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Rare British Barytes Crystal Bradwell Moor Derbyshire Genuine Natural Barite UK

£42.00

Overview – Rare British Barytes from Bradwell Moor, Derbyshire

This listing features a rare and genuine Barytes (Barite) crystal specimen sourced from Bradwell Moor, Derbyshire, one of the historically significant mineral-producing areas of the Peak District. British barytes specimens of this quality are increasingly scarce, as many classic collecting sites are long closed or protected. The photographs show the exact specimen you will receive, carefully chosen for its crystal form, natural lustre, and highly collectable geological character.

Every specimen includes a Certificate of Authenticity, confirming it as a 100% genuine natural mineral specimen.

Barytes from Bradwell Moor is admired not only for its mineralogical beauty but also for its connection to Derbyshire’s centuries-long mining heritage. These pieces are sought after by both collectors of British minerals and geological enthusiasts worldwide.

Geological Background – Bradwell Moor and the Peak District Mineral Belt

Bradwell Moor sits within the Derbyshire Peak District, a region shaped by ancient geological processes involving Carboniferous limestone, hydrothermal alteration, and long periods of mineral deposition. Mineralisation occurred when hot, mineral-rich fluids moved through fractures in the limestone host rock, precipitating minerals such as baryte, fluorite, galena, and calcite.

This geological environment created extensive hydrothermal veins that became the backbone of Derbyshire’s lead and baryte mining industry. Barytes formed as these fluids cooled, producing the distinctive crystal habits characteristic of the area.

Mineralogy – Barytes (Barite) Crystal Structure and Features

Barytes is the mineral form of barium sulfate (BaSO₄) and crystalises in the orthorhombic system, often producing tabular, bladed, or blocky crystals. Specimens from Bradwell Moor frequently display:

  • Well-defined tabular or bladed crystals, typical of Derbyshire baryte
  • Soft white, cream, honey or buff colours, depending on trace mineral content
  • Natural surface lustre, ranging from pearly to vitreous
  • Translucent zones, especially along crystal edges or internal planes
  • Distinct layered growth patterns, formed through repeated phases of hydrothermal mineralisation

Barytes is known for being unexpectedly heavy due to its high specific gravity, making it instantly recognisable when handled.

Colouration and Internal Texture

Bradwell Moor barytes often showcases subtle colour variation caused by interactions with surrounding minerals during formation. Common visual traits include:

  • Creamy white or warm beige hues, enriched with soft mineral tones
  • Internal zoning or banding, recording different stages of crystal growth
  • Fine inclusions that create delicate internal patterns
  • Translucency, allowing light to penetrate and highlight structural detail

These features give each barytes specimen a unique visual identity.

Origin Environment – Hydrothermal Mineralisation in Limestone

The mineralisation process within Bradwell Moor occurred when ascending hydrothermal fluids deposited baryte into open fractures and bedding-plane cavities within the limestone. Over extended geological timescales, these voids filled with baryte crystals, sometimes intergrown with other minerals such as:

  • Fluorite
  • Galena
  • Calcite
  • Quartz

This specimen reflects the precise environmental conditions required for baryte crystallisation: stable temperatures, mineral-saturated fluids, and open space within the host rock.

Aesthetic and Collectible Value

Rare British barytes specimens are prized for their historical provenance, mineralogical interest, and attractive crystal habits. This Bradwell Moor example is particularly desirable due to:

  • Its origin in one of the UK’s most iconic mineral districts
  • Increasing scarcity from long-closed mines
  • Its classic barytes crystal architecture
  • Its suitability for display, educational use, or long-term collection

British minerals hold a special place in European mineral collecting, and pieces from Derbyshire are among the most recognisable and historically significant.

Your Specimen

This Bradwell Moor Barytes specimen was carefully selected for its aesthetic appeal, distinct crystal shape, and excellent representation of Derbyshire’s mineral diversity. The photographs show the exact specimen available, and all sizing details are clearly provided in the listing images.

Your purchase includes a Certificate of Authenticity, confirming this is a genuine natural Barytes crystal specimen from Bradwell Moor, Derbyshire.

