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Emerald in Matrix Russia Natural Green Beryl Mineral Specimen Rough Emerald Crystal

£10.80

(Actual as seen)

Only 1 left in stock

SKU: RP0735 Category:

Description

Emerald in Matrix – Natural Green Beryl Mineral from Russia

This Emerald in Matrix specimen features natural emerald crystals embedded within their host rock, creating a striking mineral display that highlights both the gemstone variety and its geological environment. Emerald is the vivid green variety of the mineral beryl, and specimens preserved within their natural matrix are highly valued by mineral collectors because they show the crystal in its original geological context.

The listing photographs show the exact specimen you will receive, allowing collectors and buyers to clearly examine the emerald crystal colour, the surrounding matrix, and the natural mineral structure before purchase.

This crystal is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee generic card, confirming authenticity.

Please refer to the photographs for full sizing and scale.


Mineral Identification – Emerald (Beryl Group)

Emerald is a variety of the mineral beryl, a beryllium aluminium cyclosilicate known for forming hexagonal crystal structures. The distinctive green colour of emerald is caused by trace amounts of chromium, vanadium, or sometimes iron within the crystal lattice.

Key mineralogical details include:

  • Mineral Name: Beryl

  • Variety: Emerald

  • Chemical Formula: Be₃Al₂Si₆O₁₈

  • Mineral Class: Cyclosilicate

  • Crystal System: Hexagonal

  • Mohs Hardness: 7.5–8

  • Transparency: Transparent to opaque depending on crystal quality

  • Lustre: Vitreous (glass-like)

In mineral specimens such as this one, emerald crystals often appear partially embedded within the surrounding rock matrix, revealing how the mineral originally formed underground.


Geological Formation of Emerald

Emerald formation requires a very specific combination of geological conditions. Beryllium-rich fluids must interact with chromium or vanadium-bearing rocks, a relatively rare combination in nature. When these elements come together under suitable temperature and pressure conditions, emerald crystals can form.

Emerald deposits commonly develop in:

  • Metamorphic schists

  • Hydrothermal veins

  • Pegmatite-related environments

  • Contact metamorphic zones

In these geological settings, mineral-rich fluids circulate through rock fractures, allowing emerald crystals to grow slowly within cavities or along mineral veins.

The surrounding matrix often contains minerals that formed during the same geological processes.

Associated minerals commonly found alongside emerald include:

  • Quartz

  • Feldspar

  • Mica

  • Calcite

  • Biotite

  • Tourmaline

These minerals help geologists identify the environmental conditions under which the emerald formed.


Emerald Deposits in Russia

Russia is known for several historic emerald localities, particularly in the Ural Mountains, which have produced emerald specimens since the early nineteenth century. These deposits occur primarily in metamorphic environments where beryllium-bearing fluids interacted with chromium-rich rocks.

Russian emerald specimens are recognised for:

  • Distinctive natural matrix associations

  • Strong green coloration in crystal fragments

  • Geological importance within the Ural mineral belt

Specimens preserved in matrix offer collectors an authentic representation of the mineral’s natural occurrence, rather than a crystal removed from its geological setting.


Natural Colour and Crystal Characteristics

Emerald is widely recognised for its vivid green coloration, which can range from pale green to deep emerald tones depending on trace element concentration and geological conditions during formation.

Typical features seen in natural emerald specimens include:

  • Green crystal fragments or prisms within host rock

  • Internal inclusions formed during crystal growth

  • Natural fractures or mineral inclusions

  • Variations in colour intensity

These features are normal characteristics of natural emerald and provide valuable clues about the crystal’s geological history.


Emerald in Matrix for Mineral Collectors

Emerald specimens preserved within their original matrix are particularly appealing to collectors because they display both the gemstone mineral and its host rock environment. This makes them useful for both mineral display and educational geological collections.

This specimen may be suitable for:

  • Mineral and gemstone collections

  • Beryl and emerald mineral collections

  • Geological display collections

  • Educational mineral study

  • Unique natural gift items

In some traditions, emerald has been traditionally associated with symbolic or spiritual interpretations, although such associations are belief-based rather than scientific descriptions.

Because the photographs show the actual specimen, buyers can purchase with confidence knowing exactly which mineral specimen they will receive.


Authentic Natural Mineral Specimen

This Emerald in Matrix specimen from Russia is a genuine natural mineral carefully selected for its colour and geological character.

The crystal includes a Certificate of Authenticity lifetime guarantee generic card, confirming the authenticity of the mineral specimen.

Please review the listing photographs for full sizing and scale, as they form part of the description and clearly show the exact specimen you will receive.

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