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UnderstandWhat it is, what people ask, how far this page goes
Natural inorganic gem materials · Mineral species · Natural identity; treatment status unknown
Pyrite
Also known asFool’s gold
A mineral species with the formula FeS2; its edges are fairly brittle, and care is needed when wearing it with sweat or in damp conditions. This page compares how the major standards and institutions name it, what must be disclosed when selling it, whether it can be worn every day, how it is treated and identified, and which source each conclusion comes from.
Price, rarity and origin are outside the scope of this wiki.
Questions people ask about Pyrite
Every sentence below is followed by the registered fact it rests on; answers add no new facts and promise no outcome.
Q1Is pyrite the same as fool's gold, and how does it differ from gold?
Yes: pyrite is pale brass-yellow with a bright metallic lustre and is nicknamed fool's gold because it is often mistaken for gold.Handbook of MineralogyIts streak is greenish black to brownish black.Handbook of MineralogyChemically it is iron sulfide, FeS2.Handbook of Mineralogy
Q2Can pyrite get wet, and why does it sometimes crumble?
Above 60% relative humidity pyrite reacts with moisture in the air, forming hydrated iron sulphate and possibly a weak sulphuric acid.NatSCA Care and Conservation of Geological Specimens (2013)Natural history conservators advise keeping pyrite below 60% relative humidity, ideally at 45% or less, because this so-called pyrite decay can reduce a specimen to powder.NatSCA Care and Conservation of Geological Specimens (2013)
Q3How hard and durable is pyrite?
Its hardness is recorded as Mohs 6–6.5.Handbook of MineralogyIt is brittle.Handbook of MineralogyIt breaks with a conchoidal to uneven fracture.Handbook of Mineralogy
Q4How does pyrite form?
Pyrite is the most abundant and widespread sulfide mineral.Handbook of MineralogyIt forms under very varied conditions: in hydrothermal veins and magmatic segregations, in igneous rocks and pegmatites, in metamorphic rocks, and by replacement within sedimentary rocks.Handbook of Mineralogy
Q5Why is pyrite gold-coloured?
Its pale brass-yellow colour and metallic lustre arise from its iron sulfide composition.Handbook of MineralogyCIBJO describes the colour as metallic yellow with a brassy appearance.CIBJO Gemmological Laboratories Book 2024
Q6What does pyrite symbolize, and does it have healing powers?
There is no scientific evidence that pyrite has healing powers: the UK advertising regulators ASA and CAP state that they have not seen evidence that crystal therapy can treat medical conditions.ASA/CAP guidance (UK)What is recorded is the origin of its name: it comes from the Greek for fire, because striking the mineral can give off sparks.Handbook of Mineralogy
Sources cited in these answers ASA/CAP guidance (UK)
What this page can answer
This page covers
- How Pyrite forms and what gives its colourFormation setting, process and timescale; where its colour and optical effects come from, each finding graded and sourced
- How to identify PyriteHow far lab testing can go and whether a synthetic exists
- Caring for and wearing PyriteCleaning, heat, chemicals and light, as the cited sources give them; durability indicators and wearing advice
- Mohs hardness of PyriteEach value with its source and check date
- Pyrite in English, Chinese and Japanese; national standard namesNames in four languages, the GB/T standard name and the suggested listing name; and: Which of GIA, FTC, CIBJO and Gem-A have a name for it on record, and do those agree?
- Name origin and history of PyriteWhere the name comes from; how people have used it, with museum objects
- Listing and disclosing PyriteThe listing name to use; what must be disclosed before sale
- Standard clauses that define PyriteWhich clause defines it, each cross-checked
What we cannot conclude
- Whether one particular bead is natural, treated or synthetic — only a laboratory report can settle that.
- Geographic origin, unless an origin report accompanies the item.
- Price, rarity or investment value: this wiki covers naming and disclosure only.
Material research: formation, causes and history
What authoritative sources say about how this material forms, what causes its colour and optical effects, where its name comes from and how people have used it. Each statement carries an evidence grade and its sources; it describes the material in general, not any specific piece.
