Serpentine Slice Polished Natural Green Serpentine Mineral Specimen Display Genuine Serpentine Slice Crystal Stone UK Seller


£ 12.60

SERPENTINE SLICE – POLISHED NATURAL GREEN MINERAL SPECIMEN

This Serpentine slice is a genuine natural mineral specimen, carefully cut and
polished to reveal its distinctive colour patterns and internal structure. Selected for its visual appeal and quality, this piece highlights the unique characteristics of Serpentine in a refined, display-ready form. The exact specimen shown in the photographs is the one you will receive, ensuring complete confidence in your purchase.

Each piece includes a Certificate of Authenticity lifetime guarantee card, confirming it as a genuine specimen. Full sizing details are available in the listing photographs for accurate scale reference.

MINERAL COMPOSITION AND CLASSIFICATION

Serpentine is not a single mineral but a group of magnesium iron silicate minerals, typically represented by the formula (Mg,Fe)₃Si₂O₅(OH)₄. The group includes species such as antigorite, chrysotile, and lizardite, which form under similar geological conditions.

These minerals are part of the phyllosilicate class and are characterised by their layered संरचना, which contributes to their smooth texture and ability to be polished. Serpentine generally has a Mohs hardness of around 2.5 to 4, depending on the specific variety.

COLOUR, PATTERN AND SURFACE FINISH

Serpentine is widely recognised for its rich green colour, which can range from pale yellow-green to deep forest tones. This slice may display variations in colour, including mottled, veined, or marbled patterns caused by differences in mineral composition and formation processes.

The polished surface enhances these natural patterns, giving the stone a smooth, slightly waxy to silky lustre. Subtle inclusions and internal textures are often visible, adding depth and individuality to each piece.

These visual features make Serpentine slices particularly appealing for collectors and as decorative display items.

GEOLOGICAL FORMATION AND ORIGIN ENVIRONMENT

Serpentine forms through the metamorphic alteration of ultramafic rocks such as peridotite and dunite, in a process known as serpentinisation. This occurs when water interacts with magnesium-rich minerals at relatively low temperatures, transforming the original rock into serpentine minerals.

This process is commonly associated with tectonic environments such as subduction zones and oceanic crust, where mantle الصخور are exposed to water and undergo chemical परिवर्तन. Over time, these reactions produce the characteristic اللون and texture seen in Serpentine.

The resulting material can occur in massive forms, veins, or layered संरचनाएँ, which are later cut and polished into slices for display.

STRUCTURE, SHAPE AND DISPLAY APPEAL

The slice format reveals the internal structure of the stone, allowing the natural patterns and colour variations to be viewed across a flat surface.

• Smooth polished slice highlighting natural patterns

• Rich green tones with unique marbling and veining

• Ideal for display, коллекtion, or decorative use

• Each specimen is completely individual in appearance

Serpentine has been traditionally associated with connection to nature in symbolic contexts, making it a popular decorative choice while remaining valued primarily for its geological properties.

AUTHENTICITY AND PRODUCT DETAILS

• Genuine natural Serpentine slice specimen

• Includes Certificate of Authenticity lifetime guarantee card

• Carefully selected individual piece

• Exact specimen shown in photos will be received

This Serpentine slice offers a combination of natural geological formation and polished presentation, making it a distinctive and attractive addition to any mineral collection or display.