Red cap Amethyst

Red cap Amethyst

£25.00
Sale price  £25.00 Regular price 
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Red cap Amethyst

Red cap Amethyst

£25.00
Sale price  £25.00 Regular price 

This striking red cap amethyst specimen showcases a bold contrast between deep iron-rich surface coatings and underlying amethyst crystal growth. The upper section features a rugged, earthy red matrix, while the lower areas reveal clusters of purple amethyst crystals, creating a visually dynamic piece that highlights multiple stages of mineral formation within a single specimen.


Left in its natural, unpolished state, this piece preserves the raw textures and structural complexity formed over time. The contrast between the iron-stained quartz and the amethyst crystal pockets gives it a layered, almost brecciated appearance, making it both scientifically interesting and visually distinctive from every angle.


🔍 Key Features
Material: Natural amethyst (quartz) with iron-rich “red cap” formation
Formation: Natural crystal cluster with iron oxide coating and secondary amethyst growth
Colour: Deep red/brown surface tones with purple amethyst and milky quartz
Crystal Habit: Macrocrystalline quartz with druzy crystal formations
Finish: Natural, unpolished exterior
Shape: Irregular natural formation with exposed crystal pockets


📏 Dimensions
Approx. Size: 5.6cm x 4.8cm
Weight: 56 grams


🌍 Geological & Scientific Notes
Red cap amethyst forms when quartz crystals are exposed to iron-rich environments during or after their growth. The red to brown surface layer is typically caused by iron oxides (such as hematite or limonite) that coat or infuse the outer crystal surfaces.
In this specimen, the underlying amethyst formed first within a cavity or vein under hydrothermal conditions, where silica-rich fluids slowly crystallised into quartz. Later exposure to iron-bearing solutions or surrounding sediment introduced the distinctive red coating, creating the “red cap” effect.


The presence of both amethyst crystal growth and iron-rich matrix in one piece provides a clear example of multi-stage mineral formation. Quartz crystallises in the trigonal system, typically forming hexagonal prisms, though here the growth is expressed as clustered and intergrown crystals.


🧪 Mineral Information
Mineral: Quartz (Amethyst variety)
Formula: SiO₂
Colour: Purple (amethyst) with red/brown iron oxide coating
Cause of Colour: Iron impurities and natural irradiation (amethyst); iron oxides (red cap)
Lustre: Vitreous (glassy) on crystal faces, earthy on matrix
Transparency: Transparent → translucent → opaque (matrix)
Streak: White
Hardness: 7 (Mohs)
Fracture: Conchoidal
Cleavage: None
Density: ~2.65
Crystal System: Trigonal
Habit: Crystal clusters and druzy formations
Formation: Hydrothermal veins and cavities with secondary mineralisation
Common Locations: Brazil, India, Uruguay, Madagascar
🔬 Optical
Refractive Index: ~1.54–1.55


✨ Extras
Distinct contrast between iron-rich outer layer and amethyst crystals
Displays multiple stages of mineral growth in one specimen
Natural textures and crystal pockets create visual depth


📦 Condition
Natural, unpolished specimen
Surface texture and irregularities typical of raw mineral formation
Minor inclusions and matrix material present
No visible dyeing or artificial enhancement


🧼 Care Instructions
Handle carefully to protect delicate crystal points
Clean gently with a soft brush (avoid soaking)
Avoid harsh chemicals
Store separately to prevent damage to crystal surfaces

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