AAA Diamond Apophyllite on Blue Chalcedony – High Clarity Terminations
AAA Diamond Apophyllite on Blue Chalcedony – High Clarity Terminations
A high-grade diamond apophyllite cluster set on blue chalcedony, featuring sharp, glassy terminations with strong natural reflectivity and internal light play.
This piece shows a standout primary apophyllite crystal with well-defined faces and visible growth striations, surrounded by smaller secondary crystals across the matrix. The base consists of blue chalcedony, providing contrast between the microcrystalline silica and the larger, fully formed apophyllite crystals.
The clarity and structure here place this firmly in AAA grade, with excellent transparency, clean edges, and strong geometric formation.
✨ Key Features
📍 AAA grade apophyllite with high clarity
📍 Prominent main crystal with sharp terminations
📍 Secondary crystal cluster growth across matrix
📍 Natural vertical striations on crystal faces
📍 Blue chalcedony base (microcrystalline quartz)
📍 Strong light reflection and internal sparkle
📏 Dimensions
Size: 4 cm x 3 cm
Weight: 41 grams
🔬 Geological & Scientific Notes
Apophyllite Group
Chemical Formula: KCa₄Si₈O₂₀(F,OH)·8H₂O
Mineral Class: Phyllosilicate
Crystal System: Tetragonal
Hardness: 4.5–5 (Mohs)
Lustre: Vitreous (highly reflective)
Transparency: Transparent to translucent
Apophyllite commonly forms in volcanic cavities, where mineral-rich fluids allow slow crystal growth, producing well-defined geometric structures.
Chalcedony Base
Chemical Formula: SiO₂
Structure: Microcrystalline quartz
Provides the host surface for crystal growth
🧪 Formation Insight
This combination forms when:
Silica-rich fluids create a chalcedony base
Later mineral-rich fluids deposit apophyllite
Crystals grow into open space, forming sharp terminations
🧼 Care
Handle with care (apophyllite is softer than quartz)
Avoid knocks and pressure on crystal points
Clean gently with water and a soft brush
Do not use harsh chemicals
💬 Honest Note
This is a natural, untreated specimen.
Minor inclusions, internal fractures, and matrix features are part of natural crystal growth and not defects.