weathered or broken.
Uses & applications
Used extensively as dimension stone, building cladding, countertops, monuments, paving, and aggregate; this small fragment has negligible commercial value unless from a documented locality.
Geological facts
Granite’s interlocking crystals make it durable and resistant to abrasion, though feldspar can weather to clay and produce the rough surface visible here.
Field identification & locations
Common worldwide, especially in continental shields and batholiths. Identify it by its speckled quartz-feldspar-mica texture, lack of layering, and inability to scratch with a steel knife; estimated value: $1–$10 as an ordinary specimen, potentially $10–$30 if locality-documented.