
mineral
Milky quartz
Quartz (SiO₂)
AI-generated identification · may be incorrectHardness 7 Mohs; opaque white to cream with iron-stained tan areas and a vitreous-to-waxy luster. Trigonal crystal structure; no cleavage, with irregular to conchoidal fracture. The image shows a rough, weathered specimen.
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Physical properties
Hardness 7 Mohs; opaque white to cream with iron-stained tan areas and a vitreous-to-waxy luster. Trigonal crystal structure; no cleavage, with irregular to conchoidal fracture. The image shows a rough, weathered specimen.
Formation & geological history
Quartz commonly crystallizes from silica-rich fluids in veins and pegmatites, or forms in many rock types; it is geologically widespread and may be very ancient. The specimen’s exact age and source cannot be determined from the photo.
Uses & applications
Used as a silica source in glass and industrial materials; attractive pieces are collected or used decoratively, though this specimen appears ordinary rather than gem-grade.
Geological facts
Quartz is among the most abundant minerals in Earth’s crust and can persist after surrounding minerals weather away.
Field identification & locations
Likely quartz based on its pale color and massive appearance, but a photo cannot confirm identity; test for hardness and look for glass-scratching ability and lack of cleavage. Common worldwide, especially in quartz veins and pegmatites.
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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