
mineral
Clear Quartz / Diamond (untested)
Silicon Dioxide (SiO2) or Carbon (C)
AI-generated identification · may be incorrectHardness: 7 (Quartz) to 10 (Diamond); Color: Colorless and transparent; Luster: Vitreous to adamantine; Crystal system: Trigonal (Quartz) or Isometric (Diamond); Cleavage: None in Quartz, Octahedral in Diamond
- Hardness
- 7 (Quartz) to 10 (Diamond)
- Color
- Colorless and transparent
- Luster
- Vitreous to adamantine
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Physical properties
Hardness: 7 (Quartz) to 10 (Diamond); Color: Colorless and transparent; Luster: Vitreous to adamantine; Crystal system: Trigonal (Quartz) or Isometric (Diamond); Cleavage: None in Quartz, Octahedral in Diamond
Formation & geological history
Formed in hydrothermal veins, pegmatites, and metamorphic rocks (if Quartz), or deep in the Earth's mantle under high pressure and temperature (if Diamond).
Uses & applications
Used extensively in electronics, optics, jewelry, gemstone collections, and industrial abrasives.
Geological facts
Clear quartz crystals are known as 'rock crystal' and were historically believed to be permanently frozen ice. Diamonds are the hardest naturally occurring material on Earth.
Field identification & locations
Field identification can be tested using hardness scratch tests, specific gravity measurements, or thermal conductivity detectors. Found in alluvial gravels, pegmatites, and kimberlites worldwide.
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Other mineral specimens
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