How it forms
Pyrite (FeS2) is the most abundant and widespread sulfide mineral. It forms under a wide variety of conditions: as very large hydrothermal vein bodies, magmatic segregations, an accessory mineral in igneous rocks and pegmatites, in contact metamorphic deposits and metamorphic rocks, and as diagenetic replacements in sedimentary rocks. Pyrite is cubic, dimorphous with marcasite, forms a series with cattierite, and belongs to the pyrite group. Its crystals are typically cubic, pyritohedral, and octahedral, with a pale brass-yellow color and metallic luster.
Scope: Covers the origin, occurrence and composition of natural pyrite as a mineral species; does not address synthetic iron disulphide or trade claims about gold-bearing pyrite.
Sources Handbook of Mineralogy
Where it forms
Hydrothermal veins and magmatic segregations; an accessory phase within igneous rocks and pegmatites
Sources Handbook of Mineralogy
Deposits of contact-metamorphic origin, together with metamorphic rocks
Sources Handbook of Mineralogy
Through diagenetic replacement within sedimentary rocks
Sources Handbook of Mineralogy
How it forms, step by step
In hydrothermal and magmatic environments, iron and sulfur combine and precipitate in large amounts to form pyrite.
Sources Handbook of Mineralogy
During contact metamorphism and metamorphism, pyrite occurs as an accessory mineral or as ore bodies.
Sources Handbook of Mineralogy
During diagenesis in sedimentary rocks, pyrite forms by replacement (e.g., framboidal or globular aggregates).
Sources Handbook of Mineralogy
Link to appearance
Pyrite is pale brass-yellow with a metallic, splendent luster and a greenish black to brownish black streak; it is nicknamed 'fool's gold' because it is often mistaken for gold. Its crystals are typically cubic, pyritohedral, and octahedral, with granular, globular, and framboidal aggregates and striations conforming to pyritohedral symmetry.
Sources Handbook of Mineralogy
Timescale
The source states no absolute geological timescale for pyrite formation.
Sources Handbook of Mineralogy
Supporting findings
Pyrite is produced under very varied conditions: in hydrothermal veins and magmatic segregations; as an accessory phase within igneous rocks and pegmatites; in contact-metamorphic and metamorphic rocks; and through diagenetic replacement within sedimentary rocks.
Evidence grade BScope: Describes pyrite's diverse natural formation pathways.
Sources Handbook of Mineralogy
Recorded localities
Authoritative sources list the localities below; the list is not exhaustive.
Asia
- Aktchitao, KazakhstanExact position not given; not plotted
Sources Handbook of Mineralogy
Europe
- Rio Marina, Elba, Italy
Sources Handbook of Mineralogy
- Traversella, Piedmont, Italy
Sources Handbook of Mineralogy
- Navajún, La Rioja, SpainAs printed: Ambasaguas and Navajun, Logroño Province
Sources Handbook of Mineralogy
North America
- Ibex mine, Leadville, Lake County, Colorado, United States
Sources Handbook of Mineralogy
- Sparta, Randolph County, Illinois, United StatesPyrite “suns”
Sources Handbook of Mineralogy
- Santo Niño mine, near Duquesne, Santa Cruz County, Arizona, United States
Sources Handbook of Mineralogy
- French Creek mines, Chester County, Pennsylvania, United States
Sources Handbook of Mineralogy
- Carleton talc mine, Chester, Windsor County, Vermont, United States
Sources Handbook of Mineralogy
- Butte, Silver Bow County, Montana, United States
Sources Handbook of Mineralogy
- Spruce claim, King County, Washington, United States
Sources Handbook of Mineralogy
- Buick mine, Bixby, Iron County, Missouri, United States
Sources Handbook of Mineralogy
South America
- Quiruvilca mine, La Libertad, Peru
Sources Handbook of Mineralogy
- Huanzala, Huánuco, Peru
Sources Handbook of Mineralogy
Seas and coasts
- WorldwideThe most abundant and widespread sulfide
Sources Handbook of Mineralogy
These are localities recorded by authoritative sources, not an origin finding for any individual piece. The CIBJO Gemstone Book (2022, §4.2.3) says a place of origin names where a gem was mined or harvested, is a matter of opinion, does not imply a level of quality, and that cutting, processing or exporting centres must not be used to imply origin. See how far testing can go on this page, the origin determination guide and the overview of recorded localities.
