
igneous
Granite with a quartz-rich inclusion
Granite, composed chiefly of quartz, feldspar, and mica; the visible inclusion appears to be milky quartz
AI-generated identification · may be incorrectCoarse-grained, pink-tan and gray, with a granular texture and glassy gray inclusion. Quartz is Mohs 7; feldspar is about 6; granite has no single crystal structure or cleavage.
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Physical properties
Coarse-grained, pink-tan and gray, with a granular texture and glassy gray inclusion. Quartz is Mohs 7; feldspar is about 6; granite has no single crystal structure or cleavage.
Formation & geological history
Granite forms when silica-rich magma cools slowly underground, allowing large crystals to grow. Its age cannot be determined from the image; granites range from recent to billions of years old.
Uses & applications
Granite is widely used as building and dimension stone, countertops, paving, and aggregate; quartz is used in glass and electronics.
Geological facts
The pale, translucent patch is consistent with quartz, but a photograph alone cannot confirm its identity or whether it is a natural inclusion.
Field identification & locations
Identify granite by its interlocking visible mineral grains and hardness; quartz should resist scratching by a steel knife. Granite occurs worldwide in continental crust.