
mineral
Quartz (Iron-stained or Orange Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Translucent orange to tan; Luster: Vitreous/waxy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Translucent orange to tan
- Luster
- Vitreous/waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent orange to tan; Luster: Vitreous/waxy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids cooling in veins or as massive deposits. The orange color is typically caused by inclusions or surface staining of iron oxides (hematite or limonite).
Uses & applications
Used primarily in lapidary work, jewelry, and as a decorative landscaping stone. Industrial quartz is used in glassmaking and electronics.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Iron-stained varieties like this are often found in riverbeds where water has eroded and polished the specimen over time.
Field identification & locations
Identify by its hardness (will scratch glass) and lack of cleavage planes. Commonly found in riverbeds, mountains, and desert washes globally.
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Arenite (SiO2 based)
sedimentary
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Schist
Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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