Causes of colour and optical effects
Pyrite is pale brass-yellow with a greenish black to brownish black streak and metallic, splendent luster, its color and luster arising from its iron sulfide composition.
Evidence grade BScope: Describes the compositional basis of pyrite's color.
Sources Handbook of Mineralogy
Where the name comes from
Pyrite's name is Greek for "fire", since striking the mineral can give off sparks.
Evidence grade BScope: This states only the origin of the name and does not establish the material's composition, locality, natural origin, or whether it was treated.
Sources Handbook of Mineralogy
Human use and museum objects
Only four collection objects are recorded as pyrite, all from the Americas (Met 1987.394.28 Moche owl; Met 1979.206.1064 Chiriquí pendant; Met 1979.206.1015 Huastec earflare frontal, inlays probably pyrite; and Cleveland 1989.65 mirror back), the 'probably pyrite' notation retaining its uncertainty; the sparse evidence cannot summarise a general history of use.
Evidence grade AScope: Applies to the few American collection objects labelled pyrite; the museum's 'probably pyrite' notation retains its uncertainty, with no further inference drawn.
Sources The Met 1987.394.28 · The Met 1979.206.1064 · The Met 1979.206.1015 +1
Only four objects in the collection are explicitly recorded as pyrite, all from the Americas (Andean and Mesoamerican), with no Old World ancient instance. A Moche 'Owl' from Peru (Met 1987.394.28, 6th-7th century CE) includes pyrite; a Chiriquí crocodile-head pendant from Costa Rica (1979.206.1064, 700-1550 CE) is inlaid with pyrite. A Huastec earflare frontal from Mexico (1979.206.1015, 900-1300 CE) is recorded as 'iron-based metal (inlays probably pyrite)', an uncertainty retained here; and the Cleveland Museum of Art's 'Mirror Back with Great Goddess' (1989.65, 400-550 CE) was originally inlaid on the reverse with a polished pyrite mirror. Pyrite here serves mainly as a reflective mirror surface or inlay. The evidence is sparse and is reported as it stands.
Sources The Met 1987.394.28 · The Met 1979.206.1064 · The Met 1979.206.1015 +1
Scope: A museum object evidences only the existence and date of that artefact itself; it does not establish widespread ancient use of the material, nor does it attest the origin, naturalness, or treatment of any modern specimen.
Objects cited
- The Met 1987.394.28Silvered copper, shell, pyrite
- The Met 1979.206.1064Gold (cast alloy), pyrite inlay, hematite
- The Met 1979.206.1015Shell, red pigment (cinnabar), iron-based metal (inlays probably pyrite)
- Cleveland Museum of Art 1989.65slate, pigment; other side originally inlaid with polished pyrite mirror
Other research findings
Pyrite has the formula FeS2, is dimorphous with marcasite, forms a series with cattierite, and belongs to the pyrite group.
Evidence grade BScope: Concerns pyrite's composition, polymorphism, and group.
Sources Handbook of Mineralogy
Pyrite's name derives from the Greek word for fire, because sparks can be struck from the stone.
Evidence grade BScope: Concerns the name's origin, not genesis.
Sources Handbook of Mineralogy
Pyrite is the most abundant and widespread sulfide mineral.
Evidence grade BScope: Describes pyrite's overall abundance status.
Sources Handbook of Mineralogy
Limits of this research
- Research status: Formation, occurrence or other material-specific findings found in authoritative sources
- The source states no absolute age or specific P-T values for pyrite formation.
Methodology
- Origin determination and its limits
- Quality grading and value factors
- How gemmology became a technical discipline
Evidence grades
- A
- Standards bodies, government geological surveys, peer-reviewed research and museum records
- B
- Institutional educational material
- C
- Specialist databases or cautious readings
A statement is never graded above its strongest source.
This section is LumaLark's own factual restatement of public authoritative sources, credited item by item; it contains no verbatim excerpts, images or third-party logos.
DecideListing name, disclosure, care and treatments
- Suggested listing name
- Pyrite
GB/T 16552—2017 5.1.1 b) · CIBJO Gemmological Laboratories Book 2024 §7.2.1.187 “Pyrite”
Construction or treatment status
Natural identity; treatment status unknown
Related:Disclosure and cautions
This page cannot answer
Natural? · Origin · Price
A lab report settles these; this wiki covers naming and disclosure.
