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Dolomite Calcite USA Crystal Natural Mineral Specimen Genuine Stone with Certificate of Authenticity

£24.00

Dolomite and Calcite Crystal – Genuine Natural Mineral Specimen from the USA

This Dolomite and Calcite USA Crystal is an exceptional natural mineral specimen showcasing the elegant pairing of two classic carbonate minerals. The listing photograph shows the exact specimen you will receive, ensuring full confidence in its quality, structure, and unique formation. All of our crystals are 100% genuine natural specimens and come with a Certificate of Authenticity. This piece was carefully selected for its well-formed dolomite crystals, beautifully contrasting calcite growths, and the harmonious mineral association that makes it a captivating display specimen.

Mineralogical Profile: Dolomite and Calcite

This specimen features a visually striking combination of Dolomite and Calcite, each mineral contributing its own distinctive crystallographic form and colour.

Dolomite – CaMg(CO₃)₂

Dolomite is a calcium magnesium carbonate mineral that commonly forms in rhombohedral or saddle-shaped crystals. It belongs to the trigonal crystal system and is typically found in sedimentary and hydrothermal environments.

Key characteristics include:

  • Crystal Habit: Rhombohedral, blocky, or curved saddle-shaped forms
  • Colour: White, beige, grey, cream, or tinted by iron and manganese
  • Surface Texture: Pearly, silky, or slightly matte
  • Notable Features: Curved crystal faces, stepped growth surfaces, or twinning

Dolomite crystals often appear tightly clustered, forming the structural foundation of the specimen.

Calcite – CaCO₃

Calcite is among the most abundant and structurally diverse minerals on Earth, crystallising in a wide variety of forms including scalenohedrons (“dogtooth”), rhombohedrons, tabular crystals, and blocky habits.

Calcite on this specimen may display:

  • Crystal Habit: Scalenohedral, rhombohedral, or elongated growths
  • Colour: Clear, white, honey, pale yellow, or softly milky
  • Lustre: Vitreous to pearly
  • Inclusions: Possible iron tinting, fluid inclusions, or internal phantoms

The calcite crystals contrast beautifully with the more muted tones of the dolomite, creating a visually balanced mineral cluster.

Geological Formation and Natural Origin Environment

Dolomite and calcite commonly occur together in sedimentary and hydrothermal environments within geological formations such as limestone deposits, dolostone horizons, and mineral-rich veins. This combination often results from multi-stage crystallisation processes:

  1. Dolomite Formation
  2. Dolomite forms when magnesium-rich fluids percolate through limestone, replacing calcium ions with magnesium in a slow geochemical reaction known as dolomitisation. Alternately, it may precipitate directly from hydrothermal fluids.
  3. Calcite Crystallisation
  4. Calcite often forms later, as calcium-rich solutions enter cavities, vugs, or fractures within the dolomite host. Its growth may reflect changes in temperature, mineral saturation, or fluid chemistry.
  5. Layered Mineralisation
  6. The two minerals together represent a dynamic environment shaped over millions of years, with multiple mineralisation stages producing the contrasting crystal habits seen in this specimen.

Depending on the locality within the USA, trace minerals such as siderite, pyrite, or quartz may accompany dolomite–calcite clusters, contributing subtle colouration or inclusions.

Aesthetic Appeal and Display Qualities

This Dolomite and Calcite crystal specimen is visually captivating due to its complementary mineral pairings. Dolomite’s soft, earthy tones create the perfect backdrop for calcite’s brighter, more reflective crystals. The interplay of textures—dolomite’s smooth or curved faces against calcite’s sharper, more translucent points—gives the piece excellent depth and visual dimension.

Its neutral yet elegant colour palette makes it suitable for display in:

  • Mineral collections
  • Home and office décor
  • Educational and geological exhibits
  • Meditation or natural history settings

The mineral association offers both textural complexity and aesthetic harmony, making it a memorable and highly collectible display piece.

Scientific and Collector Significance

Dolomite and calcite help geologists interpret the geochemical history of their environment, including:

  • Fluid pathways
  • Temperature changes
  • Mineral replacement reactions
  • Sedimentary basin evolution

Collectors value specimens like this for:

  • Multi-mineral associations
  • Well-defined crystal habits
  • Natural contrast between mineral species
  • Geological significance tied to classic U.S. mineral localities

High-quality dolomite–calcite combinations remain popular among both novice and advanced collectors.

Authenticity and Quality Assurance

All of our crystals are fully natural, authentic specimens. This Dolomite and Calcite USA Crystal comes with a Certificate of Authenticity, and the images provided show the exact specimen you will receive. It is a beautifully balanced, mineralogically rich piece that offers both aesthetic appeal and scientific interest—an excellent addition to any crystal or mineral collection.

