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Rock Crystal Natural Chunk High Grade Clear Quartz Mineral Specimen Genuine Crystal

£12.60

High Grade Rock Crystal Natural Chunk – Genuine Clear Quartz Specimen

This stunning High Grade Rock Crystal Natural Chunk is an exceptional example of clear quartz in its raw, unaltered form. The photographs show the exact specimen you will receive, with a 1cm scale cube included to indicate accurate sizing. Every crystal we supply is a 100% genuine natural specimen and comes with a Certificate of Authenticity. This high-quality Rock Crystal chunk is ideal for collectors, interior décor, educational displays, and anyone who appreciates naturally formed mineral beauty.

What Is Rock Crystal?

Rock Crystal is the transparent, colourless variety of Quartz (SiO₂), one of the most abundant and important minerals in the Earth’s crust. It belongs to the trigonal crystal system and is part of the large silicate mineral group. Rock Crystal represents the purest form of quartz, lacking the chemical impurities that produce coloured varieties such as amethyst, citrine, or rose quartz.

Its name derives from the ancient Greek word krýstallos, meaning “ice,” as early cultures believed it was frozen water that could never melt. Today it remains highly valued for its clarity, structure, and geological significance.

Geological Origin and Formation Process

Rock Crystal forms in a wide range of geological environments, most commonly in:

  • Hydrothermal veins, where superheated, silica-rich fluids fill fractures deep underground
  • Pegmatites, coarse-grained igneous bodies that produce large, well-formed crystals
  • Geodes and vugs, hollow cavities lined with crystals
  • Metamorphic environments, where heat and pressure enable recrystallisation

Quartz crystals grow slowly over millions of years as silica precipitates from mineral-rich solutions. The resulting crystal may develop:

  • Six-sided prismatic faces
  • Sharp natural terminations
  • Parallel growth striations
  • Internal rainbows or light-scattering planes

Even as a natural chunk rather than a terminated point, this specimen retains the internal clarity and structural features associated with high-grade quartz.

Crystal Habit, Structure, and Appearance

Quartz grows in a hexagonal prismatic habit, often forming clusters or intergrown masses. This natural chunk may show:

  • Partial crystal faces, indicating its original growth orientation
  • Translucent to transparent zones, depending on internal purity
  • Fractured yet naturally healed features, revealing geological stress history
  • Subtle rainbow refractions, caused by internal micro-fractures
  • Glass-like lustre, especially on smoother surfaces

High Grade Rock Crystal is selected for its superior clarity, structural integrity, and minimal internal clouding—qualities clearly visible in this specimen.

Colour Variations and Natural Inclusions

Although Rock Crystal is typically colourless, minor internal features contribute to its individual character. These may include:

  • Feather-like inclusions, formed during rapid growth stages
  • Light-scattering planes, producing subtle flashes under direct light
  • Thin internal veils or phantoms, recording pauses in crystal development
  • Minute mineral particles, naturally trapped during formation

These inclusions do not detract from the specimen’s quality; rather, they enhance its geological uniqueness.

Mineralogical Properties

Quartz is known for its durability and optical beauty. Key mineral properties include:

  • Chemical composition: SiO₂ (silicon dioxide)
  • Hardness: 7 on the Mohs scale
  • Crystal system: Trigonal
  • Cleavage: Indistinct; conchoidal fracture
  • Lustre: Vitreous
  • Transparency: Transparent to translucent

Its hardness makes quartz resistant to scratching, while its internal structure creates the brilliant reflective qualities admired by collectors.

Geological and Collector Appeal

Rock Crystal is one of the most studied minerals in geology due to its:

  • Wide distribution in Earth’s crust
  • Role in metamorphic and hydrothermal processes
  • Ability to form large, well-defined crystals
  • Capacity to record geological history within its growth patterns

Collectors value Rock Crystal for its purity, clarity, and timeless appeal. This High Grade chunk is ideal for mineral displays, teaching collections, or decorative arrangements.

Display and Aesthetic Qualities

This Rock Crystal chunk has strong visual presence, with excellent clarity and natural sculptural form. It looks beautiful when displayed:

  • On a shelf or mantle
  • In a mineral cabinet
  • Beside plants, fossils, or other natural décor
  • Under display lighting, which enhances internal reflections

Its clean, crisp transparency allows light to flow through, creating a captivating effect that highlights the beauty of pure quartz.

All of our Crystals are 100% Genuine Specimens & come with a Certificate of Authenticity.