Related:What this page can answer
Answer at a glance
Pyrite is Pyrite (FeS2); use "Pyrite" for listings, and disclose any known treatments.
What this means for you
Before buying, check the recommended listing name "Pyrite" and any disclosed treatments on this page, and ask the seller for a grading report if in doubt.
Known uncertainty
- Last reviewed
- 2026-09-01
Care and wear
Care
Pyrite — care (chemicals): Above 60% humidity, pyrite reacts with moisture in the air, producing hydrated iron sulphate and potentially a weak sulphuric acid.
NatSCA Care and Conservation of Geological Specimens (2013)
- Treatment state
- any treatment state
Source & check 2026-10-06
- Source
- Icon & NatSCA, “Care and conservation of geological specimens” (leaflet, 2013): p.1, body text (locator checked 2026-10-06)
- Fact checked on
- 2026-10-06
Pyrite — care (storage): Specimens containing pyrite should be kept below 60% relative humidity, ideally at 45% or less; so-called pyrite decay can strike rocks, fossils and minerals alike, reducing a specimen to powder.
NatSCA Care and Conservation of Geological Specimens (2013)
- Treatment state
- any treatment state
Source & check 2026-10-06
- Source
- Icon & NatSCA, “Care and conservation of geological specimens” (leaflet, 2013): p.1, body text (locator checked 2026-10-06)
- Fact checked on
- 2026-10-06
Each row's “Source & check” expands to the full source; the date beside it is the fact check date.
Common care questions and matching entries
Each question links to the matching entries on this page; whether they answer it fully, go by the entry wording.
This table scrolls sideways on narrow screens.
| Question | Matching entries |
|---|---|
| Contact with acids, alkalis and household chemicals | Above 60% humidity, pyrite reacts with moisture in the air, producing hydrated iron sulphate and potentially a weak sulphuric acid |
Durability and wearing
Numbers in curly braces, such as {111}, are crystallographic face symbols (Miller indices): each marks a set of crystal faces or cleavage planes. They are reproduced as written in the cited source.
Mohs hardness
6–6.5
Toughness
Brittle
Cleavage
Indistinct on {001}; partings on {011} and {111}, indistinct
VerifyNames, standards, technical facts, clauses and sources
Names
Besides Pyrite, the name register records "Fool’s gold", for which no restriction on use as a name is recorded.
Standard and listing namesPyrite is not listed in GB/T 16552—2017 Annex A, and the mineral/material name that can be used directly under GB/T 16552—2017 is pyrite; the suggested listing name is also Pyrite. Trade and mineralogical namesThe mineralogical name is Pyrite, formula FeS2; the trade name or synonym Fool’s gold is also a market name. Japanese namesThe formal name of Japan's GSJ is written in Japanese. Names in four languagesFour-language names are given in Simplified Chinese, Traditional Chinese, English (Pyrite) and Japanese. Institution usageOn authority wording, CIBJO Gemmological Laboratories Book 2024 records Pyrite; the FTC text on file has no wording for this name (checked); GIA and Gem-A are unchecked; bodies without a recorded wording show the entry's own English name, which does not represent their position.
Name register
Every name recorded for this entry, with how it is classified, whether it may be matched to this entry automatically, whether it may be used as a product name, and the clause it rests on.
This table scrolls sideways on narrow screens.
| Name | Type | Matching | Use as a name | Basis |
|---|---|---|---|---|
| no restriction recorded (1) | ||||
| Fool’s goldEnglish | market name | matched automatically | no restriction recorded | editorial ruling (no clause cited) |
How each authority words this name: see Names › Authority wording.
