
mineral
Quartz with Chlorite or Epidote inclusions
Silicon Dioxide (SiO2) with inclusions
Hardness: 7 (Quartz); Color: Yellowish-tan with dark green inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture)
- Hardness
- 7 (Quartz)
- Color
- Yellowish-tan with dark green inclusions
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 (Quartz); Color: Yellowish-tan with dark green inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture)
Formation & geological history
Formed in hydrothermal veins or metamorphic environments where silica-rich fluids crystallized around existing minerals like Chlorite or Epidote. The yellow-tan hue often comes from surface iron staining (limonite).
Uses & applications
Primarily collected as a mineral specimen. Clearer versions are used in jewelry; this particular specimen is a rough field sample used for geological study.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Inclusions like the green spots seen here can significantly alter the appearance and value of a quartz specimen.
Field identification & locations
Identify in the field by its hardness (will scratch glass) and lack of cleavage. Common in many mountain ranges and riverbeds globally. Look for the contrast between the pale quartz matrix and dark mineral inclusions.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
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