Approximate retail prices. Wholesale + private sale typically 40-60% of retail. Auction premium 10-25%. For investment-grade purchase steps, see the investment checklist.
Crystal Structure
Cubic — Fe in FCC, S₂ "dumbbells" in voids; isostructural with NaCl.
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
SSulfur
53.45%
FeIron
46.55%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
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:
Shatters; sparks struck
Brittle despite metallic appearance — opposite of gold malleability. Diagnostic.
Luster
metallic
Brassy metallic — the "fool's gold" luster.
Color Cause (Chromophore)
Chromophore:
d-electron transitions
Mechanism:
metallic FeS₂
Color produced:
brassy gold
Color makes it the original "fool's gold" — but band structure quite different from Au.
FeS₂ — surprisingly diamagnetic despite Fe content. Distinguishes from pyrrhotite, which IS magnetic.
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
Streak test→ Greenish black powder
Diagnostic vs gold (golden streak).
Hardness→ Mohs 6 — scratches glass
Distinguishes from chalcopyrite (Mohs 3.5–4).
Smell when broken→ Sulfur smell when freshly broken
Faint but present in fresh material.
⚠ 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
4.95–5.10
g/cm³
heavy
FeS₂; brassy "fool's gold".
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
greenish black
Diagnostic against gold (yellow streak). Often called "fool's gold" for this reason.
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Pyrite is the most abundant sulfide on Earth and the species that gave us the term "fool's gold. " For collectors, the Shangbao Mine in Hunan is the modern reference: brassy cubes and pyritohedra of remarkable size and luster, often perched on milky quartz with selective overgrowth of orange calcite.
Text size:AAA
Pyrite is the most abundant sulfide on Earth and the species that gave us the term "fool's gold." For collectors, the Shangbao Mine in Hunan is the modern reference: brassy cubes and pyritohedra of remarkable size and luster, often perched on milky quartz with selective overgrowth of orange calcite.
Shangbao Mine produces the worldwide reference for Chinese pyrite – cubes 5-15 cm with mirror-bright faces, often in three-species combinations with quartz and orange calcite. The Huanggangzhai pyrite, by contrast, runs to pyritohedral habit and is sometimes mistaken for distinct species.
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). Pyrite. My Mineral Box. Retrieved May 23, 2026, from https://mymineralbox.com/mineral-encyclopedia/minerals/pyrite/
MLA
MyMineralBox Editorial Team. "Pyrite." My Mineral Box, 2026, https://mymineralbox.com/mineral-encyclopedia/minerals/pyrite/. Accessed May 23, 2026.
Chicago
MyMineralBox Editorial Team. "Pyrite." My Mineral Box. Last modified May 4, 2026. https://mymineralbox.com/mineral-encyclopedia/minerals/pyrite/.
BibTeX
@misc{mmb_pyrite,
author = {{MyMineralBox Editorial Team}},
title = {{Pyrite}},
year = {2026},
publisher = {My Mineral Box},
url = {https://mymineralbox.com/mineral-encyclopedia/minerals/pyrite/},
urldate = {2026-05-23}
}
Identification & care
Specimens usually show cubic, octahedral, pyritohedral; striated cube faces; massive, nodular. Its color is typically pale brass-yellow. The luster is metallic, the streak is greenish-black to brownish-black, and specimens are typically opaque. The cleavage is poor/indistinct on {001}. The fracture is irregular/uneven, conchoidal, which aids identification.
Collector context
How it forms
In terms of geology, Pyrite forms in hydrothermal veins, sedimentary (diagenetic), metamorphic, magmatic. It is commonly found in association with galena, sphalerite, chalcopyrite, quartz, calcite.
Classic Chinese localities
Pyrite also appears as a secondary or late-stage occurrence at 1 additional Chinese localities.
Why collectors care
Pyrite is among the most visually dramatic sulfides and native metals a collector can own. Bright metallic faces, sharp crystal geometry, and good matrix contrast make a single well-selected piece carry an entire cabinet; luster integrity and termination sharpness ultimately define its collector value.
What affects value
Value in Pyrite is assessed, in typical order of weight, against: (1) locality provenance; (2) crystal size; (3) termination quality and crystal completeness; (4) metallic luster integrity (absence of tarnish); (5) crystal habit elegance (parallel, radiating, or bladed); (6) matrix contrast and aesthetic balance; (7) condition and absence of re-attached crystals. Verified locality documentation and absence of cleaning residue act as strong multipliers across the above.
Naming history
The name Pyrite 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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