Rock Identifier
Granite Thin Section (Granitic rock (Phaneritic texture)) — igneous
igneous

Granite Thin Section

Granitic rock (Phaneritic texture)

Hardness: 6-7 Mohs; Color: Interstitial quartz (white/gray), feldspars (tan/brown), and micas (high-interference 'bird-eye' maple colors); Luster: Vitreous under thin section; Structure: Crystalline mosaic; Cleavage: Visible in feldspar grains.

Hardness
6-7 Mohs
Luster
Vitreous under thin section
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Interstitial quartz (white/gray), feldspars (tan/brown), and micas (high-interference 'bird-eye' maple colors); Luster: Vitreous under thin section; Structure: Crystalline mosaic; Cleavage: Visible in feldspar grains.

Formation & geological history

Formed through the slow cooling and crystallization of felsic magma deep within the Earth's crust (plutonic). Found in continental crust contexts, often dating from the Precambrian to Cenozoic eras.

Uses & applications

Used primarily for geological study and petrography to identify mineral assemblages. In bulk form, granite is used for construction, countertops, and monuments.

Geological facts

This image is captured through a petrographic microscope using cross-polarized light (XPL), which causes minerals to display vibrant interference colors based on their birefringence properties.

Field identification & locations

Identify by presence of quartz (low relief, undulatory extinction), plagioclase (twinning), and biotite or muscovite. Found in mountain ranges and batholiths worldwide.