
Mineral
Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on the Mohs scale. Color: Often colorless, white, purple (amethyst), pink (rose quartz), brown, yellow (citrine), smoky gray to black (smoky quartz). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal system). Cleavage: None (conchoidal fracture). Specific Gravity: Approximately 2.65.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Often colorless, white, purple (amethyst), pink (rose quartz), brown, yellow (citrine), smoky gray to black (smoky quartz). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal system). Cleavage: None (conchoidal fracture). Specific Gravity: Approximately 2.65.
Formation & geological history
Quartz forms in many environments, including igneous, metamorphic, and sedimentary rocks. In igneous rocks, it crystallizes from silicic magmas. In metamorphic rocks, it forms under high pressure and temperature conditions. In sedimentary rocks, it is a primary constituent of sandstones and chert, weathered from other rocks. Its formation geological age varies widely, from Precambrian to current times, depending on the specific rock formation.
Uses & applications
Quartz is used extensively in various industries. As sand, it's crucial for glass manufacturing, ceramics, and as an abrasive. Piezoelectric quartz crystals are essential in electronics for oscillators, filters, and as frequency-control devices (e.g., in watches and radios). Many varieties are popular as gemstones (e.g., amethyst, citrine, rose quartz, smoky quartz). It is also used in construction as a component of concrete and mortar.
Geological facts
Quartz is one of the most common minerals on Earth's crust, found in a wide range of geological environments. Many varieties of quartz are semi-precious gemstones. Large, well-formed quartz crystals are highly sought after by collectors.
Field identification & locations
In the field, quartz can be identified by its relative hardness (scratches glass), its glassy luster, and its characteristic conchoidal (shell-like) fracture. It does not effervesce with acid. It's commonly found in nearly all types of rocks, including granite, gneiss, quartzite, and sandstone, and as sand in riverbeds and beaches worldwide. For collectors, look for well-formed crystals in vugs and veins, or for colored varieties in pegmatites and hydrothermal deposits. The rounded, somewhat translucent appearance of the specimen in the image suggests it's a water-worn pebble, likely from a river or beach environment.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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)
Metamorphic Rock