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Vanadinite Crystal Morocco Natural Red Hexagonal Mineral Specimen

Original price was: £14.40.Current price is: £12.96.

(Actual as seen)

Only 1 left in stock

SKU: RP0058 Category:

Description

Vanadinite – Natural Hexagonal Lead Vanadate from Morocco

This Vanadinite specimen is a genuine natural mineral from Morocco, one of the world’s most renowned sources of fine crystallised Vanadinite. The photograph shows the exact piece you will receive, carefully selected for its vibrant colour, crystal form, and overall display quality. Full sizing details are available in the listing photos to provide accurate scale and proportions.

Your specimen includes a Certificate of Authenticity lifetime guarantee generic card, confirming it as a genuine Vanadinite mineral example.


Mineral Species & Scientific Classification

Vanadinite is a lead chlorovanadate mineral with the chemical formula Pb₅(VO₄)₃Cl. It belongs to the apatite mineral group and crystallises in the hexagonal crystal system. Its crystals commonly form short hexagonal prisms with flat terminations, often appearing as barrel-shaped or tabular clusters.

With a Mohs hardness of approximately 2.5 to 3, Vanadinite is relatively soft and should be handled with care. It has a resinous to subadamantine lustre and is typically opaque.

The vivid red to orange-red colour of Vanadinite is due to the presence of vanadium within its chemical structure. Variations in tone may range from deep crimson to bright red-orange depending on trace elements and formation conditions.


Crystal Habit, Colour & Surface Features

Moroccan Vanadinite is particularly prized for its well-defined hexagonal crystals and strong colour saturation. Crystals often grow in clusters on matrix rock, creating striking three-dimensional displays.

The surface of individual crystals may show natural growth lines or subtle variations in sheen. Associated matrix can include barite, calcite, limonite, or other secondary minerals depending on the locality.

This specimen is natural and untreated, with no artificial enhancement. The colour and crystal form are the direct result of geological processes.


Geological Formation – Morocco

Vanadinite forms as a secondary mineral in the oxidised zones of lead ore deposits. It develops when vanadium-bearing solutions react with lead minerals such as galena in arid or semi-arid environments.

Morocco, particularly the Mibladen and Touissit mining districts, is internationally recognised for producing some of the finest Vanadinite specimens. The region’s geological conditions allow for the growth of well-formed hexagonal crystals within cavities and fractures of the host rock.

Vanadinite often occurs alongside minerals such as wulfenite, cerussite, barite, calcite, and other oxidised lead minerals, reflecting the complex chemistry of these deposits.


Collecting, Display & Traditional Associations

Vanadinite is highly sought after by mineral collectors due to its bold red colour and classic hexagonal crystal habit. Moroccan specimens are especially desirable for their quality and crystal definition, making them excellent display pieces in mineral cabinets or curated collections.

Because Vanadinite contains lead, it should be handled responsibly and kept away from prolonged direct contact, especially by children.

In various traditions, red minerals have been traditionally associated with vitality and focus in symbolic practices. These associations are spiritual in nature and reflect cultural interpretations of naturally coloured stones.


Authenticity & Individual Selection

• Genuine natural Vanadinite
• Origin: Morocco
• Chemical formula: Pb₅(VO₄)₃Cl
• Mineral group: Apatite group
• Crystal system: Hexagonal
• Carefully selected individual specimen
• You will receive the exact piece shown
• Includes Certificate of Authenticity lifetime guarantee generic card

Each Vanadinite specimen forms through natural secondary mineral processes over geological timescales, resulting in unique crystal clusters, colour intensity, and matrix combinations in every individual piece.

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