• This is a natural Emerald crystal specimen from the Beryl mineral family
• Genuine precious gemstone is classified as a rare mineral crystal for collectors
• Total weight of the specimen is 51 grams
• Dimensions measure 55 x 41 x 25 mm
• Natural hexagonal crystal formation showcasing classic emerald morphology
• Beautiful light green color characteristic of Pakistani emeralds from Chitral
• Transparent clarity allowing light to pass through the crystals
• This is sourced from Chitral, Pakistan, a newly discovered locality for natural emeralds. 
• 100% natural and earthly mined with minor traditional oil treatment
• May birthstone, perfect for collectors and gemstone enthusiasts
• Fine mineral specimen suitable for serious crystal collectors
• Rare, authentic single specimen with museum-quality presentation

Geological and Technical Analysis

This exceptional specimen is a natural Emerald (Beryl variety, Be₃Al₂Si₆O₁₈) crystal clusters from the renowned Chitral mining district in Khyber Pakhtunkhwa, Pakistan. The specimen exhibits characteristic hexagonal prismatic crystal habit with well-defined terminations and natural growth patterns typical of pegmatitic formation environments.

Mineralogical Characteristics:

• Mineral Species: Emerald (Chromium and Vanadium-bearing Beryl)
• Crystal System: Hexagonal
• Specimen Weight: 51 grams
• Dimensions: 55 x 41 x 25 mm
• Color: Vibrant green with characteristic chromophore coloration from trace chromium and vanadium
• Luster: Vitreous to sub-vitreous on crystal faces
• Matrix: Natural host rock with metallic inclusions (likely mica schist or biotite)
• Formation: Hydrothermal pegmatite environment
• Locality: Chitral District, Khyber Pakhtunkhwa Province, Pakistan

Specimen Quality Features:

• Multiple intergrown prismatic crystals showing natural growth striations
• Excellent color saturation with classic Chitral emerald green hue
• Visible crystal terminations and natural faces
• Intact matrix attachment preserving geological context
• Metallic inclusions (mica/biotite) indicating authentic pegmatitic origin
• Translucent to transparent crystal sections
• No evidence of treatment or enhancement

Geological Significance:

Chitral emeralds form in metamorphic pegmatite veins within mica schist host rocks, created under high-pressure, high-temperature conditions during regional metamorphism. The presence of biotite and other metallic inclusions is diagnostic of the Chitral deposit and confirms the specimen's provenance. These emeralds are geologically distinct from Colombian or Zambian varieties due to their unique trace element signatures and formation environment.

This specimen represents an excellent example of Pakistani emerald mineralization and is ideal for serious mineral collectors, educational institutions, or gemological study.

Frequently Asked Questions for Emerald Collectors

Q: What makes Chitral emerald specimens valuable to mineral collectors?

A: Chitral emeralds are highly prized for their exceptional color, geological significance, and relative rarity in the mineral specimen market. Unlike faceted gems, matrix specimens like this preserve the natural crystal morphology, growth patterns, and geological context. The presence of intact hexagonal crystals with visible terminations, combined with authentic host rock and diagnostic inclusions, makes this a scientifically important and aesthetically striking collector piece. Chitral specimens are particularly valued because they represent one of Asia's most important emerald deposits.

Q: How should I care for and display this emerald crystal specimen?

A: Store this specimen in a stable environment away from direct sunlight, extreme temperature fluctuations, and high humidity. Emerald has a Mohs hardness of 7.5-8, making it relatively durable, but the crystal-matrix interface can be fragile. Display in a cushioned case or on a stable platform. Clean only with a soft, dry brush—never use water, chemicals, or ultrasonic cleaners, as these can damage the matrix or loosen crystals. Handle by the matrix rather than the crystals to prevent mechanical stress on the crystal-host rock boundary.

Q: Is this specimen suitable for gemological study or educational purposes?

A: Absolutely. This specimen is ideal for gemological education, mineralogical research, and comparative studies. It displays classic emerald crystal morphology, diagnostic inclusions, and authentic matrix that illustrate pegmatitic formation processes. The specimen can be used to study crystal growth patterns, trace element incorporation, and regional metamorphic geology. It's also valuable for teaching crystallography (hexagonal system), beryl group mineralogy, and the geological conditions required for emerald formation. The intact nature and clear provenance make it suitable for museum collections or academic reference collections.