(Actual as seen)

Only 1 left in stock

SKU: SM9359 Category:

Description

High Grade Rock Crystal Natural Chunk – Genuine Clear Quartz Specimen

This stunning High Grade Rock Crystal Natural Chunk is an exceptional example of clear quartz in its raw, unaltered form. The photographs show the exact specimen you will receive, with a 1cm scale cube included to indicate accurate sizing. Every crystal we supply is a 100% genuine natural specimen and comes with a Certificate of Authenticity. This high-quality Rock Crystal chunk is ideal for collectors, interior décor, educational displays, and anyone who appreciates naturally formed mineral beauty.

What Is Rock Crystal?

Rock Crystal is the transparent, colourless variety of Quartz (SiO₂), one of the most abundant and important minerals in the Earth’s crust. It belongs to the trigonal crystal system and is part of the large silicate mineral group. Rock Crystal represents the purest form of quartz, lacking the chemical impurities that produce coloured varieties such as amethyst, citrine, or rose quartz.

Its name derives from the ancient Greek word krýstallos, meaning “ice,” as early cultures believed it was frozen water that could never melt. Today it remains highly valued for its clarity, structure, and geological significance.

Geological Origin and Formation Process

Rock Crystal forms in a wide range of geological environments, most commonly in:

  • Hydrothermal veins, where superheated, silica-rich fluids fill fractures deep underground
  • Pegmatites, coarse-grained igneous bodies that produce large, well-formed crystals
  • Geodes and vugs, hollow cavities lined with crystals
  • Metamorphic environments, where heat and pressure enable recrystallisation

Quartz crystals grow slowly over millions of years as silica precipitates from mineral-rich solutions. The resulting crystal may develop:

  • Six-sided prismatic faces
  • Sharp natural terminations
  • Parallel growth striations
  • Internal rainbows or light-scattering planes

Even as a natural chunk rather than a terminated point, this specimen retains the internal clarity and structural features associated with high-grade quartz.

Crystal Habit, Structure, and Appearance

Quartz grows in a hexagonal prismatic habit, often forming clusters or intergrown masses. This natural chunk may show:

  • Partial crystal faces, indicating its original growth orientation
  • Translucent to transparent zones, depending on internal purity
  • Fractured yet naturally healed features, revealing geological stress history
  • Subtle rainbow refractions, caused by internal micro-fractures
  • Glass-like lustre, especially on smoother surfaces

High Grade Rock Crystal is selected for its superior clarity, structural integrity, and minimal internal clouding—qualities clearly visible in this specimen.

Colour Variations and Natural Inclusions

Although Rock Crystal is typically colourless, minor internal features contribute to its individual character. These may include:

  • Feather-like inclusions, formed during rapid growth stages
  • Light-scattering planes, producing subtle flashes under direct light
  • Thin internal veils or phantoms, recording pauses in crystal development
  • Minute mineral particles, naturally trapped during formation

These inclusions do not detract from the specimen’s quality; rather, they enhance its geological uniqueness.

Mineralogical Properties

Quartz is known for its durability and optical beauty. Key mineral properties include:

  • Chemical composition: SiO₂ (silicon dioxide)
  • Hardness: 7 on the Mohs scale
  • Crystal system: Trigonal
  • Cleavage: Indistinct; conchoidal fracture
  • Lustre: Vitreous
  • Transparency: Transparent to translucent

Its hardness makes quartz resistant to scratching, while its internal structure creates the brilliant reflective qualities admired by collectors.

Geological and Collector Appeal

Rock Crystal is one of the most studied minerals in geology due to its:

  • Wide distribution in Earth’s crust
  • Role in metamorphic and hydrothermal processes
  • Ability to form large, well-defined crystals
  • Capacity to record geological history within its growth patterns

Collectors value Rock Crystal for its purity, clarity, and timeless appeal. This High Grade chunk is ideal for mineral displays, teaching collections, or decorative arrangements.

Display and Aesthetic Qualities

This Rock Crystal chunk has strong visual presence, with excellent clarity and natural sculptural form. It looks beautiful when displayed:

  • On a shelf or mantle
  • In a mineral cabinet
  • Beside plants, fossils, or other natural décor
  • Under display lighting, which enhances internal reflections

Its clean, crisp transparency allows light to flow through, creating a captivating effect that highlights the beauty of pure quartz.

All of our Crystals are 100% Genuine Specimens & come with a Certificate of Authenticity.

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