(Actual as seen)

Only 1 left in stock

SKU: UR6672 Category:

Description

Overview – Rare British Barytes from Bradwell Moor, Derbyshire

This listing features a rare and genuine Barytes (Barite) crystal specimen sourced from Bradwell Moor, Derbyshire, one of the historically significant mineral-producing areas of the Peak District. British barytes specimens of this quality are increasingly scarce, as many classic collecting sites are long closed or protected. The photographs show the exact specimen you will receive, carefully chosen for its crystal form, natural lustre, and highly collectable geological character.

Every specimen includes a Certificate of Authenticity, confirming it as a 100% genuine natural mineral specimen.

Barytes from Bradwell Moor is admired not only for its mineralogical beauty but also for its connection to Derbyshire’s centuries-long mining heritage. These pieces are sought after by both collectors of British minerals and geological enthusiasts worldwide.

Geological Background – Bradwell Moor and the Peak District Mineral Belt

Bradwell Moor sits within the Derbyshire Peak District, a region shaped by ancient geological processes involving Carboniferous limestone, hydrothermal alteration, and long periods of mineral deposition. Mineralisation occurred when hot, mineral-rich fluids moved through fractures in the limestone host rock, precipitating minerals such as baryte, fluorite, galena, and calcite.

This geological environment created extensive hydrothermal veins that became the backbone of Derbyshire’s lead and baryte mining industry. Barytes formed as these fluids cooled, producing the distinctive crystal habits characteristic of the area.

Mineralogy – Barytes (Barite) Crystal Structure and Features

Barytes is the mineral form of barium sulfate (BaSO₄) and crystalises in the orthorhombic system, often producing tabular, bladed, or blocky crystals. Specimens from Bradwell Moor frequently display:

  • Well-defined tabular or bladed crystals, typical of Derbyshire baryte
  • Soft white, cream, honey or buff colours, depending on trace mineral content
  • Natural surface lustre, ranging from pearly to vitreous
  • Translucent zones, especially along crystal edges or internal planes
  • Distinct layered growth patterns, formed through repeated phases of hydrothermal mineralisation

Barytes is known for being unexpectedly heavy due to its high specific gravity, making it instantly recognisable when handled.

Colouration and Internal Texture

Bradwell Moor barytes often showcases subtle colour variation caused by interactions with surrounding minerals during formation. Common visual traits include:

  • Creamy white or warm beige hues, enriched with soft mineral tones
  • Internal zoning or banding, recording different stages of crystal growth
  • Fine inclusions that create delicate internal patterns
  • Translucency, allowing light to penetrate and highlight structural detail

These features give each barytes specimen a unique visual identity.

Origin Environment – Hydrothermal Mineralisation in Limestone

The mineralisation process within Bradwell Moor occurred when ascending hydrothermal fluids deposited baryte into open fractures and bedding-plane cavities within the limestone. Over extended geological timescales, these voids filled with baryte crystals, sometimes intergrown with other minerals such as:

  • Fluorite
  • Galena
  • Calcite
  • Quartz

This specimen reflects the precise environmental conditions required for baryte crystallisation: stable temperatures, mineral-saturated fluids, and open space within the host rock.

Aesthetic and Collectible Value

Rare British barytes specimens are prized for their historical provenance, mineralogical interest, and attractive crystal habits. This Bradwell Moor example is particularly desirable due to:

  • Its origin in one of the UK’s most iconic mineral districts
  • Increasing scarcity from long-closed mines
  • Its classic barytes crystal architecture
  • Its suitability for display, educational use, or long-term collection

British minerals hold a special place in European mineral collecting, and pieces from Derbyshire are among the most recognisable and historically significant.

Your Specimen

This Bradwell Moor Barytes specimen was carefully selected for its aesthetic appeal, distinct crystal shape, and excellent representation of Derbyshire’s mineral diversity. The photographs show the exact specimen available, and all sizing details are clearly provided in the listing images.

Your purchase includes a Certificate of Authenticity, confirming this is a genuine natural Barytes crystal specimen from Bradwell Moor, Derbyshire.

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