
Mineral
Quartz (likely Yellow/Orange variety, possibly Citrine or Chalcedony with iron staining)
Quartz (SiO₂)
Hardness: 7 on Mohs scale. Color: Typically white, gray, yellow, or brown, but can be found in various colors (e.g., rose quartz, amethyst, citrine). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy)
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 on Mohs scale. Color: Typically white, gray, yellow, or brown, but can be found in various colors (e.g., rose quartz, amethyst, citrine). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Quartz forms in a wide range of geological environments, including igneous, metamorphic, and sedimentary rocks. It crystallizes from silica-rich solutions in hydrothermal veins, granites, and pegmatites. It is also a major component of sandstone and other sedimentary rocks formed from the weathering and erosion of pre-existing rocks. Geological Age: Quartz has been forming throughout Earth's history, from the Precambrian to the present day.
Uses & applications
Industry: Used as an abrasive, in glass manufacturing, as a component in ceramics, and in electronics (e.g., quartz oscillators for watches and radios). Jewelry: Many varieties are semiprecious gemstones (e.g., amethyst, citrine, rose quartz, smoky quartz). Construction: A major component of sand and gravel, used in concrete and asphalt.
Geological facts
Quartz is one of the most abundant minerals in the Earth's crust. Its piezoelectric properties make it valuable in electronics. Amethyst, a purple variety of quartz, was once as valuable as ruby and emerald. Aventurine, a green variety, gets its color from fushsite inclusions. Citrine, a yellow to orange variety, is often heat-treated amethyst.
Field identification & locations
Field Identification: Look for its glassy luster, conchoidal fracture (smooth, curved breaks), and hardness (it can scratch glass and steel). It often forms hexagonal prisms with pyramidal terminations, though the specimen in the image appears to be a water-worn or tumbled fragment. Common Locations: Found globally in virtually all types of rock formations. Significant deposits of various quartz varieties are found in Brazil, Uruguay, Madagascar, the United States (Arkansas), and many other countries. Tips for Collectors: Varieties like amethyst and citrine are popular. Look for well-formed crystals or attractive colored specimens. Translucency and color saturation are key for aesthetic value.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral