| Specimen Details | |
|---|---|
| Weight | 41.83 oz’s – 1.186 kg’s |
| Dimensions | 6.364″ x 4.644″ long/wide (16.165 x 11.798 cm’s) |
| Country of Origin | Meig Mine, Sichuan province, China |
Epidote Included With Lepricosite Phantom Amethyst Quartz Cluster
NZD $415.00
SKU: Q4214
This Amethyst Quartz Cluster is Natural and has inclusions of Epidote and Lepricosite Phantoms inside it!! The color is truly amazing, and the form is nothing short of perfection. Some of the points have elestial like form! White background photo has been included to help better the display the color and shape of this piece. This specimen is in excellent condition.
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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Amethyst Clusters Origins & Background
Amethyst Clusters are among the most recognized and widely collected forms of Amethyst. Rather than growing as single points, clusters consist of multiple crystal points sharing a common base, creating a radiating crystalline surface.
The appearance of Amethyst clusters varies significantly depending on geological conditions, growth environment, and locality. Factors such as available space, mineral concentration, temperature stability, and fluid movement all influence point size, density, color zoning, and overall structure.
Some clusters form as dense carpets of small points, while others develop fewer but larger, well-terminated crystals. Color can range from pale lavender to deep violet, sometimes with zoning, phantoms, or smoky undertones.
Major sources of Amethyst clusters include Brazil, Uruguay, Zambia, Madagascar, and Russia. Each region is known for distinct characteristics — for example, Uruguay is often associated with deeper color saturation, while Brazil commonly produces larger clusters with lighter hues.
Because clusters form in open cavities, their growth is influenced by the shape and size of the host rock, resulting in highly individual specimens with natural variation and character.
Amethyst Clusters Geological Information
Amethyst clusters form when silica-rich fluids enter open cavities within volcanic or metamorphic rock and crystallize over long periods. Multiple crystal points nucleate simultaneously on the cavity walls, growing inward toward the center.
The trigonal crystal structure of Quartz causes crystals to grow as six-sided prisms with pointed terminations. When conditions allow many growth sites to remain active at once, clusters develop rather than isolated points.
Variations in fluid chemistry, temperature, and mineral availability can cause differences in point size, clarity, and coloration within a single cluster. Growth interruptions may result in features such as phantoms, growth lines, or uneven point heights.
The characteristic purple color of Amethyst results from trace iron within the Quartz lattice combined with natural irradiation and subsequent geological heating.
Common Geological Occurrences
- Volcanic basalt cavities and geodes
- Hydrothermal Quartz veins
- Metamorphic rock environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Amethyst Clusters Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to strong sunlight or heat may cause some Amethyst clusters to fade over time. Indirect or filtered light is recommended for display.
✋ Handling:
While Quartz is relatively hard, cluster points can chip if struck. Lift clusters from the base rather than by individual points.
🧼 Cleaning:
Clean using lukewarm water and a soft brush to remove dust between points. Avoid harsh chemicals or ultrasonic cleaners.
📦 Storage & Display:
Place clusters on stable surfaces where they are unlikely to be bumped. Padding beneath the base can help prevent accidental movement.
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Epidote Included Quartz Origins & Background
Epidote Included Quartz—often simply referred to as Epidote Quartz—is a Quartz crystal that contains natural inclusions of the green mineral Epidote. These inclusions may appear as wispy internal veils, sprays, or moss-like growths within the Quartz, creating a strong visual impression of vitality and movement.
This combination is found in several parts of the world, including Brazil, Pakistan, India, Alaska (USA), and select African localities. Each source produces distinctive inclusion styles, ranging from fine internal filaments to bold, clearly defined Epidote crystals encased within Quartz.
Because Quartz amplifies whatever it contains, Epidote Included Quartz has long been referred to in crystal traditions as “The Enhancer.” The Quartz acts as a magnifier, intensifying the energetic signature of Epidote while also making it more accessible and usable.
Natural Epidote inclusions should not be confused with surface coatings or artificially introduced materials. Authentic Epidote Quartz shows inclusions fully enclosed within the Quartz growth structure.
Epidote Included Quartz Geological Information
Epidote Included Quartz is composed primarily of silicon dioxide (SiO₂) with inclusions of Epidote, a calcium aluminum iron silicate mineral. Both minerals form in metamorphic and hydrothermal environments, often under conditions of pressure, heat, and fluid movement.
Epidote inclusions typically form first, with Quartz later growing around them, sealing the green mineral within the crystal. This growth sequence is what gives Epidote Quartz its characteristic “encased” appearance.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz with Epidote inclusions |
| Chemical Formula | SiO₂ + Ca₂(Al,Fe)₃(SiO₄)₃(OH) |
| Crystal System | Trigonal (Quartz) / Monoclinic (Epidote) |
| Hardness (Mohs Scale) | 7 (Quartz), 6–7 (Epidote) |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Natural green Epidote inclusions |
Why Inclusions Matter
Inclusion-bearing Quartz crystals are often valued for the way internal minerals interact with the Quartz matrix. In the case of Epidote Quartz, this interaction creates a synergistic structure where amplification and direction occur simultaneously.
Epidote Included Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Generally durable, but crystals with prominent internal fractures or fine terminations should be handled gently.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, especially for specimens with visible internal fractures. Dry thoroughly.
☀️ Light:
Light-stable under normal conditions.
📦 Storage & Display:
Store separately to protect clarity and surface luster. Suitable for grids, body placement, and regular handling.
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Phantom Quartz Origins & Background
Phantom Quartz is one of the most symbolically powerful growth forms in the Quartz family. These crystals contain visible internal “phantoms” — ghost-like images of earlier stages of the crystal’s own development preserved within the body of the crystal itself.
Each phantom represents a pause, interruption, or shift during the crystal’s growth cycle. Rather than halting development permanently, the Quartz resumes growth and carries the record of that moment forward. Because of this, Phantom Quartz has long been associated with evolution, resilience, and the ability to move forward after disruption.
Phantom Quartz occurs in many Quartz varieties, including Clear Quartz, Smoky Quartz, Amethyst, and included forms. Each variety adds its own nuance to the phantom’s expression and influence.
Phantom Quartz Geological Information
Phantom Quartz forms when a crystal’s growth is temporarily interrupted by the introduction of another substance or a change in environmental conditions. This interruption leaves a visible layer on the crystal’s termination before growth resumes, encapsulating that earlier stage within the final crystal.
Common Phantom-Causing Materials
- Chlorite: often green phantoms
- Hematite: red, brown, or metallic phantoms
- Clay or sediment: pale or earthy-toned phantoms
- Thermal changes: color-zone phantoms (often Smoky or Amethyst)
3D Phantom Formation
The most powerful and visually striking phantoms are referred to as 3D phantoms. In these specimens, the interrupting material fully coats the termination, creating a complete three-dimensional “crystal within a crystal.”
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Phantom growth) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Visible internal growth stages |
Phantom Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle gently to protect internal clarity and phantom visibility. Lift from the base where possible.
🧼 Cleaning:
Brief water rinsing is generally safe. Avoid prolonged soaking if fractures or inclusions are present.
☀️ Light:
Protect Smoky and Amethyst Phantom Quartz from prolonged intense sunlight.
📦 Storage & Display:
Display with good lighting to reveal internal phantoms. These crystals benefit from being seen and consciously worked with.
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Included Quartz Origins & Background
Included Quartz refers to Quartz crystals that contain other minerals trapped within them during growth. These inclusions may appear as needles, clouds, veils, phantoms, sprays, plates, threads, or granular deposits, each reflecting the geological conditions present at the time of formation.
Common inclusions include Chlorite, Rutile, Tourmaline, Titanium-bearing minerals, Iron oxides, and many others. Each specimen is inherently unique, as the timing, chemistry, and environment of growth determine the inclusion’s shape, placement, and density.
Included Quartz occurs worldwide, with notable localities in Brazil, Madagascar, Pakistan, India, the United States, and parts of Africa. Because inclusions record a snapshot of the crystal’s growth history, many collectors consider Included Quartz to be a visual and geological record of Earth’s evolving conditions.
Included Quartz Geological Information
Included Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, consistent with all Quartz varieties. The defining feature is the presence of one or more foreign minerals incorporated during crystal growth.
Inclusions form when Quartz grows in environments where other minerals are suspended in hydrothermal fluids. As the Quartz crystal develops, these minerals may become trapped internally rather than being excluded or deposited on the surface. Growth may continue around the inclusion, fully enclosing it within the crystal body.
In some cases, inclusions outline earlier growth stages, forming phantoms. In others, needle-like or fibrous inclusions such as Rutile or Tourmaline grow simultaneously with the Quartz, creating complex internal structures.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz with mineral inclusions |
| Chemical Formula | SiO₂ (host crystal) |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 (host crystal) |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Internal mineral inclusions |
Structural Significance
From a geological perspective, inclusions provide valuable insight into the temperature, pressure, and chemistry present during crystal formation. Each Included Quartz specimen is effectively a natural archive of its growth environment.
Included Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Included Quartz is generally durable, but internal fractures or delicate inclusions may be present. Handle gently and avoid sudden impacts.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, especially for crystals with visible fractures or porous inclusions. Dry thoroughly.
☀️ Light:
Most Included Quartz is light-stable. Some iron-rich inclusions may darken slightly with prolonged intense sunlight.
📦 Storage & Display:
Store separated from harder specimens to prevent chipping. Display securely to protect terminations.
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Amethyst Origins & Background
Amethyst has been valued across cultures for thousands of years for its rich violet coloration and its association with clarity, balance, and composure. The name Amethyst originates from the Greek word amethystos, meaning “not intoxicated,” reflecting an ancient belief that the stone helped maintain clear thinking and moderation.
Historically, Amethyst was considered a stone of royalty and spiritual authority. It adorned crowns, rings, and ceremonial objects in Ancient Greece and Rome and later throughout medieval Europe. Its purple color was rare and strongly associated with wisdom, restraint, and elevated status.
Significant Amethyst deposits are found in Brazil, Uruguay, Zambia, Madagascar, and Russia. Each locality produces crystals with distinctive growth habits, color zoning, and internal features, making provenance an important consideration for collectors and natural crystal enthusiasts.
Amethyst’s coloration develops through trace amounts of iron within the Quartz lattice combined with natural irradiation and geological heating over extended time periods. This process often creates layered growth zones that contribute to the depth and visual complexity seen in higher-quality specimens.
Some Amethyst crystals display structural growth features such as internal windows, phantoms, record keepers, and time-link faces. These are physical indicators of crystal formation traits and are valued for both the insight they provide into natural growth processes and to possible Metaphysical propoties.
Amethyst Geological Information
Amethyst is a violet variety of Quartz (Silicon Dioxide – SiO₂) that typically forms within cavities, veins, and geodes in igneous and metamorphic rock environments. Crystals usually grow as hexagonal prisms with pointed terminations.
The purple coloration results from trace iron incorporated into the Quartz structure combined with natural irradiation from surrounding rock. Subsequent geological heating stabilizes these color centers, producing hues that range from pale lavender to deep royal purple.
Amethyst commonly forms in volcanic environments, particularly within gas cavities of cooling basalt flows. Over millions of years, silica-rich fluids crystallize slowly, allowing layered growth and the development of internal zoning and structural features.
Common Geological Occurrences
- Volcanic basalt cavities and geodes
- Hydrothermal Quartz veins
- Metamorphic rock environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Amethyst Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to intense sunlight or heat may cause some Amethyst specimens to fade over time. For long-term preservation, extended placement in direct sunlight is best avoided.
✋ Handling:
Amethyst is relatively durable, but sharp impacts can chip crystal points or edges. Handle specimens gently, especially clusters and terminated points.
🧼 Cleaning:
Clean Amethyst using lukewarm water and a soft brush. Avoid harsh chemicals, ultrasonic cleaners, or abrasive tools, which may damage crystal surfaces.
📦 Storage & Display:
Prolonged exposure to intense sunlight or high heat may cause some Amethyst specimens to fade over time.
For long-term preservation, extended placement in direct sunlight is best avoided. Indirect light or filtered natural light is ideal for display. This preserves color while still allowing the crystal’s natural beauty to be appreciated.
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