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Green Onyx

Sedimentary Rock (Metamorphic in some contexts due to recrystallization)

Banded Calcite (often marketed as Onyx Marble or Green Onyx)

Also known as: Onyx Marble, Mexican Onyx, Calcite Onyx, Oriental Alabaster

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Description

Green Onyx is a variety of banded calcite, a carbonate mineral. Despite its common market name, it is not true onyx, which is a cryptocrystalline quartz (chalcedony). It is characterized by its distinctive parallel bands of varying shades of green, often interlayered with white, yellow, or brown bands. The green color can range from pale mint to deep forest green. It is relatively soft compared to true onyx, with a Mohs hardness of 3. Its translucent to transparent nature allows light to pass through, enhancing its aesthetic appeal. It is composed primarily of calcium carbonate and reacts readily with acids.

How to Identify

Color
Ranges from pale mint green to deep forest green, often with white, yellow, or brown bands. The green is typically uniform within a band but varies between bands.
Luster
Vitreous (glassy) to waxy on fresh surfaces, can be dull on weathered surfaces.
Texture
Fine-grained to medium-grained, often with a smooth, polished feel. The banding is a key textural feature.
Crystal Form
Typically massive, microcrystalline to cryptocrystalline aggregates, forming stalactitic, stalagmitic, or layered structures. Individual calcite crystals are usually too small to be seen without magnification.
Cleavage
Perfect rhombohedral cleavage in three directions, though often not visible in massive, fine-grained specimens.
Geological Environment
Forms in karst environments (caves) as speleothems (stalactites, stalagmites, flowstone) or in hot spring deposits (travertine). It is a secondary mineral formed by the precipitation of calcium carbonate from groundwater or hydrothermal fluids.

Key Facts

  • Hardness: 3 (Mohs scale)
  • Specific Gravity: 2.71 g/cm³
  • Crystal System: Trigonal
  • Color: Various shades of green, often banded with other colors.
  • Luster: Vitreous to waxy.
  • Transparency: Translucent to transparent.
  • Fracture: Conchoidal to uneven.
  • Cleavage: Perfect rhombohedral in three directions at 74°55'.
  • Composition: Calcium Carbonate (CaCO3).

Quick Check

  • Color: Green, often banded with white, yellow, or brown.
  • Luster: Vitreous to waxy.
  • Streak: White.

Physical Characteristics

  • Crystal Habit: Massive, stalactitic, stalagmitic, columnar, granular, fibrous, lamellar, or rhombohedral crystals (rarely macroscopic).
  • Cleavage Type: Perfect rhombohedral.
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) to waxy.

Formation

Green Onyx, or banded calcite, forms through the precipitation of calcium carbonate (CaCO3) from cold or hot aqueous solutions. This process typically occurs in caves as stalactites and stalagmites (speleothems), or in hot springs as travertine. The banding, which gives it its 'onyx' appearance, results from variations in the mineral content, growth rate, and water chemistry during deposition. The green coloration is usually due to the presence of trace amounts of other minerals, such as chlorite, serpentine, or iron silicates, incorporated during its formation.

Usage

Primarily used as an ornamental and decorative stone in architecture, interior design, and sculpture. It is fashioned into tiles, countertops, sinks, decorative objects, and carvings. Its translucent quality makes it popular for backlit applications. It is also used in jewelry, though less commonly than true onyx (a chalcedony variety), due to its relative softness.

Age Distribution

Varies widely, from Cenozoic to Precambrian, depending on the specific geological formation and depositional environment.

Where to Find

Mexico

Known for significant deposits, particularly in the states of Puebla and Oaxaca, producing a wide range of colors including green.

Pakistan

A major source of green onyx, particularly from the Balochistan province, known for its vibrant green hues.

Iran

Historically a significant producer of 'onyx marble' (banded calcite), with various colorations including green.

Turkey

Contains numerous travertine and cave deposits that yield banded calcite suitable for ornamental use.

Egypt

Ancient quarries in Egypt produced 'Egyptian alabaster,' which is a form of banded calcite, sometimes with greenish tints.

USA

Deposits can be found in various states with karst topography or hot springs, such as Arizona, California, and Utah, though commercial production of green varieties is less prominent.

Finding Tips

Look for Karst Topography

Focus on regions with limestone bedrock, caves, and active or ancient hot springs, as these are the primary environments for banded calcite formation.

Identify Banding

The most distinctive feature is the parallel banding. Look for layers of varying color and translucency. This differentiates it from massive, unbanded calcite.

Perform an Acid Test (Carefully)

Calcite effervesces vigorously with dilute hydrochloric acid (HCl). A small drop will produce bubbles. This is a definitive test to distinguish it from true onyx (quartz), which does not react. Always wear appropriate safety gear and use a small, inconspicuous area.

Check Hardness

Green Onyx (calcite) has a Mohs hardness of 3, meaning it can be scratched by a copper coin or a steel knife. True onyx (quartz) has a hardness of 7 and cannot be scratched by these tools.

Observe Translucency

Many varieties of green onyx are translucent, allowing light to pass through, especially in thinner sections. Hold a thin piece up to a light source to observe this characteristic.

Similar Rocks

True Onyx

Banded Chalcedony (SiO2)

Also known as: Black Onyx, Sardonyx

Marble

Recrystallized Calcite (CaCO3)

Also known as: Calcite Marble

Travertine

Porous Calcite (CaCO3)

Also known as: Tufa

Serpentine

Magnesium Silicate (e.g., Antigorite, Lizardite)

Also known as: New Jade

Scientific Classification

Mineral Class
Carbonates
Group
Calcite Group
Crystal System
Trigonal
Chemical Formula
CaCO3
Composition
Calcium Carbonate. Trace elements (e.g., iron, magnesium, manganese, copper, or organic matter) can substitute for calcium or be present as inclusions, influencing color. The green color is often due to chlorite, serpentine, or iron silicates.

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