Daisy Bed Gypsum UK Natural Crystal Cluster Mineral Specimen 50-80mm


£ 8.40

DAISY BED GYPSUM – NATURAL CRYSTAL CLUSTER FROM THE UK (50–80MM)

This Daisy Bed Gypsum specimen from the United Kingdom is a genuine natural
mineral piece, carefully selected for its distinctive radiating crystal formation and collector appeal. Measuring approximately 50–80mm (full sizing please see photo), this is a carefully chosen specimen, and the photograph provided shows an example of the actual piece you will receive. Each item includes a Certificate of Authenticity lifetime guarantee generic card, confirming it as a genuine mineral specimen.

MINERAL SPECIES & CHEMICAL COMPOSITION

Gypsum is a hydrated calcium sulfate mineral with the chemical formula:

CaSO₄·2H₂O

It crystallises in the monoclinic crystal system and forms in a wide variety of habits, including tabular crystals, fibrous masses, and radiating clusters. Daisy Bed Gypsum is named for its characteristic “daisy-like” formations, where crystals radiate outward in flattened rosette patterns.

Gypsum has a hardness of 2 on the Mohs scale, making it a relatively soft mineral. It can be easily scratched and should be handled with care to preserve its natural crystal surfaces.

CRYSTAL STRUCTURE, FORM & VISUAL FEATURES

Daisy Bed Gypsum is recognised for its attractive radial clusters that resemble the petals of a flower. These formations may display:


• Pale white to cream colouring
• Soft grey or buff tones depending on locality
• Radiating, bladed crystal growth
• Satin to pearly lustre
• Delicate, layered crystal surfaces

The 50–80mm size provides a substantial display presence, allowing the intricate crystal structure to be appreciated clearly. Each specimen is naturally unique, with variations in petal density, cluster shape, and overall symmetry.

GEOLOGICAL FORMATION & UK LOCALITY

Gypsum forms in evaporite environments, typically when mineral-rich saline waters evaporate in restricted basins such as lagoons or inland seas. As water evaporates, dissolved calcium and sulfate ions combine to crystallise gypsum.

Daisy Bed Gypsum from the UK is associated with sedimentary evaporite deposits formed millions of years ago. These deposits developed in conditions where repeated evaporation cycles allowed gypsum to crystallise in open spaces within sediment layers.

Over geological time, compaction and exposure revealed these distinctive rosette-like clusters. Associated minerals in evaporite sequences may include anhydrite, halite, and other sulfate minerals.

SIZE, PRESENTATION & AUTHENTICITY


• Mineral: Gypsum
• Chemical Formula: CaSO₄·2H₂O
• Crystal System: Monoclinic
• Origin: United Kingdom
• Size: Approximately 50–80mm (please refer to photo for full sizing reference)
• Authenticity: Includes Certificate of Authenticity lifetime guarantee generic card

This specimen is ideal for mineral collectors, sedimentary geology enthusiasts, educational displays, or as a natural decorative piece. The distinctive daisy-like crystal formation makes it especially attractive for cabinet collections.

COLLECTING & TRADITIONAL ASSOCIATIONS

Gypsum has been valued historically for both industrial and ornamental uses, but naturally formed crystal clusters such as Daisy Bed Gypsum are particularly appreciated by collectors for their unusual growth patterns.

In spiritual traditions, gypsum is traditionally associated with clarity and focus; these interpretations are cultural rather than scientific. From a mineralogical perspective, its appeal lies in its evaporite origin, hydrated calcium sulfate composition, and striking radial crystal habit.

A genuine Daisy Bed Gypsum specimen from the UK, carefully chosen for quality and supplied with certificate of authenticity, offering a classic evaporite mineral formation in an impressive 50–80mm display size.