- GSJ (Japan) formal name
- 黄鉄鉱
- Mineral / material name (not in GB/T 16552 Annex A; usable directly)
- 黄铁矿 (GB/T 16552—2017 §5.1.1 b))
- Mineralogical name
- Pyrite (FeS2)
- Trade names and synonyms
- Fool’s gold (market name)
Four-language names
- 简体中文
- 黄铁矿
- 繁體中文
- 黃鐵礦
- English
- Pyrite
- 日本語
- パイライト/黄鉄鉱
See also: Misleading and prohibited trade names · Supplementary name index
Classification
- Origin
- Natural materials
- Material domain
- Natural inorganic gem materials
- Browsing family
- Sulfide minerals
- Identity tier
- Mineral species
- Mineral chemical class
- Sulfides / sulfosalts
- Construction or treatment status
- Natural identity; treatment status unknown
What it is and how it's identified
The IMA nomenclature status of Pyrite is G, meaning grandfathered: described before the IMA existed and generally regarded as a valid mineral species. The composition (phase) is registered as pyrite; transparency opaque; the body colour of untreated Pyrite is metallic yellow, with a brass-like appearance. This site notes that in chapter 7 of the CIBJO Gemmological Laboratories Book, the colour descriptions for entries such as heliodor, chrysoprase and demantoid also mention yellow or yellowish colours.
Registered material facts
Each row carries its own source and check date and can be cited on its own; “—” means the cited source gives no value, not “none”.
Definition
Pyrite — nomenclature status: IMA status G: grandfathered (described before the IMA existed, and generally regarded as a valid species).
CIBJO Gemmological Laboratories Book 2024
Source & check 2026-09-22
- Source
- Fact checked on
- 2026-09-22
Pyrite — composition (phase): pyrite
CIBJO Gemmological Laboratories Book 2024
Source & check 2026-09-22
- Source
- Fact checked on
- 2026-09-22
Optical
Pyrite — transparency: opaque.
CIBJO Gemmological Laboratories Book 2024
Source & check 2026-09-22
- Source
- Fact checked on
- 2026-09-22
Pyrite — body colour: metallic yellow (brassy appearance).
CIBJO Gemmological Laboratories Book 2024
- Treatment state
- untreated
- Qualification
In chapter 7 of the CIBJO Gemmological Laboratories Book, the colour descriptions of Heliodor / Golden Beryl, Chrysoprase, Demantoid and other entries also name yellow or a yellowish colour.
- General note
- colour alone is not identity
Source & check 2026-09-26
- Source
- Fact checked on
- 2026-09-26
Each row's “Source & check” expands to the full source; the date beside it is the fact check date.
Testing and market
The tests the CIBJO laboratory protocol requires for this material, and what each method means, are in the protocol table on the laboratory testing page: §6.1.64.
How far testing can go
Pyrite — synthetic counterpart on the market: No synthetic counterpart of this material is commercially available
CIBJO Gemstone Book 2022
- Treatment state
- any treatment state
Source & check 2026-09-22
- Source
- Fact checked on
- 2026-09-22
Pyrite — what the CIBJO laboratory protocol says to watch for: marcasite (misnomer), steel imitation
CIBJO Gemmological Laboratories Book 2024
- Treatment state
- any treatment state
Source & check 2026-09-26
- Source
- Fact checked on
- 2026-09-26
Each row's “Source & check” expands to the full source; the date beside it is the fact check date.
Clause-level definitions
The clause-level definition of Pyrite is registered under the term Pyrite, with the clause being the IMA mineral list entry; the visible definition reads Pyrite FeS2 G ?. The cross-check is against the main table of the RRUFF/IMA mineral list and is noted as public-domain data.
This table scrolls sideways on narrow screens.
| Term | Clause | Definition | Cross-check |
|---|---|---|---|
| Pyrite | IMA Mineral List entry | Pyrite FeS2 G ? | Cross-checked against the RRUFF/IMA master mineral list (public domain data). |
Evidence and sources
Authority basis and clause sources
Sources
Further reading
Related entries and topic cluster
Parent entry and related pages on this site. Rows marked “Planned” are suggested new content and have no link yet.
This table scrolls sideways on narrow screens.
| Page | Content | Status |
|---|---|---|
| Browsing family | Sulfide minerals | Live |
| Related articles | To be added (placeholder) | Planned |
Who maintains this page
The material facts in the Pyrite entry are maintained by the LumaLark wiki and matched one by one to the standard clauses or institutional sources they cite: every fact carries its source (with a clause or page locator) and a check date, so it can be traced back to the original; clause-level definitions also carry a cross-check result. The entry exists so that buyers and sellers can check naming, disclosure and material facts item by item.