
mineral
Quartz-rich breccia or quartz vein fragment
Silica, primarily quartz (SiO₂), with possible chlorite, feldspar, or iron-oxide inclusions
AI-generated identification · may be incorrectPale blue-green, translucent to opaque, with vitreous luster and granular/interlocking texture; apparent hardness about 7 Mohs, no obvious cleavage, and conchoidal fracture. The metallic-looking patches may be mica, sulfides, or surface reflections rather than true metal.
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Physical properties
Pale blue-green, translucent to opaque, with vitreous luster and granular/interlocking texture; apparent hardness about 7 Mohs, no obvious cleavage, and conchoidal fracture. The metallic-looking patches may be mica, sulfides, or surface reflections rather than true metal.
Formation & geological history
Likely formed when silica-rich hydrothermal fluids filled fractures and crystallized, possibly incorporating altered host rock; age depends on its source locality. The blue-green coloration commonly reflects inclusions or alteration minerals.
Uses & applications
Used mainly as a collector specimen or lapidary material if it polishes well; quartz-rich material can also be used decoratively, though this irregular piece has little industrial value.
Geological facts
Quartz is one of Earth’s most abundant minerals and is piezoelectric. Color alone is not diagnostic because inclusions and weathering can strongly alter its appearance.
Field identification & locations
Common in hydrothermal veins and altered igneous or metamorphic terrains worldwide. A glassy luster, hardness near 7, lack of cleavage, and inability to scratch it with a steel knife support quartz; acid testing is unnecessary.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary