Rockby LogoRockby

Quartz with dark inclusions

Mineral (aggregate)

Quartz (SiO2) with unidentified dark mineral inclusions

Also known as: Included Quartz, Phantom Quartz (if inclusions form growth patterns), Tourmalinated Quartz (if inclusions are tourmaline)

Got a photo? Identify rocks instantly with the Rockby app

Open the app

Description

Quartz with dark inclusions refers to specimens of the mineral quartz (silicon dioxide, SiO2) that contain visible, typically small, dark-colored mineral phases embedded within the quartz matrix. The quartz itself is often transparent to translucent, allowing the inclusions to be observed. The nature of these dark inclusions is highly variable and can include a wide array of minerals such as tourmaline (schorl), chlorite, hematite, goethite, rutile (though rutile is typically golden or reddish-brown, dark varieties exist), various sulfides (e.g., pyrite, galena), or even carbonaceous material. The appearance of the inclusions can range from fine dustings, needles, or fibrous aggregates to distinct euhedral or anhedral crystals. The distribution can be random, clustered, or form distinct patterns such as phantoms, where earlier growth stages of the quartz crystal are outlined by layers of inclusions.

How to Identify

Color
Quartz matrix is typically colorless, white, or smoky. Inclusions are dark (black, dark green, dark brown, dark red).
Luster
Vitreous (glassy) for the quartz; inclusions can vary (e.g., sub-metallic for tourmaline, earthy for chlorite).
Texture
Crystalline, often with visible inclusions. Can be massive or form distinct crystals.
Crystal Form
Quartz typically forms hexagonal prisms terminated by rhombohedra. Inclusions can be acicular, fibrous, granular, or euhedral within the quartz.
Cleavage
None for quartz; inclusions may exhibit cleavage depending on the mineral (e.g., tourmaline has poor cleavage).
Geological Environment
Hydrothermal veins, pegmatites, igneous and metamorphic rocks, sedimentary geodes, and alluvial deposits.

Key Facts

  • Hardness: 7 on Mohs scale (for quartz). Inclusions may have different hardnesses but are protected by the quartz.
  • Specific Gravity: 2.65 g/cm³ (for quartz). Slightly higher if dense inclusions are abundant.
  • Crystal System: Trigonal (for quartz).
  • Color: Colorless, white, or smoky quartz with dark (black, dark green, dark brown) inclusions.
  • Luster: Vitreous.
  • Transparency: Transparent to translucent.
  • Fracture: Conchoidal.
  • Cleavage: None.
  • Composition: SiO2 (quartz) with various dark mineral inclusions (e.g., tourmaline, chlorite, hematite, goethite, sulfides, carbonaceous matter).

Quick Check

  • Color: Colorless to smoky quartz with black, dark green, or dark brown internal specks, needles, or masses.
  • Luster: Vitreous (glassy) for the quartz.
  • Streak: White (for quartz); streak of inclusions is usually not observable due to their small size and enclosure within quartz.

Physical Characteristics

  • Crystal Habit: Prismatic, often terminated by rhombohedra; massive, granular. Inclusions can be acicular, fibrous, platy, or granular.
  • Cleavage Type: None (for quartz).
  • Fracture Type: Conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous.

Formation

Quartz with dark inclusions forms under a wide range of geological conditions. The quartz itself crystallizes from silica-rich fluids (hydrothermal veins, pegmatites, igneous intrusions) or precipitates from aqueous solutions (sedimentary environments, geodes). The dark inclusions are typically pre-existing minerals that were trapped during the growth of the quartz crystal, or they crystallized contemporaneously with the quartz from the same fluid. The specific mineral forming the inclusions depends entirely on the local geological environment and the chemical composition of the parent fluid or rock.

Usage

Primarily ornamental (jewelry, carvings, decorative objects), metaphysical practices. Scientific interest for studying mineral growth and fluid inclusions.

Age Distribution

Ubiquitous throughout geological time, from Precambrian to Cenozoic, wherever quartz forms.

Where to Find

Brazil

Known for large quartz crystals with various inclusions, including tourmaline and chlorite.

Arkansas, USA

Produces clear quartz with occasional dark inclusions, often associated with hydrothermal veins.

Himalayan regions (e.g., Nepal, Pakistan)

Source of high-quality quartz, sometimes with dark mineral inclusions, particularly chlorite and tourmaline.

Alps (e.g., Switzerland, France)

Classic localities for well-formed quartz crystals, including those with dark inclusions.

Madagascar

Diverse range of quartz varieties, including those with various dark inclusions.

Finding Tips

Look for transparency

Seek out quartz specimens that are transparent or translucent enough to clearly see the internal dark inclusions.

Examine crystal faces

Well-formed quartz crystals often provide the best views of inclusion patterns, such as phantoms.

Check hydrothermal veins and pegmatites

These geological settings are prime locations for the formation of included quartz.

Use magnification

A hand lens or loupe will help in identifying the morphology and distribution of the dark inclusions.

Similar Rocks

Smoky Quartz

Smoky Quartz (SiO2)

Also known as: Morion

Rutilated Quartz

Rutilated Quartz (SiO2 with rutile inclusions)

Also known as: Venus Hair Stone

Chlorite Quartz

Quartz (SiO2) with chlorite inclusions

Also known as: Green Phantom Quartz

Tourmalinated Quartz

Quartz (SiO2) with tourmaline inclusions

Also known as: Schorl Quartz

Scientific Classification

Mineral Class
Silicate (Tectosilicate)
Group
Quartz Group
Crystal System
Trigonal
Chemical Formula
SiO2 (with various mineral inclusions)
Composition
Silicon dioxide with varying trace elements and included mineral phases.

Explore Quartz with dark inclusions

Identify rocks anywhere

Free on iOS, Android, and Web. Photo identification, full database, and your personal collection.

Open in app