Description
Natural Sodalite Mineral Specimen from Pakistan
This listing features a genuine Sodalite mineral specimen from Pakistan, a striking blue feldspathoid mineral admired for its rich colour and natural white mineral veining. Carefully selected for its colour contrast and mineral character, this specimen makes an attractive addition to mineral collections, geological displays, or decorative natural stone arrangements.
The photographs in this listing show the exact specimen you will receive, allowing you to clearly view the natural patterns, colour variations, and mineral textures before purchase. Each Sodalite specimen forms naturally and therefore displays unique visual characteristics created through geological processes.
This crystal includes a Certificate of Authenticity lifetime guarantee generic card, confirming that the mineral specimen is genuine. Full sizing details can be seen in the listing photographs to provide an accurate reference for scale.
Mineral Identification and Scientific Classification
Sodalite is a tectosilicate mineral belonging to the feldspathoid mineral group, with the chemical formula Na₈(Al₆Si₆O₂₄)Cl₂. It crystallises in the cubic crystal system, although well-defined crystals are relatively uncommon and the mineral most frequently occurs in massive form.
The mineral was first described in the early nineteenth century and is named after its high sodium content. Sodalite is recognised for its deep blue colour and distinctive white mineral inclusions.
Key mineralogical characteristics include:
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Mineral group: Feldspathoid (tectosilicate)
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Chemical composition: Sodium aluminium silicate chloride
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Crystal system: Cubic
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Hardness: 5.5–6 on the Mohs scale
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Lustre: Vitreous to greasy
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Transparency: Opaque to translucent in thin sections
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Typical colour: Deep blue with white mineral veining
Sodalite’s intense blue colour is caused by sulfur compounds within the mineral’s crystal structure.
Geological Formation and Natural Occurrence
Sodalite forms primarily within alkaline igneous rocks, particularly in silica-poor environments where feldspathoid minerals can crystallise instead of quartz. These geological environments occur in nepheline syenites, phonolites, and other alkaline intrusive rocks.
The mineral develops when magma rich in sodium, aluminium, and chlorine cools slowly beneath the Earth’s surface. As the magma crystallises, Sodalite forms alongside other alkaline minerals within the host rock.
Common minerals associated with Sodalite include:
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Nepheline
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Albite feldspar
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Calcite
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Cancrinite
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Feldspathoids
These minerals often appear together within alkaline intrusive rock formations.
Pakistan is known for producing high-quality decorative mineral specimens due to its complex geological history and mineral-rich mountain regions. The country contains numerous igneous and metamorphic environments that support the formation of colourful mineral specimens.
Colour Characteristics and Natural Patterns
The most recognisable feature of Sodalite is its rich royal blue colour, which is often combined with contrasting white mineral veins. These white areas are typically composed of calcite or feldspar minerals that formed alongside the Sodalite during the cooling of the host rock.
Typical colour variations may include:
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Deep royal blue
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Indigo blue tones
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Blue-grey areas
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White calcite or feldspar veining
The contrast between the deep blue mineral and lighter inclusions creates striking natural patterns that make Sodalite easily recognisable.
Some Sodalite specimens may also display subtle variations in colour intensity due to differences in mineral concentration and crystal growth during formation.
Mineral Collecting and Display Value
Sodalite is widely appreciated by collectors and mineral enthusiasts due to its distinctive colour and geological origin. The deep blue colour, combined with natural white veining, creates attractive specimens suitable for mineral cabinets, decorative displays, or educational collections.
Collectors often value Sodalite specimens for:
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Their vivid blue colour
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Distinctive mineral veining
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Association with alkaline igneous rocks
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Representation of feldspathoid mineral species
Polished or natural Sodalite specimens are often displayed to highlight the stone’s unique mineral patterns and colour contrast.
Cultural and Traditional Context
In some modern crystal collecting traditions, Sodalite is traditionally associated with clarity and communication, and specimens may be displayed in decorative or contemplative environments. These interpretations are based on cultural traditions rather than scientifically established mineral properties.
Authenticity and Specimen Details
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Genuine Sodalite mineral specimen
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Origin: Pakistan
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Deep blue feldspathoid mineral with natural veining
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Carefully selected collector specimen
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Exact piece shown in the listing photographs
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Full sizing reference available in listing images
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Includes Certificate of Authenticity lifetime guarantee generic card
Each Sodalite specimen forms naturally within alkaline igneous geological environments over long periods of time, producing unique colour patterns and mineral inclusions that make every piece distinctive.






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