(Actual as seen)

Only 1 left in stock

SKU: UR6689 Category:

Description

Dolomite and Calcite Crystal – Genuine Natural Mineral Specimen from the USA

This Dolomite and Calcite USA Crystal is an exceptional natural mineral specimen showcasing the elegant pairing of two classic carbonate minerals. The listing photograph shows the exact specimen you will receive, ensuring full confidence in its quality, structure, and unique formation. All of our crystals are 100% genuine natural specimens and come with a Certificate of Authenticity. This piece was carefully selected for its well-formed dolomite crystals, beautifully contrasting calcite growths, and the harmonious mineral association that makes it a captivating display specimen.

Mineralogical Profile: Dolomite and Calcite

This specimen features a visually striking combination of Dolomite and Calcite, each mineral contributing its own distinctive crystallographic form and colour.

Dolomite – CaMg(CO₃)₂

Dolomite is a calcium magnesium carbonate mineral that commonly forms in rhombohedral or saddle-shaped crystals. It belongs to the trigonal crystal system and is typically found in sedimentary and hydrothermal environments.

Key characteristics include:

  • Crystal Habit: Rhombohedral, blocky, or curved saddle-shaped forms
  • Colour: White, beige, grey, cream, or tinted by iron and manganese
  • Surface Texture: Pearly, silky, or slightly matte
  • Notable Features: Curved crystal faces, stepped growth surfaces, or twinning

Dolomite crystals often appear tightly clustered, forming the structural foundation of the specimen.

Calcite – CaCO₃

Calcite is among the most abundant and structurally diverse minerals on Earth, crystallising in a wide variety of forms including scalenohedrons (“dogtooth”), rhombohedrons, tabular crystals, and blocky habits.

Calcite on this specimen may display:

  • Crystal Habit: Scalenohedral, rhombohedral, or elongated growths
  • Colour: Clear, white, honey, pale yellow, or softly milky
  • Lustre: Vitreous to pearly
  • Inclusions: Possible iron tinting, fluid inclusions, or internal phantoms

The calcite crystals contrast beautifully with the more muted tones of the dolomite, creating a visually balanced mineral cluster.

Geological Formation and Natural Origin Environment

Dolomite and calcite commonly occur together in sedimentary and hydrothermal environments within geological formations such as limestone deposits, dolostone horizons, and mineral-rich veins. This combination often results from multi-stage crystallisation processes:

  1. Dolomite Formation
  2. Dolomite forms when magnesium-rich fluids percolate through limestone, replacing calcium ions with magnesium in a slow geochemical reaction known as dolomitisation. Alternately, it may precipitate directly from hydrothermal fluids.
  3. Calcite Crystallisation
  4. Calcite often forms later, as calcium-rich solutions enter cavities, vugs, or fractures within the dolomite host. Its growth may reflect changes in temperature, mineral saturation, or fluid chemistry.
  5. Layered Mineralisation
  6. The two minerals together represent a dynamic environment shaped over millions of years, with multiple mineralisation stages producing the contrasting crystal habits seen in this specimen.

Depending on the locality within the USA, trace minerals such as siderite, pyrite, or quartz may accompany dolomite–calcite clusters, contributing subtle colouration or inclusions.

Aesthetic Appeal and Display Qualities

This Dolomite and Calcite crystal specimen is visually captivating due to its complementary mineral pairings. Dolomite’s soft, earthy tones create the perfect backdrop for calcite’s brighter, more reflective crystals. The interplay of textures—dolomite’s smooth or curved faces against calcite’s sharper, more translucent points—gives the piece excellent depth and visual dimension.

Its neutral yet elegant colour palette makes it suitable for display in:

  • Mineral collections
  • Home and office décor
  • Educational and geological exhibits
  • Meditation or natural history settings

The mineral association offers both textural complexity and aesthetic harmony, making it a memorable and highly collectible display piece.

Scientific and Collector Significance

Dolomite and calcite help geologists interpret the geochemical history of their environment, including:

  • Fluid pathways
  • Temperature changes
  • Mineral replacement reactions
  • Sedimentary basin evolution

Collectors value specimens like this for:

  • Multi-mineral associations
  • Well-defined crystal habits
  • Natural contrast between mineral species
  • Geological significance tied to classic U.S. mineral localities

High-quality dolomite–calcite combinations remain popular among both novice and advanced collectors.

Authenticity and Quality Assurance

All of our crystals are fully natural, authentic specimens. This Dolomite and Calcite USA Crystal comes with a Certificate of Authenticity, and the images provided show the exact specimen you will receive. It is a beautifully balanced, mineralogically rich piece that offers both aesthetic appeal and scientific interest—an excellent addition to any crystal or mineral collection.

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