External databases provide CIF (Crystallographic Information File) downloads + interactive 3D viewers. AMCSD: American Mineralogist Crystal Structure Database (free, RRUFF-hosted). COD: open community-curated database.
Elemental Composition (by mass)
Element
Mass %
Visual
OOxygen
53.26%
SiSilicon
46.74%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
Cone-shaped quartz pseudomorphs after scalenohedral calcite — sometimes called "babingtonite".
Cornwall; Bohemia.
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited. › Full catalogue
Tenacity
Behavior:
brittle
Under stress:
Conchoidal fracture under blow
Hard but brittle — sharp hammer-strike produces conchoidal flakes.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Diagnostic Field Tests
Hardness→ Mohs 7 — scratches glass and steel
Reference point for the hardness scale.
HCl test→ No reaction
No fizz — distinguishes from calcite of similar habit.
Cleavage→ None — conchoidal fracture
Distinguishes from feldspar (which has cleavage).
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
2.65
g/cm³
light
Standard reference for low-SG transparent gem material.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Synthetics & Imitations
Lab-grown methods
Hydrothermal1900 · Spezia
Industrial-scale since 1950s for electronics. Lab citrine, amethyst, and rose quartz all readily synthesized.
Common imitations
Glass
Singly refractive, conchoidal fracture, gas bubbles.
Quartz is the most abundant mineral exposed at Earth's surface — and despite its commonness, it produces some of the finest collector specimens in mineralogy. From Himalayan ice-clear crystals to the deep purple amethysts of Vera Cruz, quartz is the species every collector returns to.
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Quartz is the most abundant mineral exposed at Earth's surface — and despite its commonness, it produces some of the finest collector specimens in mineralogy. From Himalayan ice-clear crystals to the deep purple amethysts of Vera Cruz, quartz is the species every collector returns to.
Tibetan and Sichuan high-altitude pegmatites produce extraordinarily clear quartz crystals with fine terminations and minimal inclusions. The Yaogangxian district yields milky quartz matrix material for fluorite specimens, while Hunan produces some of the world's best fenster (window) quartz.
Test at home — what scratches what
Will scratch your specimen: 🪨 Topaz scratch test (Mohs 8) · 💎 Corundum (sapphire/ruby) (Mohs 9) · 💠 Diamond (Mohs 10)
Always test on an inconspicuous edge first. Save the test for unimportant specimens — better to use a streak plate or knowledge of locality + paragenesis.
Cite this entry
APA
MyMineralBox Editorial Team. (2026). Quartz. My Mineral Box. Retrieved May 23, 2026, from https://mymineralbox.com/mineral-encyclopedia/minerals/quartz/
MLA
MyMineralBox Editorial Team. "Quartz." My Mineral Box, 2026, https://mymineralbox.com/mineral-encyclopedia/minerals/quartz/. Accessed May 23, 2026.
Chicago
MyMineralBox Editorial Team. "Quartz." My Mineral Box. Last modified May 4, 2026. https://mymineralbox.com/mineral-encyclopedia/minerals/quartz/.
BibTeX
@misc{mmb_quartz,
author = {{MyMineralBox Editorial Team}},
title = {{Quartz}},
year = {2026},
publisher = {My Mineral Box},
url = {https://mymineralbox.com/mineral-encyclopedia/minerals/quartz/},
urldate = {2026-05-23}
}
Identification & care
Specimens usually show prismatic, pyramidal, massive, drusy, geodes. Its color range is broad, including colorless, purple (amethyst), rose/pink, red, black (morion), yellow (citrine), brown (smoky), green, blue, and orange. The luster is vitreous, the streak is white, and specimens range from transparent to opaque. The cleavage is none / indistinct. The fracture is conchoidal, which aids identification.
Collector context
How it forms
The geological setting for Quartz is typically igneous, metamorphic, and sedimentary rocks; hydrothermal veins. It is commonly found in association with feldspar, mica, tourmaline, calcite.
Classic Chinese localities
Documented Chinese occurrences are recorded at Shangbao Mine, Jiama Cu-polymetallic deposit and Jinduicheng Mine, among others.
Why collectors care
Quartz is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.
What affects value
Value in Quartz is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
The name Quartz has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
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