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Cinnabar Lone Pine Mine Washington USA Genuine Mineral Specimen with Certificate of Authenticity

Original price was: £120.00.Current price is: £96.00.

This rare Cinnabar crystal specimen comes from the historic Lone Pine Mine in the Republic Mining District, Ferry County, Washington, USA, and originates from a distinguished ex-collection. Cinnabar, known for its deep red to crimson hues, is the primary ore of mercury and is highly sought after by mineral collectors for its vibrant color and rarity. This specimen features well-formed Cinnabar crystals with a striking luster, making it a visually appealing and valuable addition to any collection.

The Lone Pine Mine has a rich history in the mining of mercury, and this Cinnabar specimen reflects both the geological significance and aesthetic beauty of the region.

  • Material: Cinnabar (Mercury Sulfide)
  • Origin: Lone Pine Mine, Republic Mining District, Ferry County, Washington, USA
  • Provenance: Ex-collection specimen
  • Size: Please refer to the photo for exact dimensions (Scale cube = 1 cm)
  • Condition: Genuine natural Cinnabar crystal with deep red coloration and excellent structure
  • Certificate of Authenticity: Included with every purchase, certifying the specimen’s authenticity
  • Actual Specimen: The photo shows the exact Cinnabar crystal you will receive, ensuring a unique and carefully chosen piece.

Cinnabar is highly valued for its rarity, brilliant color, and historical significance as a source of mercury. This specimen is perfect for mineral collectors, geology enthusiasts, or anyone interested in the rich mining history of the Republic Mining District.

Shipping & Packaging: We take great care in securely packaging all crystals to ensure they arrive safely. Each purchase includes a Certificate of Authenticity for your peace of mind.

Add this rare Cinnabar crystal from Lone Pine Mine, Washington, USA, to your collection—an extraordinary piece of mineral and mining heritage!

(Actual as seen)

Only 1 left in stock

SKU: UR5094 Category:

Description

Genuine Cinnabar – Lone Pine Mine, Republic Mining District, Washington, USA

This Cinnabar specimen from the Lone Pine Mine, Republic Mining District, Ferry County, Washington, USA, is a genuine and carefully selected example of mercury mineralisation from a recognised American mining locality. The photograph provided shows the exact specimen you will receive. Please refer to the images for full sizing details and accurate scale.

This crystal includes a Certificate of Authenticity lifetime guarantee generic card confirming its genuine origin and mineral identification.


Mineral & Geological Classification – Cinnabar

Cinnabar is a mercury sulfide mineral with the chemical formula HgS. It is the primary ore of mercury and crystallises in the trigonal crystal system.

Mineral Name: Cinnabar
Chemical Formula: HgS
Mineral Group: Sulfide
Crystal System: Trigonal
Hardness: 2–2.5 on the Mohs scale
Lustre: Adamantine to dull
Colour: Scarlet red to deep crimson

Cinnabar is instantly recognisable due to its vivid red colour, which can range from bright scarlet to darker red tones depending on crystal form and surface condition. Crystals may occur as well-formed rhombohedral shapes, granular aggregates or massive coatings within host rock.

The high refractive index of cinnabar can produce a bright, almost glowing surface under strong light. Its colour is natural and derives from the mercury-sulfur chemical composition.


Geological Setting – Lone Pine Mine, Republic Mining District

The Republic Mining District in Ferry County, Washington, is historically known for gold and associated hydrothermal mineralisation. Cinnabar from the Lone Pine Mine formed in low-temperature hydrothermal vein systems where mercury-rich fluids circulated through fractures in host rocks.

Cinnabar commonly develops in epithermal environments, often associated with quartz veins and other sulfide minerals. In such settings, mineralising fluids rise toward the surface and deposit mercury sulfide as temperatures and pressures decrease.

Associated minerals in similar deposits may include quartz, calcite, pyrite and other sulfides depending on local geochemical conditions. The Republic District’s complex structural geology provided pathways for mineral-bearing fluids, allowing cinnabar to crystallise within open fractures and cavities.


Crystal Characteristics & Notable Traits

Cinnabar from this locality may display:

  • Bright red to crimson colouration

  • Crystalline or granular surface texture

  • Adamantine sheen on crystal faces

  • Occurrence on contrasting pale matrix

In some specimens, cinnabar forms small, sharply defined crystals, while in others it appears as fine-grained coatings or masses within quartz veins. The intense natural red colour contrasts strongly with light-coloured host rock, enhancing display appeal.

Because cinnabar is relatively soft, crystal edges may show minor natural wear. Surface features and matrix attachment are part of the mineral’s geological formation and authenticity.


Geological Importance & Collectibility

Cinnabar is significant as the principal ore of mercury and as an indicator of epithermal hydrothermal systems. Specimens from documented localities such as the Lone Pine Mine are valued for both scientific and collector interest.

The Republic Mining District holds historical importance within Washington State mining history. Mineral specimens from this area represent classic American hydrothermal mineralisation.

This piece is suitable for mineral cabinets, educational collections or collectors specialising in sulfide minerals and United States localities. As a genuine natural specimen, it displays unique characteristics shaped by its formation environment. The photograph shows the exact specimen you will receive.


Authenticity & Presentation

This Cinnabar specimen from the Lone Pine Mine has been carefully chosen for quality, colour and locality significance. Included with your purchase is a Certificate of Authenticity lifetime guarantee generic card confirming its genuine origin from Ferry County, Washington, USA.

Combining vivid natural colour with documented hydrothermal origin, this Cinnabar specimen offers mineral authenticity, regional geological importance and strong collector appeal in one carefully selected piece.

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