Diamond Apophyllite Cluster on Blue Chalcedony Druzy Matrix

Diamond Apophyllite Cluster on Blue Chalcedony Druzy Matrix

£69.00
Sale price  £69.00 Regular price 
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Diamond Apophyllite Cluster on Blue Chalcedony Druzy Matrix

Diamond Apophyllite Cluster on Blue Chalcedony Druzy Matrix

£69.00
Sale price  £69.00 Regular price 

Diamond Apophyllite Cluster on Blue Chalcedony Druzy Matrix

Overview

This visually striking specimen features a dense cluster of sharp, glassy apophyllite crystals growing across a softly contoured blue chalcedony matrix. The contrast between the highly reflective, transparent crystal faces and the fine-grained, matte druzy surface creates a layered texture that catches light from every angle.

The apophyllite forms in tightly packed cubic-to-pyramidal terminations, often referred to as “diamond apophyllite” due to their bright, mirror-like reflections. Beneath and around this growth, the chalcedony displays a smooth, botryoidal surface coated in microcrystalline quartz, producing a subtle sparkle across the blue-grey base.

Key Features

Minerals: Apophyllite, Chalcedony (Quartz)

Formation:

Secondary apophyllite crystal growth over pre-existing chalcedony (botryoidal silica surface)

Colour:

Colourless to transparent apophyllite

Blue-grey chalcedony matrix

Crystal System:

Apophyllite: Tetragonal

Lustre:

Apophyllite: High vitreous (glass-like)

Chalcedony: Waxy to micro-sparkling druzy

Transparency:

Apophyllite: Transparent to translucent

Chalcedony: Opaque to translucent

Dimensions

Weight: 165 grams

Size: 7 cm x 4.6 cm

Geological & Scientific Notes

This specimen formed in a multi-stage hydrothermal environment:

Chalcedony Formation (SiO₂):

Silica-rich fluids deposited microcrystalline quartz, creating the smooth, rounded (botryoidal) base structure.

Druzy Development:

A later phase of silica crystallisation formed a fine layer of microscopic quartz crystals, giving the surface its subtle sparkle.

Apophyllite Growth:

Under changing chemical conditions, apophyllite crystals nucleated and grew on top of the chalcedony surface. The sharp, well-defined crystal faces and internal clarity indicate relatively stable growth conditions during this final stage.

The contrast between microcrystalline chalcedony and larger apophyllite crystals clearly shows two distinct mineral growth environments preserved in one piece.

Why This Piece Stands Out

Strong contrast between glassy crystals and soft druzy matrix

Dense coverage of high-reflectivity apophyllite terminations

Clean blue chalcedony base with even druzy coating

Visible multi-stage formation (great educational value)

Balanced display shape — sits naturally

Care & Handling

Fragile crystal edges — handle with care

Avoid water and cleaning chemicals

Use a soft brush or air blower to remove dust

Store separately to prevent scratching

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