Description
Genuine Grade A Black Tourmaline with Feldspar and Quartz – Skardu, Gilgit Baltistan, Pakistan
This Grade A Black Tourmaline with Feldspar and Quartz specimen from Skardu, Gilgit Baltistan, Pakistan, is a genuine and carefully selected natural crystal combination. The photograph provided shows the exact specimen you will receive. Please refer to the images for full sizing and scale details.
This crystal includes a Certificate of Authenticity lifetime guarantee generic card confirming its genuine identity and documented Pakistani provenance.
Mineral Species & Scientific Classification
The primary mineral in this specimen is Black Tourmaline, most commonly the species Schorl, a member of the tourmaline supergroup.
Primary Mineral: Schorl (Black Tourmaline)
General Formula: NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄
Mineral Group: Cyclosilicate (Borosilicate)
Crystal System: Trigonal
Hardness: 7–7.5 Mohs
Lustre: Vitreous
Associated Minerals:
Quartz – Silicon Dioxide (SiO₂), trigonal crystal system
Feldspar – Tectosilicate group (commonly microcline or albite in pegmatites), monoclinic or triclinic systems
Black tourmaline typically forms elongated, vertically striated prismatic crystals. Quartz appears as clear to milky prismatic crystals with hexagonal symmetry, while feldspar commonly occurs as blocky, tabular or massive pale-toned crystals.
Geological Formation – Skardu Pegmatite Fields
The Skardu region of Gilgit Baltistan lies within the Karakoram and Himalayan orogenic belts, an area renowned for complex tectonic activity and world-class pegmatite mineralisation.
This specimen likely formed within granitic pegmatites, which are coarse-grained igneous bodies enriched in volatile elements such as boron. Pegmatitic environments provide ideal conditions for the crystallisation of large, well-formed minerals.
Formation process:
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Intrusion of granitic magma
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Slow cooling allowing large crystal growth
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Concentration of boron-rich fluids
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Crystallisation of tourmaline alongside quartz and feldspar
Black tourmaline crystallises early in boron-rich pegmatitic systems and may be embedded within quartz-feldspar matrices, creating striking mineral combinations.
Crystal Habit & Visual Characteristics
This Grade A specimen displays natural crystal growth of black tourmaline in association with quartz and feldspar matrix.
Typical features may include:
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Elongated prismatic black tourmaline crystals
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Vertical striations along crystal faces
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Contrasting light feldspar host rock
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Clear or milky quartz crystals
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Strong colour contrast between dark and pale minerals
The black coloration of schorl is caused primarily by iron content within the crystal structure. Surface lustre is vitreous, and crystal terminations may be flat or subtly pyramidal depending on growth conditions.
No artificial treatments or enhancements are implied; this is a natural mineral specimen.
Collectibility & Display Appeal
Mineral combinations from Skardu are internationally recognised for quality and crystal definition. The association of black tourmaline with quartz and feldspar is classic for pegmatite mineralisation and offers both aesthetic and geological interest.
Collectors value these specimens for:
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Recognised Himalayan pegmatite locality
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Classic tourmaline crystal habit
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Multi-mineral contrast
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Strong geological context
The combination of dark schorl with pale feldspar and clear quartz provides a balanced and visually appealing display specimen suitable for mineral cabinets, geological collections or educational use.
Black tourmaline has been traditionally associated in various cultures with protection in a spiritual sense, though this listing focuses entirely on mineralogical and geological characteristics.
Authenticity & Presentation
This Black Tourmaline with Feldspar and Quartz specimen has been carefully chosen for crystal quality, mineral association and locality significance. The image shown is of the exact specimen you will receive.
Included with your purchase is a Certificate of Authenticity lifetime guarantee generic card confirming this is a genuine specimen from Skardu, Gilgit Baltistan, Pakistan.
A classic example of Himalayan pegmatite mineral formation, this Grade A multi-mineral crystal specimen combines strong locality provenance, natural crystal structure and striking mineral contrast in one authentic collector’s piece.






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