
mineral
Mica-bearing quartz or feldspar fragment
Likely milky quartz (SiO₂), possibly with biotite/muscovite inclusions; feldspar cannot be excluded visually
AI-generated identification · may be incorrectTranslucent milky-white to gray, vitreous-to-waxy luster, irregular fracture with no obvious cleavage, and dark reflective inclusions. Quartz hardness is Mohs 7; feldspar is 6–6.5, so a steel nail test can help distinguish them.
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Physical properties
Translucent milky-white to gray, vitreous-to-waxy luster, irregular fracture with no obvious cleavage, and dark reflective inclusions. Quartz hardness is Mohs 7; feldspar is 6–6.5, so a steel nail test can help distinguish them.
Formation & geological history
Likely a natural fragment broken from a quartz vein or granitic/pegmatitic rock, formed by cooling silica-rich magma or hydrothermal fluids, commonly from Precambrian to younger continental crust.
Uses & applications
Quartz is used in glass, ceramics, electronics, abrasives, and ornamental specimens; attractive pieces may be polished, though this example appears mainly of collector interest.
Geological facts
The black flecks may be biotite mica, tourmaline, iron-oxide staining, or surface debris; strongly reflective flakes suggest mica inclusions.
Field identification & locations
Common in granite, pegmatite, quartz veins, and stream gravels worldwide. Quartz scratches glass and lacks visible cleavage; feldspar commonly shows two cleavage directions and may appear more opaque.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous