Marcasite

A variety of Marcasite Group

Uncommon
Marcasite specimen

What is Marcasite?

Marcasite in today's market can be found in antique jewelry stores in pins and other adornments. It wasn't always a desirably accessory, though, and was first famous as a source for sulfur. Chemically, it is identical to pyrite; however, they differ structurally due to differences in development processes.

Uses & Applications

Marcasite was historically mined and refined as a source of sulfur. However, this mineral does not have any practical applications in modern times. Some interesting specimens may be sought out by mineral collectors.

Optical Properties

Pleochroism
None

Discover Values

Rarity
3.9out of 5.0
78%
Popularity
3.6out of 5.0
72%
Beauty
4.0out of 5.0
80%
Cultural Value
4.0out of 5.0
80%
Collection Value
3.9out of 5.0
78%

Market Value Factors

Pricing varies for every rock and mineral, so use these universal factors to gauge Marcasite before comparing listings or appraisals.

Size & Weight

Larger, intact specimens usually command higher prices.

Rarity & Demand

Scarce material or popular varieties sell at a premium.

Condition & Finish

Chips, repairs, and heavy wear lower value; clean prep helps.

Treatment & Provenance

Untreated specimens with documented locality are prized.

Applies to all rocks & minerals.

Marcasite Localities Map

See where Marcasite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview
North ZoneCentral RidgeSouth Basin

Interactive map layers and collecting notes are available in the app.

Key Characteristics

Rock Types of Marcasite

Blueite (S.H.Emmons): Nickel variety of marcasite, found in Denison Drury and Townships, Sudbury Dist., Ontario, Canada. Lonchidite (August Breithaupt): Arsenic variety of marcasite, found at Churprinz Friedrich August Erbstolln Mine (Kurprinz Mine), Großschirma Freiberg, Erzgebirge, Saxony, Germany; ideal formula Fe(S, As)2 . Synonyms for this variety: kausimkies, kyrosite, lonchandite, metalonchidite (Sandberger) described at Bernhard Mine near Hausach (Baden), Germany. Sperkise : designates a marcasite having twin spearhead crystal on {101}. Sperkise derives from the German Speerkies (Speer meaning spear and Kies gravel or stone). This twin is very common in the marcasite of a chalky origin, particularly those from the Cap Blanc Nez.

Formation of Marcasite

Marcasite can be formed as both a primary or a secondary mineral. It typically forms under low-temperature highly acidic conditions. It occurs in sedimentary rocks (shales, limestones and low grade coals) as well as in low temperature hydrothermal veins. Commonly associated minerals include pyrite, pyrrhotite, galena, sphalerite, fluorite, dolomite, and calcite. As a primary mineral it forms nodules, concretions, and crystals in a variety of sedimentary rock, such as in the chalk layers found on both sides of the English Channel at Dover, Kent, England, and at Cap Blanc Nez, Pas de Calais, France, where it forms as sharp individual crystals and crystal groups, and nodules (similar to those shown here). As a secondary mineral it forms by chemical alteration of a primary mineral such as pyrrhotite or chalcopyrite.

Health & Safety Information

  • ⚠️Others
  • ⚠️Marcasite is generally safe to handle. However, it reacts with water or moisture in the air, releasing irritating sulfuric acid. Avoid getting marcasite wet, wash hands after handling it, and store it in a dry place with low humidity (below 60% is ideal). When cutting or polishing marcasite, wear a dust mask to prevent lung irritation from dust inhalation.

More Images

Marcasite specimen
Miguel Calvo
Marcasite specimen
Robert M. Lavinsky
Marcasite specimen
DanielCD

Quick Facts

Physical Properties

Color
Pale brass-yellow, tin-white on fresh exposures
Hardness (Mohs)
6 - 6.5
Density
4.875 g/cm³
Streak
Dark-gray to black
Luster
Metallic, Sub-metallic
Crystal System
Orthorhombic

Chemical Properties

Chemical Formula
FeS2
Elements
Fe, S

Also Known As

MarcasiteAlazaniteCockscomb PyriteIron SulfideKatzengold
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Marcasite FAQs

How do I identify Marcasite?

Marcasite can be identified by its hardness of 6 - 6.5 on the Mohs scale, Pale brass-yellow color, Metallic, Sub-metallic luster, Orthorhombic crystal system. Look for these key characteristics when examining specimens.

What color is Marcasite?

Marcasite typically appears in Pale brass-yellow, tin-white on fresh exposures. Color can vary depending on impurities and formation conditions.

How hard is Marcasite?

Marcasite has a hardness of 6 - 6.5 on the Mohs scale. This gives it moderate hardness.

What is the rock types of marcasite of Marcasite?

Blueite (S.H.Emmons): Nickel variety of marcasite, found in Denison Drury and Townships, Sudbury Dist., Ontario, Canada. Lonchidite (August Breithaupt): Arsenic variety of marcasite, found at Churprinz Friedrich August Erbstolln Mine (Kurprinz Mine), Großschirma Freiberg, Erzgebirge, Saxony, Germany; ideal formula Fe(S, As)2 . Synonyms for this variety: kausimkies, kyrosite, lonchandite, metalonchidite (Sandberger) described at Bernhard Mine near Hausach (Baden), Germany. Sperkise : designates a marcasite having twin spearhead crystal on {101}. Sperkise derives from the German Speerkies (Speer meaning spear and Kies gravel or stone). This twin is very common in the marcasite of a chalky origin, particularly those from the Cap Blanc Nez.

What is the formation of marcasite of Marcasite?

Marcasite can be formed as both a primary or a secondary mineral. It typically forms under low-temperature highly acidic conditions. It occurs in sedimentary rocks (shales, limestones and low grade coals) as well as in low temperature hydrothermal veins. Commonly associated minerals include pyrite, pyrrhotite, galena, sphalerite, fluorite, dolomite, and calcite. As a primary mineral it forms nodules, concretions, and crystals in a variety of sedimentary rock, such as in the chalk layers found on both sides of the English Channel at Dover, Kent, England, and at Cap Blanc Nez, Pas de Calais, France, where it forms as sharp individual crystals and crystal groups, and nodules (similar to those shown here). As a secondary mineral it forms by chemical alteration of a primary mineral such as pyrrhotite or chalcopyrite.

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