Natural Stilbite with Apophyllite Crystal Cluster – 30 g

This natural Stilbite with Apophyllite specimen features a dense cluster of clear to translucent Apophyllite crystals surrounding a prominent cream-white to pale yellow Stilbite formation. The Apophyllite crystals display sharp natural faces, excellent transparency, and bright vitreous luster, while the central Stilbite growth adds a soft, fibrous texture and subtle pearly appearance. The combination of contrasting crystal habits creates a distinctive and attractive natural zeolite specimen.

Product Details

• Mineral: Stilbite with Apophyllite

• Formation: Natural zeolite crystal cluster

• Color: Clear, white, translucent, cream and pale yellow

• Crystal Habit: Prismatic to tabular Apophyllite crystals with radiating Stilbite aggregates

• Weight: 30 g

• Size: 7 × 4 cm

• SKU: MTX-B157-N839

• Condition: Natural mineral specimen

Mineral Features

• Natural Stilbite crystal growth

• Associated Apophyllite crystals

• Prominent cream to pale yellow Stilbite formation

• Clear to translucent Apophyllite crystals

• Well-defined natural crystal faces

• Bright vitreous luster

• Soft pearly texture on Stilbite growth

• Dense intergrown zeolite formation

• Unique one-of-a-kind natural specimen

• Suitable for mineral collectors and crystal enthusiasts

• Ideal for display and collection

Geological Note

Stilbite and Apophyllite commonly occur together in cavities and fractures of volcanic rocks. Stilbite typically forms radiating, fibrous, fan-shaped, or sheaf-like aggregates, while Apophyllite commonly develops as clear to translucent prismatic or tabular crystals. These minerals form from mineral-rich hydrothermal fluids circulating through volcanic rock cavities over geological time.

Please Note: Natural mineral specimens may naturally contain variations in color, crystal formation, transparency, texture, inclusions, fractures, cavities, chips, luster, and matrix. Each specimen is naturally formed and may differ slightly from the photographed piece.