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quartz

File:Quartz_Brésil.jpg · Wikimedia Commons · See Wikimedia Commons

EntityQ43010· pop 104· linked from 3,750 articles

Also known as SiO2, α-Quarz

Quartz is a hard mineral composed of silica (silicon dioxide). Its atoms are linked in a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen atom being shared between two tetrahedra, giving an overall chemical formula of SiO2. Therefore, quartz is classified structurally as a framework silicate mineral and compositionally as an oxide mineral. Quartz is the second most common mineral or mineral group in Earth's lithosphere, comprising about 12% by mass.

OverviewAI-generated

Quartz is a mineral with the chemical formula SiO₂. It has a Mohs hardness of 7 and a density of 2.65. The mineral is assigned the IMA Mineral Symbol Qz.

In mineral classification systems, quartz is categorized under Nickel-Strunz 9th edition (updated 2009) and the 10th edition as 4.DA.05. The Strunz 8th edition lists it under series ID IV/D.01a. The MCN code for the substance is 7104.10.00.

The subject appears in the Commons category and gallery titled "Quartz." Academic literature references the term in 22,004 PubMed articles. Additionally, the topic is referenced by 3,750 other encyclopedia articles.

Synthesized by Vinony from 13 facts across 3 sources: Wikidata, PubMed, Vinony graph. Generated from structured data (not the Wikipedia text) and checked against those facts — may still contain errors.

Key facts

Mineral.name
Quartz
Mineral.category
Tectosilicate minerals
Mineral.group
Quartz group
Mineral.image
Quartz Brésil.jpg
Mineral.caption
Quartz crystal cluster from Brazil
Mineral.formula
SiO2
Mineral.IMAsymbol
Qz
Mineral.strunz
4.DA.05 (oxides)
Mineral.dana
75.01.03.01 (tectosilicates)
Mineral.system
α-quartz: trigonal β-quartz: hexagonal
Mineral.class
α-quartz: trapezohedral (class 3 2) β-quartz: trapezohedral (class 6 2 2)
Mineral.symmetry
α-quartz: P3221 (no. 154)β-quartz: P6222 (no. 180) or P6422 (no. 181)
Mineral.unit cell
a = 4.9133 Å, c = 5.4053 Å; Z = 3
Mineral.color
Colorless, pink, orange, white, green, yellow, blue, purple, dark brown, or black
Mineral.habit
6-sided prism ending in 6-sided pyramid (typical), drusy, fine-grained to microcrystalline, massive
Mineral.twinning
Common Dauphine law, Brazil law, and Japan law
Mineral.cleavage
none
Mineral.fracture
Conchoidal

via Wikipedia infobox

Research

22,004 papers

via PubMed

Wikidata facts

Subclass of
tectosilicates
Part of
sand
Image
Quartz Brésil.jpg
Show 16 more facts
Commons gallery
Quartz
Mohs' hardness
7
streak color
black
Commons category
Quartz
mineral fracture
conchoidal fracture
chemical formula
SiO₂
Nickel-Strunz 9th edition (updated 2009)
4.DA.05
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
4.DA.05
topic's main category
Category:Quartz
MCN code
7104.10.00
has characteristic
piezoelectricity
density
2.65
IMA Mineral Symbol
Qz
on focus list of Wikimedia project
Wikipedia:Vital articles/Level/4
Strunz 8th edition (series ID, updated)
IV/D.01a
Sources (5)

via Wikidata · CC0

~23 min read

Encyclopedic overview

14 sections
Contents
  • Etymology
  • Early studies
  • Crystal habit and structure
  • Varieties
  • Piezoelectricity
  • Occurrence
  • Mining
  • Related silica minerals
  • Safety
  • Synthetic and artificial treatments
  • Uses
  • See also
  • References
  • External links

Quartz is a hard mineral composed of silica (silicon dioxide). Its atoms are linked in a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen atom being shared between two tetrahedra, giving an overall chemical formula of SiO2. Therefore, quartz is classified structurally as a framework silicate mineral and compositionally as an oxide mineral. Quartz is the second most common mineral or mineral group in Earth's lithosphere, comprising about 12% by mass.

Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold.

Excerpted from Wikipedia’s “quartz” article, available under the CC BY-SA 4.0 licence.

Gallery (52)