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Chrysoprase

Mineral (variety of Chalcedony)

Chalcedony (cryptocrystalline quartz) with nickel inclusions

Also known as: Australian Jade (misnomer), Green Chalcedony

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Description

Chrysoprase is a beautiful, translucent to opaque variety of chalcedony, which is a cryptocrystalline form of quartz. Its distinctive apple-green to deep green color is caused by minute inclusions of nickel-bearing minerals. It is highly valued for its vibrant color and is often cut and polished for use in jewelry and decorative items. Unlike emerald, which owes its green color to chromium, chrysoprase's color is due to nickel, making it a distinct and unique green gemstone.

How to Identify

Color
Apple-green to deep green, sometimes yellowish-green. The color is typically uniform but can show slight banding or mottling.
Luster
Vitreous to waxy, dull on unpolished surfaces.
Texture
Smooth, microgranular, conchoidal fracture surfaces.
Crystal Form
Cryptocrystalline aggregates, typically massive, botryoidal, or stalactitic. Individual crystals are microscopic and not visible to the naked eye.
Cleavage
None, due to its cryptocrystalline nature.
Geological Environment
Found in weathered zones of nickel-rich ultramafic rocks (e.g., serpentinites, dunites) and lateritic nickel deposits. Often associated with magnesite, opal, and other secondary minerals.

Key Facts

  • Hardness: 6.5-7 on the Mohs scale
  • Specific Gravity: 2.58-2.64
  • Crystal System: Trigonal (as quartz, but cryptocrystalline aggregates appear amorphous)
  • Color: Apple-green, yellowish-green, deep green
  • Luster: Vitreous to waxy
  • Transparency: Translucent to opaque
  • Fracture: Conchoidal to uneven
  • Cleavage: None
  • Composition: Silicon dioxide (SiO2) with trace nickel (Ni) impurities

Quick Check

  • Color: Apple-green to deep green
  • Luster: Waxy to vitreous
  • Streak: White

Physical Characteristics

  • Crystal Habit: Massive, botryoidal, stalactitic, nodular aggregates. Individual crystals are microscopic.
  • Cleavage Type: None
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Vitreous to waxy

Formation

Chrysoprase forms as a secondary mineral in the weathered zones of nickel-bearing ultramafic rocks (e.g., serpentinites, dunites, peridotites) and lateritic nickel deposits. The green color is attributed to trace amounts of nickel silicate minerals, primarily bunsenite (NiO) or garnierite (a general term for nickel-bearing serpentine or talc-like minerals), finely dispersed within the cryptocrystalline quartz matrix. It typically occurs in veins, nodules, and as infillings in fractures.

Usage

Primarily used as a gemstone for cabochons, beads, carvings, and ornamental objects due to its attractive apple-green to deep green color and good polish. Historically, it has been used in jewelry since antiquity.

Age Distribution

Typically found in weathered and altered ultramafic rocks, which can range in age from Precambrian to Cenozoic, depending on the specific geological setting.

Where to Find

Marlborough, Queensland, Australia

One of the most significant and historically important sources, known for producing high-quality, vibrant apple-green chrysoprase.

Silesia, Poland

Historically a major source, particularly from the Szklary deposit, known for its good quality material.

California, USA

Deposits found in areas with serpentinite bodies, such as Tulare County.

Brazil

Various occurrences, often associated with lateritic nickel deposits.

Russia (Urals)

Known for some occurrences in nickel-rich areas.

Tanzania

Newer sources have emerged, producing good quality material.

Finding Tips

Geological Context

Focus on areas with known ultramafic rock formations (serpentinites, peridotites) that have undergone significant weathering and lateritization. Look for nickel-rich environments.

Associated Minerals

Chrysoprase often occurs with magnesite, opal, and other secondary minerals in veins and fracture fillings. The presence of these minerals can be an indicator.

Color and Luster

Look for the characteristic apple-green to deep green color. Freshly broken surfaces will have a waxy to dull luster, while polished surfaces are vitreous.

Hardness Test

Chrysoprase has a Mohs hardness of 6.5-7, meaning it can scratch glass and steel. This helps differentiate it from softer green minerals.

Translucency

Good quality chrysoprase is typically translucent, allowing some light to pass through, especially on thinner edges.

Similar Rocks

Jade (Nephrite or Jadeite)

Nephrite (calcium magnesium iron silicate) or Jadeite (sodium aluminum silicate)

Also known as: Greenstone

Green Aventurine

Quartz with Fuchsite inclusions

Also known as: Indian Jade (misnomer)

Serpentine

Magnesium iron silicate hydroxide

Also known as: New Jade (misnomer)

Prase

Quartz with actinolite or chlorite inclusions

Also known as: Leek-green Quartz

Scientific Classification

Mineral Class
Silicate (Tectosilicate)
Group
Quartz Group (Chalcedony variety)
Crystal System
Trigonal (for quartz, but cryptocrystalline)
Chemical Formula
SiO2 (with Ni as a chromophore)
Composition
Silicon dioxide with trace amounts of nickel silicate minerals (e.g., bunsenite, garnierite) responsible for the green color.

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